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Arrhenius, Gustaf (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
A method has been developed for using deep sea deposits as records of oceanic productivity and its changes. The sequence of sediments below the Equatorial Current system indicates a marked periodical change in productivity with time. This periodicity is assumed to correspond closely to the world-wide climatic changes during late Pliocene and Pleistocene. It is thought that the method offers possibilities for an accurate and detailed study of the history of the late Cenozoic climate. An explanation is given of the reaction of the Equatorial Counter Current to climatic changes.DOI: 10.1111/j.2153-3490.1950.tb00316.x
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    • -b.: T h e Swedish Deep Sca Expedition. T h e geological material and its treatment with special regard to the Eastern Pacific. Ccologiskn Furenirigetis i Sfockholm Forhartdlingrir. 7 2 , 2.
    • GRAHAMH,. W. 1941: Plankton production in relation t o character of water in the open Pacific. f o w . Maritie Reseurcli, 4. p. x89.
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    • -, 1 9 4 0 : Possible causes of change in climate and their limitations. Linri. So(. Londoti. Proc. 152, p. 190.
    • SVERDRUPH, . U., JOHNION, M. W. and FLEMING, R. H. 1946. The Oceans. N e w York.
    • WEIBULLW,. 1949: A statistical analysis of the size of Cyrtoidea in sediment cores from the East Pacific ocean. Nature, 164, p. 1047.
    • ZEUNERF,. E. 1945: The pleistocene period, itc climate, chronology and faunal succesions. London.
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