OOS 23-4
Differential effects of extreme drought on production and respiration: Synthesis and modeling analysis

Wednesday, August 13, 2014: 9:00 AM
304/305, Sacramento Convention Center
Zheng Shi, Microbiology and Plant Biology, University of Oklahoma, Norman, OK
Michell L. Thomey, Department of Biology, University of New Mexico, Albuquerque, NM
W. Mowll, Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO
Marcy E. Litvak, Department of Biology, University of New Mexico, Albuquerque, NM
Nathaniel Brunsell, Department of Geography & Atmospheric Science, University of Kansas, Lawrence, KS
Scott L. Collins, Department of Biology, University of New Mexico, Albuquerque, NM
William T. Pockman, Department of Biology, University of New Mexico, Albuquerque, NM
Melinda D. Smith, Graduate Degree Program in Ecology, Colorado State University, Ft. Collins, CO
A.K. Knapp, Graduate Degree Program in Ecology, Colorado State University, Fort Collins, CO
Yiqi Luo, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK
Background/Question/Methods

Extremes in climate may severely impact ecosystem structure and function, with both the magnitude and rate of response differing among ecosystem types and processes. We conducted a modeling analysis of the effects of extreme drought on two key ecosystem processes, production and respiration, and, to provide a broader context, we complemented this with a synthesis of published results that cover a wide variety of ecosystems.

Results/Conclusions

The synthesis indicated that across a broad range of biomes, gross primary production was generally more sensitive to extreme drought than was ecosystem respiration. Furthermore, this differential sensitivity between production and respiration increased as drought severity increased; it occurred only in grassland ecosystems, and not in evergreen needle-leaf and broad-leaf forests or woody savannahs. Model results consistently showed that net primary productivity (NPP) was reduced more than heterotrophic respiration (Rh) by extreme drought (i.e., 67% reduction in annual ambient rainfall) at all four study sites. The sensitivity of NPP to drought was directly attributable to rainfall amount, whereas the sensitivity of Rh to drought was driven by soil drying, reduced carbon (C) input and a drought-induced reduction in soil C content – a much slower process. However, differences in reductions in NPP and Rh diminished as extreme drought continued, due to a gradual decline in the soil C pool leading to further reductions in Rh. Our findings suggest that responses of production and respiration differ in magnitude, occur on different timescales, and are affected by different mechanisms under extreme, prolonged drought.