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  • 2020-2022  (1,241,797)
  • 1950-1954  (228,318)
  • 1940-1944  (110,020)
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  • 1
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    PANGAEA
    In:  Supplement to: Emiliani, Cesare (1954): Pleistocene temperature variations in the Mediterranean. Quarternaria, 2, 87-97
    Publication Date: 2024-06-26
    Description: For temperature investigations, a core in the Mediterranean Sea (No 189 of the Swedish Deep-Sea Expedition 1947-1948) was sampled at approximately 10 m intervals. Globigerina dubia, G. inflata and Globigerinoides rubra were seperated from each sample and their test were investigated for stable oxygen isotopic measurement. Oxygen isotopic analysis showed the following: 1) Ten stages are indicated. 2) The temperature minimum of stage 2 corresponds to a racliocarbon age of 17,200 years. 3) Temperature maxima of odd stages are about equal to the modern August mean, except that of stage 5 which is considerably higher and, probably reflects the influx of ice melt water. 4) Temperature minima of even stages are all very low, especially that of stage 2, and reflect conditions similar to those now prevailing around Newfoundland. 5) The temperature record indicates that during most of the time covered by the core, the Mediterranean was cooler than at present and that conditions similar to the present occurred only during comparatively short intervals. 6) Minor temperature fluctuations occur, especially in the warmer stages, which are of doubtful significance. 7) An average rate of sedimentation of 4.3 cm/1000 years is indicated for the whole core.
    Keywords: Albatross IV (1963); core_189; DEPTH, sediment/rock; Globigerina dubia, δ18O; Globigerina inflata, δ18O; Globigerinoides rubra, δ18O; NODC-0418; PC; Piston corer; SDSE_276; South Levantine Basin; SwedishDeepSeaExpedition
    Type: Dataset
    Format: text/tab-separated-values, 121 data points
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  • 2
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    PANGAEA
    In:  Supplement to: Nybelin, Orvar (1951): Introduction and Station List. In: Pettersson, H. (Ed.), Jerlov, N. and Kullenberg, B. Reports of the Swedish Deep Sea Expedition, Volume II. Swedish Natural Science Research Council Stockholm 23 - Sweden, 1-28
    Publication Date: 2024-06-26
    Description: The cores and dredges described in this report were taken during the Swedish Deep Sea Expedition from July 1947 until October 1948 aboard the S/S Albatross (Boström). A total of 370 cores and trawls during this World circumnavigation.
    Keywords: Albatross IV (1963); Comment; Core; CORE; core_43; core_44; core_45; core_46; core_47; core_48; core_50A; core_51; core_52; core_53; core_56; core_57; core_69; core_70; core_72; core_76; core_80; core_81; core_82; core_87; core_89; Date/Time of event; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Description; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; Method/Device of event; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NODC-0418; North Pacific Ocean; Position; Quantity of deposit; Sample ID; SDSE_065; SDSE_066; SDSE_068; SDSE_069; SDSE_070; SDSE_073; SDSE_076; SDSE_078; SDSE_079; SDSE_081; SDSE_086; SDSE_087; SDSE_102; SDSE_104; SDSE_105-2; SDSE_114-2; SDSE_125-2; SDSE_127-2; SDSE_128; SDSE_136-2; SDSE_139-2; SDSE_373-2; Sediment type; Size; South Atlantic Ocean; South Pacific Ocean; Substrate type; SwedishDeepSeaExpedition; TRAWL; Trawl net; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 276 data points
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  • 3
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    PANGAEA
    In:  Supplement to: Kröll, Victor (1953): Vertical Distribution of Radium in Deep-Sea Sediments. Nature, 171(4356), 742-742, https://doi.org/10.1038/171742a0
    Publication Date: 2024-06-26
    Description: The surprisingly high content of radium in certain deep-sea sediments discovered nearly fifty years ago by J. Joly remained unexplained until 1937, when H. Pettersson suggested an ocean-wide precipitation of ionium from sea water on to the ocean bottom as its origin. Extensive radium measurements on deep-sea cores raised by the Swedish Deep-Sea Expedition carried out in this institute by Pettersson, T. Bernert and me did not confirm the regular vertical distribution of radium reported by other workers. An expected rise in radium content from moderate values in the uppermost surface layers to a maximum corresponding to a radioactive equilibrium between precipitated ionium and ionium-supported radium generally occurred; but the maximum was not followed by the theoretical exponential decline downwards governed by the rate of decay of ionium, to 50 per cent in 83,000 years, to 25 per cent in 166,000 years, etc. Instead, a number of secondary maxima of radium content separated by equally pronounced minima were observed (see graph), which could not well be explained as due to intervening changes in the rate of total sedimentation. Another explanation offered was that ionium and radium are not in radioactive equilibrium; that is, the assumption underlying the use of measurements of radium as indicating the concentration in the same layer of its mother element is unjustified.
