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The deep ocean houses an ecosystem that has learned to thrive without sunlight or warmth. Welcome to the abyss. Our oceans are changing fast. Find out how Museum collections are helping scientists to understand the future of marine life. The pelagic part of the aphotic zone can be further divided into vertical regions according to temperature. The mesopelagic is the uppermost region. Its lowermost boundary is at a thermocline of 12 °C (54 °F), which, in the tropics generally lies at 700–1,000 meters (2,300–3,300 ft). Next is the bathypelagic lying between 10 and 4 °C (50 and 39 °F), typically between 700–1,000 meters (2,300–3,300 ft) and 2,000–4,000 meters (6,600–13,100 ft), lying along the top of the abyssal plain is the abyssopelagic, whose lower boundary lies at about 6,000 meters (20,000 ft). The last zone includes the deep oceanic trench, and is known as the hadalpelagic. This lies between 6,000–11,000 meters (20,000–36,000 ft) and is the deepest oceanic zone. There, we might find something to eat; of which there was little hope, out on the ocean. Professor Richard Twitchett explains what a more acidic ocean could mean for the future of marine life. Sophisticated and sensual. Private and exclusive. The Cove’s Ocean Suite offers Atlantis Paradise Resort Island guests a haven, a redefined beach vacation experience. Accentuated by luxurious amenities, all the resort services a traveler could ever want from Club Cove and capped by the pure blue of a never-ending Bahamian sky. Ocean Suites offer guests a refined level of comfort and feature a host of designer amenities—including full or French balconies with ocean views, open floor plans with step-down living areas, generous walk-in closets, spacious bathrooms with marble floors, twin granite vanities with vessel sinks, frosted glass-tile enclosed shower and a custom in-room bar. “We made ocean mining seem a lot more credible,” Sharp says. “We really misled a lot of people and it’s surprising that the story held together for so long.” © 2013 oceanpro.com.pl | www.oceanpro.com.pl Professor Richard Twitchett explains what a more acidic ocean could mean for the future of marine life. Terrestrial planets will acquire water during their accretion, some of which will be buried in the magma ocean but most of it will go into a steam atmosphere, and when the atmosphere cools it will collapse on to the surface forming an ocean. There will also be outgassing of water from the mantle as the magma solidifies—this will happen even for planets with a low percentage of their mass composed of water, so “super-Earth exoplanets may be expected to commonly produce water oceans within tens to hundreds of millions of years of their last major accretionary impact.”[73] Ocean currents greatly affect Earth’s climate by transferring heat from the tropics to the polar regions. Transferring warm or cold air and precipitation to coastal regions, winds may carry them inland. Surface heat and freshwater fluxes create global density gradients that drive the thermohaline circulation part of large-scale ocean circulation. It plays an important role in supplying heat to the polar regions, and thus in sea ice regulation. Changes in the thermohaline circulation are thought to have significant impacts on Earth’s energy budget. In so far as the thermohaline circulation governs the rate at which deep waters reach the surface, it may also significantly influence atmospheric carbon dioxide concentrations. Scientists testing North Atlantic mesopelagic fish eaten by the ocean’s top predators found that nearly 75 percent were contaminated with microplastic fibers. Researchers have also discovered microplastics in the scat of gray seals and in the Atlantic mackerel they eat.23 days ago Please reach out to UNESCO’s IOC via oceandecade@unesco.org Kantor ocean to idealne miejsce dla osób, które stawiają na wygodę, bezpieczeństwo i oszczędności. Dzięki platformie wymiany walut Ocean, wymienisz Swoją walutę nie wychodząc z domu po atrakcyjnym kursie, co pozwoli Ci zaoszczędzić znaczną sumę pieniędzy na Twojej racie kredytowej w obcej walucie. The benthic zones are aphotic and correspond to the three deepest zones of the deep-sea. The bathyal