Mycalidae Lundbeck, 1905

Łukowiak, Magdalena, 2015, Late Eocene siliceous sponge fauna of southern Australia: reconstruction based on loose spicules record, Zootaxa 3917 (1), pp. 1-65 : 34

publication ID

https://doi.org/ 10.11646/zootaxa.3917.1.1

publication LSID

lsid:zoobank.org:pub:D8CB263D-645B-46CE-B797-461B6A86A98A

DOI

https://doi.org/10.5281/zenodo.6108587

persistent identifier

https://treatment.plazi.org/id/2125D91F-1B01-295A-7ED9-C351F722F8AE

treatment provided by

Plazi

scientific name

Mycalidae Lundbeck, 1905
status

 

Family Mycalidae Lundbeck, 1905 View in CoL

Numerous mycalid spicules were found in the studied material. These nail-shaped spicules called exotyles ( Figs. 19 View FIGURE 19 F–L) are 300–400 µm long. They closely resemble spicules of the poecilosclerid sponges of the family Mycalidae . There is some morphological variability of these dermal spicules found in the studied fossil material. Some of them possess a shallow depression at the top of the disc and a small, button-shaped projection in the disc centre (e.g., see Figs. 19 View FIGURE 19 I–L) whereas the others display a flat disc with no button visible (e.g., see Figs. 19 View FIGURE 19 F–H). This variation may suggest that they represent two different species but intraspecific variability cannot be excluded as we know very little about the sponges bearing them. Those with a central depression closely resemble those of the Recent species Mycale (Rhaphidotheca) loricata ( Topsent, 1896) (see van Soest & Hajdu 2002, figs. 13A, B). The 200 µm long spicules described by Topsent do not, however, possess the button at the center of the depression ( Figs. 20 View FIGURE 20 D, E). While the exotyles with a flat disc surface and without the central button may belong to the other sister species (as the sponges bearing exotyles with a flat disc are not known among present-day species), the ones with a central depression may be assigned, most probably, to Mycale (Rhaphidotheca) cf. loricata .

The exotyles have already been described from the fossil record from the Late Eocene of Norseman (western Australia) by Hinde (1910) while Bukry noted similar spicules from the Middle Miocene from around Greenland (1979, pl. 8, fig. 3).

There were also some other club-shaped spicules found ( Figs. 30 View FIGURE 30 Q, U) that are very similar to the spicules occurring in Mycale (Rhaphidotheca) marshallhalli ( Kent, 1870) (compare with van Soest & Hajdu 2002, figs. 12C, D). Unfortunately, unquestionable assignment of these spicules to Mycale Gray, 1867a is not possible due to their generalized morphology and the fact that morphologically similar spicules occur in many different demosponge families e.g., Geodiidae [ Geodia ostracomorpha ( Lévi & Lévi, 1989) ], Heteroxyidae ( Halicnemia patera Bowerbank, 1864 ), Vulcanellidae ( Sphinctrella porosa Lebwohl, 1914 ), Guitarridae ( Guitarra fimbriata Carter, 1874 ), Placospongiidae ( Placospongia melobesioides Gray, 1867b ), Coelosphaeridae [ Forcepia (Leptolabis) luciensis (Topsent, 1888) ], Pachastrellidae [ Characella ijimai ( Lebwohl, 1914) ]. Additionally, there are some other similar, club-shaped spicules ( Figs. 30 View FIGURE 30 N–P) that may belong to the taxa mentioned above but also, in this case, their unquestionable assignment is not possible.

GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF