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Partially the deep sea fishing industry is also being subsidised by the state. Environmentalists are increasingly worried about the ecological impacts of the fisheries in the deep sea. The fauna of the deeper continental borders and seamounts – especially the rare deep sea corals – and the fisheries-wise overused deep sea fish are considered especially protection worthy. The start of the exploration of the deep sea was closely linked to the economic interests of the 19th century.

Deep Ocean

The only exceptions to this are the hydrothermal vents, where the surrounding water is around 20 to 25 °C warm. The inhabitants of the deep sea do not have light intensity and temperature changes as indicators for any kind of life cycle rhythm (such as reproduction). The metabolic processes have reduced extremely at these constantly low temperatures. This may explain why certain species are present in the coastal water of the Arctic and Antarctic, as well as the deep sea. Nematodes make up 90 percent of the organisms living in the sediment; much more rarely, crabs and polychaetes can also be found.

Cold Seeps

The eel is thought to swim into groups of shrimp or other crustaceans with its mouth wide open, scooping them up and entrapping them before filtering out the excess water and then swallowing the prey. The mouth cavity can stretch and expand to a much larger size than is expected for such a small fish and would perhaps be expected to allow this species to capture and swallow large prey items. However, study of the stomach contents or large numbers of specimens have shown that they mostly eat small crustaceans.
They are biodiversity hotspots in the vast ocean that swirls around them, each one acting like a unique oasis in the desert. Despite the low temperatures, extreme ambient pressures, absence of sunlight and low resource availability, it supports a rich abundance of life in an array of unique ecosystems. Identifying and describing deep-sea species is a slow, complex process, often taking decades, and without a name, protecting them is even harder.

THE DEEP SEA : A KEY PLAYER TO BE PROTECTED FOR CLIMATE AND ECOSYSTEMS

Seamounts affect ocean circulation and mixing, resulting in nutrient upwellings that stimulate phytoplankton growth, which in turn supports a wide array of marine life. Consequently, modifications taking place at the surface, such as oxygen exhaustion or a decrease in phytoplankton, have impacts on life in the Deep Sea and can affect ecosystem functioning. According to observations, there are significant changes of food type and quantity originating from the surface and shifting to the abysses, several thousand metres deep.

• But we’re now able to explore more and more parts of this remote realm—thanks to a new generation of incredible underwater vehicles.
• Depending on the respective region, this can be at very different water depths.
• The catalytic reaction of the enzyme luciferase oxidises into the unstable protein luciferin, a reaction by which light is created without the loss of energy through heat dissipation.
• The scientifically relevant USPAs would be ideal objects for the extension of international environmental protection to the open ocean.
• This is the continental slope, the transition between Earth’s continental surface and Earth’s oceanic seafloor.

At this point, we have a fairly good idea of the seafloor’s topography, complete with plains, ridges and trenches – because experts have used echosounders to survey its depth profile and created corresponding maps. However, less than one percent of the seafloor has been examined in detail – e.g. with regard to the fauna living there. As a result, scientists working in the deep sea constantly encounter new species and other surprises. For example, in February 2021 an AWI team discovered the world’s largest fish breeding colony in the Antarctic’s Weddell Sea.
Many fish have the ability to produce ‘chemical’ light, a phenomena called ‘bioluminescence’ by oxidizing organic compounds. We have a number of different species of angler fish which have all been collected in the North Atlantic at depth between 500 and 4,000m. The name “cookie-cutter shark” refers to its feeding habit of gouging round plugs, as if cut out with a cookie cutter, out of larger animals. Marks made by cookie-cutter sharks have been found on a wide variety of marine mammals and fishes, as well as on submarines and undersea cables. This unusual shark occurs in warm, oceanic waters worldwide, and has been recorded as deep as 3.7km. It normally grows to about 50cm in length, it has a long, cylindrical body with a short, blunt snout.

WHY THE DEEP OCEAN IS IMPORTANT

• As we investigate the submarine slopes of Galápagos volcanoes we see life that no one has photographed before.
• We share video footage and specimens with taxonomy experts around the world, giving other researchers access to the deep sea.
• Biological collections from the Curasub off Curaçao have resulted in the discovery of numerous new and rare species of fishes, marine mollusks, echinoderms and crustaceans.
• The immense pressure at depths below 2,000 meters can crush air spaces within humans.
• All three species were first discovered in 2019 over two expeditions off the coast of Central California.

Surface waters also provide oxygen for the deep abysses when they move down to the Deep Sea in the Pole Regions. For instance, on the continental shelf, microorganisms play a major role in sustainable storage of carbon produced by phytoplankton, but are also filters for methane formed by this fossilized matter. By using methane as energy, these microorganisms transform this greenhouse gas, which is much more powerful than CO2, into minerals. This process prevents greenhouse gases from resurfacing and accelerating climate change. One of the most prominent and important resources of the deep sea are the manganese nodules which can be found on the seafloor at depths between 4,000 and 5,000 m.

Deep sea mining

If the external pressure goes below a threshold value, however, the methane hydrate evaporates immediately. It must be mined in a fashion that allows contained natural gas to be collected too, with a technique that is yet to be developed. Overfishing, bad management and the destruction of vital coastal habitats have diminished the population of sole, plaice, salmon, tuna and swordfish to such a drastic low that fishing these species is no longer worth it, economically. The last catching grounds are far away from territorial waters at sea mounts. There, at the oases of the oceans, we can currently see an unregulated “gold rush” for fish. The trench area below 6,000 m depth Deep Sea is called the hadal (1 % of the earth’s surface).
Depending on the specific research goals, the AUVs can operate at various depths and be fitted with a broad range of instruments. PAUL can dive down to 3,000 metres, while the smaller SARI has to draw the line at 200 metres. Though fish can be found at all depths, their density is far lower in the bottom-most layers. In the open ocean, you can find e.g. the bizarre deep-sea anglerfishes, which live at depths of ca. The females have an organic “fishing rod” complete with bait attached to their heads, and in many species, the bait actually glows.
Soon the skeleton is picked clean, but the fall is far from nutrient depleted. Whale bone consists of roughly 60 percent fat by weight, up to 200 times the amount of nutrients typically found at the seafloor. Specially adapted worms and snails take advantage of this feast by boring into the inner bone with acid and absorbing the fats inside with the help of bacteria.

The area of the ocean between 650 and 3,300 feet (200-1,000 m) is called the mesopelagic. Barely any light filters down to these depths, and yet still life thrives here. About 90 percent of the world’s fish (by weight) live in the mesopelagic—about 10 billion tons of fish. The bristlemouth fish alone may number at about a quadrillion, making them the most numerous family of vertebrates (animals with a backbone) in the world.