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  • 1980-1984  (36)
  • 1960-1964  (93,914)
  • 1963  (93,914)
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Year
  • 1
    facet.materialart.
    Unknown
    (Table 8, page 38) Spectrographic analyses of deep sea manganese nodules from the Pacific and Indian Oceans (1963)
    PANGAEA
    In:  Supplement to: Hewett, DF; Fleischer, Michael; Conklin, Nancy (1963): Deposits of the manganese oxides; supplement. Economic Geology, 58(1), 1-51, https://doi.org/10.2113/gsecongeo.58.1.1
    Details
    Publication Date: 2024-07-01
    Description: In an earlier paper by two of the authors the conclusion was reached that the 33 recognized species of oxides of Mn could be separated into 3 groups: 1) those which appeared to be persistently supergene in origin, 2) those which appeared to be persistently hypogene, and 3) those which were supergene in some localities and hypogene in other localities. When that paper was written, there were available about 250 X-ray diffraction analyses of mineral specimens, also 35 complete and about 150 partial chemical analyses. The conclusions of that paper were based upon the interpretation of the geologic conditions under which these specimens occurred. Late in the preparation of that paper, it seemed worthwhile to make numerous semiquantitative analyses of specimens, largely from 9 western [U.S.A] states, selected carefully from 5 groups of geologic environments, in the hope that the frequency and percentages of some elements might be distinctive of the several geologic groups. For this purpose, 95 specimens were selected from the 5 groups, as follows: 19 specimens interpreted as supergene oxides by the geologists who collected them, 35 specimens of hypogene vein oxides, 22 specimens of Mn-bearing hot spring aprons, 9 specimens of stratified oxides, and 10 specimens of deep-sea nodules. The spectrographic analyses here recorded indicate that a group of elements - W, Ba, Sr, Be, As, Sb, Tl, and Ge - are present more commonly, and largely in higher percentages, in the hypogene oxide than in the supergene oxides and thus serve to indicate different sources of the Mn. Also, the frequency and percentages of some of these elements indicate a genetic relation of the manganese oxides in hypogene veins, hot spring aprons, and stratified deposits. The analyses indicate a declining percentage of some elements from depth to the surface in these 3 related groups and increasing percentages of some other elements. It is concluded that some of the elements in deep-sea nodules indicate that sources other than rocks decomposed on the continents, probably vulcanism on the floors of the seas, have contributed to their formation.
    Keywords: ALB-13; ALB-173; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-173; ALBTR-4662; Aluminium; Barium; Beryllium; Bismuth; Boron; Calcium; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; Dredge, chain bag; Dredge, rock; DRG; DRG_C; DRG_R; DWBD1; DWHD47; Elevation of event; Event label; FANB01BD; FANBD-25D; FANFARE-B; Horizon; Indian Ocean; Iron; Lanthanum; Latitude of event; Lead; LGO-BT-57 or VM14 SBT57 (SIO); Longitude of event; Magnesium; MDPC02HO-MP-025F-2; MDPC02HO-MP-033K; MIDPAC; Molybdenum; MPC-25F-2; MPC-33K; NAGA; NAGA10C; Neodymium; Nickel; Niobium; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; Photo/Video; Potassium; PV; Sample ID; Scandium; Silicon; Sodium; Spectrographic analysis; Spencer F. Baird; Stranger; Strontium; Thallium; Titanium; V14; V14-57RD; Vanadium; Vema; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 296 data points
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  • 2
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    Unknown
    (Table II, page 668-669) Distribution of elements between minerals soluble in 1M Hydroxylamine hydrochloride (Reducible); in 1m HCL (Acid-soluble) and in the insoluble residue of manganese nodules (1963)
    PANGAEA
    In:  Supplement to: Arrhenius, Gustaf (1963): Pelagic sediments. In: Hill, M.N. (Ed.) The Earth Beneath the Sea, History, The Sea - Ideas and Observations on Progress in the Study of the Seas, Wiley J, New York, U.S.A., 3, 655-727, hdl:10013/epic.46253.d001
    Details
    Publication Date: 2024-07-01
    Description: Attempts to classify pelagic sediments have been based either on appearance and composition, or on the ultimate origin of the components. In particular it appears feasible to distinguish minerals which crystallized in sea-water from those which formed in magmas, in hydrothermal solution, or by weathering under acidic conditions. It is the case of iron and manganese oxide mineral aggregates which constitute one of the major types of rock encountered on the ocean floor; according to Menard (unpublished) about 10% of the pelagic area of the Pacific is covered by such nodules. The nodules consist of intimately intergrown crystallites of different minerals among those identified, besides detrital minerals and organic matter, are opal, goethite, rutile, anatase, barite, nontronite, and at least three manganese oxide minerals of major importance. Arrhenius and Korkisch (1959) have attempted to separate from each other the different minerals constituting the nodules, in order to establish the details of their structure and the localization of the heavy metal ions. The results demonstrate (Table II) that copper and nickel are concentrated in the manganese oxide phases concentrated in the reducible fraction. Cobalt, part of the nickel and most of the chromium are distributed between these and the acid-soluble group of the non-manganese minerals, dominated by goethite and disordered FeOOH.
    Keywords: Acid soluble, total; ALB-13; ALB-2; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-2; ALBTR-4711; ALBTR-4721; Barium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; DRG; DWBD4; DWHD72; Event label; Horizon; Identification; Iron; Lanthanum; Lead; Manganese; Molybdenum; Nickel; Niobium; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Northern_Holiday; North-West Pacific Ocean; NTHL02HO-010PH; NTHL-10; Optical spectrographic analysis; Pacific Ocean; Reducible total; Residual; Scandium; Spencer F. Baird; Strontium; Thorium; Titanium; Wired profile sonde; WP; Ytterbium; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 386 data points
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  • 3
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    Unknown
    (Table 1, page 10) Cobalt and chromium content in manganese nodules from various locations (1963)
    PANGAEA
    In:  Supplement to: Arrhenius, Gustaf; Bonatti, Enrico (1963): Neptunism and vulcanism in the ocean. Progress in Oceanography, 3, 7-22, https://doi.org/10.1016/0079-6611(65)90005-4
    Details
    Publication Date: 2024-07-01
    Description: The origin of authigenic minerals on the ocean floor has been extensively discussed in the past with emphasis on two major processes; precipitation from solutions originating from submarine eruptions, and slow precipitation from sea water of dissolved elements, originating from weathering of continental rocks. It is concluded that in several marine authigenic mineral systems these processes overlap. A diagnostic principle is suggested, permitting a qualitative or semiquantitative discrimination between marine authigenic minerals crystallized from dissolved species, which have spent a long time in solution on the one hand, and the same minerals generated from solutions, near their source on the other. Extensive data are available for the manganese and iron oxide minerals forming manganese nodules. It is indicated on the basis of their composition and structure that many of the nodules found in the vicinity of the continents are made up essentially of manganese derived from continental weathering. In contrast to this group, all of the nodules found in the Pacific area of submarine vulcanism display the criteria for rapid precipitation near the source of solution. The distribution of barium minerals over the deep ocean floor is discussed.The same diagnostic principle is suggested for application to these solids, in order to discriminate between baryte and harmotome crystallized near the source of barium- rich, acidic vulcanites, and the same minerals formed from continental solution with passage through the biosphere. In the case of the authigenic aluminosilicates it is found that many of the framework elements (Si and particularly Al) have low passage time through solution, and the major fraction of these elements is consequently removed from solution in the vicinity of the eruptive source materials. Extensive modification of the crystal structures, however, takes place over long periods of time, adding particularly cations from sea water, and probably to some extent silica from siliceous fossils, which on their decay on the ocean floor appear to contribute to the silicate framework of growing zeolites. The marked fractionation of the rare earth ions between coexisting phases is pointed out, with discussion of the potential use of this phenomenon to indicate the processes of formation. The use of the hafnium/zirconium ratio as a tracer for the igneous source type is suggested, and the application of ideally imperfect tracers to establish the varying relative importance of volcanic versus halmeic source of marine minerals is discussed in general.
    Keywords: ALB-13; ALB-2; Albatross (1882-1921); Albatross1899-1900; Albatross1904-1905; ALBTR-13; ALBTR-2; ALBTR-4711; ALBTR-4721; Chromium; Cobalt; DEPTH, sediment/rock; DNWB0ABD; DOWNWIND-B1; DOWNWIND-H; Dredge; DRG; DWBD4; DWHD72; Event label; Horizon; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; Spencer F. Baird
    Type: Dataset
    Format: text/tab-separated-values, 42 data points
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  • 4
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    Unknown
    Bomenboek voor Suriname (1963)
    In:  Mededelingen van het Botanisch Museum en Herbarium van de Rijksuniversiteit te Utrecht vol. 200 no. 1, pp. 1-312
    Details
    Publication Date: 2024-02-22
    Description: The aim of this book is to provide all persons interested in the tree and wood species of Suriname with a simple means to find the name of a given tree. To this end two dichotomous keys have been drawn up with the help of punched cards prepared from studies of conserved material and field observations made by the authors. The first one makes use only of vegetative characters of leaves and twigs and a few saliant features of the bark, disregarding flower and fruit characters mostly used in floras. The second key is based on the anatomy of the wood as far as this can be observed with a good 10 X or sometimes 20 X magnifying hand-lens.\nIn the \xe2\x80\x9cInleiding\xe2\x80\x9d the terminology applied in each of the keys and in the descriptions is explained and elucidated by sketch drawings. After the keys follows the descriptive part in which the families are treated in alphabetical sequence as are the genera within each family and species within a genus. In general the taxa are taken in the same circumscription as in the \xe2\x80\x9cFlora of Suriname\xe2\x80\x9d; where a different name is accepted, following recent views, the name in the Flora has been added in brackets. Attention is drawn to the Mimosaceae and Papilionaceae which are treated here on account of their close relationship as two major subdivisions of Leguminosae, the latter name being used as general family heading.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 5
    Monograph available for loan
    Monograph available for loan
    Tektonika Sibiri; Tom 2, Tektonika Krasnojarskogo kraja (1963)
    Novosibirsk : Izdatel'stvo Sibirskogo otdelenija AN SSSR
    Associated volumes
    Details Availability
    Call number: AWI G3-24-95571-2
    In: Tektonika Sibiri, Tom 2
    Type of Medium: Monograph available for loan
    Pages: 385 Seiten , Illustrationen , 1 Kartenbeilage, 1 Errata
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 2
    Language: Russian
    Note: Kartenbeilage unter dem Titel: Tektoničeskaja Karta : Central'nogo sektora Sovetskoj Arktiki 〈1: 5 000 000〉 , CONTENTS Foreward Tectonics of Siberian Platform and Its Borderland Bounding Structures of Siberian Platform / Yu. A. Kosygin, I. V. Luchitski History of Development of Structure of North-Western Part of Siberian Platform / Ya. I. Polkin Tectonic Structure of Western Part of Siberian Platform / N. V. Drenov To the Problem of Structure of Pre-Yenisei Marginal Part of Siberian Platform / A. S. Kirillov History of Tectonic Development of South-Western Part of Siberian Platform and Rybinsk Depression / M. A. Zharkov On Peculiarities of Tectonics of Rydinsk Depression / A. I. Anatoljeva Some Relations of Siberian Platform with Its Borderlands / D. I. Musatov Tectonics of Yenisei Ridge / G. I. Kirichenko Structural-Facial Zones of Riphean and Lower Cambrian of Yenisey Ridge and North-Western Part of Eastern Sayan / M. A. Semikhatov On Tectonics of Southern Part of Yenisei Ridge / Yu. Parfenov Tectonics of Bakhta and Ucham River Basin / N. S. Malich On Mechanism of Horst-Formation in Tungussk Syneclise / L. M. PIotnikov On Forms of Structural Connections of Siberian Platform and West-Siberian Plate / K. V. Bogolepov Structure of Basement of Eastern Margin of West-Siberian Plate in Connection with Its General Tectonic Zoning / V. N. SoboIevskaya Structure of Folded Basement of Minusa Intermontane Downwarp and South-Eastern Part of West-Siberian Plate by Geophysical Data / V. S. Surkov Some New Information on Structures of Cretaceous the Eastern Margin of West-Siberian Plate / Yu. F. Pogonya-Stefanovich Tectonics of Sayano-Altai Folded Region Main Principles of Tectonic Classification of Depressions and Downwarps of Orogenic Stage of Development of Eastern Part of Sayano-Altai Region / B. N. Krasilnikov, G. M. Volontey Some Peculiarities of Deep Fractures on the Example of Folded Regions on the South of Krasnoyarsk Territory / D. I. Musatov Principal Features of Tectonics and History of Geologic Development of Eastern Sayan / A. L. Dodin On Tectonic Zonation of Eastern Sayan / V. B. Lyatski Main Features of Tectonics of Eastern Part of Eastern Sayan / O. P. AIexeyeva, V. D. Titov Some Problems of Tectonics of North-Western Part of Eastern Sayan / K. V. Radugin Tectonics of Proterozoic Era of East-Sayan (Derbinsk) Anticlinorium / A. A. SaveIyev Tectonics of Pre-Cambrian Blocks of Eastern Sayan and Khamar-Daban and Their Absolute Age / V. Ya. Khiltova, L. P . Nikitina, I. P. Buzikov, N. A. Avdontsev Main Features of Tectonics of Near-Sayan Structural-Facial Zone / P. I. Shames Problems of Tectonic Development of South-Western Part of Eastern Sayan and Adjacent Regions of Minusa Depressions / E. A. Shneider, B. P. Zubkus Tectonics of Minusa Depressions and of Their Basement / A. A. Mossakovski Some Features of Structure and Development of Western Sayan / L. P. Zonenshain On «Butt-End» (T-form) Conjugation of Structures of Western Sayan, Western Tuva and Mountain Altai / A. M. Borovikov Some Features of Tectonic Development of Territory of Tuva during Late Cambrian and Lower Paleozoic / G. A. Kudryavtsev Main Types of Development of Large Structures of Tuva Intermontane Downwarp / G. M. Volontey Tectonics of Central Sector of Soviet Arctic Tectonic Map of the North of Siberia at the Scale of 1:2 500 000 / I. P. Atlasov The Map of Neotectonics of the North of Siberia at the Scale of 1:2 500 000 / M. T. Kiryushina Tectono-Magmatic Stages of Development of Taimyr-Severnaya Zemlya Folded Region and Connection of Commercial Minerals with them / V. A. Vakar, B. Kh. Egiazarov Pre-Cambrian Basement of Taimyr and Its Deformation during Formation of Folded Region / Yu. E. Pogrebitski Tectonics and Metallogeny On Principles of Tectonic Zoning on the Example of Southern Regions of Krasnoyarsk Territory (in Connection with Problems of Metallogeny) / V. V. Bogatski On Structural-Metallogenic Zoning of Eastern Siberia and the North-East of USSR / S. V. Levchenko Tectonic Control of Trappean Ore-Bearing Intrusions of North-Western Part of Siberian Platform / A. M. ViIenski, G. I. Kavardin Tectonics of Igarka-Norilsk Region and Ore-Controling Structures / G. D. MasIov Laws Governing Localization of Ore Deposits in Norilsk-Igarka Region / V. N. Egorov Internal Structure of Early Caledonian Downwarp of Northern Part of West Sayan and Peculiarities of Its Magmatism / Sh. D. Kurtseraite Index of Regional Tectonic Nomendature Summary , СОДЕРЖАНИЕ Предисловие Тектоника Сибирской платформы и структуры ее обрамления Структуры ограничения Сибирской платформы / Ю. А. Косыгин, И. В. Лучицкий История развития структуры северо-западной: части Сибирской платформы / Я. И. Полькин Тектоническое строение западной части Сибирской платформы / Н. В. Дренов К вопросу о структуре приенисейской окраины Сибирской платформы / А. С. Кириллов История тектонического развития юго-западной части Сибирской платформы и Рыбинской впадины / М. А. Жарков Об особенностях тектоники Рыбинской впадины / А. И. Анатольева Некоторые вопросы соотношения Сибирской платформы с ее обрамлением / Д. И. Мусатов Тектоника Енисейского кряжа / Г. И. Кириченко Структурно-фациальные зоны рифея и нижнего кембрия Енисейского кряжа и северо -западной части Восточного Саяна / М А. Семихатов О тектонике южной части Енисейского кряжа / Ю. И. Парфенов Тектоника бассейна рек Бахты и Учами / Н. С. Малич О механизме горстообразования в Тунгусской синеклизе / Л. М. Плотников О формах структурной связи Сибирской платформы и Западно-Сибирской плиты / К. В. Боголепов Строение фундамента восточной окраины Западно-Сибирской плиты в связи с ее общим тектоническим районированием / В. Н. Соболевская Строение складчатого фундамента Минусинского межгорного прогиба и юго-восточной части Западно-Сибирской плиты по геофизическим данным / В. С. Сурков Некоторые новые данные по структурам мела на восточной окраине Западно-Сибирской плиты / Ю. Ф. Погоня-Стефанович Тектоника Саяио-Алтайской складчатой области Основные принципы тектонической классификации впадин и прогибов орогенного этапа развития восточной части Саяно-Алтайской области / В. Н. Красильников, Г. М . Волонтэй Некоторые особенности глубинных разломов на примере складчатых областей юга Красноярского края / Д. И. Мусатов Основные черты тектоники и истории геологического развития Восточного Саяна / А. Л. Додин К тектоническому районированию Восточного Саяна / В. Б. Ляцкий Основные черты тектоники восточной части Восточного Саяна / О. П. Алексеева, Д. В. Титов Некоторые вопросы тектоники северо-западной части Восточного Саяна / R. В. Радугин Тектоника протерозоя Восточно-Саянского (Дербинского) антиклинория / А. А. Савельев Тектоника докембрийских глыб Восточного Саяна и Хамар-Дабана и их абсолютный возраст / В. Я. Хильтова, Л. П. Никитина, И. П. Бузиков, Н. А. Авдонцев Основные черты тектоники Присаянской структурно-фациальной зоны / И. П. Шамес Вопросы тектонического развития юго-западной части Восточного Саяна и прилегающих районов Минусинских впадин / Е. А. Шнейдер, Б. П. 3убкус Тектоника Минусинских впадин и их фундамента / А. А. Моссаковский Некоторые черты структуры развития Западного Саяна / Л. П. Зоненшайн О торцовом сопряжении структур Западного Саяна, Западной Тувы и Горного Алтая / А. М. Боровиков Некоторые черты тектонического развития территории Тувы в позднем докембрии и нижнем палеозое / Г. А. Кудрявцев Основные типы развития крупных структур Тувинского межгорного прогиба / Г. М. Волонтэй Тектоника центрального сектора Советской Арктики Тектоническая карта севера Сибири масштаба 1:2 500 000 / И. П. Атласов Карта новейшей тектоники севера Сибири масштаба 1:2 500 000 / М. Т. Кирюшина Тектоно-магматические этапы развития Таймыро-Североземельской складчатой области и связь с ними полезных ископаемых / В. А. Вакар, Б. Х. Егиазаров Докембрийский фундамент Таймыра и его деформации в период образования снладчатой области / Ю. Е. Погребицкий Тектоника н металлоrения О принципах тектонического районирования на примере южных районов Красноярского края (в связи с проблемами металлогении) / В. В. Богацкий О структурно-металлогеническом районировании Восточной Сибири и Северо-Востока СССР / С. В. Левченко Тектонический контроль трапповых рудоносных интрузий северо-западной части Сибирской платформы / А. М. Виленский, Г. И. Кавардин Тектоника Игарско-Норильского района и рудоконтролирующие структуры / Г. Д. Маслов Закономерности размещения рудных месторождений в Норильско-Игарском районе / В. Н. Егоров Внутренняя структура раннекаледонского прогиба северной части Западного Саяна и особенности его магматизма / Ш. Д. Курцерайте Указатель региональных тектонических терминов Краткое содержание сборника Резюме , In kyrillischer Schrift , In russischer Sprache mit englischer Zusammenfassung
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  • 6
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    Echinostomatoidea, Notocotylata und Cyclocoelida (Trematoda, Digenea, Redioinei) aus V\xc3\xb6geln des Berliner Tierparks (1963)
    In:  Bijdragen tot de dierkunde vol. 33 no. 1, pp. 37-60
    Details
    Publication Date: 2024-01-12
    Description: Die Subsubclassis Redioinei ODENING, 1960 innerhalb der Unterklasse Digenea (VAN BENEDEN, 1858) wurde in zwei fr\xc3\xbcheren programmatischen Systementw\xc3\xbcrfen provisorisch, teilweise in Anlehnung an LA RUE (1957), gegliedert (ODENING 1960, 1961b). Ich halte es heute f\xc3\xbcr angebracht, die in jeder Beziehung bestimmbaren und festumrissenen Trematodengruppen als Ordnungen zu bewerten, wie es z.B. auch in den neueren Systemen der Cestoden der Fall ist. Diese Auffassung hat nicht nur praktische Vorz\xc3\xbcge, sondern sie befreit auch die unbestritten einheitlichen Gruppen aus hypothetischen Verbindungen. Ist es doch ein Nachteil der meisten neueren Einteilungsversuche der Digenea, da\xc3\x9f phylogenetische Hypothesen in Form von Ordnungen etabliert wurden, die nach Lage der Dinge je nach Auffassung der Autoren recht verschieden zusammengesetzt waren, w\xc3\xa4hrend die wirklich einheitlichen Gruppen mit den Zwischenkategorien (Unterordnung, \xc3\x9cberfamilie) bedacht wurden. Die Redioinei umfassen nach der neuen Wertung folgende selbst\xc3\xa4ndige Ordnungen (alphabetische Reihenfolge): 1. Allocreadiida Odening, 1960 2. Azygiida (La Rue, 1957) stat. et nom. emend. 3. Clinostomatida (Allison, 1943) stat. et nom. emend. 4. Cyclocoelida (La Rue, 1957) stat. et nom. emend. 5. Fasciolida (Poche, 1926) stat. et char. emend. 6. Hemiurida (Poche, 1926) stat. emend. 7. Opisthorchiida (La Rue, 1957) char. emend. 8. Paramphistomatida (Poche, 1926) stat. et char. emend.\nDie Ordnung Didymozoida (Poche, 1926) ist von den Redioinei auszuschlie\xc3\x9fen, da sie m\xc3\xb6glicherweise nicht zu den Digenea geh\xc3\xb6rt (siehe Baer & Joyeux 1961).
    Repository Name: National Museum of Natural History, Netherlands
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  • 7
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    Mycotic Infections occurring during an eight Year Period at the Chicago Zoological Park, Brookfield, Illinois (1963)
    In:  Bijdragen tot de dierkunde vol. 33 no. 1, pp. 83-85
    Details
    Publication Date: 2024-01-12
    Description: We present below listings of mycotic infections occurring in vertebrates at the Chicago Zoological Park from September, 1954 to December, 1962. Most of the identifications were made by Dr. Tilden and Mrs. Getty from cultures of the fungi involved. Except for a few cases noted among the mammals, the findings were made from necropsy material.\nIt is interesting to note the wide variety and numbers of birds with mycotic infections in contrast to the few findings in mammals and reptiles. Our interest in mycotic infections during this period led to the publication of the eight articles listed at the end of this paper, and the reader is referred to these for additional information on some of the cases. These studies have included research on the endotoxins of Aspergillus flavus and fumigatus, the description of a new species of Microsporum, and case reports of mycoses in animals that were previously unrecorded.
    Repository Name: National Museum of Natural History, Netherlands
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  • 8
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    Enteric Infections occuring during an eight Year Period at the Chicago Zoological Park Brookfield, Illinois (1963)
    In:  Bijdragen tot de dierkunde vol. 33 no. 1, pp. 87-88
    Details
    Publication Date: 2024-01-12
    Description: The bacteriological examinations of abnormal stools, irrespective of the apparent seriousness of the illness, is particularly important in a zoological park where it is difficult to apply measures to keep out possibly infected wild, non-resident animals and mechanical carriers, such as flies, cockroaches, etc. One obvious instance of the initiation of an epidemic by nonresident animals was the occurrence of infection with Salmonella newport among the animals in the pachyderm house. The first case in an elephant occurred about a month after S. newport had been isolated from the blood of a skunk found dead in the park. Prompt diagnosis of the first case and examination of the stools of other animals in the same building led to the discovery of further infections before symptoms occurred in the other animals. Suitable antibiotic therapy was instituted, but the first animal, an adult female elephant, was lost. All the pathogenic enteric bacteria isolated were identified as S. newport.\xc2\xb9) A fatal infection of a young forest horse with Salmonella typhimurium occurred following a long period of rainy weather leading to standing water in the enclosure. Contamination of the water by wild rats is believed to have been the most likely source of infection in this instance. No secondary cases occurred.
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  • 9
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    Typhaceae (1963)
    In:  Flora of the Netherlands Antilles vol. 1 no. 2, pp. 87-88
    Details
    Publication Date: 2024-01-12
    Description: Monoecious, marsh or aquatic plants, with perennial, creeping rootstocks and erect, terete stems. Leaves alternate, linear or strap-shaped, sheathing at the base, flat, slightly convex on the back. Flowers unisexual, densely crowded in simple, compact, cylindric spikes. Male inflorescence terminal and separated from the female spike or contiguous to it; each spike subtended by spathaceous, usually fugacious, bracts and divided at intervals by smaller caducous bracts. Perianth consisting of bristles. Male flowers with 3, rarely 1\xe2\x80\x947 stamens; the filaments free or connate; the anthers linear or oblong, basifixed, 2-celled, with longitudinal dehiscence; the connective produced beyond the cells in a conical, carnose acumen; pollen grains simple or compound. Female flowers with a one-celled, superior, stipitate and fusiform ovary; the ovule solitary and anatropous; the style elongate, slender, erect; the stigma ligulate, spathulate, lanceolate or linear. Among the female flowers many sterile ones with clavate tips. Fruit minute, stipitate, fusiform or ellipsoid, with a membranaceous or coriaceous pericarp, splitting longitudinally. Seed subcylindric or narrowly ellipsoid; the testa membranaceous; albumen farinaceous. Embryo cylindric, straight. About 8 species in one genus, widely distributed in temperate and tropical regions.
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  • 10
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    Gramineae (1963)
    In:  Flora of the Netherlands Antilles vol. 1 no. 2, pp. 121-203
    Details
    Publication Date: 2024-01-12
    Description: Annual or perennial herbs, rarely shrubby. Leaves alternate, consisting of sheath, ligule and blade. Sheaths envelopping the stem, usually with free margins; ligule borne at the mouth of the sheath, membranaceous or a rim of hairs; blades mostly elongate, flat, convolute or terete, parallel-veined. Inflorescence spicate, racemose or paniculate, bearing spikelets which consist of a shortened axis (rhachilla) and two to many scales. The two lowest scales (glumes) empty, rarely wanting; the following scales (lemmas) bearing in their axil an usually enclosed prophyll (palea) and a perfect or reduced flower. Lemma, palea and flower together forming the floret. Perfect flower consisting of 2\xe2\x80\x943 hyaline or fleshy lodicules, usually 3 (1\xe2\x80\x946) stamens and a pistil. Stamens with at anthesis rapidly elongating, filiform or ribbon-like filaments with 2-celled anthers, opening with longitudinal splits. Ovary superior, 1-celled; ovule one, anatropous; styles usually 2(1\xe2\x80\x943) with plumose stigmas. Fruit a caryopsis (i.e. the pericarp adnate to the seed) with mealy endosperm, rarely a nut, a berry or an utricle with free pericarp. Embryo small, at the base of the side opposite the hilus. About 4000 species in 500 genera; of world-wide distribution.
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    Florae Malesianae Precursores XXXIV. Notes on some genera of Celastraceae in Malaysia (1963)
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 12 no. 1, pp. 31-38
    Details
    Publication Date: 2024-01-12
    Description: There is a great diversity of opinion regarding the interpretation of the genera and some species in the former Hippocrateaceae. If one reads the comprehensive and detailed revision of the New World Hippocrateaceae by A. C. Smith (Brittonia 3, 1940, 341\xe2\x80\x94555), one may have an impression of it. For example, A. C. Smith in his monotypic genus Hemiangium, under H. excelsum, has united species which were recognized as belonging to three different genera by Miers; he has also limited Hippocratea L. to a single species, H. volubilis L., and placed more than 40 names of species and varieties in the synonymy of it.\nA detailed review of the history and generic delimitation of the family Hippocrateaceae has already ably been summarized and discussed by A. C. Smith in the above mentioned publication. I shall make only a brief account of those works which contain genera, species, or discussions related to the Malaysian flora.
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  • 12
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    Microthamnion strictissimum in Nederland (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 10, pp. 118-118
    Details
    Publication Date: 2024-01-12
    Description: In 1962 Microthamnion strictissimum Rabenhorst was found twice in the Netherlands, whereas it had not been recorded before from that country. It was collected in a shallow oligotrophic pool (Leersumse Veld, Eerste Plas, prov. Utrecht) as well as in an also shallow but eutrophic one (Herenvennen, Bergen, prov. Limburg).
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  • 13
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    Korte mededelingen (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 14, pp. 164-164
    Details
    Publication Date: 2024-01-12
    Description: Tetramyxa parasitica Goebel. In Gorteria 1, no. 12, 1963, p. 138 vermeldt C. den Hartog deze, gallen op Ruppia veroorzakende, schimmel voor de eerste maal voor ons land, en wel van enige inlagen op Schouwen en Noord-Beveland. Bij het doorzien van het Ruppia-materiaal van het Rijksherbarium en de Kon. Ned. Botanische Vereniging bleek, dat zich in laatstgenoemde collectie een plant van Ruppia maritima met Tetramyxa-gallen bevindt, verzameld in 1868 door F. Holkema \xe2\x80\x9ein een oude doorbraak in de Kuil op Texel\xe2\x80\x9d. v. O. en R.\nErica scoparia L. nu ook op Texel. Door de heer W. A. Luynenberg werd, samen met de heer G. J. de Haan en op diens aanwijzing, op Texel aan de Hoornse Slag op 27 augustus 1963 materiaal verzameld van bovengenoemde soort, die daar in een tweetal exemplaren voorkomt. De planten groeiden op enigszins gestoord terrein. Ook hier is het weer, evenals op Terschelling, voorlopig onmogelijk een bevredigende verklaring van het voorkomen te geven; het wordt er alleen maar nog raadselachtiger door. v. O. en R.
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  • 14
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    Over de standplaats van Cornus suecica in Oostfriesland (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 9, pp. 100-105
    Details
    Publication Date: 2024-01-12
    Description: This paper deals with the habitat of Cornus suecica in pine and spruce plantations near Wilhelmshaven (N.W. Germany), one of its southernmost localities in Europe. The table of records represents a transect from open pinewood to a dense, mixed pine-spruce-wood. All the shrubs, as well as the herbs and bryophytes of groups 1 obviously prefer the light wood stand, whereas those of groups 2 and especially 3 are most abundant and fertile in dense shade.\nCornus suecica and Trientalis europaea show an opposite behaviour with regard to light, and so do the two closely allied Dryopteris species, D. austriaca and D. spinulosa.
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    Een Nieuw-Zeelandse Epilobium in Nederland verwilderd (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 9, pp. 93-95
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    Publication Date: 2024-01-12
    Description: Epilobium inornatum Melville, a species native in New Zealand, and cultivated in rock-gardens, has established itself in a number of parks and gardens in the Netherlands since 1932.
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  • 16
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    Montia fontana L. in een stadstuintje (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 11, pp. 131-132
    Details
    Publication Date: 2024-01-12
    Description: The authors mention the occurrence of a terrestrial form of Montia fontana subsp. rivularis in a garden at Leiden. As this form much resembles typical specimens of subsp. fontana the differences between the two subspecies are discussed.
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  • 17
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    Spiranthes cernua (L.) Rich. op het terrein \xe2\x80\x9eDe Wolf\xe2\x80\x9d te Haren, Gr (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 9, pp. 97-98
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    Publication Date: 2024-01-12
    Description: A few specimens of Spiranthes cernua (L.) Rich., a native of Canada and the United States, were found in a wild state in the Botanical Garden \xe2\x80\x9cDe Wolf\xe2\x80\x9d at Haren, prov. Groningen, in 1961 and 1962. As S. cernua was never cultivated there, and unintentional introduction by men is rather unlikely, the authors suppose that seeds of the species, which is sometimes cultivated in aquaria and terraria, may have found their way to the garden.
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  • 18
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    Antillean Cyanophyceae from salt-pans and marine localities (1963)
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 12 no. 1, pp. 45-56
    Details
    Publication Date: 2024-01-12
    Description: A number of samples from salt-pans collected by J. Rooth in Bonaire and by Miss T. M. Emeis in Curasao were handed over to the author for identification. Fr\xc3\xa9my (1941) has published a list of Cyanophyceae collected by Wagenaar Hummelinck in Bonaire, Klein Bonaire and Cura\xc3\xa7ao in 1930 and 1932. Among the last mentioned collection there were samples from the same salt-pans in Bonaire, where also J. Rooth did his collecting. It is interesting to compare both results.\nDr Fr. Drouet had the kindness to procure some identifications for this part as well as for part II.
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    On \xe2\x80\x98Cordyceps capitata\xe2\x80\x99 (1963)
    In:  Persoonia - Molecular Phylogeny and Evolution of Fungi vol. 2 no. 4, pp. 477-482
    Details
    Publication Date: 2024-01-12
    Description: Cordyceps capitata does occur in the Netherlands, but is shown to be far less common than C. canadensis, a species not previously recorded. A brief review of the European literature demonstrates that practically all descriptions refer to Cordyceps canadensis. Both species are described and their differences indicated.
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  • 20
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    Boekbespreking (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 12, pp. 144-144
    Details
    Publication Date: 2024-01-12
    Description: Sinds vier jaar geeft het Gustav Fischer Verlag in Stuttgart een botanische bibliografie uit, de Excerpta Botanica, waarvan de \xe2\x80\x9eSectio B. Sociologica\xe2\x80\x9d onder hoofdredactie staat van professor R. T\xc3\xbcxen, Stolzenau, en in welks redactie voorts als Nederlanders Dr. W. C. de Leeuw en Dr. V. Westhoff zitting hebben. Het zal de lezers van Gorteria ongetwijfeld interesseren dat in deze serie nu ook een plantensociologische bibliografie van Nederland verschenen is, samengesteld door V. Westhoff [Bd. 3 (2), 1961, p. 81\xe2\x80\x94160 en Bd. 3 (3), 1961, p. 161\xe2\x80\x94220]. Het is een zeldzaam volledige bibliografie van 1433 titels, waarvan de waarde nog verhoogd wordt door een auteursindex (404 auteurs). Hij bestrijkt de periode 1935\xe2\x80\x941959 en sluit dus aan op de \xe2\x80\x9eBibliographia phytosociologica II. Neerlandia\xe2\x80\x9d van W. C. de Leeuw. Niet opgenomen zijn artikelen van Nederlandse auteurs over vegetaties in het buitenland of in onze voormalige en huidige overzeese gebiedsdelen. De artikelen zijn gerangschikt volgens onderwerpen en binnen deze in chronologische volgorde. Het begrip plantensociologie is zeer ruim genomen. Onder het hoofdstuk \xe2\x80\x9ePflanzensoziologie und Floristik\xe2\x80\x9d zal ook de florist menige waardevolle literatuuropgave vinden.\nEr moge nog op gewezen worden dat in de Excerpta behalve over bepaalde landen ook algemene bibliografie\xc3\xabn over bepaalde facetten van de plantensociologie verschijnen, waarvan o.a. die over de relatie vegetatie \xe2\x80\x94 bodem, areaalkaarten van plantengezelschappen, successieonderzoek, epifyten, determinatietabellen voor plantengezelschappen en statistische plantensociologie reeds verschenen zijn. Ook hierin vindt men uiteraard Nederlandse literatuur vermeld.
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    Tetramyxa parasitica, een gal op Ruppia (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 12, pp. 138-140
    Details
    Publication Date: 2024-01-12
    Description: Tetramyxa parasitica Goebel, a Plasmodiophoracean parasite, has been found on Ruppia spiralis L. ex Dum. in three places in the south-western part of the Netherlands, viz. in the Flaauwersinlaag and in the Weversinlaag on the island of Schouwen and in the \xe2\x80\x9einlaag\xe2\x80\x9d near the Torenpolder on the island of Noord-Beveland. The parasite forms more or less spherical galls on the stems (fig. 1, b), the leaves and even on the inflorescences (fig. 1, a) of the host. The galls seem to be formed only under special ecological conditions. Although the localities on Schouwen were visited every month since June 1959 the galls were only found for the first time in 1962. Salinity may perhaps be a factor involved in the sporadic appearance of these galls. In 1962 the maximum salinity in the ponds was below 10\xe2\x80\xb0 Cl\xe2\x80\x99; in the preceding years it was considerably higher.
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    Pyrola uniflora in Oostfriesland (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 10, pp. 109-110
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    Publication Date: 2024-01-12
    Description: The author describes a locality of Pyrola uniflora in N.W. Germany, 50 km from the Dutch frontier, probably its westernmost station in the plains of Central Europe. A vegetation record of this locality is given.
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  • 23
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    Korte mededelingen (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 9, pp. 107-108
    Details
    Publication Date: 2024-01-12
    Description: Phyllitis scolopendrium (L.) Newm. weer op Yoorne. Nadat alle oude groeiplaatsen verdwenen waren, hetzij door natuurlijke successie, hetzij door droge zomers of door padverbreding, vond de botanisch analyst D. van der Laan, werkzaam aan het Biol. Station te Oostvoorne tegen de noordmuur van zijn huis in de gemeente Rockanje een klein ex., dat zich in de loop van 1961 goed ontwikkelde en de winter 1961-\xe2\x80\x9962 goed doorkwam. Hij verzocht de eigenaresse de slechte muur bij het plantje niet te repareren, wat deze toezegde. Rockanje. C. Sipkes Crambe maritima L. Op 5 september 1960 vond ik op het strand bij Westenschouwen tegen de duinvoet een niet bloeiende plant, die ik voor bovengenoemde soort gehouden heb, omdat ze er net uitzag als de zeekool, die ik vroeger aan de kust van Zuid-Engeland en Bretagne aantrof. In de hoop, dat de plant de winter zou overleven en het volgende jaar in bloei zou komen, heb ik hem laten staan. Helaas heb ik hem later niet meer teruggevonden, doordat het duin daar in het najaar afgeslagen was. Serooskerke (Schouwen). Jac. Viergever
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    Die Gattungen der Myriangiales (1963)
    In:  Persoonia - Molecular Phylogeny and Evolution of Fungi vol. 2 no. 4, pp. 421-475
    Details
    Publication Date: 2024-01-12
    Description: Die Myriangiales sind ascolocul\xc3\xa4re Ascomyceten mit bitunicaten Asci und lassen sich durch Zwischenformen mit den Dothiorales verbinden. Bei ihnen entstehen die Asci im Innern von Fruchtk\xc3\xb6rpern einzeln zerstreut und sind kugelig oder breit keulig. Die 21 anerkannten Gattungen werden schl\xc3\xbcsself\xc3\xb6rmig dargestellt und anschliessend einzeln besprochen. Die Vertreter der Gattungen Myriangium und Angatia wachsen auf Schildl\xc3\xa4usen oder sind Saprophyten. Parasiten auf h\xc3\xb6heren Pflanzen werden in die Gattungen Elsino\xc3\xab, Bitancourtia, Anhellia, Diplotheca und Butleria gestellt. Bei den Vertretern der Gattungen Uleomyces, Cookella und Pycnoderma handelt es sich um Hyperparasiten auf blattbewohnenden Kleinpilzen. Die Arten der Gattungen Molleriella, Saccardinula, Micularia, Xenodium und Hyalotheles entwickeln ihre Fruchtk\xc3\xb6rper nur auf Blattdr\xc3\xbcsen oder Blatthaaren. Die Vertreter von Dictyonella, Saccardia, Byssogene und Allosoma zeichenen sich durch ein oberfl\xc3\xa4chliche Rasen bildendes Mycel aus. Auf diesem entwickeln sich die discoiden Ascomata. Von den von den Myriangiales auszuschliessenden Gattungen geh\xc3\xb6ren Annajenkinsia, Protoscypha und Myriangiella zu den Dothiorales, Ascostratum und Myxotheca zu den Lichenes, Ascosorus zu den inoperculaten Discomycetes und Piedraia wahrscheinlich zu den Pseudosphaeriales. Eine neue Art wird als Angatia brasiliensis Bezerra & v. Arx beschrieben. Die Typusarten mehrerer in die Synonymie versetzter Gattungen werden umbenannt.
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  • 25
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    Tragopogon porrifolius L. X T. pratensis L. in Friesland (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 9, pp. 99-100
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    Publication Date: 2024-01-12
    Description: Up to now hybrids of Tragopogon porrifolius L. and the subspecies pratensis and orientalis of T. pratensis L. were only known in the Netherlands from botanical gardens where they came up spontaneously between the parents. The author mentions the first wild occurrence in our country of the hybrid of T. porrifolius and T. pratensis subsp. pratensis along a dike near Wommels, prov. Friesland, where it was discovered by one of his pupils, Mr. Posthuma. Moreover a survey of the distribution of T. porrifolius in Friesland is given.
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  • 26
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    De geschiedenis van Rosa dumalis Bechst. in Nederland (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 14, pp. 153-155
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    Publication Date: 2024-01-12
    Description: The authors give a survey of the occurrence of Rosa dumalis Bechst. in the Netherlands and discuss the differences between this species and R. canina L.
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  • 27
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    Aanwinsten voor de Nederlandse adventief-flora, 4 (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 10, pp. 113-117
    Details
    Publication Date: 2024-01-12
    Description: This paper contains acquisitions to the adventitious flora of the Netherlands, mainly from the year 1962. 1. Cerastium dichotomum L. (fig. 1, d), a native of the Mediterranean region and of W. Asia, was found at Oostmahorn, prov. Friesland, near a harbour made for the reclamation of the Lauwerszee. 2. Arabis rosea DC., most likely introduced in the dunes near Bloemendaal, prov. N. Holland, with pheasant-food. The species is indigenous in Central and S. Italy, and in Sardinia and Sicily. Differences between this species and the closely related A. muralis Bertol. are discussed. 3. Pavonia urens Cav. (fig. 1, a-c). The var. hirsuta (Hochst. ex Ulbr.) Brenan of this tropical African species was found as an alien near a wool-mill at Tilburg, prov. N. Brabant. 4. Allium atropurpureum Waldst. & Kit. from the northern part of the Balkan Peninsula, like Arabis rosea probably introduced with pheasant-food, was found in the dunes of the intake of the Amsterdam Waterworks near Vogelenzang, prov. N. Holland.
    Repository Name: National Museum of Natural History, Netherlands
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  • 28
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    Aanwinsten voor de Nederlandse adventief-flora, 5 (1963)
    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 1 no. 12, pp. 141-143
    Details
    Publication Date: 2024-01-12
    Description: 1. Navarretia squarrosa (Eschsch.) Hook. & Arn. is mentioned here in addition to our last paper on the Netherlands adventitious flora, published in Gorteria 1, no. 10, 1963, p. 113\xe2\x80\x94117. The species was found in 1962 near Joure, prov. Friesland, and was most probably introduced with bird-seed. 2. All Dutch specimens formerly named Erodium chium (Burm. f.) Willd. and E. cygnorum Nees appear to belong to the Australian E. crinitum Carolin. This species was found as an alien near the wool-mills at Tilburg, prov. N. Brabant and along the river Meuse near Meers, Grevenbicht, and Itteren, prov. Limburg. In the last named localities it was most probably introduced from the wool-factories along the Vesdre in Belgium. Differences between E. cygnorum and E. crinitum are discussed.
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  • 29
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    Cornelis Andries Backer (1874\xe2\x80\x941963). In Memoriam (1963)
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 12 no. 1, pp. 1-4
    Details
    Publication Date: 2024-01-12
    Description: On February 22nd, 1963, the Rijksherbarium suffered a severe loss by the passing away of its honorary officer, since 1945, Dr C. A. Backer, at the age of 88 years. His death came by no means unexpected. He had been ailing and largely bed-ridden for nearly two years; while his mental capacities remained unaffected almost up till the last day, his body suffered from an increasing weakness of the limbs, an increasing deafness and loss of eyesight. Not suffering from pain, he endured the weakening of his body with courage and resignation, token of his indomitable spirit.\nAs two biographies, one provided with a full bibliography \xc2\xb9), and an obituary note \xc2\xb2) are published elsewhere, the accent of the present obituary lies largely on the way in which his work became involved with that of the Rijksherbarium.
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  • 30
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    A correction (1963)
    In:  Persoonia - Molecular Phylogeny and Evolution of Fungi vol. 2 no. 4, pp. 476-476
    Details
    Publication Date: 2024-01-12
    Description: In Persoonia 2: 389. 1962, the new combination Hydnellum piperatum (Coker) Maas G. was proposed, but it escaped my attention that the basionym, Sarcodon piperatus, had not been provided with a Latin description, rendering the new combination invalid. The following diagnosis, taken from Coker\xe2\x80\x99s description and augmented with a few notes of my own, should validate the name.
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  • 31
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    A Comparative Study of the Soil Fauna in forests and cultivated land on sandy soils in Suriname (1963)
    In:  Studies on the Fauna of Suriname and other Guyanas vol. 6 no. 1, pp. 1-42
    Details
    Publication Date: 2024-01-12
    Description: 1. In the coastal area of Suriname the soil and surface fauna were studied in various types of agricultural land, and compared with the fauna in the adjacent forests. 2. In primeval forest the soil macroarthropods are less numerous than in secondary forest (Formicidae excluded). They range generally from 2,000 to 3,000 per m2 in the primeval forest and from 3,000 to 4,500 per m2 in the secondary forest. In cultivated land the numbers range in general from 1,500 to 2,500 per m2.\nIn recently reclaimed land the numbers of soil macroarthropods are very small and amount to 15-30% of those in the adjacent forests. In the older agricultural soils they range from 50 up to 130% of the numbers of arthropods in forest soil. 3. The surface fauna is best developed in the secondary forest on shell ridges. In primeval forest the surface fauna is richer in the border zone than in the inner part. In cultivated land most \xe2\x80\x9cforest species\xe2\x80\x9d decrease strongly in numbers, but they are replaced by \xe2\x80\x9copen field species\xe2\x80\x9d. The numbers of surface arthropods (Formicidae, Scolytidae and Pheropsophus excluded) in the cultivated land are generally 20-40% less than in the adjacent forests. 4. On account of their much more frequent occurrence in forests the following groups were distinguished as forest inhabitants: Isopoda, Diplopoda, Dermaptera, and Staphylinidae. The following may be designated as open-field inhabitants: Lycosidae, Gryllotalpidae, Elateridae and Pheropsophus (Carabidae). 5. Of the eleven most frequent indigenous diplopod species, five were exclusively found in forest land; another five were also taken in cultivated land, but in much smaller numbers; and one species only was more numerous in the fields than in the forests. \xe2\x80\x93 Three introduced species were found in greater numbers or exclusively in cultivated land. One of these was only taken near Paramaribo, probably the centre of introduction. 6. In the cultivated land the number of ants active on the surface of the soil exceeds that in the adjacent forests by up to 900%. The ant population in the soil of cultivated land is generally only 10- 30% of that in forest soils. 7. Three of the 171 species accounted for about one third of all the ants collected. These occurred in nearly all fields and forest plots, and apparently have the widest ecological range. The qualitative composition of the ant fauna in the forests appeared to be much richer than that in the fields. 8. The microarthropod population (Acari and Collembola) in the cultivated land was surprisingly large and averaged 80% of that in the forest land. 9. There were no indications that the soil fauna (macroarthropods as well as microarthropods) is consistently smaller in the Surinam soils than in the Dutch soils. However, the greater production of plant material in the tropics and the absence of litter accumulation point to a more rapid decomposition, caused by a greater biological activity at the higher tropical temperatures.
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  • 32
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    Life History of the Red-legged Thrush (Mimocichla plumbea ardosiacea) in Puerto Rico (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 14 no. 1, pp. 1-40
    Details
    Publication Date: 2024-01-12
    Description: To the ornithologist the West Indies offer an assortment of field problems. In an area where it is unlikely that new species of birds will be discovered, and where the life histories of only a handful of birds are known, concentrated study of individual life histories becomes of prime importance.\nThis paper represents the third formal life history study of a resident Puerto Rican bird and the second of a passeriform. BIAGGI\xe2\x80\x99S work (1955) on the Puerto Rican race of the Bananaquit (Coereba flaveola portoricensis) was the first life history done on the island with any degree of thoroughness. More recently RODR\xc3\x8dGUEZVIDAL (1959) made a three-year study of the Puerto Rican Parrot (Amazona vittata vittata), which has brought to light interesting information on its previously unknown breeding habits. SPAULDING (1937) wrote three short papers in which she set down her observations on the nesting habits of three native birds.
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  • 33
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    Diplopoda of Guiana (1963)
    In:  Studies on the Fauna of Suriname and other Guyanas vol. 4 no. 1, pp. 1-157
    Details
    Publication Date: 2024-01-12
    Description: More than ten years ago, I published some notes on the taxonomy of Surinam millipedes. My intention then was to describe and record in a series of papers the material of Diplopoda in the collections of the Amsterdam and Leiden Museums, and to give a survey of the millipede fauna of Surinam.\nHowever, as this work progressed it became evident that the monographs and revisions by the authors of the previous generation were only too often a quite unreliable basis for the project planned, and that descriptions of new species were rather useless if not preceded by at least partial revisions of the nomenclature and systematics of the genera or even families involved.
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  • 34
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    Mammalian remains from an Indian site on Cura\xc3\xa7ao (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 14 no. 1, pp. 119-122
    Details
    Publication Date: 2024-01-12
    Description: The animal remains (mostly of shells, fish, and turtles) collected by Mr. H. R. VAN HEEKEREN and Mr. C. J. DU RY at the Indian site Sint Jan II, Cura\xc3\xa7ao, in March, 1960, include a few specimens of mammals. As was the case with the Indian site Santa Cruz, on Aruba (HOOIJER, 1960), several forms are represented that are no longer extant on the island, although this does not imply that all of them were strictly endemic at the time of formation of the Indian refuse heaps; they may have been imported for food or other purposes. The material dates from 1000\xe2\x80\x941500 A.D., and is therefore late pre-Columbian. The following forms are present:
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  • 35
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    Copepoda associated with West Indian Invertebrates \xe2\x80\x93 IV The genera Octopicola, Pseudanthessius and Meomicola (Cyclopoida, Lichomolgidae) (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 18 no. 1, pp. 1-74
    Details
    Publication Date: 2024-01-12
    Description: Our thanks are due to the following for their identifications of host animals: Dr. W. ADAM, Mus\xc3\xa9um Royal d\xe2\x80\x99Histoire Naturelle, Brussels (cephalopods from Cura\xc3\xa7ao); Dr. GILBERT L. VOSS, University of Miami Marine Laboratory, Florida (cephalopods from Barbados); Mrs. R. E. TEAGLE, British Museum (Natural History), London (ophiuroids from Cura\xc3\xa7ao); Dr. ELISABETH DEICHMANN, Museum of Comparative Zo\xc3\xb6logy, Harvard College, Cambridge, Mass. (the remaining echinoderms); and Dr. MARIAN H. PETTIBONE, University of New Hampshire, Durham (polychaetes). A.G.H. and R.U.G. wish to express their appreciation to Mr. ROBERT GREENHILL for his assistance during their collecting in Barbados and for obtaining a further sample of octopus in September, 1959; to Dr. IVAN GOODBODY and the staff of the Marine Laboratory, University College of the West Indies, Jamaica, for providing more amphinomid polychaetes in October, 1961; and to the Trustees of the British Museum (Natural History) through Dr. J. P. HARDING for the opportunity to examine material of Pseudanthessius thorelli. Additional collections from Barbados were made by R.U.G. in December, 1961\xe2\x80\x94January, 1962.\nThis work was supported by grants from the Netherlands Foundation for the Advancement of Research in Surinam and the Netherlands Antilles (WOSUNA), Amsterdam, and from the National Science Foundation of the United States, Washington.
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  • 36
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    Caribbean Land Molluscs: Streptaxidae (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 14 no. 1, pp. 41-76
    Details
    Publication Date: 2024-01-12
    Description: The material on which the present paper is based consists of a small number of Streptaxidae collected by Dr. P. WAGENAAR HUMMELINCK during his visits to the Caribbean Islands and the mainland of Venezuela since 1930, and further of some specimens which, at various times, have reached the author through the generosity of Mr. SERGIO ARIAS, Caracas, Dr. G. MARCUZZI, Padova, Professor S. JAECKEL, Berlin, and Mr. TJOA TJIEN MO, Bogor.\nBesides this material I also investigated some material present in the following collections and kindly put at my disposal: Naturhistorisches Museum, Basel; Zoologisches Staatsinstitut und Museum, Hamburg; British Museum (N.H.), London; American Museum of Natural History, New York; United States National Museum, Washington. I have to thank for their kind assistance: Dr. L. FORCART, Basel; Professor G. WEIDNER and Dr. P. KAISER, Hamburg; Dr. W. J. REES and Dr. GALBRAITH, London; Miss D. E. BLISS, New York; Dr. H. A. REHDER, Washington; and last but not least the late Mr. HUGH WATSON, Cambridge, England, for his most valuable and expert advice. I am also greatly obliged to Mr. PAUL KESSELS, Tilburg, Netherlands, for his help in composing the histograms.
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  • 37
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    Unerwartetes Vorkommen von Taumelk\xc3\xa4fern (Gyrinidae) auf Cura\xc3\xa7ao (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 14 no. 1, pp. 123-125
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    Publication Date: 2024-01-12
    Description: Von den \xe2\x80\x9cInseln unter dem Winde\xe2\x80\x9d, dem s\xc3\xbcdlichsten, in Ost-Westrichtung dem Festland von Venezuela vorgelagerten Teil des Antillenbogens, waren bisher keiner Gyriniden bekannt. Erst k\xc3\xbcrzlich erfuhr ich durch Dr. P. WAGENAAR HUMMELINCK, Utrecht, dass auf Cura\xc3\xa7ao, einer der westlichsten dieser Inseln, Vertreter dieser K\xc3\xa4ferfamilie erbeutet worden seien, deren Sammler, Ir. R. H. COBBEN von der Landbouwhogeschool in Wageningen, mir seine Ausbeute entgegenkommend zum Studium zur Verf\xc3\xbcgung stellte. Beiden Herren danke ich hiermit bestens f\xc3\xbcr ihre Freundlichkeit.\nDas Material war besonders interessant hinsichtlich seiner faunistischen Zusammensetzung, denn w\xc3\xa4hrend die eine der in ihm enthaltenen Arten festl\xc3\xa4ndischen Ursprungs ist, geh\xc3\xb6rt die andere zur karibischen Fauna. Bemerkenswert ist auch, dass beide Arten trotz des abgelegenen Fundorts keine wesentlichen rassischen Besonderheiten aufweisen.
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  • 38
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    Ophiuroidea of the Lesser Antilles (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 15 no. 1, pp. 24-50
    Details
    Publication Date: 2024-01-12
    Description: This paper deals mainly with a collection of ophiuroids from the Lesser Antilles sent to the British Museum (Natural History) by Dr. P. WAGENAAR HUMMELINCK in 1959. The identifications were made by ROSEMARY PARSLOW, but the discussion and figures of Amphiodia and Ophiocomella are by AILSA CLARK.\nThe material was collected in 1948/49 and 1955. Specimens gathered by HUMMELINCK in 1930 and 1936 are mentioned in ENGEL\xe2\x80\x99S report on \xe2\x80\x9cEchinoderms from Aruba, Cura\xc3\xa7ao, Bonaire and northern Venezuela\xe2\x80\x9d (1939).
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  • 39
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    Asteroids from the Netherlands Antilles and other Caribbean localities (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 15 no. 1, pp. 72-101
    Details
    Publication Date: 2024-01-12
    Description: The material brought back by Dr. P. WAGENAAR HUMMELINCK from his various trips to the West Indies includes a number of starfish, which \xe2\x80\x94 with exception of the specimens belonging to Astropectinidae, Echinasteridae and Goniasteridae \xe2\x80\x94 were given to the present author as a subject for taxonomic examination. This resulting contribution to science is the outcome of no more than a few months of practical work under the direction of Dr. HUMMELINCK, and can therefore not be other than a rather superficial study, in which only additional material from the museums in Amsterdam and Leiden has been considered.\nThe material covered in this paper comprises: Oreaster reticulatus (L.), from BIMINI, NEW PROVIDENCE, CUBA, JAMAICA, HISPANIOLA, ST. MARTIN, LOS TESTIGOS, MARGARITA, BONAIRE, ARUBA, and BRAZIL. \xe2\x80\x94 Plates III\xe2\x80\x94VI. Linckia guildingii Gray, from BIMINI, NEW PROVIDENCE, ST. KITTS, BONAIRE, KLEIN BONAIRE, CURA\xc3\x87AO, ARUBA, and BRAZIL. \xe2\x80\x94 Plate VII. Ophidiaster guildingii Gray, from CURA\xc3\x87AO. \xe2\x80\x94 Plate VIII. Asterina folium (L\xc3\xbctken), from COLOMBIA (Santa Marta). \xe2\x80\x94 Plate IX. Asterina hartmeyeri D\xc3\xb6derlein, from ST. JOHN, ST. MARTIN, BONAIRE, and ARUBA. \xe2\x80\x94 Plate IX. Asterina marginata (Perrier), from BRAZIL. \xe2\x80\x94 Plate IX. Luidia senegalensis (Lam.), from ANTIGUA, COCHE, VENEZUELA mainland, COLOMBIA (Rio Hacha), and BRASIL. \xe2\x80\x94 Plates X\xe2\x80\x94XI. Luidia clathrata (Say), from \xe2\x80\x9cWEST INDIES\xe2\x80\x9d. \xe2\x80\x94 Plates X\xe2\x80\x94XI. Luidia alternata (Say), from COLOMBIA (R\xc3\xado Hacha). \xe2\x80\x94 Plates VIII, X.
