Maria Seton 
Luana Schena from the University of Zurich has just completed her summer internship in the EarthByte group, albeit remotely. Luana was working on a database of seafloor ages from DSDP/ODP/IODP drill holes from published data and focused on the world’s back-arc basins. This database will become a great complement to our present day seafloor age … Read more…
Postgraduate research scholarship at the EarthByte Group Up to $84,000 stipend scholarship to support a PhD student to research plate-plume interactions. Highlights Value Eligibility $28,000 pa (for up to 3 years) Full-time PhD student at the School of Geosciences Hold an honours or master’s degree How to apply Send expressions of interest to Dr … Read more…
Abstract: We present an updated oceanic crustal age grid and a set of complementary grids including spreading rate, asymmetry, direction and obliquity. Our dataset is based on a selected set of magnetic anomaly identifications and the plate tectonic model of Müller et al. (2019). We find the mean age of oceanic crust is 64.2 Myrs, … Read more…
Abstract: A major topic of debate in Earth and climate science surrounds the timing of closure of the Central American Seaway. While it is clear that the gateway was closed by ~2.8 Ma, recent studies based on geological and marine molecular evidence have suggested an earlier closing time of early to mid-Miocene. Here, we examine … Read more…
Abstract: Long-term variations in eustatic sea level in an ice-free world, which existed through most of the Mesozoic and early Cenozoic eras, are partly driven by changes in the volume of ocean basins. Previous studies have determined ocean basin volume changes from plate tectonic reconstructions since the Mesozoic; however, these studies have not considered a … Read more…
Abstract: Plate reconstructions since the breakup of Pangaea are mostly based on the preserved spreading history of ocean basins, within absolute reference frames that are constrained by a combination of age-progressive hotspot tracks and palaeomagnetic data. The evolution of destructive plate margins is difficult to constrain from surface observations as much of the evidence has … Read more…