A deep Eastern Equatorial Pacific thermocline during the early Pliocene warm period
During the early Pliocene warm period (∼4.6–4.2Ma) in the Eastern Equatorial Pacific upwelling region, sea surface temperatures were warm in comparison to modern conditions. Warm upwelling regions have global effects on the heat budget and atmospheric circulation, and are argued to have contributed...
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Veröffentlicht in: | Earth and planetary science letters 2012-11, Vol.355-356, p.152-161 |
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Sprache: | eng |
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