Export of biogenic carbon and structure and dynamics of the pelagic food web in the Gulf of St. Lawrence Part 1.: Seasonal variations

被引:28
作者
Savenkoff, C [1 ]
Vézina, AF
Roy, S
Klein, B
Lovejoy, C
Therriault, JC
Legendre, L
Rivkin, R
Bérubé, C
Tremblay, JÉ
Silverberg, N
机构
[1] Fisheries & Oceans Canada, Maurice Lamontagne Inst, Div Ocean Sci, Mt Joli, PQ G5H 3Z4, Canada
[2] Inst Natl Rech Sci Oceanol, Rimouski, PQ G5L 3A1, Canada
[3] Univ Laval, GIROQ, Quebec City, PQ G1K 7P4, Canada
[4] Mem Univ Newfoundland, Ctr Ocean Sci, St Johns, NF A1C 5S7, Canada
[5] Univ Quebec, Ctr Oceanog, Rimouski, PQ G5L 3A1, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
D O I
10.1016/S0967-0645(99)00119-8
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The seasonal changes in photosynthetic production, respiration, sinking flux of organic carbon, and food web structure are described in the Gulf of St. Lawrence over a two-year period during the Canadian Joint Global Ocean Flux Study (JGOFS) program. The results show contrasts in net metabolism between periods of low (winter and spring) and high (summer and fall) vertical stability. The winter-spring period was associated with an autotrophic pelagic food web: predominance of large phytoplankton cells, large zooplankton, and high herbivorous potential transfers towards the zooplankton. The stratified summer-fall period was associated with a heterotrophic food web: dominance of small phytoplankton cells, replacement of the size class occupied by large phytoplankton with large heterotrophic dinoflagellates and ciliates, smaller zooplankton, and dominance of omnivorous transfers towards the zooplankton, Despite differences in algal size and composition as well as in size structure of the trophic compartments between winter-spring and summer-fall, the particulate organic carbon fluxes observed at 50 m depth was quantitatively similar during these two periods. Even though winter photosynthetic production was relatively low, the high chlorophyll a concentration, the size structure of the trophic compartments, and the high contribution of large phytoplankton cells (mainly diatoms) to biological activity were similar to those observed during the spring and could explain the high heterotrophic biomass observed during winter. Crown copyright (C) 1999 Published by Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:585 / 607
页数:23
相关论文
共 52 条
[1]  
AHMED S I, 1976, Marine Chemistry, V4, P133, DOI 10.1016/0304-4203(76)90002-5
[2]  
Aminot A., 1983, CNEXO BREST, P119
[3]  
Andersen P., 1988, Advances in Limnology, V31, P243
[4]  
[Anonymous], ADV MICROB ECOL
[5]   THE RELATIONSHIP BETWEEN COMMUNITY RESPIRATION AND ETS ACTIVITY IN THE OCEAN [J].
ARISTEGUI, J ;
MONTERO, MF .
JOURNAL OF PLANKTON RESEARCH, 1995, 17 (07) :1563-1571
[6]  
BERUBE C, 1996, THESIS U QUEBEC RIMO
[7]   BIOGEOCHEMICAL SIGNIFICANCE OF BACTERIAL BIOMASS IN THE OCEANS EUPHOTIC ZONE [J].
CHO, BC ;
AZAM, F .
MARINE ECOLOGY PROGRESS SERIES, 1990, 63 (2-3) :253-259
[8]  
DASILVA NML, 1991, THESIS U P M CURIE P
[9]  
de Lafontaine Y., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P99
[10]  
DELGIORGIO PA, 1992, J PLANKTON RES, V14, P1723