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  • 40
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    Some Caribbean Coleoptera Cerambycidae (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 18 no. 1, pp. 75-102
    Details
    Publication Date: 2024-01-12
    Description: The notes on Cerambycidae in this paper are based on small collections of material sent to me by Dr. P. WAGENAAR HUMMELINCK of the Zo\xc3\xb6logisch Laboratorium, Utrecht; Ir. R. H. COBBEN of the Laboratorium voor Entomologie, Wageningen; Dr. H. F. HOWDEN of the Entomological Research Institute, Dept. of Agriculture, Ottawa; the Museum Frey, Tutzing bei M\xc3\xbcnchen; Dr. T. H. FARR of the Institute of Science, Kingston, Jamaica, as well as specimens from my own collection.\nThe opportunity is taken of listing material from new localities and of figuring a few species which have not previously been figured so far as I am aware, as well as describing a number of new genera and species.
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  • 41
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    Metamorphic history of the Central Pyrenees Part II, Valle de Ar\xc3\xa1n, Sheet 4 (1963)
    In:  Leidse Geologische Mededelingen vol. 28 no. 1, pp. 321-376
    Details
    Publication Date: 2024-01-12
    Description: The structural geology and metamorphic petrology of the Bosost area in the Valle de Ar\xc3\xa1n (Central Pyrenees) is discussed. The rocks exposed in this area consist of Cambro-Ordovician mica-schists with numerous granite and pegmatite bodies, phyllites and limestones; Silurian slates and schists and Devonian schists and limestones.\nThe major structure dating from the Hercynian orogeny is the Garonne dome with essentially horizontal schistosity. Large steep folds in the Devonian accompanied by axial plane slaty cleavage are folded disharmonically with regard to the Cambro-Ordovician. Both kinds of structures date from the main phase. A second and later phase with N-S foldaxes was accompanied by laminar flow in E-W direction as shown by numerous rotated porphyroblasts. A third and fourth phase of deformation have folds with vertical axial planes in NW-SE and E-W direction. These last three phases are characterized by minor and microfolds only.\nThe method of investigating microstructures mainly with regard to porphyroblasts is discussed first; then its application. This resulted in the establishment of four metamorphic zones: a biotite-zone; a staurolite-andalusite-cordierite-zone; an andalusite-cordierite-zone and a cordierite-sillimanite-zone; in this order with increasing grade. The higher zones have passed through each of the lower grade ones, so that the cordierite-sillimanite-zone has the most complex history. Staurolite is the first aluminium-silicate to crystallize with increasing temperature, than andalusite, cordierite and finally sillimanite. Before sillimanite started to form, staurolite was already unstable; at the beginning of sillimanite crystallization andalusite became unstable.\nCale-silicate rocks in the Ordovician limestone in the cordierite-sillimanite-zone contain bytownite, grossularite, diopside and vesuvianite.\nGranite and pegmatite bodies and sills occur in all the aluminium-silicate bearing zones, but most abundant in the cordierite-sillimanite-zone. Their emplacement lasted from shortly after the first phase until after the fourth. The culminating point lies around the fourth phase. The granites are mainly composed of albite, quartz, and muscovite; the pegmatites carry smaller or larger amounts of microcline.\nChemical analyses of phyllites and mica-schists have shown that the composition of both rock groups is essentially the same. With increasing silicium content, aluminium and potassium decrease. The granites have high alcali percentages with sodium predominating over potassium.
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  • 42
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    A fabric study of Lherzolites (1963)
    In:  Leidse Geologische Mededelingen vol. 28 no. 1, pp. 1-102
    Details
    Publication Date: 2024-01-12
    Description: The solution of the problem whether the ultrabasic inclusions in lavas are accumulation products of early crystallized minerals of the lavas in which they occur, or fragments of the earth\xe2\x80\x99s peridotite shell carried to the surface by the eruptive force of the lavas, largely depends on the answer to the question whether these inclusions are tectonites or not.\nThe structure of the specimens from Auvergne (France), which formed the main subject of this study, has been proved conclusively to be of a tectonic nature, from the macroscopically visible intersecting slip planes which are definitely younger than the banding of the specimen, as well as from microscopic evidence that suggests that both the olivine and enstatite crystals are concentrated in the intersecting slip planes. The fabric of olivine and enstatite proved to be symmetrical in respect of these slip planes, although remnants of an initial, predeformational orientation related with the banding still persist. In order to establish the relation between the old and the new fabric a comparative study of the fabric of a nodule from Dreiser Weiher (chapter II) and the crystal orientation of the banded sample from Auvergne (chapter III) has been made. It was concluded that the tectonic fabric of the sample from Auvergne could be interpreted as the result of a mechanical rotation of the composing crystals around two rotation axes, from their earlier orientation which is observed in the German specimen, into their new orientation which is symmetrical in respect of the intersecting slip planes. The rotation axis of olivine proved to be parallel to the intersection of the banding and a slip plane (S1), the rotation axis of enstatite is parallel to the intersection of the second slip planes (S2) and a plane normal to the banding, which is characterized by the X01\xe2\x80\x94Yen girdle in the pre-deformational fabric. The geometry of the observed fabric further suggests that the crystals rotated in opposite sense over supplementary angles around the rotation axes.\nThe distribution of olivine in the intersecting planes as well as the above mentioned rotation were further proved in a second sample from Auvergne on which an axial distribution analysis was carried out. The results of this analysis confirmed the expectations that crystals of a specific orientation are concentrated in intersecting directions in the plane of observation. The lattice orientation of olivine proved to be dominated by an orientation of {010} parallel to S1 and [010] sub-parallel to S2, while the enstatite crystals showed a strong preferred orientation of [001] sub-parallel to S1 and [100] in S2. The comparison of the preferred orientation of the X01 axes in five samples of different mineralogical composition has demonstrated that the preferred orientation of the X01 axes increases with increasing olivine content. All these results point to a tectonic nature of the structure of the ultrabasic inclusions in the lavas of Auvergne. Since the Mg/Fe distribution in the pyroxenes of the nodules suggests that these minerals crystallized at temperatures well above those of magmatic assemblages, it was concluded that the studied specimens are not derived by crystal fractionation from the lavas in which they occur, but are likely to be fragments of the earth\xe2\x80\x99s peridotite shell.\nThe fabric of the type-locality of the lherzolites in the French Pyrenees proved to be secondary and symmetrical in respect of the local Alpine stress field in such a way that the Z axes of both olivine and enstatite are parallel to the major axis of the stress deviator. The interpretation of this tectonic fabric of olivine has been based on the translation mechanism of olivine, described by Chudoba and Frechen (1950).\nIn the last chapter attention has been paid to some recent theories and experiments which all lead to the conclusion that the orientation of crystals during growth, either in a uniaxial stress field or under a temperature gradient, is governed by the lattice of the crystals involved, a conclusion that might be useful for the interpretation of olivine fabrics, for the results of this study suggest that the crystal structure and not the grain shape governs he fabric of many ultrabasic rocks.
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  • 43
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    Note sur le Bassin Houiller de Cinera-Matallana (1963)
    In:  Leidse Geologische Mededelingen vol. 29 no. 1, pp. 303-311
    Details
    Publication Date: 2024-01-12
    Description: In the north of Spain, in the province of Le\xc3\xb3n, in the neighbourhood of Ci\xc3\xb1era and Matallana, a limnic coalbasin extends between the rivers Rio Curue\xc3\xb1o and Rio Bernesga, with a E\xe2\x80\x94W strike of the layers.\nThis coalbasin, the length of which is 15 km and which is not more than 5 km wide, follows a direction, which is E\xe2\x80\x94W parallel to the Cantabrian Mountainrange.\nThe deposit, which have a regular tectonical aspect on the north side, become more complicated on the south side and especially in the eastern part.\nThe structure of the basin is an asymmetric synclinorium. The axial plane is nearer the southern part of the basin. The dip-slopes in the north flank are less steep than those in the south flank, where the layers overkeep to the north in some places.\nRarely, a specific horizon runs through the basin without pinching out or without changing the composition of the sediment.\nThe greater part of the layers of coal in exploitation are in the western part of the basin.\nThe sedimentation began with the coarse grained conglomerates along the north side and especially the conglomerates at Correcillas in the N\xe2\x80\x94E, the thickness of which is nearly 250 m.\nThe age of the sediments is Stefanian B.
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  • 44
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    The Ultramafites and layered Gabbro Sequences (1963)
    In:  Leidse Geologische Mededelingen vol. 28 no. 1, pp. 177-296
    Details
    Publication Date: 2024-01-12
    Description: On Stjern\xc3\xb6y, Seiland and the neighbouring peninsulas of \xc3\x96ksfjord and Bergsfjord ultramafic bodies of peridotite and pyroxenite with associated layered gabbro sequences occur within a complex of highly metamorphic gabbro gneisses, rocks akin to pyroxene-granulites and mafic charnockites. As is shown on the basement map in insert of backflap the layered gabbro is generally concordant with the foliation of the surrounding gneisses but locally shows transgressive features. Within this mafic province occurrences of hornblendite, carbonatite, and nephelinesyenite are also found, the latter affiliation of rocks probably being the result of metasomatic processes.\nThe petrography and general mineralogy of the ultramafic, gabbroic, and metamorphic types of rocks are described in detail. In the layered gabbro sequences on Stjern\xc3\xb6y there exists no gravitational crystallization differentiation such as is found in other stratiform gabbro-peridotite complexes; the variation in the composition of the characteristic minerals is too small, and irregular at that. The textural relations point to incipient fracturing along grain-boundaries and, especially, to deuteric processes which can be inferred from the abundance of spinel-pyroxene symplectites. The characteristic rims of symplectite around olivine are clearly demonstrated in the photographs 2 and 3 on plate C.\nIn texture and structure the gabbro gneisses and intercalated syenitic and meta-sedimentary rocks on Stjern\xc3\xb6y exhibit considerable clastic and plastic deformation. Their mineral association points to an intense regional metamorphism near or within the granulite facies; by means of the ACF diagrams, fig. 9a and 9b, it is shown that the plotted mineral parageneses may be stable in the hornblendegranulite and the pyroxene-granulite subfacies.\nThe investigation of co-existing clinopyroxene, orthopyroxene, and olivine in the layered gabbro-peridotite sequence on Stjern\xc3\xb6y indicates that high pressures and temperatures prevailed at the time of their formation. In tie-line trends of co-existing pyroxenes the layered gabbros from Stjern\xc3\xb6y are remarkably similar, not to the normal type of stratiform gabbro-peridotite complexes, but to peridotite nodules in certain basaltic lavas. (compare fig. 5a and 6a). As is shown in fig. 6b the tie-lines joining co-existing orthopyroxene and clinopyroxene from gabbro gneisses exhibit similar trends; these data most probably point to an extreme metamorphism of anhydrous rocks at great depth within the earth\xe2\x80\x99s crust.\nThe chemical analyses of samples of the ultramafic sequence, as plotted in the QLM diagram of fig. 8a, exhibit a linear trend of differentiation; this suggests a simple process of fractional melting or crystallization. The projection points of the gabbro gneiss occupy a central position in this differentiation trend on Stjern\xc3\xb6y; thus the gabbro gneiss provides a suitable material for such a process. High lime content is another chemical characteristic of gabbro and related ultramafic rocks on Stjern\xc3\xb6y (fig. 8b); hence the major femic mineral is a calcium-rich clinopyroxene, whereas magnesium-rich orthopyroxene predominates in the stratiform type of layered complex.\nClearly, then, the layered gabbro and related ultramafite within the mafic province of western Finnmark differs considerably in major features from the wellknown layered gabbro-peridotite occurrences such as Bushveld, Stillwater or Skaergaard. Finally the results of the mineralogical and chemical investigations are discussed from the petrogenetic point of view. A hypothesis is offered for the emplacement of layered gabbro and ultramafite on Stjern\xc3\xb6y involving differential anatexis with local palingenesis in a deepseated zone of the Caledonian orogen.
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  • 45
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    Notes on Chameleons, II: Chamaeleo laevigularis (L. M\xc3\xbcller, 1926), a synonym of Chamaeleo johnstoni (Boulenger, 1901) (1963)
    In:  Beaufortia vol. 10 no. 117, pp. 44-47
    Details
    Publication Date: 2024-01-12
    Description: In 1926 LORENZ M\xc3\x9cLLER described a new chameleon, labelled \xe2\x80\x9cEast London, Kapland\xe2\x80\x9d. M\xc3\x9cLLER remarked on the terra typica: \xe2\x80\x9cIch erhielt dieses Cham\xc3\xa4leon mit einem anderen, der Gruppe des Ch. pumilus angeh\xc3\xb6rigen, von meinem Freund Prof. Dr. Fr. Werner in Wien, der die beiden Cham\xc3\xa4leons vor einigen Jahren von der Naturalienhandlung Boettcher in Berlin gekauft hatte. Wie mir Prof. Werner schrieb, zweifelte er die Richtigkeit des Fundortes f\xc3\xbcr das hier neu beschriebene Cham\xc3\xa4leon an.\xe2\x80\x9d In \xe2\x80\x9dThe Lizards of South Africa\xe2\x80\x9d FITZSIMONS (1943) mentioned Chamaeleon laevigularis as a \xe2\x80\x9dspecies auctorum\xe2\x80\x9d, of which he remarked (p. 174): \xe2\x80\x9dThe above description, based on a young specimen supposedly from East London, is certainly not applicable to any of the known species of South African chameleons, while the feebly marked dorsal ridge and the absence of a gular crest preclude its inclusion with the Cape chameleons of the Lophosaura group, which are all characterized by a more or less distinct dorsal and gular crest. It is thus extremely doubtful if the type locality (East London) given is correct and until such time as the contrary is proved by further collecting, laevigularis cannot with any certainty be regarded as a South African form.\xe2\x80\x9d
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  • 46
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    Scale insects from Thailand with description of a Filippia n.sp (1963)
    In:  Beaufortia vol. 10 no. 115, pp. 29-39
    Details
    Publication Date: 2024-01-12
    Description: Filippia orientalis n.sp. can be recognized by the following characters.\nThe adult female has next to chisel-shaped spines around the margin of the body 4 such spines on the outer side of the anal plates (fig. 11). The adult male has only one long seta (about 250 \xce\xbc) in the glandular depressions which produce the caudal wax-tails. The first stage larva is provided with long stigmatic spines (ca. 60 \xce\xbc) and slender conical spines along the margin of the body (fig. 19). The second stage larva has chisel-shaped spines around the margin of the body like the adult female (fig. 22). On the anal plates only the discal and the apical seta are chisel-shaped, the 2 setae on the mesal side of the plate have the usual shape (fig. 20).\nTypes in the Zoological Museum at Amsterdam, of second stage larvae, prepupae and pupae in the Museum of Natural History at Leiden.
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  • 47
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    Eine neue Art der Gattung Fieberiella Signoret, 1880 (Insecta, Homoptera) aus Griechenland (1963)
    In:  Beaufortia vol. 10 no. 118, pp. 48-50
    Details
    Publication Date: 2024-01-12
    Description: Vom Herrn W. H. Gravestein, Amsterdam, erhielt ich eine Anzahl Zikaden zur Bestimmung, die w\xc3\xa4hrend einer Entomologischen Exkursion des Zoologischen Museums Amsterdam in Griechenland gesammelt worden sind. Darunter befand sich auch eine neue Fieberiella-Art. Eine taxionomische Bearbeitung der drei bisher bekannten Arten der Gattung Fieberiella Signoret befindet sich zur Zeit im Druck (W. WAGNER, 1963). In dieser Arbeit werden auch die m\xc3\xa4nnlichen Genitalien der bisher bekannten Arten abgebildet. Die neue Art benenne ich zu Ehren ihres Entdeckers, Herrn J. R. Duffels, Amsterdam.
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  • 48
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    Notes on Chameleons I. Comparative cytology: aid and new complications in Chameleon-taxonomy (1963)
    In:  Beaufortia vol. 9 no. 108, pp. 201-218
    Details
    Publication Date: 2024-01-12
    Description: 1. Comparison is made between the subdivision of the genus Chamaeleo in groups of species based on cytological considerations (MATTHEY & VAN BRINK) and the subdivision of this genus in groups based on taxonomical considerations (HILLENIUS). Both subdivisions were developed independently from each other and show relatively few discordances (see Table 2). 2. Detailed discussion is given of the case of two specimens (Ch. voeltzkowi and Ch. monoceras), taxonomically to be regarded as belonging to Ch. rhinoceratus. Their chromosome-patterns, however, differ so greatly as most probably not to be able to yield fertile offspring. They should then be regarded as belonging to different species. As the chromosomepatterns of the types of Ch. rhinoceratus c.s. are unknown (only accessible in fresh specimens), it is advised for the moment to let the taxonomic considerations prevail. 3. In the Conclusion an attempt is made to explain the discordances between the subdivision of MATTHEY & VAN BRINK and of HILLENIUS.
