Predicted levels of aragonite saturation (ΩAr) in different areas of the Arctic Ocean. a) In 2050; b) in 2100 (S3). Area of the East Siberian Arctic Shelf (ESAS) marked by a black rectangle. Graphic: Semiletov, et al., 2016 / Nature Geoscience

18 April 2016 (Stockholm University) – When organic material released from thawing permafrost is transported to the sea it gets broken down in the seawater contributing to a more rapid acidification of the Arctic Ocean, finds new research by scientists from Stockholm University and colleagues.

Ocean acidification is an important consequence of humankind’s release of carbon dioxide (CO2) into the atmosphere from fossil fuel burning. It is widely thought that when excess atmospheric CO2 reacts with seawater it forms carbonic acid, which, in turn, “acidifies” the ocean, causing dramatic changes to ocean ecosystems. The Arctic Ocean is particularly sensitive to such changes. Now, a new study by scientists from Sweden, the USA, and Russia, published in Nature Geoscience proposes a novel mechanism for Arctic Ocean acidification involving release and subsequent breakdown of organic matter from thawing permafrost and carbon-rich river runoff in seawater.

“It is predicted that accumulation of atmospheric CO2 in ocean surface waters will make the ocean twice as acidic by the end of this century. The Arctic Ocean is more sensitive to ocean acidification because more CO2 can dissolve in cold water. Our measurements show much higher levels of acidification of the Arctic Ocean than those previously reported by the IPCC (Intergovernmental Panel on Climate Change) among others,” says Örjan Gustafsson, Professor at ACES.

A “particularly vulnerable area”

The new study culminated from decade-long observations in the remote East Siberian Arctic Shelf, which is comprised of the Laptev Sea, the East Siberian Sea and the Russian part of the Chukchi Sea. It is the largest shelf sea system of the World Ocean and one that the authors call “a particularly vulnerable target area.”

“The East Siberian Arctic Shelf is an extremely climate-sensitive system that makes up approximately a quarter of the Arctic continental shelf. It receives river discharges from four large rivers, which transport terrestrial organic carbon as a result of permafrost thawing. In addition, the Shelf includes riverbanks, deltas and coastlines with thousand of kilometres of ice complexes. This system is strongly affected by global warming which has caused the steep coastline to erode by several metres per year, releasing old material from the permafrost into the seawater,” says Örjan Gustafsson.

“Extreme” aragonite under-saturation in the East Siberian Arctic Shelf waters

The team tracked the progress of acidification in the East Siberian Arctic Shelf by estimating the saturation state of aragonite, a soluble crystalline form of calcium carbonate, in water samples collected during research expeditions from 1999 to 2011. Aragonite is crucial for marine organisms to form their skeletons or shells. With fewer carbonate ions, the seawater becomes “under-saturated” with respect to aragonite. To pinpoint whether the source of CO2 is from the atmosphere or the land, the researchers calculated the isotopic signatures of carbon and oxygen in the water samples.

“Our results show that carbon release from thawing coastal permafrost and growing river discharge cause persistent, and potentially increasing aragonite under-saturation of seawater in the East Siberian Arctic Shelf,” says Örjan Gustafsson. According to the authors, the “extreme” aragonite under-saturation in the East Siberian Arctic Shelf reflects seawater acidity levels much higher than those projected in this region for the end of this century, as these are currently based only on atmospheric CO2.

“This indirect trigger of massive ocean acidification in the East Siberian Arctic Shelf illustrates the complexity of the Earth system under increasing anthropogenic pressure,” says Örjan Gustafsson.

Contact

Örjan Gustafsson
Phone + 46 8 674 7317
orjan.gustafsson@aces.su.se

Severe Arctic Ocean acidification via permafrost thawing and river runoff


Observed dynamics in the annual mean discharge (W) of the Siberian Arctic Rivers and in the annual mean air temperature in 1936-2006. a) Observed dynamics revealed an 11.8 percent increase in the annual mean W observed during the seven decades, which corresponds to ≈1.2°C increase in mean air temperature in this region; b) Increase in the annual discharge of the Lena River observed during the last 30 years (1975-2005) composed 22.6 percent; increase in the period 1935-1975 composed 6 percent. Graphic: Semiletov, et al., 2016 / Nature Geoscience

ABSTRACT: Ocean acidification affects marine ecosystems and carbon cycling, and is considered a direct effect of anthropogenic carbon dioxide uptake from the atmosphere1, 2, 3. Accumulation of atmospheric CO2 in ocean surface waters is predicted to make the ocean twice as acidic by the end of this century4. The Arctic Ocean is particularly sensitive to ocean acidification because more CO2 can dissolve in cold water5, 6. Here we present observations of the chemical and physical characteristics of East Siberian Arctic Shelf waters from 1999, 2000–2005, 2008 and 2011, and find extreme aragonite undersaturation that reflects acidity levels in excess of those projected in this region for 2100. Dissolved inorganic carbon isotopic data and Markov chain Monte Carlo simulations of water sources using salinity and δ18O data suggest that the persistent acidification is driven by the degradation of terrestrial organic matter and discharge of Arctic river water with elevated CO2 concentrations, rather than by uptake of atmospheric CO2. We suggest that East Siberian Arctic Shelf waters may become more acidic if thawing permafrost leads to enhanced terrestrial organic carbon inputs and if freshwater additions continue to increase, which may affect their efficiency as a source of CO2.

Acidification of East Siberian Arctic Shelf waters through addition of freshwater and terrestrial carbon

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