Rapid coupling between solid earth and ice volume during the Quaternary

Rapid coupling between solid earth and ice volume during the Quaternary

The solid earth plays a major role in controlling Earth’s surface climate. Volcanic degassing of carbon dioxide (CO 2 ) and silicate chemical weathering are known to regulate the evolution of climate on a geologic timescale (> 10 6  yr), but the relationship between the solid earth and the shorte...

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Veröffentlicht in:Scientific reports 2021-03, Vol.11 (1), p.5695-14, Article 5695
Hauptverfasser: Kuwahara, Yusuke, Yasukawa, Kazutaka, Fujinaga, Koichiro, Nozaki, Tatsuo, Ohta, Junichiro, Sato, Honami, Kimura, Jun-Ichi, Nakamura, Kentaro, Yokoyama, Yusuke, Kato, Yasuhiro
Format: Artikel
Sprache:eng
Schlagworte:
704/106/2738
704/106/413
704/2151/209
704/2151/3930
704/829/827
Carbon dioxide
Climate change
Degassing
Earth
Humanities and Social Sciences
Ice
Ice sheets
Isotopes
multidisciplinary
Ocean floor
Osmium
Science
Science (multidisciplinary)
Sea level
Seawater
Weathering
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Zusammenfassung:The solid earth plays a major role in controlling Earth’s surface climate. Volcanic degassing of carbon dioxide (CO 2 ) and silicate chemical weathering are known to regulate the evolution of climate on a geologic timescale (> 10 6  yr), but the relationship between the solid earth and the shorter (
ISSN:2045-2322
2045-2322
DOI:10.1038/s41598-021-84448-7