Reconstructing paleoclimate in central Italy since Late Pleistocene: the Lake Trasimeno ostracod record

An 8.59 m long sedimentary core was retrieved from Lake Trasimeno (central Italy) in order to reconstruct the climate history of central Italy throughout the last ca. 47,000 cal yr BP using ostracod assemblages as the main proxy. Lake Trasimeno's ostracod fauna pointed out several lake level ch...

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Bibliographic Details
Main Author: Marchegiano, Marta
Other Authors: Ariztegui, Daniel
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Université de Genève 2017
Subjects:
Online Access:https://archive-ouverte.unige.ch/unige:105656
https://doi.org/10.13097/archive-ouverte/unige:105656
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spelling ftunivgeneve:oai:unige.ch:unige:105656 2023-05-15T16:29:04+02:00 Reconstructing paleoclimate in central Italy since Late Pleistocene: the Lake Trasimeno ostracod record Marchegiano, Marta Ariztegui, Daniel 2017 https://archive-ouverte.unige.ch/unige:105656 https://doi.org/10.13097/archive-ouverte/unige:105656 eng eng Université de Genève info:eu-repo/semantics/altIdentifier/urn/urn:nbn:ch:unige-1056568 unige:105656 https://archive-ouverte.unige.ch/unige:105656 doi:10.13097/archive-ouverte/unige:105656 Free access / No access until 2021-06-17 info:eu-repo/semantics/embargoedAccess info:eu-repo/classification/ddc/550 Paleoclimate Paleoenvironment Ostracods Mediterranean area Lake Trasimeno Limnogeology Micropaleontology Text info:eu-repo/semantics/doctoralThesis Thesis Thèse 2017 ftunivgeneve https://doi.org/10.13097/archive-ouverte/unige:105656 2022-02-08T22:28:53Z An 8.59 m long sedimentary core was retrieved from Lake Trasimeno (central Italy) in order to reconstruct the climate history of central Italy throughout the last ca. 47,000 cal yr BP using ostracod assemblages as the main proxy. Lake Trasimeno's ostracod fauna pointed out several lake level changes. A comparison with other proxies in the same core and the correlation with the oxygen isotope curve from Greenland allowed to interpret them as climatically driven changes (humid and arid periods). The analyses of Trasimeno core allowed us to improve the existing knowledge about the evolution of climatically-forced environmental conditions for the last 47,000 cal yr BP. The comparison with other climatic records indicates that the lake is sensitive to global climatic patterns. Furthermore, these results are challenging existing views about latitudinal moisture distribution in the Italian peninsula and, thus, contribute to constrain the outcome of climate models for the Mediterranean area. Doctoral or Postdoctoral Thesis Greenland Université de Genève: Archive ouverte UNIGE Greenland
institution Open Polar
collection Université de Genève: Archive ouverte UNIGE
op_collection_id ftunivgeneve
language English
topic info:eu-repo/classification/ddc/550
Paleoclimate
Paleoenvironment
Ostracods
Mediterranean area
Lake Trasimeno
Limnogeology
Micropaleontology
spellingShingle info:eu-repo/classification/ddc/550
Paleoclimate
Paleoenvironment
Ostracods
Mediterranean area
Lake Trasimeno
Limnogeology
Micropaleontology
Marchegiano, Marta
Reconstructing paleoclimate in central Italy since Late Pleistocene: the Lake Trasimeno ostracod record
topic_facet info:eu-repo/classification/ddc/550
Paleoclimate
Paleoenvironment
Ostracods
Mediterranean area
Lake Trasimeno
Limnogeology
Micropaleontology
description An 8.59 m long sedimentary core was retrieved from Lake Trasimeno (central Italy) in order to reconstruct the climate history of central Italy throughout the last ca. 47,000 cal yr BP using ostracod assemblages as the main proxy. Lake Trasimeno's ostracod fauna pointed out several lake level changes. A comparison with other proxies in the same core and the correlation with the oxygen isotope curve from Greenland allowed to interpret them as climatically driven changes (humid and arid periods). The analyses of Trasimeno core allowed us to improve the existing knowledge about the evolution of climatically-forced environmental conditions for the last 47,000 cal yr BP. The comparison with other climatic records indicates that the lake is sensitive to global climatic patterns. Furthermore, these results are challenging existing views about latitudinal moisture distribution in the Italian peninsula and, thus, contribute to constrain the outcome of climate models for the Mediterranean area.
author2 Ariztegui, Daniel
format Doctoral or Postdoctoral Thesis
author Marchegiano, Marta
author_facet Marchegiano, Marta
author_sort Marchegiano, Marta
title Reconstructing paleoclimate in central Italy since Late Pleistocene: the Lake Trasimeno ostracod record
title_short Reconstructing paleoclimate in central Italy since Late Pleistocene: the Lake Trasimeno ostracod record
title_full Reconstructing paleoclimate in central Italy since Late Pleistocene: the Lake Trasimeno ostracod record
title_fullStr Reconstructing paleoclimate in central Italy since Late Pleistocene: the Lake Trasimeno ostracod record
title_full_unstemmed Reconstructing paleoclimate in central Italy since Late Pleistocene: the Lake Trasimeno ostracod record
title_sort reconstructing paleoclimate in central italy since late pleistocene: the lake trasimeno ostracod record
publisher Université de Genève
publishDate 2017
url https://archive-ouverte.unige.ch/unige:105656
https://doi.org/10.13097/archive-ouverte/unige:105656
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_relation info:eu-repo/semantics/altIdentifier/urn/urn:nbn:ch:unige-1056568
unige:105656
https://archive-ouverte.unige.ch/unige:105656
doi:10.13097/archive-ouverte/unige:105656
op_rights Free access / No access until 2021-06-17
info:eu-repo/semantics/embargoedAccess
op_doi https://doi.org/10.13097/archive-ouverte/unige:105656
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