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  • 1950-1954  (228,318)
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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
    Call number: PIK 24-95750
    Description / Table of Contents: Es gibt massenhaft Lektüre über den Klimawandel, doch zwei Arten bestimmen das Genre: die eine, die auf dramatische Weise vor der Apokalypse warnt, und die andere, die den Alarmismus als trojanisches Pferd politischer Kräfte entlarven will. Beide blenden Wesentliches aus: Einerseits hat die Wissenschaft überzeugend dargelegt, dass es ein Klimaproblem gibt, andererseits wird es tatsächlich politisch ausgebeutet. Anstatt also eine der beiden Kategorien zu bedienen, erzählt dieses Buch, wie aus dem Nischenfach der Meteorologie das bestimmende Thema unserer Zeit wurde. Das liegt keineswegs nur daran, dass die globale Erwärmung manifeste Risiken mit sich bringt, sondern auch daran, dass Wissenschaft als Vehikel für Macht, Einfluss und Geld missbraucht wird. Während der Klimawandel voranschreitet, eskaliert zugleich ein Lobbykrieg, der Einzelinteressen dient, aber die Lösung des zugrundeliegenden Problems erschwert. Dubiose Studien und politisierte Wissenschaftler stärken global operierende Institutionen und unterwerfen Deutschland im Dienste des Umweltschutzes einer unbarmherzigen Agenda.
    Type of Medium: Monograph available for loan
    Pages: 285 Seiten , Illustrationen , 21.5 cm x 13.5 cm
    Edition: 1. Auflage
    ISBN: 978-3-86489-461-9 , 9783864894619
    Language: German
    Note: Inhalt Prolog I. Kampf um Einfluss 1. Ignorierter Pionier: Der erste Klimaforscher 2. Zwischen Militär und Katastrophe: Die Relevanz-Falle 3. »Earth Day«: Umweltschutz wird links 4. Umweltschutz als Statuskampf: Alte Reiche gegen neue Reiche 5. Eiszeit-Alarm: Wissenschaft als Autoritätsressource 6. UN-Umweltkonferenz: Neue Bühne für Rivalen 7. Ölkrise: Rohstoff-Waffe gegen den Westen II. CO2 wird Machtfrage 8. Erwärmung statt Eiszeit: Geniale Propheten 9. Polarisierung: Konservative Gegner der Klimaforschung 10. Erste Klimakonferenz: Auf Konfrontationskurs 11. Kalter Krieg ums Klima: Der verschollene Klimaforscher 12. Medien als Adjutanten: Wie die Atomlobby die Klimakatastrophe in Deutschland populär gemacht hat 13. Villach-Treffen '85: Der Wow-Effekt 14. Gründung des Weltklimarats: Ausgetrickste USA III. Das wichtigste Thema der Welt 15. »Global Warming Has Begun«: Der Sündenfall 16. CO2-Woodstock: Die NGO-Industrie entdeckt das Klima 17. Eklat an der Ostsee: Ringen um Deutungshoheit 18. Erdgipfel '92: Die neue Weltordnung 19. Frankenstein-Syndrom: Wissenschaft, zum Liefern verdammt 20. Bedrohte Geschäftsmodelle: Angriff der Skeptiker 21. Forscher-Triumph über Skeptiker: Die Überwindung des Trotz-Positivismus IV. Auf der Suche nach dem Menschensignal 22. Gefährliche Nähe: »Noble Cause Corruption« 23. »Bäume sind mir wichtig«: Deutschland will Klima-Musterschüler sein 24. Windige Werbung: Immer-schlimmer-ismus 25. Überfrachtete Klimaforschung: Der Knacks 26. Das ersehnte Ergebnis: Klaus Hasselmann und die Entdeckung des Menschensignals 27. UN-Klimaverhandlungen: Der Placebo-Effekt V. Es wird persönlich 28. Misslungener Putsch: Die verflixte Chef-Rochade 29. Krieg um den Hockeyschläger: Tribalistische Konkurrenz 30. UN-Klimarat: Kleine Fehler, großer Skandal 31. Attacken der Klimalobby: Die Mär von den schlimmeren Wetterkatastrophen 32. Befangenheit beim Klimarat: Kabale und Stürme 33. Hurrikane: Falsche Maskottchen des Klimawandels 34. Nicht neutrale Boten: Klimaschützer verhindern Klimaschutz 35. Kulturelle Kognition: Wir gegen sie VI. Politisierte Wissenschaft 36. Regierungsbericht: Bestellter Weltuntergang 37. Klima-Klientelismus: Die Unterdrückung der Kernfrage 38. Extremszenarien: Kühler Klimarat 39. Autorität der Klimamodelle: Verheißung von Kontrolle 40. »Burning Embers«: Die wirkungsvolle Glut-Grafik 41. Konsens-Behauptung: Die Mär von den 97 Prozent, die sich einig sind 42. 