|Barrel sponge (Xestospongia testudinaria, Haplosclerida)|
The Demospongiae are the largest class in the phylum Porifera. Their "skeletons" are made of spicules consisting of fibers of the protein spongin, the mineral silica, or both. Where spicules of silica are present, they have a different shape from those in the otherwise similar glass sponges. The demosponges include 81% of all species of sponges with nearly 7,000 species worldwide (World Porifera Database), they are predominantly leuconoid in structure.
The many diverse orders in this class include all of the large sponges. Most are marine dwellers, but one order (Spongillida) live in freshwater environments. Some species are brightly colored, with great variety in body shape; the largest species are over 1 m (3.3 ft) across. They reproduce both sexually and asexually.
The Demospongiae have an ancient history, the first demosponges may have appeared during the Precambrian deposits at the end of the Cryogenian "Snowball Earth" period, where their presence has been indirectly detected by fossilized steroids, called steranes, hydrocarbon markers characteristic of the cell membranes of the sponges, rather than from direct fossils of the sponges themselves. They represent a continuous 100-million-year-long chemical fossil record of demosponges through the end of the Neoproterozoic. The earliest Demospongiae fossil was discovered in the lower Cambrian (Series 2, Stage 3; approximately 515 Ma) of the Sirius Passet Biota of North Greenland: this single specimen had a spicule assemblage similar to that found in the subclass Heteroscleromorpha. The earliest sponge-bearing reefs date to the Early Cambrian (they are the earliest known reef structure built by animals, exemplified by a small bioherm constructed by archaeocyathids and calcified microbes at the start of the Tommotian stage about 540–535 million years ago (Mya), found in southeast Siberia. A major radiation occurred in the Lower Cambrian and further major radiations in the Ordovician possibly from the middle Cambrian. (Finks, 1970
The extant Demospongiae have been organized into 14 orders that encompass 88 families, 500 genera, and more than 8000 described species.
Hooper and van Soest give the following classification of demosponges into orders:
- Subclass Homoscleromorpha Bergquist 1978
- Homosclerophorida Dendy 1905
- Subclass Tetractinomorpha
- Subclass Ceractinomorpha Levi 1953
However, molecular and morphological evidence show that the Homoscleromorpha do not belong in this class. The Homoscleromorpha was therefore taken out of the Demospongiae, and became the fourth class of Demospongiae.
Morrow & Cárdenas (2015) propose a revision of the Demospongiae higher taxa classification, essentially based on molecular data of the last ten years. They recommend the use of three subclasses: Verongimorpha, Keratosa and Heteroscleromorpha. They retain seven (Agelasida, Chondrosiida, Dendroceratida, Dictyoceratida, Haplosclerida, Poecilosclerida, Verongiida) of the 13 orders from Systema Porifera. They recommend the abandonment of five order names (Hadromerida, Halichondrida, Halisarcida, lithistids, Verticillitida) and resurrect or upgrade six order names (Axinellida, Merliida, Spongillida, Sphaerocladina, Suberitida, Tetractinellida). Finally, they create seven new orders (Bubarida, Desmacellida, Polymastiida, Scopalinida, Clionaida, Tethyida, Trachycladida). These added to the recently created orders (Biemnida and Chondrillida) make a total of 22 orders in the revised classification. These changes are now implemented in the World Porifera Database (http://www.marinespecies.org/porifera/), part of the World Register of Marine Species.
