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  • 1965-1969  (651,849)
  • 1940-1944  (110,020)
Collection
Language
Years
Year
  • 1
    Series available for loan
    Series available for loan
    Karlsruhe : Braun ; 1.1941(1940) - 59.1999(1997); 2000(1999) -
    Call number: S 91.0710 ; S 91.0710 (2020) ; S 91.0710 (2021) ; S 91.0710 (2022) ; S 91.0710 (2023)
    Type of Medium: Series available for loan
    ISSN: 0174-254X
    Location: Archive - must be ordered
    Location: Archive - must be ordered
    Location: Archive - must be ordered
    Location: Archive - must be ordered
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Publication Date: 2024-05-15
    Keywords: BC; Box corer; Calculated; Calculated from mass/volume; Carbon, organic, total; Chlorine; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK2096; Iron, acid-soluble; Iron/Sulfur ratio; Kieler Bucht; Sulfate/Chlorine ratio; Sulfur; Sulfur, total; Sulfur, water-insoluble; Sulfur, water-insoluble, without organic S; Sulfur in sulfate; Sulfur in sulfide; Water content, wet mass; δ34S, sulfate; δ34S, sulfur, water-insoluble; δ34S, sulfur, water-insoluble, without organic S; δ34S, total
    Type: Dataset
    Format: text/tab-separated-values, 213 data points
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  • 3
    Publication Date: 2024-05-15
    Keywords: BC; Box corer; Calculated; Calculated from mass/volume; Carbon, organic, total; Chlorine; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK2094; Iron, acid-soluble; Iron/Sulfur ratio; Kieler Bucht; Sulfate/Chlorine ratio; Sulfur; Sulfur, total; Sulfur, water-insoluble; Sulfur, water-insoluble, without organic S; Sulfur in sulfate; Sulfur in sulfide; Water content, wet mass; δ34S, sulfate; δ34S, sulfide; δ34S, sulfur, water-insoluble; δ34S, sulfur, water-insoluble, without organic S; δ34S, total
    Type: Dataset
    Format: text/tab-separated-values, 297 data points
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  • 4
    Publication Date: 2024-05-15
    Keywords: BC; Box corer; Calculated; Calculated from mass/volume; Carbon, organic, total; Chlorine; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK2091; Iron, acid-soluble; Iron/Sulfur ratio; Kieler Bucht; Sulfate/Chlorine ratio; Sulfur; Sulfur, total; Sulfur, water-insoluble; Sulfur, water-insoluble, without organic S; Sulfur in sulfate; Sulfur in sulfide; Water content, wet mass; δ34S, sulfate; δ34S, sulfide; δ34S, sulfur, water-insoluble; δ34S, sulfur, water-insoluble, without organic S; δ34S, total
    Type: Dataset
    Format: text/tab-separated-values, 214 data points
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  • 5
    Publication Date: 2024-05-15
    Keywords: BC; Box corer; Calculated; Calculated from mass/volume; Carbon, organic, total; Chlorine; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; GIK2092; Iron, acid-soluble; Iron/Sulfur ratio; Kieler Bucht; Sulfate/Chlorine ratio; Sulfur; Sulfur, total; Sulfur, water-insoluble; Sulfur, water-insoluble, without organic S; Sulfur in sulfate; Sulfur in sulfide; Water content, wet mass; δ34S, sulfate; δ34S, sulfide; δ34S, sulfur, water-insoluble; δ34S, sulfur, water-insoluble, without organic S; δ34S, total
    Type: Dataset
    Format: text/tab-separated-values, 226 data points
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  • 6
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    PANGAEA
    In:  Lamont-Doherty Earth Observatory of Columbia University, New York
    Publication Date: 2024-05-02
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; Elevation of event; Event label; Identification; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; RC10; RC10-003RD; RC10-101; RC10-101C1; RC10-101C3; RC10-103C1; RC10-104C4; RC10-11; RC10-110; RC10-123; RC10-123C4; RC10-13; RC10-131; RC10-153; RC10-154; RC10-164; RC10-165; RC10-168; RC10-171; RC10-172; RC10-176; RC10-178; RC10-179; RC10-182; RC10-205; RC10-21C2; RC10-21C3; RC10-233; RC10-239; RC10-244; RC10-26C6; RC10-26C7; RC10-274; RC10-278; RC10-279; RC10-36C1; RC10-36C2; RC10-40C2; RC10-40C4; RC10-41C1; RC10-41C2; RC10-41C4; RC10-44C2; RC10-45C3; RC10-49C2; RC10-49C3; RC10-69C2; RC10-70C1; RC10-76; RC10-77; RC10-78; RC10-79; RC10-7C2; RC10-7C6; RC10-81; RC10-87C7; RC10-88; RC10-8C1; RC10-8C2; RC10-91; RC10-93; RC10-96C2; RC10-96C4; RC10-97C1; RC10-97C4; RC10-97C5; RC10-98C1; RC10-98C3; RC10-98C4; RC10-99C2; Robert Conrad; Sediment type; Size; Substrate type; Uniform resource locator/link to file; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 1142 data points
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  • 7
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    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 R/V Robert Conrad 9 Expedition from October 1964 until September 1965 by the Lamont Geological Observatory, Columbia University. An approximate total of 350 cores, dredges and camera stations were recovered and are available at Lamont-Doherty Earth Observatory for sampling and study.
    Keywords: Atlantic Ocean; Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; 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; RC09; RC09-1; RC09-100; RC09-102; RC09-104; RC09-106C; RC09-107C; RC09-109; RC09-111; RC09-113; RC09-114; RC09-115; RC09-116; RC09-119; RC09-12; RC09-120C; RC09-122C; RC09-123; RC09-124; RC09-124C; RC09-125; RC09-125C; RC09-13; RC09-131; RC09-132; RC09-134; RC09-139; RC09-141; RC09-142; RC09-143; RC09-144; RC09-148; RC09-149; RC09-151; RC09-152; RC09-157; RC09-158; RC09-159; RC09-160; RC09-167; RC09-169; RC09-170; RC09-172; RC09-177; RC09-181; RC09-182; RC09-182C; RC09-184C; RC09-188; RC09-1C; RC09-209; RC09-210; RC09-212; RC09-215; RC09-217; RC09-218; RC09-224; RC09-226; RC09-26; RC09-29; RC09-30; RC09-31; RC09-33C; RC09-35; RC09-37C; RC09-39; RC09-39C; RC09-3RD; RC09-40C; RC09-41; RC09-42; RC09-42C; RC09-43; RC09-43C; RC09-45; RC09-47; RC09-48; RC09-49; RC09-5; RC09-51; RC09-51C; RC09-52C; RC09-53; RC09-56C; RC09-58C; RC09-6; RC09-61C; RC09-62C; RC09-65C; RC09-66C; RC09-67C; RC09-68; RC09-68C; RC09-69; RC09-69C; RC09-70; RC09-70C; RC09-73; RC09-74; RC09-75; RC09-77; RC09-78C; RC09-8; RC09-83; RC09-85C; RC09-86; RC09-86C; RC09-87; RC09-87C; RC09-88; RC09-88C; RC09-89; RC09-90; RC09-90C; RC09-91; RC09-92; RC09-94; RC09-95; RC09-96; RC09-99; Robert Conrad; Sediment type; Size; Substrate type; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 2123 data points
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  • 8
    Series available for loan
    Series available for loan
    Berlin [u.a.] : Borntraeger
    Associated volumes
    Call number: 9/SR 90.0077(7)
    In: Beiträge zur regionalen Geologie der Erde
    Type of Medium: Series available for loan
    Pages: XI, 230 S. + 4 Kt.-Beil., 2 Beil.
