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Enhanced rainfall in the Western Mediterranean during deposition of sapropel S1: stalagmite evidence from Corchia cave (Central Italy)

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dc.contributor.authorZanchetta, G
dc.contributor.authorDrysdale, Russell N
dc.contributor.authorHellstrom, John Charles
dc.contributor.authorFallick, A.E.
dc.contributor.authorIsola, I.
dc.contributor.authorGagan, Michael
dc.contributor.authorPareschi, M.T.
dc.date.accessioned2015-12-08T22:41:41Z
dc.date.issued2007
dc.date.updated2015-12-08T10:29:48Z
dc.description.abstractA stable isotope record from a stalagmite collected from Antro del Corchia cave (Apuan Alps, Central Italy), supported by 17 uranium-series ages, indicates enhanced regional rainfall between ca 8.9 and 7.3 kyr cal. BP at the time of sapropel S1 deposition. Within this phase, the highest rainfall occurred between 7.9 and 7.4 kyr cal. BP. Comparison with different marine and lake records, and in particular with the Soreq Cave record (Israel), suggests substantial in-phase occurrence of enhanced rainfall between the Western and Eastern Mediterranean basins. There is no convincing evidence for major climatic change at the time of the "8.2 kyr event".
dc.identifier.issn0277-3791
dc.identifier.urihttp://hdl.handle.net/1885/36752
dc.publisherPergamon-Elsevier Ltd
dc.sourceQuaternary Science Reviews
dc.subjectKeywords: Catchments; Caves; Lakes; Rain; Climate change; Isotopes; Uranium; Corchia cave; Lake records; Uranium-series ages; Climate change; Rain; climate change; comparative study; marine record; rainfall; sapropel; stable isotope; stalagmite; uranium series dati
dc.titleEnhanced rainfall in the Western Mediterranean during deposition of sapropel S1: stalagmite evidence from Corchia cave (Central Italy)
dc.typeJournal article
local.bibliographicCitation.lastpage286
local.bibliographicCitation.startpage279
local.contributor.affiliationZanchetta, G, University of Pisa
local.contributor.affiliationDrysdale, Russell N, University of Newcastle
local.contributor.affiliationHellstrom, John Charles, University of Melbourne
local.contributor.affiliationFallick, A.E., Scottish Universities Environmental Research Center
local.contributor.affiliationIsola, I., Instituto Nazionale di Geofisica e Vulcanologia
local.contributor.affiliationGagan, Michael, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationPareschi, M.T., Instituto Nazionale di Geofisica e Vulcanologia
local.contributor.authoruidGagan, Michael, u9203225
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040203 - Isotope Geochemistry
local.identifier.absfor040605 - Palaeoclimatology
local.identifier.ariespublicationu4353633xPUB140
local.identifier.citationvolume26
local.identifier.doi10.1016/j.quascirev.2006.12.003
local.identifier.scopusID2-s2.0-33847224812
local.type.statusPublished Version

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