Search results for " Sea level rise"

showing 3 items of 3 documents

Introducing INTERMED International Workshop – Intertidal organisms as a proxy for climate change.

2009

Intermed climate change temperature sea level rise
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Human settlements in the Mediterranean and the sea level changes from 12 ka to the present

2012

Understanding past sea-level change plays an important role in determining the underlying causes, and also allows the extrapolation of past sea levels to locations and epochs for which there are no instrumental data. A compilation of global sea-level estimates based on deep-sea oxygen isotope ratios at millennial-scale resolution or higher was published since ‘70. These global sea level curves do not take in account isostasy and tectonics. Observed sea level change can be reconstructed from dated fossils, coral reef terraces, speleothems, emerged and forming terraces on coastal areas, archaeological and other markers well connected with sea level. Because of the lack of coral reefs in the M…

Mediterranean climatePalaeoshorelinesea level rise; palaeoshorelines; late pleistocene; palaeoshorelines.; holoceneHoloceneSettore GEO/04 - Geografia Fisica E GeomorfologiaHolocene Late Pleistocene Sea level rise PalaeoshorelinesHolocene; Late pleistocene; Palaeoshorelines; Sea level rise; GeologyGeologyLate pleistoceneSea level riseOceanographyGeographySea level riseLate PleistoceneHuman settlementPalaeoshorelinesHoloceneSea levelPalaeoshorelines.
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The Brolo Island, a lentil in the “Ocean”

2010

The north-eastern Sicily coast reflects the effects of Holocene active tectonics associated to subduction system of Ionian crust beneath the Calabrian arc (CAPUTO et alii, 1970; WESTAWAY, 1993, DOGLIONI et alii, 1999). The latter, characterized by a stack of crystalline rock and its sedimentary cover, is the highest structural element in the Sicily chain. The Calabrian arc is a region that records one of the major Quaternary vertical tectonic movement in the whole Mediterranean basin. This uplift, well documented from Last Interglacial, is expressed as vertical variation of the height of the Quaternary marine terraces inner margin that characterize the north-eastern Sicily coast. The uplift…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaHolocene Sicily sea level rise tectonics.
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