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Patterns of CaCO₃deposition in the eastern tropical Pacific Ocean for the last 150 kyr: Evidence for a southeast Pacific depositional spike during marine isotope stage (MIS) 2

ScholarsArchive at Oregon State University

Field Value
Title Patterns of CaCO₃deposition in the eastern tropical Pacific Ocean for the last 150 kyr: Evidence for a southeast Pacific depositional spike during marine isotope stage (MIS) 2
Names Lyle, Mitchell (creator)
Mix, Alan C. (creator)
Pisias, Nicklas G. (creator)
Date Issued 2002 (iso8601)
Note Copyright 2002 by the American Geophysical Union
Abstract We constructed biogenic mass accumulation rate (MAR) time series for eastern Pacific core transects across the equator
at ~105˚and ~85˚W and along the equator from 80˚to 140˚W. We used empirical orthogonal function (EOF) analysis to
extract spatially coherent patterns of CaCO₃deposition for the last 150 kyr. EOF mode 1 (51% variance) is a CaCO₃MAR
spike centered in marine oxygen isotope stage 2 (MIS 2) found under the South Equatorial Current. EOF mode 2 (19% of
variance) is high north of the equator. EOF mode 3 (9% of variance) is an east-west mode centered along the North
Equatorial Counter Current. The MIS 2 CaCO₃spike is the largest event in the eastern Pacific for the last 150 kyr: CaCO₃MARs are 2–3 times higher at 18 ka than elsewhere in the record, including MIS 6. It is caused by high CaCO₃production
rather than minimal dissolution. EOF 2, while it resembles deep water flow patterns, nevertheless, shows coherence to Corg
deposition and is probably also driven by CaCO₃production.
Genre Article
Identifier Lyle, Mitchell, Alan Mix, and Nicklas Pisias. "Patterns of CaCO₃deposition in the eastern tropical Pacific Ocean for the last 150 kyr: Evidence for a southeast Pacific depositional spike during marine isotope stage (MIS) 2." Paleoceanography 17.2 (2002).

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