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Phylogénie moléculaire de polychètes Alvinellidae des sources hydrothermales actives de l'océan Pacifique
Titre alternatif
Producteur
Contributeur(s)
Éditeur(s)
John Libbey Eurotext Ltd
Identifiant documentaire
9-30698
Identifiant OAI
oai:archimer.ifremer.fr:30698
Auteur(s):
Feral, Jean-pierre,Philippe, Hervé,Desbruyeres, Daniel,Laubier, Lucien,Derelle, Evelyne,Chenuil, Anne
Mots clés
phylogénie
ARNr 285
sources hydrothermales
océan PaciFique
polychète
Terebellomorpha
Alvinellidae
Alvinella
Paralvinella
phylogeny
28S rRNA
hydrothermal vents
Pacific Ocean
Polychaeta
Terebellomorpha
Alvinellidae
Alvinella
Paralvinella.
Date de publication
01/08/1994
Date de création
Date de modification
Date d'acceptation du document
Date de dépôt légal
Langue
fre
Thème
Type de ressource
Source
Comptes Rendus De L Academie Des Sciences Serie Iii-sciences De La Vie-life Sciences (0764-4469) (John Libbey Eurotext Ltd), 1994-08 , Vol. 317 , N. 8 , P. 771-779
Droits de réutilisation
info:eu-repo/semantics/openAccess
Région
Département
Commune
Description
Phylogenetic trees were inferred by both distance and parsimony methods, using aligned sequences of the 28S rRNA 5'-end of 17 Polychaete species. Aphelinidae is a monophyletic taxon among the Terebellomorpha which also make a monophyletic group. Alvinella (2/2 species studied) is also a monophyletic taxon. The Paralvinella species (3/9 species) we studied cluster also in a monophyletic group. The D-1 domain of Alvinella is longer in other Polychates (30 nucleotides more). This is explained by the insertions of groups of 3 to 11 nucleotides whose fixation probable did not change so much rRNA conformation. This fixation could have been promoted by the necessity of fast recolonizations of new active hydrothermal vents (spatial isolation and ephemeral habitat). The comparison of the studied sequences of Polychates with those of coastal temperate and polar marine invertebrates shows that the relatively high Cytosine-Guanosine (C+G) level found in alvinellid sequences is not directly related to the particular characteristics of the hydrothermal environment as recently hypothetized.
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