Distribution patterns of fish assemblages in an Eastern Mediterranean intermittent river

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Éditeur(s) EDP Sciences
Identifiant documentaire 11-dkey/10.1051/kmae/2015026
Identifiant OAI oai:edpsciences.org:dkey/10.1051/kmae/2015026
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Auteur(s): L. Vardakas,E. Kalogianni,S. Zogaris,N. Koutsikos,T. Vavalidis,D. Koutsoubas,N. Th. Skoulikidis
Mots clés distribution patterns fish assemblages Mediterranean intermittent drought modèles de distribution assemblages de poissons Méditerranée intermittent sécheresse
Date de publication 19/11/2015
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Source https://doi.org/10.1051/kmae/2015026
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The distribution patterns of fish assemblages within streams can provide insights for river type classifications and may warrant specific conservation actions. However, there is limited knowledge of how fish assemblages assort along a longitudinal axis in Mediterranean intermittent streams. Patterns in spatial and temporal distribution of fish communities were analysed in a Mediterranean intermittent river (Evrotas River) located in Southern Greece, hosting three endemic range restricted species of high conservation concern, during the period 2007−2009, with 80% of the river’s total length desiccating in the 2007 and 2008 droughts. The general trend was an increase in fish density and species richness along an upstream-downstream gradient. Fish assemblages from upstream to downstream were characterized by a decrease of the most rheophilic species (Squalius keadicus) and an increase of the most stagnophilic species (Tropidophoxinellus spartiaticus). Three river segments, characterized by a high degree of homogeneity were delineated. Habitat and environmental preferences for the studied fish species were identified, with elevation and low flowing habitats being the most important environmental factors affecting fish distribution patterns. The current study provides evidence that even in an intermittent river an assemblage pattern following a longitudinal gradient can be identified, mainly due to the lack of instream barriers that allows recolonization after flow resumption.

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