FN Archimer Export Format
PT J
TI Geochemical Characteristics of Iron in Sediments from the Sea of Marmara
BT 
AF YANG, Hailin
   LU, Hailong
   RUFFINE, Livio
AS 1:1,2;2:1,3;3:4;
FF 1:;2:;3:PDG-REM-GM-LCG;
C1 Peking Univ, Coll Engn, Dept Energy & Resources Engn, Beijing 100871, Peoples R China.
   China Univ Geosci, Sch Ocean Sci, Beijing 100083, Peoples R China.
   Peking Univ, Inst Ocean Res, Beijing 100871, Peoples R China.
   IFREMER, Ctr Bretagne, Dept REM, Unite Geosci Marines,Lab Cycles Geochim & Resourc, F-29280 Plouzane, France.
C2 UNIV PEKING, CHINA
   UNIV CHINA GEOSCI, CHINA
   UNIV PEKING, CHINA
   IFREMER, FRANCE
SI BREST
SE PDG-REM-GM-LCG
IN WOS Ifremer jusqu'en 2018
   copubli-int-hors-europe
   copubli-sud
IF 2.43
TC 5
UR https://archimer.ifremer.fr/doc/00423/53455/54347.pdf
LA English
DT Article
CR MARSITECRUISE
BO Pourquoi pas ?
DE ;Iron geochemistry;The Sea of Marmara;Sediment;Redox environment
AB Two ~1000 cm long sediment cores were recovered from the Sea of Marmara, one with the occurrence of gas hydrates in the Western High, and the other without hydrates in the Cinarcik Basin. Differences in mineralogical and chemical compositions have been identified between the two sediment cores. Based on the results of the mineralogical and geochemical analyses, the main sources of the sediments are quite similar for both investigated areas, but the authigenic components are different, particularly iron sulfides and carbonates. Authigenic Fe(II) carbonate are much higher in Core MRS-CS-05 in the Western High, while crystalline Fe(III) phases are more abundant in Core MRS-CS-16 in the Cinarcik Basin. Notably, the enrichments of greigite (Fe3S4), a metastable ferromagnetic iron sulfide mineral and intermediate polysulfide, as well as iron carbonates are identified at 400 cmbsf with the maximum iron content in Core MRS-CS-05. These indicate the presence of a more reducing and acidic environment in the Western High, mainly due to higher organic matter content and seepage of heavy hydrocarbons in the sediments. 
PY 2018
PD JUN
SO Deep-sea Research Part Ii-topical Studies In Oceanography
SN 0967-0645
PU Pergamon-elsevier Science Ltd
VL 153
UT 000449444700010
BP 121
EP 130
DI 10.1016/j.dsr2.2018.01.010
ID 53455
ER

EF