Uncoupling of bacteria and phytoplankton during the austral spring bloom in Gerlache Strait, Antarctic Peninsula

被引:77
作者
Bird, DF
Karl, DM
机构
[1] Univ Quebec, Dept Sci Biol, Montreal, PQ H3C 3P8, Canada
[2] Univ Hawaii, Sch Ocean & Earth Sci & Technol, Honolulu, HI 96822 USA
关键词
bacteria; Antarctic Peninsula; Gerlache Strait; spring bloom; heterotrophic nanoflagellates; microbial food web; grazing; heterotrophic dinoflagellates;
D O I
10.3354/ame019013
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The response of the bacterial (Bacteria and Archaea) community to vernal phytoplankton blooms was examined over a grid of stations in Gerlache Strait, Antarctic Peninsula, during the RACER II program (29 October to 26 November 1989). Total bacterial production (0.13 to 10.6 mg C m(-3) d(-1)). based on the incorporation of H-3-leucine into protein, increased with increasing chlorophyll a (chl a) concentration. Bacterial cell-specific growth rate also increased with increasing primary production among stations. Nevertheless, bacterial cell abundance was greatest at the sites that had the lowest chi a concentrations, and declined wherever phytoplankton bloomed. Early bloom communities had few nanoprotist grazers; grazing was undetectable by the Landry-Hassett dilution method during this period. Fully developed bloom communities (chl a > 10 mg m(-3)) had a profusion of nanoprotist grazers (median 3000 cells ml(-1)). Despite relatively low ingestion rates per individual (0.9 bacteria cell(-1) h(-1)), the abundant grazing community kept bacterial biomass very low in Gerlache Strait, to the point that the metabolism of the pelagic bacterial surface community was only a minor fraction of total ecosystem metabolism. Grazing was the apparent cause, although biomass limitation of the bacteria due to lack of resources (e.g. bioavailable dissolved organic matter) may be the ultimate cause of the uncoupling of bacterial and phytoplanktonic communities in these habitats.
引用
收藏
页码:13 / 27
页数:15
相关论文
共 98 条
[91]   SIGNIFICANCE OF BACTERIAL BIOMASS IN LAKES AND THE OCEAN - COMPARISON TO PHYTOPLANKTON BIOMASS AND BIOGEOCHEMICAL IMPLICATIONS [J].
SIMON, M ;
CHO, BC ;
AZAM, F .
MARINE ECOLOGY PROGRESS SERIES, 1992, 86 (02) :103-110
[92]   LUCIFER DYES - HIGHLY FLUORESCENT DYES FOR BIOLOGICAL TRACING [J].
STEWART, WW .
NATURE, 1981, 292 (5818) :17-21
[93]   Predator regulation of aquatic microbial abundance in simple food webs of sub-Antarctic lakes [J].
Tranvik, LJ ;
Hansson, LA .
OIKOS, 1997, 79 (02) :347-356
[94]  
VENRET M, 1990, ANTARCT J US, V25, P164
[95]   DETERMINATION OF BACTERIAL NUMBER AND BIOMASS IN MARINE-ENVIRONMENT [J].
WATSON, SW ;
NOVITSKY, TJ ;
QUINBY, HL ;
VALOIS, FW .
APPLIED AND ENVIRONMENTAL MICROBIOLOGY, 1977, 33 (04) :940-946
[96]   IRON IN THE WATER COLUMN OF THE WEDDELL SEA [J].
WESTERLUND, S ;
OHMAN, P .
MARINE CHEMISTRY, 1991, 35 (1-4) :199-217
[97]   Nutrients, organic carbon and organic nitrogen in the upper water column of the Arctic Ocean: implications for the sources of dissolved organic carbon [J].
Wheeler, PA ;
Watkins, JM ;
Hansing, RL .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 1997, 44 (08) :1571-+
[98]  
[No title captured]