Bathymetric change is investigated within the transgressive phase of an extensive Early Cretaceous (Aptian-Albian) marine flooding of the Australian continent. Lithofacies and biofacies associations, found in nine outcrop sections and four continuously cored bore sections in the northeastern Eromanga Basin, are used to reconstruct depositional environments and to determine palaeobathymetry. Shoreface (c . 0–2m water depth), transitional (c . <10m), upper offshore (c . <50m), and lower offshore (c . 50–100m) facies are distinguished. Curves showing bathymetric changes are constructed for each stratigraphic section, and are placed in a time framework by biozones and compared across the region. Three depositional cycles are tentatively recognized during the transgressive phase. The first depositional cycle includes the Gilbert River Formation and the lower part of the Doncaster Member, and ranged from early Aptian (or late Barremian) to within the late Aptian. During maximum flooding, water depth was greatest in the southwest of the study area. Most sediment accumulation occurred under standstill conditions, and a fall in relative sea level occurred at the end of the cycle in all areas within the study region. The second cycle, during the later part of the late Aptian, includes the upper Doncaster Member and the Jones Valley Member. Most sediment accumulation occurred under fluctuating water depths, but a fall in relative sea level ends the cycle in all areas. The third depositional cycle includes the Ranmoor Member, and was represented by a significant late Early Albian transgressive pulse, recognized in age-equivalent formations from widely separated basins in Australia. At maximum flooding, the sea-floor was deepest in the northeast and shallowest in the southwest of the study area. The reversal in the direction of the bathymetric gradient between cycle 1 and cycle 3 in the region is probably related to tectonism along the eastern Australian margin. The apparent lack of correspondence between the Australian Albian record and the global sea-level curve suggests that continental-wide tectonism was an important influence in determining Australian sea levels during this time.
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