A revised Holocene sea-level curve for the southeast coast of New South Wales, Australia, is
presented based on a review of previously published geochronological results for fossil …

Carbonate eolianite forms distinctive coastal landforms on many mid-latitude continents and
islands. Numerous studies of extensive continental and smaller island deposits in both …

The Gulf of Carpentaria is an epicontinental sea (maximum depth 70m) between Australia
and New Guinea, bordered to the east by Torres Strait (currently 12m deep) and to the west …

When mollusc shells are analysed conventionally for amino acid geochronology, the entire
population of amino acids is included, both inter-and intra-crystalline. This study investigates …

Located in a tectonically stable, intraplate setting and in the far field of former ice sheets, the
southern Australian passive continental margin represents a globally important region for …

The Leeuwin Current can be tracked from the western margin of the Australian continent to
the southern margin by the record of fossilized organisms typical of warm-water marine …

Aminostratigraphies of Quaternary non-marine deposits in Europe have been previously
based on the racemization of a single amino acid in aragonitic shells from land and …

Warm‐water molluscs were transported to Wanganui Basin from the northeastern North
Island during Pleistocene time as planktotrophic larvae. This is not possible at present, so …

The River Murray Estuary, a Ramsar Wetland Site, has experienced considerable rapid
coastal change during the Quaternary. The interplay of aeolian processes, river flows, tidal …

Aragonitic calcium carbonate (CaCO 3) terrestrial mollusc shells with complex shell
microstructures, such as those in the African subfamily Achatininae, have the potential to be …