In the Huskisson River area of western Tasmania the strat-igraphically important early Upper Cambrian agnostid trilobite Glyptagnostus reticulatus (Angelin), occurs about 25 metres below the top of a sparsely fossiliferous Cambrian sequence. The sequence is overlain with apparent conformity by Junee Group sediments. The taxonomic position of two subspecies of G. reticulatus, viz: G.r. angelini (Resser) and G. r. reticulatus (Angelin) is reviewed
The Denison Range Basin is one of several small basins along the Adamsfield Trough, a Cambrian euge...
Monograptus thomasi, Early Devonian, occurs west of Cabbage Tree Hill, Beaconsfield, Tasmania, in ro...
An important Late Middle Cambrian fossil locality occurs 2 km west of St. Valentines Peak in north-w...
Two trilobite taxa, Agnostus (Homagnostus) sp. and Pseudagnostus (Pseudagnostus) idalis huskissonens...
A late Middle Cambrian (Ptychagnostus) punctuosus or P. nathorsti Zone) fauna occurs in the Que Rive...
Ten species of agnostid trilobites, including a new species, Utagnostus(?) nevel, are described from...
A small, poorly preserved, but stratigraphically significant fauna from Tom Creek in western Tasmani...
The first Middle Cambrian trilobites to be described from southwestern Tasmania come from two locali...
Sediments containing two almost entirely different Upper Middle Cambrian faunas are in direct conta...
The Climie Formation, which is about 460 metres thick in the type section of the Dundas Group, conta...
Near Middlesex Road, 9 km northeast of the Hellyer mine, northwestern Tasmania, a mineral exploratio...
An arthropod from the Que River Beds of western Tasmania is tentatively referred to the Order AG...
A well-exposed middle Late Cambrian to Early Ordovician clastic sequence, herein referred to as the ...
Eight unnamed species of brachiopods and one indetenninate hyolithid species are described and figur...
1. Introduction. II. Previous literature. III.The stratigraphical succession in Tasmania. IV. The...
The Denison Range Basin is one of several small basins along the Adamsfield Trough, a Cambrian euge...
Monograptus thomasi, Early Devonian, occurs west of Cabbage Tree Hill, Beaconsfield, Tasmania, in ro...
An important Late Middle Cambrian fossil locality occurs 2 km west of St. Valentines Peak in north-w...
Two trilobite taxa, Agnostus (Homagnostus) sp. and Pseudagnostus (Pseudagnostus) idalis huskissonens...
A late Middle Cambrian (Ptychagnostus) punctuosus or P. nathorsti Zone) fauna occurs in the Que Rive...
Ten species of agnostid trilobites, including a new species, Utagnostus(?) nevel, are described from...
A small, poorly preserved, but stratigraphically significant fauna from Tom Creek in western Tasmani...
The first Middle Cambrian trilobites to be described from southwestern Tasmania come from two locali...
Sediments containing two almost entirely different Upper Middle Cambrian faunas are in direct conta...
The Climie Formation, which is about 460 metres thick in the type section of the Dundas Group, conta...
Near Middlesex Road, 9 km northeast of the Hellyer mine, northwestern Tasmania, a mineral exploratio...
An arthropod from the Que River Beds of western Tasmania is tentatively referred to the Order AG...
A well-exposed middle Late Cambrian to Early Ordovician clastic sequence, herein referred to as the ...
Eight unnamed species of brachiopods and one indetenninate hyolithid species are described and figur...
1. Introduction. II. Previous literature. III.The stratigraphical succession in Tasmania. IV. The...
The Denison Range Basin is one of several small basins along the Adamsfield Trough, a Cambrian euge...
Monograptus thomasi, Early Devonian, occurs west of Cabbage Tree Hill, Beaconsfield, Tasmania, in ro...
An important Late Middle Cambrian fossil locality occurs 2 km west of St. Valentines Peak in north-w...
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