2004
DOI: 10.1080/00364820310003307
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Community structure of intertidal meiofauna along a gradient of morphodynamic states on an exposed North Sea beach

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Cited by 17 publications
(15 citation statements)
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“…Moreover, the average meiobenthos densities and number of taxa recorded in the present study compares well with values reported on Atlantic, European beaches (e.g. Moore 1979;Rodríguez 2004;Kotwicki et al 2005a). Despite being in the range of other temperate zone beaches, the data in this work showed higher densities than those found by Renaud-Debyser & Salvat (1963) from the French Atlantic coast, Fenchel et al (1967) in the North Sea and Schmidt (1968) and Schmidt (1969) from Sylt island.…”
Section: Discussionsupporting
confidence: 83%
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“…Moreover, the average meiobenthos densities and number of taxa recorded in the present study compares well with values reported on Atlantic, European beaches (e.g. Moore 1979;Rodríguez 2004;Kotwicki et al 2005a). Despite being in the range of other temperate zone beaches, the data in this work showed higher densities than those found by Renaud-Debyser & Salvat (1963) from the French Atlantic coast, Fenchel et al (1967) in the North Sea and Schmidt (1968) and Schmidt (1969) from Sylt island.…”
Section: Discussionsupporting
confidence: 83%
“…However, more variability was detected, with copepods as the most abundant taxa at six sites. Copepods are usually the most abundant group in areas of coarse sands such as site B2B (Brown & McLachlan 1990;Rodríguez 2004), but in this study copepods were dominant in medium (B4C and B7A) and fine sand sites (B4A, B4B and B6A) too. Even if less frequently, other studies found copepods as dominant taxa in medium ) and fine sands (Moore 1979).…”
Section: Discussionmentioning
confidence: 91%
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“…Nestas ocasiões, segundo RODRÍGUEZ (2004), em praias arenosas com sedimentos finos a meiofauna está exposta à ação erosiva das ondas, que causa a suspensão de grande número de organismos para a coluna d'água, aumentando as taxas de mortalidade. Processos similares parecem ocorrer em Ajuruteua, onde o médiolitoral é erodido com o aumento da energia das ondas e das correntes de marés no período chuvoso, acarretando o aplainamento da face da praia, com grande mobilização de sedimentos para o infralitoral (ALVES & EL-ROBRINI, 2006).…”
Section: Methodsunclassified
“…Devido à interação desses fatores, as praias sofrem mudanças morfológicas e trocas de sedimento com regiões adjacentes em diferentes escalas temporais (SHORT, 2003). Como conseqüência deste presumido rigor ambiental, estas áreas foram muitas vezes consideradas desertos biológicos (MCLACHLAN & BROWN, 2006), e somente em anos recentes foi demonstrado que sua fauna bentônica pode ser diversa e abundante (ARMONIES & REISE, 2000;RODRÍGUEZ, 2004;MCLACHLAN & DORVLO, 2005).…”
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