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Responses to Quaternary Climate Change |
Catania University, Dip. Scienze Geologiche di Oceanologia e Paleoecologia, Corso Italia, 55, I-95129 Catania, Italy
A short Lower Pleistocene section, cropping out in SE Sicily, is studied. The sequence mainly consists of richly fossiliferous sandy layers with Arctica islandica, deposited in mid-shelf environments. Molluscs, bryozoans, serpuloideans and calcareous algae are investigated, to identify species with palaeoclimatological implications. Apart from some well-known North Atlantic molluscs, other species are identified as palaeoclimatological tools. Cooling evidence is provided by such palaeoclimatological indicators and by the increasing shell size in some species.
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M. Pedley and M. Grasso The response of cool-water carbonates to eustatic change in microtidal, Mediterranean Quaternary settings of Sicily Geological Society, London, Special Publications, 2006; 255: 137 - 156. [Abstract] [PDF] |
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