The Unique Skeleton of Siliceous Sponges (Porifera; Hexactinellida and Demospongiae) That Evolved first from the Urmetazoa During the Proterozoic: a Review
Biogeosciences, 4, 219–232, 2007 www.biogeosciences.net/4/219/2007/ Biogeosciences © Author(s) 2007. This work is licensed under a Creative Commons License. The unique skeleton of siliceous sponges (Porifera; Hexactinellida and Demospongiae) that evolved first from the Urmetazoa during the Proterozoic: a review W. E. G. Muller¨ 1, Jinhe Li2, H. C. Schroder¨ 1, Li Qiao3, and Xiaohong Wang4 1Institut fur¨ Physiologische Chemie, Abteilung Angewandte Molekularbiologie, Duesbergweg 6, 55099 Mainz, Germany 2Institute of Oceanology, Chinese Academy of Sciences, 7 Nanhai Road, 266071 Qingdao, P. R. China 3Department of Materials Science and Technology, Tsinghua University, 100084 Beijing, P. R. China 4National Research Center for Geoanalysis, 26 Baiwanzhuang Dajie, 100037 Beijing, P. R. China Received: 8 January 2007 – Published in Biogeosciences Discuss.: 6 February 2007 Revised: 10 April 2007 – Accepted: 20 April 2007 – Published: 3 May 2007 Abstract. Sponges (phylum Porifera) had been considered an axial filament which harbors the silicatein. After intracel- as an enigmatic phylum, prior to the analysis of their genetic lular formation of the first lamella around the channel and repertoire/tool kit. Already with the isolation of the first ad- the subsequent extracellular apposition of further lamellae hesion molecule, galectin, it became clear that the sequences the spicules are completed in a net formed of collagen fibers. of sponge cell surface receptors and of molecules forming the The data summarized here substantiate that with the find- intracellular signal transduction pathways triggered by them, ing of silicatein a new aera in the field of bio/inorganic chem- share high similarity with those identified in other metazoan istry started.
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