    Series Statement: Beiträge zur regionalen Geologie der Erde 7
    Language: German
    Location: Reading room
    Branch Library: GFZ Library
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  • 9
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    Diesterweg
    Publication Date: 2024-04-22
    Type: Article , PeerReviewed
    Format: text
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  • 10
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    PANGAEA
    In:  Supplement to: Bonatti, Enrico; Joensuu, Oiva (1966): Deep-Sea Iron Deposit from the South Pacific. Science, 154(3749), 643-645, https://doi.org/10.1126/science.154.3749.643
    Publication Date: 2024-04-20
    Description: Along with specimens of manganese oxides and basalt, rocks containing more than 30 percent iron by weight and consisting mainly of poorly crystallized goethite have been dredged from the flanks of a seamount located on the East Pacific Rise. The Fe-Mn ratio varies widely among the various oxide rocks deposited at this locality and at another seamount in the same area. The deposit was probably formed by fractional precipitation of iron and manganese which had been introduced locally into the bottom water by hydrothermal solutions of volcanic origin, and by leaching from deep-sea basaltic lavas.
    Keywords: Aluminium oxide; AMPH-002D; AMPH01AR; AMPH01AR-002D; AMPHITRITE; Argo; Barium; Boron; Calcium oxide; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Dredge; DRG; Iron; Loss on drying; Magnesium oxide; Manganese; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Optical spectrographic analysis; Pacific Ocean; Potassium oxide; Sample ID; Silicon dioxide; Strontium
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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  • 11
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    PANGAEA
    In:  Supplement to: Cordes, Eilhard (1966): Aufbau und Bildungsbedingungen der Schwermineralseifen bei Skagen (Dänemark). Meyniana, 16, 1-35, https://doi.org/10.2312/meyniana.1966.16.1
    Publication Date: 2024-04-19
    Description: Aufbau und Ausdehnung der Schwermineral-Anreicherungen (Ilmenit, Granat, Amphibol) am Strand südlich Skagens wurden in langen Schürfgräben untersucht. Die Seifenlagen ziehen durchgehend vom Kliff-Fuß bis zur mittleren Meereshöhe hin und liegen meist diskordant auf der alten Strandschichtung. Ihre strandparallele Ausdehnung beträgt bis zu 100 m. Aufgebaut werden sie aus dünnen Schwermineral-Lamellen, die in kleinerem Umfang überall in den Strandablagerungen zu finden sind und hier das Gefüge nachzeichnen (Rippeln, Strandwallschichtung, Schichtstörungen). Die Seifenbildung geht in einem Gebiet mit verstärktem Küstenabtrag vor sich (Lee-Erosion südlich der Hafenmolen von Skagen). Dieses deutet darauf hin, daß die Schwerminerale bei Aufarbeitung bereits vorhandener Sedimente infolge ihres unterschiedlichen hydraulischen Verhaltens Zurückbleiben und schließlich angereichert werden. Die Korngrößenverteilung der Minerale in verschiedenen Sedimentproben zeigen, daß mit steigender Schwermineral-Anreicherung eine Kornverfeinerung und Zunahme der spezifisch schwersten Minerale (opake Erzminerale und Zirkon) auftritt. In ähnlicher Weise werden die Sortierungswerte besser. Die Aufbereitung des Sedimentes wird, in Anlehnung an v. ENGELHARDT (1939), mit einem doppelten Sortierungsvorgang durch die Wasserbewegung am Strand erklärt. Beim Absinken des Sandes nach dem Brecherschwall tritt eine Vorsortierung ein, die den Abtransport der leichteren und größeren Minerale im Sog begünstigt. Verbindungen zu Vorstellungen der Aufbereitungstechnik (Rundherdverfahren) und Hydrodynamik ('laminare Unterschicht') werden hergestellt. Die Dünensande Skagens sind infolge ihres hohen Schwermineralgehaltes und günstiger Äquivalentgrößen der einzelnen Minerale besonders bedeutsam für die Seifenbildung am Strand.
    Keywords: Europe, Denmark; HAND; Sampling by hand; Skagen1964
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 12
    Publication Date: 2024-04-19
    Keywords: Amphibole; Area/locality; Distance; Europe, Denmark; Garnet; HAND; Heavy minerals; Median, grain size; Opaque minerals; Sample ID; Sampling by hand; Skagen1964
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 13
    Publication Date: 2024-04-19
    Keywords: Amphibole; Area/locality; Epidote; Europe, Denmark; Garnet; HAND; Heavy minerals; Median, grain size; Minerals, other; Opaque minerals; Sample ID; Sampling by hand; Skagen1964; Sorting; Zircon
    Type: Dataset
    Format: text/tab-separated-values, 300 data points
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  • 14
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    PANGAEA
    In:  Antarctic Research Facility, Florida State University
    Publication Date: 2024-04-07
    Description: Cores, submarine photography and dredges described in this report were taken during the R/V Eltanin Cruise 17 in 1965 by the Department of Geology, Florida State University. Cores and dredges were recovered for 49 stations along with bottom photography and are available at the Antarctic Research Facility, Florida State University for sampling and study.
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge; DRG; ELT17; ELT17.001-PC; ELT17.001-RD; ELT17.003-PC; ELT17.003-PH; ELT17.004-PH; ELT17.005A-PH; ELT17.006-PC; ELT17.007-PC; ELT17.007-PH; ELT17.008-PC; ELT17.008-PH; ELT17.009-RD; ELT17.013-RS; ELT17.015-PC; ELT17.018-PC; ELT17.022-PC; ELT17.023-PC; ELT17.027-PC; ELT17.027-PH; ELT17.029-BT; ELT17.029-PC; ELT17.029-PH; ELT17.030A-PH; ELT17.030-PC; ELT17.031-PC; ELT17.031-PH; ELT17.032A-PH; ELT17.032-PC; ELT17.032-PH; ELT17.032-TC; ELT17.035-BT; ELT17.036-BT; ELT17.036-PH; ELT17.10C; ELT17.18C; ELT17.19C; ELT17.20C; ELT17.29C; ELT17.2C; ELT17.30C; ELT17.32C; ELT17.33C; ELT17.34C; ELT17.4C; ELT17.5C; ELT17.9C; Eltanin; Event label; File name; GC; Gravity corer; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; TC; TRAWL; Trawl net; Trigger corer; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 745 data points
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  • 15
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    PANGAEA
    In:  Antarctic Research Facility, Florida State University
    Publication Date: 2024-04-07
    Keywords: Comment; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Dredge, rock; DRG_R; ELT15; ELT15.001-PC; ELT15.003-MT; ELT15.003-PC; ELT15.004-BT; ELT15.004-PC; ELT15.005-BT; ELT15.006-PC; ELT15.006-RD; ELT15.007-MT; ELT15.007-PC; ELT15.008-BT; ELT15.008-PC; ELT15.009-PC; ELT15.011-PC; ELT15.012-PC; ELT15.013-PC; ELT15.013-RD; ELT15.015-PC; ELT15.016-BT; ELT15.016-PC; ELT15.018-PC; ELT15.019-PC; ELT15.021-PC; ELT15.023-TC; ELT15.025-PC; ELT15.026-PC; ELT15.027-PC; ELT15.028-PC; ELT15-10C; ELT15-12C; ELT15-14C; ELT15-17C; ELT15-18C; ELT15-19C; ELT15-21C; ELT15-22C; ELT15-24C; ELT15-25C; ELT15-26C; ELT15-28C; ELT15-2C; ELT15-3C; ELT15-4C; ELT15-5C; ELT15-7C; ELT15-8C; ELT15-9C; Eltanin; Event label; File name; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; PC; Photo/Video; Piston corer; Position; PV; Quantity of deposit; Sediment type; Size; Southern Ocean; Substrate type; TC; TRAWL; Trawl net; Trigger corer; Uniform resource locator/link to image; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 1015 data points
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  • 16
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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
    Publication Date: 2024-03-15
    Description: 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.