1,5.Grad: Niemand weiß, wie das UN-Ziel in den Klimavertrag gelangt ist 43. Greta Thunberg: Das Geheimnis des einsamen Schulstreiks VII. Triumph der Klimalobby 44. Masterplan: Der Aufstieg der Klimalobby 45. Deutschlands Klimalobby: Die Große Transformation 46. Eingebettet: Journalisten und die Klimalobby 47. Zweifelhafte Klimawandel-Beweise: Den Nachrichtenzyklus schaffen 48. Klimanotstand: »Ich bin nicht radikal. Die Situation ist radikal.« 49. »RCP8.5«: Nützliche Horrorprognosen 50. »ESG«: Klimadiktat für Unternehmen 51. »Planetare Grenzen«: Die Behauptung von Knappheit verleiht Macht 52. Kipppunkte: Erkämpfte Drohkulisse 53. Verfassungsgericht: Fragliche Klimathesen als Corpus Delicti Nachwort: Was nottut Danksagung Quellen
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 6
    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
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  • 7
    facet.materialart.
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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
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  • 8
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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
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  • 9
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    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 7 no. 1, pp. 1-145
    Publication Date: 2024-01-12
    Description: The present paper is an extension of my revision of the Malaysian species of the genus Dillenia L. (Wormia Rottb. included) inserted in the revision of the Dilleniaceae in the Flora Malesiana ser. I, vol. 4, part 3, pp. 141\xe2\x80\x94174, published in December 1951. A critical revision of the whole genus has never been published before; the unfortunate result of this has been that the delimitation of Dillenia and Wormia, usually as distinct genera, has been based on different characters by various authors. The extension of the revision for the Flora Malesiana so as to include the extra-malaysian species enabled me to study a number of species, the knowledge of which certainly confirmed me in my idea that the characters on which Dillenia and Wormia had been separated before are certainly not the primary characters, to be used in the taxonomic treatment of the genus.\nAll specimens and literature mentioned in this work have been examined by me, unless indicated otherwise; excepted are the specimens of the U.S. National Herbarium., of which I have only examined those collections, of which no duplicates were available from other herbaria. Particulars, not to be taken from the herbarium specimens themselves, such as habit, height, diameter, colour, etc., have been taken from the collectors\xe2\x80\x99 notes and, as far as reliable, from the literature, and are inserted in the descriptions; if there are contradictory data, they are discussed under the Notes.
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 10
    facet.materialart.
    Unknown
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 7 no. 3, pp. 595-598
    Publication Date: 2024-01-12
    Description: Exbucklandia R. W. Brown ( Bucklandia R. Br. non Pr. ex Sternb., Symingtonia Steen.) In an article on \xe2\x80\x9cAlterations in some fossil and living floras\xe2\x80\x9d (J. Wash. Ac. Sc. 36: 348. Oct. 1946) R. W. Brown proposed the new generic name Exbucklandia for the Hamamelidaceous genus Bucklandia R. Br., non Pr. ex Sternb., while describing a new fossil species from the United States. He also transferred B. populnea to the new genus. Unfortunately I had overlooked this publication when proposing Symingtonia to replace Bucklandia R. Br. (Acta Bot. Neerl. 1: 443\xe2\x80\x94444. 1952). Exbucklandia will have to be accepted for it in future. The Indo-Chinese species B. tonkinensis Lecomte should be referred to as Exbucklandia tonkinensis (Lecomte) Steen. comb. nov. I have to thank Dr E. H. Walker for pointing my attention to R. W. Brown\xe2\x80\x99s paper.
    Repository Name: National Museum of Natural History, Netherlands
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