Loading...
Loading...
Available on 1 platform
Sign in to view source links and access this dataset
A sequence of biostratigraphic events spanning the middle to late Eocene was deduced from calcareous nannofossil assemblages in four sections of southeastern Australia's Otway Basin. The study compares this sequence with its counterpart in New Zealand and aligns it with tropical planktic foraminiferal zones, revising the placement of key foraminiferid events. Marine ingressions during the middle Eocene were diachronous across the basin, coinciding with a major change in sea-floor spreading rates south of Australia.
File formats are PDF and HTML, suggesting the primary data may be embedded within textual reports.