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Late Quaternary sea-level changes along the Tyrrhenian coast near Orbetello (Tuscany, central Italy): palaeoenvironmental reconstruction using ostracods
A multidisciplinary study has been carried out on a 51 m long core, drilled on coastal lowlands near the Albegna River (Tuscany, Central Italy). Both sedimentological and faunal analyses (ostracods and molluscs) indicate a coastal lagoon environment repeatedly influenced both by the rising Holocene...
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Published in: | Marine micropaleontology 1999-09, Vol.37 (3), p.289-311 |
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creator | Mazzini, I. Anadon, P. Barbieri, M. Castorina, F. Ferreli, L. Gliozzi, E. Mola, M. Vittori, E. |
description | A multidisciplinary study has been carried out on a 51 m long core, drilled on coastal lowlands near the Albegna River (Tuscany, Central Italy). Both sedimentological and faunal analyses (ostracods and molluscs) indicate a coastal lagoon environment repeatedly influenced both by the rising Holocene sea and the Albegna River alluvial inflow. δ
13C, δ
18O, Mg/Ca, Sr/Ca and
87Sr/
86Sr analyses were performed on
Cyprideis torosa shells in order to detail the influence of Albegna River freshwater on the coastal lagoon water. The analytical data illustrate the difficulties of using geochemical proxies in marginal marine settings. Four radiocarbon dates provide a chronostratigraphy for the early Holocene part of the core. The data are used to reconstruct Late Pleistocene to early Holocene palaeoenvironments along this part of the coast and show the development of freshwater environments followed by a coastal brackish lagoon formed in response to the initial Holocene rapid rise in relative sea level. An attempt is made to relate sediments and age data from the core to the relative sea-level curve for the Tyrrhenian Sea. |
doi_str_mv | 10.1016/S0377-8398(99)00023-7 |
format | article |
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13C, δ
18O, Mg/Ca, Sr/Ca and
87Sr/
86Sr analyses were performed on
Cyprideis torosa shells in order to detail the influence of Albegna River freshwater on the coastal lagoon water. The analytical data illustrate the difficulties of using geochemical proxies in marginal marine settings. Four radiocarbon dates provide a chronostratigraphy for the early Holocene part of the core. The data are used to reconstruct Late Pleistocene to early Holocene palaeoenvironments along this part of the coast and show the development of freshwater environments followed by a coastal brackish lagoon formed in response to the initial Holocene rapid rise in relative sea level. An attempt is made to relate sediments and age data from the core to the relative sea-level curve for the Tyrrhenian Sea.</description><identifier>ISSN: 0377-8398</identifier><identifier>EISSN: 1872-6186</identifier><identifier>DOI: 10.1016/S0377-8398(99)00023-7</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>brackish lagoon ; central Italy ; Cyprideis torosa ; Holocene ; Marine ; Mollusca ; Ostracoda ; ostracods ; rising sea level</subject><ispartof>Marine micropaleontology, 1999-09, Vol.37 (3), p.289-311</ispartof><rights>1999 Elsevier Science B.V.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a458t-9d2f53843e65aa0a3293b11bb23092b236c0aebbb1da76195d0ae988c9543ee03</citedby><cites>FETCH-LOGICAL-a458t-9d2f53843e65aa0a3293b11bb23092b236c0aebbb1da76195d0ae988c9543ee03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,786,790,27957,27958</link.rule.ids></links><search><creatorcontrib>Mazzini, I.</creatorcontrib><creatorcontrib>Anadon, P.</creatorcontrib><creatorcontrib>Barbieri, M.</creatorcontrib><creatorcontrib>Castorina, F.</creatorcontrib><creatorcontrib>Ferreli, L.</creatorcontrib><creatorcontrib>Gliozzi, E.</creatorcontrib><creatorcontrib>Mola, M.</creatorcontrib><creatorcontrib>Vittori, E.</creatorcontrib><title>Late Quaternary sea-level changes along the Tyrrhenian coast near Orbetello (Tuscany, central Italy): palaeoenvironmental reconstruction using ostracods</title><title>Marine micropaleontology</title><description>A multidisciplinary study has been carried out on a 51 m long core, drilled on coastal lowlands near the Albegna River (Tuscany, Central Italy). Both sedimentological and faunal analyses (ostracods and molluscs) indicate a coastal lagoon environment repeatedly influenced both by the rising Holocene sea and the Albegna River alluvial inflow. δ
13C, δ
18O, Mg/Ca, Sr/Ca and
87Sr/
86Sr analyses were performed on
