The Neoproterozoic era was punctuated by the Sturtian (about 710 million years ago) and Marinoan (about 635 million years ago) intervals of glaciation. In South Australia, the rocks left behind by the glaciations are separated by a succession of limestones and shales, which were deposited at tropical latitudes. Here we describe millimetre- to centimetre-scale fossils from the Trezona Formation, which pre-dates the Marinoan glaciation. These weakly calcified fossils occur as anvil, wishbone, ring and perforated slab shapes and are contained within stromatolitic limestones. The Trezona Formation fossils pre-date the oldest known calcified fossils of this size by 90 million years, and cannot be separated from the surrounding calcite matrix or ...
This paper explores the effects of preservation and taphonomy on the ultrastructure of recent and fo...
StW 573, Little Foot, is the most complete Australopithecus skeleton yet discovered, with many of it...
A small brachiopod–gastropod fauna from a core close to the base of the Calytrix Formation wit...
The Neoproterozoic era was punctuated by the Sturtian (about 710 million years ago) and Marinoan (ab...
The 3,430-million-year-old Strelley Pool Chert (SPC) (Pilbara Craton, Australia) is a sedimentary ro...
Precambrian stromatolites in South Australia are almost entirely restricted to the folded rock seque...
The 3,430-million-year-old Strelley Pool Chert ( SPC) ( Pilbara Craton, Australia) is a sedimentary ...
The Neoproterozoic Era was one of major biotic change against a background marked by fluctuations in...
have yielded Early and Middle Cambrian small skeletal fossils (SSF) accompanied by calcified cyanoba...
The 3.43 billion-year-old Strelley Pool Chert, Pilbara Craton, Western Australia, contains compellin...
Cave deposits of infill sediments and associated vertebrate fossils provide a valuable source of inf...
The Herefordshire Lagerstätte represents a fully marine Silurian ecosystem, three dimensionally soft...
The lower Cambrian (Series 2) White Point Conglomerate (WPC) on Kangaroo Island, South Australia con...
Scanning electron microscopy revealed micronsized globular and coccoid objects, associated with fila...
Estimates of Precambrian eukaryotic diversity and disparity indicate broad trends of increase in the...
This paper explores the effects of preservation and taphonomy on the ultrastructure of recent and fo...
StW 573, Little Foot, is the most complete Australopithecus skeleton yet discovered, with many of it...
A small brachiopod–gastropod fauna from a core close to the base of the Calytrix Formation wit...
The Neoproterozoic era was punctuated by the Sturtian (about 710 million years ago) and Marinoan (ab...
The 3,430-million-year-old Strelley Pool Chert (SPC) (Pilbara Craton, Australia) is a sedimentary ro...
Precambrian stromatolites in South Australia are almost entirely restricted to the folded rock seque...
The 3,430-million-year-old Strelley Pool Chert ( SPC) ( Pilbara Craton, Australia) is a sedimentary ...
The Neoproterozoic Era was one of major biotic change against a background marked by fluctuations in...
have yielded Early and Middle Cambrian small skeletal fossils (SSF) accompanied by calcified cyanoba...
The 3.43 billion-year-old Strelley Pool Chert, Pilbara Craton, Western Australia, contains compellin...
Cave deposits of infill sediments and associated vertebrate fossils provide a valuable source of inf...
The Herefordshire Lagerstätte represents a fully marine Silurian ecosystem, three dimensionally soft...
The lower Cambrian (Series 2) White Point Conglomerate (WPC) on Kangaroo Island, South Australia con...
Scanning electron microscopy revealed micronsized globular and coccoid objects, associated with fila...
Estimates of Precambrian eukaryotic diversity and disparity indicate broad trends of increase in the...
This paper explores the effects of preservation and taphonomy on the ultrastructure of recent and fo...
StW 573, Little Foot, is the most complete Australopithecus skeleton yet discovered, with many of it...
A small brachiopod–gastropod fauna from a core close to the base of the Calytrix Formation wit...