Bacterial growth in experimental plankton assemblages and seawater cultures from the Phaeocystis antarctica bloom in the Ross Sea, Antarctica

被引:49
作者
Ducklow, H
Carlson, C
Smith, W
机构
[1] Coll William & Mary, Virginia Inst Marine Sci, Gloucester Point, VA 23062 USA
[2] Bermuda Biol Stn Res, Ferry Reach GE01, St Georges, Bermuda
关键词
bacterioplankton; microbial foodweb; carbon cycle; Antarctica; Phaeocystis;
D O I
10.3354/ame019215
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
A series of seawater culture experiments was carried out during the Phaeocystis antarctica bloom in the Ross Sea polynya (76.5 degrees S, 180 degrees W; November to December 1994 and December 1995 to January 1996) to examine bacterioplankton growth and derive empirical factors for estimating bacterial production rates. Bacterial growth was exponential over 3 to 10 d in all experiments, at rates of ca 0.1 to 0.7 d(-1), even in persistently cold waters (-2 to + 1 degrees C). Growth rates were lower in the early part of the bloom (early to mid-November) and highest during the period of peak primary productivity (2 to 4 g C m(-2) d(-1) in late November through December). Apparent lag phases in the growth curves lasting 1 to 7 d could be accounted for mathematically by subpopulations in the bacterial assemblages growing exponentially at different rates, with no need to invoke inactive, nondividing or nonviable populations. Lags were absent during the period of peak primary production, suggesting adaptation of the bacteria to ambient DOM. Growth was not stimulated by small temperature increases (Delta+2 to 4 degrees C), and was not balanced by removal processes in untreated 'whole' water samples. Growth rates were broadly similar to other directly observed bacterial growth rates in the Antarctic and did not appear to differ from rates in warmer waters. Conversion factors for thymidine and leucine averaged 8 and 0.8 x 10(17) cells mol(-1), respectively, not dissimilar to estimates from temperate waters. These findings suggest that bacteria were growing actively in 0 to -2 degrees C waters under rich bloom conditions, and lend strong sup port to the hypothesis that bacterioplankton metabolism controls DOC accumulation in Antarctic waters, at least at the low rates of DOM supply we infer from field and experimental observations. Bacterioplankton responded within 10 to 20 d to the evolving P. antarctica bloom and did not appear to behave substantially differently from lower latitude bloom systems.
引用
收藏
页码:215 / 227
页数:13
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