<p><span style="font-weight: 400;">Prior to the Industrial Revolution of the 18th and 19th centuries, global oxygen levels had remained relatively stable for millions of years. As atmospheric carbon dioxide concentrations increase due to the burning of fossil fuels, excess heat from the Sun gets trapped, which in turn raises average ocean temperatures.</span></p><p><div data-conversation-spotlight=""></div></p><p><span style="font-weight: 400;">Because of its naturally volatile state, atomic oxygen doesn’t accumulate on Earth in large quantities; oxygen supplies in the ocean and atmosphere continuously regenerate so that fish, mammals and terrestrial life can flourish. In fact,</span><a href="http://earthsky.org/earth/how-much-do-oceans-add-to-worlds-oxygen"> <span style="font-weight: 400;">50-85 percent</span></a><span style="font-weight: 400;"> of Earth’s oxygen is generated by phytoplankton, tiny algae that release oxygen through photosynthesis.</span></p><p class="shortcode-media shortcode-media-rebelmouse-image"><img type="lazy-image" data-runner-src="https://assets.rebelmouse.io/eyJhbGciOiJIUzI1NiIsInR5cCI6IkpXVCJ9.eyJpbWFnZSI6Imh0dHBzOi8vYXNzZXRzLnJibC5tcy8yMjA0MTI5Ni9vcmlnaW4uanBnIiwiZXhwaXJlc19hdCI6MTY1MDcwOTQ4Nn0.N_4f_kqj3MX9Sjl2iw3ogxFVC5SvT6J3DElU51F-y0o/img.jpg?width=980" id="38fb6" class="rm-shortcode" data-rm-shortcode-id="c5f97641e3975bebd46952695be138a7" data-rm-shortcode-name="rebelmouse-image"><small class="image-media media-caption" placeholder="add caption...">Phytoplankton. Source: <a href="https://assets.rbl.ms/22041301/origin.jpg">National Oceanic and Atmospheric Administration</a></small></p><p><span style="font-weight: 400;">As temperatures in Earth’s oceans rise, natural processes like photosynthesis that release oxygen into the water cannot keep up with demand. Warm water does not hold onto atomic oxygen. Individual oxygen atoms are unstable (making it highly combustible, hence its use as rocket fuel) and bond with other oxygen atoms to form O2, which comprises 20 percent of Earth’s atmosphere. Molecules of O2 also bond with oxygen atoms to form O3 (ozone), the thin atmospheric layer that blocks ultraviolet light from the Sun. Furthermore, oxygen atoms bond with other elements, like carbon, to form compounds like carbon dioxide, leading to a feedback loop of more surface heating.</span></p><p><span style="font-weight: 400;">Climate change was also determined to be the cause of “</span><a href="http://www.independent.co.uk/environment/ocean-heatwaves-climate-change-sea-temperature-rise-bleaching-sea-life-fish-global-warming-a8162096.html"><span style="font-weight: 400;">the blob</span></a><span style="font-weight: 400;">;” an enormous heatwave in 2016 that affected a quarter of the world’s oceans. Excess ocean heat decimated ecosystems throughout the oceans and led to the death of countless marine organisms. In a </span><a href="http://www.ametsoc.net/eee/2016/2016_bams_eee_low_res.pdf"><span style="font-weight: 400;">study</span></a><span style="font-weight: 400;"> in the </span><i><span style="font-weight: 400;">Bulletin of the American Meteorological Society</span></i><span style="font-weight: 400;">, lead researcher Dr. Eric Oliver and his team analyzed the effects “the blob” had on the seas off Australia’s northern coast, as well as the northern Pacific Ocean between Russia and Alaska. Heatwaves, like the blob in 2016, are responsible for killing thousands of marine animals, including birds and whales. Increases in oceanic heat also lead to the bleaching of coral reefs, such as the Great Barrier Reef in Australia. </span></p><p><span style="font-weight: 400;">“S</span><span style="font-weight: 400;">cientists are inherently conservative about making grand claims, but we can say with 99 percent confidence that anthropogenic climate change made this marine heatwave several times more likely, and there’s an increasing probability of such extreme events in the future,” Dr. Oliver concluded. The series of heatwaves comprising the blob were the longest lasting and most intense ever recorded.</span></p><p></p><p><b>Climate change and pollution are literally choking Earth’s oceans.</b></p><p><span style="font-weight: 400;">Researchers at Arizona State University published the largest ever</span><a href="http://advances.sciencemag.org/content/3/8/e1701020.full"> <span style="font-weight: 400;">study</span></a><span style="font-weight: 400;"> of dead zones and coastal hypoxia in the journal </span><i><span style="font-weight: 400;">Science Advances.