Climate variability and storm impacts as major drivers for human coastal marsh withdrawal over the Neolithic period (Southern Brittany, NW France)
Relationships between climate variations, vegetation dynamics, and early human activities during the Neolithic have been reconstructed from high-resolution pollen and foraminiferal records obtained from cores retrieved from coastal wetland located in southern Brittany (Guidel, NW France). Our data s...
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creator | Fernane, A. Penaud, A. Gandouin, E. Goslin, J. Van Vliet-Lanoë, B. Vidal, M. |
description | Relationships between climate variations, vegetation dynamics, and early human activities during the Neolithic have been reconstructed from high-resolution pollen and foraminiferal records obtained from cores retrieved from coastal wetland located in southern Brittany (Guidel, NW France). Our data show that the area around Guidel corresponded to a dense temperate forest locally replaced by riparian forest in the marsh, without any human disturbance during the early Neolithic. During the mid-Neolithic, between 6500 and 5500calyears BP, the first episode of probable human settlement is recorded, as suggested by the increase of anthropogenic plants. This early record of human impact is consistent with archeological studies that find a high concentration of funeral monuments around Guidel during this cultural period. This complex first phase is interrupted by the disappearance of anthropogenic influence coinciding with a cold/humid climate period in the region characterized by recurrent major storms. Then, at the transition between the middle to late Neolithic, at 5500calyears BP, a second phase of human retreat is signaled by both vegetation dynamics and archeological records; this interval also coincides with a climatic deterioration marked by cold/humid conditions recorded in the region (Sorrel et al., 2012). The results of the present study imply that human settlement/departure over the Neolithic was probably influenced by climatic variations. During the Bronze Age, Iron Age, and Middle Ages, a progressive decline of the arboreal forest, synchronous with an increase of anthropogenic plants, confirms the high and persistent human activity around the site. Furthermore, our results at Guidel suggest a different anthropogenic trend recorded between north and south Brittany. The human impact is well recorded during the Neolithic at Guidel, while in northern Brittany human settlement is not recorded before the Bronze Age, consistent with existing archeological data.
•Impact of climate deterioration on human displacement in coastal area.•Coastal evolution in Brittany during the Holocene.•Early record of human impact during the mid-Neolithic is consistent with archeological studies. |
doi_str_mv | 10.1016/j.palaeo.2015.05.029 |
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•Impact of climate deterioration on human displacement in coastal area.•Coastal evolution in Brittany during the Holocene.•Early record of human impact during the mid-Neolithic is consistent with archeological studies.</description><identifier>ISSN: 0031-0182</identifier><identifier>EISSN: 1872-616X</identifier><identifier>DOI: 10.1016/j.palaeo.2015.05.029</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Brittany coastal area ; Climate variability ; Climatology ; Continental interfaces, environment ; Earth Sciences ; Foraminifera ; Holocene ; Human settlement ; Pollen ; Sciences of the Universe</subject><ispartof>Palaeogeography, palaeoclimatology, palaeoecology, 2015-10, Vol.435, p.136-144</ispartof><rights>2015 Elsevier B.V.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a442t-fd2eb914a22fe42b4b30e06c13047e768a074929c8fddc81e0e22ffabff7c6bf3</citedby><cites>FETCH-LOGICAL-a442t-fd2eb914a22fe42b4b30e06c13047e768a074929c8fddc81e0e22ffabff7c6bf3</cites><orcidid>0000-0001-6970-9630 ; 0000-0003-3578-4549</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.palaeo.2015.05.029$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>230,314,778,782,883,3539,27907,27908,45978</link.rule.ids><backlink>$$Uhttps://hal.science/hal-01445162$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Fernane, A.</creatorcontrib><creatorcontrib>Penaud, A.</creatorcontrib><creatorcontrib>Gandouin, E.</creatorcontrib><creatorcontrib>Goslin, J.