Composition and significance of picophytoplankton in Antarctic waters

被引:144
作者
Wright, Simon W. [1 ,2 ]
Ishikawa, Akira [3 ]
Marchant, Harvey J. [1 ,2 ]
Davidson, Andrew T. [1 ,2 ]
van den Enden, Rick L. [1 ,2 ]
Nash, Geraldine V. [1 ]
机构
[1] Australian Antarctic Div, Kingston, Tas 7050, Australia
[2] Antarctic Climate & Ecosyst Cooperat Res Ctr, Hobart, Tas 7001, Australia
[3] Mie Univ, Grad Sch Bioresources, Tsu, Mie 5148507, Japan
基金
日本学术振兴会;
关键词
Picophytoplankton; Phytoplankton; Antarctic; Pigments; CHEMTAX; Microscopy; SIZE-FRACTIONATED PHYTOPLANKTON; SOUTHERN-OCEAN; COMMUNITY STRUCTURE; PELAGIC ECOSYSTEM; SURFACE WATERS; MARINE; PICOPLANKTON; PRODUCTIVITY; NANOPLANKTON; CAROTENOIDS;
D O I
10.1007/s00300-009-0582-9
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Filter fractionated picophytoplankton from Antarctic coastal waters (summer 2001) represented only 7-33% of total phytoplankton, even though total stocks were low (average Chl a = 0.32 mu g l(-1), range = 0.13-1.03 mu g l(-1)). Though all cells passed a 2 mu m filter, electron microscopy revealed most cells were over 2 mu m, principally Parmales, Phaeocystis sp., and small diatoms. CHEMTAX analysis of HPLC pigment data suggested type 8 haptophytes (e.g. Phaeocystis sp. plus Parmales and pelagophytes) contributed 7-58% of picoplanktonic chlorophyll a, type 6 haptophytes (e.g. coccolithophorids) 18-59%, diatoms 0-18% (mostly type 2 diatoms, e.g. Pseudonitzschia sp., 0-15%), prasinophytes 0-17%, with cell fragments of cryptophytes 0-40%, and dinoflagellates 0-11%. Only stocks of type 8 haptophytes and prasinophytes differed significantly due to successional changes. Zeaxanthin concentrations exceeded estimates from previous cyanobacterial counts and may derive from non-photosynthetic bacteria.
引用
收藏
页码:797 / 808
页数:12
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