An artist rendering of a Southern Ocean pteropod. (Illustration: Kristen Krumhardt/University of Colorado Boulder)
Marine microorganisms in the Southern Ocean may find themselves in a deadly vise grip by century鈥檚 end as ocean acidification creates a shallower horizon for life, new 抖阴旅行射 Boulder research finds.
The modeling study, in the journal听Nature Climate Change, forecasts that at current carbon dioxide emission rates, the depth at which some shelled organisms can survive will shrink from an average of 1,000 meters today to just 83 meters by the year 2100, a drastic reduction in viable habitat.
The steep drop, which could happen suddenly over a period as short as one year in localized areas, could impact marine food webs significantly and lead to cascading changes across ocean ecosystems, including disruptions of vital global fisheries.
Acidification occurs when oceans absorb atmospheric carbon dioxide (CO2) created by burning fossil fuels. The absorption alters the water鈥檚 chemistry, lowering its pH and reducing the amount of available carbonate, which microorganisms like corals and pteropods use to construct their calcium carbonate shells.
鈥淭hese calcifying organisms will struggle to build and maintain their shells as acidification proceeds,鈥� said Nicole Lovenduski, corresponding author of the study and a professor in 抖阴旅行射 Boulder鈥檚听Department of Atmospheric and Oceanic Sciences听(ATOC) and听听鈥淚n the future, a pocket of corrosive water will sit just below the surface, making life difficult for these communities of primarily surface-dwelling organisms.鈥�
鈥淭his study shows that our current carbon dioxide emission rates are influencing not only the chemistry of the Southern Ocean but its food web structure as well,鈥� said Simone Metz, program director in the National Science Foundation鈥檚 Division of Ocean Sciences, which funded the research.听
The Southern Ocean is particularly vulnerable to acidification due to colder waters which increase the solubility of CO2听as well as persistent upwelling that brings carbon-rich water close to the surface.
The study, led by then-抖阴旅行射 Boulder undergraduate research assistant Gabriela Negrete-Garc铆a, used data from the Community Earth System Model (CESM) to forecast ocean acidification under several CO2听emission assumption scenarios, looking specifically at the changes in calcium carbonate saturation. The team also examined water samples collected from previous ship-board expeditions to the Southern Ocean.
鈥淲e suspect that previous studies have overlooked the emergence of the shallow horizon by averaging together data from a number of different models as opposed to looking at individual model realizations,鈥漵aid Negrete-Garc铆a, formerly of INSTAAR and now a graduate student at the Scripps Institution of Oceanography.
While the individual simulations of the model differed on the timing of the threshold change鈥攚ith some predicting it as early as 2006 and others as late as 2038鈥攖he research suggests that the change may be an inevitability in large regions of the Southern Ocean regardless of future mitigation efforts.
鈥淚f emissions were curbed tomorrow, this suddenly shallow horizon would still appear, even if possibly delayed,鈥� Lovenduski said. 鈥淎nd that inevitability, along with the lack of time for organisms to adapt, is most concerning.鈥�
Additional co-authors of the study included Kristen Krumhardt of 抖阴旅行射 Boulder, Claudine Hauri of the University of Alaska Fairbanks and Siv Lauvset of the NORCE Norwegian Research Centre. The National Science Foundation provided funding for the research.
