Modelling atmospheric CO2 changes at geological time scales

By trapping infrared radiation, atmospheric CO2 contributes significantly to the greenhouse warming of the planetary surface. Hence, it is thought to have played a key role in the evolution of the Earth's climate over geological time. The history of atmospheric CO2 is available only for the las...

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Main Authors: François Louis, Grard Aline, Goddéris Yves
Format: Article
Language:English
Published: Association Carnets de Geologie 2005-12-01
Series:Carnets de Géologie
Subjects:
Online Access:http://paleopolis.rediris.es/cg/CG2005_M02/CG2005_M02_Abstract02.html
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author François Louis
Grard Aline
Goddéris Yves
author_facet François Louis
Grard Aline
Goddéris Yves
author_sort François Louis
collection DOAJ
description By trapping infrared radiation, atmospheric CO2 contributes significantly to the greenhouse warming of the planetary surface. Hence, it is thought to have played a key role in the evolution of the Earth's climate over geological time. The history of atmospheric CO2 is available only for the last few hundred thousand years from the analysis of the air trapped in cores of ice. Therefore, data regarding Pre-Pleistocene atmospheric CO2 must be derived from proxies. These provide indirect estimates of atmospheric CO2 and are much less reliable than ice-core data. The main proxies used to reconstruct atmospheric CO2 are: the 13C isotopic fractionation of marine organisms, the paleo-pH recorded in the boron isotopic composition of ancient carbonates, the stomatal density of fossil leaves and the 13C isotopic composition of paleosols.
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spelling doaj.art-7e7ea319793c4556a02acb606e9a468a2023-09-02T10:15:08ZengAssociation Carnets de GeologieCarnets de Géologie1765-25531634-07442005-12-01CG2005M02_Abstract02Modelling atmospheric CO2 changes at geological time scalesFrançois LouisGrard AlineGoddéris YvesBy trapping infrared radiation, atmospheric CO2 contributes significantly to the greenhouse warming of the planetary surface. Hence, it is thought to have played a key role in the evolution of the Earth's climate over geological time. The history of atmospheric CO2 is available only for the last few hundred thousand years from the analysis of the air trapped in cores of ice. Therefore, data regarding Pre-Pleistocene atmospheric CO2 must be derived from proxies. These provide indirect estimates of atmospheric CO2 and are much less reliable than ice-core data. The main proxies used to reconstruct atmospheric CO2 are: the 13C isotopic fractionation of marine organisms, the paleo-pH recorded in the boron isotopic composition of ancient carbonates, the stomatal density of fossil leaves and the 13C isotopic composition of paleosols.http://paleopolis.rediris.es/cg/CG2005_M02/CG2005_M02_Abstract02.htmlatmosphereCO2modellingcarbon cycleclimategeochemical cycle
spellingShingle François Louis
Grard Aline
Goddéris Yves
Modelling atmospheric CO2 changes at geological time scales
Carnets de Géologie
atmosphere
CO2
modelling
carbon cycle
climate
geochemical cycle
title Modelling atmospheric CO2 changes at geological time scales
title_full Modelling atmospheric CO2 changes at geological time scales
title_fullStr Modelling atmospheric CO2 changes at geological time scales
title_full_unstemmed Modelling atmospheric CO2 changes at geological time scales
title_short Modelling atmospheric CO2 changes at geological time scales
title_sort modelling atmospheric co2 changes at geological time scales
topic atmosphere
CO2
modelling
carbon cycle
climate
geochemical cycle
url http://paleopolis.rediris.es/cg/CG2005_M02/CG2005_M02_Abstract02.html
work_keys_str_mv AT francoislouis modellingatmosphericco2changesatgeologicaltimescales
AT grardaline modellingatmosphericco2changesatgeologicaltimescales
AT godd233risyves modellingatmosphericco2changesatgeologicaltimescales