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Macrocystella Callaway, the earliest glyptocystitid cystoid

Macrocystella mariae Callaway 1877, type species of Macrocystella, has a stem which is divisible into proximal and distal portions; a theca composed of 4 basal, 5 infra-lateral, 5 lateral, 6 radial, and some oral plates; a large periproct surrounded by 5 thecal plates; biserial unbranched brachioles grouped into 5 ambulacra and arising from the margins of the flattened oral surface. In all these respects it agrees with Mimocystites bohemicus Barrande 1887, type species of Mimocystites which becomes a subjective junior synonym of Macrocystella.

Discohelix (Archaeogastropoda, Euomphalacea) as an index fossil in the Tethyan Jurassic

Morphological features, growth, mode of life, and stratigraphical distribution are examined in more than 300 extremely well-preserved specimens of Discohelix from the Sicilian Lower and Middle Jurassic. In some species parabolic ribs similar to those in ammonites are formed owing to resorbtion during brief discontinuities in growth. Deviated peristomes recurring at an angle of more or less 72° and resulting in a pentagonal outline of the shell, are developed in two species for which the new subgenus Pentagonodiscus (type species D.(P.) angusta n. sp.) is established.

Pedicellariae of two Silurian echinoids from western England

Pedicellariae have been discovered on the Silurian (Ludlovian) echinoids Echinocystites pomum and Palaeodiscus ferox from Leintwardine, England. All pedicellariae of both species are tridentate in form and simple in morphology. Most are interambulacral in position. Pedicellariae of E. pomum are abundant, all are probably three-valved, and of variable size. Those of P. ferox are relatively rare, apparently two-valved, and small in size. These pedicellariae, and an Australian occurrence, are the oldest known echinoid pedicellariae.

Famennian ammonoids from New South Wales

Seven species and two subspecies belonging to four genera of ammonoids (Clymeniina and Goniati-tina) are described from a Famennian horizon, Platyclymenia Zone, a few hundred feet below the erosive base of the Carboniferous in the vicinity of Keepit Dam, near Tamworth, New South Wales. Three new species of Clymeniina are described: Genuclymenia keepitensis, Platyclymenia (Platyclymenia) teicherti, and P. (P.) alterna.

Chubbina, a new Cretaceous alveolinid genus from Jamaica and Mexico

Chubbina jamaicensis gen. et. sp. nov. and Chubbina macgillavryi spt nov, from the Cretaceous rocks of Jamaica and southern Mexico are described. Borelis cardenasensis Barker and Grimsdale is placed in the new genus. Chubbina appears to be a useful index for the Upper Cretaceous (Upper Campanian to Maastrich-tian) of the Greater Antilles and Central America.

Studies on Triassic fossil plants from Argentina. IV. The leaf genus Dicroidium and its possible relation to Rhexoxylon stems

The cuticle of four species of the genus Dicroidium is described. The material has been found in close association with Rhexoxylon stems in the locality of Ischigualasto, San Juan Province, Argentina. Two new combinations are proposed: Dicroidium zuberi (Szajnocha) and Dicroidium elongatum (Carruthers). It is proposed that Dicroidium leaves are related to Rhexoxylon stems (a) because they are associated in four Triassic localities of South Africa and Argentina, and (b) because there is a structural relation of both organs with the Palaeozoic pteridosperms.

Astrocystites distans sp. nov., an edrioblastoid from the Ordovician of eastern Australia

A new Ordovician edrioblastoid, Astrocystites distans sp. nov., and other miscellaneous pelmatozoan plates are described from the lower part of the Cliefden Caves Limestone WNW. of Mandurama, New South Wales. The edrioblastoid is similar to the only other species of Astrocystites known, A. ottawaensis Whiteaves from the Trenton Limestone of Ottawa, which was hitherto the sole representative of the group. This represents the first record of an edrioblastoid outside North America. Sections of the Australian material have revealed details of internal structures not previously known in the group.
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