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Phytoplankton photosynthesis-irradiance relationships in a large, managed, eutrophic, subtropical lake: The influence of lake stage on ecological homogeneity

机译:大型,有管理,富营养化的亚热带湖泊中浮游植物的光合作用-辐照关系:湖泊阶段对生态均匀性的影响

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Phytoplankton photosynthesis-irradiance curves are routinely generated as part of the long-term plankton monitoring program of a large, eutrophic, subtropical lake (Lake Okeechobee, Florida). Because previous water chemistry and phytoplankton research found the lake to be more heterogeneous under lower lake stage than under higher lake stage conditions, these photosynthesis data were used to investigate whether phytoplankton from four geographically distinct stations exhibited similar photosynthetic behavior during a period of high lake stage as opposed to spatially heterogeneous photosynthetic behavior after a managed recession and drought reduced water depths. Integrated samples were collected February 1997-October 2001 from the four stations. Photosynthesis-irradiance curves (C-14-bicarbonate method) were gen- B erated, leading to mean lake-wide values ( +/-SD) of photosynthetic parameters, (x P-m(B), and E-k, of 0.049 +/- 0.046 mg C (mg Chl-a)(-1) h(-l) (mumol photons m(-2) s(-1))(-1), 7.71 +/- 5.81 mg C (mg Chl-a)(-1) h(-1), and 189 +/- 101 mumol photons m(-2) s(-1), respectively. The parameters did not differ between stations under high lake stage conditions (with one exception), but alpha(B) and P-m(B) differed significantly between stations after the reduction in lake stage, suggesting a shift toward ecological heterogeneity. Variation in photosynthetic parameters was predicted by a different suite of environmental variables for low and high lake stage conditions. These results point to the importance of lake stage to the ecological function of this shallow, subtropical system.
机译:浮游植物的光合作用-辐照度曲线通常作为大型富营养化亚热带湖泊(奥基乔比湖,佛罗里达州)的长期浮游生物监测程序的一部分生成。由于先前的水化学和浮游植物研究发现,在低湖位阶段比高湖位条件下的湖泊具有更高的异质性,因此利用这些光合作用数据来调查来自四个地理上不同站点的浮游植物在高湖位时期是否表现出相似的光合行为。与受控的衰退和干旱减少了水深后的空间异质光合行为相反。 1997年2月至2001年10月从这四个站点收集了综合样本。生成了光合作用-辐照度曲线(C-14-碳酸氢盐法),导致整个湖面的光合参数平均值(+/- SD)(x Pm(B)和Ek为0.049 +/-) 0.046 mg C(mg Chl-a)(-1)h(-l)(mumol光子m(-2)s(-1))(-1),7.71 +/- 5.81 mg C(mg Chl-a) (-1)h(-1)和189 +/- 101 mumol光子m(-2)s(-1)在高湖位条件下,各站的参数没有差异(一个例外),但是湖泊阶段减少后,不同站点之间的α(B)和Pm(B)存在显着差异,这表明向生态异质性转变;通过不同的环境变量组预测了低和高湖泊阶段条件下光合参数的变化。指出了湖台对这种浅亚热带系统生态功能的重要性。

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