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231Pa/230Th evidence for a weakened but persistent Atlantic meridional overturning circulation during Heinrich Stadial 1

Louisa I. Bradtmiller (), Jerry F. McManus and Laura F. Robinson
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Louisa I. Bradtmiller: Macalester College
Jerry F. McManus: Lamont-Doherty Earth Observatory of Columbia University
Laura F. Robinson: Woods Hole Oceanographic Institution

Nature Communications, 2014, vol. 5, issue 1, 1-8

Abstract: Abstract The strength of Atlantic meridional overturning circulation is believed to affect the climate over glacial-interglacial and millennial timescales. The marine sedimentary 231Pa/230Th ratio is a promising paleocirculation proxy, but local particle effects may bias individual reconstructions. Here we present new Atlantic sedimentary 231Pa/230Th data from the Holocene, the last glacial maximum and Heinrich Stadial 1, a period of abrupt cooling ca. 17,500 years ago. We combine our results with published data from these intervals to create a spatially distributed sedimentary 231Pa/230Th database. The data reveal a net 231Pa deficit during each period, consistent with persistent 231Pa export. In highly resolved cores, Heinrich 231Pa/230Th ratios exceed glacial ratios at nearly all depths, indicating a significant reduction, although not cessation, of overturning during Heinrich Stadial 1. These results support the inference that weakened overturning was a driver of Heinrich cooling, while suggesting that abrupt climate oscillations do not necessarily require a complete shutdown of overturning.

Date: 2014
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:5:y:2014:i:1:d:10.1038_ncomms6817

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DOI: 10.1038/ncomms6817

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