A Pronounced Spike in Ocean Productivity Triggered by the Chicxulub Impact

There is increasing evidence linking the mass-extinction event at the Cretaceous-Paleogene boundary to an asteroid impact near Chicxulub, Mexico. Here we use model simulations to explore the combined effect of sulfate aerosols, carbon dioxide and dust from the impact on the oceans and the marine bio...

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Main Authors: Brugger, Julia, Feulner, Georg, Hofmann, Matthias, Petri, Stefan
Format: Article in Journal/Newspaper
Language:English
Published: Hoboken, NJ : Wiley 2021
Subjects:
550
Online Access:https://dx.doi.org/10.34657/7078
https://oa.tib.eu/renate/handle/123456789/8037
id ftdatacite:10.34657/7078
record_format openpolar
spelling ftdatacite:10.34657/7078 2023-05-15T17:50:16+02:00 A Pronounced Spike in Ocean Productivity Triggered by the Chicxulub Impact Brugger, Julia Feulner, Georg Hofmann, Matthias Petri, Stefan 2021 https://dx.doi.org/10.34657/7078 https://oa.tib.eu/renate/handle/123456789/8037 en eng Hoboken, NJ : Wiley Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Biospherics Carbon dioxide Geology FOS Earth and related environmental sciences Sulfur compounds Carbon isotopes Chicxulub impact Combined effect Cretaceous-Paleogene boundary Mass extinction events Sulfate aerosols Temperature decrease Terrestrial biosphere Oceanography aerosol algal bloom carbon dioxide carbon isotope empirical analysis mass extinction ocean acidification sulfate Mexico [North America] Asteroidea 550 article CreativeWork 2021 ftdatacite https://doi.org/10.34657/7078 2022-04-01T09:37:59Z There is increasing evidence linking the mass-extinction event at the Cretaceous-Paleogene boundary to an asteroid impact near Chicxulub, Mexico. Here we use model simulations to explore the combined effect of sulfate aerosols, carbon dioxide and dust from the impact on the oceans and the marine biosphere in the immediate aftermath of the impact. We find a strong temperature decrease, a brief algal bloom caused by nutrients from both the deep ocean and the projectile, and moderate surface ocean acidification. Comparing the modeled longer-term post-impact warming and changes in carbon isotopes with empirical evidence points to a substantial release of carbon from the terrestrial biosphere. Overall, our results shed light on the decades to centuries after the Chicxulub impact which are difficult to resolve with proxy data. Article in Journal/Newspaper Ocean acidification DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Biospherics
Carbon dioxide
Geology
FOS Earth and related environmental sciences
Sulfur compounds
Carbon isotopes
Chicxulub impact
Combined effect
Cretaceous-Paleogene boundary
Mass extinction events
Sulfate aerosols
Temperature decrease
Terrestrial biosphere
Oceanography
aerosol
algal bloom
carbon dioxide
carbon isotope
empirical analysis
mass extinction
ocean acidification
sulfate
Mexico [North America]
Asteroidea
550
spellingShingle Biospherics
Carbon dioxide
Geology
FOS Earth and related environmental sciences
Sulfur compounds
Carbon isotopes
Chicxulub impact
Combined effect
Cretaceous-Paleogene boundary
Mass extinction events
Sulfate aerosols
Temperature decrease
Terrestrial biosphere
Oceanography
aerosol
algal bloom
carbon dioxide
carbon isotope
empirical analysis
mass extinction
ocean acidification
sulfate
Mexico [North America]
Asteroidea
550
Brugger, Julia
Feulner, Georg
Hofmann, Matthias
Petri, Stefan
A Pronounced Spike in Ocean Productivity Triggered by the Chicxulub Impact
topic_facet Biospherics
Carbon dioxide
Geology
FOS Earth and related environmental sciences
Sulfur compounds
Carbon isotopes
Chicxulub impact
Combined effect
Cretaceous-Paleogene boundary
Mass extinction events
Sulfate aerosols
Temperature decrease
Terrestrial biosphere
Oceanography
aerosol
algal bloom
carbon dioxide
carbon isotope
empirical analysis
mass extinction
ocean acidification
sulfate
Mexico [North America]
Asteroidea
550
description There is increasing evidence linking the mass-extinction event at the Cretaceous-Paleogene boundary to an asteroid impact near Chicxulub, Mexico. Here we use model simulations to explore the combined effect of sulfate aerosols, carbon dioxide and dust from the impact on the oceans and the marine biosphere in the immediate aftermath of the impact. We find a strong temperature decrease, a brief algal bloom caused by nutrients from both the deep ocean and the projectile, and moderate surface ocean acidification. Comparing the modeled longer-term post-impact warming and changes in carbon isotopes with empirical evidence points to a substantial release of carbon from the terrestrial biosphere. Overall, our results shed light on the decades to centuries after the Chicxulub impact which are difficult to resolve with proxy data.
format Article in Journal/Newspaper
author Brugger, Julia
Feulner, Georg
Hofmann, Matthias
Petri, Stefan
author_facet Brugger, Julia
Feulner, Georg
Hofmann, Matthias
Petri, Stefan
author_sort Brugger, Julia
title A Pronounced Spike in Ocean Productivity Triggered by the Chicxulub Impact
title_short A Pronounced Spike in Ocean Productivity Triggered by the Chicxulub Impact
title_full A Pronounced Spike in Ocean Productivity Triggered by the Chicxulub Impact
title_fullStr A Pronounced Spike in Ocean Productivity Triggered by the Chicxulub Impact
title_full_unstemmed A Pronounced Spike in Ocean Productivity Triggered by the Chicxulub Impact
title_sort pronounced spike in ocean productivity triggered by the chicxulub impact
publisher Hoboken, NJ : Wiley
publishDate 2021
url https://dx.doi.org/10.34657/7078
https://oa.tib.eu/renate/handle/123456789/8037
genre Ocean acidification
genre_facet Ocean acidification
op_rights Creative Commons Attribution 4.0 International
CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.34657/7078
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