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Ultrastructure and mineral composition of serpulid tubes (Polychaeta,Annelida)
Authors:OLEV VINN  HARRY A TEN HOVE  HARRY MUTVEI  KALLE KIRSIMÄE
Institution:1. Department of Geology, University of Tartu, Vanemuise 46, 51014 Tartu, Estonia;2. Zoological Museum, University of Amsterdam, POB 94766, 1090 GT Amsterdam, the Netherlands;3. Department of Palaeozoology, Swedish Museum of Natural History, Box 50007, SE‐104 05 Stockholm, Sweden
Abstract:We have studied the tube ultrastructure of 44 recent species from 36 serpulid genera. Twelve distinct ultrastructures are identified. Serpulids possess very diverse tube ultrastructures, in contrast with the traditional point of view. Most species show single‐layered tubes, but 34% of these species have between two and four ultrastructurally different layers. Tubes are mostly bimineralic, and are composed of aragonite and calcite; however, one of the polymorphs is always dominant. All the studied single‐layered tubes with a lamello fibrillar tube ultrastructure are exclusively calcitic; prismatic structures, both in regular or irregular orientation, are either calcitic or aragonitic in composition. There is no correlation between tube mineralogy, and ultrastructure, and marine, brackish, and freshwater environments. We find that 47% of the serpulid species studied possess a unique combination of tube structure characters. © 2008 The Linnean Society of London, Zoological Journal of the Linnean Society, 2008, 154 , 633–650.
Keywords:biomineralization  Serpulidae  skeletal ultrastructure
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