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  • 2005-2009  (5)
  • 1960-1964  (86,778)
  • 1962  (86,778)
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  • 1
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    Unknown
    PANGAEA
    In:  Scripps Institution of Oceanography, UC San Diego | Supplement to: SCRIPPS Institution of Oceanography (1962): PROA Expedition April-August 1962, list of core and dredge samples, R/V Spencer F. Baird. Scripps Institution of Oceanography, UC San Diego, unpublished, 64 pp, https://www.ngdc.noaa.gov/mgg/curator/data/spencer_f._baird/proa/15065003.pdf
    Publication Date: 2024-05-26
    Description: The cores and dredges described in this report were taken on the PROA Expedition in April 1962 until August 1962 by the Scripps Institution of Oceanography from the R/V Spencer F. Baird. A total of 180 cores and dredges were recovered and are available at Scripps for sampling and study.
    Keywords: Comment; Core; CORE; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; Elevation of event; Event label; GC; Gravity corer; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Photo/Video; Piston corer; Position; PROA; PROA-009D; PROA-011P; PROA-011PG; PROA-015D; PROA-029D; PROA-063PG; PROA-072D; PROA-079P; PROA-084P; PROA-099P; PROA-101P; PROA-102C1; PROA-102C2; PROA-103V; PROA-105G; PROA-108C; PROA-108P; PROA-108PG; PROA-112P; PROA-113P; PROA-113PG; PROA-113V; PROA-116P; PROA-123G; PROA-137G; PROA-139G; PROA-141G; PROA-147G; PROA-147V; PROA-148G; PROA-150G; PROA-151G; PROA-156G; PROA-157G; PROA-159G; PROA-160G; PROA-161G; PROA-162G; PROA-167G; PROA-168G; PROA-169G; PROA-175G; PROA-PC7; PV; Quantity of deposit; Sediment type; Size; Spencer F. Baird; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 467 data points
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  • 2
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    Unknown
    PANGAEA
    In:  Lamont-Doherty Earth Observatory of Columbia University, New York
    Publication Date: 2024-05-02
    Description: The cores and dredges described in this report were taken during the Vema 2 Expedition from July to December 1953 by the Lamont Geological Observatory, Columbia University from the R/V Vema. An approximate total of 12 cores, dredges and camera stations were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Piston corer; Position; Quantity of deposit; Sediment type; Substrate type; V02; V02-13; Vema; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Lamont-Doherty Earth Observatory of Columbia University, New York
    Publication Date: 2024-05-02
    Keywords: Atlantic Ocean; Carribean sea; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; Dredge, rock; DRG; DRG_R; Elevation of event; Event label; File name; Identification; Indian Ocean; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Pacific Ocean; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; Tasman Sea; Uniform resource locator/link to image; V18; V18-102; V18-104; V18-107; V18-108; V18-109; V18-10RD; V18-11; V18-110; V18-111; V18-113; V18-115; V18-116; V18-117; V18-118; V18-119; V18-119C; V18-119SBT; V18-11RD; V18-120SBT; V18-121; V18-123; V18-124; V18-125; V18-128; V18-129C; V18-13; V18-130C; V18-132; V18-133; V18-133C; V18-134C; V18-136; V18-137; V18-137C; V18-138; V18-139; V18-14; V18-142; V18-143; V18-143C; V18-145; V18-14C; V18-14RD; V18-15; V18-152C; V18-153; V18-154C; V18-15C; V18-16; V18-160; V18-161; V18-162; V18-163; V18-164; V18-165; V18-16C; V18-17; V18-170; V18-171; V18-176; V18-178C; V18-179; V18-179C; V18-180; V18-180C; V18-182; V18-185; V18-186; V18-187; V18-189; V18-191; V18-192; V18-193; V18-195; V18-196; V18-197; V18-198; V18-199; V18-19RD; V18-2; V18-200; V18-203; V18-204; V18-211; V18-211C; V18-212C; V18-213; V18-213C; V18-214; V18-214C; V18-217; V18-219C; V18-21C; V18-21RD; V18-220C; V18-221; V18-221C; V18-222; V18-222C; V18-223; V18-223C; V18-224; V18-224C; V18-225; V18-226; V18-226C; V18-227C; V18-22C; V18-232; V18-233; V18-235; V18-235C; V18-236; V18-236C; V18-238C; V18-239C; V18-23C; V18-24; V18-241; V18-246C; V18-247; V18-248; V18-248C; V18-25; V18-250; V18-252; V18-25C; V18-26; V18-263C; V18-266C; V18-26C; V18-26RD; V18-27; V18-270C; V18-28; V18-281; V18-282; V18-283; V18-284; V18-285; V18-286; V18-286C; V18-287; V18-292; V18-295; V18-297C; V18-299; V18-29RD; V18-30; V18-300; V18-302; V18-305; V18-305C; V18-307; V18-309; V18-30RD; V18-31; V18-310; V18-311; V18-312; V18-312C; V18-313; V18-314; V18-315; V18-318; V18-319; V18-32; V18-320; V18-321; V18-322; V18-324; V18-325; V18-328; V18-329; V18-32RD; V18-330; V18-332; V18-33RD; V18-341; V18-345; V18-346; V18-348; V18-349; V18-351; V18-352; V18-353; V18-356; V18-358; V18-359; V18-36; V18-360; V18-361; V18-362; V18-363; V18-364; V18-366; V18-368; V18-37; V18-371; V18-372; V18-373; V18-374; V18-375; V18-376; V18-377; V18-38; V18-40C; V18-45C; V18-45SBT; V18-46C; V18-5; V18-50; V18-52; V18-6; V18-69; V18-6RD; V18-7; V18-70; V18-72; V18-73; V18-75; V18-79; V18-7C; V18-8; V18-80; V18-81; V18-82; V18-83; V18-90; V18-91; V18-92; V18-97; Vema; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 4508 data points
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  • 4
    Monograph available for loan
    Monograph available for loan
    Novosibirsk : Izdatel'stvo Sibirskogo otdelenija AN SSSR
    Associated volumes
    Call number: AWI G3-24-95571-1
    In: Tektonika Sibiri, Tom 1
    Type of Medium: Monograph available for loan
    Pages: 396 Seiten , Illustrationen , 1 Kartenbeilage
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 1
    Language: Russian
    Note: CONTENTS Preface General Problems On the Basis Systems and Types of Tectonic Structures of Meso-Cenozoic Continent of Asia / Yu. A. Kosygin, I. V. Lutchitski Scheme of Classification and General Regularities of Distribution of Mesozoic and Cenozoic Tectonic Depressions of Platforms and Folded Zones of Northern and Eastern Asia / A. S. Khomentovski West Siberia and Kazakhstan Tectonics of Eastern Versant of the Urals Within the Area of Mesozoic and Paleogene Deposits / N. I. ArkhangeI'ski New Geophysical Data on Tectonics of Middle Ob' Area / N. I. PavIenkova Mesozoic Structures of the Region of Southern Paleozoic Boundaries of West Siberian Lowland / A. L. Matveyevskaya The Kazakhstan Depressions / E. D. ShIygin Materials on Morphology and History of Development of Recent Structures of Eastern Kazakhstan and Some Theoretic Problems / F. S. Moiseyenko Recent Tectonics of Western Parf of Altai-Sayan Region / F. S. Moiseyenko Some Problems of Tectonic Structure of Eelee Depression / A. B. Lee To the Problem of Structure of Mesozoic Structural Stage of Tuva / G. M. VoIontei On Relation of Mesozoic and Paleozoic Structures of Northern Part of Minusa. Intermontane Downwarp and Adjacent Part of West Siberian Plate / A. G. Kats, B. N. Krasil'nikov Tectonics of South-Western Part of West Siberian Lowland According to Geophysical Data / V. S. Surkov To the Problem of Tectonic Structure of the Region of Conjugation of West Siberian Plate and Siberian Platform / K. V. BogoIepov, A. P. Shevtsov New Data on the North-Western Hypogene Extension of Yenisei Mountain Ridge Under Mesozoic Cover of West Siberian Plate / I. M. Tabatski, A. Ya. Chupakhin The Arctic region The Tectonic Map of Meso-Cenozoic Downwarps of Norther Part of Siberian Platform of Scale 1:250 000 and the Method of Its Construction / I. P. AtIasov Main Features of Recent Tectonics and of Development of Endogenous Relief of Polar Part of Mesozoic Downwarp of Middle Siberia / S. A. StreIkov Eastern Siberia and Transbaikalian Region Basis Features of Tectonics of Mesozoic and Cenozofc Deposits of Yakutia / K B. Mokshantsev, V. V. YeIovskikh Tectonic Structure and Principal Stages of Formation of Verkhoyansk Downwarp / A. V. Leiptsig, V. V. Panov Tectonics of Western Part of Vilui Depression / G. S. Fradkin Recent Tectonics of Vilui Depression and its Relation to Ancient Structures / V. V. ZabaIuyev Tectonics of South Yakutian Downwarp / V. V. Mokrinski To the Problem of History of Formation of Meso-Cenozoic Depressions of Aldan Shield / A. G. Kats On Meso-Cenozoic Structure of Near-Baikal Region / N. A. FIorensov Geologic Structure of Meso-Cenozoic Depressions of Central Part of Vitim High Plateau / P. V. Osokin, V. V. BaIkhanov On Cenozoic History of Some Parts of Vitim High Plateau and Ikat Mountain Rarige (Upper Course of Vitim River) / A. N. BuIgatov To the Problem of Meso-Cenozoic Structures of Buryatia / Ts. O. Ochirov On Tectonics of Buryat ASSR Area / G. A. Kibanov Geologic-Tectonic Outline of Central Transbaikalian Region / V. V. Starchenko Formations and Tectonics of Mesozoic Downwarps of Mongolo-Okhotsk Belt / M. S. Nagibina The Far East Basis Problems of Tectonics of Central Part of the Far East (South of Khabarovsk Territory and Amur Region) / L. I. Krasny Tectonics of Meso-Cenozoic Superposed Downwarp of Djugdjur Foothills / V. M. MoraIev Meso-Cenozoic Depressions of Southern Part of the Far East / Yu. B. Ustinovski Some Specific Features of Tectonics of Tertiary Sedimentary Beds of Southern Part of Sikhote-Alin' / Yu. Ya. Gromov China Geologic Structure of Mesozoic Depressions of China / M. I. Varentsov, Van Tszin-bo, G. E. Ryabukhin, A. I. Levchenko Appendix: To the Problem of Existeme of the «Kellog-Teul'ches arch» / Yu. F. Pogonya-Stefanovich On the Article of Yu. F. Pogonya-Stefanovich / K. V. BogoIepov Resolution of the Scientific Council on Tectonics of Siberia and the Far East Programm of Investigation of Mesozoic and Cenozoic Depressions of Siberia and the Far East Index of Local Tectonic Nomenclature , СОДЕРЖАНИЕ Предисловие Общие вопросы Об основных системах и типах тектонических структур мезозойско-кайнозойского континента Азии / Ю. А. Косыгин, И. В. Лучицкий Схема классификации и общие закономерности размещения тектонических мезозойских и кайнозойских впадин платформ и складчатых зон Северной и Восточной Азии / А. С. Хоментовский Западная Сибирь и Казахстан Тектоника восточного склона Урала в пределах распространения мезозойских и палеогеновых отложений / Н. И. Архангельский Новые геофизические данные о тектонике среднего Приобья / Н. И. Павленкова Мезокайнозойские структуры области южного палеозойского обрамления Западно-Сибирской низменности / А. Л. Матвеевская Впадины Казахстана / Е. Д. Шлыгин Материалы по морфологии и истории развития новейших структур Восточного Казахстана и некоторые вопросы теории / Ф. С. Моисеенко Новейшая тектоника западной части Алтае-Саянской области / Ф. С. Моисеенко Некоторые вопросы тектонического строения илийской впадины / А. Б. Ли К вопросу о строении мезозойского структурного яруса Тувы / Г. М. Волонтэй О соотношении мезозойских и палеозойских структур в северной части Минусинского межгорного прогиба и прилежащей части Западно-Сибирской плиты / Я. Г. Кац, Б. Н. Красильников Тектоника юго-восточной части Западно-Сибирской низменности по геофизическим данным / В. С. Сурков К вопросу о тектоническом строении области сопряжения Западно-Сибирской плиты и Сибирской платформы / К. В. Боголепов, А. П. Шевцов Новые данные о северо-западном глубинном продолжении Енисейского кряжа под мезозойским чехлом Западно-Сибирской плиты / И. М. Табацкий, А. Я. Чупахин Арктика Тектоническая карта мезокайнозойских прогибов севера Сибирской платформы в масштабе 1:2 500 000 и метод ее составления / И. П. Атласов Главнейшие черты новейшей тектоники и развития эндогенного рельефа заполярной части мезозойских прогибов средней Сибири / С. А. Стрелков Восточная Сибирь и Забайкалье Основные черты тектоники мезозойских и кайнозойских отложений Якутии / К. Б. Мокшанцев, В. В. Еловских Тектоническое строение и основные этапы формирования Приверхоянского прогиба / А. В. Лейпциг, В. В. Панов Тектоника западной части Вилюйской впадины / Г. С. Фрадкин Новейшая тектоника Вилюйской синеклизы и связь ее с древними структурами / В. В. Забалуев Тектоника Южно-Якутского краевого прогиба / В. В. Мокринский К вопросу об истории формирования мезокайнозойских впадин Алданского щита / А. Г. Кац О мезозойско-кайнозойской структуре Прибайкалья / Н. А. Флоренсов Геологическое строение мезокайнозойских впадин центральной части Витимского плоскогорья / П. В. Осокин, В. В. Балханов О кайнозойской истории Витимского плоскогорья и Икатского хребта (бассейн верховья р. Витим) / А. Н. Булгатов К вопросу о мезокайнозойских структурах Бурятии / Ц. О. Очиров К тектонике территории БАССР / Г. А. Кибанов Геолого-тектонический очерк Центрального Забайкалья / В. В. Старченко Формации и тектоника мезозойских прогибов Монголо-Охотского пояса / М. С. Нагибина Дальний Восток Основные вопросы тектоники центральной части Дальнего Востока (юг Хабаровского края и Амурская область) / Л. И. Красный Тектоника Предджугджурского мезокайнозойского наложенного прогиба / В. М. Моралев Мезозойско-кайнозойские впадины южной части Дальнего Востока / Ю. Б. Устиновский Некоторые особенности тектоники третичных осадочных толщ южной части Сихотэ-Адиня / Ю. Я. Громов Китай О геологическом строении мезокайнозойских впадин Китая / М. И. Варенцов, Ван Цзин-бо, Г. Е. Рябухин, А. И. Левченко Приложение К вопросу о существовании «Келлоr-Теульчесского вала» / Ю Ф. Погоня-Стефанович О заметке Ю. Ф. Погони-Стефановича / К. В. Боголепов Решение научного совета по тектонике Сибири и Дальнего Востока Программа исследования мезозойских и кайнозойских впадин Сибири и Дальнего Востока Указатель региональных тектонических терминов , In kyrillischer Schrift
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 5
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 32 no. 1, pp. 65-69
    Publication Date: 2024-01-12
    Description: The incidence of Proteocephalus filicollis in Pungitius pungitius, Gasterosteus aculeatus f. hemigymnus and Gasterosteus aculeatus f. trachurus has been studied. It is very low in both forms of Gasterosteus, but 16% of Pungitius was infected. The monthly examination of minimally 27 and maximally 223 Pungitius pungitius indicates that an annual cycle exists neither in the incidence nor in genital development. It seems probable that Proteocephalus filicollis in Pungitius pungitius is less affected by low temperatures than worms of the same species in Gasterosteus aculeatus.\nReference is made to intercurrent helminth infections.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 6
    facet.materialart.
