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  • 2020-2023
  • 1965-1969  (135.947)
  • 1967  (135.947)
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  • 1
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    PANGAEA
    In:  Supplement to: Traganza, Eugene D (1967): Dynamics of the carbon dioxide system on the Great Bahama Bank. Bulletin of Marine Science, 17(2), 348-366, https://www.ingentaconnect.com/content/umrsmas/bullmar/1967/00000017/00000002/art00010
    Publikationsdatum: 2024-03-15
    Beschreibung: Carbon dioxide is lost from the ocean by calcium carbonate precipitation (-p), photosynthesis (-b) and gas evasion at the sea surface (-g). Among the most active sites are warm shallow seas. In this paper seasonal studies on the Great Bahama Bank relate these processes in an equation which takes into account the indirect effects of advection (a), evaporation (e), and eddy diffusion (d). Calcium carbonate precipitation is very seasonal and accounts for about half of the total losses. The delta sum CO2/deltaCa ratio is always about 1.87 on the bank. A high summer carbonate loss is inversely correlated with summer increases of chlorinity and temperature suggesting that CaCO3 is precipitated inorganically or biogenic production of CaCO3 is regulated by these parameters or both.
    Schlagwort(e): Alkalinity, total; Aragonite saturation state; Bicarbonate; Bicarbonate ion; Calcification/Dissolution; Calcification rate of calcium carbonate; Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, total; Chloride; Coast and continental shelf; Date; Entire community; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); North Atlantic; OA-ICC; OCE; Ocean Acidification International Coordination Centre; Oceanography; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Salinity; Temperate; Temperature, water; Traganza_Great_Bahama_Bank
    Materialart: Dataset
    Format: text/tab-separated-values, 279 data points
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  • 2
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    PANGAEA
    Publikationsdatum: 2024-03-06
    Schlagwort(e): Betula sp., fruits; Betula sp., fruit scales; Calluna vulgaris; Carex sect. Eucarex; Carex sect. Vignea; Caryophyllaceae; Ceratophyllum demersum; Chara, oogonia; Counting, palynology; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EDEA; Edelman auger; Elm_B; Juncus; Lower Saxony, Northern Germany; Menyanthes; Najas minor; Nuphar; Nymphaea; Pinus, seeds; Pollen zone; Polygonum lapathifolium; Potamogeton cf. lucens; Potamogeton fluitans; Potamogeton friesii; Potamogeton natans; Potamogeton perfoliatus; Potamogeton praelongus; Potamogeton pusillus; Potamogeton sp.; Potamogeton trichoides; Ranunculus sceleratus; Rubus idaeus; Rumex maritimus; Rumex sp.; Umbelliferae
    Materialart: Dataset
    Format: text/tab-separated-values, 798 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
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    PANGAEA
    Publikationsdatum: 2024-03-06
    Schlagwort(e): 1b; Betula nana, fruits; Betula nana, fruit scales; Betula sp., fruits; Betula sp., fruit scales; Brasenia; Calluna vulgaris; Carex sect. Eucarex; Carex sect. Vignea; Caryophyllaceae; Ceratophyllum demersum; Chara, oogonia; Counting, palynology; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; EDEA; Edelman auger; Elm_K; Juncus; Lower Saxony, Northern Germany; Menyanthes; Najas minor; Nuphar; Nymphaea; Nymphaea: hairs; Pinus, seeds; Pollen zone; Polygonum lapathifolium; Polygonum sp.; Potamogeton cf. lucens; Potamogeton natans; Potamogeton praelongus; Potamogeton sp.; Potamogeton trichoides; Ranunculus sceleratus; Rubus idaeus; Rumex maritimus; Rumex sp.; Sagittaria sagittifolia; Umbelliferae
    Materialart: Dataset
    Format: text/tab-separated-values, 1773 data points
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  • 4
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    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 3 no. 9, pp. 148-148
    Publikationsdatum: 2024-02-22
    Beschreibung: A second list of species found near Hellevoetsluis, prov. S. Holland, on heaps of stones used for the Delta-works. See also Gorteria 3 (4), 1966, p. 49\xe2\x80\x9451.
    Repository-Name: National Museum of Natural History, Netherlands
    Materialart: info:eu-repo/semantics/article
    Format: application/pdf
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  • 5
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    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 3 no. 13, pp. 209-211
    Publikationsdatum: 2024-02-08
    Beschreibung: Two adventitious species of the genus Beckmannia Host have been found in the Netherlands. They can be distinguished as follows: 1. Stems mostly tuberously thickened at the base. Spikelets always 2-flowered (fig. 1, a). Glumes always more or less irregularly dentate at the mostly rounded and mostly very shortly acuminate apex, and with often very shortly ciliate margins, hardly swollen when ripe. Ripe stamens mostly distinctly exserted; anthers 1,6\xe2\x80\x942,1 mm long (fig. 1, b) B. eruciformis (L.) Host 1\xe2\x80\x99. Stems not thickened at the base. Spikelets 1-flowered (fig. 1, c); sometimes a few 2-flowered spikelets are present in the spike. Glumes entire at the acute and distinctly acuminate apex, and with glabrous margins, mostly rather strongly swollen when ripe. Ripe stamens mostly but slightly exserted; anthers 0,7\xe2\x80\x941,1 mm long (fig. 1, d) ... B. syzigachne (Steud.) Fern.
    Repository-Name: National Museum of Natural History, Netherlands
    Materialart: info:eu-repo/semantics/article
    Format: application/pdf
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  • 6
    Monographie ausleihbar
    Monographie ausleihbar
    [Moskva] : Izdatel'stvo Moskovskogo Universiteta
    Signatur: AWI G3-24-95658
    Materialart: Monographie ausleihbar
    Seiten: 302 Seiten , Illustrationen
    Sprache: Russisch
    Anmerkung: СОДЕРЖАНИЕ Предисловие Введение Глава 1. Процессы замерзания - таяния горных пород и свойства мерзлых пород Мерзлые горные породы - многофазные и многокомпонентные системы Содержание жидкой воды и льда в мерзлых породах. Температурные условия замерзания воды в породах Свойства мерзлых горных пород Типы замерзания воды в горных породах Физические процессы в оттаивающих горных породах Изменение объема мерзлых пород и образование трещин Основные закономерности строения мерзлых горных пород Глава II. Сезонная и вечная мерзлота Сезонная мерзлота Вечная мерзлота Глава III. Криогенез как процесс литогенеза Зоны охлаждения Земли как зоны особого типа литогенеза Лед как минерал . Типы подземного льда Место криолитоrенеза в общей системе литогенеза Глава IV. Криогенные горные породы Криолиты - ледяные мономинеральные породы Криолититы - льдистые полиминеральные породы Криоэлювииты - вторичные продукты криолитогенеза Глава V. Типы криолитогенеза Эпиrенетический тип криолитогенеза Сингенетический тип криолитогенеза О термокарсте Глава VI. География криолитогенеза Зональность процессов криолитогенеза Криолитогенез как региональное явление Мерзлотно-геологическое районирование области вечной мерзлоты в СССР Заключение Литература , English translation of Table of Contents Preface Introduction Chapter 1. Freezing processes - thawing of rocks and properties of frozen rocks Frozen rocks - multiphase and multicomponent systems Content of liquid water and ice in frozen rocks. Temperature conditions for freezing water in rocks Properties of frozen rocks Types of water freezing in rocks Physical processes in thawing rocks Changes in the volume of frozen rocks and the formation of cracks Basic patterns of the structure of frozen rocks Chapter II. Seasonal and permafrost Seasonal permafrost Permafrost Chapter III. Cryogenesis as a process of lithogenesis Cooling zones of the Earth as zones of a special type of lithogenesis Ice as a mineral Types of underground ice Place of cryolithogenesis in the general system of lithogenesis Chapter IV. Cryogenic rocks Cryolites - icy monomineral rocks Cryolites - icy polymineral rocks Cryoeluviites - secondary products of cryolithogenesis Chapter V. Types of cryolithogenesis Epi-genetic type of cryolithogenesis Syngenetic type of cryolithogenesis About thermokarst Chapter VI. Geography of cryolithogenesis Zoning of cryolithogenesis processes Cryolithogenesis as a regional phenomenon Permafrost-geological zoning of the permafrost region in the USSR Conclusion Literature , In kyrillischer Schrift
    Standort: AWI Lesesaal
    Zweigbibliothek: AWI Bibliothek
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  • 7
    Publikationsdatum: 2024-01-12
    Beschreibung: A re-examination of the types of Lithobius occultus Silvestri, 1894, and Lithobius excellens Silvestri, 1894, from Italy, has shown that the two are based on specimens of the same species which takes the name of Eupolybothrus (Schizopolybothrus) excellens (Silvestri, 1894), and is probably most closely related to E. tabularum (Verhoeff, 1937). A tentative survey of the subgenera of the genus Eupolybothrus Verhoeff, 1907, is given, and a new subgenus, Leptopolybothrus nov. subgen., type-species Lithobius leptopus Latzel, 1880, is erected.
