...
首页> 外文期刊>Hydrobiologia >Intra-habitat heterogeneity of microbial food web structure under the regime of eutrophication and sediment resuspension in the large subtropical shallow Lake Taihu, China.
【24h】

Intra-habitat heterogeneity of microbial food web structure under the regime of eutrophication and sediment resuspension in the large subtropical shallow Lake Taihu, China.

机译:大型亚热带浅水太湖富营养化和沉积物悬浮状态下微生物食物网结构的栖息地内异质性。

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Planktonic microbial community structure and classical food web were investigated in the large shallow eutrophic Lake Taihu (2338 km2, mean depth 1.9 m) located in subtropical Southeast China. The water column of the lake was sampled biweekly at two sites located 22 km apart over a period of twelve month. Site 1 is under the regime of heavy eutrophication while Site 2 is governed by wind-driven sediment resuspension. Within-lake comparison indicates that phosphorus enrichment resulted in increased abundance of microbial components. However, the coupling between total phosphorus and abundance of microbial components was different between the two sites. Much stronger coupling was observed at Site 1 than at Site 2. The weak coupling at Site 2 was mainly caused by strong sediment resuspension, which limited growth of phytoplankton and, consequently, growth of bacterioplankton and other microbial components. High percentages of attached bacteria, which were strongly correlated with the biomass of phytoplankton, especially Microcystis spp., were found at Site 1 during summer and early autumn, but no such correlation was observed at Site 2. This potentially leads to differences in carbon flow through microbial food web at different locations. Overall, significant heterogeneity of microbial food web structure between the two sites was observed. Site-specific differences in nutrient enrichment (i.e. nitrogen and phosphorus) and sediment resuspension were identified as driving forces of the observed intra-habitat differences in food web structure..
机译:在中国亚热带东南部的大型浅水富营养化太湖(2338 km2,平均深度1.9 m)中研究了浮游生物微生物群落结构和经典食物网。在十二个月的时间内,每两周在相距22 km的两个地点对湖水柱进行采样。站点1处于严重富营养化状态,而站点2则由风驱动的沉积物重悬控制。湖内比较表明磷富集导致微生物组分丰度增加。但是,两个部位之间的总磷和微生物成分的丰度之间的耦合是不同的。在站点1处观测到的耦合比在站点2处强得多。在站点2处弱耦合主要是由于强烈的沉积物再悬浮所致,这限制了浮游植物的生长,进而限制了浮游细菌和其他微生物成分的生长。在夏季和初秋期间,在站点1发现高比例的附着细菌,这些细菌与浮游植物的生物量(尤其是微囊藻属)密切相关,但在站点2没有发现这种相关性。这可能导致碳流量差异通过不同位置的微生物食物网。总体而言,观察到两个地点之间微生物食物网结构的显着异质性。养分富集(即氮和磷)和沉积物再悬浮的特定地点差异被确定为食物网结构中观察到的栖息地差异的驱动力。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号