Persistent oceanic anoxia and elevated extinction rates separate the Cambrian and Ordovician radiations
about
Marine anoxia and delayed Earth system recovery after the end-Permian extinction.Decoupling biogeochemical records, extinction, and environmental change during the Cambrian SPICE event.Innovation not recovery: dynamic redox promotes metazoan radiations.Oxygenation as a driver of the Great Ordovician Biodiversification EventHow is biodiversity produced? Examining speciation processes during the GOBE
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Persistent oceanic anoxia and elevated extinction rates separate the Cambrian and Ordovician radiations
description
im Juli 2015 veröffentlichter wissenschaftlicher Artikel
@de
wetenschappelijk artikel
@nl
наукова стаття, опублікована в липні 2015
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name
Persistent oceanic anoxia and ...... rian and Ordovician radiations
@en
Persistent oceanic anoxia and ...... rian and Ordovician radiations
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type
label
Persistent oceanic anoxia and ...... rian and Ordovician radiations
@en
Persistent oceanic anoxia and ...... rian and Ordovician radiations
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prefLabel
Persistent oceanic anoxia and ...... rian and Ordovician radiations
@en
Persistent oceanic anoxia and ...... rian and Ordovician radiations
@nl
P2093
P356
P1433
P1476
Persistent oceanic anoxia and ...... rian and Ordovician radiations
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P2093
Cole T. Edwards
Jonathan M. Adrain
Matthew R. Saltzman
Stephen R. Westrop
P304
P356
10.1130/G36814.1
P407
P577
2015-07-28T00:00:00Z
P819
2015Geo....43..807S