Response of primary production and calcification to changes of pCO2 during experimental blooms of the coccolithophorid Emiliania huxleyi -: art. no. GB2023

被引:164
作者
Delille, B [2 ]
Harlay, J
Zondervan, I
Jacquet, S
Chou, L
Wollast, R
Bellerby, RGJ
Frankignoulle, M
Borges, AV
Riebesell, U
Gattuso, JP
机构
[1] Univ Bergen, Bjerknes Ctr Climate Res, N-5007 Bergen, Norway
[2] Univ Liege, Unite Oceanog Chim, Interfac Ctr Marine Res MARE, B-4000 Liege, Belgium
[3] Free Univ Brussels, Lab Oceanog Chim & Geochim Eaux, B-1050 Brussels, Belgium
[4] Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany
[5] Univ Kiel, Leibniz Inst Marine Sci, D-24105 Kiel, Germany
[6] CNRS, UMR Cartell 42, Stn INRA Hydrobiol Lacustre, F-74203 Thonon Les Bains, France
[7] Univ Paris 06, CNRS, UMR 7093, Lab Oceanog Villefranche, F-06234 Villefranche Sur Mer, France
关键词
D O I
10.1029/2004GB002318
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
[1] Primary production and calcification in response to different partial pressures of CO2 (PCO2) ("glacial,'' "present,'' and "year 2100'' atmospheric CO2 concentrations) were investigated during a mesocosm bloom dominated by the coccolithophorid Emiliania huxleyi. The day-to-day dynamics of net community production (NCP) and net community calcification (NCC) were assessed during the bloom development and decline by monitoring dissolved inorganic carbon (DIC) and total alkalinity ( TA), together with oxygen production and 14 C incorporation. When comparing year 2100 with glacial PCO2 conditions we observed: ( 1) no conspicuous change of net community productivity (NCPy); ( 2) a delay in the onset of calcification by 24 to 48 hours, reducing the duration of the calcifying phase in the course of the bloom; ( 3) a 40% decrease of NCC; and ( 4) enhanced loss of organic carbon from the water column. These results suggest a shift in the ratio of organic carbon to calcium carbonate production and vertical flux with rising atmospheric PCO2.
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页码:1 / 14
页数:14
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