    Keywords: Albatross IV (1963); Core; CORE; core_87; Deposit type; DEPTH, sediment/rock; Identification; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; NODC-0418; North Pacific Ocean; Radium; SDSE_136-2; SwedishDeepSeaExpedition
    Type: Dataset
    Format: text/tab-separated-values, 3 data points
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  • 4
    Publication Date: 2024-06-26
    Keywords: Albatross IV (1963); Alboran Sea; Arabian Sea; Canarias Sea; CTD, handheld; Date/Time of event; Density, sigma, in situ; DEPTH, water; Eastern Basin; Elevation of event; Event label; Flores Sea; Gases, dissolved; Gulf of Aden; hCTD; Indian Ocean; Lakshadweep Sea; Latitude of event; Longitude of event; NODC-0418; North Pacific Ocean; Number; Pacific Ocean; pH; Philippine Sea; Phosphate; Red Sea; Salinity; SDSE_043CTD; SDSE_045CTD; SDSE_047CTD; SDSE_048CTD; SDSE_049CTD; SDSE_052CTD; SDSE_055CTD; SDSE_058CTD; SDSE_059CTD; SDSE_060CTD; SDSE_062CTD; SDSE_063CTD; SDSE_065CTD; SDSE_067CTD; SDSE_069CTD; SDSE_070CTD; SDSE_072CTD; SDSE_074CTD; SDSE_076CTD; SDSE_077CTD; SDSE_078CTD; SDSE_079CTD; SDSE_080CTD; SDSE_081CTD; SDSE_082CTD; SDSE_084CTD; SDSE_085CTD; SDSE_086CTD; SDSE_087CTD; SDSE_088CTD; SDSE_089CTD; SDSE_090CTD; SDSE_091CTD; SDSE_093CTD; SDSE_094CTD; SDSE_102CTD; SDSE_105CTD; SDSE_108CTD; SDSE_111CTD; SDSE_113CTD; SDSE_115CTD; SDSE_116CTD; SDSE_119CTD; SDSE_121CTD; SDSE_122CTD; SDSE_123CTD; SDSE_126CTD; SDSE_128CTD; SDSE_129CTD; SDSE_130CTD; SDSE_131CTD; SDSE_133CTD; SDSE_135CTD; SDSE_137CTD; SDSE_138CTD; SDSE_143CTD; SDSE_150CTD; SDSE_157CTD; SDSE_162CTD; SDSE_173CTD; SDSE_183-184CTD; SDSE_190CTD; SDSE_196CTD; SDSE_200CTD; SDSE_202CTD; SDSE_204CTD; SDSE_205CTD; SDSE_206CTD; SDSE_207CTD; SDSE_208CTD; SDSE_211CTD; SDSE_213CTD; SDSE_216CTD; SDSE_220CTD; SDSE_223CTD; SDSE_225CTD; SDSE_227CTD; SDSE_228CTD; SDSE_232CTD; SDSE_235CTD; SDSE_240CTD; SDSE_243CTD; SDSE_244CTD; SDSE_246CTD; SDSE_247CTD; SDSE_248CTD; SDSE_251CTD; SDSE_254CTD; SDSE_261CTD; SDSE_262CTD; SDSE_263CTD; SDSE_266CTD; SDSE_267CTD; SDSE_268CTD; SDSE_269CTD; SDSE_270CTD; SDSE_271CTD; SDSE_272CTD; SDSE_285CTD; SDSE_301CTD; SDSE_306CTD; SDSE_307CTD; SDSE_308CTD; SDSE_309CTD; SDSE_314CTD; SDSE_319CTD; SDSE_321CTD; SDSE_322CTD; SDSE_323CTD; SDSE_325CTD; SDSE_326CTD; SDSE_327CTD; SDSE_328CTD; SDSE_330CTD; SDSE_332CTD; SDSE_333CTD; SDSE_335CTD; SDSE_336CTD; SDSE_337CTD; SDSE_340CTD; SDSE_342CTD; SDSE_343CTD; SDSE_344CTD; SDSE_345CTD; SDSE_347CTD; SDSE_349CTD; SDSE_351CTD; SDSE_353CTD; SDSE_354CTD; SDSE_357CTD; SDSE_360CTD; SDSE_362CTD; SDSE_367CTD; SDSE_371CTD; SDSE_373CTD; SDSE_384CTD; SDSE_387CTD; SDSE_400CTD; Silicate; South Atlantic Ocean; South Pacific Ocean; Strait of Gibraltar; SwedishDeepSeaExpedition; Temperature, water; Western Basin
    Type: Dataset
    Format: text/tab-separated-values, 15537 data points
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  • 5
    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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  • 6
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    Unknown
    Diesterweg
    Publication Date: 2024-04-22
    Type: Article , PeerReviewed
    Format: text
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  • 7
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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
    Type: doc-type:carthographicMaterial
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  • 8
    Publication Date: 2024-01-12
    Description: Voorjaar 1949 ontving ik een kleine collectie levende vissen uit Suriname (Nederlands Guiana), door een zeeman verzameld in een poel nabij Paramaribo. Helaas is de juiste vindplaats niet nader aangegeven, dan enige kilometers ten zuiden van de hoofdstad.\nOnmiddellijk na ontvangst werden de vissen, die hier het onderwerp van bespreking zijn, in een groot gezelschapsaquarium (150 X 60 X 50 cm. hoog) ondergebracht, dat reeds werd bevolkt door verscheidene Nannostomini, Hasemania marginata, Rivulus cylindraceus, Acanthophthalmus kuhli, Dermogenus pusillus en Nannacara anomala en N. taenia.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 9
