Phytoplankton biomass, production and potential export in the North Water

被引:89
作者
Klein, B [1 ]
LeBlanc, B
Mei, ZP
Beret, R
Michaud, J
Mundy, CJ
von Quillfeldt, CH
Garneau, ME
Roy, S
Gratton, Y
Cochran, JK
Bélanger, S
Larouche, P
Pakulski, JD
Rivkin, RB
Legendre, L
机构
[1] Univ Laval, Dept Biol, GRIOQ, Quebec City, PQ G1K 7P4, Canada
[2] Mem Univ Newfoundland, Ctr Ocean Sci, St Johns, NF A1C 5S7, Canada
[3] Minist Peches & Oceans, Inst Maurice Lamontagne, Mont Joli, PQ G5H 3Z4, Canada
[4] SUNY Stony Brook, Marine Sci Res Ctr, Stony Brook, NY 11794 USA
[5] INRS, ETE, St Foy, PQ G1V 4C7, Canada
[6] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada
[7] Norwegian Polar Res Inst, Tromso, Norway
[8] Univ Manitoba, Dept Geog, Ctr Earth Observat Sci, Winnipeg, MB R3T 2N2, Canada
基金
美国国家科学基金会; 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(02)00174-1
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The seasonal patterns of phytoplankton biomass and production were determined in the North Water, located between Greenland and Ellesmere Island (Canadian Arctic), in August 1997, April-July 1998, and August-September 1999. The patterns differed among the four defined regions of this large polynya, i.e. North (> 77.5degreesN), East (> 75degreesW), West (< 75degreesW), and South (< 76degreesN). Phytoplankton biomass and production were low during April throughout the North Water. Biomass first increased in the East during April. From there, the biomass spread north- and westwards during May-June, when the bloom culminated (chlorophyll a concentrations up to 19.8 mg m(-3)). The large-sized (> 5 mum) fraction dominated the biomass and production during the bloom. During July, August, and September, biomass and production decreased over the whole region, with the highest biomass, dominated by large cells, occurring in the North. The annual particulate and dissolved phytoplankton production were the highest ever reported for the high Arctic, reaching maximum values of 254 and 123 g C m(-2) yr(-1), respectively, in the East. Rates in the North and West were considerably lower than in the East (ca. two- and three-fold, respectively). The f-ratios (i.e. ratio of new to total production), derived from the size structure of phytoplankton, were high north of 76degreesN (0.4-0.7). Regionally, this indicated a high potential export of particulate organic carbon (Epoc) from the phytoplankton community to other trophic compartments and/or downwards in the East (15 5 g C m-2 yr-1), with lower values in the North and West (i.e. 77 and 42 g C m(-2) yr(-1), respectively). The seasonal and spatial patterns of Epoc were consistent with independent estimates of potential carbon export. Phytoplankton biomass and production were generally dominated by the large size fraction, whereas Epoc seemed to be dominated,by the large size fraction early in the season and by the small size fraction (< 5 mum) from June until the end of the growing season. (C) 2002 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:4983 / 5002
页数:20
相关论文
共 36 条
[1]  
BACLE J, 2000, THESIS MCGILLL U
[2]  
BELANGER S, 2000, ANAL SPATIO TEMPOREL
[3]  
BELANGER S, 2002, UNPUB J GEOPHYSICAL
[4]   PHYTOPLANKTON EXUDATION OF ORGANIC-MATTER - WHY DO HEALTHY CELLS DO IT [J].
BJORNSEN, PK .
LIMNOLOGY AND OCEANOGRAPHY, 1988, 33 (01) :151-154
[5]   INCREASED PHYTOPLANKTON PRIMARY PRODUCTION IN THE MARSDIEP AREA (WESTERN DUTCH WADDEN SEA) [J].
CADEE, GC .
NETHERLANDS JOURNAL OF SEA RESEARCH, 1986, 20 (2-3) :285-290
[6]   Nutrients, primary production and microbial heterotrophy in the southeastern Chukchi Sea: Arctic summer nutrient depletion and heterotrophy [J].
Cota, GF ;
Pomeroy, LR ;
Harrison, WG ;
Jones, EP ;
Peters, F ;
Sheldon, WM ;
Weingartner, TR .
MARINE ECOLOGY PROGRESS SERIES, 1996, 135 (1-3) :247-258
[7]  
de Lafontaine Y., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P99
[8]   UPTAKE OF NEW AND REGENERATED FORMS OF NITROGEN IN PRIMARY PRODUCTIVITY [J].
DUGDALE, RC ;
GOERING, JJ .
LIMNOLOGY AND OCEANOGRAPHY, 1967, 12 (02) :196-&
[9]   PARTICULATE ORGANIC-MATTER FLUX AND PLANKTONIC NEW PRODUCTION IN THE DEEP OCEAN [J].
EPPLEY, RW ;
PETERSON, BJ .
NATURE, 1979, 282 (5740) :677-680
[10]  
GOSSELIN M, 1997, DEEP-SEA RES, V44, P163