</creatorcontrib><creatorcontrib>Van Vliet-Lanoë, B.</creatorcontrib><creatorcontrib>Vidal, M.</creatorcontrib><title>Climate variability and storm impacts as major drivers for human coastal marsh withdrawal over the Neolithic period (Southern Brittany, NW France)</title><title>Palaeogeography, palaeoclimatology, palaeoecology</title><description>Relationships between climate variations, vegetation dynamics, and early human activities during the Neolithic have been reconstructed from high-resolution pollen and foraminiferal records obtained from cores retrieved from coastal wetland located in southern Brittany (Guidel, NW France). Our data show that the area around Guidel corresponded to a dense temperate forest locally replaced by riparian forest in the marsh, without any human disturbance during the early Neolithic. During the mid-Neolithic, between 6500 and 5500calyears BP, the first episode of probable human settlement is recorded, as suggested by the increase of anthropogenic plants. This early record of human impact is consistent with archeological studies that find a high concentration of funeral monuments around Guidel during this cultural period. This complex first phase is interrupted by the disappearance of anthropogenic influence coinciding with a cold/humid climate period in the region characterized by recurrent major storms. Then, at the transition between the middle to late Neolithic, at 5500calyears BP, a second phase of human retreat is signaled by both vegetation dynamics and archeological records; this interval also coincides with a climatic deterioration marked by cold/humid conditions recorded in the region (Sorrel et al., 2012). The results of the present study imply that human settlement/departure over the Neolithic was probably influenced by climatic variations. During the Bronze Age, Iron Age, and Middle Ages, a progressive decline of the arboreal forest, synchronous with an increase of anthropogenic plants, confirms the high and persistent human activity around the site. Furthermore, our results at Guidel suggest a different anthropogenic trend recorded between north and south Brittany. The human impact is well recorded during the Neolithic at Guidel, while in northern Brittany human settlement is not recorded before the Bronze Age, consistent with existing archeological data.
•Impact of climate deterioration on human displacement in coastal area.•Coastal evolution in Brittany during the Holocene.•Early record of human impact during the mid-Neolithic is consistent with archeological studies.</description><subject>Brittany coastal area</subject><subject>Climate variability</subject><subject>Climatology</subject><subject>Continental interfaces, environment</subject><subject>Earth Sciences</subject><subject>Foraminifera</subject><subject>Holocene</subject><subject>Human settlement</subject><subject>Pollen</subject><subject>Sciences of the Universe</subject><issn>0031-0182</issn><issn>1872-616X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2015</creationdate><recordtype>article</recordtype><recordid>eNp9kVGL1DAQx4souJ5-Ax_yeAd2naTZtH0RzuXOE5bzQUXfwjSd0CxtsybZPfZr-InNUvFRGJhh5jd_mPkXxVsOaw5cvd-vDzgi-bUAvllDDtE-K1a8qUWpuPr5vFgBVLwE3oiXxasY9wAgVCVWxe_t6CZMxE4YHHZudOnMcO5ZTD5MzE0HNCkyjGzCvQ-sD-5EITKb6-E44cyMx5hwzPMQB_bk0tAHfMoNn0GWBmKP5LPs4Aw7UHC-Z9df_TEPwsw-BpcSzud37PEHuw84G7p5XbywOEZ68zdfFd_v775tH8rdl0-ft7e7EqUUqbS9oK7lEoWwJEUnuwoIlOEVyJpq1SDUshWtaWzfm4YTUCYtdtbWRnW2uipuFt0BR30I-Q3hrD06_XC705cecCk3XIkTz-z1wh6C_3WkmPTkoqFxxJn8MWpewwZU20iVUbmgJvgYA9l_2hz0xS6914td-mKXhhyizWsfljXKJ58cBR2No_yP3gUySffe_V_gD9bholw</recordid><startdate>20151001</startdate><enddate>20151001</enddate><creator>Fernane, A.</creator><creator>Penaud, A.</creator><creator>Gandouin, E.</creator><creator>Goslin, J.</creator><creator>Van Vliet-Lanoë, B.</creator><creator>Vidal, M.