Flood Basalts and Mass Extinctions

Flood basalts were Earth's largest volcanic episodes that, along with related intrusions, were often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events, hyperthermals, and mass extinction events. Volatile emissions, both from magmatic degassing and vaporized fro...

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Main Authors: Clapham, Matthew E, Renne, Paul R
Format: Book
Language:unknown
Published: eScholarship, University of California 2019
Subjects:
Online Access:https://escholarship.org/uc/item/3q4714cg
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spelling ftcdlib:oai:escholarship.org:ark:/13030/qt3q4714cg 2023-06-11T04:15:37+02:00 Flood Basalts and Mass Extinctions Clapham, Matthew E Renne, Paul R 2019-05-30 application/pdf https://escholarship.org/uc/item/3q4714cg unknown eScholarship, University of California qt3q4714cg https://escholarship.org/uc/item/3q4714cg public Climate Action Life Below Water climate change ocean acidification anoxia extinction selectivity physiology Physical Sciences Earth Sciences Geochemistry & Geophysics monograph 2019 ftcdlib 2023-05-29T17:59:47Z Flood basalts were Earth's largest volcanic episodes that, along with related intrusions, were often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events, hyperthermals, and mass extinction events. Volatile emissions, both from magmatic degassing and vaporized from surrounding rock, triggered short-term cooling and longer-term warming, ocean acidification, and deoxygenation. The magnitude of biological extinction varied considerably, from small events affecting only select groups to the largest extinction of the Phanerozoic, with less-active organisms and those with less-developed respiratory physiology faring especially poorly. The disparate environmental and biological outcomes of different flood basalt events may at first order be explained by variations in the rate of volatile release modulated by longer trends in ocean carbon cycle buffering and the composition of marine ecosystems. Assessing volatile release, environmental change, and biological extinction at finer temporal resolution should be a top priority to refine ancient hyperthermals as analogs for anthropogenic climate change. ▪ Flood basalts, the largest volcanic events in Earth history, triggered dramatic environmental changes on land and in the oceans. ▪ Rapid volcanic carbon emissions led to ocean warming, acidification, and deoxygenation that often caused widespread animal extinctions. ▪ Animal physiology played a key role in survival during flood basalt extinctions, with reef builders such as corals being especially vulnerable. ▪ The rate and duration of volcanic carbon emission controlled the type of environmental disruption and the severity of biological extinction. Book Ocean acidification University of California: eScholarship
institution Open Polar
collection University of California: eScholarship
op_collection_id ftcdlib
language unknown
topic Climate Action
Life Below Water
climate change
ocean acidification
anoxia
extinction selectivity
physiology
Physical Sciences
Earth Sciences
Geochemistry & Geophysics
spellingShingle Climate Action
Life Below Water
climate change
ocean acidification
anoxia
extinction selectivity
physiology
Physical Sciences
Earth Sciences
Geochemistry & Geophysics
Clapham, Matthew E
Renne, Paul R
Flood Basalts and Mass Extinctions
topic_facet Climate Action
Life Below Water
climate change
ocean acidification
anoxia
extinction selectivity
physiology
Physical Sciences
Earth Sciences
Geochemistry & Geophysics
description Flood basalts were Earth's largest volcanic episodes that, along with related intrusions, were often emplaced rapidly and coincided with environmental disruption: oceanic anoxic events, hyperthermals, and mass extinction events. Volatile emissions, both from magmatic degassing and vaporized from surrounding rock, triggered short-term cooling and longer-term warming, ocean acidification, and deoxygenation. The magnitude of biological extinction varied considerably, from small events affecting only select groups to the largest extinction of the Phanerozoic, with less-active organisms and those with less-developed respiratory physiology faring especially poorly. The disparate environmental and biological outcomes of different flood basalt events may at first order be explained by variations in the rate of volatile release modulated by longer trends in ocean carbon cycle buffering and the composition of marine ecosystems. Assessing volatile release, environmental change, and biological extinction at finer temporal resolution should be a top priority to refine ancient hyperthermals as analogs for anthropogenic climate change. ▪ Flood basalts, the largest volcanic events in Earth history, triggered dramatic environmental changes on land and in the oceans. ▪ Rapid volcanic carbon emissions led to ocean warming, acidification, and deoxygenation that often caused widespread animal extinctions. ▪ Animal physiology played a key role in survival during flood basalt extinctions, with reef builders such as corals being especially vulnerable. ▪ The rate and duration of volcanic carbon emission controlled the type of environmental disruption and the severity of biological extinction.
format Book
author Clapham, Matthew E
Renne, Paul R
author_facet Clapham, Matthew E
Renne, Paul R
author_sort Clapham, Matthew E
title Flood Basalts and Mass Extinctions
title_short Flood Basalts and Mass Extinctions
title_full Flood Basalts and Mass Extinctions
title_fullStr Flood Basalts and Mass Extinctions
title_full_unstemmed Flood Basalts and Mass Extinctions
title_sort flood basalts and mass extinctions
publisher eScholarship, University of California
publishDate 2019
url https://escholarship.org/uc/item/3q4714cg
genre Ocean acidification
genre_facet Ocean acidification
op_relation qt3q4714cg
https://escholarship.org/uc/item/3q4714cg
op_rights public
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