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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>2018-01-17T12:06:02Z</responseDate> <request identifier=oai:HAL:hal-01571958v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-01571958v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:UMR5140</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Fluvial response to the last Holocene rapid climate change in the Northwestern Mediterranean coastlands</title> <creator>Degeai, Jean-Philippe</creator> <creator>Devillers, Benoit</creator> <creator>Blanchemanche, Philippe</creator> <creator>DEZILEAU, Laurent</creator> <creator>Oueslati, Hamza</creator> <creator>Tillier, Margaux</creator> <creator>Bohbot, Herve</creator> <contributor>Archéologie des Sociétés Méditerranéennes (ASM) ; Université Paul-Valéry - Montpellier 3 (UM3) - Ministère de la Culture et de la Communication (MCC) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>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)</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> <source>ISSN: 0921-8181</source> <source>Global and Planetary Change</source> <publisher>Elsevier</publisher> <identifier>hal-01571958</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-01571958</identifier> <source>https://hal.archives-ouvertes.fr/hal-01571958</source> <source>Global and Planetary Change, Elsevier, 2017, 152, pp.176-186. 〈10.1016/j.gloplacha.2017.03.008〉</source> <identifier>DOI : 10.1016/j.gloplacha.2017.03.008</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gloplacha.2017.03.008</relation> <language>en</language> <subject lang=en>Fluvial dynamics</subject> <subject lang=en>Historical flooding</subject> <subject lang=en>Lagoonal sequence</subject> <subject lang=en>North Atlantic cooling</subject> <subject lang=en>Late Holocene</subject> <subject lang=en>Northwestern Mediterranean</subject> <subject>[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>The variability of fluvial activity in the Northwestern Mediterranean coastal lowlands and its relationship with modes of climate change were analysed from the late 9th to the 18th centuries CE. Geochemical analyses were undertaken from a lagoonal sequence and surrounding sediments in order to track the fluvial inputs into the lagoon. An index based on the K/S and Rb/S ratios was used to evidence the main periods of fluvial activity. This index reveals that the Medieval Climate Anomaly (MCA) was a drier period characterized by a lower fluvial activity, while the Little Ice Age (LIA) was a wetter period with an increase of the river dynamics. Three periods of higher than average fluvial activity were evidenced at the end of the first millennium CE (ca. 900–950 cal yr CE), in the first half of the second millennium CE (ca. 1150–1550 cal yr CE), and during the 1600s–1700s CE (ca. 1650–1800 cal yr CE). The comparison of these fluvial periods with other records of riverine or lacustrine floods in Spain, Italy, and South of France seems to indicate a general increase in fluvial and flood patterns in the Northwestern Mediterranean in response to the climate change from the MCA to the LIA, although some episodes of flooding are not found in all records. Besides, the phases of higher than average fluvial dynamics are in good agreement with the North Atlantic cold events evidenced from records of ice-rafted debris. The evolution of fluvial activity in the Northwestern Mediterranean coastlands during the last millennium could have been driven by atmospheric and oceanic circulation patterns.Keywords</description> <date>2017-05</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>