2005
DOI: 10.1038/nature04095
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Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms

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Cited by 3,899 publications
(3,211 citation statements)
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References 49 publications
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“…Many marine organisms are very sensitive to changes in ocean CO 2 chemistry -especially those biota that use carbonate ions dissolved in the sea water to form protective calcium carbonate shells or skeletal structures. Surface ocean pH has decreased by about 0.1 pH units (corresponding to a 30% increase in hydrogen ion concentration and a 16 % decline in carbonate concentrations) since pre-industrial times (Guinotte et al 2003;Feely et al, 2004;Orr et al, 2005;Guinotte & Fabry, 2008;Doney et al, 2009). This rate of acidification is at least 100 times faster than at any other time in the last 20 million years.…”
Section: Ocean Acidificationmentioning
confidence: 99%
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“…Many marine organisms are very sensitive to changes in ocean CO 2 chemistry -especially those biota that use carbonate ions dissolved in the sea water to form protective calcium carbonate shells or skeletal structures. Surface ocean pH has decreased by about 0.1 pH units (corresponding to a 30% increase in hydrogen ion concentration and a 16 % decline in carbonate concentrations) since pre-industrial times (Guinotte et al 2003;Feely et al, 2004;Orr et al, 2005;Guinotte & Fabry, 2008;Doney et al, 2009). This rate of acidification is at least 100 times faster than at any other time in the last 20 million years.…”
Section: Ocean Acidificationmentioning
confidence: 99%
“…Even though globally-averaged ! arag values in surface waters remain above unity for a doubling of atmospheric CO 2 , large parts of the Southern Ocean and the Arctic Ocean are projected to become undersaturated with respect to aragonite as early as 2030-2060 (Orr et al 2005;McNeil and Matear 2008;Steinacher et al, 2009). Aragonite undersaturation means that these waters will become corrosive to the aragonite and high-magnesium calcite shells secreted by a wide variety of marine organisms.…”
Section: Ocean Acidificationmentioning
confidence: 99%
“…Increased p CO 2 in surface waters alters the carbonate chemistry of sea water, ultimately increasing hydrogen ion (H + ), bicarbonate ion (HCO 3 − ), and dissolved inorganic carbon (DIC) concentrations and decreasing pH and carbonate ion (CO 3 2− ) concentrations. This process is termed ocean acidification (Caldeira & Wickett, 2003; Orr, Fabry, & Aumont, 2005). While occurring in all of the world's oceans, the largest changes in carbonate chemistry are expected to occur in the Arctic seas (Steinacher et al., 2009; Bellerby, Anderson, & Azetsu‐Scott, 2013).…”
Section: Introductionmentioning
confidence: 99%
“…uring the past two centuries, human activities exerted a growing influence over the global climate system, mostly through greenhouse gas emissions and chiefly CO 2 derived from burning fossil fuels 1,2 . This increasing global footprint of human activities on the biosphere has led some to use the term 'the Anthropocene' , to denote the present period of anthropogenically induced global environmental change 3 .…”
mentioning
confidence: 99%