Abstract
Demosponges (phylum Porifera) are among the first multicellular organisms on the planet and represent a unique archive of biosilica-based skeletal structures with species-specific microstructures called spicules. With more than 80 morphotypes, this class of sponges is recognized as a unique source of amorphous silica with superficial ornamentation patterned by organic phases. In this study, we investigated spicules of selected representatives of the family Geodiidae (order Tetractinellida), to identify F-actin-containing axial filaments within these 3D skeletal microconstructs defined as oxyspherasters and sterrasters. Their desilicification using 10% HF leads to isolation of multifilamentous, radially oriented organic matrices, which resemble the shape and size of the original spicules. Our data show that highly specific indicators of F-actin such as iFluorTM 594-Phalloidin, iFluorTM 488-Phalloidin, as well as iFluorTM 350-Phalloidin unambiguously confirm its localization within demineralized oxyspherasters and sterrasters of 11 diverse demosponges species belonging to the subfamily Geodiinae (genera Geodia, Rhabdastrella) and the subfamily Erylinae (genera Caminella, Caminus, Erylus, Pachymatisma). Well-defined periodicity in Geodia cydonium sterrasters actin filaments has been observed using atomic force microscopy (AFM) for the first time. The findings of F-actin as a possible pattern driver in spicules of geodiids brings additional light to our knowledge of spiculogenesis in this group. However, no specific actin structures were found between the geodiid subfamilies or genera thereby suggesting a common actin process, present already at the emergence of the family (~170 million years ago).
Published Version
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