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Trophodynamics of selected mesozooplankton in the west-Indian sector of the Polar Frontal Zone, Southern Ocean

机译:南大洋极地锋带西印度洋部分中层浮游动物的对流动力学

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Mesozooplankton community structure and grazing impact were investigated at 15 stations in the west-Indian sector of the Polar Frontal Zone during the third dynamics of Eddie impacts on Marion's ecosystem cruise, conducted during April 2004. An intense frontal feature, likely the convergence of the Sub-Antarctic and Antarctic Polar Fronts, was identified running in a north-eastward direction across the survey area. Total integrated chlorophyll-a (chl-a) biomass ranged from 4.15 mg m(-2) to 22.81 mg m(-2) and was dominated by picophytoplankton at all stations. Mesozooplankton abundances ranged from 163.84 ind m(-2) to 2,478.08 ind m(-2) and biomass between 6.70 mg Dwt. m(-2) and 23.40 mg Dwt. m(-2). The mesozooplankton community was dominated almost entirely by copepods, which contributed between 35% and 79% (mean=63%; SD=+/- 12%) of the total numbers. The pteropoda, Limacina retroversa, contributed up to 30% (mean=10%; SD=+/- 8%) of the total numbers. Numerical analysis identified two distinct mesozooplankton communities separated by the intense frontal feature, namely the Antarctic and the Sub-Antarctic Zone Groups. Ingestion rates of the four numerically dominant copepod species (Calanus simillimus, Clausocalanus spp., Ctenocalanus spp. and Oithona similis) and the pteropod, L. retroversa, were estimated using the gut fluorescence technique. Total grazing impact ranged from 0.156 mg (pigm) m(-2) to 2.958 mg (pigm) m(-2) or between 1% and 29% of the available chl-a per day. The four copepods contributed approximately 36% of the total daily grazing impact, while the pteropod contributed to a mean of 64%, indicating that this zooplankton group may play an important role in the Southern Ocean carbon cycle. In general, the highest daily grazing impact was exhibited in the Antarctic Zone Group (mean=12% phytoplankton standing stock per day).
机译:在2004年4月进行的埃迪对马里恩生态系统巡航的第三次动力学过程中,对极地额叶带西印度部分的15个站点的Mesozooplankton群落结构和放牧影响进行了调查。强烈的额叶特征,可能是亚热带的融合-南极和南极极地线被确定为在整个调查区域内向东北方向延伸。总的综合叶绿素-a(chl-a)生物量范围从4.15 mg m(-2)到22.81 mg m(-2),并且在所有站点上都以浮游植物为主。中型浮游生物的丰度范围为163.84 ind m(-2)至2,478.08 ind m(-2),生物量在6.70 mg Dwt之间。 m(-2)和23.40 mg Dwt。 m(-2)。中型浮游动物群落几乎完全被co足类动物所占据,co足类动物占总数的35%至79%(平均= 63%; SD = + /-12%)。翼足类(Limacina retroversa)占总数的30%(平均= 10%; SD = + /-8%)。数值分析确定了由强烈的锋面特征隔开的两个不同的中生浮游动物群落,即南极和亚南极带。使用肠道荧光技术估算了四种数值上占优势的co足类动物(Calanus simillimus,Clausocalanus spp。,Ctenocalanus spp。和Oithona similis)和翼足类L. retroversa的摄食率。总放牧影响范围为0.156 mg(pigm)m(-2)至2.958 mg(pigm)m(-2)或每天可用chl-a的1%至29%。四个co足类动物贡献了约36%的每日总放牧影响,而翼足类动物贡献了平均64%,表明该浮游动物可能在南大洋碳循环中发挥重要作用。一般而言,南极区域组的放牧影响最大(平均=每天浮游植物种群占12%)。

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