Marsupial mole
The marsupial moles are rare and poorly understood
burrowing mammals
of the deserts of western Australia.
There are thought to be two species: the Southern Marsupial
Mole (Notoryctes typhlops), and the Northern
Marsupial Mole (Notoryctes caurinus), so similar
to one another that they cannot be reliably told apart in the
field.
Marsupial moles spend most of their time underground, coming
to the surface only occasionally, probably mostly after rains.
They are blind, their eyes having become reduced to vestigal lenses
under the skin, and they have no external ears, just a pair of
tiny holes hidden under thick hair.
The head is cone-shaped, with a leathery shield over the muzzle,
the body tubular, the tail a short, bald stub. They are between
12 and 16 cm long, weigh 40 to 60 grams, and are uniformly covered
in fairly short, very fine pale cream to white hair with an iridescent
golden sheen.
Marsupial moles provide a remarkable example of convergent
evolution, with moles
generally, and with the golden moles of Africa
in particular. Although only related to other moles in that all
are mammals, the external similarity is an extraordinary reflection
of the similar evolutionary paths they have followed.
For many years their place within the Marsupialia
was hotly debated, some workers regarding it as an offshoot of
the Diprotodontia
(the order to which most living marsupials belong), others noting
similarities to a variety of other creatures, and making suggestions
that, in hindsight, appear bizarre. A 1989 review of the early
literature, slightly paraphrased, states:
- When Stirling (1888) initially was unable to find the epipubic
bones in Marsupial Moles, speculation was rife: the Marsupial
Mole wasa monotreme,
it was the link between monotremes and marsupials, it had it
closest affinities with the (placental) golden moles, it was
convergent with edentates,
it was a polyprotodont diprotodont, and so on. [1]
The mystery was not helped by the complete silence of the fossil
record. On the basis that marsupial moles have some characteristics
in common with almost all other marsupials, they were eventually
classified as an entirely separate
order:
the
Notoryctemorphia. Molecular level analysis
in the early
1980s
showed that the marsupial moles are not closely related to any of
the living marsupials, and that they appear to have followed a separate
line of development for a very long time, at least 50 million years.
In 1985, the
vast newly discovered limstone fossil deposits at Riverseigh in
northern Queensland
yeilded a major surprise: marsupial mole fossils between 15 and
20 million years old, which were by no means identical to the
living species but clearly related, and possibly even of a direct
ancestor. In itself, the discovery of a Miocene
marsupial mole presented no great mysteries. Just like the modern
forms, it had many of the features that are assumed to be adaptations
for a life burrowing in desert sands, in particular the powerful,
spadelike forelimbs. The Riversleigh fossil deposits, however,
are from an environment that was not remotely desert-like: in
the Miocene, the Riversleigh area was a tropical rainforest.
One suggestion advanced was that the Miocene marsupial mole
used its limbs for swimming rather than burrowing, but the mainstream
view is that it probably specialised in burrowing through a thick
layer of moss, roots, and fallen leaf litter on the rainforest
floor, and thus, when the continent began its long, slow desertification,
the marsupial moles were already equipped with the basic tools
that they now use to burrow in the sand dunes of the Western Australian
desert.