Environmental drivers of coccolithophore abundance and calcification across Drake Passage (Southern Ocean)
Environmental drivers of coccolithophore abundance and calcification across Drake Passage (Southern Ocean)
复制标题
DOI:
10.5194/bg-13-5917-2016
复制
发表时间:
2016-11
期刊:
影响因子:
4.9
通讯作者:
A. Charalampopoulou;A. Poulton;D. Bakker;M. Lucas;M. Stinchcombe;T. Tyrrell
中科院分区:
文献类型:
--
作者:
A. Charalampopoulou;A. Poulton;D. Bakker;M. Lucas;M. Stinchcombe;T. Tyrrell
Abstract. Although coccolithophores are not as numerically common or as diverse in the Southern Ocean as they are in subpolar waters of the North Atlantic, a few species, such as Emiliania huxleyi, are found during the summer months. Little is actually known about the calcite production (CP) of these communities or how their distribution and physiology relate to environmental variables in this region. In February 2009, we made observations across Drake Passage (between South America and the Antarctic Peninsula) of coccolithophore distribution, CP, primary production, chlorophyll a and macronutrient concentrations, irradiance and carbonate chemistry. Although CP represented less than 1 % of total carbon fixation, coccolithophores were widespread across Drake Passage. The B/C morphotype of E. huxleyi was the dominant coccolithophore, with low estimates of coccolith calcite (∼ 0.01 pmol C coccolith−1) from biometric measurements. Both cell-normalised calcification (0.01–0.16 pmol C cell−1 d−1) and total CP (