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    In:  Zoologische Verhandelingen vol. 12 no. 1, pp. 1-64
    Publication Date: 2024-01-12
    Description: The increased importance which the European red mite (Paratetranychus pilosus (Can. et Fanz.)) (= Metatetranychus ulmi (Koch)) has assumed in recent years has led to an intensive study of its biology and natural history.\nIn the course of these investigations many workers, and in particular those in Nova Scotia (vide Lord, 1949), have become convinced that this pest can be controlled, on apple trees at least, by natural means and that some of the most active agents in its eradication are the representatives of that group of predaceous mites which Vitzthum (1941) placed in the subfamily Phytoseiinae Ber\'lese, 1916 1). As the late Dr. A. C. Oudemans of Arnhem included many if not most of these species in the genus Typhlodromus as he conceived it, this paper is in essence a revision of that genus.\nPresumably because of their small size and limited distribution, which is largely contingent upon readily available populations of their hosts, little attention has been paid to these predators from either the ecological or taxonomic point of view. A cursory survey of the literature pertaining to the predaceous relationship which exists between the Phytoseiinae herein to be discussed and the tetranychid mites may serve as an appraisal of this economically significant group of mites. Koch (1839) in describing what now appears to be a typhlodromid, viz., Gamasus vepallidus, made no reference to its possible predaceous habits. Scheuten (1857) thought that the eriophyids which he found associated in numbers with his Typhlodromus pyri were its offspring. Berlese (1882-1898), however, had a better understanding of these relationships and was able to state in his redescription of G. vepallidus as Seius (Seiulus) vepallidus (K.) that it was a predator of small acari as well as being a mycophage. His countryman, Ribaga (1902), writing of the
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 10
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    In:  Zoologische Verhandelingen vol. 11 no. 1, pp. 1-34
    Publication Date: 2024-01-12
    Description: CONTENTS\nIntroduction............... 3\nSystematic survey of the Limacidae of the central and western Canary Islands 5 Biogeographical notes on the Limacidae of the Canary Islands . . . . 21 Alphabetical list of the persons who collected or observed Limacidae in the Canary Islands.............. 31\nLiterature............... 32\nINTRODUCTION\nIn the spring of 1947 I was so fortunate as to join for some 9 weeks the Danish Zoological Expedition to the Canary Islands. During my stay I collected materials for the Rijksmuseum van Natuurlijke Historie at Leiden, paying special attention to the land- and freshwater Mollusca. This paper contains the first results of the examination of the Mollusca collected.\nMy Danish friends Dr. Gunnar Thorson and Dr. Helge Vols\xc3\xb8e generously put at my disposal the non-marine Mollusca they collected during their stay in the Canaries. When the material has been worked up, duplicates will be deposited in the Zoological Museum at Copenhagen.\nI am indebted to several persons who helped me in various ways in the investigations here published. Prof. Dr. N. Hj. Odhner (Stockholm) very kindly put at my disposal a MS list of all the Mollusca of the Canary Islands and their distribution, which he had compiled for private use. Mr. Hugh Watson (Cambridge) never failed to help me by examining or lending specimens, and in detailed letters gave me the benefit of his great experience.\nDuring my stay in Paris in March 1950 Dr. G. Ranson and Dr. A. Franc put at my disposal for examination the Canarian slugs present in the Mus\xc3\xa9um
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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