Trace element geochemistry of microbialites: towards an independent record of biogenicity, microbial communities, and seawater chemistry. A vast amount of Australia's mineral wealth is held in rocks of Precambrian age, yet those rocks are notoriously difficult to date and correlate owing to the rarity of fossils. Successful discrimination of different microbialites using biochemically sensitive trace elements will provide a firm basis and rationale for stromatolite biostratigraphy and greatly in ....Trace element geochemistry of microbialites: towards an independent record of biogenicity, microbial communities, and seawater chemistry. A vast amount of Australia's mineral wealth is held in rocks of Precambrian age, yet those rocks are notoriously difficult to date and correlate owing to the rarity of fossils. Successful discrimination of different microbialites using biochemically sensitive trace elements will provide a firm basis and rationale for stromatolite biostratigraphy and greatly increase our ability to understand the geological evolution and distribution of Precambrian rocks and resources. Additionally, a better understanding of the information content of stromatolites will yield considerable insight into the origin of life on Earth and its relationship to Earth's evolving chemistry and environment. Read moreRead less
Australia's oldest jawed fishes: evolution, biostratigraphy and biogeography. The research focusses on a collection of disarticulated remains of placoderms, a group of extinct armoured fishes which dominated Devonian waters (410-354 Mya). The oldest Australian placoderm macroremains so far described are of late Pragian age (400 Mya), and recognized as a highly endemic fauna. An older limestone from New South Wales has yielded new material which includes sclerotic capsules and dermal plates of ....Australia's oldest jawed fishes: evolution, biostratigraphy and biogeography. The research focusses on a collection of disarticulated remains of placoderms, a group of extinct armoured fishes which dominated Devonian waters (410-354 Mya). The oldest Australian placoderm macroremains so far described are of late Pragian age (400 Mya), and recognized as a highly endemic fauna. An older limestone from New South Wales has yielded new material which includes sclerotic capsules and dermal plates of small placoderms. Earliest Devonian (Lochkovian) acanthodians and the new placoderms, unlike the younger taxa, seem closely related to coeval faunas from the circum-Arctic region. The material will help resolve relationships and distribution of these early jawed vertebrates.Read moreRead less