Abstract
Lithologic, faunal, isotopic, and paleomagnetic analyses indicate that the section represents the most complete deep sea record of climatic evolution hitherto recovered at high latitudes in the N Hemisphere. In the upper part of the section, the whole of the standard oxygen isotope record of the past million years is well preserved. The onset of ice-rafting and glacial-interglacial alternations occurs at about 2.4 Myr ago. -Authors
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CITATION STYLE
Zimmerman, H. B. (1984). History of Plio-Pleistocene climate in the northeastern Atlantic, Deep Sea Drilling Project Hole 552A. Initial Reports DSDP, Leg 81, Southampton to Azores. US Govt. Printing Office; UK distributors, IPOD Committee, NERC, Swindon. https://doi.org/10.2973/dsdp.proc.81.137.1984
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