(Appendix) Planktonic foraminifera abundances in ODP Site 138-847B ...

Sediments from Site 847 in the eastern equatorial Pacific Ocean provide a record of the variability of the equatorial divergence and associated upwelling. We interpret the variation in foraminifer assemblages in the context of regional Oceanographic change. Our record is composed of three time slice...

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Bibliographic Details
Main Authors: McKenna, V S, Farrell, John W, Murray, David W, Clemens, Steven C
Format: Dataset
Language:English
Published: PANGAEA 1995
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.807318
https://doi.pangaea.de/10.1594/PANGAEA.807318
Description
Summary:Sediments from Site 847 in the eastern equatorial Pacific Ocean provide a record of the variability of the equatorial divergence and associated upwelling. We interpret the variation in foraminifer assemblages in the context of regional Oceanographic change. Our record is composed of three time slices selected from the last 0.9 Ma. A Q-mode analysis of foraminifer abundance data results in a four-factor model that was used to quantify the faunal changes and to characterize paleoceanographic variability. The species of foraminifers with high factor scores for each factor suggested a specific set of Oceanographic conditions. The timing of the high loadings for each factor appears to be associated with a particular part of a glacial cycle. Thus, we interpreted our findings in the context of the glacial/interglacial cycle proposed by Imbrie et. al. (1992). This idealized cycle consists of four stages that are defined by characteristic changes in specific elements of the climate system. We evaluated how such ... : DEPTH, sediment is given in mbsf. Time Slice 1 (TSI) covers oxygen isotope stages 1 to 6 (0-0.135 Ma), Time Slice 2 (TS2) covers stages 11 to 14 (0.395-0.572 Ma), and Time Slice 3 (TS3) covers stages 18 to 21 (0.704-0.852 Ma). ...