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 279 data points
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  • 17
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    PANGAEA
    Publication Date: 2024-03-06
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 798 data points
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  • 18
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    PANGAEA
    Publication Date: 2024-03-06
    Keywords: 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
    Type: Dataset
    Format: text/tab-separated-values, 1773 data points
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  • 19
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-03
    Description: research
    Language: German
    Type: doc-type:book
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  • 20
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-03
    Description: research
    Keywords: Die divergierende Humus-Metabolik benachbarter Sauer-Braunerden und Rendsinen unter Wald im Licht organischer Stoffgruppen-Untersuchungen
    Language: German
    Type: doc-type:book
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  • 21
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-03
    Description: Voruntersuchungen zu dieser Arbeit befaßten sieb mit der stoffgruppen-chemischen Auftrennung der organischen Substanz in den organo-mineralischen A -Horizonten von benachbarten und typischen Rendsinen und Sauer-Braunerden unter Laub und Coniferen-Forsten der mitteldeutschen Berg- und RUgel-Landschaften. Die Untersuchungen ergaben: Bei gleichen Baumbeständen und in einer Distanz von nur wenigen Metern war der Gleichgewichts-Humusspiegel in den Ab-Horizonten (0 - 25 cm) der Rendsinen ca. 4-mal so hoch wre der mittlere Humus-Gehalt in den oberen 15 cm der Sauer-Braunerden. Die organische Substanz der eutrophen, kalkhaltigen Rendsinen bestand zu hohen Anteilen aus höher-polymeren Huminstoffen (Huminsäuren und lluminen), während bei den stark sauren Braunerden die Fraktionen der niedermolekularen Fulvosäuren und Streustoffe den Hauptanteil der organischen Komponente bildeten. Für die Sauer-Braunerden konnte anband der Verteilung von aggres- siven Fulvosäuren, organischen Säuren (z.B. Uronsäuren) und Kohlenhydraten nachgewiesen werden, daß die Humus- Zufuhr zum Mineralkörper des Bodens zu erheblichen Teilen durch Infiltration bewerkstelligt wird. Bei den Rendsinen erfolgt dagegen die Inkorporation durch intensive biolo- gisch-mechanische Beimischung. Während bei den Rendsinen der Umsatz der organischen Sub- stanz überwiegend im oberen Abschnitt des Solums abläuft und eine Auflage-Humus-Decke fehlt, spielt sich bei den Sauer-Braunerden der Umsatz hauptsächlich in der Humus- Auflage ab. Die Mengen und das Spektrum der organischen Substanzen, die infiltrativ in das mineralische Substrat gelangen und dort fixiert oder abgebaut werden, sind im Vergleich zu den Rendsinen gering. Sie scheinen durch eine selektiv abbau-wirksame biologische (Pilz-) Sperre in der Auflage-Decke oder an deren Untergrenze bestimmt zu werden. Als Fazit dieser Untersuchungen wurde empfohlen, zur Klä- rung der unterschiedlichen Humus-Metabolik mit Hilfe standorts-biologischer Methoden das Gewicht auf die Klärung folgender beiden Fragen zu legen:
    Description: research
    Keywords: Bodenbildung ; Bodenchemie ; Humusboden ; Metabolit ; Geoökosystem
    Language: German
    Type: doc-type:book
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  • 22
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-03
    Description: research
    Keywords: Jungpleistozäne Hangformung in Mitteleuropa Beiträge zur Kenntnis ; Deutung und Bedeutung ihrer räumlichen und zeitlichen Differenzierung
    Language: German
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-03
    Description: research
    Keywords: Nigeria ; Hangentwicklung
    Language: German
    Type: doc-type:book
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  • 24
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-03-03
    Description: Die Fragestellung, die den hier mitgeteilten Untersuchungen zugrunde liegt, hat sich aus Forschungsarbeiten ergeben, die einem ganz anderen Problemkreis gewidmet waren: Es handelte sich dabei um die Frage nach den Entwicklungsprozessen und dem Entwicklungsstand der Bodenbildung im Alleröd, Es ist dies die bedeutendste der kurzen vorholozänen Bodenbildungs-Phasen, in der aus den spätglazialen Periglazial-Ablagerungen, dem im bodenkundliehen Sinne "frischen Ausgangs-Material", wie Löß, Frost-Wanderschutt, Flugsand etc., die ersten schwach entwickelten "Böden" hervorgingen. Die Kenntnis der allerödzeitlichen Bodenbildung ist insofern von Bedeutung, als die Böden in der auf das Alleröd folgenden jüngeren Tundrenzeit meist nur noch in geringem Maße zerstört wurden und als "präforma-tive Bodenentwicklungsphasen den Ablauf der später ein- setzenden holozänen Bodenentwicklung beeinflußt oder vorgezeichnet haben können. Als geeignetes Studienobjekt bieten sich die begrabenen Alleröd-Böden im Bereich und in der Umrandung der Rheinischen Masse an, deren zeitliche Begrenzung nach "oben" an vielen Stellen durch die mächtige Sediment-Decke der trachytischen Asche der Laacher-See-Eruptionen festgelegt ist. Wir nahmen zunächst an, daß die unter den mehrere Meter mächtigen Bims-Decken begrabenen Böden und Sedimente ohne nachträgliche holozäne Veränderungen konserviert worden seien. Im Laufe der angestellten Untersuchungen an den Alleröd-Böden und ihren Ausgangs-Sedimenten wurden wir jedoch belehrt, daß dies nicht der Fall ist. Die in den Bims-Decken ablaufenden V erwitterungs- und Stoff-Abfuhr-Prozesse wirken sich gravierend auf die Unterlage aus, so daß von einer "Fossilierung" im engeren Sinne nicht gesprochen werden kann. Diese Feststellung machte es erforderlich, sich mit den V erwitterungs-Prozessen der Laacher Bims-Ablagerungen auseinanderzusetzen, was in der vorliegenden Arbeit geschehen soll. Die Kenntnis dieser Verwitterungs-Abläufe im Tuff ist darüber hinaus für bodengenetische Betrachtungen im westdeutschen Raum von genereller Bedeutung. Ein erheblicher Teil der allerödzeitlichen Landoberfläche dieses Raumes hat eine m.o.w. starke Beimengung vulkanischer Asche erfahren, die sich bei bodengenetischen Bilanz -Untersuchungen schwer einkalkulieren läßt. Die Ansprache bestimmter Mineral-Neubildungen (wie z.B. Kaolinit, Allophan) als "aschenbürtig" könnte hierbei wichtige Hinweise liefern.
