Abstract
Deep Sea Drilling Project Site 366 recovered a record with a minor unconformity in the "middle' Oligocene and a condensed middle Miocene section. Ocean Drilling Program Site 667 recovered an apparently continuous "middle' Oligocene to lower middle Miocene record and a similar condensed middle Miocene section. The Oligocene to lower Miocene sections were deposited at similar sedimentation rates (~11-16 m/m/y.). In addition to earliest Oligocene and middle Miocene δ18O increases, a distinct δ18O increase occurred near the Oligocene/Miocene boundary. Carbon isotope variations provide similar potential for improving correlations. -from Authors
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CITATION STYLE
Miller, K. G., Wright, J. D., & Brower, A. N. (1989). Oligocene to Miocene stable isotope stratigraphy and planktonic foraminifer biostratigraphy of the Sierra Leone Rise (DSDP Site 366 and ODP Site 667). Proc., Scientific Results, ODP, Leg 108, Eastern Tropical Atlantic, 279–294. https://doi.org/10.2973/odp.proc.sr.108.177.1989
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