</span></i><span style="font-weight: 400;"> Scientists hoped to understand how dead zones occur from natural processes. Around 94 million years ago, Earth experienced an “Oceanic Anoxic Event” (named OAE-2) in which oxygen levels in the oceans decreased, driven by “various combinations of increased surface temperatures (</span><a href="http://advances.sciencemag.org/content/3/8/e1701020.full#ref-2"><i><span style="font-weight: 400;">2</span></i></a><span style="font-weight: 400;">), sea level rise (</span><a href="http://advances.sciencemag.org/content/3/8/e1701020.full#ref-3"><i><span style="font-weight: 400;">3</span></i></a><span style="font-weight: 400;">), nutrient trapping (</span><a href="http://advances.sciencemag.org/content/3/8/e1701020.full#ref-4"><i><span style="font-weight: 400;">4</span></i></a><span style="font-weight: 400;">), and pulses of magmatic activity,” study leader Chandlin M. Ostrander explains. The 50,000-year-long event led to a major extinction, wiping out 27 percent of marine invertebrates.</span></p><p><span style="font-weight: 400;">While Cretaceous Era OAE-2 was the result of an uptick in global volcanic activity, the study concludes that “increased ocean deoxygenation is already apparent in the modern ocean, because marine O2 has decreased by 2% over roughly the last half century (</span><a href="http://advances.sciencemag.org/content/3/8/e1701020.full#ref-41"><i><span style="font-weight: 400;">41</span></i></a><span style="font-weight: 400;">), and recent models predict a continued loss of 0.5 to 3.5% over the next half century (</span><a href="http://advances.sciencemag.org/content/3/8/e1701020.full#ref-1"><i><span style="font-weight: 400;">1</span></i></a><span style="font-weight: 400;">,</span><a href="http://advances.sciencemag.org/content/3/8/e1701020.full#ref-42"> <i><span style="font-weight: 400;">42</span></i></a><span style="font-weight: 400;">), which would result in huge expansions of ocean anoxia within the next few thousand years.” While these processes (minus human pollution) do happen naturally,, industrialized society is responsible for the rate at which oceanic oxygen is dropping.</span></p><p><span style="font-weight: 400;">Simply put, human activity is causing another Oceanic Anoxic Event.</span></p><p><span style="font-weight: 400;">Further evidence of humanity’s detrimental effect on Earth’s oceans can be found in a second </span><i><span style="font-weight: 400;">Science</span></i><a href="http://science.sciencemag.org/content/359/6371/eaam7240"> <span style="font-weight: 400;">study</span></a><span style="font-weight: 400;"> published in January 2018. “In the open ocean, global warming, which is primarily caused by increased greenhouse gas emissions, is considered the primary cause of ongoing deoxygenation,” explains lead researcher Denise Breitburg. “Expansion of low-oxygen zones can increase production of N2O, a potent greenhouse gas; reduce eukaryotic biodiversity; alter the structure of food webs; and negatively affect food security and livelihoods.” Nitrous oxide (N2O) is a powerful greenhouse gas produced in low-oxygen zones. Although it has a shorter half-life than carbon dioxide, its heat-trapping ability is hundreds of times stronger. </span></p><p><span style="font-weight: 400;">Hypoxic zones, which are being found off every inhabited coastal region on Earth, are driven by toxic, chemical-laden runoff. Coastal human habitation is the </span><i><span style="font-weight: 400;">only</span></i><span style="font-weight: 400;"> cause of coastal hypoxia. </span></p><p><span style="font-weight: 400;">Since 1950, oxygen-empty oceanic “dead zones” have quadrupled and coastal regions of perilously low oxygen levels have multiplied by a factor of ten (there are at least 500 known), according to a UNESCO-led</span><a href="http://www.unesco.org/new/en/natural-sciences/ioc-oceans/sections-and-programmes/ocean-sciences/global-ocean-oxygen-network/"> <span style="font-weight: 400;">analysis</span></a><span style="font-weight: 400;"> of Breitburg’s</span><a href="http://science.sciencemag.org/content/359/6371/eaam7240"> <span style="font-weight: 400;">study</span></a><span style="font-weight: 400;">. Unfortunately, these areas are only what have been observed thus far. There could be many more coastal hypoxia zones where monitoring efforts are either non-existent or still in their infancy. </span></p><p><span style="font-weight: 400;">The largest</span><a href="https://www.epa.gov/nutrientpollution/effects-dead-zones-and-harmful-algal-blooms"> <span style="font-weight: 400;">dead zone</span></a><span style="font-weight: 400;"> is in the Gulf of Mexico, covering in excess of 10,000 square kilometers. Prof Robert Diaz at the Virginia Institute of Marine Science, who reviewed the new study, offered a sobering</span><a href="https://www.theguardian.com/environment/2018/jan/04/oceans-suffocating-dead-zones-oxygen-starved"> <span style="font-weight: 400;">claim</span></a><span style="font-weight: 400;">: "no other variable of such ecological importance to coastal ecosystems has changed so drastically in such a short period of time from human activities as dissolved oxygen.”</span></p><p></p><p><span style="font-weight: 400;">Dead zones in the open ocean now encompass 4.5 million square kilometers, equivalent to the area of 46 percent of the continental United States.</span></p><p><span style="font-weight: 400;">“This is mainly the result of human activities that are increasing global temperatures (CO2-induced warming) and increasing loads of nutrients from agriculture, sewage, and industrial waste, including pollution from power generation from fossil fuels and biomass,” states the</span><a href="http://www.unesco.org/new/en/natural-sciences/ioc-oceans/sections-and-programmes/ocean-sciences/global-ocean-oxygen-network/"> <span style="font-weight: 400;">Global Ocean Oxygen Network</span></a><span style="font-weight: 400;"> (GO2NE), the faction of</span><a href="https://en.unesco.org/"> <span style="font-weight: 400;">UNESCO</span></a><span style="font-weight: 400;"> that performed the analysis. GO2NE is “committed to providing a global and multidisciplinary view of deoxygenation, with a focus on understanding its multiple aspects and impacts.” </span></p><p><span style="font-weight: 400;">Phytoplankton rapidly multiply in nutrient-rich environments, which pollutants containing nitrates and phosphates provide. Initially, a dense colony of algae releases some oxgyen, but the boon is short-lived. Swarms of surface algae prevent sunlight from reaching underwater plant life, killing it and its essential production of oxygen. When large, concentrated populations of phytoplankton run out of food and die en masse, they sink to the ocean floor where they are broken down by microbes and other organisms. These microscopic scavengers also consume substantial amounts of oxygen, furthering overall oceanic depletion. Once all the remaining oxygen is used up, hypoxic zones become dead zones.</span></p><p class="shortcode-media shortcode-media-rebelmouse-image"><img type="lazy-image" data-runner-src="https://assets.rebelmouse.io/eyJhbGciOiJIUzI1NiIsInR5cCI6IkpXVCJ9.eyJpbWFnZSI6Imh0dHBzOi8vYXNzZXRzLnJibC5tcy8yMjA0MTI5OC9vcmlnaW4uanBnIiwiZXhwaXJlc19hdCI6MTYzNDE1MTE1Mn0.n4vb4rBcjZ7lnS0-_dVF7ARQM9tj7w9-pLS_EB1vgJ4/img.jpg?width=980" id="57cf6" class="rm-shortcode" data-rm-shortcode-id="67804d46fdcfb776634cd6e3d12a0b67" data-rm-shortcode-name="rebelmouse-image"><small class="image-media media-caption" placeholder="add caption..."><a href="https://assets.rbl.ms/22041302/origin.jpg"></a> Gulf of Mexico Algae Bloom, 2017. Source: <a href="https://assets.rbl.ms/22041302/origin.jpg">Inhabitat</a></small></p><p><span style="font-weight: 400;">In its analysis, GO2NE identifies ten alarming trends in declining oxygen levels in Earth’s oceans:</span></p><p><span style="font-weight: 400;">“Increasing temperatures will reduce the capacity of the ocean to hold oxygen in the future;</span></p><ol class="ee-ol"><li style="font-weight: 400;"><span style="font-weight: 400;">Oxygen deficiency is predicted to worsen in estuaries, coastal areas and oxygen minimum zones in the open ocean;</span></li><li style="font-weight: 400;"><span style="font-weight: 400;">The ocean’s capacity to produce oxygen will be reduced in the future.</span></li><li style="font-weight: 400;"><span style="font-weight: 400;">Habitat loss is expected to worsen, leading to vertical and horizontal migration of species;</span></li><li style="font-weight: 400;"><span style="font-weight: 400;">Oxygen deficiency will alter biogeochemical cycles and food webs;</span></li><li style="font-weight: 400;"><span style="font-weight: 400;">Lower oxygen concentrations are projected to result in a decrease in reproductive capacity and biodiversity loss;</span></li><li style="font-weight: 400;"><span style="font-weight: 400;">There are important local decreases of commercially important species and aquaculture production;</span></li><li style="font-weight: 400;"><span style="font-weight: 400;">Harmful Algal Blooms might benefit from nutrients released in bottom waters due to hypoxia (e.g. in the Baltic Sea);</span></li><li style="font-weight: 400;"><span style="font-weight: 400;">Reduced ocean oxygen concentrations will lead to an increase in greenhouse gas emissions, thereby initiating feedbacks on climate change;</span></li><li style="font-weight: 400;"><span style="font-weight: 400;">Future scenarios for oxygen depend on a combination of drivers related to global environmental change and land-use, including warming, growing human population, and extensive coastal agricultural practices, which, in turn, act together in affecting marine ecosystems – thus, a multi-stressor approach is important."