Dynamic model constraints on oxygen-17 depletion in atmospheric O 2 after a snowball Earth

A large perturbation in atmospheric CO2 and O2 or bioproductivity will result in a drastic pulse of 17O change in atmospheric O2, as seen in the Marinoan Oxygen-17 Depletion (MOSD) event in the immediate aftermath of a global deglaciation 635 Mya. The exact nature of the perturbation, however, is de...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Cao, Xiaobin, Bao, Huiming
Format: Text
Language:unknown
Published: LSU Digital Commons 2013
Subjects:
Online Access:https://digitalcommons.lsu.edu/geo_pubs/61
https://doi.org/10.1073/pnas.1302972110
https://digitalcommons.lsu.edu/context/geo_pubs/article/1060/viewcontent/61.pdf
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spelling ftlouisianastuir:oai:digitalcommons.lsu.edu:geo_pubs-1060 2023-06-11T04:17:12+02:00 Dynamic model constraints on oxygen-17 depletion in atmospheric O 2 after a snowball Earth Cao, Xiaobin Bao, Huiming 2013-09-03T07:00:00Z application/pdf https://digitalcommons.lsu.edu/geo_pubs/61 https://doi.org/10.1073/pnas.1302972110 https://digitalcommons.lsu.edu/context/geo_pubs/article/1060/viewcontent/61.pdf unknown LSU Digital Commons https://digitalcommons.lsu.edu/geo_pubs/61 doi:10.1073/pnas.1302972110 https://digitalcommons.lsu.edu/context/geo_pubs/article/1060/viewcontent/61.pdf Faculty Publications Non-mass-dependent Photochemical reaction Postglacial cap carbonate Stratosphere text 2013 ftlouisianastuir https://doi.org/10.1073/pnas.1302972110 2023-05-28T18:24:25Z A large perturbation in atmospheric CO2 and O2 or bioproductivity will result in a drastic pulse of 17O change in atmospheric O2, as seen in the Marinoan Oxygen-17 Depletion (MOSD) event in the immediate aftermath of a global deglaciation 635 Mya. The exact nature of the perturbation, however, is debated. Here we constructed a coupled, four-box, and quick-response biosphere-atmosphere model to examine both the steady state and dynamics of the MOSD event. Our model shows that the ultra-high CO2 concentrations proposed by the "snowball' Earth hypothesis produce a typical MOSD duration of less than 106 y and a magnitude of 17O depletion reaching approximately -35‰. Both numbers are in remarkable agreement with geological constraints from South China and Svalbard. Moderate CO2 and low O2 concentration (e.g., 3,200 parts per million by volume and 0.01 bar, respectively) could produce distinct sulfate 17O depletion only if postglacial marine bioproductivity was impossibly low. Our dynamic model also suggests that a snowball in which the ocean is isolated from the atmosphere by a continuous ice cover may be distinguished from one in which cracks in the ice permit ocean-atmosphere exchange only if partial pressure of atmospheric O2 is larger than 0.02 bar during the snowball period and records of weathering-derived sulfate are available for the very first few tens of thousands of years after the onset of the meltdown. In any case, a snowball Earth is a precondition for the observed MOSD event. Text Svalbard LSU Digital Commons (Louisiana State University) Svalbard Proceedings of the National Academy of Sciences 110 36 14546 14550
institution Open Polar
collection LSU Digital Commons (Louisiana State University)
op_collection_id ftlouisianastuir
language unknown
topic Non-mass-dependent
Photochemical reaction
Postglacial cap carbonate
Stratosphere
spellingShingle Non-mass-dependent
Photochemical reaction
Postglacial cap carbonate
Stratosphere
Cao, Xiaobin
Bao, Huiming
Dynamic model constraints on oxygen-17 depletion in atmospheric O 2 after a snowball Earth
topic_facet Non-mass-dependent
Photochemical reaction
Postglacial cap carbonate
Stratosphere
description A large perturbation in atmospheric CO2 and O2 or bioproductivity will result in a drastic pulse of 17O change in atmospheric O2, as seen in the Marinoan Oxygen-17 Depletion (MOSD) event in the immediate aftermath of a global deglaciation 635 Mya. The exact nature of the perturbation, however, is debated. Here we constructed a coupled, four-box, and quick-response biosphere-atmosphere model to examine both the steady state and dynamics of the MOSD event. Our model shows that the ultra-high CO2 concentrations proposed by the "snowball' Earth hypothesis produce a typical MOSD duration of less than 106 y and a magnitude of 17O depletion reaching approximately -35‰. Both numbers are in remarkable agreement with geological constraints from South China and Svalbard. Moderate CO2 and low O2 concentration (e.g., 3,200 parts per million by volume and 0.01 bar, respectively) could produce distinct sulfate 17O depletion only if postglacial marine bioproductivity was impossibly low. Our dynamic model also suggests that a snowball in which the ocean is isolated from the atmosphere by a continuous ice cover may be distinguished from one in which cracks in the ice permit ocean-atmosphere exchange only if partial pressure of atmospheric O2 is larger than 0.02 bar during the snowball period and records of weathering-derived sulfate are available for the very first few tens of thousands of years after the onset of the meltdown. In any case, a snowball Earth is a precondition for the observed MOSD event.
format Text
author Cao, Xiaobin
Bao, Huiming
author_facet Cao, Xiaobin
Bao, Huiming
author_sort Cao, Xiaobin
title Dynamic model constraints on oxygen-17 depletion in atmospheric O 2 after a snowball Earth
title_short Dynamic model constraints on oxygen-17 depletion in atmospheric O 2 after a snowball Earth
title_full Dynamic model constraints on oxygen-17 depletion in atmospheric O 2 after a snowball Earth
title_fullStr Dynamic model constraints on oxygen-17 depletion in atmospheric O 2 after a snowball Earth
title_full_unstemmed Dynamic model constraints on oxygen-17 depletion in atmospheric O 2 after a snowball Earth
title_sort dynamic model constraints on oxygen-17 depletion in atmospheric o 2 after a snowball earth
publisher LSU Digital Commons
publishDate 2013
url https://digitalcommons.lsu.edu/geo_pubs/61
https://doi.org/10.1073/pnas.1302972110
https://digitalcommons.lsu.edu/context/geo_pubs/article/1060/viewcontent/61.pdf
geographic Svalbard
geographic_facet Svalbard
genre Svalbard
genre_facet Svalbard
op_source Faculty Publications
op_relation https://digitalcommons.lsu.edu/geo_pubs/61
doi:10.1073/pnas.1302972110
https://digitalcommons.lsu.edu/context/geo_pubs/article/1060/viewcontent/61.pdf
op_doi https://doi.org/10.1073/pnas.1302972110
container_title Proceedings of the National Academy of Sciences
container_volume 110
container_issue 36
container_start_page 14546
op_container_end_page 14550
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