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...

Deskribapen osoa

Xehetasun bibliografikoak
Egile nagusia: O'Connor, LK
Beste egile batzuk: Robinson, S
Formatua: Thesis
Hizkuntza:English
Argitaratua: 2018
Gaiak: