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Monograph: Fish from the freshwater lower Cretaceous of Victoria, Australia with comments on the palaeo-environment

Special Papers in Palaeontology - No. 9 - Cover Image
Publication: Special Papers in Palaeontology
Number: 9
Publication Date: 1971
Page(s): 1 124
Authored By: Michael Waldman
Addition Information

How to Cite

WALDMAN, M. J. 1971. Fish from the freshwater lower Cretaceous of Victoria, Australia with comments on the palaeo-environment. Special Papers in Palaeontology9, 1–124.

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Abstract

5 families of fish are known from Koonwarra: Ceratodontidae (Dipnoi), Coccolepididae (Palaeonisciformes), Archaeomaenidae (Pholidophoriformes), Koonwarriidae nov., and Leptolepididae (Clupeiformes). The third and fourth families appear to be limited to Australia.

The Ceratodontidae are known from a single specimen, referable to Ceratodus sp. The Coccolepididae are sparsely represented by Coccolepis woodwardi sp. nov. Only one species of archaeomaenid is known from the site, Wadeichthys oxyops gen. et sp. nov. This is the most primitive archaeomaenid known, possessing enamelled scales overall, an unossified notochord, an uncompacted caudal skeleton, and preopercular pit-lines and sensory canals similar to those of some parasemionotids.

Koonwarria manifrons gen. et sp. nov., type genus of the new family Koonwarriidae, appears to be derived from the archaeomaenids and is considered to be a teleost. The caudal skeleton is compact and homo-heterocercal, with elongate uroneurals and well-formed hypurals. The scales are cycloid and skull pit-lines are greatly reduced.

A new species of Leptolepis, L. koonwarri, is closely related to L. talbragarensis from the Jurassic of New South Wales. It may also have affinities with the Cretaceous L. diasii from Brazil and Clupavlls brodiei from the English Upper Jurassic. L. koonwarri is a mosaic form with 'advanced' skull features such as the loss of the postorbital and possession of few preopercular canal branches, but the axial and caudal skeleton is of primitive leptolepid form.

The palaeo-environment was lacustrine or paludal, and mass mortality occurred periodically due to anoxic winter conditions beneath an ice-cover; the phenomenon known as 'winterkill'. The graded laminations present in the fish-bed are thought to be seasonal and to represent successive spring floodings, with settling of sediment during the years of the fish-bed. They may therefore be described as varves. Although such laminae are most common in deep, cold lakes, the widespread aquatic arthropod fauna is characteristic of a modern shallow-water environment. The number and variety of terrestrial insects and the small size of the fish also indicate shallow waters.

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