The distribution of the polychaete assemblages in southern Irish Sea a
nd its approaches (7-130 m depth) was investigated using cluster analy
sis and non-metric multidimensional scaling (MDS). Three main station
groupings were determined from the 51 quantitatively assessed stations
and their distinguishing species identified. The possible factors inf
luencing these assemblages were studied using canonical correspondence
analysis (CANOCO ordination program) and the recently developed BIO-E
NV procedure of the PRIMER (Plymouth Routines in Multivariate Ecologic
al Research) software package. Both techniques indicated sediment part
icle size and depth as the variables best ''explaining'' the species d
istributions. Species diversity was found to be highest in the offshor
e gravelly sediments and lowest in the inshore sands and muddy sands.
There was nevertheless evidence for a depth-related increase in divers
ity and evenness among the softer sediments. The high species richness
values (as determined by the Hurlbert rarefaction methodology) of the
more uniformly diverse gravels compared well with estimates from soft
deep-sea areas. These findings lend support to the theory that benthi
c diversity in the deep-sea is higher than on the shelf-at least for s
andy and muddy sediments. Conversely, the richness of the gravels cont
radicts the belief that high benthic diversities are only to be found
in the deep-sea and tropical shallow waters.