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Australia: The Land Where Time Began |
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Geilston Bay Local Fauna, Hobart, Tasmania
The marsupials in this deposit are recognisable as being related to the later Australian groups typical of the Cainozoic. Among these remains are those of a phalangerid, a diprotodontoid, a burramyid and a specimen that it is believed may be a dasyurid. Basalt that is at least 22 Ma overlies this site, putting to near the boundary between the Miocene and Oligocene
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Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading |