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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>4</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/cpd-4-1021-2008</doi>
	<article_url>http://www.clim-past-discuss.net/4/1021/2008/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/4/1021/2008/cpd-4-1021-2008.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/4/1021/2008/cpd-4-1021-2008.pdf</fulltext_pdf>
	<start_page>1021</start_page>
	<end_page>1045</end_page>
	<publication_date>2008-09-29</publication_date>
	<article_title content_type="html">Exploring the climatic impact of the continental vegetation on the Mezosoic atmospheric CO&lt;sub&gt;2&lt;/sub&gt; and climate history</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Donnadieu</name>
			<email>yannick.donnadieu@lsce.ipsl.fr</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>Y. Goddéris</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>N. Bouttes</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Laboratoire des Sciences du Climat et de l&apos;Environnement (LSCE), unité mixte CNRS-CEA-UVSQ, Gif/Yvette, France</affiliation>
		<affiliation numeration="2" content_type="html">Laboratoire des Mécanismes et Transferts en Géologie (LMTG), Toulouse, France</affiliation>
	</affiliations>
	<abstract content_type="html">In this contribution, we continue our exploration of the factors defining the
Mesozoic climatic history. We improve the Earth system model GEOCLIM designed
for long term climate and geochemical reconstructions by adding the explicit
calculation of the biome dynamics using the LPJ model. The coupled
GEOCLIM-LPJ model thus allows the simultaneous calculation of the climate
with a 2-D spatial resolution, the coeval atmospheric CO&lt;sub&gt;2&lt;/sub&gt;, and the
continental biome distribution. We found that accounting for the climatic
role of the continental vegetation dynamics (albedo change, water cycle and
surface roughness modulations) strongly affects the reconstructed geological
climate. Indeed the calculated partial pressure of atmospheric CO&lt;sub&gt;2&lt;/sub&gt; over
the Mesozoic is twice the value calculated when assuming a uniform constant
vegetation. This increase in CO&lt;sub&gt;2&lt;/sub&gt; is triggered by a global cooling of the
continents, itself triggered by a general increase in continental albedo
owing to the development of desertic surfaces. This cooling reduces the
CO&lt;sub&gt;2&lt;/sub&gt; consumption through silicate weathering, and hence results in a
compensating increase in the atmospheric CO&lt;sub&gt;2&lt;/sub&gt; pressure. This study
demonstrates that the impact of land plants on climate and hence on
atmospheric CO&lt;sub&gt;2&lt;/sub&gt; is as important as their geochemical effect through the
enhancement of chemical weathering of the continental surface. Our
GEOCLIM-LPJ simulations also define a climatic baseline for the Mesozoic,
around which exceptionally cool and warm events can be identified.</abstract>
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</article>