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  • 49
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    Notes on the fishes of Western New Guinea I (1963)
    In:  Zoologische Mededelingen vol. 38 no. 14, pp. 221-242
    Details
    Publication Date: 2024-01-12
    Description: INTRODUCTION\nIn the summer of 1954, I received an invitation from the Netherlands New Guinea Government to undertake a faunistic investigation of the fish fauna of the area. It was thought advisable for the promotion of the local New Guinea fisheries, to first obtain a more thorough knowledge of the fish fauna of the region, based on a collection as complete as could be attained within a reasonable time. As such a collecting trip could be expected to yield results of considerable zoological and zoogeographical importance, I gladly accepted this unique opportunity.\nA most fortunate circumstance was that my visit coincided with an already previously planned collecting trip to the same area by two of my colleagues, Dr. L. D. Brongersma, at the time deputy-director and curator of herpetology, now director of the Leiden Museum, and Dr. L. B. Holthuis, curator of carcinology at the same institution. The resulting mutual assistance and pooling of technical facilities subsequently proved to contribute notably to the success of my explorations.\nWhile the voyage was sponsored by the Netherlands Government, numerous facilities and much, often indispensable, support were rendered by the Government of Netherlands New Guinea, by the Royal Netherlands Navy, by the missions of the Dutch Reformed Church and the Roman Catholic Church, and by the Christian and Missionary Alliance. Invaluable further assistance was received from private persons too numerous to be mentioned here all by name.\nThe following notes, though primarely based on the material collected during our 1954-1955 survey, will occasionally also include data based on
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  • 50
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    A revision of the genus Candacia (Copepoda: Calanoida) with an annotated list of the species and a key for their identification (1963)
    In:  Zoologische Mededelingen vol. 38 no. 10, pp. 171-194
    Details
    Publication Date: 2024-01-12
    Description: The genus Candacia 2) was erected by Dana (1846) for certain copepods found in collections obtained by the U. S. Exploring Expedition of 18381842. When the species referable to this genus were first described three years later, Dana (1849) changed the generic name to Candace. Giesbrecht (1892) established the family Candacidae to accommodate Candace but six years later Giesbrecht & Schmeil (1898) used Dana\'s first proposed generic name, Candacia, and accordingly changed the family name to Candaciidae.\nThese latter two names have been used by most authors since about 1900.\nI wish to thank Dr. W. Vervoort for reading and criticizing the manuscript, Miss Abigail Hooper for checking literature references and for preparing distribution charts, and my wife, Joan, for help in preparing the illustrations. I also wish to thank Drs. T. E. Bowman and A. Fleminger for criticizing the key.\n\nDIVISION OF THE GENUS AND A LIST OF THE SPECIES\nSars (1903) recognized that two types of males were included in the species then referable to Candacia and he indicated that the genus could probably be divided into two genera. Twelve species have subsequently been described all of which are referable to one of the types recognized by Sars.\nThe genus is here divided into two genera, Paracandacia nov. gen. and Candacia s. s. the diagnoses of which are given below.\nParacandacia nov. gen.\nTYPE SPECIES. Candace truncata Dana, 1849 (= Paracandacia truncata).\nSince no types were mentioned by Dana and none of his specimens is apparently extant a female specimen collected in the Pacific Ocean (oo\xc2\xb035\'N 170\xc2\xb011\'E) and deposited in the U. S. National Museum (Cat. No. 107600) is
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  • 51
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    Concise survey of localities and collection numbers of zoological and botanical specimens, collected by the Netherlands biological expedition to Turkey 1959 (1963)
    In:  Zoologische Mededelingen vol. 38 no. 8, pp. 129-151
    Details
    Publication Date: 2024-01-12
    Description: I.\nINTRODUCTION\nIn the spring of 1959 E. Hennipman, P. Nijhoff, C. Swennen, A. S.\nTulp, W. J. M. Vader and W. J. J. O. de Wilde made a biological collecting expedition to Turkey. The record of this journey of the "Nederlandse Biologische Expeditie Turkije 1959" appeared in "De Levende Natuur" vol. 64, supplement to no. 5 (1961). Here follows a condensed description of the localities where material was collected as well as a list of collection numbers of the zoological and botanical specimens.\nThe route followed by the expedition is indicated on map 1, on which are also indicated the areas shown in the more detailed maps 2, 3, 4 and 5.\nSince, on the one hand, geographical names in Turkey are subject to alterations and on the other certain names are used several times for quite different places, the numerous topographical synonyms and homonyms repeatedly cause confusion in literature. That is why all geographical names occurring in this contribution are fixed by means of the maps. All data are taken from the maps 1 : 200,000 of the Turkish Ordnance Survey.\nThe complete zoological collection is now in the Rijksmuseum van Natuurlijke Historie at Leiden.\nOf the botanical collection, the specimens of which are labelled: "Flora Turcomanniae Asiaticae, iter Leydense 1959", the first set, containing among other things all unique specimens, is now in the Rijksherbarium in Leiden.\nDuplicate sets were sent to the Laboratorium voor Plantensystematiek en -geografie at Wageningen, the Royal Botanic Gardens at Kew, the Botanisches Museum in Berlin, the Botanisch Museum en Herbarium at Utrecht and the Botanik Enstit\xc3\xbcs\xc3\xbc in Ankara.
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  • 52
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    Reduction of Placolobium Mig. to Ormosia Jackson (Leg.-Pap.) (1963)
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 12 no. 1, pp. 70-70
    Details
    Publication Date: 2024-01-12
    Description: At the request of Mr Airy Shaw the type specimen of Placolobium sumatranum Miq. Fl. Ind. Bat. 1, 1 (1855) 1082 has been examined from the Herbarium at Utrecht by kind permission of Prof. Lanjouw. It is very scrappy and consists of a loose rachis and leaflets and unfortunately the fruit valves described by Miquel are not present and could not be found among the carpologica by Miss Mennega.\nA close examination of the specimen has, however, shown that exactly similar specimens are found under Ormosia macrodisca Baker, showing the slightly sunken veins, areolae of similar size, epidermis with slightly granular surface and same colour, leaflets of same texture, and petiolules thickened, wrinkled transversely with shallow grooves. Moreover, the rachis also fits exactly that of O. macrodisca, is of the same size, lengthwise ribbed, and with the blackish trichomes at the nodes. From the description the fruit valves must also be similar to those of Ormosia macrodisca. Obviously Miquel had received leaves of a sterile twig and a loose fruit (without seed) picked from the ground. At that time the species was undescribed and he was unaware that such large woody fruits occurred in the genus. The species is rather widely distributed and several later collections have been made in Central Sumatra according to Mrs. Knaap in Reinwardtia 6 (1962) 230.
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  • 53
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    Florae Malesianae Precursores XXXII. Some new Cyperaceae (1963)
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 12 no. 1, pp. 23-30
    Details
    Publication Date: 2024-01-12
    Description: Herba perennis, rhizomate lignoso, adscendente. Culmus erectus, radicibus crassis teretibus 2\xe2\x80\x943 mm diam. sustensus, dense foliatus, c. 50 cm altus. Folia linearia, rigida, opaca, glaucescentia, basin conduplicatam versus straminea, apice sensim in flagellum triquetrum scaberrimum angustata, usque ad 50 cm longa, 5\xe2\x80\x947 mm lata, marginibus nervoque medio subtus apicem versus dense acuteque serrata, nervo medio subtus prominente, nervis lateralibus vix distinctis. Scapi brevissimi, in axillis foliorum caulinorum absconditi, spiculam unicam gerentes. Spiculae subsessiles, ovoideae, apice acutae, c. 15 mm longae, 7\xe2\x80\x9410 mm latae. Glumae multinerviae, inferiores vacuae, coriaceae, ovatae, acutae, fuscae, membranaceo-marginatae, 8\xe2\x80\x949 mm longae; glumae florigerae lanceolatae, tenuiores, 9\xe2\x80\x9410 mm longae. Flores lineares, 8\xe2\x80\x9410 mm longi, squamellis 6 membranaceis, binis lateralibus ad carinam tenuiter ciliolatis. Stamina 3, antheris linearibus 5\xe2\x80\x946 mm longis. Stigmata 3. Nux drupacea, subpyriformis, apice in rostrum breve subcurvatum acuminata, rugulosa, cinereo-fusca, 6 mm longa, 3 mm lata, stipite brevi \xc2\xbd mm longo.\nNORTH BORNEO. Dist. Sandakan, Malubok Kinabatangan, in swamp forest, Nov. 18, 1960, W. Meijer SAN 23592 (L, typus).
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  • 54
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    Pacific plant areas. Introduction (1963)
    In:  Pacific Plant Areas vol. 1 no. 1, pp. 1-8
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    Publication Date: 2024-01-12
    Description: Pacific Plant Areas was first suggested by Prof. Dr. H. J. Lam, Director of the Rijksherbarium, Leyden, during the 6th Pacific Science Congress held at Berkeley, California, in 1939.\xc2\xb2 In the 7th Pacific Science Congress held in Auckland and Christchurch, New Zealand, in 1949, Doctor Lam made a detailed progress report on the project.\xc2\xb9 A further report consisting of an enumeration of the collections made in various islands of the Pacific basin was made by Prof. Dr. W.R.B. Oliver of Wellington, New Zealand, who was chairman of the Committee from 1949 to 1953, in the 8th Pacific Science Congress held in Manila in 1953.\xc2\xb3 During the Congress, its Standing Committee on Pacific Plant Areas was made a subsection of its Botany Section, and Doctor Oliver was succeeded as chairman of the subsection by Doctor Lam who, during the preceding years, had collected a considerable number of tentative distribution maps of genera and species with the help of a number of collaborators.
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  • 55
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    Preliminary List of Syrphidae known from Suriname and British and French Guiana (1963)
    In:  Studies on the Fauna of Suriname and other Guyanas vol. 5 no. 1, pp. 1-33
    Details
    Publication Date: 2024-01-12
    Description: The family of Syrphid flies (\xe2\x80\x9cHover flies\xe2\x80\x9d or \xe2\x80\x9cFlower flies\xe2\x80\x9d) is richly represented in the Neotropical region. FLUKE\xe2\x80\x99S Catalogue of Neotropical Syrphidae, finished in September 1953, records 107 genera and 1,507 species, exclusive of 100 \xe2\x80\x9cspecies incertae sedis.\xe2\x80\x9d (In actual fact, 1,508 species are enumerated, but Baccha picta Wiedemann (FLUKE, p. 259) is an Ethiopian species.) The large genera Volucella with 274 species, Baccha with 269 species, Mesograpta with 130 species, and Eristalis with 106 species, seem to have had their greatest opportunity of development in this region. However, some of the names will probably prove to be synonyms, since the descriptions by earlier authors are often too short and insufficient to enable a species to be recognized with certainty. As a rule, the species described by recent authors are quite recognizable. \nUp to a few years ago the number of Syrphids described or known from Suriname was very small. Moreover, one of them, Volucella ardua Wiedemann, proved to be synonymous with Volucella tympanitis Fabricius, as stated by CURRAN, who studied WIEDEMANN\xe2\x80\x99S type specimens. Of course, the number of the species taken on occasion in Suriname is somewhat larger; but, as far as is known, no enumeration has ever been published.
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  • 56
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    The Shallow water Holothurians of Cura\xc3\xa7ao, Aruba and Bonaire (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 14 no. 1, pp. 77-99
    Details
    Publication Date: 2024-01-12
    Description: The holothurians from the southern end of the Caribbean area are incompletely known. CLARK (1919) discussed a few specimens taken from Tobago, British West Indies, and DEICHMANN (1926) prepared a report on the holothurians from the Barbados-Antigua Expedition. ADA TEN BROEKE (1927) listed 7 holothurians from Cura\xc3\xa7ao, collected by C. J. VAN DER HORST. This list constituted the first mention of holothurians from the area. CLARK (1933) listed one additional specimen in his \xe2\x80\x9cHandbook of the Littoral Echinoderms of Porto Rico and the Other West Indian Islands\xe2\x80\x9d. ENGEL (1939), included three additional sea cucumbers in his report on the echinoderms which were gathered by P. WAGENAAR HUMMELINCK. Neither ENGEL (1939) nor TEN BROEKE (1927) described their specimens. I have found three additional species new to the fauna of the above islands. Two of these specimens, Thyoneria cognata and Trachythonidium occidentale are the first Dendrochirota to be reported from the Netherlands Antilles.\nAfter this report has been completed, ELISABETH DEICHMANN (1963) produced a short survey of the \xe2\x80\x98Shallow water Holothurians known from the Caribbean Waters\xe2\x80\x99 in which several new data are to be found gathered from material which was collected by WAGENAAR HUMMELINCK in 1948/49 and 1955.
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  • 57
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    Borkenk\xc3\xa4fer der Bodenfauna in Surinam (1963)
    In:  Studies on the Fauna of Suriname and other Guyanas vol. 6 no. 1, pp. 52-64
    Details
    Publication Date: 2024-01-12
    Description: Dr. J. van der Drift hat im Jahre 1959 in Surinam umfangreiche Untersuchungen \xc3\xbcber die Bodenfauna angestellt, wobei unter anderen \xc3\xbcber 2.500 Scolytiden bezw. Platypodiden zutage kamen, die mir entgegenkommenderweise zur Bearbeitung \xc3\xbcberlassen wurden. Die Determination ergab dabei zwanzig Arten und eine Unterart der Familie Scolytidae und zwei Platypodidae. Von den Scolytiden k\xc3\xb6nnen vier Arten und eine Unterart als neu betrachtet werden.\nDie Scolytiden stellen dabei den gr\xc3\xb6\xc3\x9ften Teil des Kontingents, innerhalb dieser Familie steht wiederum die Gattung Xyleborus an erster Stelle und in dieser vor allem Xyleborus mascarensis Eichh., ein tropisches Allerweltstier mit mehr als 2.300 Exemplaren und zwar ausschlie\xc3\x9flich Weibchen. An zweiter Stelle steht Xyleborus rugosipennis subsp. incertus mit 36 Weibchen. Die gro\xc3\x9fe Zahl der gefundenen Xyleborus mascarensis Eichh. mag dadurch erkl\xc3\xa4rt werden, da\xc3\x9f diese Art au\xc3\x9ferordentlich polyphag ist und \xc3\xbcberhaupt zu den h\xc3\xa4ufigsten tropischen Xyleborus-Arten z\xc3\xa4hlt. Alle Xyleborus-Arten, ebenso Sampsonius dampfi Schedl und die Platypodiden sind Ambrosiak\xc3\xa4fer und k\xc3\xb6nnen nur zur Brut schreiten, wenn frisch gef\xc3\xa4lltes oder von Wind geworfenes bezw. gebrochenes Holz vorhanden ist. Fehlt diese Voraussetzung, was besonders zeitweise in Gegenden vorkommt, die eine ausgepr\xc3\xa4gte Trockenperiode aufweisen, dann ist der K\xc3\xa4fer gezwungen, den geeigneten Zeitpunkt, den Beginn der Regenzeit, abzuwarten und dies gibt eine Erkl\xc3\xa4rung f\xc3\xbcr das h\xc3\xa4ufige Vorkommen in den oberen Bodenschichten.
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  • 58
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    Copepoda associated with West Indian Invertebrates \xe2\x80\x93 II Cancerillidae, Micropontiidae (Siphonostoma) (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 15 no. 1, pp. 1-23
    Details
    Publication Date: 2024-01-12
    Description: Our thanks are due to Mrs. R. E. TEAGLE, British Museum (Natural History), London, and Dr. ELISABETH DEICHMANN, Museum of Comparative Zo\xc3\xb6logy, Harvard College, Cambridge, for identifying the echinoderm hosts from Cura\xc3\xa7ao and Jamaica respectively. Support by grants from the Netherlands Foundation for the Advancement of Research in Surinam and the Netherlands Antilles (WOSUNA), Amsterdam, and the National Science Foundation of the United States is also acknowledged.\nPaper number I in this series appeared in Studies Fauna Cura\xc3\xa7ao 13, no. 56, p. 1\xe2\x80\x9420 (1962).
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  • 59
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    A palynological study on the Quaternary of British Guiana (1963)
    In:  Leidse Geologische Mededelingen vol. 29 no. 1, pp. 125-168
    Details
    Publication Date: 2024-01-12
    Description: Pollen diagrams have been prepared of eight sections of Quaternary sediments from different localities on the coastal plain of British Guiana, and partly dated with the C 14 method. A Riss-W\xc3\xbcrm interglacial transgression, a W\xc3\xbcrm-glacial regression and a Holocene transgression have been established. The W\xc3\xbcrm-glacial vegetation on the place of the present coastal plain area was a poor grass-savanna type. The Holocene transgression at about 9500 B.P. is represented at 23 m. below present sea level and the maximum attained around 6500 B.P. when the relative sealevel was at least 2\xc2\xbd m. above that at present.
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  • 60
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    Successive Hercynian structures in some areas of the Central Pyrenees (1963)
    In:  Leidse Geologische Mededelingen vol. 28 no. 1, pp. 103-176
    Details
    Publication Date: 2024-01-12
    Description: In the central part of the axial zone of the Pyrenees five distinct phases of folding have been distinguished from the study of minor structures. Traces of a very early phase have been found only in the northern and southern part of the region, which appear on the map as oblique fold structures, and are most prominent from the divergency of lineations and fold axes in these parts of the region. The present aspect of the mountain chain is primarily due to the effects of the main phase in which strong compression produced tight but non isoclinal folds with axial plane slaty cleavage. In the Garonne Dome the slaty cleavage was initially flatlying, in general parallel to the bedding, but occasional folds with crosscutting cleavage have been found. Steep slaty cleavage folds of the Devonian overlying the flatlying slaty cleavage folds of the Cambro-Ordovician of this dome form a beautiful example of disharmonie folding. The main phase slaty cleavage has been found to be folded in the greater part of the area investigated, generally by small minor accordion folds. In several areas two phases of refolding have been distinguished, one with a trend diagonal to the orogene, one parallel, E\xe2\x80\x94W. The intensity of the refolding is strongest in the oldest strata of the sequence. The succession of phases is evident from the folding of the planes of reference and twisting of the lineations. The patterns of the stereographic plots of data do not always show clear evidence of the succession. Knick zones accompanied the end of the Hercynian history of the mountain chain which mainly consisted of arching of the orogene, together with faulting and blockwise tilt. This period of deformation shows several characteristics of tensional stress.
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  • 61
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    Notes on some specimens of the genus Plecotus Geoffroy, 1818 (Mammalia, Chiroptera) from the Netherlands (1963)
    In:  Beaufortia vol. 10 no. 113, pp. 7-18
    Details
    Publication Date: 2024-01-12
    Description: In 1912, MILLER united all the West European bats with very long ears joined across the forehead and with 36 teeth into one species, Plecotus auritus (LINNAEUS, 1758). By doing so he followed BLASIUS (1857), DOBSON (1878) and TROUESSART (1910). This situation, one species without subspecies, remained till 1940. In that year V. & E. MARTINO described a subspecies of the Long-eared Bat, Plecotus auritus meridionalis, based on animals from Slovenia, Yugoslavia. The animals were characterized by having larger skulls than the bats in Northern Europe.\nIn 1957, BAUER studied a collection of bats from Spain. He described a new subspecies, Plecotus auritus hispanicus, on bats from the surroundings of Linares de Riofrio, Salamanca. The bullae auditori of the Spanish animals were smaller than those of animals from Austria. The bats from Salamanca were more yellow-brown-coloured than the animals from Austria; the latter were grey-coloured with a brownish hue. From the description of BAUER (1957) it is clear that the author came across a taxonomic problem he could not explain at that time.
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  • 62
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    On red coloured shrimps (Decapoda, Caridea) from tropical land-locked saltwater pools (1963)
    In:  Zoologische Mededelingen vol. 38 no. 16, pp. 261-279
    Details
    Publication Date: 2024-01-12
    Description: In a number of widely separated places in the tropics, both in the Atlantic and in the Indo-West Pacific, bright red coloured caridean shrimps have been reported from a most peculiar habitat. This habitat is formed by salt water pools which are seemingly shut off from the sea and are often situated at a considerable distance from the shore; these pools, however, must have an underground connection with the sea as their water level falls and rises with the tides. In several instances the pools are in total darkness (in caves) or in semi-darkness.\nApart from this habitat and their red colour, the six species of shrimps so far observed in these pools have very little in common: they belong to 5 different genera and represent 3 different families. All of them seem to be restricted to this type of habitat. It is the object of this paper to bring together all the available information on these species so as to draw the attention to this curious phenomenon.\nIn the paragraphs "Material examined" the following abbreviations have been used to indicate the institutions where the material is deposited: I.R.S.M. = Institut de Recherches Scientifiques de Madagascar, Tananarive; R.M.N.H. = Rijksmuseum van Natuurlijke Historie, Leiden; U.S.N.M. = United States National Museum, Washington, D.C.\n\nATYIDAE\nHalocaridina new genus Definition. \xe2\x80\x94 Atyid prawns of small size. Rostrum unarmed. Carapace without supra-orbital, antennal or pterygostomian spines. Telson with two pairs of dorsal spines. Eyes reduced, but with pigment. Carpus of both first and second cheliped deeply excavated anteriorly. Palm of chelipeds distinct.
