Journal article
Basalt–seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: Deconstructing OAE 2 (Cenomanian–Turonian, Late Cretaceous)
- Abstract:
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Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major palaeoceanographic phenomenon that took place during an interval of extreme global warmth when large amounts of organic matter entered the marine burial record, probably triggered by increased availability of nutrients for planktonic biota. Three sections (Eastbourne, Sussex, UK; Raia del Pedale, Campania, Italy; and Tarfaya, Morocco) recording this event illustrate the influence on marine geochemistry of mafic volcanic...
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- Publication status:
- Published
- Peer review status:
- Peer reviewed
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(Preview, Version of record, pdf, 2.4MB, Terms of use)
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- Publisher copy:
- 10.1111/sed.12305
Authors
- Publisher:
- Wiley
- Journal:
- Sedimentology More from this journal
- Volume:
- 64
- Issue:
- 1
- Pages:
- 16–43
- Publication date:
- 2016-07-01
- Acceptance date:
- 2016-06-29
- DOI:
- EISSN:
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1365-3091
- ISSN:
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0037-0746
- Keywords:
- Pubs id:
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pubs:631850
- UUID:
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uuid:00ae535f-7a27-4ac1-9918-38e1cc75bc24
- Local pid:
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pubs:631850
- Source identifiers:
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631850
- Deposit date:
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2016-07-05
- ARK identifier:
Terms of use
- Copyright holder:
- Jenkyns et al
- Copyright date:
- 2016
- Notes:
- © 2016 The Authors. Sedimentology © 2016 International Association of Sedimentologists. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License.
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