    Unknown
    In:  Flora of the Netherlands Antilles vol. 1 no. 1, pp. 1-84
    Publication Date: 2024-01-12
    Description: Epiphytic or usually terrestrial ferns with a short fleshy rhizome bearing only one or a few, mostly fleshy, leaves, these erect, petiolate, continuous with the rhizome, the lamina usually divided into a sterile and a stalked fertile portion; veins free or reticulate. Sporangia with a wall composed of several layers of cells, opening with a slit, containing numerous trilete thick-walled subspherical spores of one kind. Four genera, two monotypic, the others with about 60 species of almost world-wide distribution.
    Repository Name: National Museum of Natural History, Netherlands
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  • 7
    Publication Date: 2024-01-12
    Description: The examination of two aberrant Pteropods collected during a trip with the whale factory-ship \xe2\x80\x9dm.s. Willem Barendsz\xe2\x80\x9d led to the conclusion that they were animals in a resting stage. The histology and the anatomy of the totally aberrant soft parts was discussed. The shells of the specimens indicate that these animals are the species Clio antarctica Dall, 1908. One aberrant specimen belonging to the species Clio sulcata (Pfeffer, 1879), collected during the same trip with the whale factory-ship, was examined and it shows that this animal was in a stage between the resting stage and the normal, active, stage. Three specimens of the species Clio pyramidata (Linnaeus, 1767, forma lanceolata (Lesueur, 1813), collected by the Texas and the Dana expedition, were studied as they showed the same aberrations from the normal full grown form as the other three animals previously mentioned. It was clear that the three specimens of the form lanceolata were also in a resting stage and their anatomy and histology were identical with those of the aberrant animals of the species Clio antarctica Dall, 1908.\nThe resting stage seems to have developed from a more specialized stage, as a great store of reserve food was present, while the intestinal duct was not functional and, moreover, the gonad was active.\nThe relation and the distribution of the species Clio pyramidata Linnaeus, 1767, Clio sulcata (Pfeffer, 1879), Clio antarctica Dall, 1908 and Clio martensii (Pfeffer, 1880) was studied and it seems better to consider these species as belonging to one polytypic species and, therefore, as synonymous with Clio pyramidata Linnaeus, 1767. It may be very well possible that Proclio subteres Hubendick, 1951 also belongs to the species Clio pyramidata Linnaeus, 1767. And if that is the case, Proclio subteres Hubendick, 1951 is in all probability synonymous with Clio pyramidata Linnaeus, 1767 forma antarctica (Dall, 1908).
