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Late Holocene evolution of Tiber river delta and geoarchaeology of Claudius and Trajan Harbor, Rome

Datos Bibliográficos

ID12134135
AutoresCarlo Giraudi (National Agency for New Technologies, Energy and Sustainable Economic Development, autor de correspondencia), Cristiana Tata (National Agency for New Technologies, Energy and Sustainable Economic Development), Lidia Paroli
Año2009
Volumen24
Número3
Páginas371-382
Fecha de publicación2009-04-16
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaGeoarchaeology (JOURNAL)
Identificadores de la revistaISSN: 0883-6353 • E-ISSN: 1520-6548
EditorialWiley (PUBLISHER • GB)
DOI10.1002/gea.20270
OpenAlexW2012374405
IdiomaEN
Citas recibidas26
Referencias citadas6

This study provides new information on the evolution of the Tiber delta during the late Holocene, and describes the record of sedimentation in the Port of Claudius and Trajan. The Tiber flowed into the Tyrrhenian Sea in the area of the Port of Claudius and Trajan between the 8th and 5th centuries B.C. The harbor basins excavated by the Romans during the 1st and 2nd centuries A.D. were filled with sediments containing saltwater fauna, then brackish‐water fauna, and finally by alluvial and marsh deposits. The Port of Claudius and Trajan was silted in as a consequence of episodes of alluviation that correlate with environmental events, possibly triggered by global climate changes. © 2009 Wiley Periodicals, Inc

Alluvium · Archaeology · Brackish water · Delta · Fauna · Geoarchaeology · Geography · Holocene · Salinity · Archaeology and ancient environmental studies · Marine and environmental studies · Maritime and Coastal Archaeology · Geology · Oceanography · Paleontology

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Obras citantes distintas26
Citas por año1,63
Intervalo de citas2010 - 2026 (17)
Velocidad de citacióncurrent
Altamente citadoNo
Tipos de citaNeutras: 26
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