zone covers the continental slope down to about 4,000 meters (13,000 ft). The abyssal zone covers the abyssal plains between 4,000 and 6,000 m. Lastly, the hadal zone corresponds to the hadalpelagic zone, which is found in oceanic trenches. Obszar szelfu i stoku kontynentalnego są zbudowane ze skorupy kontynentalnej i przez geologów zaliczane do kontynentów. Obszary basenów oceanicznych, rowów oceanicznych i grzbietów śródoceanicznych mają skorupę typu oceanicznego i tworzą właściwy wszechocean. Formą pośrednią są tzw. mikrokontynenty – obszary położone na dnie oceanu, całkowicie lub prawie całkowicie przykryte wodą, a zbudowane ze skorupy kontynentalnej lub mieszanej. Istnienie oceanu na księżycu Saturna zwiększa szanse na znalezienie życia pozaziemskiego w naszym Układzie Słonecznym. OMI serves to enrich and expand the public’s understanding of ocean science and conservation through the collaborative creation, exhibition, and open-distribution of innovative visual media as well as artistic approaches to ocean education. We are a nonprofit systems change incubator. We work with industry players, technologists, and NGOs to create business solutions to ocean challenges. Vast and wondrous, our ocean covers more than 70% of our planet. It controls the weather and climate. It provides life, food and medicine. It is key to a thriving global economy and has inspired art, poetry and tales of adventures for centuries. Yet through neglect and a startling lack of access it has lingered as an afterthought in our conservation and exploration efforts. Fish are common passive mobs found in oceans and rivers. They come in 4 main variants: cod, salmon, puffer fish, and tropical fish. Oceans, seas, lakes and other bodies of liquids can be composed of liquids other than water, for example the hydrocarbon lakes on Titan. The possibility of seas of nitrogen on Triton was also considered but ruled out.[74] There is evidence that the icy surfaces of the moons Ganymede, Callisto, Europa, Titan and Enceladus are shells floating on oceans of very dense liquid water or water–ammonia.[75][76][77][78][79] Earth is often called the ocean planet because it is 70% covered in water.[80][81] Extrasolar terrestrial planets that are extremely close to their parent star will be tidally locked and so one half of the planet will be a magma ocean.[82] It is also possible that terrestrial planets had magma oceans at some point during their formation as a result of giant impacts.[83] Hot Neptunes close to their star could lose their atmospheres via hydrodynamic escape, leaving behind their cores with various liquids on the surface.[84] Where there are suitable temperatures and pressures, volatile chemicals that might exist as liquids in abundant quantities on planets include ammonia, argon, carbon disulfide, ethane, hydrazine, hydrogen, hydrogen cyanide, hydrogen sulfide, methane, neon, nitrogen, nitric oxide, phosphine, silane, sulfuric acid, and water.[85] Nine teams are advancing in the XPRIZE Foundation’s $7 million contest to create technologies that will scale up humanity’s ability to understand and chart the deep ocean.10 days ago On 1 November 1967, a UN committee was meeting in New York and the ambassador from the island nation of Malta was invited to speak. Dr Arvid Pardo faced an uphill struggle. He was suggesting that the deep oceans should be reserved for peaceful activities and that the mineral wealth should be shared by all of mankind. Według tektoniki płyt skorupa ziemska powstaje w przybliżeniu w takim samym tempie, w jakim jest niszczona w strefach subdukcji, a łączna objętość oceanów nie ulega zmianie (nie licząc rozrostu i topnienia lodowców). Jedne oceany mogą powiększać się tylko kosztem innych; w historii Ziemi istniały zbiorniki oceaniczne, które zamknęły się na skutek ruchu kontynentów (paleooceany), a ich osady wypiętrzyły się tworząc łańcuchy górskie (m.in. Himalaje). Dzisiejsze oceany Atlantycki, Arktyczny i Indyjski są geologicznie młodymi oceanami, które powstały w erze mezozoicznej i rozrastają się obecnie kosztem Pacyfiku. The Ocean Media Institute is a global media collective that serves to create, educate, and advocate for the protection of the ocean. 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