Leg 1 (May 7th – May 23rd)
Leg 1 begins in the Malacca Strait, one of the busiest shipping lanes in the world. Onboard, the paleoceanography team utilized the ship’s sub-bottom profilers to identify areas of interest for collecting sediment cores to capture snapshots of historical oceanic conditions, nutrient levels, sediment composition and microbial life. Deploying a gravity core, a tool composed of a long collection cylinder, allowed researchers to autonomously collect sediment cores up to 3-meters long that are then frozen in the ship’s laboratories.Combining this data with water quality measurements from CTD castsgives researchers unique insights into the present and historical ocean and seafloor dynamics of this fluctuating region.
After exiting the Malacca strait, the OceanXplorer began mapping the Mergui basin – an area suspected to have evidence of a submarine landslide. The ROV pilots collected push cores for the geoscience team onboard, while submersibles collected footage of a unique aggregation of giant isopod burrows in the surrounding area. After transiting north of Banda Aceh, the search for hydrothermal vents began.Although two plume signatures were detected by the multibeam sonars, the ROV could not locate their source. However,the team was successful in finding a shallow vent field near the volcanic Weh Island and deployed a team of divers to conduct visual transects, sediment sampling, rock and water sampling as well as CTD casts. Most surprising was the discovery of dozens of Catshark eggs nestled in the crevices of the vent sites. It's suspected that this species is utilizing the heat from the vents to incubate and accelerate development of their young – a behavior that has also been reported in Pacific White Skates in the Galapagos Islands (Salinas-de-León et al., 2018).
The OceanXplorer transited to the offshore Simeulue Basin to conduct CTD casts and ROV dives in the Sunda Trench. The geoscience team onboard sent the ROV to the site of the suspected epicenter of the 2004 Indian Ocean earthquake and tsunami responsible for devastating damage along the Indonesian coastline, as well as the coastlines of Malaysia, Maldives, Seychelles, Thailand, Myanmar, Sri Lanka, India, and even across the Indian Ocean in Somalia. The ROV dive revealed the area is devoid of life compared to the high biodiversity found in the abyssal plain to the north, indicating potential ongoing geological disruption in the area.