- Subclass Heteroscleromorpha Cárdenas, Pérez, Boury-Esnault, 2012
- order Agelasida Verrill, 1907
- order Axinellida Lévi, 1953
- order Biemnida Morrow et al., 2013
- order Bubarida Morrow & Cárdenas, 2015
- order Clionaida Morrow & Cárdenas, 2015
- order Desmacellida Morrow & Cárdenas, 2015
- order Haplosclerida Topsent, 1928
- order Merliida Vacelet, 1979
- order Poecilosclerida Topsent, 1928
- order Polymastiida Morrow & Cárdenas, 2015
- order Scopalinida Morrow & Cárdenas, 2015
- order Sphaerocladina Schrammen, 1924
- order Spongillida Manconi & Pronzato, 2002
- order Suberitida Chombard & Boury-Esnault, 1999
- order Tethyida Morrow & Cárdenas, 2015
- order Tetractinellida Marshall, 1876
- order Trachycladida Morrow & Cárdenas, 2015
- Heteroscleromorpha incertae sedis
- Subclass Verongimorpha Erpenbeck et al., 2012
- Sublclass Keratosa Grant, 1861
Demosponge systematics is an active area of research, and much is still to be learned. However, some rudimentary outlines can be made. The basal clade of the Demospongiae is the Homoscleromorpha, characterized by the possession of larvae more reminiscent of those of the Calcarea than those of the rest of the Demospongiae. Demosponges other than the Homoscleromorpha are split into two major groups, the Tetractinomorpha and the Ceractinomorpha. These two groups share characters that indicate common descent, such as a distinctive type and the presence of spongin. Currently, the two groups are each characterized by distinctive types of microscleres, though some doubt still remains as to whether the distinctive microsclere types evolved only once in each group. Fossils of each of these groups are known from the Cambrian, suggesting an early radiation of the major clades of demosponges. The Lithistida, a taxonomic grouping into which many of the fossil demosponges fall, is most certainly polyphyletic with members in both the Tetractinomorpha and the
- Homoscleromorpha: order Homosclerophorida
- Keratosa: orders Dendroceratida, Dictyoceratida and Verticillitida
- Myxospongiae: orders Chondrosida, Halisarcida and Verongida
- Haplosclerida (marine species)
- Remainder of the demosponges: orders Agelasida, Astrophorida, Hadromerida, Halichondrida, Poecilosclerida, Spirophorida and Haploscerida (freshwater species)
The branching order appears to be (Homoscleromorpha, (Keratosa, Myxospongiae)(Haplosclerida [marine species], remainder of the demosponges) ).
Chaetetids, more formally called "chaetetid hyper-calcified demosponges" (West, 2011), are common calcareous fossils composed of fused tubules. They were previously classified as extinct corals, bryozoans, algae, stromatoporoids and sclerosponges. The chaetetid skeleton has now been shown to be of polyphyletic origin and with little systematic value. Extant chaetetids are also described. This skeleton is now known from three demosponge orders (Hadromerida, Poecilosclerida, and Agelasida). Fossil chaetetid hyper-calcified demosponges can only be classified with information on their spicule forms and the original mineralogy of their skeletons (West, 2011).
Spermatocytes develop from the transformation of choanocytes and oocytes arise from archeocytes. Repeated cleavage of the zygote egg takes place in the mesohyl and forms a parenchymella larva with a mass of larger internal cells surrounded by small, externally flagellated cells. The resulting swimming larva enters a canal of the central cavity and is expelled with the exhalant current.
Methods of asexual reproduction include both budding and the formation of gemmules. In budding, aggregates of cells differentiate into small sponges that are released superficially or expelled through the oscula. Gemmules are found in the freshwater family Spongellidae. They are produced in the mesohyl as clumps of archeocytes, are surrounded with a hard layer secreted by other amoebocytes. Gemmules are released when the parent body breaks down, and are capable of surviving harsh conditions. In a favorable situation, an opening called the micropyle appears and releases amoebocytes, which differentiate into cells of all the other types.
The most economically important group of demospongians to human are the bath sponges. These are harvested by divers and can also be grown commercially. They are bleached and marketed; the spongin gives the sponge its softness and absorbency.
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- Robert Riding and Andrey Yu. Zhuravlev, "Structure and diversity of oldest sponge-microbe reefs: Lower Cambrian, Aldan River, Siberia", Geology 23.7 (July 1995:649-52) doi:10.1130/0091-7613(1995)023<0649:SADOOS>2.3.CO;2
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