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Od czasu odkrycia w latach 50. XX w. zjawiska ekspansji dna oceanicznego, czyli powstawania zupełnie nowej skorupy ziemskiej w strefach grzbietów śródoceanicznych, oraz w wyniku badań wieku osadów oceanicznych i samej skorupy, rozwinęło się kilka teorii geotektonicznych, spośród których powszechnie dziś akceptowana jest teoria tektoniki płyt. But even more alarming was the suspicion of the Russians. To convince them that Howard Hughes was genuinely interested in nodules, executives were despatched to conferences on ocean mining where they described in detail their plans to harvest the rocks. Our oceans have absorbed most of the planet’s warming—over 90%—and a significant amount of our carbon pollution. Warmer oceans are driving stronger storms and bleaching coral reefs. As oceans absorb carbon dioxide, they become more acidic, threatening most shelled organisms, including small crustaceans fundamental to the marine food chain. The pelagic zone can be further subdivided into two subregions: the neritic zone and the oceanic zone. The neritic zone encompasses the water mass directly above the continental shelves whereas the oceanic zone includes all the completely open water. Together we’re building an online community for people to share ideas, collaborate, and invent technology that could help keep our oceans healthy. The Ocean Media Institute is a global media collective that serves to create, educate, and advocate for the protection of the ocean. As a creative hub for individuals and organizations worldwide, our goal is to work in collaboration with artists and filmmakers, organizations and academic institutions, aquaria and museums to produce, exhibit, and openly distribute media that promotes public understanding of ocean science and conservation. Endangered Waves can empower and incentivize surfers (there are 24 million worldwide) to monitor the health of their coastlines through crowdsourced data. Surfers can use this app to create crowdsourced data to identify and then reduce hazards in their local surf breaks. In the US, tourism and recreation comprise 72% of employment in the ocean economy and 31% of its gross value. Creating apps that cater to this market isn’t indulgent, it’s good business sense. Wiatry wiejące nad rozległymi obszarami wodnymi powodują powstawanie na powierzchni oceanu fal. Katastrofalne zjawiska, takie jak podwodne trzęsienia ziemi, wybuchy wulkanów czy rozległe osuwiska wywołują niszczące fale tsunami. Znacznie rzadziej tsunami może powstać na skutek upadku planetoidy, która trafi w powierzchnię oceanu. “We invest a lot of money and enthusiasm for missions to space – but there’s nothing living out there. The sea bed is teeming with life. We really need a mission to planet ocean – it’s the last frontier.” He was still chuckling when he spoke, sage from much experience of ocean travel. Według hipotezy ekspandującej Ziemi powstanie oceanów było aktem jednorazowym. Zgodnie z nią rozrost skorupy powoduje powiększanie się wszystkich oceanów i całej planety, był więc taki moment, kiedy nie było na Ziemi oceanów w dzisiejszym znaczeniu. Hipoteza ta nie potrafi wytłumaczyć istnienia ofiolitów, czyli zespołów skał identycznych z powstającymi pod powierzchnią oceanów, a znajdujących się obecnie niekiedy w głębi kontynentu. Resources are available for GIS for ocean planning and for aid transparency. We’ve drilled the ocean floor for oil and gas, scarred it with trenches for communications cables, poisoned it with old radioactive waste and chemical weapons, and polluted its remotest corners with a blizzard of discarded plastic. So, is mining a step too far? In fact, getting to the deepest reaches of the ocean is so expensive that some people – like Oscar-winning director James Cameron – take it upon themselves to explore underwater spaces rarely visited by humans. Lifeforms native to the ocean include: One of the authors, Prof Edward Hill from the UK National Oceanography Centre told BBC News: “The ocean is critical to our economic future. Nine billion people will be looking to the ocean for more food. Yet we know so little of what’s down there. It’s always been there, but a layer of the ocean is so distinct from the waters above and below it that it needed its own category. Scientists surveying an ocean area targeted for deep-sea mining have shown how much is left to discover about the biodiversity of the Clarion-Clipperton Zone, a five-million-square-kilometre region in the central Pacific Ocean. Dr Bruno Simões tells us how he pursued sea snakes from the mangroves to the open ocean to learn about their vision. The first inkling that the ocean floor might hold a treasure trove of minerals came in the late 19th Century when a Royal Navy ship, HMS Challenger, was sent on a pioneering expedition. Instead of exploring the coasts of new lands, the ship was to investigate the oceans themselves. Cod spawn in normal, cold, and lukewarm oceans. The value of the world’s oceans is set to double by 2030 but we know less about the bottom of the sea than we do about Mars. The deep ocean houses an ecosystem that has learned to thrive without sunlight or warmth. Welcome to the abyss. email : biuro@karchercenter-ocean.pl Od czasu odkrycia w latach 50. XX w. zjawiska ekspansji dna oceanicznego, czyli powstawania zupełnie nowej skorupy ziemskiej w strefach grzbietów śródoceanicznych, oraz w wyniku badań wieku osadów oceanicznych i samej skorupy, rozwinęło się kilka teorii geotektonicznych, spośród których powszechnie dziś akceptowana jest teoria tektoniki płyt. Stay in touch with others in the oceans industry who are interested in GIS and location analytics. Join the conversation on GeoNet. Earth may be the blue planet, but beneath the ocean waves lies a vast forest of green.  WWF is working collaboratively on the brightest conservation ideas that focus on building a more resilient ocean through sustainable fishing practices and protecting important regions, like the Arctic and threatened mangrove forests. Pledge to work together to solve the world’s greatest environmental problems and protect our oceans. The geologist Bram Murton has warned of “an ill-informed knee-jerk reaction” to ocean mining which, he says, offers the potential to support a low-carbon future. Ocean & Coastal Management is an international journal published 12 times per year dedicated to the study of all aspects of ocean and coastal management at international, national, regional, and local levels. Research ships are vital for advancing marine science but are costly to operate. Oscar Pizarro, a scientist at the University of Sydney’s Australian Centre for Field Robotics and the Schmidt Ocean Institute, thinks automated expeditions are the future of ocean science.about 1 month ago Our mission is to explore our global ocean, inspiring and educating people throughout the world to act responsibly for its protection, documenting the critical connection between humanity and nature, and celebrating the ocean’s vital importance to the survival of all life on our planet. “We have largely thought of fish as very alien and very simple, so we didn’t really care how we killed them,” Braithwaite says. “If we look at trawl netting, that’s a pretty gruesome way for fish to die: the barometric trauma of getting ripped from the ocean into open air, and then slowly suffocating. Can we do that more humanely? Yes. Should we? Probably, yes. We’re mostly not doing it at the moment because it’s more expensive to kill fish humanely, especially in the wild.” We cannot manage what we cannot measure. The following are examples of ocean management applications that will be supported by improved data and knowledge generated under the UN Decade of Ocean Science for Sustainable Development: 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. 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