Coastal marine strata of last interglacial age are preserved extensively around the southern
Australian coastline. The sedimentary facies have many features in common with adjacent …

Marginal marine strata of last interglacial age occur in a range of morphostratigraphic
settings around the Australian coastline. The lithofacies are similar to their Holocene …

In the last decades, the understanding of temperate carbonate systems has improved
considerably, but their development over glacial–interglacial timescales is still understudied …

Abstract Yorke Peninsula in southern Australia is an important region for reconstructing
relative sea-level histories due to its location on the eastern margin of the tectonically stable …

Carbonate-dominant sediments are currently forming and accumulating over the extensive
marine shelf of the passive margin of southern Australia. A dearth of continental detritus …

The last interglacial maximum (Marine Isotope Substage 5e [MIS 5e], 128–116 ka) is a
distinctive event in recent Earth history. Shoreline successions of this age are important for …

The shallow seas surrounding Northern Australia, far away from former ice sheets and on a
tectonically stable margin, is ideally suited for sea-level reconstructions as hydro-isostatic …

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 …

Shallow-marine, mixed carbonate–terrigenous sediments have been accumulating in water
depths of 20–110 m on Wanganui shelf, central-western New Zealand, during the latest …

Aeolianite successions of low-gradient continental margins commonly show complex
records of coastal dune deposition linked to a wide range of sea-level positions and climatic …