Submerged coral reefs were mapped in the Gulf of Carpentaria by Geoscience Australia using a multibeam sonar seabed mapping system and underwater video.
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Walking along the beach at night or sailing on a darkened sea, you will often see sparkling lights in the water. This is bioluminescence—the emission of visible light by an organism as a result of a natural chemical reaction. A remarkable diversity of marine animals and microbes are able to produce their own light, and in most of the volume of the ocean, bioluminescence is the primary source of light. Luminescence is nearly absent in freshwater, with the exception of some insect larvae, a freshwater limpet, and unsubstantiated reports from deep in Lake Baikal. On land, fireflies are the most conspicuous examples, but other luminous taxa include other beetles, insects like flies and springtails, fungi, centipedes and millipedes, a snail, and earthworms. This discrepancy between marine and terrestrial luminescence is not fully understood, but several properties of the ocean are especially favorable for the evolution of luminescence: (a) comparatively stable environmental conditions prevail, with a long uninterrupted evolutionary history; (b) the ocean is optically clear in comparison with rivers and lakes; (c) large portions of the habitat receive no more than dim light, or exist in continuous darkness; and (d) interactions occur between a huge diversity of taxa, including predator, parasite, and prey.
via Haddock, Moline and Case (2010), Bioluminescence in the Sea – Annual Review of Marine Science, 2(1):443.
References and Further Information
They are an ancient species of flowering plants that grow submerged in all of the world’s oceans. Seagrasses link offshore coral reefs with coastal mangrove forests. Today, these “prairies of the sea,” along with mangroves, are on the decline globally. Scientists fear the diminishing vegetation could result in an ecosystem collapse from the bottom of the food chain all the way to the top.
Known as “hotspots of biodiversity,” seagrasses and mangroves attract and support a variety of marine life. However, worldwide damage and removal of these plants continue at a rapid pace. Changing Seas travels along Florida’s coastline to get a better understanding of the significant roles mangroves and seagrass play within the state. Can biologists prevent a negative ripple-effect throughout the marine food web before it’s too late? How will rising sea levels impact these plants as well at the communities that depend on them?
A benthic lander is a large three-legged frame with oceanographic instruments and sensors attached to it. These measure a range of parameters in-situ at the seabed; such as in this case, the current speed, temperature, salinity and turbulence. They are designed to operate in some cases 1000s of meters below the sea surface. Weights or ballasts are used to make the otherwise positively buoyant lander land down on the seafloor.
Here it was deployed from the Irish research vessel the Celtic Voyager in Galway Bay, West of Ireland, during a cruise by the National University of Ireland, Galway. The lander remains monitoring the conditions at the seabed for one month, in this case at depth of ~25m. Whilst out at sea during this period, it observes the impact of storm waves on the sediment transport. By making measurements at various heights above the seabed, it can obtain a profile of the benthic boundary layer and allow us to study how this changes during a storm.
By adding different sensors, you can also measure the chemical and biophysical properties of the water at the sediment-water interface. In-situ measurements allow us to study in the natural laboratory of the sea, without the need to remove anything. The measurements obtained by benthic landers are often used to verify as well as compliment laboratory results made under controlled situations.
It also has an acoustic positioning transponder which responds to the ship’s positioning call, to locate it for collection after its deployment. The weights or ballasts are released, with the buoyancy from the yellow floats allowing the lander to float back up to the surface.