4.1 Article

Influence of stream-floodplain biogeochemical linkages on aquatic foodweb structure along a gradient of stream size in a tropical catchment

期刊

FRESHWATER SCIENCE
卷 32, 期 1, 页码 217-229

出版社

UNIV CHICAGO PRESS
DOI: 10.1899/11-117.1

关键词

biogeochemical linkages; floodplain; food web structure; carbon; stable isotopes; specific ultraviolet absorbance; flood pulse; Kimberley

资金

  1. Australian Government's Commonwealth Environment Research Facilities initiative
  2. Australian Government's Raising National Water Standards Program
  3. Fisheries Research and Development Corporation
  4. Queensland Government's Smart State Innovation Fund

向作者/读者索取更多资源

We measured nutrients and dissolved organic matter (DOM) in surface water and floodplain sediments to evaluate biogeochemical linkages between streams and floodplairts in 3 streams of increasing size in a tropical catchment in northwestern Australia. We hypothesized that stream-floodplain biogeochemical connectivity, measured as similar DOM concentrations and spectroscopic properties of streamwater and floodplain sediment leachate, would decrease with increasing stream size. We expected decreasing connectivity to shift support of aquatic foodweb structure from mainly allochthonous C in small streams to algal C in larger streams. Streamwater and sediment leachate concentrations of NH4-N, NO3-N, soluble reactive P. and DOM varied several-fold across the 3 sites but showed no strong pattern in stream-floodplain connectivity with increasing stream size. Fluorescence index, specific ultraviolet absorbance, and delta C-13-dissolved organic C (DOC) for stream water and sediment leachate were most similar to each other at the mid-size Adcock River, indicating tight river-floodplain biogeochemical connectivity via input of allochthonous DOM and NH4-N to stream water. delta C-13 and delta N-15 signatures for key producers and consumers for all 3 streams showed that invertebrate consumers probably were supported by a range of in-stream (e.g., benthic and filamentous algae) and floodplain (allochthonous leaf litter) sources, whereas fish strongly reflected delta C-13-enriched sources (e.g., benthic algae). Allochthonous C was probably only a minor energy source for metazoa, but we propose that river-floodplain biogeochemical linkages may be important for other aspects of ecosystem productivity, such as input of inorganic nutrients to support in-stream primary production. Terrestrial-aquatic biogeochemical linkages may be critical but poorly quantified components of river-floodplain ecosystems.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.1
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据