European Ocean Biodiversity Information System

[ report an error in this record ]basket (0): add | show Print this page

The intra-annual variability of soft-bottom macrobenthos abundance patterns in the North Channel of the Seine estuary
Desroy, N.; Janson, A.-L.; Denis, L.; Charrier, G.; Lesourd, S.; Dauvin, J.-C. (2007). The intra-annual variability of soft-bottom macrobenthos abundance patterns in the North Channel of the Seine estuary. Hydrobiologia 588(1): 173-188. https://dx.doi.org/10.1007/s10750-007-0661-2
In: Hydrobiologia. Springer: The Hague. ISSN 0018-8158; e-ISSN 1573-5117
Also appears in:
Lafite, R.; Garnier, J.; De Jonge, V.N. (Ed.) (2007). Consequences of estuarine management on hydrodynamics and ecological functioning: ECSA 38th Symposium - Rouen 2004 Co-organisation Seine-Aval Programme and ECSA. Hydrobiologia, 588. Springer: The Netherlands. 302 pp., more
Peer reviewed article  

Available in  Authors 
    Vlaams Instituut voor de Zee: Non-open access 353354 [ request ]

Keywords
    Anthropogenic effects
    Benthic communities
    Sediments
    Temporal variations
    ANE, British Isles, North Channel [Marine Regions]; ANE, France, Seine Estuary [Marine Regions]
    Marine/Coastal
Author keywords
    temporal variability; bentho-pelagic coupling; sediment; Abra albacommunity; anthropogenic impacts; port 2000

Authors  Top 
  • Desroy, N.
  • Janson, A.-L.
  • Denis, L.
  • Charrier, G.
  • Lesourd, S.
  • Dauvin, J.-C.

Abstract
    Temporal and spatial variability of the Abra alba-Pectinaria koreni and Macoma balthica communities was examined in the northern part of the Seine estuary (North Channel) over different space and time scales in order to assess the role that the hydrologic regime and/or anthropogenic influences play in defining benthic communities over time. Sediment in the North Channel displayed strong spatial and temporal variability, sustained by intense sediment transport episodes. Total macrobenthic abundances ranged widely on the course of the year and there was no evidence of a seasonal signal for the density fluctuations, whatever the spatial scale considered. The bio-sedimentary dynamics can be divided into two periods: the first corresponds to the high flow rate period (January-May) during which fauna is influenced by fine silt/clay deposition, and the second to the low flow rate period (June-December) during which sandy deposits prevail. Despite the absence of significant correlations between sediment composition and abundance, episodes of sediment transport seem to be an important structuring mechanism in the Seine estuary. As a consequence, the faunal composition varied throughout the year. The winter and spring fauna, characterised by species living on muddy fine-sands or muds, were enriched during the summer and autumn by species living in clean fine sand, such as Donax vittatus, Nephtys cirrosa or Spio decoratus, mainly represented by adult individuals. Secondary settlement of drifters may explain the rapid structuration of assemblages a few days after the sandy deposits. Our results suggest the importance of the bentho-pelagic coupling, primarily induced by the sedimentary instability, on the macrobenthic fauna dynamics. The intra-annual variability of assemblages at the mouth of the Seine river and the silted situation of the North Channel might simply be the result of the silting up and alteration of the inner estuary, generated by several decades of man-made modifications and natural processes.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors