SCHUUR LAB - ECOSYSTEM DYNAMICS RESEARCH

  • Eight Mile Lake, AK; C. Schädel
  • Eight Mile Lake, AK; C. Schädel
  • Alaska Range; credit: C. Schädel
  • Automated Flux Chambers
  • Eriophorum Vaginatum
  • foggy mountains in Healy
  • Winter setting in Healy, AK
  • Winter snow fences
  • Dall Sheep, Denali National Park
  • Fall at CiPEHR
  • Spring at CiPEHR
  • Fall at the Gradient site; credit: E. Webb
  • Snowfences at CiPEHR; credit: S. Natali
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CiPEHR

Marguerite Mauritz

Marguerite Mauritz

Contact Information:

Post-doctoral Research Associate

Center for Ecosystem Sciences and Society

Department of Biological Sciences

Northern Arizona University

Flagstaff, AZ 86011

USA

email:

Research Interests

 

As arctic temperatures rise, we expect to see dramatic changes due to thawing permafrost soils. Permafrost stores half the total amount of carbon (C) found in soils globally, and twice as much C as is found in the atmosphere. As permafrost thaws, the stored C becomes vulnerable to loss because low temperatures no longer limit microbial activity. However, thawing soils and warmer temperatures may also allow plants to access more nutrients and grow deeper roots. In the short-term greater plant growth can therefore offset C losses from the soil. Uncertainty about how plants and microbes interact, as the ecosystem continues to change, makes it extremely difficult to predict how warming will affect permafrost C dynamics in both the short, and the long term. Using data from a 5 year field warming experiment in the Tundra, lab soil incubations and 13C&14C signatures from soil respiration, I am interested in improving our understanding of how rising arctic temperatures will affect the C balance of arctic ecosystems.

  • How does warming impact C balance of arctic ecosystems?
  • How do changes in the plant community interact to determine the C balance of the ecosystem?
  • How rapidly is C lost from the soil, once temperature constraints are lifted?
  • What are the mechanisms responsible for stabilizing C in the soil?
  • Do greater plant root activity and more extensive soil thawing create a priming effect to stimulate even greater soil C loss?
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