The C37 alkenone record of seawater temperature during seasonal thermocline stratification

被引:43
作者
Bentaleb, I
Grimalt, JO
Vidussi, F
Marty, JC
Martin, V
Denis, M
Hatté, C
Fontugne, M
机构
[1] CSIC, Cid, Dept Environm Chem, ES-08034 Barcelona, Catalonia, Spain
[2] Phys & Chim Marines Lab, F-06238 Villefranche Sur Mer, France
[3] COM, Lab Oceanog & Biogeochim, UMR 6535, F-13288 Marseille, France
[4] CNRS, CEA, Lab Mixte, Ctr Faibles Radioact, F-91198 Gif Sur Yvette, France
关键词
particulate pigments; C-37-C-38; alkenones; total organic carbon; nitrogen; Ligurian Sea; seawater temperature; thermocline stratification;
D O I
10.1016/S0304-4203(98)00079-6
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The concentrations of suspended particulate pigments, C-37-C-38 alkenones, total organic carbon and nitrogen in the Ligurian Sea (northwestern Mediterranean) have been studied at 5 and 30 m depth during well defined thermocline conditions. An accurate description of the short term changes of these compounds has been achieved by means of four 36-h sampling cycles each encompassing consecutive filtration periods of 4 h. During sampling the thermocline changes were followed closely by simultaneous measurements of water column temperature, salinity and other physical parameters. The analysis of the collected samples indicates that the Haptophyte pigments and alkenones are essentially synthesized at the levels of highest primary production and therefore the C-37 alkenone record reflects the seawater temperature at this depth level. The study also shows that part of these alkenones are distributed throughout the water column in association to the suspended particles. This process results in C-37 alkenone distributions that, due to their high resistance to chemical and microbial degradation, record the temperature of the highest primary productivity layers even at shallow (e.g., 5 m depth) or deep (e.g., 1100 m depth) waters. (C) 1999 Elsevier Science B.V. All rights reserved.
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页码:301 / 313
页数:13
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