Myrmecobiidae Waterhouse, 1841

Beck, Robin M. D., Voss, Robert S. & Jansa, Sharon A., 2022, Craniodental Morphology And Phylogeny Of Marsupials, Bulletin of the American Museum of Natural History 2022 (457), pp. 1-353 : 220

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https://doi.org/10.1206/0003-0090.457.1.1

DOI

https://doi.org/10.5281/zenodo.6974916

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scientific name

Myrmecobiidae Waterhouse, 1841
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Myrmecobiidae Waterhouse, 1841 View in CoL

CONTENTS: Myrmecobius (fig. 41).

STEM AGE: 20.2 Mya (95% HPD: 14.4–25.3 Mya).

CROWN AGE: N/A.

UNAMBIGUOUS CRANIODENTAL AUTAPOMORPHIES: Masseteric process present and projecting ventrally below plane of molar alveoli (char. 6: 0→1; ci = 0.125); jugal terminates in a ventrally expanded ectoglenoid crest (char. 22: 0→1; ci = 0.167); glenoid process of alisphenoid absent (char. 23: 1→ 0; ci = 0.125); scars of M. temporalis origin on braincase not fused middorsally to form sagittal crest in adults (char. 27: 1→0; ci = 0.059); maxillopalatine fenestrae consistently absent (char. 36: 1→0; ci = 0.111); posterolateral palatal foramina present, with complete posterior margins (char. 40: 1→0; ci = 0.200); palate extends posterior to presphenoid-basisphenoid suture (char. 42: 0→1; ci = 1.000); pterygoids separated from presphenoid by palatine-basisphenoid contact (char. 46: 0→1; ci = 0.111); pterygoids long, extending posteriorly to sheath the ventral margin of the carotid canal (char. 47: 0→1; ci = 0.333); masseteric fossa perforated by a distinct masseteric foramen (char. 99: 0→1; ci = 0.333); angular process weakly or not inflected (char. 102: 0→1; ci = 0.250); premolariform second upper premolar (P2) distinctly taller than premolariform P3 (char. 119: 2→0; ci = 0.118); i2 alveolus like those of i1 and i3 (char. 149: 0→1; ci = 0.250); paraconid well developed, but paracristid indistinct or absent on m1 (char. 159: 0→2; ci = 0.400); paraconid well developed, but paracristid indistinct or absent on m2 and m3 (char. 161: 0→2; ci = 0.667); cristid obliqua absent or indistinct (char. 167: 0→1; ci = 0.500); hypoconid small and indistinct (char. 172: 0→1; ci = 0.333); and entocristid indistinct or absent (char. 176: 0→1; ci = 0.077).

COMMENTS: Kealy and Beck (2017: table 1 View TABLE 1 ) defined Myrmecobiidae as the most inclusive clade including Myrmecobius fasciatus , but excluding Dasyurus viverrinus and Thylacinus cynocephalus . Under this definition, our dated total-evidence analysis ( fig. 33) indicates that the fossil dasyuromorphians † Barinya and † Mutpuracinus are myrmecobiids, as did the dated total-evidence analysis of Kealy and Beck (2017: fig.3). Given our estimate for the age of the split between the Myrmecobius lineage and Dasyuridae (median: 24.9 Mya; 95% HPD: 21.8–29.4 Mya) and those of other recent studies (e.g., Mitchell et al., 2014; Westerman et al., 2016; Kealy and Beck, 2017), we would expect stemmyrmecobiids in the fossil record from at least the early Miocene onward; the earliest of these would presumably have had a “typical,” unreduced dasyuromorphian dentition, in contrast to the secondarily simplified dentition of Myrmecobius . Thus, it is not implausible that † Barinya and † Mutpuracinus are indeed early myrmecobiids. However, the Myrmecobius + Barinya + Mutpuracinus clade receives only relatively weak support here (BPP = 0.67), and only one craniodental feature optimizes as an unambiguous synapomorphy, namely loss of the posterior cutting edge of P3 (char. 124: 1→2; ci = 0.667), which is clearly the case in † Barinya ( Wroe, 1999) , but which cannot be scored in † Mutpuracinus based on available material ( Murray and Megirian, 2000; Murray and Megirian, 2006a). We consider the evidence that Barinya and Mutpuracinus are stem myrmecobiids to be equivocal pending further studies, so we here restrict Myrmecobiidae to Myrmecobius .

Myrmecobius is characterized by a long list of craniodental apomorphies not seen in other dasyuromorphians: many of these are dental, but there are also a large number of unusual cranial features (see also Archer, 1976b, 1984c; Archer and Kirsch, 1977; Friend, 1989; Cooper, 2000). At least some of these apomorphies are likely related to myrmecophagy, including several relating to simplification of the molars (reflecting little or no occlusion between the upper and lower dentition; Charles et al., 2013).

Archer, M. 1976 b. The basicranial region of marsupicarnivores (Marsupialia), inter-relationships of carnivorous marsupials, and affinities of the insectivorous marsupial peramelids. Zoological Journal of the Linnean Society 59 (3): 217 - 322.

Archer, M., and J. A. W. Kirsch. 1977. The case for Thylacomyidae and Myrmecobiidae, or why are marsupial families so extended? Proceedings of the Linnean Society of New South Wales 102: 18 - 25.

Archer, M. 1984 c. The Australian marsupial radiation. In M. Archer and G. Clayton (editors), Vertebrate zoogeography and evolution in Australasia: 633 - 808. Perth: Hesperian Press.

Charles, C., F. Sole, H. G. Rodrigues, and L. Viriot. 2013. Under pressure? Dental adaptations to termitophagy and vermivory among mammals. Evolution 67 (6): 1792 - 1804.

Cooper, C. E. 2000. Myrmecobius fasciatus (Dasyuromorphia: Myrmecobiidae). Mammalian Species 43 (881): 129 - 140.

Friend, J. A. 1989. 22. Myrmecobiidae. In D. W. Walton and B. J. Richardson (editors), Fauna of Australia, vol. 1 B. Mammalia: 1 - 18. Canberra: AGPS.

Kealy, S., and R. M. D. Beck. 2017. Total evidence phylogeny and evolutionary timescale for Australian faunivorous marsupials (Dasyuromorphia). BMC Evolutionary Biology 17 (1): 240.

Mitchell, K. J., et al. 2014. Molecular phylogeny, biogeography, and habitat preference evolution of marsupials. Molecular Biology and Evolution 31 (9): 2322 - 2330.

Murray, P. F., and D. Megirian. 2000. Two new genera and three new species of Thylacinidae (Marsupialia) from the Miocene of the Northern Territory, Australia. Beagle, Records of the Museums and Art Galleries of the Northern Territory 16: 145 - 162.

Murray, P. F., and D. Megirian. 2006 a. Cranial morphology of the Miocene thylacinid Mutpuracinus archibaldi (Thylacinidae, Marsupialia) and relationships within the Dasyuromorphia). Alcheringa: an Australasian Journal of Palaeontology Special Issue 1: 229 - 276.

Waterhouse, G. R. 1841 a. The natural history of Marsupialia or pouched animals. Edinburgh: W. H. Lizars.

Westerman, M., et al. 2016. Phylogenetic relationships of dasyuromorphian marsupials revisited. Zoological Journal of the Linnean Society 176 (3): 686 - 701.

Wroe, S. 1999. The geologically oldest dasyurid (Marsupialia), from the Miocene Riversleigh, northwestern Queensland. Palaeontology 42: 1 - 27.