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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Bibliografische gegevens
Hoofdauteur: O'Connor, LK
Andere auteurs: Robinson, S
Formaat: Thesis
Taal:English
Gepubliceerd in: 2018
Onderwerpen: