Thermoluminescence dating tests of Pleistocene sediments from uplifted marine shorelines along the southwest coastline of the Calabrian Peninsula (southern Italy)

This paper presents TL age estimates of Pleistocene raised marine terraces: from southern Calabria (southern Italy). It focuses on the dating of last interglacial shallow-marine sand deposits. including several Tyrrhenian key reference deposits whose stratigraphic assignment is based on biostratigraphic evidence (presence of a Strombus bubonius fauna) and geochronometric data (amino-acid data calibrated with U/Th dates on coral). The TL age estimates are obtained (in alkali feldspar coarse grains using their blue TL emission. They are in rood agreement with the IR-OSL ape estimates obtained on the same feldspar samples. Our feldspar TL method is tested on two Tyrrhenian key reference sites, Ravagnese and Bovetto. in the Reggio di Calabria area. Their measured TL age estimates (97 +/- 11 ka and 100 +/- 10 ka) are lower than their estimated geological age (i.e. Oxygen Isotope Substage 5e). The correction for longterm fading suggested by Mejdahl (1988). is tested on these two samples using a lifetime of 446 ka as estimated from both Calabrian and Miocene sand collected within the same area. This correction would yield preliminary TL ages (116+/-13 ka and 116 +/- 12 ka that are in better agreement with the expected geological age. The application of our it method to paleoshorelines lying below the Tyrrhenian reference shoreline of Ravagnese-Bovetto, yields stratigraphically consistent TL age estimates. The TL method is also applied to two supposedly pre-last interglacial paleoshorelines which are geomorphologically older than the Tyrrhenian reference shorelines, They remain however chronologically undifferentiated. both by the TL and the amino-acid methods. Finally. the preliminary feldspar TL results obtained on the Miocene and the Calabrian sand deposits (> 1 Ma). suggest that our feldspar TL method is limited, in the SW Calabrian area. to about 200 ka. (C) 1997 Elsevier Science B.V.