Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8302
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dc.contributor.authorallZanchetta, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.authorallVan Welden, A.; Geological Survey of Norway (NGU), Trondheim, Norwayen
dc.contributor.authorallBaneschi, I.; IGG-CNR sez. Pisa, Pisa, Italyen
dc.contributor.authorallDrysdale, R. N.; Department of Resource Management and Geography, University of Melbourne, Victoria, Australiaen
dc.contributor.authorallSadori, L.; Dipartimento di Biologia Ambientale, Università ‘La Sapienza’, Rome, Italyen
dc.contributor.authorallRoberts, N.; School of Geography, Earth and Environmental Sciences, University of Plymouth, UKen
dc.contributor.authorallGiardini, M.; Dipartimento di Biologia Ambientale, Università ‘La Sapienza’, Rome, Italyen
dc.contributor.authorallBeck, C.; Laboratoire de Géodynamique des Chaînes Alpines, Université de Savoie, Le Bourget du Lac, Franceen
dc.contributor.authorallPascucci, V.; Dipartimento Scienze Botaniche, Ecologiche e Geologiche University of Sassari, Sassari, Italyen
dc.contributor.authorallSulpizio, R.; Dipartimento Scienze della Terra e Geoambientali, University of Bari, Bari, Italyen
dc.date.accessioned2012-10-19T13:10:56Zen
dc.date.available2012-10-19T13:10:56Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/8302en
dc.description.abstractA multi-proxy record is presented for approximately the last 4500 cal a BP from Lake Shkodra, Albania/Montenegro. Lithological analyses, C/N ratio and δ13C of the organic and inorganic carbon component suggest that organic matter and bulk carbonate are predominantly authigenic. The δ18O record of bulk carbonate indicates the presence of two prominent wet periods: one at ca. 4300 cal a BP and one at ca. 2500–2000 cal a BP. The latter phase is also found in southern Spain and Central Italy, and represents a prominent event in the western and central Mediterranean. In the last 2000 years, four relatively wet intervals occurred between ca. 1800 and 1500 cal a BP (150–450 AD), 1350–1250 (600–700 AD), 1100–800 (850–1150 AD), and at ca. 90 cal a BP (1860 AD). Between ca. 4100 and 2500 cal a BP δ18O values are relatively high, with three prominent peaks indicating drier conditions at ca. 4100–4000 cal a BP, ca. 3500 and at ca. 3300 cal a BP. Four additional drier events are identified at 1850 (ca. 100 AD), 1400 (ca. 550 AD), 1150 (800 AD) and ca.750 cal a BP (1200 AD). The pollen record does not show changes in accordance with these episodes owing to the poor sensitivity of vegetation in this area, which is dominated by an orographic rainfall effect and where changes in altitudinal vegetation belts do not affect the pollen rain in the lake catchment. However, since ca. 900 cal a BP a significant decrease in the percentage arboreal pollen and in pollen concentrations suggest major deforestation produced by human activities. Copyright © 2012 John Wiley & Sons, Ltd.en
dc.language.isoEnglishen
dc.publisher.nameWiley-Blackwellen
dc.relation.ispartofJournal of Quaternary Scienceen
dc.relation.ispartofseries8/27 (2012)en
dc.subjectLake Shkodraen
dc.subjectlate Holoceneen
dc.subjectMediterraneanen
dc.subjectpalaeoclimateen
dc.subjectstable isotopesen
dc.titleMultiproxy record for the last 4500 years from Lake Shkodra (Albania/Montenegro)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber780-789en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.identifier.doi10.1002/jqs.2563en
dc.description.obiettivoSpecifico3.7. Dinamica del clima e dell'oceanoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.relation.issn0267-8179en
dc.relation.eissn1099-1417en
dc.contributor.authorZanchetta, G.en
dc.contributor.authorVan Welden, A.en
dc.contributor.authorBaneschi, I.en
dc.contributor.authorDrysdale, R. N.en
dc.contributor.authorSadori, L.en
dc.contributor.authorRoberts, N.en
dc.contributor.authorGiardini, M.en
dc.contributor.authorBeck, C.en
dc.contributor.authorPascucci, V.en
dc.contributor.authorSulpizio, R.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italiaen
dc.contributor.departmentGeological Survey of Norway (NGU), Trondheim, Norwayen
dc.contributor.departmentIGG-CNR sez. Pisa, Pisa, Italyen
dc.contributor.departmentDepartment of Resource Management and Geography, University of Melbourne, Victoria, Australiaen
dc.contributor.departmentDipartimento di Biologia Ambientale, Università ‘La Sapienza’, Rome, Italyen
dc.contributor.departmentSchool of Geography, Earth and Environmental Sciences, University of Plymouth, UKen
dc.contributor.departmentDipartimento di Biologia Ambientale, Università ‘La Sapienza’, Rome, Italyen
dc.contributor.departmentLaboratoire de Géodynamique des Chaînes Alpines, Université de Savoie, Le Bourget du Lac, Franceen
dc.contributor.departmentDipartimento Scienze Botaniche, Ecologiche e Geologiche University of Sassari, Sassari, Italyen
dc.contributor.departmentDipartimento Scienze della Terra e Geoambientali, University of Bari, Bari, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia-
crisitem.author.deptGeological Survey of Norway (NGU), Trondheim, Norway-
crisitem.author.deptUniversity of Plymouth, UK-
crisitem.author.deptDipartimento di Biologia Ambientale, Università ‘La Sapienza’, Rome, Italy-
crisitem.author.deptUniversité de Savoie - France-
crisitem.author.deptCIRISIVU, c/o Dipartimento Geomineralogico, Universita' di Bari-
crisitem.author.orcid0000-0002-7080-9599-
crisitem.author.orcid0000-0001-7867-031X-
crisitem.author.orcid0000-0002-2774-6705-
crisitem.author.orcid0000-0003-4834-3056-
crisitem.author.orcid0000-0002-3930-5421-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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