A two‐step process for the reflooding of theMediterranean after theMessinianSalinityCrisis

Basin Research - Tập 24 Số 2 - Trang 125-153 - 2012
François Bache1,2,3, Speranta‐Maria Popescu4, Marina Rabineau5, Christian Gorini1,3, Jean‐Pierre Suc1,3, Georges Clauzon6, Louis Géli7, Jean‐Loup Rubino8, Mihaela Melinte-Dobrinescu9, Ferrán Estrada10, Laurent Londeix11, Rolando Armijo4, Bertrand Meyer1,3, Laurent Jolivet12, Estelle Leroux7,5, Daniel Aslanian7, Antônio Tadeu dos Reis13, Ludovic Mocochain14, Nikola Dumurdžanov15, Ivan Zagorchev16, Vesna Lesić17, Dragana Tomić17, M. Namık Çağatay18, Jean‐Pierre Brun19, Dimitrios Sokoutis15, István Csató20, Gülsen Uçarkuş18, Z. Çakır18
1CNRS, UMR 7193, ISTeP, F-75005 Paris, France
2GNS Science, P.O. Box 30368, Lower Hutt 5040, New Zealand
3UPMC Univ Paris 06, UMR 7193, ISTeP, F-75005, Paris, France
4Laboratoire de Tectonique, Institut de Physique du Globe de Paris (UMR 7154 CNRS), Paris Cedex, France
5IUEM Domaines océaniques (UMR 6538) 1 place Nicolas Copernic 29280 Plouzané France
6C.E.R.E.G.E. (UMR 6635) Université Paul Cézanne Europôle de l'Arbois BP 80 13545 Aix‐en‐Provence Cedex 04 France
7IFREMER Géosciences marines LGG BP 70 29280 Plouzané Cedex France
8TOTAL, TG/ISS, CSTJF, Avenue Laribeau, 64018, Pau Cedex, France
9National Institute of Marine Geology and Geoecology, 23-25 Dimitrie Onciul Street, P.O. Box 34-51, 70318 Bucharest, Romania
10Instituto de Ciencias del Mar de Barcelona, C.S.I.C., Paseo Juan de Borbon s/n, 08039 Barcelona, Spain
11Université Bordeaux 1, UMR 5805 CNRS ‘EPOC’ avenue des Facultés 33405 Talence cedex France
12ISTO (UMR 6113) Université d'Orléans 45071 Orléans Cedex 2 France
13Departamento de Oceanografia Geologica/UERJ‐Brazil Rua São Francisco Xavier 524, 48 Andar, Maracaña Rio de Janeiro RJ CEP 20.550‐900 Brazil
14Laboratoire de Géologie (UMR 8538) Ecole Normale Supérieure 24 rue Lhomond 75231 Paris Cedex 05 France
15ISES, Vrije Universiteit Amsterdam, 1081 HV Amsterdam, The Netherlands
16Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria
17Geolomagnetic Institute, Kraljice Natalije 45, 11000 Belgrad, Republic of Serbia
18Istanbul Technical University, School of Mines and Eurasia Institute of Earth Sciences, Maslak, 34469 Istanbul, Turkey
19Géosciences Rennes, UMR 6118, Université Rennes 1, 35042 Rennes Cedex, France
20Department of Geology, Collin College, 2800 Spring Creek Pkwy, Plano, TX, 75075 USA

Tóm tắt

AbstractTheMessinianSalinityCrisis is well known to have resulted from a significant drop of theMediterranean sea level. Considering both onshore and offshore observations, the subsequent reflooding is generally thought to have been very sudden. We present here offshore seismic evidence from theGulf ofLions and re‐visited onshore data fromItaly andTurkey that lead to a new concept of a two‐step reflooding of theMediterraneanBasin after theMessinianSalinityCrisis. The refilling was first moderate and relatively slow accompanied by transgressive ravinement, and later on very rapid, preserving the subaerialMessinianErosionalSurface. The amplitude of these two successive rises of sea level has been estimated at ≤500 m for the first rise and 600–900 m for the second rise. Evaporites from the centralMediterranean basins appear to have been deposited principally at the beginning of the first step of reflooding. After the second step, which preceeded theZancleanGlobalStratotypeSection andPoint, successive connections with theParatethyanDacicBasin, then theAdriatic foredeep, and finally theEuxinianBasin occurred, as a consequence of the continued global rise in sea level. A complex morphology with sills and sub‐basins led to diachronous events such as the so‐called ‘LagoMare’.This study helps to distinguish events that were synchronous over the entireMediterranean realm, such as the two‐step reflooding, from those that were more local and diachronous. In addition, the shoreline that marks the transition between these two steps of reflooding in theProvenceBasin provides a remarkable palaeogeographical marker for subsidence studies.

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