    Repository-Name: National Museum of Natural History, Netherlands
    Materialart: info:eu-repo/semantics/article
    Format: application/pdf
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  • 8
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    In:  Zoologische Verhandelingen vol. 90 no. 1, pp. 1-56
    Publikationsdatum: 2024-01-12
    Beschreibung: INTRODUCTION\nIn the past, many authors emphasized the great variability in the morphology of the members of the genus Gammarus. At the same time, such "varieties" were distributed in waters ranging from entirely fresh to purely marine. Both ideas, the morphological variability and the great salinity tolerance, have not been substantiated by more modern investigations. The descriptive and experimental work, first of all that of Sexton, has shown that the morphological characters of the various forms are very stable, at least at a given stage of maturity, and that very slight details suffice for their characterization. These closely related forms are intersterile (Spooner, 1947, 1951 ; Kinne, 1954; Wautier & Roux, 1959) and behave ecologically different (e.g. Spooner, 1947; Segerstr\xc3\xa5le, 1947; Kinne, 1954). Because of their intersterility and since the distribution areas overlap (cf. Segerstr\xc3\xa5le, 1947, fig. 6; Nijssen, 1963), most authors now follow Kinne, 1954, in considering the "forms" of Gammarus good species. The idea that the specific characters (more in particular, the "hairiness") would be brought forward through environmental factors, such as salinity, was disproved by Spooner (1947), who showed that the characteristic formation of the cuticular structures was independent of the salinity, and genetically determined.\nSexton (many papers), but especially Spooner (1947), Segerstr\xc3\xa5le (1947), and Kinne (1954) have done excellent work in straightening the taxonomic status of the marine and brackish water species of Gammarus of the Atlantic coasts of Europe. Their work chiefly, clarified the morphology and ecology of Gammarus duebeni Lilljeborg, 1851 and of a number of forms previously confused under the name of G. locusta (Linnaeus, 1758). The
    Repository-Name: National Museum of Natural History, Netherlands
    Materialart: info:eu-repo/semantics/article
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  • 9
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    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 15 no. 1, pp. 25-29
    Publikationsdatum: 2024-01-12
    Beschreibung: Sous le nom de Neevea repens, Batters (1900) d\xc3\xa9crivit une petite Algue rouge microscopique et endozo\xc3\xafque r\xc3\xa9colt\xc3\xa9e par J. T. Neeve \xc3\xa0 Deal (Kent). Cette Algue vivait dans un Bryozoaire ( (Flustra foliacea) formant, associ\xc3\xa9e \xc3\xa0 1\xe2\x80\x99 Erythropeltis discigera Schmitz var. flustrae Batt., de petites taches roses \xc3\xa0 peine perceptibles.\nBatters consid\xc3\xa9ra cette algue comme le repr\xc3\xa9sentant d\xe2\x80\x99un genre nouveau qu\xe2\x80\x99il rapprocha d\xe2\x80\x99une part des Goniotrichum et d\xe2\x80\x99autre part des Erythropeltis. S\xe2\x80\x99il ressemble au premier par sa reproduction, qui se manifeste par la lib\xc3\xa9ration de cellules isol\xc3\xa9es hors de l\xe2\x80\x99enveloppe g\xc3\xa9latineuse du thalle, il en diff\xc3\xa8re par sa morphologie et sa situation endozo\xc3\xafque. La disposition des cellules en disque tr\xc3\xa8s irr\xc3\xa9gulier \xc3\xa9loigne \xc3\xa9galement le genre Neevea des Erythropeltis.
    Repository-Name: National Museum of Natural History, Netherlands
    Materialart: info:eu-repo/semantics/article
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  • 10
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    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 15 no. 1, pp. 55-62
    Publikationsdatum: 2024-01-12
    Beschreibung: The following notes refer to the typification of the two oldest species names applied in the genus Gelidium, including also comments on other related topics. Gelidium is probably the most confused genus, both nomenclaturally and taxonomically, of the Rhodophyta. This investigation began in an attempt to determine the correct names to be applied to the British species of the genus, but it was soon discovered that a much wider geographical consideration was necessary. I would like to take this opportunity to pay tribute to the help and assistance which has been afforded by Dr. J. Th. Koster in this and other investigations, over a period of many years.\nExtreme ecological and seasonal polymorphism are the principal causes of the present situation in the genus Gelidium. Extensive fieldwork over the past seventeen years has given some indication of the limits of taxa (Dixon, 1958, 1966), in so far as the European representatives are concerned. The nomenclatural problems are, however, still largely untouched. The purpose of the present paper is to examine critically the typification of the two oldest epithets referred to the genus Gelidium. These are: 1. cartilagineum, based on Fucus cartilagineus Linnaeus (1753), 2. corneum, based on Fucus corneus Hudson (1762).
    Repository-Name: National Museum of Natural History, Netherlands
    Materialart: info:eu-repo/semantics/article
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