A multi-proxy reconstruction of Late Cretaceous climate
<p>The Late Cretaceous (100.5–66.0 Ma) was a greenhouse world with high atmospheric CO<sub>2</sub>, which fluctuated on long and short timescales, that can provide insights into how Earth’s climate system operates under different CO<sub>2</sub> levels to today. This the...
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| Formáid: | Tráchtas |
| Teanga: | English |
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2018
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