    Description: research
    Keywords: Bodenfeuchte ; Grundwasserstand ; Grundwasserspiegel ; Lössboden ; Würmeiszeit ; Bodenchemie Niedersachsen ; Chemische Verwitterung ; Bimsstein ; Tuff ; Trachyt ; Laacher See
    Language: German
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  • 25
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    PANGAEA
    In:  Supplement to: Johnson, C E; Glasby, Geoffrey P (1969): Mössbauer Effect determination of particle size in microcrystalline iron-manganese nodules. Nature, 222(5191), 376-377, https://doi.org/10.1038/222376a0
    Publication Date: 2024-03-01
    Description: Iron-manganese nodules from the ocean floor have been extensively studied. But, because of the fine grain size of the particles of the nodules, structural identification by X-ray and electron diffraction techniques is difficult and the mineralogy of the iron oxide phase has not been well characterized. The observation of the Mössbauer spectrum-in which each nucleus absorbs gamma-rays independently-is not limited by particle size in the same way as is the observation of Bragg peaks in diffraction measurements, in which radiation must be scattered coherently from a large number of atoms. The magnetic hyperfine splitting in the Mössbauer spectrum of magnetic materials is affected, however, when the particles are so small that they become superparamagnetic. We describe here an investigation using the 57Fe Mössbauer effect of two iron-manganese nodules in which the iron oxide phase could not be detected by X-ray or electron diffraction.
    Keywords: Chromium; Cobalt; Copper; D16; D6243; D6273; Description; Discovery (1962); Dredge, rock; DRG_R; Event label; Gulf of Aden; Indian Ocean, Carlsberg Ridge; Iron; Lead; Manganese; Minerals, surface area; Molybdenum; Mössbauer spectroscopy; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Sample ID; Silicon dioxide; Titanium; Vanadium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
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  • 26
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    In:  Supplement to: Gorham, Eville; Swaine, Dalway J (1965): The influence of oxidizing and reducing conditions upon the distribution of some elements in lake sediments. Limnology and Oceanography, 10(2), 268-279, https://doi.org/10.4319/lo.1965.10.2.0268
    Publication Date: 2024-02-26
    Description: Analyses for Fe, Mn, Pb, Zn, Co, P, Mo, Ba, Sr, Ti, Li, Rb, Na, K, Be, Cr, V, Y, Ag, Cu, C, S, Sn, Ni, Ga, Zr, and La have been carried out on some oxidate crusts, oxidized surface muds, reduced subsurface muds, and glacial clays collected in Windermere and Esthwaite Water in the English Lake District. The relatively organic lake muds exhibit the highest concentrations of C, S, Cu, Sn, and Ni. Many of the oxidate crusts exhibit strong enrichment in Mn, Fe, Ba, Sr, Pb, and Zn. Ti, Li, Rb, Co, P, and Mo are also enriched in some crusts. S, Sn, and Ni reach their highest levels in the reducing subsurface muds, but Mn, and to a lesser extent Fe and Mo, are higher in the oxidized than in the reduced muds. Relations between the elements in the various sediments are examined, and the English oxidate crusts are compared with lake and stream ores in Sweden and Finland, and with marine manganese nodules. These marine nodules are frequently enriched in Cu, Ni, Co, Mo, V, Ag, and Sn to a far higher degree than the freshwater ferromanganese concretions. Some freshwater crusts exhibit enrichments in Pb, Zn, and Ba of the same order as those observed in marine manganese nodules.
    Keywords: Barium; Boron; Carbon, organic, total; Chromium; Cobalt; Copper; DEPTH, sediment/rock; Description; Dredge; DRG; Event label; Flame photometry; Gallium; Identification; Iron; Lake Ullswater, United Kingdom; Lake Windermere, United Kingdom; Lanthanum; Lead; Lithium; Manganese; Molybdenum; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; Phosphorus; Potassium; Rubidium; Silver; Sodium; Spectrophotometer (Unicam SP500); Spectroscopy, cathode layer arc; Strontium; Sulfur, total; Tin; Titanium; Ullswater_G; Vanadium; Wet chemistry; Windermere_G; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 232 data points
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  • 27
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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
    Publication Date: 2024-02-22
    Description: 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
    Type: info:eu-repo/semantics/article
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  • 28
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    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 4 no. 2, pp. 27-28
    Publication Date: 2024-02-22
    Description: The author mentions a second find of Lactuca tatarica (L.) C. A. Mey. in the harbour of Rotterdam in 1966, in a ruderal locality. The number of specimens increased in 1967.
    Repository Name: National Museum of Natural History, Netherlands
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  • 29
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    Berliner Lithogr. Inst., Berlin
    In:  SUB Göttingen | KART B 140:5160[1940];KART H 140:Bad Warmbrunn
    Publication Date: 2024-02-21
    Description: Geologische Karte 1: 25 000 mit Erläuterungen. Digitalisat des FID GEO (Fachinformationsdienst Geowissenschaften der festen Erde), erstellt durch das GDZ (Göttinger Digitalisierungszentrum, SUB Göttingen), Karte aus dem Bestand der SUB Göttingen. GeoTIFF erstellt durch FID GEO, SUB Göttingen.
    Description: map
    Description: DFG, SUB Göttingen
    Keywords: ddc:912 ; ddc:554.3 ; Geologische Karte ; Warmbrunn ; Cieplice Śląskie-Zdrój ; GeoTIFF
    Language: German
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  • 30
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    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 17 no. 2, pp. 303-311
    Publication Date: 2024-02-08
    Description: The area of distribution of most Myriophyllum species is insufficiently known. In this paper, many new localities are recorded for 16 species from SE. Asia, Malesia, Madagascar, and Africa, and a key is added. One species from New Guinea, M. coronatum, is described as new (fig. I). Of the other species the synonymy is complete, but no descriptions are given; of each the distribution and ecology is cited, and if necessary critical remarks are added.\nUnder the new species the second remark deals with the possible desirability of distinguishing subgenera or sections within the genus. It is concluded that, as the species show a reticulate affinity by parallelism, especially as regards reductions in both vegetative and sexual organs, the usefulness of distinguishing infrageneric taxa is debatable and not advisable.
    Repository Name: National Museum of Natural History, Netherlands
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  • 31
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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
    Publication Date: 2024-02-08
    Description: 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
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  • 32
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    In:  Gorteria: tijdschrift voor de floristiek, de plantenoecologie en het vegetatie-onderzoek van Nederland vol. 4 no. 6/8, pp. 103-108
    Publication Date: 2024-02-08
    Description: Five species of Atriplex s.s. have been found as aliens in the Netherlands. In the following key the indigenous A. laciniata and the species belonging to the A. patula-complex have been included. Of the latter a tentative revision will appear next year. The key is to be used for dried plants with completely mature fruits only.
