Is Ocean Acidification an Open-Ocean Syndrome? Understanding Anthropogenic Impacts on Seawater pH

Ocean acidification due to anthropogenic CO2 emissions is a dominant driver of long-term changes in pH in the open ocean, raising concern for the future of calcifying organisms, many of which are present in coastal habitats. However, changes in pH in coastal ecosystems result from a multitude of dri...

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Bibliographic Details
Published in:Estuaries and Coasts
Main Authors: Duarte, Carlos M., Hendriks, Iris E., Moore, Tommy S., Olsen, Ylva S., Steckbauer, Alexandra, Ramajo, Laura, Carstensen, Jacob, Trotter, Julie A., McCulloch, Malcom
Other Authors: Ministerio de Economía y Competitividad (España), European Commission, Commonwealth Scientific and Industrial Research Organisation (Australia), Baltic Nest Institute (Sweden)
Format: Article in Journal/Newspaper
Language:English
Published: Estuarine Research Federation 2013
Subjects:
pH
Online Access:http://hdl.handle.net/10261/88859
https://doi.org/10.1007/s12237-013-9594-3
https://doi.org/10.13039/501100003329
https://doi.org/10.13039/501100000780
https://doi.org/10.13039/501100000943
Description
Summary:Ocean acidification due to anthropogenic CO2 emissions is a dominant driver of long-term changes in pH in the open ocean, raising concern for the future of calcifying organisms, many of which are present in coastal habitats. However, changes in pH in coastal ecosystems result from a multitude of drivers, including impacts from watershed processes, nutrient inputs, and changes in ecosystem structure and metabolism. Interaction between ocean acidification due to anthropogenic CO2 emissions and the dynamic regional to local drivers of coastal ecosystems have resulted in complex regulation of pH in coastal waters. Changes in the watershed can, for example, lead to changes in alkalinity and CO2 fluxes that, together with metabolic processes and oceanic dynamics, yield high-magnitude decadal changes of up to 0.5 units in coastal pH. Metabolism results in strong diel to seasonal fluctuations in pH, with characteristic ranges of 0.3 pH units, with metabolically intense habitats exceeding this range on a daily basis. The intense variability and multiple, complex controls on pH implies that the concept of ocean acidification due to anthropogenic CO2 emissions cannot be transposed to coastal ecosystems directly. Furthermore, in coastal ecosystems, the detection of trends towards acidification is not trivial and the attribution of these changes to anthropogenic CO2 emissions is even more problematic. Coastal ecosystems may show acidification or basification, depending on the balance between the invasion of coastal waters by anthropogenic CO2, watershed export of alkalinity, organic matter and CO2, and changes in the balance between primary production, respiration and calcification rates in response to changes in nutrient inputs and losses of ecosystem components. Hence, we contend that ocean acidification from anthropogenic CO2 is largely an open-ocean syndrome and that a concept of anthropogenic impacts on marine pH, which is applicable across the entire ocean, from coastal to open-ocean environments, provides a superior ...