{"id":28,"date":"2014-05-27T14:14:38","date_gmt":"2014-05-27T14:14:38","guid":{"rendered":"http:\/\/blog.ldeo.columbia.edu\/2014report\/?page_id=28"},"modified":"2015-02-10T19:05:42","modified_gmt":"2015-02-10T19:05:42","slug":"oceanacidification","status":"publish","type":"page","link":"https:\/\/blog.ldeo.columbia.edu\/2014report\/research\/oceanacidification\/","title":{"rendered":"Ocean Acidification"},"content":{"rendered":"

Modern Ocean Acidification Is Outpacing Ancient Upheaval<\/strong><\/p>\n

Some 56 million years ago, a massive pulse of carbon dioxide added to the atmosphere sent global temperatures soaring. In the oceans, carbonate sediments dissolved, some organisms went extinct and others evolved.<\/p>\n

Scientists have long suspected that ocean acidification caused the crisis\u2014similar to today, as manmade CO2<\/sub> combines with seawater to change its chemistry. Now, for the first time, researchers have quantified the extent of surface acidification from those ancient days, and the news is not good: the oceans are on track to acidify at least as much as they did then, only at a much faster rate.<\/p>\n

The scientists estimate that ocean acidity increased by about 100 percent in a few thousand years or more, and stayed that way for the next 70,000 years. In that radically changed environment, some creatures died out whereas others adapted and evolved. The study is the first to use the chemical composition of fossils to reconstruct surface ocean acidity at the Paleocene-Eocene Thermal Maximum (PETM), a period of intense warming on land and throughout the oceans as a result of high levels of CO2<\/sub>.<\/p>\n

\u201cThis could be the closest geological analog to modern ocean acidification,\u201d said Lamont paleoceanographer and study co-author B\u00e4rbel H\u00f6nisch. \u201cAs massive as it was, it still happened about 10 times more slowly than what we are doing today.\u201d<\/p>\n

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Ocean acidification in the modern ocean is already affecting some marine life, as shown by the partly dissolved shell of this planktic snail, or pteropod, caught off the Pacific Northwest. (Nina Bednar\u0161ek\/NOAA)<\/p><\/div>\n

The oceans have absorbed about a third of the carbon humans have pumped into the air since industrialization, helping to keep Earth\u2019s thermostat lower than it would be otherwise. But that uptake of carbon has come at a price. Chemical reactions caused by that excess CO2<\/sub> have made seawater grow more acidic, limiting the uptake of carbonate ions that corals, mollusks and calcifying plankton need to build their shells and skeletons.<\/p>\n

In the last 150 years or so, the pH of the oceans has dropped substantially, from 8.2 to 8.1\u00a0\u2013\u00a0equivalent to a 25 percent increase in acidity. By the end of the century, ocean pH is projected to fall another 0.3 pH units, to 7.8. Although the researchers found a comparable pH drop during the PETM \u2013 0.3 units \u2013\u00a0the shift happened over a few thousand years.<\/p>\n

\u201cWe are dumping carbon into the atmosphere and ocean at a much higher rate today\u2014within centuries,\u201d said study coauthor Richard Zeebe, a paleoceanographer at the University of Hawaii. \u201cIf we continue on the emissions path we are on right now, acidification of the surface ocean will be way more dramatic than during the PETM.\u201d<\/p>\n

From seafloor sediments drilled off Japan, the researchers analyzed the shells of plankton that lived at the surface of the ocean during the PETM. Two different methods for measuring ocean chemistry at the time \u2013\u00a0the ratio of boron isotopes in their shells, and the amount of boron \u2013 yielded similar estimates of acidification.<\/p>\n

What caused the burst of carbon at the PETM is still unclear. One popular explanation is that an overall warming trend may have sent a pulse of methane from seafloor sediments into the atmosphere, setting off events that released more Earth-warming gases into the air and oceans. Up to half of the tiny animals that live in mud on the seafloor \u2013 benthic foraminifera \u2013\u00a0died out during the PETM, possibly along with life further up the food chain.<\/p>\n

Other species thrived in this changed environment and new ones evolved. In the oceans, dinoflagellates extended their range from the tropics to the Arctic, while on land, hoofed animals and primates appeared for the first time. Eventually, the oceans and atmosphere recovered as elements from eroded rocks washed into the sea and neutralized the acid.<\/p>\n

Today, signs are already emerging that some marine life may be in trouble. In a recent study led by Nina Bednar\u0161ek at the U.S. National Oceanic and Atmospheric Administration, more than half of the tiny planktic snails, or pteropods, that she and her team studied off the coast of Washington, Oregon and California showed badly dissolved shells. Ocean acidification has been linked to the widespread death of baby oysters off Washington and Oregon since 2005, and may also pose a threat to coral reefs, which are under additional pressure from pollution and warming ocean temperatures.<\/p>\n

\u201cSeawater carbonate chemistry is complex, but the mechanism underlying ocean acidification is very simple,\u201d said study lead author Donald Penman, a graduate student at University of California at Santa Cruz. \u201cWe can make accurate predictions about how carbonate chemistry will respond to increasing carbon dioxide levels. The real unknown is how individual organisms will respond and how that response cascades through ecosystems.\u201d<\/p>\n","protected":false},"excerpt":{"rendered":"

Modern Ocean Acidification Is Outpacing Ancient Upheaval Some 56 million years ago, a massive pulse of carbon dioxide added to the atmosphere sent global temperatures soaring. In the oceans, carbonate sediments dissolved, some organisms went extinct and others evolved. Scientists have long suspected that ocean acidification caused the crisis\u2014similar to today, as manmade CO2 combines […]<\/p>\n","protected":false},"author":17,"featured_media":0,"parent":24,"menu_order":20,"comment_status":"closed","ping_status":"closed","template":"","meta":{"__cvm_playback_settings":[],"__cvm_video_id":""},"_links":{"self":[{"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/pages\/28"}],"collection":[{"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/users\/17"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/comments?post=28"}],"version-history":[{"count":10,"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/pages\/28\/revisions"}],"predecessor-version":[{"id":408,"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/pages\/28\/revisions\/408"}],"up":[{"embeddable":true,"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/pages\/24"}],"wp:attachment":[{"href":"https:\/\/blog.ldeo.columbia.edu\/2014report\/wp-json\/wp\/v2\/media?parent=28"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}