Age refinement of the Messinian salinity crisis onset in the Mediterranean

Terra Nova - Tập 25 Số 4 - Trang 315-322 - 2013
Vinicio Manzi1,2, Rocco Gennari1,2, F.J. Hilgen3, Wout Krijgsman4, Stefano Lugli5, Marco Roveri1,2, Francisco Javier Sierro6
1Alpine Laboratory of Paleomagnetism (ALP), Via Madonna dei Boschi 76, Peveragno, 12016, CN, Italy
2Dipartimento di Fisica e Scienze della Terra Università degli Studi di Parma Parco Area delle Scienze 157/A 43100 Parma Italy
3Department of Earth Sciences, Utrecht University, Budapestlaan 4, Utrecht, 3584 CD, The Netherlands
4Paleomagnetic Laboratory Fort Hoofddijk, Utrecht University, Utrecht, the Netherlands
5Dipartimento di Scienze della Terra, Università degli Studi di Modena e Reggio Emilia, Piazza S. Eufemia 19, 41100 Modena, Italy
6Department of Geology, University of Salamanca, 37008 Salamanca, Spain

Tóm tắt

AbstractWe propose a revised age calibration of the Messinian salinity crisis onset in the Mediterranean at 5.971 Ma based on the recognition of an extra gypsum cycle in the transitional interval of the Perales section (Sorbas basin, Spain) and the revision of the magnetostratigraphy of the Monticino section (Vena del Gesso basin, Italy). This age re‐calibration allows to state more accurately that: (i) the interval encompassing theMSC‐onset is continuous, thus ruling out any erosional feature or stratigraphic hiatus related to a major sea‐level fall affecting the Mediterranean; (ii) the first gypsum was deposited during the summer insolation peak at 5.969 Ma associated with an eccentricity minimum and roughly coincident with glacial stageTG32; (iii) theMSC‐onset was preconditioned by the tectonically‐driven reduction of the hydrological exchanges with the Atlantic Ocean and finally triggered by glacial conditions in the northern hemisphere and by arid conditions in northern Africa.

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