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  • 63
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    Distribution maps of Pacific plants (1963)
    In:  Pacific Plant Areas vol. 1 no. 1, pp. 247-297
    Details
    Publication Date: 2024-01-12
    Description: Name: Dolichandrone spathacea (L. f.) K. SCH., Fl. Kais. Wilh. Land (1889) 123.\nFamily: Bignoniace\xc3\xa6.
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  • 64
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    Bibliography of Pacific and Malaysian plant maps of Phanerogams (1963)
    In:  Pacific Plant Areas vol. 1 no. 1, pp. 9-246
    Details
    Publication Date: 2024-01-12
    Description: With the start of the publication of the Pacific Plant Areas the need was felt for a bibliography of maps which have been published in the past, even though it appeared that the majority of these maps were not up to date. The quality of the published maps varies enormously from the very clear and elaborated ones in the Pflanzenareale to the curiously aborted one of Parasponia, and to the completely hopeless tangle of lines and dots found on some other ones. Various methods have been employed, from very rough to very detailed, from mere outlines to detailed dotted localities, from a map for each taxon to several taxa on one map. Some authors have delineated tracks instead of areas, as Danser has done in his paper on Polygonaceae, without stating the fact, however. Sometimes the maps were reduced to a scale which is so small that it gave a hopeless result, especially if printed on non-glossy paper. In several cases reading the map is hardly possible without a magnifying glass, and even if the maps are clear enough it is mostly advisable to check the data with the text.\nAlso the facts on which these maps were based were various; some resulted from monographical work, others were obviously solely based on literature; many were copied time and again, especially the show-examples.
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  • 65
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    On the Neotropical Acanthocinini (Col., Cerambycidae, Lamiinae) (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 17 no. 1, pp. 57-96
    Details
    Publication Date: 2024-01-12
    Description: In continuation of my examination of the Neotropical Acanthocinini, the occasion arises to deal with certain Caribbean species, because of material from various sources, sent to me by Dr. P. WAGENAAR HUMMELINCK, of the Zo\xc3\xb6logisch Laboratorium der Rijksuniversiteit Utrecht; Ir. R. H. COBBEN, of the Laboratorium voor Entomologie der Landbouwhogeschool, Wageningen; Dr. T. H. FARR, of the Museum of Science, Kingston, Jamaica, and the Museum Frey, Tutzing bei M\xc3\xbcnchen, as well as material from my own collection.\nThe material covered in this paper comprises the following species: Lagocheirus araneiformis guadeloupensis Dillon, from St. John, St. Martin, and St. Eustatius; Fisherostylus bruneri (Fisher) gen. nov., from Cuba; Leplostyloides turbidus gen. nov., sp. n., from Saba, and St. Eustatius (pl. I 1\xe2\x80\x942); Styloleptus nigrofasciatus sp. n., from Hispaniola (pl. I 3); Styloleptus divisus sp. n., from Hispaniola (pl. I 4); Antilleptostylus nigricans (Fisher) gen. nov., from Puerto Rico; Pygmaleptostylus pygmaeus (Fisher) gen. nov., from Cuba; Atrypanius trinidadensis sp. n., from Trinidad (Pl. II 3); Urgleptes sandersoni sp. n., from Puerto Rico (Pl. II 2); Urgleptes haitiensis sp. n., from Hispaniola (Pl. II 1); Urgleptes cobbeni sp. n., from Saba, and St. Eustatius (Pl. III 1\xe2\x80\x943); Urgleptes puertoricensis sp. n., from Puerto Rico (Pl. IV 1\xe2\x80\x943); Pentheochaetes trinidadensis sp. n., from Trinidad (Pl. IV 4); Nyssodrystes freyorum sp. n., from Trinidad and Venezuela (Pl. IV 5).
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  • 66
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    Three new Species and six new Records of small Serranoid Fishes from Cura\xc3\xa7ao and Puerto Rico (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 19 no. 1, pp. 77-110
    Details
    Publication Date: 2024-01-12
    Description: Among the fishes taken during a recent collecting trip to Cura\xc3\xa7ao are three very colorful small serranoids which represent undescribed species. Two of the three new fishes are grammids of the previously monotypic genus Lipogramma, and their discovery necessitates a slight modification of the generic description. The remaining fish is provisionally placed in Chorististium (this genus may not be distinct from Liopropoma). Five other small serranids and one grammistid not known from Cura\xc3\xa7ao were also collected: Chorististium rubre, and C. mowbrayi, Serranus annularis, S. luciopercanus, Schultzea beta Pseudogramma bermudensis. Four of these fishes have also been taken in Puerto Rico for the first time and two of the new species as well.\nThe holotype of each new species has been deposited in the United States National Museum (USNM). Paratypes have been variously placed in the U.S. National Museum, Academy of Natural Sciences of Philadelphia (ANSP), Marine Laboratory of the University of Miami (UMML), Rijksmuseum van Natuurlijke Historie at Leiden (RMNH) and the University of Puerto Rico at Mayag\xc3\xbcez (UPR).
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  • 67
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    Karibische Landmilben \xe2\x80\x93 I. Uropodina (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 16 no. 1, pp. 1-58
    Details
    Publication Date: 2024-01-12
    Description: Von Herrn Dr. P. WAGENAAR HUMMELINCK, Utrecht, erhielt ich \xc3\xbcber siebzig R\xc3\xb6hrchen mit der Bitte, die darin enthaltenen und von ihm in Westindien gesammelten Landmilben zu bestimmen. Ich komme dieser Aufforderung gerne nach. Nach einem kurzen Besuch Floridas im Fr\xc3\xbchling 1960 ist es f\xc3\xbcr mich interessant, auch die Milbenfauna der Antillen kennen zu lernen und mit der Floridas zu vergleichen.\nIch werde zun\xc3\xa4chst einige Mitteilungen ver\xc3\xb6ffentlichen \xc3\xbcber die Uropodina, welche in 13 Fundorten mit 140 Exemplaren vertreten waren:
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  • 68
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    The Marine Mollusca of St. Martin, Lesser Antilles, collected by H.J. Krebs (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 16 no. 1, pp. 59-87
    Details
    Publication Date: 2024-01-12
    Description: In 1864 an anonymous list of species of the West Indian marine mollusks was published in Denmark. There were only twenty copies printed, seven of which were lost during transportation to the West Indies (CLENCH et al., 1947\xe2\x80\x941948, p. 23). The author was HENDRIK JOHANNES KREBS (1821\xe2\x80\x941907), Fig. 117, a Danish apothecary who lived on St. Thomas, Virgin Islands, from 1843 to 1870. Being the owner of a wholesale firm, he travelled throughout the West Indies, which gave him an opportunity to collect shells and plants. His species list was entitled: \xe2\x80\x9cThe West-Indian Marine Shells with some remarks. A manuscript printed for circulation between collectors.\xe2\x80\x9d It was published by W. Laub\xe2\x80\x99s Widow & Chr. Jorgensen, at Nykj\xc3\xb6bing, Falster.\nAs this work is very rare, a republication was issued by CLENCH, AGUAYO & TURNER (1947\xe2\x80\x941948). The republication is preceded by some remarks, and concludes with a portrait of KREBS, a biography and a bibliography. For more data concerning KREBS, reference should be made to this republication.
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  • 69
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    Nemerteans from Cura\xc3\xa7ao (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 17 no. 1, pp. 41-56
    Details
    Publication Date: 2024-01-12
    Description: All species treated in this paper were collected by me between January and June 1962, during my stay at the \xe2\x80\x9cCara\xc3\xafbisch Marien-Biologisch Instituut\xe2\x80\x9d (Caribbean Marine Biological Institute), Cura\xc3\xa7ao.\nI am deeply indebted to the Government of the Netherlands, which awarded me a grant enabling me to work in Cura\xc3\xa7ao; to Dr. INGVAR KRISTENSEN, Director of the Institute mentioned, for the kind hospitality shown to me; and to my friend Miss HERTHA CAPRILES, who spared no effort to make my stay on \xe2\x80\x9cdushi Corsou\xe2\x80\x9d as pleasant as possible.
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  • 70
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    Opisthobranchs from the Lesser Antilles (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 19 no. 1, pp. 1-76
    Details
    Publication Date: 2024-01-12
    Description: Thanks to help of the Government of the Netherlands, Dr. DIVA DINIZ CORR\xc3\x8aA, a lecturer in our Department, was able to work at the \xe2\x80\x9cCara\xc3\xafbisch Marien-Biologisch Instituut\xe2\x80\x9d (Caribbean Marine Biological Institute; Carmabi) Cura\xc3\xa7ao, from January to July 1962. Besides actinians and nemerteans for her own studies she collected opisthobranchs for us, sketched them alive, and took notes of their shape and colours.\nFurthermore, Dr. PIETER WAGENAAR HUMMELINCK, of Utrecht, has sent us his collections, with exception of the Aplysiidae, caught in 1930, which were already studied by ENGEL (1936).
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  • 71
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    The Turbellarian Hofstenia miamia in the Caribbean Sea (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 17 no. 1, pp. 38-40
    Details
    Publication Date: 2024-01-12
    Description: Some years ago I described Hofstenia miamia from Virginia Key, in the Miami area (CORREA 1960, p. 211 ff.). The species was based on a single specimen found among algae in the intertidal zone. When a grant from the Government of the Netherlands gave me the chance to work at the Caribbean Marine Biological Institute, Cura\xc3\xa7ao, I found the species again. Many specimens came up from Thalassia and algae growing in low water in Piscadera Baai in February and March 1962. Though these worms are only 4 mm in length, they occur sufficiently frequently to attract the attention of future workers, and are therefore published as new members of the fauna of Cura\xc3\xa7ao. Moreover the species seems to be rather common in the Caribbean Sea, as Dr. P. WAGENAAR HUMMELINCK (Utrecht) found it quite accidentally on July 17, 1955, in Deep Bay, Antigua, among algae in the low-tide zone of a rocky beach, without Thalassia.\nI take the opportunity of extending and emending my previous description by means of this larger material.
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  • 72
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    Systematics and Distribution of Siphocypraea mus and Propustularia surinamensis (Gastropoda, Cypraeidae) (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 15 no. 1, pp. 51-71
    Details
    Publication Date: 2024-01-12
    Description: The systematic place of \xe2\x80\x9cCypraea\xe2\x80\x9d mus Linn\xc3\xa9 is discussed, and it is concluded that the species belongs in Siphocypraea (Akleistostoma). The \xe2\x80\x9cvarieties\xe2\x80\x9d tuberculata Gray and bicornis Sowerby should be withdrawn; they are only forms with callosities. Callus formations are often found in Cypraeidae. The distribution has been compiled from definite locality data; it covers the Caribbean coast of Colombia, and the coast of Venezuela as far as East of Paraguan\xc3\xa1. S. mus does not occur around Cura\xc3\xa7ao or any other island of the West Indies. \xe2\x80\x9cCypraea\xe2\x80\x9d surinamensis Perry belongs in the genus Propustularia. It is a Caribbean species, localities in Africa being incorrect. The locality data are compiled from the literature, most records date from the nineteenth century. Since the species is very rare, its exact distribution remains uncertain.
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  • 73
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    Rugose corals from the carboniferous of Northern Palencia (Spain) (1963)
    In:  Leidse Geologische Mededelingen vol. 29 no. 1, pp. 1-123
    Details
    Publication Date: 2024-01-12
    Description: From Carboniferous deposits exposed on the southern slope of the Cantabric mountain chain, 58 rugose coral species are described. The rugose coral fauna of this area is not yet completely known. 32 of the species are new, 13 are unnamed and 12 are identical with or closely related to Upper Middle Carboniferous species from the Moscow and Donetz basins of Russia. These species have a fairly long stratigraphie range and their occurrence is largely conditioned by favourable environment.\nHillia is erected as a subgenus of Lithostrotionella. New genera have not been founded, existing genera have been interpreted rather widely. The species recorded belong to the following genera or subgenera: Rotiphyllum, Bradyphyllum, Amplexocarinia, Polycoelia, Sochkineophyllum, Ufimia, Cyathaxonia, Lophophyllidiurn, Stereostylus, Zaphrentites, Duplophyllum?, Euryphyllum, Lithostrotion, Arachnastraea, Clisiophyllum, Dibunophyllum, Koninckophyllum, Corwenia, Pseudozaphrentoides, Bothrophyllum, Lonsdaleia, Lithostrotionella, Hillia, Koninckocarinia, Carcinophyllum, Axolithophyllum, Lonsdaleoides, Amygdalophylloides, Ivanovia.\nThe distribution of the corals in the Carboniferous of Palencia is shown on Tables I to III (p. 108). The age of the formations from which the corals were obtained ranges from the Namurian up into the Westphalian D, as established by goniatite and plant evidence, or from the Bashkirian to the Upper Moscovian on fusulinid evidence.
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    A new forma of the species Clio pyramidata Linnaeus, 1767 and a new resting-stage of Clio pyramidata Linnaeus, 1767 forma sulcata (Pfeffer, 1879) (Gastropoda, Pteropoda) (1963)
    In:  Beaufortia vol. 10 no. 114, pp. 19-28
    Details
    Publication Date: 2024-01-12
    Description: A new form is described in the polytypic species Clio pyramidata LINNAEUS, 1767. This new forma excisa was found at 57\xc2\xb031\'S 02\xc2\xb056\'W and it is related to the forms convexa (BOAS, 1886) and sulcata (PFEFFER, 1879). The shape of the shell of the new form excisa shows a great resemblance to the shape of the shell of these two forms and also a resemblance is present to the shape of the shell of the form martensii (PFEFFER, 1880). This resemblance, however, may indicate a relationship as well as a parallel development. The new forma and the form martensii live in the same area, so that the chemo-physical characteristics of the water may have caused a parallel development. As indicated in a previous paper, the polytypic species Clio pyramidata consists of several forms which can be divided into two groups, one with the form antarctica. (DALL, 1908) as the most sourthern form and the other one with the form sulcata as the most southern one. As the new form shows a relation in shape with the forms sulcata, convexa and martensii and not with the form antarctica, it seems correct to suppose that the new form excisa belongs to the same group in the polytypic species in which the forms sulcata and convexa are placed.\nIn the same sample some specimens of the forma sulcata were present, and among these, two were in a resting-stage and one in an intermediatestage. A real resting-stage in the forma sulcata was never found before.
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    Supplement to a monograph of the Indo-Australian Clausiliidae (1963)
    In:  Zoologische Mededelingen vol. 38 no. 9, pp. 153-169
    Details
    Publication Date: 2024-01-12
    Description: Since the publication of my monograph of the Indo-Australian Clausiliidae (Loosjes, 1953) I obtained some additional information, consisting mainly of new distribution records and data on shell-structures. The present paper deals with these additional data, while furthermore two new species are described.\nThe specimens concerned were obtained on loan from the following Museums: Zo\xc3\xb6logisch Museum, Amsterdam (Z.M.A.), Rijks Museum van Natuurlijke Historie, Leiden (R.M.N.H.), Museo Civico di Storia Naturale di Genova (M.C.G.), Natur-Museum Senckenberg, Frankfurt am Main (S.M.F.), Ueberseemuseum, Bremen (U.M.B.).\nMy thanks are due to Mrs. W. S. S. van der Feen-van Benthem Jutting, Dr. C. O. van Regteren Altena, Prof. Dr. E. Tortonese, Dr. A. Zilch, Dr.\nH. Knipper, Dr. M. A. Lieftinck, Mr. L. J. M. Butot, Mr. A. M. R. Wegner and to the owners of the private collections mentioned below.\nPhaedusa H. & A. Adams, 1855 Sectio Phaedusa Phaedusa corticina corticina (L. Pfeiffer, 1842) 1953 Loosjes, p. 17 1954 Zilch, p. 31 1954 Knipper, p. 260 1959 Van Benthem Jutting, p. 127 (Ph. corticina) West Java Radjamandala, altitude 650 m, leg. J. M. A. van Groenendael, 1939 (L. J. M. Butot collection, 3 specimens); dimensions (in mm) : shell aperture number of whorls
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  • 76
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    Observations on the North African serotine bat, Eptesicus serotinus isabellinus (Temminck, 1840) (Mammalia: Chiroptera) (1963)
    In:  Zoologische Mededelingen vol. 38 no. 12, pp. 207-212
    Details
    Publication Date: 2024-01-12
    Description: Eptesicus isabellinus was originally described as Vespertilio isabellinus by Temminck (1840, p. 205, pl. 52 figs. 1, 2) from a series of specimens obtained by J. F. H. Clifford Cocq van Breugel in the vicinity of Tripoli, Libya. Unfortunately Temminck\'s original description did not include any cranial measurements and as a result the precise affinities of this bat have been uncertain ever since. Lataste (1887, p. 625) described a small serotine bat from the vicinity of Cairo, which he named Vesperugo (Vesperus) Innesi. He stated that he had compared this with a specimen of E. isabellinus (the essential data of which were not given) and that E. innesi was smaller.\nLataste evidently regarded E. isabellinus as a form of E. serotinus (Schreber, 1774). Once again, however, full cranial measurements were not given for the new form E. innesi. Harrison (1962) re-examined the lectotype and other specimens of E. innesi in the British Museum; extracted the skull of the lectotype and gave full cranial and external measurements. Setzer (1957, p. 40) in his review of Libyan mammals, treated E. isabellinus as a distinct species and stated that it had not been taken since Temminck\'s description. He noted that Zavattari (1934, p. 887) listed it as Vespertilio serotinus isabellinus. Allen (1939, p. 87) also listed it as a subspecies of E. serotinus. Ellerman & Morrison-Scott (1951, p. 156) treated E. isabellinus as a distinct species on the grounds that the measurements given by Tate (1942, p. 275) were too small for E. serotinus and they regarded Lataste\'s small species E. innesi as a subspecies of it.\nIn view of all this uncertainty it seemed essential to re-examine the original type material of E. isabellinus and make direct comparisons with E. innesi and the European E. serotinus in order to finally clarify its status. Three
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  • 77
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    Indo-malayan and Papuan fig wasps (Hymenoptera, Chalcidoidea) : 2. The genus Pleistodontes Saunders (Agaonidae) (1963)
    In:  Zoologische Mededelingen vol. 38 no. 19, pp. 303-321
    Details
    Publication Date: 2024-01-12
    Description: Until now, the genus Pleistodontes Saunders is known from the Australian continent and from Lord Howe Island. Two species were introduced into the Hawaiian Islands.\nSamples of fig wasps from New Guinea and from the Solomon Islands were sent to me by Mr. E. J. H. Corner. They proved to consist of new species of Pleistodontes, which are described below. In addition, some new records of Australian species, mostly taken from the collection of the Hawaiian Sugar Planters\' Association ("H.S.P.A."), Honolulu, are given, and the type species of the genus is redescribed. The records and "descriptions" by Girault are not considered in the present paper, as the typical material is being studied by Mr. E. F. Riek.\nA discussion on the host records follows the descriptions of the species.\nPleistodontes blandus spec. nov.\nMaterial. \xe2\x80\x94 Eight immature \xe2\x99\x80, 14 \xe2\x99\x82, ex Ficus glandifera Summerh. (det. E. J. H.\nCorner), Solomon Is., leg. Kajewski, no. 3494; coll. Museum Leiden, no. 438; holotype, \xe2\x99\x82, slide no. 438b, allotype, \xe2\x99\x80, slide 438a, paratypes, \xe2\x99\x80 \xe2\x99\x82, slides 438c, d.\nDescription. \xe2\x80\x94 Male. Head (fig. 10) distinctly longer than its maximum width, and nearly twice as long as wide anteriorly; with the usual pubescence next to the antennal groove and behind the hypostomal margin. Eyes large.\nMandible, fig. 9. Labium and maxillae (fig. 6): the labium bare, the maxillae with two long hairs on the ventral lobes. Antenna, fig. 8. The scape twice as long as wide, with some hairs on the antaxial surface; the pedicel thrice as long as wide, about half as long as the scape, with one antaxial hair at mid length; the third and fourth segments subequal, incompletely separated, the third segment with two antaxial hairs, the fourth with one
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  • 78
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    Notes on new or rare marine fishes from Surinam (1963)
    In:  Zoologische Mededelingen vol. 38 no. 18, pp. 295-301
    Details
    Publication Date: 2024-01-12
    Description: The fish collection of the Leiden Museum has recently been enriched by the donation of a few small or moderate collections of fishes assembled in tropical Atlantic America. As these proved to contain some representatives of species rarely encountered or even new to science and, moreover, provided interesting distributional information, publication of a few notes containing the principal data seems of interest.\nNote I. \xe2\x80\x94 A collection of about 40 specimens from Surinam, representing 29 species mostly marine, was received from Ir. Z. Salverda, who appears to have collected them himself. Unfortunately, Ir. Salverda omitted adding more detailed locality information, but all marine species can be expected to occur throughout the whole of the coastal region. Two of these species, each represented by a single example, seem of sufficient interest to be recorded here in the present and the second note.\nCarcharhinus porosus (Ranzani) Carcharhinus porosus, Bigelow & Schroeder, 1948, pp. 394-399, figs. 74, 75. 1 ex., 267 (355) mm, \xe2\x99\x82, RMNH reg. no. 24704, Surinam.\nIt is remarkable that Bigelow & Schroeder seem to have recorded the first specimen(s) from Surinam while, considering their references, the species, though differently named, has been known to occur in both French and British Guiana waters for more than a hundred years. As Bigelow & Schroeder state that nothing is known of the habits of the present species, merely adding that it is probably a littoral species, I surmise that the species is not abundant.\nThe specimen completely agrees with Bigelow & Schroeder\'s extensive description; the teeth seem to number 13 + 1 + 13/12 + 1 + 12.
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  • 79
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    Reviews (1963)
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 12 no. 1, pp. 173-176
    Details
    Publication Date: 2024-01-12
    Description: An account of phytochemical substance has been provided by Wiesner\xe2\x80\x99s Rohstoffe des Pflanzenreichs, arranged by products, another account has been given by Karrer, compounds of established constitution arranged according to a chemical system. Though useful, none of these works, including also those of Czapek and Wehmer, aims, however, to use phytochemistry as an auxiliary branch of plant taxonomy.\nIt does seem necessary here to stress in a concise way the importance of the subject for taxonomy. All of us have used some coarse phytochemical characters, looked at characteristic glands and crystals, observed and used colours of dried leaves, tasted plants for bitter substances, sniffed at aromatic oils, and other secondary compounds. The use of these characters as arguments for taxonomic purpose has, however, been erratic and only been employed if very obvious and/or abundant. Everyone of us looked for refinement of the aspect. This is the principal aim of the present endeavour.
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  • 80
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    Reduction of Gagnepain\xe2\x80\x99s genera Cryptanthela, Dimerodiscus, and Tridynamia (Concolvulaceae) (1963)
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 12 no. 1, pp. 39-40
    Details
    Publication Date: 2024-01-12
    Description: In Notulae Systematicae 14, fasc. 1 (1950) 24\xe2\x80\x9427, Gagnepain published three new genera of Convolvulaceae, viz. Cryptanthela (l.c. p. 24), Dimerodiscus (l.c. p. 25), and Tridynamia (l.c. p. 26), each of them based on a single species. These species are respectively Cryptanthela sericea Gagnep., Dimerodiscus fallax Gagnep., and Tridynamia eberhardtii Gagnep., all found in Indo-China. The types are preserved in the Paris Herbarium.\nThrough the kindness of the Director of the Phanerogamic division of the \xe2\x80\x9cMuseum National d\xe2\x80\x99Histoire Naturelle\xe2\x80\x9d in Paris, I had the opportunity to study the types, with the following result.
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  • 81
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    Les Collemboles Poduromorphes du Surinam (1963)
    In:  Studies on the Fauna of Suriname and other Guyanas vol. 6 no. 1, pp. 43-51
    Details
    Publication Date: 2024-01-12
    Description: Avant d\xe2\x80\x99aborder l\xe2\x80\x99\xc3\xa9tude des poduromorphes du Surinam, je remercie mon Ma\xc3\xaetre Cl. Delamare Deboutteville qui a bien voulu me confier l\xe2\x80\x99\xc3\xa9tude de ceux-ci r\xc3\xa9colt\xc3\xa9s par Monsieur J. van der Drift. Dans ce mat\xc3\xa9riel j\xe2\x80\x99ai trouv\xc3\xa9 trois esp\xc3\xa8ces de poduromorphes dont une nouvelle pour la science.\nCes esp\xc3\xa8ces sont les suivantes: Brachystomella parvula (Sch\xc3\xa4ffer 1896), Arlesia albipes (Folsom 1927), Neotropiella vanderdrifti n.sp.
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  • 82
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    A new subspecies of the Scorpion Rhopalurus Hasethi (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 15 no. 1, pp. 102-117
    Details
    Publication Date: 2024-01-12
    Description: In his paper on \xe2\x80\x9cScorpions\xe2\x80\x9d from Cura\xc3\xa7ao, Aruba, Bonaire and the Venezuelan Islands, WAGENAAR HUMMELINCK (Stud. fauna Cur. 2, 1940, p. 141) drew attention to the fact that specimens of Rhopalurus hasethi from the island of Aruba possess, on the average, four pectinal teeth less than specimens from Cura\xc3\xa7ao, the island from which the species was originally described. Lack of time and material prevented this author from paying full attention to other differences. He confined himself to giving a small table, in which the following numbers of pectinal teeth were reported, without a distinction being made between males and females.\nCura\xc3\xa7ao (85 specimens) (22\xe2\x80\x94) 25 \xe2\x80\x94 27.0 \xe2\x80\x94 29 (\xe2\x80\x9430) Bonaire (38 specimens) 24 \xe2\x80\x94 26.6 \xe2\x80\x94 28 (\xe2\x80\x9429) Ave de Barlovento (4 specimens) 24 \xe2\x80\x94 25.4 \xe2\x80\x94 27 Aruba (19 specimens) 21 \xe2\x80\x94 23.1 \xe2\x80\x94 25
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  • 83
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    Copepoda associated with West Indian Invertebrates \xe2\x80\x93 III The Genus Anthessius (Cyclopoida, Myicolidae) (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 17 no. 1, pp. 1-37
    Details
    Publication Date: 2024-01-12
    Description: For the identification of certain of the mollusks with which the copepods to be described were associated we wish to thank Dr. RUTH D. TURNER, Museum of Comparative Zo\xc3\xb6logy, Harvard College, Cambridge, and Mr. C. J. VAN EEKEN, Zo\xc3\xb6logisch Museum, Amsterdam. We also express our appreciation to Mr. J. A. VAN DREVELDT (Amsterdam) for his assistance in the preparation of the drawings of the last two species.\nThis study has been supported by grants from the Netherlands Foundation for the Advancement of Research in Surinam and the Netherlands Antilles (WOSUNA), Amsterdam, and from the National Science Foundation of the United States, Washington.
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  • 84
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    Shallow water Holothurians known from the Caribbean waters (1963)
    In:  Studies on the Fauna of Cura\xc3\xa7ao and other Caribbean Islands vol. 14 no. 1, pp. 100-118
    Details
    Publication Date: 2024-01-12
    Description: The most important contribution to our knowledge about the holothurian fauna of the islands along the coast of northern South America is ENGEL\xe2\x80\x99S brief report of 1939, based on Dr. WAGENAAR HUMMELINCK and earlier workers collections, up to the year 1936. His list comprises 13 species, of which all except Pentacta pygmaea (Th\xc3\xa9el) are included in HUMMELINCK\xe2\x80\x99S recent collections, which furthermore adds four more species. This expanded list is almost identical with that which recently has been compiled for the Puerto Rican waters, and with the inclusion of a few more species known from Surinam, Trinidad and Jamaica, etc., it looks as if now one has a fairly complete list of all the shallow water holothurians which occur in the Caribbean region.\nAfter the identification of HUMMELINCK\xe2\x80\x99S new material had been completed, Mr. ELISHA S. TIKASINGH (1963) has produced a more extensive report on \xe2\x80\x98The shallow water Holothurians of Cura\xc3\xa7ao, Aruba and Bonaire\xe2\x80\x99, which will be of much help to the students of holothurians in the southern part of the Caribbean.
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  • 85
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    Origin of the Stephanian Red Beds in the Ocejo Basin (Prov. of Leon, Spain) (1963)
    In:  Leidse Geologische Mededelingen vol. 28 no. 1, pp. 377-387
    Details
    Publication Date: 2024-01-12
    Description: In the valley of Ocejo (prov. Le\xc3\xb3n) a series of alternating conglomerates, sandstones, siltstones, and shales with a red colour are found. This series is 180 m thick, of Stephanian B + C age, and at present dips \xc2\xb1 30\xc2\xb0W.\nSedimentological analysis gives the following data: (1) quartz is the dominant detrital mineral, hematite and clay form the cement; (2) the components of the conglomerates are chiefly limestones of cobble size, the fine-grained sediments and matrices being chiefly siltstones with varying admixtures of clay size material; (3) the limestone pebbles have low roundness- and flatness-index values.\nThe sediment was deposited by torrents at the foot of a rising mountain area. The source region had a thick cover of red soil on top of limestones. Rapid erosion in these elements caused the deposition of limestone conglomerates in a red matrix during a period in which the climate was warm and humid.
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  • 86
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    Studies on the Genus Orbitolina (Foraminiferida) (1963)
    In:  Leidse Geologische Mededelingen vol. 29 no. 1, pp. 181-253
    Details
    Publication Date: 2024-01-12
    Description: The genus Orbitolina is described in detail and is shown to be represented by one species only: Orbitolina lenticularis (Blumenbach). This species can be subdivided into form-groups, based on the characteristics of the megalospheric embryonic apparatus. The evolution of the species is orthogenetic. The specimens probably lived with the apex of the cone pointed downward.\nThe microspheric test starts with a strepto-spiral, the megalospheric test with an embryonic apparatus consisting of a proloculus, a deuteroconch, and a varying number of epiembryonic chambers. The embryonic apparatus is the only consistent feature on which the age of Orbitolina can be determined; the method applied will be described. The neanic chamber layers consist of tubular chamber passages; the chamber layers are interconnected by oblique, aligned stolons, placed alternately left and right of the chamber passages.\nThe contemporaneous allies Coskinolinoides texanus Keijzer, Dictyoconus walnutensis (Carsey), Orbitolinopsis kiliani (Prever), Dictyoconus floridanus (Cole) subsp. elongata (Moullade) and Simplorbitolina manasi Ciry & Rat are described and some remarks are presented on the family Orbitolinidae.
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  • 87
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    Tertiary and Quaternary sedimentation in the Conflent (1963)
    In:  Leidse Geologische Mededelingen vol. 28 no. 1, pp. 297-319
    Details
    Publication Date: 2024-01-12
    Description: S\xc3\x89DIMENTATION PLIOC\xc3\x88NE ET QUATERNAIRE DANS LE CONFLENT, FOSS\xc3\x89 INTRAMONTAGNEUX DANS LES PYR\xc3\x89N\xc3\x89\nES ORIENTALES\nCette contribution contient quelques r\xc3\xa9sultats d\xe2\x80\x99\xc3\xa9tudes s\xc3\xa9dimentologiques sur les d\xc3\xa9p\xc3\xb4ts plioc\xc3\xa8nes at quaternaires remplissant le foss\xc3\xa9 qui traverse les Pyr\xc3\xa9n\xc3\xa9es orientales en direction oblique. Les donn\xc3\xa9es s\xc3\xa9dimentologiques pourront fournir quelques indications sur les conditions de d\xc3\xa9p\xc3\xb4t et sur la provenance de ces assises, ainsi que sur le climat.\nPour les couches rouges de Codalet, remplies de fragments de schiste, l\xe2\x80\x99opinion de Bourcart selon laquelle elles ont \xc3\xa9t\xc3\xa9 form\xc3\xa9es par des coul\xc3\xa9es boueuses, est confirm\xc3\xa9e. Elles proviennent de sols rouges form\xc3\xa9s avant le Plioc\xc3\xa8ne sur les schistes du Pal\xc3\xa9ozoique Ancien.\nLes arkoses de Marquixanes, contenant des cailloux de granite, indiquent un climat plus sec. Ces deux d\xc3\xa9p\xc3\xb4ts datent, selon Bourcart, du d\xc3\xa9but du Plioc\xc3\xa8ne.\nL\xe2\x80\x99assise d\xe2\x80\x99Escaro, \xc3\xa0 grands blocs, montre la transition de d\xc3\xa9position par coul\xc3\xa9es boueuses vers une s\xc3\xa9dimentation fluviale. La diff\xc3\xa9rence entre la composition des cailloux et des min\xc3\xa9raux lourds de ce d\xc3\xa9p\xc3\xb4t et celle dans les d\xc3\xa9p\xc3\xb4ts actuels montre que les conditions \xc3\xa9taient bien diff\xc3\xa9rentes: le massif du Canigou \xc3\xa9tait bien moins \xc3\xa9lev\xc3\xa9 qu\xe2\x80\x99aujourd\xe2\x80\x99hui et en partie couvert de sols jaunes, parfois m\xc3\xaame rouges.\nL\xe2\x80\x99assise de Tern\xc3\xa8re, qui en partie remplace celle d\xe2\x80\x99Escaro vers l\xe2\x80\x99E, est plut\xc3\xb4t un produit de s\xc3\xa9dimentation torrentielle. Il est probable que ces deux assises datent de la fin du Plioc\xc3\xa8ne et m\xc3\xaame qu\xe2\x80\x99elles pourront \xc3\xaatre contemporaines des Sables d\xe2\x80\x99Ille.\nCes derni\xc3\xa8res sont des d\xc3\xa9p\xc3\xb4ts fluviaux typiques. Les intercalations argileuses ont fourni un ensemble pollinique et des fragments d\xe2\x80\x99os de Rhinoceros etruscus (Falc.) qui indiquent un \xc3\xa2ge fin-Plioc\xc3\xa8ne ou Villafranchien.\nTous ces d\xc3\xa9p\xc3\xb4ts ont \xc3\xa9t\xc3\xa9 affect\xc3\xa9s par des mouvements tectoniques, d\xc3\xa9j\xc3\xa0 d\xc3\xa9crits ant\xc3\xa9rieurement, qui ont accompagn\xc3\xa9 la surrection de la cha\xc3\xaene pyr\xc3\xa9n\xc3\xa9enne pendant le Plioc\xc3\xa8ne et le d\xc3\xa9but du Quaternaire.
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  • 88
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    Erg\xc3\xa4nzende Beschreibungen und Bemerkungen zu Indonesischen Arten aus den Unterfamilien Dryophthorinae und Cossoninae (Coleoptera, Curculionidae) (176. Beitrag zur Kenntnis der Curculioniden) (1963)
    In:  Beaufortia vol. 9 no. 109, pp. 219-231
    Details
    Publication Date: 2024-01-12
    Description: Durch freundliche \xc3\x9cbermittlung seitens Herrn Dr. L. G. E. Kalshoven, Blaricum, wurde mir aus den Museen zu Amsterdam und Leiden weiteres Material aus den Unterfamilien Dryophthorinae und Cossoninae zu Studienzwecken \xc3\xbcbersandt, wof\xc3\xbcr ich auch an dieser Stelle meinen besten Dank aussprechen m\xc3\xb6chte. Es erm\xc3\xb6glichte die Klarung von Zweifelsfragen, die sich ergeben hatten, sowie die Beschreibung einiger weiterer Arten aus verschiedenen Gattungen dieser zum Teil umfangreichen Unterfamilien.\nDie Holotypen der von Drescher, Jacobson und Mj\xc3\xb6berg gesammelten neuen Arten sind im Zoologischen Museum, Amsterdam, diejenigen des von Kalshoven gesammelten Materials im Rijksmuseum van Natuurlijke Historie, Leiden aufgehoben. Fur die liebensw\xc3\xbcrdige \xc3\x9cberlassung von Paratypen bin ich Herrn Dr. Kalshoven sehr dankbar.
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  • 89
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    Some notes on the distribution and the ecology of the amphipod Gammarus fossarum Koch, 1835, in the Netherlands (Crustacea, Malacostraca) (1963)
    In:  Beaufortia vol. 10 no. 116, pp. 40-43
    Details
    Publication Date: 2024-01-12
    Description: Gammarus fossarum Koch, 1835 est une esp\xc3\xa8ce commune dans la partie sud du Limbourg (Pays-Bas), o\xc3\xb9 elle est pr\xc3\xa9sente dans l\xe2\x80\x99eau douce, non polluee, d\xe2\x80\x99un pH de 6,2 \xc3\xa0 7,0. Les \xc3\xa9tudes en campagne, effectu\xc3\xa9es en 1962 d\xc3\xa9montrent la pr\xc3\xa9sence de l\xe2\x80\x99esp\xc3\xa8ce \xc3\xa0 six localit\xc3\xa9s en dehors du Limbourg, c\xe2\x80\x99est-\xc3\xa0-dire pr\xc3\xa8s d\xe2\x80\x99Arnhem et de Nim\xc3\xa8gue, o\xc3\xb9 elle vit dans les m\xc3\xaames conditions qu\xe2\x80\x99au Limbourg. D\xe2\x80\x99ailleurs, il y a un \xc3\xa9chantillon de Gammarus fossarum au Mus\xc3\xa9e zoologique d\xe2\x80\x99Amsterdam, ramass\xc3\xa9 en 1949 dans un ruisseau dans la commune de Gendringen (la Gueldre), mais des recherches plus r\xc3\xa9centes ne d\xc3\xa9couvrirent pas sa pr\xc3\xa9sence en cet endroit, fait probablement attribuable \xc3\xa0 la pollution actuelle de ses eaux.\nDans 60% des localit\xc3\xa9s connues dans les Pays-Bas Gammarus fossarum coexiste avec Gammarus pulex. Leurs aires de r\xc3\xa9partitoin se recouvrent considerablement. Des hybrides ne sont pas encore connus, ni dans la nature, ni obtenus exp\xc3\xa9rimentalement. D\xe2\x80\x99ailleurs, la morphologie des m\xc3\xa2les adultes est tr\xc3\xa8s diff\xc3\xa9rente.\nAinsi, Gammarus fossarum est consid\xc3\xa9r\xc3\xa9 ici comme une bonne esp\xc3\xa8ce et pas comme une sous-esp\xc3\xa8ce de Gammarus pulex.
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  • 90
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    Entwicklungsstufen der mioz\xc3\xa4nen Cricetodontinae (Mammalia, Rodentia) Mittelspaniens und ihre stratigraphische Bedeutung (1963)
    In:  Beaufortia vol. 10 no. 119, pp. 51-157
    Details
    Publication Date: 2024-01-12
    Description: During the summer holidays of 1960 to 1963 a great many localities of Miocene and Pliocene mammals were discovered in the Southern part of Zaragoza province (Spain).\nRemains of both large and small mammals were found, the latter by sieving clays and marls. This small fauna consists mainly of Cricetodontinae, Gliridae, Sciuridae, Lagomorpha and Insectivora.\nThe object of the present study is the Cricetodontinae. Other families of the same localities will be described by H. de Bruyn of the State University of Utrecht, Netherlands. The localities are situated along the S.W. border of the Calatayud-Teruel basin. Apart from small local faulting and folding along the margin of the basin the sediments are undisturbed. This circumstance and the nearly continuous exposures made it possible to determine the relative stratigraphic position of the sites. With the stratigraphic succession as a directive it proved to be possible to follow the evolution of the Cricetodontinae step by step. The Cricetodon material found in the region falls into four groups. Within each group species are closely related. 1. The group minor (based on Cricetodon minor LARTET, 1851) comprises small species with elongated M1. The oldest member of this group is Cricetodon minor primitivus n. ssp. from the Valtorres locality near Calatayud. This form develops to C. collongensis MEIN, 1958, from Vieux-Collonges (France). The author considers this to be a subspecies of C. minor LARTET. Cricetodon minor collongensis was found in several Spanish localities. The evolutionary development of this form appears to be C. minor minor LARTET on the one side and C. gregarius SCHAUB, 1925 on the other. Representatives of both branches were found in the Calatayud-Daroca region. In the course of time members of the gregarius branch grow gradually larger, whereas in the minor branch they stay of about the same size. 2. The group larteti (based on Cricetodon larteti SCHAUB, 1925) comprises species of medium size. The molars are short and broad, squarishly built, and show definite reduction. The early and middle Miocene ancestors of Cricetodon larteti were now discovered in Spain, namely C. koenigswaldi n.sp. and C. darocensis n.sp. The most notable feature of the evolutionary trend in this group is a gradual increase in size. 3. The group affinis (based on Cricetodon affinis SCHAUB, 1925) comprises species of small and medium size. The molars are squat and show little reduction. C. brevis SCHAUB is synonymous with C. affinis. The type specimen of C. brevis from La Grive-St. Alban (France) is considered to be a small specimen of C. affinis. Cricetodon brevis from Sansan, being markedly different from the above mentioned, had better be named Cricetodon cf. vindoboniensis SCHAUB & ZAPFE, 1953.\nIt is fairly certain that the species from Villafeliche II A (Spain) is identical to the latter. 4. The group sansaniensis (based on Cricetodon sansaniensis LARTET, 1851) comprises large species. The molars have high relief and fat cusps. Only one locality (Manchones) provided sufficient material for analysis. Comparison of this material with finds from France and North-Spain led to the conclusion that there are two identical lines of evolution within the group. These are most probably closely related, though the common ancestor is not yet known. One branch leads from C. meini n.sp. (from Vieux-Collonges) through a somewhat more highly developed member (from Manchones) to C. decedens (from La Grive-St. Alban, and the Valles-Penades). The other branch, which is also known from Vieux-Collonges, though not yet described, leads to sansaniensis from Sansan. Cricetodon sansaniensis from La Grive seems somewhat more developed and might well be called C. rhodanicus DEPERET. The highest developed member of this branch is found in the Valles-Penades (not yet described).\nWith the above mentioned data of the evolutionary trends in the Cricetodontinae it was tried to correlate some of the well-known Miocene localities in France with the sites in the Calatayud-Daroca region (fig. 17). There proved to be a good agreement between miocene Cricetodon fauna of Spain and France, whereas no similarity was found with the North-African fauna from Beni-Mellal (Morocco). Comparison of the living species Cricetus cricetus canescens NEHRING and Mesocricetus auratus (WATERHOUSE) with the Cricetodontinae of Western Europe shows that none of these can be an ancestor of the recent Cricetinae. Certain primitive characters of the dentition of Cricetus have already disappeared in all known Cricetodontinae. The oligocene genus Cricetops from Mongolia is the only one that more or less satisfies the demands one should theoretically make on an ancestor of the Cricetinae. It is probable that the Cricetinae are originally an Asiatic family, arriving in Europe more or less at the same time as Hipparion and crowding out the Cricetodontinae. The common ancestor of Cricetodontinae and Cricetinae is at least of Oligocene age.
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  • 91
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    Zoological Results of a Collecting Journey to Yugoslavia, 1954. 7: Harpacticiden (Crustacea Copepoda) von der dalmatinischen K\xc3\xbcste (1963)
    In:  Beaufortia vol. 10 no. 112, pp. 257-262
    Details
    Publication Date: 2024-01-12
    Description: Das Mittelmeer geh\xc3\xb6rt zu den im Hinblick auf seine Besiedlung mit Harpacticiden am besten untersuchten Gebieten der Erde. Es wird darin nur von der europ\xc3\xa4ischen Atlantikk\xc3\xbcste \xc3\xbcbertroffen. Die von mir in der vorliegenden Arbeit gemeldeten Arten waren alle bereits aus dem Mittelmeerbereich bekannt. Erstmalig f\xc3\xbcr das adriatische Meer wurden davon festgestellt Von der K\xc3\xbcste des adriatischen Meeres bereits bekannt, aber vom jugoslavischen K\xc3\xbcstenabschnitt noch nicht gemeldet waren Eudactylopus robustus und Amonardia normani.\nDiarthrodes ponticus, Amphiascus angustipes, die nun auch an der jugoslavischen K\xc3\xbcste nachgewiesen sind.\nSchizopera jugurtha stephanidesi und Nitocra spinipes, PESTA bekannte Form wird als eine Unterart von Die bisher als Schizopera stephanidesi Schizopera jugurtha aufgefasst.
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  • 92
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    A Comparative Study of the Feeding Mechanisms of some African Cyprinidae (Pisces, Cypriniformes) (1963)
    In:  Bijdragen tot de dierkunde vol. 33 no. 1, pp. 3-35
    Details
    Publication Date: 2024-01-12
    Description: Although there exists an extremely voluminous literature on Cyprinid fishes and the morphology and physiology of some species has been intensively studied by various authors, very little is yet known about feeding mechanisms and their functioning in most members of this family.\nSo far as known, only some European species \xe2\x80\x94 e.g. Cyprinus carpio, Carassius auratus, Rutilus rutilus Gobio gobio \xe2\x80\x94 one Asian (Labeo rohita), and one African (Labeo horie) have been investigated thoroughly as regards their morphology in relation to their feeding habits. Moreover ,the ecology of most African species is only scantily known.
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  • 93
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    Cyperaceae (1963)
    In:  Flora of the Netherlands Antilles vol. 1 no. 2, pp. 89-120
    Details
    Publication Date: 2024-01-12
    Description: Annual or perennial grass-like herbs with short or long rhizomes. Culms trigonous to triquetrous or rarely cylindric and septate (Cyperus articulatus). Leaves narrow, with closed sheaths, sometimes with a ligule opposite to the blade. Inflorescence consisting of a solitary spikelet or capitulum, or many spikelets in heads or spikes or simple to compound umbels. The branches often subtended by conspicuous bracts. Flowers in the axil of a glume, bisexual or unisexual, usually consisting of 1\xe2\x80\x943 stamens and/or one pistil, sometimes provided with a perigon of bristles. Glumes distichous or spirally arranged. Stamens with slender or filiform filaments. Ovary 1-celled; style 2\xe2\x80\x943-branched. Fruit a nut. Endosperm mealy. About 3200 species in nearly 80 genera, all over the world.
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  • 94
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    The Vascular System in the Kidneys of the Common Porpoise (Phocoena phocoena (L.)) (1963)
    In:  Bijdragen tot de dierkunde vol. 33 no. 1, pp. 71-81
    Details
    Publication Date: 2024-01-12
    Description: Studying the kidneys of the Common Porpoise and the Fin Whale it was found that there is a second venal system next to the normal venal system. The arterial and venal system as found in the kidneys of the dog are present in the kidneys of the Common Porpoise without typical differences but there is also a venal system situated outside the renculi which conducts the blood from the venae arcutae to the vene cava. This system is found in the kidneys of the Common Seal but here it is replacing the system of the vena renalis which it does not do in the kidneys of the Common Porpoise.\nIn the kidneys of the Common Porpoise and the Fin Whale both the plexus which surround the pelvic cavity and the ureter are present and they show to be nearly similar to those described for the kidneys of the dog. Between the renculi it is found that the plexus mentioned are somewhat more developed than in the dog. The morphology of the plexus is also identical to that of the plexus in the dog, and it is supposed that their function will be also the same in the Common Porpoise and in the dog.
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  • 95
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    Ecological data on some neotropical Scolytidae, Platypodidae and Bostrychidae (Coleoptera), mainly of Surinam (1963)
    In:  Beaufortia vol. 9 no. 110, pp. 232-240
    Details
    Publication Date: 2024-01-12
    Description: When working at the Tropical Institute, Amsterdam (1952\xe2\x80\x941957), some cases came to my notice of small borers belonging to the Scolytidae, Platypodidae and Bostrychidae attacking newly felled timber in Surinam and causing the same well-known trouble as in other tropical regions. My interest in the neotropical representatives of these families was further aroused by the material handed to me by my friend J. G. Betrem who had collected it during the two months that he carried on investigations into the status of Xyleborus morigerus in coffee plantations near Cali, Colombia, in 1959. This led me to assembling and assorting the material of these families of West Indian origin to be found in the collections of the Leiden and Amsterdam museums. This material was rather scanty and partly unnamed but it still provided some interesting data. Recently Mr. P. H. van Doesburg jr, entomologist at the Landbouwproefstation (Agricultural Experiment Station) at Paramaribo submitted some newly acquired Scolytidae which he had collected in the Surinam plantations. They provided some data on the habits and economic status of the little borers additional to those compiled by J. B. M. van Dinther in his book on the Insect pests of cultivated plants in Surinam (1960), in which survey a few species collected by him but not fully identified, were mentioned. At my request I then received for examination the latter specimens kept in the collection of the Entomological Laboratory at Wageningen, and, through the kind cooperation of Dr. D. C. Geyskes and Mr. van Doesburg, also all the material preserved in the collections of the Surinam Museum and the Experiment Station at Paramaribo. My main interest was directed towards the ecological data and a search was made for information to be found in earlier reports and in the literature of adjacent countries. In this way sufficient relevant data accumulated to warrant the publication of the present paper. For the identification of species unknown to us and the verification of old names I applied to Professor S. L. Wood, Provo, Utah, U.S.A. on various occasions. A few Bostrychidae were identified by the late Professor J. M. Vrijdagh, Brussels.
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  • 96
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    The Anatomy and Function of the Ear of the Bottle-nosed Dolphin Tursiops truncatus (1963)
    In:  Beaufortia vol. 9 no. 111, pp. 241-256
    Details
    Publication Date: 2024-01-12
    Description: 3. An account is given of sound conductivity experiments which were carried out on the auditory structures in a very fresh, dead specimen of Tursiops. 4. The probable function of the external auditory meatus is discussed in relationship to the arrangement of the accessory air sinuses of the middle ear. 5. The so-called \xe2\x80\x9dauditory scanning\xe2\x80\x9d behaviour in odontocete cetaceans is commented upon in the light of preliminary experimental evidence of a vocal sound diffraction pattern.
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  • 97
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    Notizen zur Fortpflanzungsbiologie und Jugendentwicklung zweier Grubenottern (Serpentes: Crotalidae: Crotalus atrox und Agkistrodon p. piscivorus) (1963)
    In:  Bijdragen tot de dierkunde vol. 33 no. 1, pp. 61-69
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    Publication Date: 2024-01-12
    Description: \xc3\x9cber die postembryonale Entwicklung \xe2\x80\x94 besonders die Gewichtszunahme \xe2\x80\x94 junger Giftschlangen (Viperiden, Crotaliden, Elapiden) gibt es aus naheliegenden Gr\xc3\xbcnden nur wenige eingehendere Untersuchungen. KLAUBER (1956) bringt an Hand eines gro\xc3\x9fen Materials eine Zusammenfassung einschl\xc3\xa4giger Freilandbeobachtungen und -messungen an einer Reihe von Crotalus-Arten und fa\xc3\x9ft die Gewichts-L\xc3\xa4ngen- Relationen der erbeuteten Tiere nach Monaten tabellarisch zusammen. Statistisch ergibt sich dabei ein Index W = CLP (W = Gewicht, L = Gesamtl\xc3\xa4nge, C und p sind artliche Konstanten, die bei \xe2\x99\x80\xe2\x99\x80 gr\xc3\xb6\xc3\x9fer sind als bei \xe2\x99\x82\xe2\x99\x82: adulte \xe2\x99\x80\xe2\x99\x80 sind schwerer als \xe2\x99\x82\xe2\x99\x82 gleicher L\xc3\xa4nge, die absolut schwersten Tiere sind aber infolge absolut gr\xc3\xb6\xc3\x9ferer L\xc3\xa4nge stets \xe2\x99\x82\xe2\x99\x82). F\xc3\xbcr Crotalus atrox z.B. betr\xc3\xa4gt der Klaubersche Index W = 550 L3, 3 (eine 100 cm lange Schlange wiegt also 550 g).\nDiese Werte repr\xc3\xa4sentieren den gro\xc3\x9fen Durchschnitt aus einer Vielzahl verschiedener Messungen an immer wieder neuen Individuen der jeweiligen Altersstufen. Regelm\xc3\xa4\xc3\x9fige Gewichtskontrollen an ein und demselben Individuum lassen sich dagegen nur in Gefangenschaft exakt durchf\xc3\xbchren. Wir nehmen daher die Gelegenheit wahr, die Entwicklung einiger im Tierpark Berlin gez\xc3\xbcchteter Grubenottern (Crotalus atrox und Agkistrodon piscivorus) im einzelnen zu verfolgen und \xe2\x80\x94 auch im Hinblick auf terraristische und pathologische Probleme, wie sie in Zoologischen G\xc3\xa4rten auftreten \xe2\x80\x94 zu kommentieren.
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  • 98
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    Notes on the Flora of Java VIII (1963)
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 12 no. 1, pp. 61-69
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    Publication Date: 2024-01-12
    Description: Michelia pilifera Bakh. \xc6\x92., nom. nou.\nMichelia velutina Bl., Fl. Jav. (1829) Magn., p. 17, non DC., Prod. 1 (1824) 79.
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  • 99
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    The Opilionida (Arachnida) of the Netherlands (1963)
    In:  Zoologische Verhandelingen vol. 63 no. 1, pp. 1-70
    Details
    Publication Date: 2024-01-12
    Description: INTRODUCTION\nUntil now very little has been published on the harvestmen of The Netherlands. The earliest paper known to me is by Goedaert (1669), who mentions Phalangium opilio from The Netherlands and gives the following "biological" information: "The animals originate from mush-rooms; they eat salpetre; catch flies with their many-jointed tarsi; at night they play, because there is nothing to prey on". For a long time this was the only "knowledge" concerning Dutch Opilionida, except that according to Houttuyn (1769), Bennet and Van Olivier (1825), Van der Hoeven (1828, 1859), Snellen van Vollenhoven (1859), and Rombouts (1875), the above-mentioned species occurs throughout The Netherlands. An outstanding anatomical study of the sexual organs of a number of species, by De Graaf, appeared in 1882. In "Les Arachnides de Belgique" the Belgian naturalist Becker (1896) records the presence of Nemastoma lugubre 2), Phalangium opilio, and Platybunus triangularis from localities throughout The Netherlands, and Mitopus morio and Odiellus spinosus from Maastricht. The first important publication on distribution and biology of Dutch harvestmen, is by Loman (1900). He mentions the following species: Phalangium opilio, Opilio parietinus, Leiobunum rotundum, Mitopus morio (common from North to South); Oligolophus tridens, Odiellus spinosus, Platybunus triangularis (on sandy soil, in woods, and in heaths); Nemastoma lugubre, Nemastoma quadripunctatum (in South Limburg). Oudemans (1916) and Arnoud (1955) briefly recorded the presence of Trogulus tricarinatus in Limburg. Van der Drift (1950) listed a number of species collected during his investigation of a beech forest, whilst Van der Hammen (1947, 1950) mentions Mitostoma chrysomelas
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  • 100
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    Clausiliidae (Gastropoda, Pulmonata) collected by the Netherlands biological expedition to Turkey in 1959 (1963)
    In:  Zoologische Mededelingen vol. 38 no. 15, pp. 243-260
    Details
    Publication Date: 2024-01-12
    Description: The route of the Netherlands Biological Expedition to Turkey in 1959 is published elsewhere (Hennipman a.o., 1961; Anonymus, 1963). As is mentioned there also, the zoological material collected is preserved in the Rijksmuseum van Natuurlijke Historie at Leiden. I am greatly indebted to Dr. C. O. van Regteren Altena, curator of that Museum, for placing the Clausiliidae collected by the expedition at my disposal. Moreover my thanks are due to Mrs. W. S. S. van der Feen-van Benthem Jutting, Amsterdam, and Dr. A. Zilch, Frankfurt am Main, for specimens lent for the purpose of comparison.\nThe Clausiliidae were all collected by Mr. W. J. M. Vader, one of the members of the expedition. Only one sample is from Greece (Porto Lagos), the others are from Istanbul, near the Bosporus, and from Asiatic Turkey.\nAll the samples are preserved dry, the soft parts having hardened in the top whorls of the shells by loss of moisture.\nIn the systematic account the arrangement given in the \xe2\x80\x9eHandbuch der Pal\xc3\xa4ozo\xc3\xb6logie" vol. 6 by Wenz-Zilch (1959/60) is followed.\nSome of the specimens are in the author\'s collection and in the collection of Mr. W. J. M. Vader.\n\nPHAEDUSINAE\nTribus Serrulineae Serrulina Mousson, 1873 Serrulina (Serrulina) serrulata (L. Pfeiffer, 1847) Material examined. \xe2\x80\x94 Turkey, Vilayet of Trabzon, 3 km S. of Hamsik\xc3\xb6y (pl. XX), about 45 km SSW. of the city of Trabson, altitude ca. 1900 m, in a wet forest with firs and beech trees; a small number of specimens was
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