Cyprideis torosa shells in order to detail the influence of Albegna River freshwater on the coastal lagoon water. The analytical data illustrate the difficulties of using geochemical proxies in marginal marine settings. Four radiocarbon dates provide a chronostratigraphy for the early Holocene part of the core. The data are used to reconstruct Late Pleistocene to early Holocene palaeoenvironments along this part of the coast and show the development of freshwater environments followed by a coastal brackish lagoon formed in response to the initial Holocene rapid rise in relative sea level. An attempt is made to relate sediments and age data from the core to the relative sea-level curve for the Tyrrhenian Sea.</description><subject>brackish lagoon</subject><subject>central Italy</subject><subject>Cyprideis torosa</subject><subject>Holocene</subject><subject>Marine</subject><subject>Mollusca</subject><subject>Ostracoda</subject><subject>ostracods</subject><subject>rising sea level</subject><issn>0377-8398</issn><issn>1872-6186</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1999</creationdate><recordtype>article</recordtype><recordid>eNqFkd9qVDEQxoMouLY-gpAracFj86cnJ_FGpNhaWCil63WYkzPbjWSTNclZ2DfxcU274m1vZpjM75sw8xHygbPPnHF18cDkMHRaGn1mzDljTMhueEUWXA-iU1yr12TxH3lL3pXyq0FcSbUgf5ZQkd7PLeYI-UALQhdwj4G6DcRHLBRCio-0bpCuDjlvMHqI1CUolUaETO_yiBVDSPRsNRcH8fCJOow1Q6C3FcLh_AvdQQBMGPc-p7htzdbL6FIsNc-u-hTpXHz7JrUHcGkqp-TNGkLB9__yCfl5_X119aNb3t3cXn1bdnDZ69qZSax7qS8lqh6AgRRGjpyPo5DMiBaVY4DjOPIJBsVNP7XSaO1M3zTI5An5eJy7y-n3jKXarS-urQMR01ysMMpoNogXQT5IwZnUDeyPoMuplIxru8t-225rObNPhtlnw-yTG9YY-2yYHZru61GHbd29x2yL8xgdTr6dqtop-Rcm_AWgoaEI</recordid><startdate>19990901</startdate><enddate>19990901</enddate><creator>Mazzini, I.</creator><creator>Anadon, P.</creator><creator>Barbieri, M.</creator><creator>Castorina, F.</creator><creator>Ferreli, L.</creator><creator>Gliozzi, E.</creator><creator>Mola, M.</creator><creator>Vittori, E.</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>H96</scope><scope>L.G</scope><scope>8BQ</scope><scope>8FD</scope><scope>JG9</scope></search><sort><creationdate>19990901</creationdate><title>Late Quaternary sea-level changes along the Tyrrhenian coast near Orbetello (Tuscany, central Italy): palaeoenvironmental reconstruction using ostracods</title><author>Mazzini, I. ; Anadon, P. ; Barbieri, M. ; Castorina, F. ; Ferreli, L. ; Gliozzi, E. ; Mola, M. ; Vittori, E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a458t-9d2f53843e65aa0a3293b11bb23092b236c0aebbb1da76195d0ae988c9543ee03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1999</creationdate><topic>brackish lagoon</topic><topic>central Italy</topic><topic>Cyprideis torosa</topic><topic>Holocene</topic><topic>Marine</topic><topic>Mollusca</topic><topic>Ostracoda</topic><topic>ostracods</topic><topic>rising sea level</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mazzini, I.</creatorcontrib><creatorcontrib>Anadon, P.</creatorcontrib><creatorcontrib>Barbieri, M.</creatorcontrib><creatorcontrib>Castorina, F.</creatorcontrib><creatorcontrib>Ferreli, L.</creatorcontrib><creatorcontrib>Gliozzi, E.</creatorcontrib><creatorcontrib>Mola, M.</creatorcontrib><creatorcontrib>Vittori, E.</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</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) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>Materials Research Database</collection><jtitle>Marine micropaleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mazzini, I.</au><au>Anadon, P.</au><au>Barbieri, M.</au><au>Castorina, F.</au><au>Ferreli, L.</au><au>Gliozzi, E.</au><au>Mola, M.</au><au>Vittori, E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Quaternary sea-level changes along the Tyrrhenian coast near Orbetello (Tuscany, central Italy): palaeoenvironmental reconstruction using ostracods</atitle><jtitle>Marine micropaleontology</jtitle><date>1999-09-01</date><risdate>1999</risdate><volume>37</volume><issue>3</issue><spage>289</spage><epage>311</epage><pages>289-311</pages><issn>0377-8398</issn><eissn>1872-6186</eissn><notes>ObjectType-Article-1</notes><notes>SourceType-Scholarly Journals-1</notes><notes>ObjectType-Feature-2</notes><notes>content type line 23</notes><notes>ObjectType-Article-2</notes><notes>ObjectType-Feature-1</notes><abstract>A multidisciplinary study has been carried out on a 51 m long core, drilled on coastal lowlands near the Albegna River (Tuscany, Central Italy). Both sedimentological and faunal analyses (ostracods and molluscs) indicate a coastal lagoon environment repeatedly influenced both by the rising Holocene sea and the Albegna River alluvial inflow. δ
13C, δ
18O, Mg/Ca, Sr/Ca and
87Sr/
86Sr analyses were performed on
Cyprideis torosa shells in order to detail the influence of Albegna River freshwater on the coastal lagoon water. The analytical data illustrate the difficulties of using geochemical proxies in marginal marine settings. Four radiocarbon dates provide a chronostratigraphy for the early Holocene part of the core. The data are used to reconstruct Late Pleistocene to early Holocene palaeoenvironments along this part of the coast and show the development of freshwater environments followed by a coastal brackish lagoon formed in response to the initial Holocene rapid rise in relative sea level. An attempt is made to relate sediments and age data from the core to the relative sea-level curve for the Tyrrhenian Sea.</abstract><pub>Elsevier B.V</pub><doi>10.1016/S0377-8398(99)00023-7</doi><tpages>23</tpages></addata></record> |
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subjects | brackish lagoon central Italy Cyprideis torosa Holocene Marine Mollusca Ostracoda ostracods rising sea level |
title | Late Quaternary sea-level changes along the Tyrrhenian coast near Orbetello (Tuscany, central Italy): palaeoenvironmental reconstruction using ostracods |
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