The Oosterschelde Estuary (The Netherlands): A Case-Study of a Changing Ecosystem 1994
DOI: 10.1007/978-94-011-1174-4_20
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Changes in the sublittoral hard substrate communities in the Oosterschelde estuary (SW Netherlands), caused by changes in the environmental parameters

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Cited by 12 publications
(14 citation statements)
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“…The fixed zonation pattern changed its position, owing to the contracted tidal amplitude. The increased overall shelter of the estuary allows sessile animals and plants to grow in spots previously inaccessible (De Kluijver & Leewis, 1994 ;Meier & Waardenburg, 1994) .…”
Section: Responses At the Ecosystem Levelmentioning
confidence: 99%
“…The fixed zonation pattern changed its position, owing to the contracted tidal amplitude. The increased overall shelter of the estuary allows sessile animals and plants to grow in spots previously inaccessible (De Kluijver & Leewis, 1994 ;Meier & Waardenburg, 1994) .…”
Section: Responses At the Ecosystem Levelmentioning
confidence: 99%
“…They were made using micro-electronic equipment [WTW salinity-conductivity-O 2 meter (Hanna Instruments, Vila do Conde, Portugal), Lovibond Checkit pH-meter (Hanna Instruments)]; water clarity was determined using the Secchi disc (KC Denmark, Research Equipment, Silkeborg, Denmark). Furthermore, the total hydro-dynamism was measured, based on the corrosion of plaster in the water (Kaandorp 1986;Kluijver and Leewis 1994).…”
Section: Abiotic Parametersmentioning
confidence: 99%
“…Therefore, our deWnition of communities used here is a directly or indirectly interacting assemblage of algae and invertebrates which remains stable in time under a given set of abiotic factors. This classiWcation allows to recognise diVerent intertidal communities and to identify changes within its elements (de Kluijver 1997). In this concept, biotic interactions are not negated, but compared to the regulation by the physical environment they are considered of minor importance.…”
Section: Discussionmentioning
confidence: 99%
“…hydrozoans, mussels, tube-building polychaetes). The encrusting layer (EL) was formed by epilithic organisms adhering directly to the substratum, such as bryozoans or encrusting algae of the genus Phymatolithon or Ralfsia (see also de Kluijver 1991de Kluijver , 1993de Kluijver , 1997.…”
Section: Survey Methodsmentioning
confidence: 99%
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