Ice Age Geology of the Great Barrier Reef

The upper continental slope and shelf edge of the southern Great Barrier Reef is largely unknown and poorly mapped. After a successful expedition mapping the northern Great Barrier Reef, R/V Falkor will traverse to the southern reaches of the Great Barrier Reef World Heritage Area. The goal of the expedition is to explore ancient undersea features that formed during the last Ice Age, when sea level was almost 120m lower than it is today. While once an exposed part of the Australian coastline, these features submerged, or ‘drowned,’ as glaciers and ice sheets melted and sea level rose, flooding Australia’s continental shelf. R/V Falkor’s team will use high-resolution multibeam sonar to search for these Ice Age past shorelines, drowned reefs, pinnacles, and shelf-edge terraces, as well as ancient river channels and deltas that connect to the ocean basin. Additionally, the search is on to find the southern extent of an even older limestone platform which may represent the ~20 million-year-old base upon which the present Great Barrier Reef has grown.

Schmidt Ocean Institute is thrilled to see Chief Scientist, Mardi McNeil, of the Queensland University of Technology lead this voyage, after her time as an SOI student opportunities participant in 2017. Mardi and her team will also be accompanied by Schmidt Ocean Institute’s Artist-at-Sea participant Taloi Havini, a Bougainville and Sydney based contemporary artist. Her work from this expedition will be featured in her first international solo exhibit at the Ocean Space, Venice, Italy in 2021.

20,000 Years Ago

Twenty thousand years ago, during the last ice age, most of earth’s water was locked in ice and glaciers. The sea level around Australia’s coastline was approximately 100 to 120 meters lower. As a result, Australia’s continental shelf was exposed during the last glacial period. In the present-day, many areas where coral grows used to be exposed land. Back then, a narrower band of coral reef thrived in the location of what is now the edge of the continental shelf of east Australia. As sea level rose, this coral reef drowned and the ocean covered a number of landscapes unique to the Australian continent. 

In order to uncover some of these drowned landscapes, the expedition will systematically survey the Fraser and Capricorn-Bunker shelf, the Capricorn Channel, and southern Swain Reef edges and slopes. The Capricorn-Bunker and Swain Reefs make up the southern extent of the present-day Great Barrier Reef, and mark the transition from tropical to temperate ocean conditions to the south. The goal of the science team is to determine whether the drowned reef system that has been extensively mapped in the northern and central GBR resembles the drowned reefs in the southern GBR, or whether such drowned reefs extend this far south at all. Understanding the southern extent of the drowned reefs and examining these lost landscapes is a vital piece of the puzzle in the examination of the history and formation of the Great Barrier Reef as we know it today. 

Mapping the Ice Age Submerged Landscapes 

The primary exploration tool for this expedition is R/V Falkor’s advanced mapping technology. Multibeam sonar will create detailed maps of the seafloor, illuminating ancient submerged reef terraces, pinnacles, rivers and shorelines. Falkor’s mapping system is highly effective in capturing high-resolution imagery of Australia’s seafloor features, as demonstrated through previous expeditions like Northern Depths of the Great Barrier Reef and Seamounts, Canyons, and Reefs of the Coral Sea.

The multibeam bathymetry datasets created from this expedition will be added to Geoscience Australia’s public AusSeabed data portal. They will also be added to the GEBCO Seabed 2030 project, which seeks to map the world’s entire seafloor by 2030. These detailed undersea maps are critical for Australia’s future management decisions within the Great Barrier Reef Marine Park and coinciding UNESCO World Heritage Area. As the Great Barrier Reef is a designated World Heritage Area, Australia is committed to protecting the it’s rich environmental and cultural significance for future generations. 

Corals Make Clouds 

To complement the Ice Age GBR mapping campaign,  this expedition will also measure atmospheric aerosol particles produced by coral reefs. Aerosols produced by corals are a natural process that can create cloud cover, protecting coral from harsh sunlight. An aerosol sampler will be used during the expedition to take constant measurements. The aerosol data will be used by the Reef Restoration and Adaptation Program to investigate technologies to reduce coral bleaching by creating cooling cloud cover. The data will help create more robust atmospheric models to be added to the CSIRO eReefs hydrodynamic models.

Dr Andrew Carroll, Geoscience Australia, prepares equipment to help understand the benthic communities of deepwater reefs in the Coral Sea.
Fledermaus graphic of planned survey areas. Greyscale data is previous data collected in the area. Brightly colored surface area is recent data from our last expedition. The blue color on the reef is LiDAR data. There is a general background of "interpolated data (blue to green) in the background.
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