Reevaluating Links Between Meteorite Impacts and Early Cenozoic Global Warming

Abstract The Paleocene‐Eocene Thermal Maximum (PETM) and the lower Chron 29n hyperthermal event were recently proposed to have been triggered by the meteorite impacts that formed the Marquez Dome (Texas, USA; 58.3 ± 3.1 Ma) and Boltysh (Ukraine; 65.39 ± 0.14 Ma) craters, respectively. We use shock p...

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Main Authors: A. Zorzi, S. M. Tikoo, G. C. Beroza, N. H. Sleep
Format: Article
Language:English
Published: Wiley 2022-06-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2022GL099313
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author A. Zorzi
S. M. Tikoo
G. C. Beroza
N. H. Sleep
author_facet A. Zorzi
S. M. Tikoo
G. C. Beroza
N. H. Sleep
author_sort A. Zorzi
collection DOAJ
description Abstract The Paleocene‐Eocene Thermal Maximum (PETM) and the lower Chron 29n hyperthermal event were recently proposed to have been triggered by the meteorite impacts that formed the Marquez Dome (Texas, USA; 58.3 ± 3.1 Ma) and Boltysh (Ukraine; 65.39 ± 0.14 Ma) craters, respectively. We use shock physics hydrocode simulations and radiative forcing calculations to quantify the expected global temperature increase associated with impacts of different scales via the release of CO2 and CH4 sourced from target rocks into the atmosphere. Our results suggest that the <2 km diameter impactors associated with the Marquez Dome and Boltysh craters were too small to have induced hyperthermal‐like (>1 K) temperature changes, even if target rocks were carbon‐rich; >10 km diameter impactors may produce hyperthermal events, but such large impacts are predicted to be uncommon during the Cenozoic era (2–4 objects per Gyr).
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institution Kabale University
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publishDate 2022-06-01
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series Geophysical Research Letters
spelling doaj-art-389ace4336c64720b697f508beaddfe62025-01-22T14:38:16ZengWileyGeophysical Research Letters0094-82761944-80072022-06-014912n/an/a10.1029/2022GL099313Reevaluating Links Between Meteorite Impacts and Early Cenozoic Global WarmingA. Zorzi0S. M. Tikoo1G. C. Beroza2N. H. Sleep3Department of Geological Sciences Stanford University Stanford CA USADepartment of Geological Sciences Stanford University Stanford CA USADepartment of Geophysics Stanford University Stanford CA USADepartment of Geophysics Stanford University Stanford CA USAAbstract The Paleocene‐Eocene Thermal Maximum (PETM) and the lower Chron 29n hyperthermal event were recently proposed to have been triggered by the meteorite impacts that formed the Marquez Dome (Texas, USA; 58.3 ± 3.1 Ma) and Boltysh (Ukraine; 65.39 ± 0.14 Ma) craters, respectively. We use shock physics hydrocode simulations and radiative forcing calculations to quantify the expected global temperature increase associated with impacts of different scales via the release of CO2 and CH4 sourced from target rocks into the atmosphere. Our results suggest that the <2 km diameter impactors associated with the Marquez Dome and Boltysh craters were too small to have induced hyperthermal‐like (>1 K) temperature changes, even if target rocks were carbon‐rich; >10 km diameter impactors may produce hyperthermal events, but such large impacts are predicted to be uncommon during the Cenozoic era (2–4 objects per Gyr).https://doi.org/10.1029/2022GL099313impact phenomenaclimate impactpaleoclimatologyabrupt/rapid climate changeCenozoic
spellingShingle A. Zorzi
S. M. Tikoo
G. C. Beroza
N. H. Sleep
Reevaluating Links Between Meteorite Impacts and Early Cenozoic Global Warming
Geophysical Research Letters
impact phenomena
climate impact
paleoclimatology
abrupt/rapid climate change
Cenozoic
title Reevaluating Links Between Meteorite Impacts and Early Cenozoic Global Warming
title_full Reevaluating Links Between Meteorite Impacts and Early Cenozoic Global Warming
title_fullStr Reevaluating Links Between Meteorite Impacts and Early Cenozoic Global Warming
title_full_unstemmed Reevaluating Links Between Meteorite Impacts and Early Cenozoic Global Warming
title_short Reevaluating Links Between Meteorite Impacts and Early Cenozoic Global Warming
title_sort reevaluating links between meteorite impacts and early cenozoic global warming
topic impact phenomena
climate impact
paleoclimatology
abrupt/rapid climate change
Cenozoic
url https://doi.org/10.1029/2022GL099313
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AT smtikoo reevaluatinglinksbetweenmeteoriteimpactsandearlycenozoicglobalwarming
AT gcberoza reevaluatinglinksbetweenmeteoriteimpactsandearlycenozoicglobalwarming
AT nhsleep reevaluatinglinksbetweenmeteoriteimpactsandearlycenozoicglobalwarming