Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
about
Mercury anomalies and the timing of biotic recovery following the end-Triassic mass extinctionMercury enrichment indicates volcanic triggering of Valanginian environmental change.Evolution caused by extreme events.Mercury evidence for pulsed volcanism during the end-Triassic mass extinction.End-Cretaceous akaganéite as a mineral marker of Deccan volcanism in the sedimentary record.Mercury, volcanism, and mass extinctions.Recognition of a likely two phased extinction at the K-Pg boundary in Antarctica.
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Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
description
im Januar 2016 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в січні 2016
@uk
name
Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
@en
Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
@nl
type
label
Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
@en
Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
@nl
prefLabel
Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
@en
Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
@nl
P2093
P356
P1433
P1476
Mercury anomaly, Deccan volcanism, and the end-Cretaceous mass extinction
@en
P2093
Alcides Nobrega Sial
Gerta Keller
Jahnavi Punekar
Luiz Drude de Lacerda
Thierry Adatte
P304
P356
10.1130/G37451.1
P407
P50
P577
2016-01-07T00:00:00Z
P819
2016Geo....44..171F