</span></li></ol><p class="shortcode-media shortcode-media-rebelmouse-image"><img type="lazy-image" data-runner-src="https://assets.rebelmouse.io/eyJhbGciOiJIUzI1NiIsInR5cCI6IkpXVCJ9.eyJpbWFnZSI6Imh0dHBzOi8vYXNzZXRzLnJibC5tcy8yMjA0MTI5OS9vcmlnaW4uanBnIiwiZXhwaXJlc19hdCI6MTYxNTY0NzY0N30.rBpzhNq-NeK58oK-akoHlf6l4mRQ81zqx3g1N748H5E/img.jpg?width=980" id="41220" class="rm-shortcode" data-rm-shortcode-id="830b5416e131290073b76a6f2eebd227" data-rm-shortcode-name="rebelmouse-image"><small class="image-media media-caption" placeholder="add caption...">Deoxygenation numbers and effects. Source: <a href="https://assets.rbl.ms/22041303/origin.jpg">UNESCO</a></small></p><p><span style="font-weight: 400;">The most important takeaway from the studies and subsequent analyses, however, is that the current Oceanic Anoxic Event is </span><i><span style="font-weight: 400;">entirely </span></i><span style="font-weight: 400;">preventable and completely reversible. By reducing and eliminating pollution-containing toxic runoff and carbon emissions, Earth’s oceans can recover, and global disaster can be avoided. But humans are stubborn creatures, and the longer we kick the proverbial can down the road, the higher the price future generations will pay for our willful and selfish inaction.</span></p><p><b>What consequences will civilization face if oxygen concentrations keep declining?</b></p><p class="shortcode-media shortcode-media-rebelmouse-image"><img type="lazy-image" data-runner-src="https://assets.rebelmouse.io/eyJhbGciOiJIUzI1NiIsInR5cCI6IkpXVCJ9.eyJpbWFnZSI6Imh0dHBzOi8vYXNzZXRzLnJibC5tcy8yMjA0MTMwMC9vcmlnaW4uanBnIiwiZXhwaXJlc19hdCI6MTY2NDIwNTk2OH0.SKjMY66vY_EbN8lPauaM774yVmuRmv-HpBSuiJlfdDU/img.jpg?width=980" id="5603d" class="rm-shortcode" data-rm-shortcode-id="ce89d2157cbef7ae574a8257f906455b" data-rm-shortcode-name="rebelmouse-image"><small class="image-media media-caption" placeholder="add caption..."><a href="https://assets.rbl.ms/22041305/origin.jpg"></a> Earth's coastal lights as seen from space. Source: <a href="https://visibleearth.nasa.gov/view.php?id=55167">NASA</a></small></p><p><span style="font-weight: 400;">In the image above, take note of how densely populated coastlines align perfectly with coastal hypoxic zones. More than 2.4 billion people, or a third of the human race, live within 100 kilometers of an oceanic coast.</span><a href="https://www.theguardian.com/environment/2018/jan/04/oceans-suffocating-dead-zones-oxygen-starved"> <span style="font-weight: 400;">Future coastal dead zones</span></a><span style="font-weight: 400;"> will be devoid of fish, which feed 500 million people and whose industry employs 350 million people around the world. Citizens of poorer countries will be the first to experience massive food shortages. To compensate, fishing rates will increase in healthier waters, but this will only exacerbate</span><a href="http://overfishing.org/"> <span style="font-weight: 400;">global over-fishing</span></a><span style="font-weight: 400;">. Overgrowth of algae in dead zones can also contaminate drinking water, leading to illness in people and fauna.</span></p><p><span style="font-weight: 400;">The same forces upsetting the balance of oxygen shifts in the oceans will affect various natural cycles that regulate Earth's climate. Warm oceans are the primary supply of energy for hurricanes and typhoons; coastal cities can expect inundation from ever-more powerful storm surges churned up by more intense tropical cyclones. In 2017, three mammoth hurricanes respectively slammed into Texas, Florida and Puerto Rico, killing over 1,000 people and causing over</span><a href="https://thesocialedgen.wpengine.com/environment/cost-of-climate-change/"> <span style="font-weight: 400;">$300 billion</span></a><span style="font-weight: 400;"> in damage. Hurricane Harvey, which drowned much of Houston, Texas, in September 2017, was the most expensive natural disaster in US history with a price tag of between $125 and $200 billion.</span></p><p><span style="font-weight: 400;">Humanity caused this, and humanity can fix it. The question is, will we?</span></p>
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