Fossil Echidnas (Megalibgwilia) Family Tachyglossidae
Specimens of fossil echidnas Megalibgwilia
Fossil material for Megalibgwilia ramsayi includes 4 intact skulls. The fossil skull Z2031.1 (Fig. 1) is held by the Tasmanian Museum and Art Gallery and is originally from the Montagu Cave in North-western Tasmania (Murray, 1978a, b). It may have an age of about 13,000 years (Goede and Bada, 1985; Griffiths et al., 1991). The other three specimens are P20488, P23144, P22811 from the Museum of South Australia. All three are from Henschke Fossil Cave at Naracoorte (Griffiths et al., 1991). Dating of those cave deposits yielded a minimum age of 16,700 and a maximum age of 90,000 to 120,000 years (Ayliffe and Veeh, 1988; Griffiths et al., 1991).
Z2031.1 (See Figure 1 and 4) was scanned in a medical scanner (Siemens Somatom) at the Calvary Hospital in Hobart. Two of the three South Australian specimens (P20488, P23144) were scanned with a Sky-Scan in vivo microCT system, located at Adelaide Microscopy, The University of Adelaide. Specimen P22811 was too wide for the 7 cm bore of the Adelaide microCT scanner.
Features on the endocranium of fossil echidnas
Figures 4 and 5 show 3D reconstructions from CT scans of the skulls of Z2031.1 (Fig. 4) and P23144 (Fig. 5). In all specimens studied by CT, impressions of cortical sulci (indicated by Greek letters) are visible on the skull interior. Sulci alpha, beta and zeta are of particular functional significance, because they define boundaries between functional areas identified by electrophysiology (Lende, 1964, Krubitzer et al., 1995). The motor or manipulation field lies between the alpha and beta sulci and the primary somatosensory cortex (S1) lies posterior to the alpha sulcus on the lateral cortical surface. Most of the primary visual cortex (V1) lies between the alpha and zeta sulci on the dorsal surface of the brain (see short and long-beaked echidna brains). Both the pattern and length of sulci appear identical in living and extinct echidnas (i.e. short and long-beaked) suggesting that functional cortical topography and gyrification have not changed significantly over the last 40,000 years (Ashwell et al., 2014).
References
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Ayliffe LE, Veeh HH (1988) Uranium series dating of speleothems and bones from Victoria Cave, Naracoorte, South Australia. Chemical Geology (Isotope Geoscience Section) 72, 211-234.
Goede A, Bada JL (1985) Electron spin resonance of Quaternary bone material from Tasmanian caves – a comparison with ages determined by aspartic acid racemization and C14. Australian Journal of Earth Science 32, 155-162.
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