Five cores from the southern Tyrrhenian and Ionian seas were studied for their tephra and cryptotephra content in the 4.4–2.0 ka time interval. The chronological framework for each core was obtained by accelerator mass spectrometry 14C dating, the occurrence of distinct marker tephra and stratigraphic correlation with adjacent records. Tephrochronology allowed us to correlate the analyzed deposits with tephra markers associated with Somma-Vesuvius (79 ad), Ischia Island (Cretaio), Mt Etna (FG, FL and FS) and Campi Flegrei (Astroni-Agnano Monte Spina) events. For the first time in the marine setting, a large single glass data set is provided for the Late Holocene Etnean marker beds including the FS tephra (ca. 4.3 ka). Moreover, unknown depo...
Tephra layers are assuming an increasingly important role in the dating and correlation of Late Quat...
The identification and characterisation of high-frequency climatic changes during the Holocene requi...
The identification and characterisation of high-frequency climatic changes during the Holocene requi...
Five cores from the southern Tyrrhenian and Ionian seas were studied for their tephra and cryptoteph...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ 18 O) anal...
We present a major, trace and rare earth element characterization of single glass shards from fiftee...
A detailed tephrostratigraphic study supported by stable isotope (à18O) analyses and AMS 14C dating ...
A tephrochronological investigation was carried out at site ND14Q (1013 m of water depth), located i...
A tephrochronological investigation was carried out at site ND14Q (1013 m of water depth), located i...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ18O) analys...
Tephra layers are assuming an increasingly important role in the dating and correlation of Late Quat...
The identification and characterisation of high-frequency climatic changes during the Holocene requi...
The identification and characterisation of high-frequency climatic changes during the Holocene requi...
Five cores from the southern Tyrrhenian and Ionian seas were studied for their tephra and cryptoteph...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ 18 O) anal...
We present a major, trace and rare earth element characterization of single glass shards from fiftee...
A detailed tephrostratigraphic study supported by stable isotope (à18O) analyses and AMS 14C dating ...
A tephrochronological investigation was carried out at site ND14Q (1013 m of water depth), located i...
A tephrochronological investigation was carried out at site ND14Q (1013 m of water depth), located i...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ18O) analys...
Tephra layers are assuming an increasingly important role in the dating and correlation of Late Quat...
The identification and characterisation of high-frequency climatic changes during the Holocene requi...
The identification and characterisation of high-frequency climatic changes during the Holocene requi...