- Abstract:
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It is well established that greenhouse conditions prevailed during the Cretaceous Period (~ 145–66 Ma). Determining the exact nature of the greenhouse-gas forcing, climatic warming and climate sensitivity remains, however, an active topic of research. Quantitative and qualitative geochemical and palaeontological proxies provide valuable observational constraints on Cretaceous climate. In particular, reconstructions of Cretaceous sea-surface temperatures (SSTs) have been revolutionised firstly...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Publisher's version
- Files:
-
-
(pdf, 3.3mb)
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- Publisher copy:
- 10.1016/j.earscirev.2017.07.012
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- Publisher:
- Elsevier Publisher's website
- Journal:
- Earth-Science Reviews Journal website
- Volume:
- 172
- Pages:
- 224-247
- Publication date:
- 2017-07-27
- Acceptance date:
- 2017-07-24
- DOI:
- ISSN:
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1872-6828
- Pubs id:
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pubs:709669
- URN:
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uri:67069c06-2913-4e61-90cb-13e29ff557e9
- UUID:
-
uuid:67069c06-2913-4e61-90cb-13e29ff557e9
- Local pid:
- pubs:709669
- Copyright holder:
- O'Brien et al.
- Copyright date:
- 2017
- Notes:
- Copyright © 2017 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY license (http://creativecommons.org/licenses/BY/4.0/).
Journal article
Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes
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