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New Study Reveals How Sensitive U.S. East Coast Regions May Be to Ocean Acidification

By Guest PostApril 1, 2013Environmentacidic, acidic environment, bicarbonate, buffer capacity, carbon dioxide, carbon in ocean, carbonate, carbonic acid, changes in acidity, chemical survey, CO2, co2 levels, coastal ocean acidification, continental scale, coral, corpus christi, dic, dissolved co2, dissolved inorganic carbon, florida strait, galveston, georgia, glaciers, gulf of maine, gulf of mexico, influx of co2, labrador sea, melting sea ice, middle atlantic bight, Mississippi, ocean acidification, offshore, oysters, pteropods, rik wanninkhof, robert h byrne, ronald h brown, snails, texas, total alkalinity, tsung hung peng, university of georgia, us east coast, water ph, whoi, wie jen huang, wie jun cai, xinping hu, zhaohui aleck wang

A continental-scale chemical survey in the waters of the eastern U.S. and Gulf of Mexico is helping researchers determine how distinct bodies of water will resist changes in acidity. The study, which measures varying levels of carbon dioxide (CO₂) and other forms of carbon in the ocean, was conducted by scientists from 11 institutions across the U.S. and was published in the journal Limnology and Oceanography.

“Before now, we haven’t had a very clear picture of acidification status on the east coast of the U.S.,” says Zhaohui ‘Aleck’ Wang, the study’s lead author and a chemical oceanographer at Woods Hole Oceanographic Institution (WHOI). “It’s important that we start to understand it, because increase in ocean acidity could deeply affect marine life along the coast and has important implications for people who rely on aquaculture and fisheries both commercially and recreationally.” (more…)

Rising Carbon Dioxide Levels at End of Last Ice Age Not Tied to Pacific Ocean, As Had Been Suspected

By Guest PostOctober 9, 2011Environmentalan mix, carbon dioxide, co2 levels, coast of southwestern oregon, continental ice sheets, david lund, deep ocean, glacial times, heat trapping greenhouse gas, irvine, john southon, last ice age, levels of atmospheric carbon dioxide, microscopic shells, oregon state university, paleoclimatologist, plankton, radiocarbon dating, reservoir of carbon during glacial times, sediment core, university of california, university of michigan, ventilation rate

ANN ARBOR, Mich.— After the last ice age peaked about 18,000 years ago, levels of atmospheric carbon dioxide rose about 30 percent. Scientists believe that the additional carbon dioxide—a heat-trapping greenhouse gas—played a key role in warming the planet and melting the continental ice sheets. They have long hypothesized that the source of the gas was the deep ocean.

But a new study by a University of Michigan paleoclimatologist and two colleagues suggests that the deep ocean was not an important source of carbon during glacial times. The finding will force researchers to reassess their ideas about the fundamental mechanisms that regulate atmospheric carbon dioxide over long time scales. (more…)

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New Study Reveals How Sensitive U.S. East Coast Regions May Be to Ocean Acidification

Rising Carbon Dioxide Levels at End of Last Ice Age Not Tied to Pacific Ocean, As Had Been Suspected