Food webs and carbon flux in the Barents Sea

被引:366
作者
Wassmann, Paul [1 ]
Reigstad, Marit
Haug, Tore
Rudels, Bert
Carroll, Michael L.
Hop, Haakon
Gabrielsen, Geir Wing
Falk-Petersen, Stig
Denisenko, Stanislav G.
Arashkevich, Elena
Slagstad, Dag
Pavlova, Olga
机构
[1] Univ Tromso, Norwegian Coll Fishery Sci, N-9037 Tromso, Norway
[2] Inst Marine Res, Tromso Branch, N-9294 Tromso, Norway
[3] Inst Marine Res, FI-00561 Helsinki, Finland
[4] Norwegian Polar Res Inst, N-9296 Tromso, Norway
[5] Akvaplan Niva, N-9296 Tromso, Norway
[6] Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow 117851, Russia
[7] Russian Acad Sci, Inst Zool, St Petersburg 199034, Russia
[8] SINTEF Fisheries & Aquaculture, N-7465 Trondheim, Norway
关键词
D O I
10.1016/j.pocean.2006.10.003
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Within the framework of the physical forcing, we describe and quantify the key ecosystem components and basic food web structure of the Barents Sea. Emphasis is given to the energy flow through the ecosystem from an end-to-end perspective, i.e. from bacteria, through phytoplankton and zooplankton to fish, mammals and birds. Primary production in the Barents is on average 93 g C m(-2) y(-1), but interannually highly variable (19%), responding to climate variability and change (e.g. variations in Atlantic Water inflow, the position of the ice edge and low-pressure pathways). The traditional focus upon large phytoplankton cells in polar regions seems less adequate in the Barents, as the cell carbon in the pelagic is most often dominated by small cells that are entangled in an efficient microbial loop that appears to be well coupled to the grazing food web. Primary production in the ice-covered waters of the Barents is clearly dominated by planktonic algae and the supply of ice biota by local production or advection is small. The pelagic-benthic coupling is strong, in particular in the marginal ice zone. In total 80% of the harvestable production is channelled through the deep-water communities and benthos. 19% of the harvestable production is grazed by the dominating copepods Calanus finmarchicus and C. glacialis in Atlantic or Arctic Water, respectively. These two species, in addition to capelin (Mallotus villosus) and herring (Clupea harengus), are the keystone organisms in the Barents that create the basis for the rich assemblage of higher trophic level organisms, facilitating one of the worlds largest fisheries (capelin, cod, shrimps, seals and whales). Less than 1% of the harvestable production is channelled through the most dominating higher trophic levels such as cod, harp seals, minke whales and sea birds. Atlantic cod, seals, whales, birds and man compete for harvestable energy with similar shares. Climate variability and change, differences in recruitment, variable resource availability, harvesting restrictions and management schemes will influence the resource exploitation between these competitors, that basically depend upon the efficient energy transfer from primary production to highly successful, lipid-rich zooplankton and pelagic fishes. (c) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:232 / 287
页数:56
相关论文
共 306 条
[1]   TOWARD NEW MASS AND HEAT BUDGETS FOR ARCTIC OCEAN [J].
AAGAARD, K ;
GREISMAN, P .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS AND ATMOSPHERES, 1975, 80 (27) :3821-3827
[2]  
AAREFJORD H, 1995, DIET HARBOUR PORPOIS, P211
[3]  
*ACIA, 2001, REP ARCT CLIM IMP AS
[4]   A STUDY OF THE CLIMATIC SYSTEM IN THE BARENTS SEA [J].
ADLANDSVIK, B ;
LOENG, H .
POLAR RESEARCH, 1991, 10 (01) :45-49
[5]  
AJIAD AM, 1990, INT COUNC EXPL SEA C
[6]   MODELING THE SIGNIFICANCE OF ZOOPLANKTON GRAZING FOR EXPORT PRODUCTION [J].
AKSNES, DL ;
WASSMANN, P .
LIMNOLOGY AND OCEANOGRAPHY, 1993, 38 (05) :978-985
[7]   The sub-ice algal community in the Chukchi sea: large- and small-scale patterns of abundance based on images from a remotely operated vehicle [J].
Ambrose, WG ;
von Quillfeldt, C ;
Clough, LM ;
Tilney, PVR ;
Tucker, T .
POLAR BIOLOGY, 2005, 28 (10) :784-795
[8]   Variation in Serripes groenlandicus (Bivalvia) growth in a Norwegian high-Arctic fjord:: evidence for local- and large-scale climatic forcing [J].
Ambrose, William G., Jr. ;
Carroll, Michael L. ;
Greenacre, Michael ;
Thorrold, Simon R. ;
McMahon, Kelton W. .
GLOBAL CHANGE BIOLOGY, 2006, 12 (09) :1595-1607
[9]   A highly unstable Holocene climate in the subpolar North Atlantic:: evidence from diatoms [J].
Andersen, C ;
Koç, N ;
Moros, M .
QUATERNARY SCIENCE REVIEWS, 2004, 23 (20-22) :2155-2166
[10]   NUTRIENT REGENERATION IN COLD, HIGH SALINITY BOTTOM WATER OF THE ARCTIC SHELVES [J].
ANDERSON, LG ;
JONES, EP ;
LINDEGREN, R ;
RUDELS, B ;
SEHLSTEDT, PI .
CONTINENTAL SHELF RESEARCH, 1988, 8 (12) :1345-1355