Obdurodon dicksoni was a large (up to 60cm long head to tail), spoon-billed platypus from the Riversleigh area of north-western Queensland. Its skull is one of the most perfect fossils known from Riversleigh. Older Obdurodon species are known from central Australia, and a closely related species, Monotrematum sudamericanum, from the Paleocene of Patagonia, evidence that platypuses were once Gondwanan. Unlike the living platypus, these fossil platypuses had functional molar teeth.

The Riversleigh area during the early to middle Miocene would have been a mosaic of lakes, pools and caves in a karst (limestone) environment. Palaeoecological studies suggest that the environment had rainforest along the waterways and more open forest or woodland away from the watercourses.

Platypuses have a mix of features that relate either to their amphibious lifestyle or to their great antiquity. Obdurodon dicksoni is known only from a skull, lower jaw and teeth. These show that Obdurodon dicksoni was a large, spoon-billed platypus with an unusually flat, robust skull, fully rooted molars and premolars, but no dentition anterior to the premolars. The lower jaw, unlike that of the living platypus, has well developed angular and coronoid processes. To date, there are no known postcranial fossils of Obdurodon dicksoni.

Obdurodon probably fed on insect larvae, yabbies and other crustaceans, and perhaps small vertebrate animals such as frogs and fish. The skull of Obdurodon dicksoni is unusually flat, almost like that of a crocodile, and it is possible that this large platypus spent more time feeding on the surface (perhaps snapping at insects on the water's surface) and less time feeding on bottom-dwelling invertebrates, as the living platypus does. The well developed, rooted teeth of Obdurodon dicksoni suggest a more varied diet than that of the living platypus, perhaps including larger prey (for instance, a greater percentage of fish, tadpoles or froglets).

Obdurodon dicksoni, like all monotremes, would have been an egg-layer. Like the living platypus, it probably made burrows in the banks of rivers and streams, and fed on benthic aquatic invertebrates. Since its skeleton is unknown, there is little further knowledge of its lifestyle.

Obdurodon dicksoni is known from a well preserved skull (with premolar teeth in place), two lower jaw fragments and numerous isolated teeth. A second species of Obdurodon, Obdurodon insignis from the late Oligocene Tirari Desert locality in central Australia, is represented by molar teeth, a fragment of a lower jaw and a partial pelvis. There are also molar teeth of a third species of Obdurodon from the Mammalon Hill locality, Tirari Desert, central Australia.

The evolutionary relationships of monotremes are the subject of much debate, and no consensus has yet been reached. Monotremes may be related to other Southern Hemisphere mammals with triangulated teeth but a primitive jaw form. Alternatively, they may be descended from an as-yet-unknown group of early mammals or near-mammals.

Relationships between members of the platypus family are more clear, although there is comparatively little in the way of fossils and ideas could change if more material surfaces. It is certain that the toothless living platypus, Ornithorhynchus, is descended from a Cainozoic platypus (one of the Obdurodon species) with functional teeth. Obdurodon dicksoni, with its extreme bill shape, may not be the direct ancestor of Ornithorhynchus; instead, a smaller and more lightly built platypus, like Obdurodon insignis, may be a closer relative.