Abstract

Sponges (phylum Porifera) are phylogenetically ancient Metazoa that use silicon to form their skeletons. The process of biomineralization in sponges is one of the important problems being examined in the field of research focused on sponge biology. Primmorph cell culture is a convenient model for studying spiculogenesis. The aim of the present work was to produce a long-term primmorph culture from the freshwater Baikal sponge Lubomirskia baikalensis (class Demospongiae, order Haplosclerida and family Lubomirskiidae) in both natural Baikal water and artificial Baikal water to study the influence of silicate concentration on formation and growth of spicules in primmorphs. Silicate concentration plays an important role in formation and growth of spicules, as well as overabundance of silica leads to destruction of cell culture primmorphs. We also found that the composition of chemical elements (Si, O, C, and Na) varied along the length of growing spicules at cultivation in different media. The long-term culture of Baikal sponge primmorphs will be necessary for further investigations, and this system may serve as a powerful in vitro model to study spiculogenesis in Baikal siliceous sponges during the early stages of intracellular spicule formation to identify genes that affect biomineralization.

Highlights

  • We developed a primmorph culture from the endemic Baikal sponge L. baikalensis as a model to study biosilica formation

  • We report spicule formation in L. baikalensis primmorphs that were grown in various media

  • We indicated that spicules are formed and grow in primmorphs during in vitro cultivation in natural Baikal water (NBW)

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Summary

Introduction

Sponges (phylum Porifera) are the phylogenetically oldest Metazoa. Demosponges recorded before the end the Marinoan glaciation (635Myr ago) exist at present [1]. Processes of biomineralization and biosilification in sponges are the subject of active research and debate. Three sponge clades (class Demospongiae, order Hexactinellida) produce silica skeletons [2]. Their skeletons consist of spicules that form species-specific shapes. Their mineral components consist of silicon dioxide, silicon in amorphous opal-A and the bonded protein spongin (an analogue of collagen) [3,4]. The secretion of silica spicules in sponges is an intracellular process [3,5]. Many silica spicule-forming sponges have been characterized as containing and expressing silicatein genes [6,7,8,9]. Formation of spicules is a genetically controlled process and highly relevant to nanobiotechnology [6,11,12,13]

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