First evidence of chitin as a component of the skeletal fibers of marine sponges. Part I. Verongidae (demospongia: Porifera)

✍ Scribed by Hermann Ehrlich; Manuel Maldonado; Klaus-dieter Spindler; Carsten Eckert; Thomas Hanke; René Born; Caren Goebel; Paul Simon; Sascha Heinemann; Hartmut Worch

• Publisher: John Wiley and Sons
• Year: 2007
• Tongue: English
• Weight: 365 KB
• Volume: 308B
• Category: Article
• ISSN: 1552-5007
• DOI: 10.1002/jez.b.21156

✦ Synopsis

Abstract

The Porifera (sponges) are often regarded as the oldest, extant metazoan phylum, also bearing the ancestral stage for most features occurring in higher animals. The absence of chitin in sponges, except for the wall of peculiar resistance bodies produced by a highly derived fresh‐water group, is puzzling, since it points out chitin to be an autapomorphy for a particular sponge family rather than the ancestral condition within the metazoan lineage. By investigating the internal proteinaceous (spongin) skeleton of two demosponges (A__plysina__ sp. and Verongula gigantea) using a wide array of techniques (Fourier transform infrared (FTIR), Raman, X‐ray, Calcofluor White Staining, Immunolabeling, and chitinase test), we show that chitin is a component of the outermost layer (cuticle) of the skeletal fibers of these demosponges. FTIR and Raman spectra, as well as X‐ray difractograms consistently revealed that sponge chitin is much closer to the α‐chitin known from other animals than to β‐chitin. These findings support the view that the occurrence of a chitin‐producing system is the ancestral condition in Metazoa, and that the α‐chitin is the primitive form in animals. J. Exp. Zool. (Mol. Dev. Evol.) 308B:347–356, 2007. © 2007 Wiley‐Liss, Inc.