Seasonal phytoplankton development and new production in the central Greenland Sea

被引:50
作者
Rey, F [1 ]
Noji, TT [1 ]
Miller, LA [1 ]
机构
[1] Inst Marine Res, N-5817 Bergen, Norway
来源
SARSIA | 2000年 / 85卷 / 04期
关键词
new production; nutrients; phytoplankton; carbon cycle; Greenland Sea;
D O I
10.1080/00364827.2000.10414584
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The seasonal development of the phytoplankton in the central Greenland Sea, based on sampling at different time intervals in the period 1993-1995, is consistent with patterns observed in adjacent similar regions. Phytoplankton growth started in early May and developed gradually through May reaching a peak in early June. The spring phytoplankton was mainly composed of diatoms and the prymnesiophyte Phaeocystis pouchetii. Spring primary production rates, its determined by the radioactive carbon method, averaged 752 mg C m(-2) d(-1) during May and June. The summer situation was characterised by strong stratification and an upper mixed layer of about 30 metres that became completely depleted of nutrients and contained low phytoplankton biomass by August. New production in the growing season from May to August, estimated from the total production and published f-ratios was 52 g C m(-2), while new production estimated from the disappearance of nitrate in the same period, along a transect across the central Greenland Sea, was 62 g C m(-2). These results are in good agreement with those from previous investigations and provides the basis for an assessment of the role of biology on the carbon cycling in the central Greenrand Sea when discussed in relation to the inorganic carbon cycling and related biological processes in the area.
引用
收藏
页码:329 / 344
页数:16
相关论文
共 28 条
[1]   REDFIELD RATIOS OF REMINERALIZATION DETERMINED BY NUTRIENT DATA-ANALYSIS [J].
ANDERSON, LA ;
SARMIENTO, JL .
GLOBAL BIOGEOCHEMICAL CYCLES, 1994, 8 (01) :65-80
[2]   Flux of particulate matter through copepods in the Northeast Water Polynya [J].
Daly, KL .
JOURNAL OF MARINE SYSTEMS, 1997, 10 (1-4) :319-342
[3]   UPTAKE OF NEW AND REGENERATED FORMS OF NITROGEN IN PRIMARY PRODUCTIVITY [J].
DUGDALE, RC ;
GOERING, JJ .
LIMNOLOGY AND OCEANOGRAPHY, 1967, 12 (02) :196-&
[4]  
EHRHARDT M, 1983, METHODS SEAWATER ANA, P267
[5]  
FOYN L, 1981, FISKEN HAVET B, V4, P1
[6]   NEW SPECTROPHOTOMETRIC EQUATIONS FOR DETERMINING CHLOROPHYLLS A, B, C1 AND C2 IN HIGHER-PLANTS, ALGAE AND NATURAL PHYTOPLANKTON [J].
JEFFREY, SW ;
HUMPHREY, GF .
BIOCHEMIE UND PHYSIOLOGIE DER PFLANZEN, 1975, 167 (02) :191-194
[7]   OCEANOGRAPHIC CONDITIONS IN THE MARGINAL ICE-ZONE NORTH OF SVALBARD IN EARLY FALL 1979 WITH AN EMPHASIS ON MESOSCALE PROCESSES [J].
JOHANNESSEN, OM ;
JOHANNESSEN, JA ;
MORISON, J ;
FARRELLY, BA ;
SVENDSEN, EAS .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1983, 88 (NC5) :2755-2769
[8]  
KEENE NK, 1991, POLAR BIOL, V11, P219
[9]   NITROGEN CYCLING IN THE BARENTS SEA - SEASONAL DYNAMICS OF NEW AND REGENERATED PRODUCTION IN THE MARGINAL ICE-ZONE [J].
KRISTIANSEN, S ;
FARBROT, T ;
WHEELER, PA .
LIMNOLOGY AND OCEANOGRAPHY, 1994, 39 (07) :1630-1642
[10]   ENVIRONMENTAL-CONTROL AND POTENTIAL FATE OF SIZE-FRACTIONATED PHYTOPLANKTON PRODUCTION IN THE GREENLAND SEA (75-DEGREES-N) [J].
LEGENDRE, L ;
GOSSELIN, M ;
HIRCHE, HJ ;
KATTNER, G ;
ROSENBERG, G .
MARINE ECOLOGY PROGRESS SERIES, 1993, 98 (03) :297-313