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Corrigendum to "Basin-scale controls on the molybdenum-isotope composition of seawater during Oceanic Anoxic Event 2 (Late Cretaceous)" [Geochim. Cosmochim. Acta 178 (2016) 291-306]

Abstract:
A recent molybdenum-isotope estimate of the extent of anoxic and euxinic conditions in the world ocean during Oceanic Anoxic Event 2 (~94 Ma) concluded by discussing a contrast between the new results with existing estimates of marine euxinia based on sulphur isotopes. This suggested contrast was erroneous; when areal extents of marine anoxia and euxinia are calculated for both isotopic proxies, the agreement is actually striking, and highlights the fact that large areas of the global ocean probably remained well ventilated during this event.
Publication status:
In press
Peer review status:
Peer reviewed

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Publisher copy:
10.1016/j.gca.2015.12.036

Authors

More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author


Publisher:
Elsevier
Journal:
Geochimica et Cosmochimica Acta More from this journal
Publication date:
2016-06-01
Acceptance date:
2016-06-18
DOI:
ISSN:
1872-9533


Pubs id:
pubs:631848
UUID:
uuid:e3c00036-5f11-490c-9e15-9fe3edf8386d
Local pid:
pubs:631848
Source identifiers:
631848
Deposit date:
2016-07-05
ARK identifier:

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