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The Cape York Peninsula lies in the far northern Great Barrier Reef (GBR) Marine Park. The peninsula is one of the most isolated regions of the Australian continent and little is known about what lies in the offshore deeper waters. Scientists consider these deeper waters to be a frontier area of the GBR.
There are three major issues that limit widespread and frequent seafloor imaging: cost, personnel to operate platforms, and the technical complexity of long-duration vehicles. The engineering team working on this project aim to increase researchers’ ability to gather scientifically useful seafloor imagery in coastal and shelf environments with technologies that can increase ease of use while reducing costs of acquisition.
As ocean temperatures increase, a pressing global challenge in marine science is to better understand the distribution and characteristics of the critical habitats that support mesophotic and deep-water coral communities.
Within Australia’s largest marine reserve, the recently established Coral Sea Marine Park, lies the Queensland Plateau, one of the world’s largest continental margin plateaus at nearly 300,000 square kilometers.
The 1888 Ritter Island (Papua New Guinea) landslide was the largest historical volcanic-island landslide ever recorded and generated a devastating regional tsunami.
Ashmore Reef Marine Park is home to unique coral ecosystems: Mesophotic Coral Ecosystems (MCEs). While the waters of Australia are famous for shallower coral systems such as the Great Barrier Reef, MCEs there (and around the globe) remain largely unknown and undocumented.
Very few deep sea areas both in and outside of Australia have been well-sampled over large spatial and temporal scales, and a large number of species still remain undiscovered and unnamed.
Rising water temperatures and increasing carbon dioxide concentrations remain among the greatest threats to ocean ecosystems globally. This warming trend and associated ocean acidification poses a unique threat to species that use calcium carbonate to build their shells or skeletons, such as corals.
This expedition will feature exploration of the Emperor Seamount Chain while researching biodiversity and its drivers. Using currents, mapping, and radio isotopes to track water masses – as well as genetic sampling of corals – the team will determine the driving force behind coral distribution in this region.
This expedition will feature exploration of the Emperor Seamount Chain while researching biodiversity and its drivers. Using currents, mapping, and radio isotopes to track water masses – as well as genetic sampling of corals – the team will determine the driving force behind coral distribution in this region.
