Abstract
Arid and semiarid ecosystems (drylands) may dominate the trajectory of biosphere-to-atmosphere carbon (C) exchange, and understanding dryland CO2 efflux is important for C cycling at the global-scale. However, unknowns remain regarding how temperature and moisture interact to regulate dryland soil respiration (R s ), while ‘islands of fertility’ in drylands create spatially heterogeneous R s . At a site in southeastern Utah, USA we added or removed litter (0–650 % of control) in plots associated with either shrubs or biological soil crust-dominated interspaces between vascular plants. We measured R s , soil temperature (Ts), and water content (θ) repeatedly from October 2013 to November 2014. R s was highest following rain in late summer at Ts ~30 °C, and lowest mid-summer at Ts > 40 °C, resulting in apparent negative temperature sensitivity of R s at high temperatures, and positive temperature sensitivity at low-moderate temperatures. We used Bayesian statistical methods to compare models capturing a range of hypothesized relationships between Ts, θ, and R s . The best model indicates that apparent negative temperature sensitivity of R s at high Ts reflects the control of water content, not high temperatures. Modeled Q10 ranged from 2.7 to 1.4 between 5 and 45 °C. Litter addition had no effect on Q10 or reference respiration (R ref = R s at 20 °C and optimum θ) beneath shrubs, and little effect on R ref in interspaces, yet R ref was 1.5 times higher beneath shrubs than in interspaces. Altogether, these results suggest reduced R s often observed at high Ts in drylands is dominated by the control of θ, and, on shorter-timescales, variable litter inputs exert minimal control over R s .
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Acknowledgments
This material is based upon work supported by the U.S. Department of Energy Office of Science, Office of Biological and Environmental Research Terrestrial Ecosystem Sciences Program, under Award Number DE-SC-0008168 and by the U.S. Geological Survey Ecosystems Mission Area. We thank Pete Chuckran for his excellent work with plot installation and measurements, and we are appreciative of all of the technicians who worked on this project. We are grateful to our D-DIRT collaborators Heather Throop and Marie-Anne de Graaff for their ideas and collaboration. We also thank Jessie Young for her valuable feedback on an earlier version of the manuscript. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
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10533_2016_200_MOESM1_ESM.zip
Supplementary material 1 Compressed folder containing model code, for all 20 models in.R and.stan format, data in.csv format, as well as instructions for installing Rstan and running the code provided (ZIP 47 kb)
10533_2016_200_MOESM2_ESM.xlsx
Supplementary material 2 Table containing prior distributions, prior 95 % intervals, and posterior 95 % credible intervals for each parameter in each model (XLSX 32 kb)
10533_2016_200_MOESM3_ESM.pdf
Supplementary material 3 Maximum soil respiration (R s ) for 99 studies taken from the Global Soil Respiration Database (Bond-Lamberty and Thomson 2010) compared to mean annual precipitation (MAP) and mean annual temperature (MAT) (PDF 160 kb)
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Tucker, C.L., Reed, S.C. Low soil moisture during hot periods drives apparent negative temperature sensitivity of soil respiration in a dryland ecosystem: a multi-model comparison. Biogeochemistry 128, 155–169 (2016). https://doi.org/10.1007/s10533-016-0200-1
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DOI: https://doi.org/10.1007/s10533-016-0200-1