Abstract
As mentioned in the introduction deep-sea deposits were first explored in a comprehensive fashion during the British Challenger Expedition (1873–1876). Many thousands of samples were subsequently studied by John Murray (1841–1914), naturalist on the Challenger. He and his co-worker A. F. Renard published a weighty report on the results, which laid the foundation for all later work in this field of research. The first great step beyond Murray’s work were the results of the German Meteor Expedition, almost half a century later (1927–1929). A new branch of oceanography started with the recovery of long cores by the Swedish Albatross Expedition (1947–1949), that is, Pleistocene oceanography. It revolutionized our understanding of the great Ice Ages. Another great step came in 1968 with GLOMAR Challenger and the Deep Sea Drilling Project, which provided the samples for Tertiary and Cretaceous ocean history.
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Further Reading
Hill MN (ed) (1963) The sea, Ideas and observations on progress in the study of the seas, vol 3. Interscience, New York
Lisitzin AP (1972) Sedimentation in the world ocean. SEPM Spec Publ 17, Soc Econ Paleontol Mineral Tulsa, Okla
Hsü KJ, Jenkyns H (eds) (1974) Pelagic sediments on land and under the sea. Spec Publ Int Assoc Sedimentol 1
Bolli HM, Saunders JB, Perch-Nielsen K (eds) (1985) Plankton stratigraphy. Cambridge Univ Press, New York
Chester R (1990) Marine geochemistry. Unwin Hyman, London
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© 1993 Springer-Verlag Berlin Heidelberg
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Seibold, E., Berger, W.H. (1993). Deep-Sea Sediments — Patterns, Processes, and Stratigraphic Methods. In: The Sea Floor. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-22519-6_9
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DOI: https://doi.org/10.1007/978-3-662-22519-6_9
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