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CUATRO CIENEGAS
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Molecular and isotopic evidence reveals the end-Triassic carbon isotope excursion is not from massive exogenous light carbon
by
Fox, Calum P.
,
Cui, X.
,
Whiteside, J.H.
,
Olsen, P.E.
,
Summons, R.E.
,
Grice, Kliti
Published in
Proceedings of the National Academy of Sciences
(2020)
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Cui, X.
1
Fox, Calum P.
1
Grice, Kliti
1
Olsen, P.E.
1
Summons, R.E.
1
Whiteside, J.H.
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Topic
2-METHYLHOPANOID PRODUCTION
1
ATLANTIC MAGMATIC PROVINCE
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CUATRO CIENEGAS
FACIES DEVELOPMENT
FRESH-WATER MICROBIALITES
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JURASSIC BOUNDARY HORIZONS
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LOWER RHINE BASIN
Multidisciplinary Sciences
PALEOENVIRONMENTAL CONDITIONS
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PHOTIC ZONE EUXINIA
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SEA-LEVEL CHANGE
Science & Technology
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Science & Technology - Other Topics
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biomarkers
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carbon isotopes
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end-Triassic mass extinction
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large igneous provinces
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Curtin University: espace
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English
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Open Polar Keyword
Ocean acidification
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