. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 712 ARKHENIUS [chap. 25 characterized by less variability with time of the carbonate content. The Pliocene-Pleistocene transition is indicated by a drop in the temperature of the bottom water, shown by the oxygen isotope distribution in benthonic Fora- minifera (Emiliani and Edwards, 1953), and by a marked change in the fossil CaC03 90% 0_ Depth. lOOOi cm Core SW 60 1°35'N,134°57'W 30 60% -i—\—\—I—\—r. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. 712 ARKHENIUS [chap. 25 characterized by less variability with time of the carbonate content. The Pliocene-Pleistocene transition is indicated by a drop in the temperature of the bottom water, shown by the oxygen isotope distribution in benthonic Fora- minifera (Emiliani and Edwards, 1953), and by a marked change in the fossil CaC03 90% 0_ Depth. lOOOi cm Core SW 60 1°35'N,134°57'W 30 60% -i—\—\—I—\—r. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.
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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectoceanbottom
