Planktonic foraminifera in ODP Hole 160-963A, supplement to: Sprovieri, Rodolfo; Di Stefano, Enrico; Incarbona, Alessandro; Oppo, Delia W (2006): Suborbital climate variability during Marine Isotopic Stage 5 in the central Mediterranean basin: evidence from calcareous plankton record. Quaternary Science Reviews, 25(17-18), 2332-2342Rodolfo Sprovieri, Enrico Di Stefano, Alessandro Incarbona & Delia W Oppo
New faunal and floral records from Ocean Drilling Project Hole 963A, resolved at ?80-year spacing, provide evidence of suborbital scale climate variability in the central Mediterranean Sea throughout Marine Isotope Stage (MIS) 5. Cold events in the central Mediterranean Sea, indicated by low abundances of warm species and high abundances of cold species, are also evident in a planktonic foraminifera paleoclimatic curve. They have been linked to NGRIP Greenland ice core “C” events and appear...
16 citations reported since publication in 2006.
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