Spatial variation in phytoplankton dynamics in the Belgian coastal zone of the North Sea studied by microscopy, HPLC-CHEMTAX and underway fluorescence recordings

被引:62
作者
Muylaert, K
Gonzales, R
Franck, M
Lionard, M
Van der Zee, C
Cattrijsse, A
Sabbe, K
Chou, L
Vyverman, W
机构
[1] Katholieke Univ Leuven, Dept Biol, B-3001 Heverlee, Belgium
[2] Free Univ Brussels, Lab Oceanog Chim & Geochim Eaux, B-1050 Brussels, Belgium
[3] Flanders Marine Inst, VLIZ, B-8400 Oostende, Belgium
关键词
phytoplankton; diatoms; Phaeocystis; HPCL; CHEMTAX; Southern Bight of North Sea; Scheldt or Schelde estuary;
D O I
10.1016/j.seares.2005.12.002
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
Spatial variation in the succession of phytoplankton in the Belgian Coastal Zone (BCZ) was investigated by monitoring phytoplankton biomass and community composition using microscopical cell counts, HPLC pigment analyses and in vivo fluorescence recordings. Monthly monitoring of phytoplankton community composition at five stations revealed a succession of three distinct diatom communities. The succession of these three communities was the same at each site, but the succession from the winter-spring to the summer community Occurred one month earlier and the succession from the summer to the autumn community one month later at the SW than at the NE stations of the BCZ. Monthly monitoring of chlorophyll a at ten fixed sites and inspection of in vivo fluorescence recordings during various cruises of RV 'Zeeleeuw' indicated that the spring bloom started about one month earlier in the SW part of the BCZ than in the NE part. The spatial difference in the onset of the spring bloom was ascribed to the higher water column turbidity at the NE coast compared to the SW coast. Although a Phaeocystis bloom occurred at all monitoring stations, a clear spatial variation in the magnitude of such blooms was observed, with more intense blooms at the NE coast than at the SW coast. A close relation was observed between the intensity of the Phaeocystis bloom and the availability of inorganic nutrients (N and P) before the onset of the bloom. Comparison of microscopical cell counts and CHEMTAX analysis of accessory pigment data indicated that HPLC analysis may be a useful tool for monitoring Phaeocystis in the North Sea. The presence of chlorophyll c(3) containing diatoms, however, probably resulted in the detection of small quantities of Phaeocystis by HPLC-CHEMTAX analysis when microscopical analyses showed that the species was absent. (c) 2006 Elsevier B.V All rights reserved.
引用
收藏
页码:253 / 265
页数:13
相关论文
共 45 条
[1]   Size distribution of algal pigments and phytoplankton assemblages in a coastal-estuarine environment: contribution of small eukaryotic algae [J].
Ansotegui, A ;
Sarobe, A ;
Trigueros, JM ;
Urrutxurtu, I ;
Orive, E .
JOURNAL OF PLANKTON RESEARCH, 2003, 25 (04) :341-355
[2]   19′-hexanoyloxyfucoxanthin may not be the appropriate pigment to trace occurrence and fate of Phaeocystis:: the case of P-globosa in Belgian coastal waters [J].
Antajan, E ;
Chrétiennot-Dinet, MJ ;
Leblanc, C ;
Daro, MH ;
Lancelot, C .
JOURNAL OF SEA RESEARCH, 2004, 52 (03) :165-177
[3]   Modeling the response of water quality in the Seine river estuary to human activity in its watershed over the last 50 years [J].
Billen, G ;
Garnier, J ;
Ficht, A ;
Cun, C .
ESTUARIES, 2001, 24 (6B) :977-993
[4]   ALGAL CAROTENOIDS .39. PHAEOCYSTIS SP CLONE 677-3 - A TROPICAL MARINE PLANKTONIC PRYMNESIOPHYTE WITH FUCOXANTHIN AND 19'-ACYLOXYFUCOXANTHINS AS CHEMOSYSTEMATIC CAROTENOID MARKERS [J].
BJORNLAND, T ;
GUILLARD, RRL ;
LIAAENJENSEN, S .
BIOCHEMICAL SYSTEMATICS AND ECOLOGY, 1988, 16 (05) :445-452
[5]   Distribution and air-water exchange of carbon dioxide in the Scheldt plume off the Belgian coast [J].
Borges, AV ;
Frankignoulle, M .
BIOGEOCHEMISTRY, 2002, 59 (1-2) :41-67
[6]   Annual variations of phytoplankton biomass in the Eastern English Channel: comparison by pigment signatures and microscopic counts [J].
Breton, E ;
Brunet, C ;
Sautour, B ;
Brylinski, JM .
JOURNAL OF PLANKTON RESEARCH, 2000, 22 (08) :1423-1440
[7]   Phytoplankton dynamics during the spring bloom in the South-eastern English Channel [J].
Brunet, C ;
Brylinski, JM ;
Bodineau, L ;
Thoumelin, G ;
Bentley, D ;
Hilde, D .
ESTUARINE COASTAL AND SHELF SCIENCE, 1996, 43 (04) :469-483
[8]   Phytoplankton in the Marsdiep at the end of the 20th century;: 30 years monitoring biomass, primary production, and Phaeocystis blooms [J].
Cadée, GC ;
Hegeman, J .
JOURNAL OF SEA RESEARCH, 2002, 48 (02) :97-110
[9]   Is phytoplankton growth in the Wadden Sea light or nitrogen limited? [J].
Colijn, F ;
Cadée, GC .
JOURNAL OF SEA RESEARCH, 2003, 49 (02) :83-93
[10]   MODIFICATION OF THE BIOGEOCHEMICAL CYCLE OF SILICA WITH EUTROPHICATION [J].
CONLEY, DJ ;
SCHELSKE, CL ;
STOERMER, EF .
MARINE ECOLOGY PROGRESS SERIES, 1993, 101 (1-2) :179-192