Oxygen isotope composition of benthic and planktonic foraminifera from ODP Holes 146-893A and 167-1017B, supplement to: Cannariato, Kevin G; Kennett, James P (2005): Structure of the penultimate deglaciation along the California margin and implications for Milankovitch theory. Geology, 33(2), 157-160

Kevin G Cannariato & James P Kennett
The detailed structure and timing of the penultimate deglaciation are insufficiently defined yet critical for understanding mechanisms responsible for abrupt climate change. Here we present oxygen isotope records (from planktonic and benthic foraminifera) at unprecedented resolution encompassing late marine oxygen isotope stage (MIS) 6 and Termination II (ca. 150-120 ka) from the Santa Barbara Basin, supported by additional southern California margin records, a region highly sensitive to millennial-scale climate oscillations during the last deglaciation. These...
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