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- W2076403122 abstract "Earth's climate underwent a major transition from the warmth of the late Pliocene, when global surface temperatures were ~2° to 3°C higher than today, to extensive Northern Hemisphere glaciation (NHG) ~2.73 million years ago (Ma). We show that North Pacific deep waters were substantially colder (4°C) and probably fresher than the North Atlantic Deep Water before the intensification of NHG. At ~2.73 Ma, the Atlantic-Pacific temperature gradient was reduced to <1°C, suggesting the initiation of stronger heat transfer from the North Atlantic to the deep Pacific. We posit that increased glaciation of Antarctica, deduced from the 21 ± 10-meter sea-level fall from 3.15 to 2.75 Ma, and the development of a strong polar halocline fundamentally altered deep ocean circulation, which enhanced interhemispheric heat and salt transport, thereby contributing to NHG." @default.
- W2076403122 created "2016-06-24" @default.
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- W2076403122 creator A5030181995 @default.
- W2076403122 creator A5063121136 @default.
- W2076403122 creator A5064756534 @default.
- W2076403122 date "2014-11-14" @default.
- W2076403122 modified "2023-10-17" @default.
- W2076403122 title "Antarctic role in Northern Hemisphere glaciation" @default.
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- W2076403122 doi "https://doi.org/10.1126/science.1255586" @default.
- W2076403122 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/25342658" @default.
- W2076403122 hasPublicationYear "2014" @default.
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