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Porifera source details
Cárdenas, P. (2020). Surface Microornamentation of Demosponge Sterraster Spicules, Phylogenetic and Paleontological Implications. Frontiers in Marine Science. 7.
391673
10.3389/fmars.2020.613610 [view]
Cárdenas, P.
2020
Surface Microornamentation of Demosponge Sterraster Spicules, Phylogenetic and Paleontological Implications
Frontiers in Marine Science
7
Publication
Available for editors
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Siliceous spicules in demosponges exist in a variety of shapes, some of which look like minute spheres of glass. They are called “sterrasters” when they belong to the Geodiidae family (Tetractinellida order) and “selenasters” when they belong to the Placospongiidae family (Clionaida order). Today, the Geodiidae represent a highly diverse sponge family with more than 340 species, occurring in shallow to deep waters worldwide, except for the Antarctic. The molecular phylogeny of Geodiidae is currently difficult to interpret because we are lacking morphological characters to support most of its clades. To fill this knowledge gap, the surface microornamentations of sterrasters were compared in different genera. Observations with scanning electron microscopy revealed four types of surfaces, which remarkably matched some of the Geodiidae genera: type I characteristic of Geodia, type II characteristic of Pachymatisma, Caminus, and some Erylus; type III characteristic of other Erylus; type IV characteristic of Caminella. Two subtypes were identified in Geodia species: warty vs. smooth rosettes. These different microornamentations were mapped on new Geodiidae COI (Folmer fragment) and 28S (C1–D2) phylogenetic trees. The monophyly of the Geodiidae was once again challenged, thereby suggesting that sterrasters have evolved independently at least three times: in the Geodiinae, in the Erylinae and in Caminella. Surface microornamentations were used to review the fossil record of sterrasters and selenasters through the paleontology literature and examination of fossils. It was concluded that “rhaxes” in the literature may represent mixes of sterrasters and selenasters: while Rhaxella spicules may belong to the Placospongiidae, Rhaxelloides spicules belong to the Geodiidae. The putative Geodiidae fossil genera, Geoditesia, and Geodiopsis, are reallocated to Tetractinellida incertae sedis. Isolated Miocene-Pliocene fossil sterrasters Hataina (Huang, 1967), Silicosphaera (Hughes, 1985) and Conciliaspongia (Robinson and Haslett, 1995) become junior synonyms of Geodia (Lamarck, 1815). Overall, the fossil record suggested that Geodiidae was present at least since the Middle Jurassic (163–166 Mya), while Geodia sterrasters were present since the Santonian/Campanian boundary, Late Cretaceous (83.6 Mya).
Paleontology, Fossils, Paleobiology
Systematics, Taxonomy Date action by
Caminella prima (Sim-Smith & Kelly, 2015) (basis of record)
Conciliaspongia Robinson & Haslett, 1995 † accepted as Geodia Lamarck, 1815 (source of synonymy) Conciliaspongia rarus Robinson & Haslett, 1995 † accepted as Geodia rara (Robinson & Haslett, 1995) † (source of synonymy) Geodia cordata (Wiedenmayer, 1989) (additional source) Geodia garoupa Carvalho, Lopes, Cosme & Hajdu, 2016 (additional source) Geodia margarita Sim-Smith & Kelly, 2015 (additional source) Geodia nodosa (Sim-Smith & Kelly, 2015) (source of synonymy) Geodia pocillum Van Soest, 2017 (additional source) Hataina Huang, 1967 † accepted as Geodia Lamarck, 1815 (source of synonymy) Hataina ovata Huang, 1967 † accepted as Geodia ovata (Huang, 1967) † (source of synonymy) Silicosphaera Hughes, 1985 † accepted as Geodia Lamarck, 1815 (source of synonymy) Silicosphaera asteroderma Hughes, 1985 † accepted as Geodia asteroderma Hughes, 1985 † (source of synonymy) |