Exploring links between climate change, ocean chemistry, and the rise of multicellular life: The Ediacaran sedimentary record of central Australia (2014–2016)

Abstract:
For most of Earth history, single-celled organisms were the only forms of life on the planet. Not until roughly 600 million years ago do fossils of multicellular animals appear in the rock record. Explanations for the Ediacaran rise of multicellularity include extreme climate change, meteorite impact, and oxygenation of the global ocean. Evaluation of these hypotheses is complicated by the fact that stratigraphic records that span the appropriate time interval are rare. This project is focused on the C, O, and Zn isotopic records preserved by Ediacaran marine rocks in the Amadeus Basin of central Australia. Results will contribute to a more complete record of fluctuations in ocean chemistry during a key interval of Earth history.
Grant type:
ARC Discovery Early Career Researcher Award
Funded by:
Australian Research Council