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Tertiary solenoporacean algae and the reproductive structures of the Solenoporaceae

Knowledge of the supposed reproductive structures of the Solenoporaceae (Rhodophyta, calcareous algae, mostly Palaeozoic and Mesozoic) is reviewed, and then compared with evidence from a study of well-preserved Tertiary Solenoporaceae. Even in this material reproductive bodies cannot be identified with certainty. A suggested evolutionary history of the family relates the supposed reproductive processes to cell-structure, anatomy, and palaeoecology, comparing each with that of the related Corallinaceae.

A Viséan cephalopod fauna from New South Wales

A fauna consisting of numerous specimens of the ammonoid Beyrichoceras travellynense sp. nov., together with the nautiloids Mooreoceras regulare sp. nov., Vestinautilus sp., and Knightoceras? sp., is described from the Bingleburra Formation of the Gresford District, north-west of Newcastle, New South Wales. It is suggested that the fauna may be correlated with the middle to upper part of the Beyrichoceras zone of Europe.

Odontoma in a northern mammoth

A fossil odontoma presumably derived from Mammuthus primigenius has been collected from late Pleistocene deposits in the Yukon Territory, Canada. Odontomas are not as commonly recognized as some other pathological conditions in extinct vertebrates, but the majority of undoubted cases reported are from Pleistocene proboscideans of North America and Asia. Some reports in other mammalian orders from other regions may be questioned.

Palaeotaxodont bivalves from the Permian of New Zealand

Fifteen species of palaeotaxodont bivalves are described from the upper Artinskian and Kungurian marine deposits of New Zealand. New species are Nuculopsis imperta, N. oviformis, Quadratonucula asymmetrica, Polidevcia antequadrata, Glyptoleda intricata, G. flexuosa, and G. simplicata. One new genus Nucundata is proposed, with new species N, undata, N. truncata, N. obligua, and N. prolonga. An Australian species Nuculana concinna of Fletcher non Dana is renamed Polidevcia nodulosa sp. nov.

Assemblages of miospores from some Upper Carboniferous coals and their associated sediments in the Yorkshire coalfield

An investigation has been made of the miospore assemblages in the coals at the bottom and top of certain Yorkshire seams and in the adjacent seat-earths and roof measures. The assemblages from the sediments are similar and are often richer in numbers of species than those from the adjacent coals. The spores provide no evidence for the existence on the seat-earths of a distinctive type of vegetation differing significantly in composition from that which formed the initial peat layer. Several spore genera do, however, show greater frequency of occurrence in the sediments than in the coals.
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