Reading Pleistocene eustasy in a tectonically active siliciclastic shelf setting (Crotone peninsula, southern Italy)

Constraints on the amplitude of Mid-Pliocene (3.6–2.4 Ma) eustatic sea-level fluctuations from the New Zealand shallow-marine sediment record

“…Naish et al 1998). Similar shallow-marine evidence for NH glacio-eustasy has been described from Japan (Cronin et al 1994;Kitamura et al 1994), Italy (Rio et al 1996) and California (Clifton et al 1988).…”

An integrated sequence stratigraphic, palaeoenvironmental, and chronostratigraphic analysis of the Tangahoe Formation, southern Taranaki coast, with implications for mid‐Pliocene (c. 3.4–3.0 Ma) glacio‐eustatic sea‐level changes

“…Moreover, Naish et al (1998) presented a composite cyclostratigraphy from Wanganui Basin that provided shallow-marine evidence for most of the 48 or so fluctuations in the Northern Hemisphere ice sheets inferred from δ 18 O records (e.g., Shackleton et al 1995). Similar shallow-marine evidence for Northern Hemisphere glacioeustasy has been described from Japan (Cronin et al 1994;Kitamura et al 1994), Italy (Rio et al 1996), and California (Clifton et al 1988).…”

Magnetic fabric of Plio-Pleistocene sediments from the Crotone fore-arc basin: Insights on the recent tectonic evolution of the Calabrian Arc (Italy)

“…Finally fastest regional subsidence rates were attained during the early Pleistocene, as documented by the deposition of a thick succession of monotonous, muddy slope deposits (Roda, 1964;Rio et al, 1996;Capraro et al, 2011). The younger part of the succession (middle Pleistocene) is characterized by a distinct shallowingupwards trend predating the definitive uplift of the basin, which probably occurred in the latest middle Pleistocene (Capraro et al, 2011;Zecchin et al, 2011).…”

“…In particular, the first sequence encompasses the Serravallian to early Messinian interval, the second developed from middle Messinian to early Pliocene, and the third from middle Pliocene to middle Pleistocene. Interpretation of the older part of the local stratigraphy (Miocene) is still ambiguous, as the component sediments are, in general, not amenable to standard bio-magnetostratigraphic analyses (Roda, 1964;Rio et al, 1996).…”