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2005 | 47 | 2 |

Tytuł artykułu

Zonation of macrofauna across sandy beaches and surf zones along the Dutch coast

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Języki publikacji

EN

Abstrakty

EN
On nine beaches and two transects in the surf zone along the Dutch coast the presence of benthic macrofauna was studied in relation to basic abiotic characteristics. According to Short’s classification system, Dutch beaches are mesotidal and dissipative (Ω = 8.6), and the RTR is low (1.52–1.27), which means that they are not tide-dominated. BSI ranged from 1.4 to 1.1 for the northern and western Dutch coasts respectively and had an overall value of 1.2. The rates of exposure of the beaches varied between 8 and 12, and are therefore regarded as sheltered to moderately exposed. The Dutch beaches display a geographical trend in beach types. Those of the Wadden Sea islands in the northern part of the Netherlands are dissipative, flat, fine-grained, and host high densities of many species of benthic macrofauna. The beaches along the western Dutch coast are less dissipative, steeper, with a higher mean grain size; the species diversity and abundance there are lower. Species diversity and abundance on the beaches increase from the high- to the low-water line. The maximum number of species was found between 0 and –1 m relative to the mean tidal level. The abundance peaks just above the mean tidal level, while the biomass reaches a maximum at the mean tidal level. Species diversity and abundance are low in the surf zone, but increase towards deeper water. Species numbers are high and the abundance is very high in the trough between the two bars. The relation between the diversity and abundance of macrobenthic species on the one hand, and the sediment composition, water column depth, and position between the bars on the other show a clear pattern of zonation for the beach, surf zone and near-shore: (1) a supralittoral zone with insects and air-breathing crustaceans, (2) a midshore zone, with intertidal species, (3) a lower shore zone, whose species extend into the shallow surf zone, and (4) a zone of sublittoral fauna in the trough between the two breaker bars within the surf zone.

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-

Czasopismo

Rocznik

Tom

47

Numer

2

Opis fizyczny

p.265-282,fig.,ref.

Twórcy

autor
  • National Institute for Coastal and Marine Management, Kerklaan 30, 9750 AE Haren, The Netherlands
autor

Bibliografia

  • Beukema J. J., 1981, Quantitative data on the benthos of the Wadden Sea proper, [in:] Report 4 of the Wadden Sea working group, N. Dankers, H. Kuhl & W. J. Wolff (eds.), Stichting Veth tot Steun aanWaddenonderzoek, Leiden, 134–142.
  • Beukema J. J., 2002, Expected changes in the benthic fauna of Wadden Sea tidal flats as a result of sea-level rise or bottom subsidence, J. Sea Res., 47(1), 25–39.
  • Brown A.C., McLachlan A., 1990, Ecology of sandy shores, Elsevier, Amsterdam, 1–328.
  • Beyst B., Buysse D., Dewicke A., Mees J., 2001, Surf zone hyperbenthos of Belgian sandy beaches: seasonal patterns, Estuar. Coast. Shelf Sci., 53 (6), 877–895.
  • Dahl E., 1952, Some aspects of the ecology and zonation of the fauna on sandy beaches, Oikos, 4, 1–27.
  • Degraer S., Volckaert A., Vincx M., 2003, Macrobenthic zonation patterns along a morphodynamical continuum of macrotidal, low tide bar/rip and ultradissipative sandy beaches, Estuar. Coast. Shelf Sci., 56 (3)–(4), 459–468.
  • Jaramillo E., McLachlan A., Dugan J., 1995, Total sample area and estimates of species richness in exposed sandy beaches, Mar. Ecol. Prog. Ser., 119, 311–314.
  • McLachlan A., Cockcroft A.C., Malan D. E., 1984, Benthic faunal response to a high energy gradient, Mar. Ecol. Prog. Ser., 16, 51–63.
  • McLachlan A., Jaramillo E., 1995, Zonation on sandy beaches, Oceanogr. Mar. Biol. Ann. Rev., 33, 305–335.
  • McLachlan A., Jaramillo E., Donn T.E.,Wessels F., 1993, Sandy beach macrofauna communities and their control by the physical environment: a geographical comparison, J. Coastal Res., 15, 27–38.
  • Short A.D., 1992, Beach systems of the central Netherlands coast: processes, morphology and structural impacts in a storm driven multi-bar system, Mar. Geol., 107, 103–137.
  • Short A.D., 1996, The role of wave height, period, slope, tide range and embaymentisation in beach classifications: a review, Rev. Chil. Hist. Nat., 69, 589–604.

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Bibliografia

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