Vovelle, J.&Gaill, F. 1986. Données morphologiques, histochimiques et microanalytiques sur l'élaboration du tube organominéral d'Alvinella pompejana, Polychète des sources hydrothermales, et leurs implications Phylogénétiques. [Morphological, histochemical and microanalytical data on the elaboration of the organomineral tube ofAlvinella pompejana, a polychaete from hydrothermal vents, and its phylogenetic implications.]The material elaborated byAlvinellu pompejunaDesbruyères&Laubier, 1980, a polychaete worm from hydrothermal vents in the East Pacific, to build up its tube originates from an anterior ventral ‘glandular shield'. Mucocytes rich in sulphated glycosaminoglycan provide an accessory component, but the bulk is formed from homogeneous granules, secreted by the deep ‘main’ cells of this shield. The organic part of the granules, as demonstrated by histochemistry, is proteinaceous, while the mineral part, as proved by microanalysis, includes phosphorus, calcium, iron and in smaller amounts magnesium and zinc. The material of the tube shows an increase in the ratio iron‐calcium. Phosphorus may be bound to the organic part, but there is no sulphur present in it. In the laminated tube, scanning electron microscopy and microanalysis detect an enrichment in heterogeneous components of different constitution (balls and crystals). Silica, pointed out as characteristic of fossil worm tubes but absent in secretions, is not of endogenous origin. The original composition of theAlvinellatube can thus be related to that of other examples of the order Terebellida who live in a less drast