glass sponges and feather stars
Explore Oceans Institute

Abyssal and Hadal East Indian Ocean

The Minderoo-UWA Deep-Sea Research Centre and Caladan Oceanic embarked on a 25 day voyage aboard the DSSV Pressure Drop to explore, to sample and map key seabed features of the East Indian Ocean at abyssal and hadal depths (3000 - 7000 metres deep).

 

Follow their voyage here.

Perth Canyon

Perth Canyon

Latitude: -31.7°SLongitude: 114.2°E

The Perth Canyon was formed by the ancient Swan River that flows through Perth. Cascading down the edge of the continental slope, the river outflow carved out the canyon many millions of years ago. Located 20 km west of Rottnest Island, it is 1.5 km deep and 15 km across – similar in size to the Grand Canyon.

 

The shape of the canyon ducts moves cold water in the Leeuwin Undercurrent into the canyon increasing nutrients in the surface waters, feeding phytoplankton that support a huge variety of marine life from the surface to the sea floor.

Perth Canyon- large red crab

Two baited landers were deployed at the head of Perth Canyon and within the Perth Canyon  Marine Park. Both landers were in 1000 m water depth.

These relatively shallow deployments recorded high abundance of crustaceans (crabs) and fish compared to those at Wallaby-Zenith Fracture Zone (WZFZ) and the Wallaby-Cuvier Escarpment (WCE) and also recorded a small shark.

Crystal crab- Chaceon albus Geryonidae

One crab was so large it shifted the lander while it fed on the bait. Crystal crabs (Chaceon albus) were present at both landers. This species is common along the Coast of Western Australia and is fished commercially between Fremantle and the North West Cape.

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