Generally, small and frequent changes in upper Miocene and lower Pliocene foraminiferal d18O and d13C in Hole 552A are not easily interpreted without correlation with other sites.-from Author
CITATION STYLE
Keigwin, L. D. (1984). Stable isotopic results on upper Miocene and lower Pliocene foraminifers from Hole 552A. Initial Reports DSDP, Leg 81, Southampton to Azores, 595–597. https://doi.org/10.2973/dsdp.proc.81.115.1984
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