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Rapid coupling between solid earth and ice volume during the Quaternary
Kuwahara, Y.; Yasukawa, K.; Fujinaga, K.; Nozaki, T.; Ohta, J.; Sato, H.; Kimura, J.-I.; Nakamura, K.; Yokoyama, Y.; Kato, K. (2021). Rapid coupling between solid earth and ice volume during the Quaternary. NPG Scientific Reports 11(1): 5695. https://dx.doi.org/10.1038/s41598-021-84448-7
In: Scientific Reports (Nature Publishing Group). Nature Publishing Group: London. ISSN 2045-2322; e-ISSN 2045-2322
|   |
| Auteurs | | Top |
- Kuwahara, Y.
- Yasukawa, K.
- Fujinaga, K.
- Nozaki, T.
|
- Ohta, J.
- Sato, H.
- Kimura, J.-I.
|
- Nakamura, K.
- Yokoyama, Y.
- Kato, K.
|
| Abstract |
The solid earth plays a major role in controlling Earth’s surface climate. Volcanic degassing of carbon dioxide (CO2) and silicate chemical weathering are known to regulate the evolution of climate on a geologic timescale (> 106 yr), but the relationship between the solid earth and the shorter (< 105 yr) fluctuations of Quaternary glacial–interglacial cycles is still under debate. Here we show that the seawater osmium isotope composition (187Os/188Os), a proxy for the solid earth’s response to climate change, has varied during the past 300,000 years in association with glacial–interglacial cycles. Our marine Os isotope mass-balance simulation reveals that the observed 187Os/188Os fluctuation cannot be explained solely by global chemical weathering rate changes corresponding to glacial–interglacial climate changes, but the fluctuation can be reproduced by taking account of short-term inputs of (1) radiogenic Os derived from intense weathering of glacial till during deglacial periods and (2) unradiogenic Os derived from enhanced seafloor hydrothermalism triggered by sea-level falls associated with increases of ice sheet volume. Our results constitute the first evidence that ice sheet recession and expansion during the Quaternary systematically and repetitively caused short-term (< 105 yr) solid earth responses via chemical weathering of glacial till and seafloor magmatism. This finding implies that climatic changes on < 105 yr timescales can provoke rapid feedbacks from the solid earth, a causal relationship that is the reverse of the longer-term (> 106 yr) causality that has been conventionally considered. |
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