Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-10T14:22:01.617Z Has data issue: false hasContentIssue false

Biogeographical affinities of polychaetes from Îles Crozet

Published online by Cambridge University Press:  28 January 2003

JACEK SICINSKI
Affiliation:
Laboratory of Polar Biology and Oceanobiology, Department of Invertebrate Zoology and Hydrobiology, University of Łódź, Banacha 12/16, 90-237 Łódź, Poland
PATRICK GILLET
Affiliation:
Centre d'Etude et de Recherche sur les Ecosystemes Aquatiques, Institute of Fundamental and Applied Research, UCO, place André Leroy, 3, BP 808, F-49008 Angers Cedex 01, France

Abstract

The study of polychaetes from the Marion Dufresne expedition to the Îles Crozet in 1982 provided 45 species from depths ranging from 50–1055 m. The most abundant was Eunice pennata, found at all depths and in all types of substratum in about 66% of the samples. This species with Laetmonice producta, Harmothoe spinosa and Lanice marionensis made up over 50% of all polychaete specimens. A homogenous polychaete assemblage dominated by the above mentioned group of species was encountered in the shallower stations (100–300 m). A mosaic-like and less abundant polychaete fauna with some characteristic, abundant species: Amage sculpta, Laetmonice wyvillei, Leanira quatrefagesi and Melinna cristata was encountered in the deeper stations (300–1055 m). Clear similarities between the polychaete fauna of Îles Crozet and soft-sediment polychaete assemblages of Marion and Prince Edward Islands were noticed. No such affinity was encountered with the polychaete fauna of Îles Kerguelen. Their position in relation to the Polar Front as well as possible differences in bottom deposits (calcareous versus siliceous) may in part explain these dissimilarities. The biogeographical status of Kerguelen Islands is also discussed.

Type
Research Article
Copyright
© Antarctic Science Ltd 2002

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)