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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:32:28Z</responseDate> <request identifier=oai:HAL:hal-00903607v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00903607v1</identifier> <datestamp>2018-01-15</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:EPHE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:CBAE</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:PSL</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>A comparison of charcoal measurements for reconstruction of Mediterranean paleo-fire frequency in the mountains of Corsica</title> <creator>Leys, Berangere</creator> <creator>Carcaillet, Christopher</creator> <creator>Dezileau, Laurent</creator> <creator>Ali, Adam A.</creator> <creator>Bradshaw, Richard H. W.</creator> <contributor>Centre de Bio-Archéologie et d'Ecologie (CBAE) ; Université Montpellier 2 - Sciences et Techniques (UM2) - École pratique des hautes études (EPHE) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>Risques ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>School of Environmental Sciences, University of Liverpool, ; University of Liverpool</contributor> <source>ISSN: 0033-5894</source> <source>EISSN: 1096-0287</source> <source>Quaternary Research</source> <publisher>Elsevier</publisher> <identifier>hal-00903607</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00903607</identifier> <source>https://hal.archives-ouvertes.fr/hal-00903607</source> <source>Quaternary Research, Elsevier, 2013, 79 (3), pp.337-349. 〈10.1016/j.yqres.2013.01.003〉</source> <identifier>DOI : 10.1016/j.yqres.2013.01.003</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2013.01.003</relation> <language>en</language> <subject lang=en>Methodology</subject> <subject lang=en>Mediterranean ecosystem</subject> <subject lang=en>Holocene</subject> <subject lang=en>Loss on ignition</subject> <subject lang=en>Fire histories</subject> <subject lang=en>Sedimentary charcoal</subject> <subject>[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment</subject> <subject>[SDE.MCG] Environmental Sciences/Global Changes</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>Fire-history reconstructions inferred from sedimentary charcoal records are based on measuring sieved charcoal fragment area, estimating fragment volume, or counting fragments. Similar fire histories are reconstructed from these three approaches for boreal lake sediment cores, using locally defined thresholds. Here, we test the same approach for a montane Mediterranean lake in which taphonomical processes might differ from boreal lakes through fragmentation of charcoal particles. The Mediterranean charcoal series are characterized by highly variable charcoal accumulation rates. Results there indicate that the three proxies do not provide comparable fire histories. The differences are attributable to charcoal fragmentation. This could be linked to fire type (crown or surface fires) or taphonomical processes, including charcoal transportation in the catchment area or in the sediment. The lack of correlation between the concentration of charcoal and of mineral matter suggests that fragmentation is not linked to erosion. Reconstructions based on charcoal area are more robust and stable than those based on fragment counts. Area-based reconstructions should therefore be used instead of the particle-counting method when fragmentation may influence the fragment abundance.</description> <date>2013-05</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>