What drives biological nitrogen fixation in high arctic tundra: Moisture or temperature?

TY - JOUR

T1 - What drives biological nitrogen fixation in high arctic tundra: Moisture or temperature?

AU - Rousk, Kathrin

AU - Sørensen, Pernille Lærkedal

AU - Michelsen, Anders

N1 - CENPERMOA[2019]

PY - 2018/2

Y1 - 2018/2

N2 - Biological nitrogen (N2) fixation is one of the main sources of available N for pristine ecosystems such as subarctic and arctic tundra. Although this has been acknowledged more than a decade ago, few attempts have been undertaken to identify the foremost driver of N2 fixation in the high Arctic. Here, we report results from in situ measurements of N2 fixation throughout the main growing period (June-August) in high arctic tundra, Greenland, in climate change treatments, shading and warming, and control. Nitrogen fixation was also measured in cores that received additional water prior to the measurements. The climate change field treatments did not lead to significant changes in any measured parameters; however, N2 fixation was promoted by adding water, and moisture was the most important factor influencing N2 fixation in all climate change field treatments. Maximum N2 fixation rates were measured below 14C soil temperature, which is much lower than the theoretical and previously reported temperature optimum for the nitrogenase enzyme. Diazotroph (N2 fixing bacteria) communities are adapted to low temperatures in high arctic settings, and increased temperature in a future climate may lead to decreased N2 fixation rates, or to a shift in diazotroph communities.

AB - Biological nitrogen (N2) fixation is one of the main sources of available N for pristine ecosystems such as subarctic and arctic tundra. Although this has been acknowledged more than a decade ago, few attempts have been undertaken to identify the foremost driver of N2 fixation in the high Arctic. Here, we report results from in situ measurements of N2 fixation throughout the main growing period (June-August) in high arctic tundra, Greenland, in climate change treatments, shading and warming, and control. Nitrogen fixation was also measured in cores that received additional water prior to the measurements. The climate change field treatments did not lead to significant changes in any measured parameters; however, N2 fixation was promoted by adding water, and moisture was the most important factor influencing N2 fixation in all climate change field treatments. Maximum N2 fixation rates were measured below 14C soil temperature, which is much lower than the theoretical and previously reported temperature optimum for the nitrogenase enzyme. Diazotroph (N2 fixing bacteria) communities are adapted to low temperatures in high arctic settings, and increased temperature in a future climate may lead to decreased N2 fixation rates, or to a shift in diazotroph communities.

U2 - 10.1002/ecs2.2117

DO - 10.1002/ecs2.2117

M3 - Journal article

SN - 2150-8925

VL - 9

JO - Ecosphere (Washington, D.C.)

JF - Ecosphere (Washington, D.C.)

IS - 2

M1 - e02117

ER -