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...

Disgrifiad llawn

Manylion Llyfryddiaeth
Prif Awdur: O'Connor, LK
Awduron Eraill: Robinson, S
Fformat: Traethawd Ymchwil
Iaith:English
Cyhoeddwyd: 2018
Pynciau: