por
Marra, F.,
Pereira, A.,
Jicha, B.,
Nomade, S.,
Biddittu, I.,
Florindo, F.,
Muttoni, G.,
Niespolo, E. M.,
Renne, P. R.,
Scao, V.
Publicado 2022
“…In particular, we find a precise match between the ages of gravel deposition and the occurrence of moderate sea-level rise events which anticipate those more marked during the glacial termination V and IV in the Red Sea relative sea level curve, as already verified by data from the
Tiber River catchment basin. Such correspondence suggests that gravel deposition is facilitated by melting of Apennine mountain range glaciers, which provide the water transport energy and a surplus of clastic input to the rivers draining the mountain regions and flowing into the Tyrrhenian Sea. …”
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