FN Archimer Export Format
PT J
TI The region of the Strandja Sill (North Turkey) and the Messinian events
BT 
AF SUC, Jean-Pierre
   GILLET, Herve
   CAGATAY, M. Namik
   POPESCU, Speranta-Maria
   LERICOLAIS, Gilles
   ARMIJO, Rolando
   MELINTE-DOBRINESCU, Mihaela Carmen
   SEN, Sevket
   CLAUZON, Georges
   SAKINC, Mehmet
   ZABCI, Cengiz
   UCARKUS, Gulsen
   MEYER, Bertrand
   CAKIR, Ziyadin
   KARAKAS, Cagil
   JOUANNIC, Gwenael
   MACALET, Rodica
AS 1:1,2;2:3;3:4;4:5;5:6;6:7;7:8;8:9;9:10;10:4;11:4;12:11;13:1,2;14:4;15:7;16:;17:;
FF 1:;2:;3:;4:;5:PDG-DAEI;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;
C1 Univ Paris 06, Univ Paris 04, UMR 7193, iSTeP, F-75005 Paris, France.
   iSTeP, CNRS, UMR 7193, F-75005 Paris, France.
   Univ Bordeaux 1, EPOC, F-33405 Talence, France.
   Istanbul Tech Univ, Fac Mines, Dept Geol Engn, TR-34469 Istanbul, Turkey.
   GeoBioStratData Consulting, F-69140 Rillieux La Pape, France.
   IFREMER, F-92138 Issy Les Moulineaux, France.
   Inst Phys Globe Paris, CNRS, Tecton & Mecan Lithosphere, UMR 7154, F-75238 Paris 05, France.
   Natl Inst Marine Geol & Geoecol, Bucharest 70318, Romania.
   Museum Natl Hist Nat, CNRS, UMR 7207, Ctr Rech Paleobiodiversite & Paleoenvironm, Paris, France.
   Aix Marseille Univ, CNRS, IRD, CEREGE UM34, F-13545 Aix En Provence, France.
   Istanbul Tech Univ, Eurasia Inst Earth Sci, TR-34469 Istanbul, Turkey.
   Cerema, DTer Est, Lab Reg Pants & Chaussees Nancy, F-54510 Tomblaine, France.
   Natl Inst Hydrol & Water Management, Bucharest 013686, Romania.
C2 UNIV PARIS 06, FRANCE
   ISTEP, FRANCE
   UNIV BORDEAUX, FRANCE
   UNIV ISTANBUL, TURKEY
   GEOBIOSTRATDATA CONSULTING, FRANCE
   IFREMER, FRANCE
   IPGP, FRANCE
   GEOECOMAR, ROMANIA
   MNHN, FRANCE
   UNIV AIX MARSEILLE, FRANCE
   UNIV TECH ISTANBUL, TURKEY
   CEREMA, FRANCE
   NIHWM, ROMANIA
SI SIEGE
SE PDG-DAEI
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 2.788
TC 25
UR https://archimer.ifremer.fr/doc/00251/36217/34768.pdf
LA English
DT Article
CR BLASON
   BLASON 2
   MD 139 / ASSEMBLAGE - 1
BO Le Suroît
   Marion Dufresne
DE ;Mediterranean-Paratethys connection;Onshore-offshore stratigraphy;Messinian Salinity Crisis;Erosion;Fluvial network
AB The two sides of the Strandja Sill show a highly discontinuous stratigraphic succession since the Late Oligocene. This area, together with the Sea of Marmara Basin, is usually proposed as the gateway for the Paratethyan freshwaters and organisms that constituted the Lago Mare facies in the Mediterranean Sea during the Messinian Salinity Crisis (MSC). Our investigations involving new field observations and datings, together with previous studies, suggest that the sill has possibly experienced such a connection at around 8 Ma, i.e. significantly before the crisis. The proposal of a sea-level drop of the Black Sea before 7 Ma is not supported by our data on dinoflagellate cysts. Consistency of calcareous nannofossil succession at DSDP Site 380 is reinforced, allowing to reassert that subaerial erosion impacted both the southwestern Black Sea and the central Marmara – Dardanelles area during the peak of the MSC. At that time, this region was crossed by two oppositely directed fluvial networks, further supporting the absence of a marine gateway through the Strandja Sill. It is concluded that none of the Lago Mare events recorded in the Mediterranean during the MSC were the consequence of the passage of Paratethyan waters and organisms through this area. In the Black Sea, the well-dated Messinian fluvial erosion can be followed offshore. The overlying prograding deltaic deposits attest to a fast marine reflooding after the crisis. This constitutes a comprehensive erosion - sedimentation model in an area intensively explored for hydrocarbons.
PY 2015
PD SEP
SO Marine And Petroleum Geology
SN 0264-8172
PU Elsevier Sci Ltd
VL 66
UT 000365055800010
BP 149
EP 164
DI 10.1016/j.marpetgeo.2015.01.013
ID 36217
ER

EF