The effect of the Pliocene temperature pattern on silicate weathering and Pliocene–Pleistocene cooling
Abstract CO 2 CO 2 ∘ C, suggesting that the demise of the permanent El Niño could have had a small amplifying effect on cooling from the early Pliocene into the Pleistocene. For the reduced Equator–pole gradient, the weathering increases and decreases largely cancel, leading to no detectable difference in global temperature at carbon cycle equilibrium. A robust SST reconstruction of the Pliocene is needed for a quantitative evaluation of the weatherability pattern effect.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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The effect of the Pliocene temperature pattern on silicate weathering and Pliocene–Pleistocene cooling ; volume:19 ; number:7 ; year:2023 ; pages:1461-1479 ; extent:19
Climate of the past ; 19, Heft 7 (2023), 1461-1479 (gesamt 19)
- Creator
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Maffre, Pierre
Chiang, John C. H.
Swanson-Hysell, Nicholas L.
- DOI
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10.5194/cp-19-1461-2023
- URN
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urn:nbn:de:101:1-2023072704274659374242
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:55 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Maffre, Pierre
- Chiang, John C. H.
- Swanson-Hysell, Nicholas L.
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