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The Holocene record of environmental changes in the ‘Stagno di Maccarese’ marsh (Tiber river delta, central Italy)

Bibliographic Data

ID12268167
AuthorsCarlo Giraudi (National Agency for New Technologies, Energy and Sustainable Economic Development, corresponding author)
Year2012
Volume22
Issue12
Pages1461-1471
Publication date2012-09-18
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683612455543
OpenAlexW2045748986
LanguageEN
Citations received2
References cited28

The stratigraphic study of the Stagno di Maccarese, carried out on the sediments exposed in about 7 km of trenches excavated in an area of approximately 1.5 km 2 , has shown that in the course of the Holocene many environmental variations have taken place. The complex evolution of the marsh is demonstrated by the variations in water salinity and the presence of erosion surfaces and soils between the sediments. In the early Holocene, the area studied was an isolated marsh with water having variable salinity, and it was only about 6000 cal. yr BP that it was encompassed in the system of inner delta marshes. In the delta environment, the water of the marsh was oligohaline until about 9th–8th centuries bc, brackish from 9th–8th centuries bc to about 600 yr BP, and later oligohaline until the 19th century drainage. A number of environmental variations are connected with local phenomena, such as erosion of the beach ridges and Tiber floods, but the others can be correlated chronologically with climatic events recorded at regional and global scale. The millennial variations seem to be connected with changes in insolation, while abrupt variations can be correlated chronologically with the IRD events dated at 8200, 5900, 4200, 2800, 1400 and 500 cal. yr BP

Brackish marsh · Brackish water · Delta · Erosion · Geography · Holocene · Marsh · Physical geography · River delta · Salinity · Salt marsh · Wetland · Coastal and Marine Dynamics · Geology and Paleoclimatology Research · Maritime and Coastal Archaeology · Ecology · Geology · Oceanography · Paleontology

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  • Middle to Late Holocene glacial variations, periglacial processes and alluvial sedimentation on the higher Apennine massifs (Italy)

    Open Access•Carlo Giraudi•Quaternary Research•2005

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    Open Access•Carlo Giraudi•Quaternary Research•2009

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    Open Access•Maria Gabriella Carboni, Luisa Bergamin et al.•Quaternary Research•2010

  • A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates

    Open Access•Gérard C Bond, Gerard Bond et al.•Science•1997

  • Insolation values for the climate of the last 10 million years

    Open Access•Alfons Berger, Marie‐France Loutre et al.•Quaternary Science Reviews•1991

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    Open Access•Michel Magny, Jacques‐louis De Beaulieu et al.•Quaternary Science Reviews•2007

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    Open Access•Paul A Mayewski, Eelco E Rohling et al.•Quaternary Research•2004

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    Open Access•Massimo Caldara, Ilena Caroli et al.•Quaternary International•2008

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  • The Holocene climatic evolution of Mediterranean Italy

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    Open Access•Ulrich E Joerin, Thomas F Stocker et al.•The Holocene•2006

  • The sediments of the ‘Stagno di Maccarese’ marsh (Tiber river delta, central Italy)

    Open Access•Carlo Giraudi•The Holocene•2011

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    Open Access•P Bellotti, Gilberto Calderoni et al.•The Holocene•2011

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    Open Access•Carlo Giraudi, Cristiana Tata et al.•Geoarchaeology•2009

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Citations per year0.17
Citation span2014 - 2026 (13)
Highly citedNo

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