Genesis of Organic Matter in the Kara Sea Bottom Sediments

被引:6
作者
Vetrov, A. A. [1 ]
Romankevich, E. A. [1 ]
机构
[1] Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia
基金
俄罗斯基础研究基金会;
关键词
CARBON; ACCUMULATION; DELTA-C-13;
D O I
10.1134/S0001437011040187
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Based on simultaneous use of organic and geochemical indicators (delta C-13, C/N, and n-alkanes\), the genesis of organic matter (OM) in recent bottom sediments of the Kara Sea was characterized. Maps for percentages and absolute masses of marine and terrigenous OM were drawn. The masses of buried marine and terrigenous OM were compared to its supply to the sea and onto the sea bottom.
引用
收藏
页码:608 / 615
页数:8
相关论文
共 26 条
[11]  
Kodina L.A., 2002, Reports Polar Mar. Res., V419, P143
[12]  
Kodina L. A., 2002, BERICHTE POLAR MESFO, P134
[13]   Organic carbon flow in the Ob, Yenisey Rivers and Kara Sea of the Arctic region [J].
Krishnamurthy, RV ;
Machavaram, M ;
Baskaran, M ;
Brooks, JM ;
Champ, MA .
MARINE POLLUTION BULLETIN, 2001, 42 (09) :726-732
[14]   Organic carbon isotope ratios (δ13C) of Arctic Amerasian Continental shelf sediments [J].
Naidu, AS ;
Cooper, LW ;
Finney, BP ;
Macdonald, RW ;
Alexander, C ;
Semiletov, IP .
INTERNATIONAL JOURNAL OF EARTH SCIENCES, 2000, 89 (03) :522-532
[15]  
Petrova V. I., 2004, ORGANIC CARBON CYCLE, P204
[16]  
Rachold V, 2004, ORGANIC CARBON CYCLE IN THE ARCTIC OCEAN, P33
[17]   Accumulation of particulate organic carbon at the Eurasian continental margin during late Quaternary times: controlling mechanisms and paleoenvironmental significance [J].
Stein, R ;
Boucsein, B ;
Fahl, K ;
de Oteyza, TG ;
Knies, J ;
Niessen, F .
GLOBAL AND PLANETARY CHANGE, 2001, 31 (1-4) :87-104
[18]  
Stein R., 1996, Ber Polarforscher, V212, P243
[19]  
Stein R., 1999, BER POLARFORSCH, P229
[20]  
Stein R., 2004, ORGANIC CARBON CYCLE, P24