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Thesis

A multi-proxy reconstruction of Late Cretaceous climate

Abstract:

The Late Cretaceous (100.5–66.0 Ma) was a greenhouse world with high atmospheric CO2, which fluctuated on long and short timescales, that can provide insights into how Earth’s climate system operates under different CO2 levels to today. This thesis applies a multi-proxy approach to reconstructing palaeoclimate through the collapse of the Late Cretaceous greenhouse, at tectonic to sub-orbital timescales, with the goal of disentangling CO2 from other climatic...

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Division:
MPLS
Department:
Earth Sciences
Role:
Author

Contributors

Role:
Supervisor
Role:
Supervisor
ORCID:
0000-0002-2728-0984
Type of award:
DPhil
Level of award:
Doctoral
Awarding institution:
University of Oxford
Language:
English
Subjects:
Deposit date:
2022-09-18

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