    Repository Name: National Museum of Natural History, Netherlands
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  • 33
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    In:  Supplement to: Hartmann, Martin; Lohmann, Ludwig (1968): Untersuchungen an der heißen Salzlauge und am Sediment des Atlantis II-Tiefs in Roten Meer. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe C Geologie und Geophysik, Gebrüder Bornträger, Berlin, Stuttgart, C1, 13-20
    Publication Date: 2024-02-03
    Description: Two water samples and two sediment samples taken in 1965 by the R. V. "Meteor" in the area of the hot salt brine of the Atlantis II-Deep were chemically investigated, and in addition the sediment samples were subjected to X-ray and optical analysis. The investigation of the sulfur-isotope-ratios showed the same values for all water samples. This information combined with the Ca-sulfate solubility data leads us to conclude that, for the most part, the sulfate content of the salt brine resulted from mixing along the boundary with the normal seawater. In this boundary area gypsum or anhydrite is formed which sinks down to the deeper layers of the salt brine where it is redisolved when the water becomes undersaturated. In the laboratory, formation of CaS04 precipitate resulted from both the reheating of the water sample from the uppermost zone of the salt brine to the in-situ-temperature as well as by the mixing of the water sample with normal Red Sea water. The iron and manganese delivered by the hot spring is separated within the area of the salt brine by their different redox-potentials. Iron is sedimented to a high amount within the salt brine, while, as evidenced by its small amounts in all sediment samples, the more easily reducible manganese is apparently carried out of the area before sedimentation can take place. The very good layering of the salt brine may be the result of the rough bottom topography with its several progressively higher levels allowing step-like enlargements of the surface areas of each successive layer. Each enlargement results in larger boundary areas along which more effective heat transfer and mixing with the next layer is possible. In the sediment samples up to 37.18% Fe is found, mostly bound as very poorly crystallized iron hydroxide. Pyrite is present in only very small amounts. We assume that the copper is bound mostly as sulfide, while the zinc is most likely present in an other form. The sulfur-isotope-investigations indicate that the sulfur in the sediment, bound as pyrite and sulfides, is not a result of bacterical sulfate-reduction in the iron-rich mud of the Atlantis II-Deep, but must have been brought up with the hot brine.
    Keywords: Alkalinity, total; Atlantis II Deep; BC; Box corer; Calcium; Calcium carbonate; Carbon, organic, total; Chloride; Comment; Copper; Description; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Iron; Loss on ignition; M1; M1_1207; Magnesium; Manganese; Meteor (1964); ORDINAL NUMBER; Oxygen; pH; Sample code/label; Sulfate; Sulfur, total; Zinc; δ34S, sulfate
    Type: Dataset
    Format: text/tab-separated-values, 65 data points
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  • 34
    Publication Date: 2024-02-03
    Keywords: Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_005; M1_006; M1_CTD005; M1_CTD006; Mediterranean Sea; Meteor (1964); Nitrate; Oxygen; Oxygen, microelectrode, ex-situ; Phosphate; Salinity; Silicate; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 450 data points
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  • 35
    Publication Date: 2024-02-03
    Keywords: Alkalinity, total; Ammonia; Calcium; Calculated; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Eastern Arabian Sea; Elevation of event; Event label; Fluoride; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Meteor (1964); Nitrate; Nitrite; Oxygen; Oxygen, microelectrode, ex-situ; pH; Phosphate; Phosphorus, total; Red Sea; Salinity; Silicate; Temperature, water; Turnover-thermometer; Western Arabian Sea
    Type: Dataset
    Format: text/tab-separated-values, 38537 data points
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  • 36
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    In:  Supplement to: Dietrich, Günter; Düing, Walter; Grasshoff, Klaus; Koske, Peter H (1966): Physikalische und chemische Daten nach Beobachtungen des Forschungsschiffes Meteor im Indischen Ozean 1964/65. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A2, 1-155
    Publication Date: 2024-02-03
    Description: The present volume gives the observed physical and chemical data obtained by R.V. "Meteor" in the Indian Ocean during cruise 1964/65. The tables are based on the computations made by the National Oceanographic Data Center (NODC) in Washington. In addition to the normally communicated data, the tables contain four chemical parameters: alkalinity, ammonia, fluoride, and calcium.
    Keywords: Biscaya; CTD/Rosette; CTD-RO; Eastern Arabian Sea; GIK/IfG; Golf of Aden, Arabian Sea; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; M1; M1_001; M1_005; M1_006; M1_023; M1_026; M1_028; M1_029; M1_039; M1_042; M1_043; M1_045; M1_049; M1_053; M1_055; M1_056; M1_062; M1_066; M1_069; M1_071; M1_072; M1_090; M1_091; M1_092; M1_093; M1_094; M1_095; M1_096; M1_099; M1_100; M1_101; M1_102; M1_103; M1_104; M1_105; M1_106; M1_107; M1_108; M1_109; M1_111; M1_112; M1_113; M1_114; M1_115; M1_116; M1_117; M1_118; M1_124; M1_125B; M1_126; M1_127; M1_128; M1_129; M1_130; M1_131; M1_132; M1_133; M1_134; M1_135; M1_136; M1_137; M1_138; M1_139; M1_142; M1_143; M1_144; M1_145; M1_146; M1_147; M1_148; M1_149; M1_150; M1_151; M1_152; M1_153; M1_154; M1_155; M1_156; M1_157; M1_158; M1_160; M1_161; M1_162; M1_163; M1_164; M1_165; M1_166; M1_167; M1_168; M1_169; M1_170; M1_171; M1_172; M1_173; M1_174; M1_175; M1_176; M1_177; M1_178; M1_179; M1_180; M1_181; M1_182; M1_183; M1_184; M1_185; M1_186; M1_187; M1_188; M1_189; M1_190; M1_194; M1_195; M1_196; M1_197; M1_198; M1_199; M1_200; M1_201; M1_202; M1_205; M1_206; M1_207; M1_208; M1_209; M1_210; M1_211; M1_215; M1_217; M1_218; M1_219; M1_221; M1_222; M1_223; M1_224; M1_225; M1_226; M1_227; M1_228; M1_229; M1_232; M1_233; M1_234; M1_235; M1_236; M1_237; M1_238; M1_239; M1_240; M1_241; M1_CTD001; M1_CTD005; M1_CTD006; M1_CTD023; M1_CTD026; M1_CTD028; M1_CTD029; M1_CTD039; M1_CTD042; M1_CTD043; M1_CTD045; M1_CTD049; M1_CTD053; M1_CTD055; M1_CTD056; M1_CTD062; M1_CTD066; M1_CTD069; M1_CTD071; M1_CTD072; M1_CTD090; M1_CTD091; M1_CTD092; M1_CTD093; M1_CTD094; M1_CTD095; M1_CTD096; M1_CTD099; M1_CTD100; M1_CTD101; M1_CTD102; M1_CTD103; M1_CTD104; M1_CTD105; M1_CTD106; M1_CTD107; M1_CTD108; M1_CTD109; M1_CTD111; M1_CTD112; M1_CTD113; M1_CTD114; M1_CTD115; M1_CTD116; M1_CTD117; M1_CTD118; M1_CTD124; M1_CTD125; M1_CTD126; M1_CTD127; M1_CTD128; M1_CTD129; M1_CTD130; M1_CTD131; M1_CTD132; M1_CTD133; M1_CTD134; M1_CTD135; M1_CTD136; M1_CTD137; M1_CTD138; M1_CTD139; M1_CTD142; M1_CTD143; M1_CTD144; M1_CTD145; M1_CTD146; M1_CTD147; M1_CTD148; M1_CTD149; M1_CTD150; M1_CTD151; M1_CTD152; M1_CTD153; M1_CTD154; M1_CTD155; M1_CTD156; M1_CTD157; M1_CTD158; M1_CTD160; M1_CTD161; M1_CTD162; M1_CTD163; M1_CTD164; M1_CTD165; M1_CTD166; M1_CTD167; M1_CTD168; M1_CTD169; M1_CTD170; M1_CTD171; M1_CTD172; M1_CTD173; M1_CTD174; M1_CTD175; M1_CTD176; M1_CTD177; M1_CTD178; M1_CTD179; M1_CTD180; M1_CTD181; M1_CTD182; M1_CTD183; M1_CTD184; M1_CTD185; M1_CTD186; M1_CTD187; M1_CTD188; M1_CTD189; M1_CTD190; M1_CTD194; M1_CTD195; M1_CTD196; M1_CTD197; M1_CTD198; M1_CTD199; M1_CTD200; M1_CTD201; M1_CTD202; M1_CTD205; M1_CTD206; M1_CTD207; M1_CTD208; M1_CTD209; M1_CTD210; M1_CTD211; M1_CTD215; M1_CTD217; M1_CTD218; M1_CTD219; M1_CTD221; M1_CTD222; M1_CTD223; M1_CTD224; M1_CTD225; M1_CTD226; M1_CTD227; M1_CTD228; M1_CTD229; M1_CTD232; M1_CTD233; M1_CTD234; M1_CTD235; M1_CTD236; M1_CTD237; M1_CTD238; M1_CTD239; M1_CTD240; M1_CTD241; Mediterranean Sea; Meteor (1964); Red Sea; Western Arabian Sea
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  • 37
    Publication Date: 2024-02-03
    Keywords: Biscaya; Calculated; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; GIK/IfG; IIOE - International Indian Ocean Expedition; Institute for Geosciences, Christian Albrechts University, Kiel; Latitude of event; Longitude of event; M1; M1_001; M1_CTD001; Meteor (1964); Oxygen; Oxygen, microelectrode, ex-situ; Salinity; Temperature, water; Turnover-thermometer
    Type: Dataset
    Format: text/tab-separated-values, 176 data points
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  • 38
    Monograph available for loan
    Monograph available for loan
    [Moskva] : Izdatel'stvo Moskovskogo Universiteta
    Call number: AWI G3-24-95658
    Type of Medium: Monograph available for loan
    Pages: 302 Seiten , Illustrationen
    Language: Russian
    Note: 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
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  • 39
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Seckel, Hansjörg; Stober, Manfred (1968): Höhenänderung des grönländischen Inlandeises 1959 - 1968. Polarforschung, 38(1/2), 215-221, hdl:10013/epic.29319.d001
    Publication Date: 2024-01-15
    Description: The members of the two International Glaciological Greenland Expeditions (EGIG) in 1959 and 1968 determined the altitudes in the West-East-profile by levelling. The comparison of these two measurements gives evidence of the change of altitudes and of the surface-waves. The ways of measurement and of analysis are described here. The graphic representation of the result is discussed here in connexion with the possible causes.
    Keywords: Distance; EGIG; Expédition Glaciologique Internationale au Groenlande; ICESUR; Ice survey; RULER; Ruler stick; Sampling/drilling ice; Snow thickness
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 40
    Publication Date: 2024-01-12
    Description: Cosmopsaltria agatha Moulton is removed from the synonymy of Orientopsaltria montivaga (Distant) and reallocated in Orientopsaltria. The drawings of the male genitalia facilitate the distinction of both species.
    Repository Name: National Museum of Natural History, Netherlands
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  • 41
    Publication Date: 2024-01-12
    Description: 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
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  • 42
    Publication Date: 2024-01-12
    Description: The myicolid copepod Pseudomyicola spinosus is reported from 22 new hosts (pelecypods) in Bermuda and the West Indies, from 1 new host (a pelecypod) in Madagascar, and from an ascidian (Pyuridae) in Cura\xc3\xa7ao (probably an accidental association). P. spinosus is redescribed, based on specimens from Isognomon alatus in Bermuda. Among 316 P. spinosus from Bermuda, Puerto Rico, Jamaica, Barbados, Brazil, Senegal, Madagascar, and Jugoslavia the dimensions of the body and caudal ramus varied widely. The ornamentation of the anal segment showed four different conditions of spination, and sometimes included an extra long ventral setule on either or both sides.\nThe specimens studied are regarded as one species, P. spinosus, without apparent subspecific differences. The following are considered as synonyms of P. spinosus: P. glaber Pearse, 1947, Myicola tageli Pearse, 1947, P. anomalocardiae Narchi, 1965, and P. mirabilis Humes, 1959.
    Repository Name: National Museum of Natural History, Netherlands
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  • 43
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 37 no. 1, pp. 3-10
    Publication Date: 2024-01-12
    Description: Extensive reports on losses in zoo animals are very rare. As fas as we know only London, Paris, Philadelphia and Washington give yearly reports. Of these London and Paris give very complete information. One of the reasons that so few zoos publish their results may be that it is always more pleasant to give information about successes than about failures.\nIn our opinion, however, it is no use to disguise the truth and for other zoos it can be very useful to have the opportunity to compare results. The period described in this paper is part of an important era in the history of our zoo, a period of reconstruction, rebuilding and, of increasing the collection. This period will last another 10-15 years or so as at that time the really old and worn-out buildings will have been replaced and appropriate facilities for the veterinarian will have been achieved. At the same time this period has seen great advances in veterinary care. The Cap-Chur pistol in use in our zoo since 1960 made injection possible of any animal at any time. The increasing arsenal of therapeutics and the international contacts by way of the international symposia on diseases of zoo animals have contributed largely to a better medical care of zoo animals. Thus prevention of diseases is becoming more and more important. In our opinion the effective disinfectant halamid (Chloraminum) plays an important r\xc3\xb4le in this respect.
    Repository Name: National Museum of Natural History, Netherlands
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  • 44
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 36 no. 1, pp. 3-16
    Publication Date: 2024-01-12
    Description: Da\xc3\x9f eine Tiergruppe pelagischer Anpassung, wie die Zahnwale, in den mit dem Ozean nur mittelbar, via Nordsee, in Verbindung stehenden K\xc3\xbcstenmeeren Schwedens eine weit bescheidenere Rolle spielt als an der atlantischen K\xc3\xbcste Europas, ist nat\xc3\xbcrlich und vorauszusetzen. Von 23 europ\xc3\xa4ischen Arten sind f\xc3\xbcr Schweden bis jetzt nur 14, die meisten als seltene Irrg\xc3\xa4ste, festgestellt worden. Desto mehr man sich dabei l\xc3\xa4ngs der K\xc3\xbcste von der Nordsee entfernt, desto geringer wird die Anzahl. Schon an der Westk\xc3\xbcste sinkt sie von 14 im Skagerrak bis nur 9 Arten im Kattegatt. In der Ostsee hat man an der S\xc3\xbcdk\xc3\xbcste zuerst noch 8, an der Ostk\xc3\xbcste 4 und im Bottnischen Meerbusen endlich nur 2 (Abb. 1).\nAls heimische, zu allen Jahreszeiten \xc3\xb6fters antreffbare Bewohner kann man f\xc3\xbcr die Westk\xc3\xbcste nur zwei Arten nennen \xe2\x80\x94 den ziemlich h\xc3\xa4ufigen Schweinswal (Phocaena phocoena) und den weit selteneren Langfinnendelphin ( Lagenorhynchus albirostris). Das gro\xc3\x9fe Brackwassergebiet der Ostsee hat nur den Schweinswal allein heimisch. Der gr\xc3\xb6\xc3\x9fte Teil seines Bestandes verl\xc3\xa4\xc3\x9ft jedoch in der Regel dieses Gebiet f\xc3\xbcr die Winterzeit. Seine Wanderz\xc3\xbcge von und zu der Ostsee sind den K\xc3\xbcstenbewohnern, besonders der \xc3\x96resundgegend und der S\xc3\xbcdk\xc3\xbcste seit altem wohlbekannt und wurden an dazu geeigneten Stellen, wie Ravlunda an der Ostk\xc3\xbcste von Schonen (LINNAEUS, 1751) oder Torekov und die Laholmbucht im S\xc3\xbcdostteil des Kattegattes (NILSSON, 1847), noch im vorigen Jahrhundert zum Fang dieser Kleinwale ausgenutzt (Abb. 2). Im Gegensatz zu der herbstlichen Schweinswalsjagd in den d\xc3\xa4nischen Sunden geschah dies hier haupts\xc3\xa4chlich w\xc3\xa4hrend der Fr\xc3\xbcjahrwanderung der Tiere.
    Repository Name: National Museum of Natural History, Netherlands
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  • 45
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 35 no. 1, pp. 101-126
    Publication Date: 2024-01-12
    Description: L\xe2\x80\x99A. d\xc3\xa9crit ou cite 47 esp\xc3\xa8ces de Poissons characo\xc3\xafdes r\xc3\xa9cemment r\xc3\xa9colt\xc3\xa9s par M. H. P. Pijpers au Surinam.\nQuatre formes nouvelles pour la science sont d\xc3\xa9crites: Moenkhausia surinamensis, Moenkhausia georgiae, Moenkhausia hemigrammoides et Curimatus esperanzae pijpersi; deux autres avaient \xc3\xa9t\xc3\xa9 d\xc3\xa9crites dans des notes ant\xc3\xa9rieures: Hemibrycon surinamensis et Hyphessobrycon georgettae; deux enfin sont signal\xc3\xa9es comme \xc3\xa9tant des formes nouvelles qui seront nomm\xc3\xa9es \xc3\xa0 partir d\xe2\x80\x99un mat\xc3\xa9riel plus abondant: elles appartiennent respectivement aux genres Myleus et Hemiodopsis (Hemiodus auct.).\nHemigrammus lunatus, Jobertina eleotrioides et Parodon guyanensis sont nouveaux pour la faune du Surinam.\nLa synonymie Hemigrammus orthus = Hyphessobrycon bellotti est sugg\xc3\xa9r\xc3\xa9e.\nDes cl\xc3\xa9s de d\xc3\xa9termination sont propos\xc3\xa9es pour les groupes suivants: groupe doceana du genre Moenkhausia, esp\xc3\xa8ces des Guyanes du genre Creatochanes, Stethaprionidi et ssp. de Poptella orbicularis.\nCertains sujets sont plus particuli\xc3\xa8rement discut\xc3\xa9s: valeur taxonomique et \xc3\xa9volution de la ligne lat\xc3\xa9rale, ssp. de Moenkhausia lepidura et de Poptella orbicularis, biom\xc3\xa9trie et \xc3\xa9cotaxonomie de Gasteropelecus sternicla et de Carnegiella strigata, et revue du sous-genre Hemiodopsis.
    Repository Name: National Museum of Natural History, Netherlands
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  • 46
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 35 no. 1, pp. 3-38
    Publication Date: 2024-01-12
    Description: 1. In Whales variations in the thickness of the baleen plates are supposed to give an insight into certain cyclical processes in the life of the animal. To a certain extent, by means of these variations, it is possible to reach conclusions about the age of the animal and/or about its recent period of life.\nIn order to get a better insight in the significance of the variations in thickness of the baleen plate, researches are made in the histogenesis of the baleen plate of Fin Whales and Blue Whales, caught in the Antarctic waters. The variations in thickness are caused by variations in thickness of the cortex of the baleen plate. 2. The \xe2\x80\x9croot\xe2\x80\x9d of the baleen plate consists of the following parts: the corium wall, the epithelium that covers the corium wall, the cortex and the epithelium of the gum. 3. In the epithelium of the gum arched bands of varying width are visible. These bands run into the outer layer of the cortex. There is a correlation between the width of these bands and the height of the thickenings of the cortex, in which they end. These bands are not present in the epithelium that covers the corium wall. In both epithelia corium papillae are found. On the top of each papilla a row of spherical cells is formed. In the epithelium that covers the corium wall these rows of spherical cells all run into the cortex and there they cannot be distinguished from the surrounding cornified material. This is also correct for the very few rows of spherical cells originating from the corium papillae near the base of the corium wall. These rows run into the first band of flattened cells of the gum. They become flattened with the cells of the stratum spinosum of the gum in this band, forming the very first layer of the cortex. The other rows of spherical cells in the gum, even those immediately adjacent to the cortex, all run parallel to each other and to the outer surface of the cortex. They never run into the cortex. This shows clearly that the cell material of the gum forms the first and outer layer of the cortex of a baleen plate near the base of the corium wall. Cell material of the gum is not added to the cortex in any other place. 4. The cortex of a baleen plate is formed by two epithelia, the epithelium of the gum and the epithelium that covers the corium wall. Variations in the thickness of the cortex and consequently of the baleen plate, which are visible as peaks and hollows in the record, are only formed by variations in the addition of material by the epithelium of the gum. 5. One of the functions of the epithelium that covers the corium wall is that it serves as a layer by which the cortex slides from the corium wall. The long range and gradual increase in thickness of the baleen plate, and consequently also of the cortex, is mainly a result of the addition of material to the inner side of the cortex by this epithelium. 6. It is shown that the peaks and hollows are instantaneous formations, resulting from increased mitotic activity in the epithelium of the gum. These extra thickenings are only formed at a special point at the very first origin of the cortex. So the \xe2\x80\x9cgrowth periods\xe2\x80\x9d in which the records of baleen plates can be divided, by means of the \xe2\x80\x9cregular\xe2\x80\x9d occurrence of peaks and hollows, are conclusive in age determination. 7. The variations in thickness of the cortical layer of the baleen plate visible as peaks in the records, are probably caused by changes in the physiological balance of the Fin Whale. These changes are of comparatively short duration. They may e.g. be caused by the mitotic stimulating activity of hormones, produced by the ovaries during ovulation. Owing to such a stimulus more material is added to both sides of the cortex. This is visible as a thickening only on the outer surface because here all the extra material is added at one point, whereas to the inner side of the cortex material is added along the whole length. 8. The cells of the stratum spinosum in the \xe2\x80\x9croot\xe2\x80\x9d of the baleen plate maintain their mutual contact in the desmosomes. These structures are always visible in all microscopic sections of the various parts of this stratum. 9. The coarse tonofibrils run through the cells from the desmosomes in one part of the cell wall to the desmosomes in another, mostly opposite, part. 10. The tonofibrils are not present in all cells of the stratum spinosum of the gum and nowhere in the stratum spinosum of the epithelium between the corium wall and the cortex. 11. The presence of tonofibrils in the stratum spinosum of the gum of the Fin Whale and the Blue Whale is most probably caused by shrinkage of the cells, e.g. under the influence of the fixing fluid. The main direction of this shrinkage of the cells and the direction in which the tonofibrils run, is determined by forces that work on the cells in the epithelium, caused by mitotic activity.
    Repository Name: National Museum of Natural History, Netherlands
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  • 47
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 38 no. 1, pp. 23-30
    Publication Date: 2024-01-12
    Description: An occipito-parietal skull fragment of a male specimen of Odobenus antverpiensis (Rutten, 1907), from the mouth of the River Scheldt (Netherlands) is described and figured. The animal lived probably about the transition Scaldisian-Merxemian (Pliocene-Pleistocene). It lived in coastal marine surroundings rich in shell-bearing molluscs and is not necessarily an indication of cool conditions.
    Repository Name: National Museum of Natural History, Netherlands
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  • 48
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 38 no. 1, pp. 13-15
    Publication Date: 2024-01-12
    Description: Keeping and breeding animals which are threatened with extinction in their natural habitat, should be one of the most important tasks of zoological gardens today. Efforts should be focussed on finding the zootechnical solution of problems which will arise inevitably, especially if rare species, or those that have the reputation of being difficult to keep or to breed, are concerned.\nThe Orang-Utan ( Pongo pygmaeus (Hoppius)) has been kept in Zoos for more than a century. As a matter of fact this species was on exhibition regularly in the Zoos of the Netherlands during the nineteenth century. Orang-Utans were, a hundred years ago, much more common in the Zoological Gardens of Amsterdam and Rotterdam than Chimpanzees. Longevity records however were very poor indeed. Hundreds and hundreds of these apes must have been imported on Dutch ships to keep up a regular stock. This is not surprising, because the least knowledge of the basic needs of these apes was lacking. Unsuitable food, lack of medicine and the wrong opinion that tropical animals should be kept in overheated quarters, caused the death of innumerable animals. The direct cause of death was either intestinal trouble or Tuberculosis. Under these circumstances breeding could not be expected. The first female Orang-Utan which came to a Zoo with its baby, the famous Buschi in Dresden Zoo, caused quite a sensation. But even in recent times the breeding of apes proved to be difficult. With better zoo-technical knowledge, Chimpanzees can be bred regularly. Orang-Utan and Gorilla however maintained the reputation of being difficult breeders. The first Zoo that started breeding Orangs regularly was Philadelphia. Afterwards several other Zoos, among which the Royal Rotterdam Zoo, succeeded in building up a breeding group. The Rotterdam Zoo was the first in breeding a second generation.
    Repository Name: National Museum of Natural History, Netherlands
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  • 49
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 38 no. 1, pp. 31-38
    Publication Date: 2024-01-12
    Description: On 22-VII-1960 I caught some specimens of Salamandra salamandra fastuosa Schreiber between Lago Ercina and Lago Enol, \xc2\xb1 1000 m above Covadonga (Picos de Europa, Cantabrian Mountains, Spain). On 14-VIII-1961 from one of the salamanders two young were born (length 40 and 45 mm). Only one specimen showed traces of gills \xc2\xb1 1.5 mm long, both specimens were in all other characters completely metamorphosed, also the colour pattern resembled the typical fastuosa-pattern, i.e. longitudinal yellow stripes almost without interruption (see fig. 1). The 15th of August two more young were born, both with gills, the smallest specimen (35 mm) in the form of a normal larva (fig. 2) with gills of \xc2\xb1 4 mm and with a normal larval coloration. One day later a fifth young was born, also purely larval in form and colour. The last one was completely metamorphosed on 3-X-1961. Freytag mentions 2-3 months for the larval period, so the development of the young fastuosa which were not discernable from normal larvae, took only a relatively short time. No more than 5 young were born.\nIn March 1967 the same female deposited \xc2\xb1 30 unfertilized eggs in the water of the paludarium. The difference between the small litter and the large number of eggs (in large specimens 70 or more larvae may be born) suggests a same kind of pregnancy as in Salamandra atra, in which only two completely metamorphosed young are born, which are fed before birth with the other eggs.
    Repository Name: National Museum of Natural History, Netherlands
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  • 50
    facet.materialart.
    Unknown
    In:  Bijdragen tot de dierkunde vol. 36 no. 1, pp. 69-73
    Publication Date: 2024-01-12
    Description: 1. Bei der Geburt behalten die Weibchen von Myotis myotis und Eptesicus serotinus die typische H\xc3\xa4ngelage der Flederm\xc3\xa4use, den Kopf nach unten, bei. Sie heften sich jedoch auch mit den Krallen an der Unterlage fest, wodurch der K\xc3\xb6rper ggf. die Schr\xc3\xa4glage des Daches bekommt. Hierbei kr\xc3\xbcmmen sie den Schwanz bogenf\xc3\xb6rmig. 2. Das ausgesto\xc3\x9fene Junge klettert zwischen dem K\xc3\xb6rper der Mutter und der Unterlage am K\xc3\xb6rper derselben zur Brustzitze und saugt sich fest. 3. Es wird von der Mutter eifrig beleckt. Durch seitliches H\xc3\xa4ngen des Hinterteiles seines K\xc3\xb6rpers rei\xc3\x9ft das Junge die Nabelschnur ab, wozu oft l\xc3\xa4ngere Zeit und heftiges Zerren notwendig ist. 4. Die vertrocknete Nabelschnur rei\xc3\x9ft an der Placenta ab. Diese wird kurz darauf ausgesto\xc3\x9fen und von der Mutter aufgefressen. 5. Beim Belecken des Jungen bei\xc3\x9ft die Mutter die Nabelschnur an diesem ab. Sie f\xc3\xa4llt zu Boden und wird zwischen den Kotkr\xc3\xbcmchen gefunden. 6. Die L\xc3\xa4nge der Nabelschnur l\xc3\xa4\xc3\x9ft einen R\xc3\xbcckschlu\xc3\x9f auf die Dauer der Abrei\xc3\x9fbewegung und auf ein \xc3\xa4hnliches Verhalten anderer Arten bei der Geburt zu. 7. Bei einer Totgeburt sucht das Alttier sich dieser durch Umherklettern zu entbinden, gelingt dies nicht, so bei\xc3\x9ft sie die Nabelschnur bei sich ab.
    Repository Name: National Museum of Natural History, Netherlands
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