    Repository Name: National Museum of Natural History, Netherlands
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  • 8
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 32 no. 1, pp. 1-48
    Publication Date: 2024-01-12
    Description: In der vorliegenden Arbeit wird die Geburt des Kaninchens (multipares S\xc3\xa4ugetier) und des Rindes (unipares S\xc3\xa4ugetier) beschrieben und mit der Geburt anderer S\xc3\xa4uger verglichen. Das Verhalten der Mutter bei der Geburt hat sich nicht ge\xc3\xa4ndert trotz der Domestikation. Die Geburt findet meistens statt zu der Zeit, da die Tiere gew\xc3\xb6hnlich ruhen. Dies wird von Sympathicus-Parasympathicus-Rhythmus bedingt. Die entleerten Uterusteile der Ratte und wahrscheinlich aller Multiparen ziehen sich stark zusammen, weshalb die sp\xc3\xa4teren Jungen keinen l\xc3\xa4ngeren Weg zur Vulva zur\xc3\xbcckzulegen haben und also nicht mehr von Erstickungsgefahr bedroht werden als die ersten.\nDie Lage der uniparen S\xc3\xa4uger kommst zustande infolge Formanbequemung, Gravitation und der Raumverh\xc3\xa4ltnisse in der Bauchh\xc3\xb6hle. Eine ausf\xc3\xbchrlichere Zusammenfassung von Kapitel V findet man auf Seite 23.\nDer erste Atemzug wird ausgel\xc3\xb6st durch die St\xc3\xb6rung des plazentaren Gasstoffwechsels. Nur bei asphyctischen Jungen kann die Atmung einsetzen durch die Wirkung \xc3\xa4usserer Reize (Kap. VI).\nDer spontane Nabelschnurriss der Wale und der Huftiere, ausser dem Schwein und dem Flusspferd, findet statt an einer oder mehreren pr\xc3\xa4formierten Rissstellen. Diese Stellen sind anatomisch und histologisch verschiedenartig gebaut. Bei den Tieren, deren Nabelschnur an einer willk\xc3\xbcrlichen Stelle durchbissen wird oder spontan reisst, sind diese Eigent\xc3\xbcmlichkeiten nicht vorhanden. Eine Zusammenfassung von Kapitel VII findet man auf Seite 46.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 9
    Publication Date: 2024-01-12
    Description: During a recent survey of Pacific psammophilous and phycophilous copepods an isolated female Bomolochus was found, the identification of which, in absence of its host, proved to be particularly troublesome. It became necessary to check the descriptions of all species of the genus Bomolochus Von Nordmann, 1832, and of several other genera of Bomolochidae, in the course of which I tried to find a satisfactory grouping of the many species described.\nThis effort in so far proved to be disappointing that a fairly large number of species is so inadequately characterized that recognition, in absence of the host, is next to impossible. Taxonomy of parasitic copepods has, unfortunately, long been influenced by the obstinate notion that each host species should necessarily harbour its own parasitic species. This idea has overstressed the importance of the host, at the cost of information, particularly morphological information, concerning the parasitic animal, so that at present there is an overwhelming number of parasitic copepods of uncertain position, uncertain status or inadequate definition, impeding a much wanted natural grouping of the numerous species of parasitic Copepoda. The importance of complete structural information, especially for those species that are able to leave their host temporarily, cannot be too greatly stressed and it is gratifying to find such information in many of the modern publications (Stock, 1953, 1955; Shen, 1957; Shiino, 1957; Yamaguti, 1936, 1939, 1953, et al.). In the present paper I have presented, in condensed form, all available information on the Bomolochidae; I have suggested a subdivision of the genus Bomolochus, redescribed the female of Bomolochus bellones Burmeister and added the description of two new species. It is hoped that this paper will stimulate the redescription of doubtful or insufficiently described forms, preferably
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 10
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    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 11 no. 2, pp. 494-494
    Publication Date: 2024-01-12
    Description: In the Flora of Tropical Africa C. B. Clarke (6) pointed out that in the collection of \xe2\x80\x9cScleria foliosa Hochst., Abyssinia, prope Chire, Dillon & Petit\xe2\x80\x9d specimens of true S. foliosa Hochst. ex A. Rich. (4) are mixed with some of S. schimperiana Boeck. (1) and that \xe2\x80\x9cit would be very difficult to sort them without looking at the nut\xe2\x80\x9d. He referred S. dillonii Boeck. (2) to the synonymy of S. foliosa, and herein he was followed by all subsequent authors including Nelmes (3) and Robinson (5).\nHowever, already Boeckeler was aware of the fact that the Chire collection is a mixture, and on \xe2\x80\x9cS. foliosa Hb. Dillon et Petit. \xe2\x80\x94 an etiam Richardi? \xe2\x80\x94 pro parte (c. S. foliosa Hochst. intermixta)\xe2\x80\x9d he based his S. dillonii, different from S. foliosa mainly by its globose or depressed-globose, smooth nuts.
    Repository Name: National Museum of Natural History, Netherlands
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