Salinity changes and anoxia resulting from enhanced run-off during the late Permian global warming and mass extinction event
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Salinity changes and anoxia resulting from enhanced run-off during the late Permian global warming and mass extinction event ; volume:14 ; number:4 ; year:2018 ; pages:441-453
Climate of the past ; 14, Heft 4 (2018), 441-453
- Creator
- DOI
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10.5194/cp-14-441-2018
- URN
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urn:nbn:de:101:1-2018061316395784189113
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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16.08.2025, 5:29 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- van Soelen, Elsbeth E.
- Twitchett, Richard J.
- Kürschner, Wolfram Michael
Other Objects (12)
Salinity changes and anoxia resulting from enhanced runoff during the late Permian global warming and mass extinction event
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Anoxia and salinity changes: a new Permian catastrophe record
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No mass extinction for land plants at the Permian–Triassic transition
Trajectories of Late Permian – Jurassic radiolarian extinction rates: no evidence for an end-Triassic mass extinction
Unravelling climate conditions preceding the End-Permian Mass Extinction: Insights from latest Permian interannual tropical variability and extreme events
The role of seawater warming for the end-Permian mass extinction event
Evidence for a prolonged Permian–Triassic extinction interval from global marine mercury records
Shifts in magnetic mineral assemblages support ocean deoxygenation before the end-Permian mass extinction
Initial pulse of Siberian Traps sills as the trigger of the end-Permian mass extinction
Age and pattern of the southern high-latitude continental end-Permian extinction constrained by multiproxy analysis
Salinity changes and anoxia resulting from enhanced runoff during the late Permian global warming and mass extinction event
Gradual warming prior to the end‐Permian mass extinction
Anoxia and salinity changes: a new Permian catastrophe record
Whirling in the late Permian: ancestral Gyrinidae show early radiation of beetles before Permian-Triassic mass extinction
No mass extinction for land plants at the Permian–Triassic transition
Trajectories of Late Permian – Jurassic radiolarian extinction rates: no evidence for an end-Triassic mass extinction
Unravelling climate conditions preceding the End-Permian Mass Extinction: Insights from latest Permian interannual tropical variability and extreme events
The role of seawater warming for the end-Permian mass extinction event
Evidence for a prolonged Permian–Triassic extinction interval from global marine mercury records
Shifts in magnetic mineral assemblages support ocean deoxygenation before the end-Permian mass extinction
Initial pulse of Siberian Traps sills as the trigger of the end-Permian mass extinction
Age and pattern of the southern high-latitude continental end-Permian extinction constrained by multiproxy analysis
Salinity changes and anoxia resulting from enhanced runoff during the late Permian global warming and mass extinction event
Gradual warming prior to the end‐Permian mass extinction
Anoxia and salinity changes: a new Permian catastrophe record
Whirling in the late Permian: ancestral Gyrinidae show early radiation of beetles before Permian-Triassic mass extinction
No mass extinction for land plants at the Permian–Triassic transition
Trajectories of Late Permian – Jurassic radiolarian extinction rates: no evidence for an end-Triassic mass extinction
Unravelling climate conditions preceding the End-Permian Mass Extinction: Insights from latest Permian interannual tropical variability and extreme events
The role of seawater warming for the end-Permian mass extinction event
Evidence for a prolonged Permian–Triassic extinction interval from global marine mercury records
Shifts in magnetic mineral assemblages support ocean deoxygenation before the end-Permian mass extinction
Initial pulse of Siberian Traps sills as the trigger of the end-Permian mass extinction