Effects of flow and fine sediment dynamics on the turnover of stream invertebrate assemblages

Cristina Buendia, Chris N. Gibbins, Damia Vericat, Ramon J. Batalla

Research output: Contribution to journalArticlepeer-review

46 Citations (Scopus)


Interactions between flow regime, sediment dynamics and benthic invertebrates have seldom been studied in rivers experiencing naturally high suspended sediment loads. This paper examines invertebrate responses to hydrological and sedimentary processes over an annual cycle in a morphologically heterogeneous reach of a river that receives large volumes of fine sediment. Flow regime and sedimentary conditions showed a marked seasonal pattern, with fine sediment accumulating during low flows and after small flood events and not being removed until the large floods that occurred in autumn. The magnitude of sediment accumulation differed between habitats (e.g. being greater in pools than in riffles). The turnover in invertebrate assemblages, measured as beta diversity, was greatest in winter and decreased during summer as deposited fine sediment accumulated across the reach, suggesting that observed patterns of turnover were influenced by seasonal and habitat-specific rates of sedimentation. Some of the spatial and temporal patterns in invertebrate assemblages were subtle, complex and difficult to interpret, but co-inertia analysis indicated an overriding influence of low flows and associated sedimentation on their composition. Floods capable of entraining coarser bed material, along with smaller events accompanied by extensive mobilization of fine sediment, also influenced assemblages and resulted in immediate changes to assemblage composition and abundance. Assemblages appeared to exhibit resilience over the timescale of the study, with similar assemblages found at the beginning and at the end of the study period. Copyright © 2013 John Wiley & Sons, Ltd.
Original languageEnglish
Pages (from-to)1105-1123
Number of pages19
Issue number4
Early online date23 Oct 2013
Publication statusPublished - Aug 2014

Bibliographical note

The authors would like to thank the members of the RIUS team (Fluvial Dynamics Research Group, University of Lleida, www.fluvialdynamics.com) for the valuable help during fieldwork. The third author has a Ramon y Cajal Fellowship (RYC‐2010‐06264) funded by the Spanish Ministry of Science and Innovation. Special thanks are due to the Ebro Water Authorities for issuing permissions to install the equipment and carry out field campaigns. Part of this work has been undertaken within the framework of the research project Consolider Ingenio 2010 CSD2009‐00065 funded by the Spanish Ministry of Economy and Competitiveness.


  • fine sediment
  • beta-diversity
  • floods
  • low flows


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