FN Archimer Export Format
PT J
TI The 100-ka and rapid sea level changes recorded by prograding shelf sand bodies in the Gulf of Lions (western Mediterranean Sea)
BT 
AF BASSETTI, Maria-Angela
   BERNE, Serge
   JOUET, Gwenael
   TAVIANI, M
   DENNIELOU, Bernard
   FLORES, J
   GAILLOT, Arnaud
   GELFORT, R
   LAFUERZA, S
   SULTAN, Nabil
AS 1:1,2;2:1,2;3:2;4:3;5:2;6:4;7:5;8:6;9:7;10:2;
FF 1:PDG-DOP-DCB-GM-LES;2:PDG-DOP-DCB-GM-LES;3:PDG-DOP-DCB-GM-LES;4:;5:PDG-DOP-DCB-GM-LES;6:;7:;8:;9:;10:PDG-DOP-DCB-GM-LES;
C1 Univ Perpignan, Inst Modelisat & Anal Geoenvironm & Sante, F-66860 Perpignan, France.
   Inst Francais Rech Exploitat Mer, F-29280 Plouzane, France.
   CNR, Ist Sci Marine, I-40129 Bologna, Italy.
   Univ Salamanca, Fac Ciencias, E-37008 Salamanca, Spain.
   Technopole Brest Iroise, Altran Quest, CS 23866, F-29238 Brest 3, France.
   Inst Geowissensch Gemeinschaftsaufgaben, D-30655 Hannover, Germany.
   Univ Barcelona, GRC Geociencies Marines, Dept Estratig & Paleontol & Geociencies Mari, E-08028 Barcelona, Spain.
C2 UNIV PERPIGNAN, FRANCE
   IFREMER, FRANCE
   CNR, ITALY
   UNIV SALAMANCA, SPAIN
   TECHNOPOLE BREST IROISE, FRANCE
   INST GEOWISSENSCH GEMEINSCHAFTSAUFGABEN, GERMANY
   UNIV BARCELONA, SPAIN
SI BREST
SE PDG-DOP-DCB-GM-LES
   PDG-DOP-DCB-NSE-AS
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-univ-france
IF 2.979
TC 49
UR https://archimer.ifremer.fr/doc/2008/publication-4929.pdf
LA English
DT Article
CR BEACHMED
   PROMESS 1
BO Le Suroît
   Bavenit
DE ;Paleoclimate;Mediterranean;Quaternary;Shoreface
AB Thick forced regressive units on the wide continental shelf of the Gulf of Lions (western Mediterranean) recorded the composite effect of sea level changes during the Quaternary. They are mostly composed of coastal siliciclastic and bioclastic wedges showing clinoform geometry. These deposits have been intensively explored through high-resolution seismic investigations, but only recently it was possible to ground truth seismic interpretations, based on a long (100 m) borehole that crossed the succession and recovered a large part of the mainly sandy deposits (similar to 84% recovery). A multiproxy analysis of the sedimentary succession shows that (1) the stratal architecture of the shelf margin is defined by major bounding surfaces that are polygenic erosion surfaces associated with coarse-grained material incorporating abundant and diverse shells, including cold-water fauna (presently absent from the Mediterranean Sea). Between each surface, coarsening upward units with steep (up to 5 degrees) foresets are made of massive (more than 20 m thick) sands with possible swaley and hummocky cross-stratification, passing seaward to sands with muddy intervals and, further offshore, alternating highly boiturbated sands and silts. Each prograding wedge corresponds to a forced-regressive shoreface (or delta front/prodelta), deposited during the overall sea level falls occurring at (relatively slow) interglacial/glacial transition and therefore represents the record of 100 ka cyclicity. Higher-frequency Milankovitch cyclicities are also probably represented by distinct shoreface/delta front wedges; (2) detailed examination of the architecture and chronostratigraphy of the most recent sequence shows that minor bounding surfaces, corresponding to abrupt shallowing of sedimentary facies, separate downward stepping parasequences within the last 100 ka sequence. These events are in phase with millennial-scale glacial climatic and sea level variability, the downward shift surfaces corresponding to the falls during the coldest stadials. These deposits provide a comprehensive and well-constrained Pleistocene analog to the numerous shoreface deposits attributed to falling-stage systems tracts recognized in ancient stratigraphic records, studied at the outcrop scale.
PY 2008
PD NOV
SO Geochemistry Geophysics Geosystems - G3
SN 1525-2027
PU American Geophysical Union
VL 9
IS Q11R05
UT 000260990400001
DI 10.1029/2007GC001854
ID 4929
ER

EF