Abstract
In this study, the authors determined the oxygen and carbon isotopic compositions of three planktonic foraminiferal species, a benthonic foraminifer, and calcareous nannofossil assemblages, throughout DSDP (Deep Sea Drilling Project) site 284, which extends in age from Late Miocene to present-day. This investigation is the first to compare the stable isotopic composition of several different microfossil forms throughout such a Late Cenozoic sequence. The objectives of the study were: (1) to compare and contrast the oxygen isotopic records of several different microfossils; (2) to evaluate the isotopic data in terms of paleotemperature and paleoglacial history during the Late Cenozoic; (3) to provide additional data on carbon isotope variations in the Late Cenozoic; and (4) evaluate possible relations between the stratigraphic distribution of volcanic glass (ash) and the oxygen isotopic-paleoclimatic record.
Cite
CITATION STYLE
Kennett, J. P., Shackleton, N. J., Margolis, S. V., Goodney, D. E., Dudley, W. C., & Kroopnick, P. M. (1979). LATE CENOZOIC OXYGEN AND CARBON ISOTOPIC HISTORY AND VOLCANIC ASH STRATIGRAPHY: DSDP SITE 284, SOUTH PACIFIC. Am J Sci, 279(1), 52–69. https://doi.org/10.2475/ajs.279.1.52
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