FN Archimer Export Format
PT J
TI Late Pleistocene to Recent ostracod assemblages from the western Black Sea
BT 
AF BOOMER, Ian
   GUICHARD, Francois
   LERICOLAIS, Gilles
AS 1:1;2:2;3:3;
FF 1:;2:;3:PDG-DOP-DCB-GM-LES;
C1 Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, W Midlands, England.
   CEA, CNRS, UVSQ, LSCE,Lab Sci Climate & Environm, F-91198 Gif Sur Yvette, France.
   IFREMER, Ctr Brest, Lab Environm Sedimentaires, F-29280 Plouzane, France.
C2 UNIV BIRMINGHAM, UK
   CEA, FRANCE
   IFREMER, FRANCE
SI BREST
SE PDG-DOP-DCB-GM-LES
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
IF 0.719
TC 31
TU Centre national de la recherche scientifique
   Commissariat à l'énergie atomique et aux énergies alternatives
   Université de Versailles Saint-Quentin-en-Yvelines
UR https://archimer.ifremer.fr/doc/00025/13646/10887.pdf
LA English
DT Article
CR BLASON
   MD 139 / ASSEMBLAGE - 1
BO Le Suroît
   Marion Dufresne
DE ;Ponto-Caspian;Black Sea;Ostracoda;Pleistocene;Holocene
AB During the last glacial phase the Black Sea basin was isolated from the world's oceans due to the lowering of global sea-levels. As sea-levels rose during the latest glacial and early Holocene period, the Black Sea was once again connected to the eastern Mediterranean via the Dardanelles-Marmara-Bosporus seaway. In recent years, trace element and stable isotope analyses of ostracod assemblages have yielded important details regarding the hydrological evolution of the Black Sea during these events. Despite this focus on the geochemical signatures of the ostracods, little if any attention has been paid to the taxonomic composition of the ostracod assemblages themselves and there are notably few publications on the sub-littoral fauna of this important water body. We present a summary of the most abundant ostracod taxa of the Black Sea during the late glacial to early Holocene phase (dominated by the Candonidae, Leptocytheridae and Loxoconchidae) and chart their response to the subsequent environmental changes in the early Holocene with the pre-connection, low salinity 'lacustrine' fauna being replaced by one with a more Mediterranean aspect. Many of these taxa are illustrated using SEM for the first time, providing an important initial step in establishing taxonomic stability within Black Sea ostracod studies and noting faunal similarities with neighbouring areas, such as the Caspian Sea.
PY 2010
PD DEC
SO Journal Of Micropalaeontology
SN 0262-821X
PU Geological Soc Publ House
VL 29
UT 000285456700003
BP 119
EP 133
DI 10.1144/0262-821X10-003
ID 13646
ER

EF