Journal article
Did Late Cretaceous cooling trigger the Campanian–Maastrichtian Boundary Event?
- Abstract:
-
The Campanian – Maastrichtian (83–66 Ma) was a period of global climate cooling, featuring significant negative carbon-isotope (δ13C) anomalies, such as the Late Campanian Event (LCE) and the Campanian – Maastrichtian Boundary Event (CMBE). A variety of factors, including changes in temperature, oceanic circulation and gateway opening, have been invoked to explain these δ13C perturbations, but no precise mechanism has yet been well constrained. In order to improve our understanding of these e...
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- Publication status:
- Published
- Peer review status:
- Peer reviewed
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Authors
Bibliographic Details
- Publisher:
- Borntraeger Science Publishers Publisher's website
- Journal:
- Newsletters on Stratigraphy Journal website
- Volume:
- 51
- Issue:
- 2
- Pages:
- 145-166
- Publication date:
- 2018-03-01
- Acceptance date:
- 2017-03-17
- DOI:
- EISSN:
-
2363-6122
- ISSN:
-
0078-0421
Item Description
- Keywords:
- Pubs id:
-
pubs:686479
- UUID:
-
uuid:c919cd98-085f-4865-9256-fc44722916ed
- Local pid:
- pubs:686479
- Source identifiers:
-
686479
- Deposit date:
- 2017-03-21
Terms of use
- Copyright holder:
- Linnert et al
- Copyright date:
- 2018
- Notes:
- Copyright © 2017 The authors. This article is Open Access under the terms of the Creative Commons CC BY licence.
- Licence:
- CC Attribution (CC BY)
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