</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>C1K</scope><scope>F1W</scope><scope>H95</scope><scope>L.G</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0001-6970-9630</orcidid><orcidid>https://orcid.org/0000-0003-3578-4549</orcidid></search><sort><creationdate>20151001</creationdate><title>Climate variability and storm impacts as major drivers for human coastal marsh withdrawal over the Neolithic period (Southern Brittany, NW France)</title><author>Fernane, A. ; Penaud, A. ; Gandouin, E. ; Goslin, J. ; Van Vliet-Lanoë, B. ; Vidal, M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a442t-fd2eb914a22fe42b4b30e06c13047e768a074929c8fddc81e0e22ffabff7c6bf3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2015</creationdate><topic>Brittany coastal area</topic><topic>Climate variability</topic><topic>Climatology</topic><topic>Continental interfaces, environment</topic><topic>Earth Sciences</topic><topic>Foraminifera</topic><topic>Holocene</topic><topic>Human settlement</topic><topic>Pollen</topic><topic>Sciences of the Universe</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fernane, A.</creatorcontrib><creatorcontrib>Penaud, A.</creatorcontrib><creatorcontrib>Gandouin, E.</creatorcontrib><creatorcontrib>Goslin, J.</creatorcontrib><creatorcontrib>Van Vliet-Lanoë, B.</creatorcontrib><creatorcontrib>Vidal, M.</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Palaeogeography, palaeoclimatology, palaeoecology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fernane, A.</au><au>Penaud, A.</au><au>Gandouin, E.</au><au>Goslin, J.</au><au>Van Vliet-Lanoë, B.</au><au>Vidal, M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Climate variability and storm impacts as major drivers for human coastal marsh withdrawal over the Neolithic period (Southern Brittany, NW France)</atitle><jtitle>Palaeogeography, palaeoclimatology, palaeoecology</jtitle><date>2015-10-01</date><risdate>2015</risdate><volume>435</volume><spage>136</spage><epage>144</epage><pages>136-144</pages><issn>0031-0182</issn><eissn>1872-616X</eissn><abstract>Relationships between climate variations, vegetation dynamics, and early human activities during the Neolithic have been reconstructed from high-resolution pollen and foraminiferal records obtained from cores retrieved from coastal wetland located in southern Brittany (Guidel, NW France). Our data show that the area around Guidel corresponded to a dense temperate forest locally replaced by riparian forest in the marsh, without any human disturbance during the early Neolithic. During the mid-Neolithic, between 6500 and 5500calyears BP, the first episode of probable human settlement is recorded, as suggested by the increase of anthropogenic plants. This early record of human impact is consistent with archeological studies that find a high concentration of funeral monuments around Guidel during this cultural period. This complex first phase is interrupted by the disappearance of anthropogenic influence coinciding with a cold/humid climate period in the region characterized by recurrent major storms. Then, at the transition between the middle to late Neolithic, at 5500calyears BP, a second phase of human retreat is signaled by both vegetation dynamics and archeological records; this interval also coincides with a climatic deterioration marked by cold/humid conditions recorded in the region (Sorrel et al., 2012). The results of the present study imply that human settlement/departure over the Neolithic was probably influenced by climatic variations. During the Bronze Age, Iron Age, and Middle Ages, a progressive decline of the arboreal forest, synchronous with an increase of anthropogenic plants, confirms the high and persistent human activity around the site. Furthermore, our results at Guidel suggest a different anthropogenic trend recorded between north and south Brittany. The human impact is well recorded during the Neolithic at Guidel, while in northern Brittany human settlement is not recorded before the Bronze Age, consistent with existing archeological data.
•Impact of climate deterioration on human displacement in coastal area.•Coastal evolution in Brittany during the Holocene.•Early record of human impact during the mid-Neolithic is consistent with archeological studies.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.palaeo.2015.05.029</doi><tpages>9</tpages><orcidid>https://orcid.org/0000-0001-6970-9630</orcidid><orcidid>https://orcid.org/0000-0003-3578-4549</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Brittany coastal area Climate variability Climatology Continental interfaces, environment Earth Sciences Foraminifera Holocene Human settlement Pollen Sciences of the Universe |
title | Climate variability and storm impacts as major drivers for human coastal marsh withdrawal over the Neolithic period (Southern Brittany, NW France) |
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