2003
DOI: 10.1016/s0075-9511(03)80022-1
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Lotic communities of two small temporary karstic stream systems (East Westphalia, Germany) along a longitudinal gradient of hydrological intermittency

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Cited by 36 publications
(35 citation statements)
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“…Karst spring discharges reflect periods of poor or abundant precipitations due to specific recharge conditions and the locally prevalent climate regime (Bonacci, 2015;Fiorillo et al, 2015). In such conditions streamflow regime is recognized as the principal variable affecting the success and distribution of aquatic biota (Meyer and Meyer, 2000;Meyer et al, 2003;Konrad et al, 2008). Limited knowledge of the effects of temporary seasonal drying of karst springs on stream biota introduces numerous questions when comparing biological integrity of these specific habitats to perennially flowing streams (Reiss and Chifflard, 2015).…”
Section: Introductionmentioning
confidence: 99%
“…Karst spring discharges reflect periods of poor or abundant precipitations due to specific recharge conditions and the locally prevalent climate regime (Bonacci, 2015;Fiorillo et al, 2015). In such conditions streamflow regime is recognized as the principal variable affecting the success and distribution of aquatic biota (Meyer and Meyer, 2000;Meyer et al, 2003;Konrad et al, 2008). Limited knowledge of the effects of temporary seasonal drying of karst springs on stream biota introduces numerous questions when comparing biological integrity of these specific habitats to perennially flowing streams (Reiss and Chifflard, 2015).…”
Section: Introductionmentioning
confidence: 99%
“…Studies in United Kingdom (Smith et al 2003), Switzerland (Ruegg & Robinson 2004), Germany (Meyer et al 2003), Portugal (Aguiar et al 2002), and Algeria (Arab et al 2004), have shown that intermittent streams are typically species-poor compared with nearby perennial streams, whereas studies in Australia (Boulton & Suter 1986) and United States (Dieterich & Anderson 2000) have found that the species diversity in intermittent streams can be as high as in perennial streams. The degree of faunal similarity between intermittent and perennial streams also appears to differ between and within countries.…”
Section: Introductionmentioning
confidence: 99%
“…Destaca-se a importância das dimensões espacial (vertical, longitudinal e lateral) e temporal, devendo serem observadas mudanças físicas, químicas e biológicas, processos hidrológicos e geomorfológicos, ocasionados por fenômenos naturais ou por intervenção humana (Petts 2000;Brown e Pasternack, 2008;Hu et al, 2008). Na dimensão longitudinal do rio, observa-se o conceito de "Contínuo Fluvial" proposto por Vannote et al (1980), bastante citado na literatura eco-hidrológica para ecossistemas em movimento (Meyer, et al, 2003;Ciesielka e Bailey, 2007;Gore, 2007;Jørgensen et al, 2007;Callanan et al, 2008;Boulton et al, 2008;Burcher, 2009), que considera dentre outros aspectos, a contínua mudança nas condições ambientais do fluxo de primeira ordem para ordens superiores, dividindo o rio em três regiões geomorfológicas distintas: região de nascente (alta contribuição terrestre de sedimentos orgânicos), médio curso (mais relacionado com a produção de algas e plantas aquáticas) e proximidade da foz (disposiçãoà turbidez, carga elevada de sedimentos procedentes de montante). Montgomery (1999), no conceito de MEDEIROS, P. C.; SOUZA, F. A. S.; RIBEIRO, M. M. R. Aspectos conceituais sobre o regime hidrológico para a definição do hidrograma ambiental.…”
Section: O Fluxo De áGua E a Ecologia Dos Riosunclassified