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ORIGINAL ARTICLES

Depth-related changes in the arctic epibenthic megafaunal assemblages of Kangerdlugssuaq, East Greenland

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Pages 191-204 | Published online: 06 Sep 2007
 

Abstract

The effects of depth-related differences in environmental factors (pressure, hydrography, habitat and disturbance) on the benthic megafauna at the mouth of Kangerdlugssuaq Fjord in Arctic Greenland were investigated using a towed camera platform and autonomous underwater vehicle photographs. Large reductions in faunal density (60,132 to 1881 individuals ha−1) and increases in diversity (H′=0.93–2.54), through increases in richness (ES(220)=7.6–18.8) and reductions in dominance (Berger–Parker index=0.77–0.38) were found between 270 and 720 m water depth. Assemblages were separated into distinct shallow, intermediate and deep faunas by multivariate community analysis. In the shallower sites there were high levels of iceberg disturbance, directly reducing diversity as well as creating a complex, patchy environment inhabited by high densities of mobile suspension-feeding epifauna. In the deeper areas there was small-scale disturbance from the deposition of drop stones, but at a relatively low frequency and magnitude, which allowed increased species diversity. Proportions of deposit-feeding epifaunal and infaunal taxa rose with depth, as indicated by an increase with depth in faunal traces. Decreases in faunal density probably resulted from decreased food supply with depth.

Published in collaboration with the University of Bergen and the Institute of Marine Research, Norway, and the Marine Biological Laboratory, University of Copenhagen, Denmark

Published in collaboration with the University of Bergen and the Institute of Marine Research, Norway, and the Marine Biological Laboratory, University of Copenhagen, Denmark

Acknowledgements

Field studies were conducted as part of the UK National Environment Research Council (NERC) Autosub Under Ice (AUI) programme (NER/T/S/2000/00994) on board the Royal Research Ship James Clark Ross (cruise JR106). The authors wish to thank all on board for their help during the cruise. We would like to thank Jeffrey Evans (Scott Polar Research Institute) for assistance in analysing swath data and Karen Heywood, Paul Dodd and Martin Price (University of East Anglia) for help in the analysis of hydrographic data. D. Jones was supported for the duration of the work by NERC studentship NER/S/A/2002/10397.

Notes

Published in collaboration with the University of Bergen and the Institute of Marine Research, Norway, and the Marine Biological Laboratory, University of Copenhagen, Denmark

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