Pigment adaptations in surface phytoplankton along the eastern boundary of the Atlantic Ocean

被引:52
作者
Barlow, RG
Aiken, J
Moore, GF
Holligan, PM
Lavender, S
机构
[1] Marine & Coastal Management, ZA-8012 Cape Town, South Africa
[2] Plymouth Marine Lab, Plymouth PL1 3DH, Devon, England
[3] So Oceanog Ctr, Southampton SO14 3ZH, Hants, England
[4] Univ Plymouth, Inst Marine Studies, Plymouth PL4 8AA, Devon, England
关键词
pigment indices; ocean colour; Atlantic ocean; eastern transect;
D O I
10.3354/meps281013
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Pigment and ocean colour data were used to characterise the phytoplankton at the surface along an eastern boundary transect of the Atlantic Ocean in May and June 1998. Five major regions were delineated, including the Benguela and Canary upwelling systems off SW and NW Africa, the temperate NE Atlantic, the northern oligotrophic gyre and a southern oligotrophic zone. Diagnostic indices were derived to assess the chemotaxonomic composition of the phytoplankton community, while photo-pigment indices were derived to investigate pigment adaptations across the regions. A large range in chlorophyll a concentrations was observed along the transect, varying from 0.03 to 30.6 mg m(-3). The levels were high in the high productivity regions, with mean concentrations being 3-fold greater in the Benguela region compared to the Canary and temperate NE Atlantic. Chlorophyll a levels were low in the oligotrophic regions, but concentrations in the southern oligotrophic region were double those in the northern. Diagnostic indices revealed that microplankton dominated the community in the Benguela region, nanoplankton dominated the temperate NE Atlantic and a mixed community of micro- and nanoplankton were present in the Canary region. Picoplankton comprised the majority of the communities in the 2 oligotrophic regions. Photo-pigment indices indicated that variation in the chlorophyll a proportion of total pigments was small, averaging 45 % across the transect, but the accessory pigment pool varied considerably. Chlorophyll c and photosynthetic carotenoids were prominent in the high productivity regions, resulting in photosynthetic pigments (chlorophylls plus carotenoids) accounting for 87 to 93 % of total pigments. In contrast, the level of photoprotective carotenoids was high in oligotrophic regions, resulting in a photosynthetic pigment content of only 68 %.
引用
收藏
页码:13 / 26
页数:14
相关论文
共 38 条
[1]   REMOTE-SENSING OF OCEANIC BIOLOGY IN RELATION TO GLOBAL CLIMATE CHANGE [J].
AIKEN, J ;
MOORE, GF ;
HOLLIGAN, PM ;
MALIN .
JOURNAL OF PHYCOLOGY, 1992, 28 (05) :579-590
[2]   The Atlantic Meridional Transect: overview and synthesis of data [J].
Aiken, J ;
Rees, N ;
Hooker, S ;
Holligan, P ;
Bale, A ;
Robins, D ;
Moore, G ;
Harris, R ;
Pilgrim, D .
PROGRESS IN OCEANOGRAPHY, 2000, 45 (3-4) :257-312
[3]   Spatial variations in the chlorophyll-specific absorption coefficients of phytoplankton and photosynthetically active pigments in the equatorial Pacific [J].
Allali, K ;
Bricaud, A ;
Claustre, H .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1997, 102 (C6) :12413-12423
[4]   Nitrogen- and irradiance-dependent variations of the maximum quantum yield of carbon fixation in eutrophic, mesotrophic and oligotrophic marine systems [J].
Babin, M ;
Morel, A ;
Claustre, H ;
Bricaud, A ;
Kolber, Z ;
Falkowski, PG .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1996, 43 (08) :1241-1272
[5]   Phytoplankton pigment and absorption characteristics along meridional transects in the Atlantic Ocean [J].
Barlow, RG ;
Aiken, J ;
Holligan, PM ;
Cummings, DG ;
Maritorena, S ;
Hooker, S .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 2002, 49 (04) :637-660
[6]   Monsoonal influence on the distribution of phytoplankton pigments in the Arabian Sea [J].
Barlow, RG ;
Mantoura, RFC ;
Cummings, DG .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1999, 46 (3-4) :677-699
[7]   Improved resolution of mono- and divinyl chlorophylls a and b and zeaxanthin and lutein in phytoplankton extracts using reverse phase C-8 HPLC [J].
Barlow, RG ;
Cummings, DG ;
Gibb, SW .
MARINE ECOLOGY PROGRESS SERIES, 1997, 161 :303-307
[8]   Spatial and temporal variability of phytoplankton pigment distributions in the central equatorial Pacific Ocean [J].
Bidigare, RR ;
Ondrusek, ME .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1996, 43 (4-6) :809-833
[9]   SPECIFIC PHYTOPLANKTON BIOMASSES AND THEIR RELATION TO PRIMARY PRODUCTION IN THE TROPICAL NORTH-ATLANTIC [J].
CLAUSTRE, H ;
MARTY, JC .
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS, 1995, 42 (08) :1475-1493
[10]   TANSLEY REVIEW .30. THE PHYTOPLANKTONIC WAYS OF LIFE [J].
FOGG, GE .
NEW PHYTOLOGIST, 1991, 118 (02) :191-232