Journal article
Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes
- 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...
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- Publication status:
- Published
- Peer review status:
- Peer reviewed
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(Version of record, pdf, 3.3MB)
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- Publisher copy:
- 10.1016/j.earscirev.2017.07.012
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Authors
Funding
Bibliographic Details
- 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
- Source identifiers:
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709669
Item Description
- Keywords:
- Pubs id:
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pubs:709669
- UUID:
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uuid:67069c06-2913-4e61-90cb-13e29ff557e9
- Local pid:
- pubs:709669
- Deposit date:
- 2017-07-28
Terms of use
- 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/).
- Licence:
- CC Attribution (CC BY)
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