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...
| المؤلف الرئيسي: | |
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| مؤلفون آخرون: | |
| التنسيق: | أطروحة |
| اللغة: | English |
| منشور في: |
2018
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| الموضوعات: |