Zooplankton response to a phytoplankton bloom near South Georgia, Antarctica

被引:85
作者
Atkinson, A
Shreeve, RS
Pakhomov, EA
Priddle, J
Blight, SP
Ward, P
机构
[1] British Antarctic Survey, Natural Environment Research Council, Cambridge CB3 OET, High Cross, Madingley Road
[2] Southern Ocean Group, Department of Zoology and Entomology, Rhodes University, Grahamstown 6140
关键词
Southern Ocean; zooplankton; copepods; feeding rates; diets; diatom bloom;
D O I
10.3354/meps144195
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
A shelf site near the island of South Georgia was sampled during a spring bloom in January 1994. Chlorophyll a (chi a) values declined from 19 to 6 mg m(-3) during the 8 d of sampling. The bloom comprised mainly long pennate diatoms and large colonies of centric diatoms; a 200 mu m sieve retained over two-thirds of the chi a. Mesozooplankton biomass was high, 12.3 g dry mass m(-2) within the top 200 m, and comprised mainly copepods. A series of Longhurst Hardy Plankton Recorder profiles showed that the numerical dominants (Oithona similis, Drepanopus forcipatus and pteropods) resided mainly within the top 20 m, whereas the large, biomass-dominant copepods had secondary maxima rather deeper within the thermocline. Diel vertical migration was not a feature of this community, being limited to metridiid and euchaetiid copepods. Gut fluorescence measurements on 7 large copepod species showed that all fed during both day and night, although guts tended to be fullest during afternoon and night. About 20% of chi a grazed by these copepods occurred below the mixed layer, thus representing a potentially direct export of carbon from the system via sinking faecal pellets. Algal carbon rations (% body carbon ingested per day) of mixed layer copepods ranged from 3% (Rhincalanus gigas) to 20% (small copepods). With the exception of R. gigas, these values from gut fluorescence agreed with independent estimates from the site following the decline of chi a during incubations in ambient seawater. Despite low clearance sates, ingestion rates (per copepodid) were at the upper end of recorded Antarctic values, suggesting food saturation. Calanoides acutus and R. gigas cleared diatoms (including the highly elongated 0.5 to 1 mm forms) at maximal rates, Metridia spp., Calanus propinquus and small copepods, by contrast, cleared dinoflagellates and ciliates faster than diatoms of similar size. The total mixed layer zooplankton probably removed < 5% of daily primary production and < 5% of protozoan standing stocks per day.
引用
收藏
页码:195 / 210
页数:16
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