NDLI: Climatic variability and anthropogenic signatures in the Gulf of Salerno (southern-eastern Tyrrhenian Sea) during the last half millennium

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Late Holocene sedimentary changes in shallow water settings: the case of the Sele river offshore in the Salerno Gulf (south-eastern Tyrrhenian Sea, Italy)

Holocene environmental evolution of the costal sector in front of the Poseidonia-Paestum archaeological area (Sele plain, southern Italy)

Sedimentology and depositional history of the travertines outcropping in the Poseidonia-Paestum archaeological area

An overview of soil erosion modelling compatible with RUSLE approach

Evolution of the Sele River coastal plain (southern Italy) during the Late Quaternary by inland and offshore stratigraphical analyses

Distribution of benthic foraminifera from the southern Tyrrhenian continental shelf (South Italy)

Relative sea-level rise and marine erosion and inundation in the Sele river coastal plain (Southern Italy): scenarios for the next century

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Climatic variability and anthropogenic signatures in the Gulf of Salerno (southern-eastern Tyrrhenian Sea) during the last half millennium

Content Provider	Springer Nature Link
Author	Vallefuoco, Mattia Lirer, Fabrizio Ferraro, Luciana Pelosi, Nicola Capotondi, Lucilla Sprovieri, Mario Incarbona, Alessandro
Copyright Year	2011
Abstract	The high-resolution study of sediment core C90-1 m collected at the continental shelf of the Gulf of Salerno (southern Tyrrhenian Sea) provides an excellent opportunity to show paleoenvironmental changes during the last 500 years induced by natural variability and human impact. Based on $^{210}$Pb and $^{137}$Cs measurements, the sedimentation rate results 0.20 cm/year for the last 100 years. The high sampling resolution (1 cm sample spacing) of core C90-1 m, 105 cm long, provides a time resolution of approximately 5 years/cm. Quantitative changes in the planktonic and benthonic foraminiferal assemblages combined with δ$^{18}$O$_{ G.ruber }$ variations allow to identify regional climatic and oceanographic signals. A significant turnover between herbivorous and opportunistic species and carnivorous planktonic foraminifera after the Maunder event suggests changes in river runoff and/or an increase in coastal flooding events in the studied area. Variations in the microfauna since 1940 yAD document environmental changes induced by the construction of a dam in the Sele River.
Starting Page	13
Ending Page	23
Page Count	11
File Format	PDF
ISSN	20374631
Journal	Rendiconti Lincei
Volume Number	23
Issue Number	1
e-ISSN	17200776
Language	English
Publisher	Springer Milan
Publisher Date	2011-11-19
Publisher Place	Milan
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Planktonic and benthonic foraminifera Oxygen stable isotope stratigraphy Last half millennium Continental shelf Tyrrhenian Sea Life Sciences Biomedicine general Environment Earth Sciences History of Science
Content Type	Text
Resource Type	Article

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Late Holocene sedimentary changes in shallow water settings: the case of the Sele river offshore in the Salerno Gulf (south-eastern Tyrrhenian Sea, Italy)

Distribution of benthic foraminifera from the southern Tyrrhenian continental shelf (South Italy)

Last deglaciation paleoclimatology in the Cefalù Basin — southern Tyrrhenian Sea

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Imaging continental shelf shallow stratigraphy by using different high-resolution seismic sources: an example from the Calabro-Tyrrhenian margin (Mediterranean Sea)

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Late Quaternary paleoceanographic evolution of the Aegean Sea: planktonic foraminifera and stable isotopes

Seasonal variations in planktonic foraminiferal flux and the chemical properties of their shells in the southern South China Sea

Climatic variability and anthropogenic signatures in the Gulf of Salerno (southern-eastern Tyrrhenian Sea) during the last half millennium

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