1. Impact of climate and land degradation on soil carbon fluxes in dry semiarid grasslands in SE Spain
- Author
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João Raimundo, Carlos García-Gutiérrez Báez, Cecilio Oyonarte, Ana Rey, Luis M. Carrascal, and Emiliano Pegoraro
- Subjects
0106 biological sciences ,Soil CO 2 efflux ,Biological soil crust ,Soil Science ,Degraded grasslands ,Precipitation ,Plant Science ,complex mixtures ,01 natural sciences ,Grassland ,Temporal autocorrelation ,medicine ,Climate change ,Mediterranean dry grasslands ,geography ,geography.geographical_feature_category ,Moisture ,food and beverages ,Seasonality ,04 agricultural and veterinary sciences ,Soil carbon ,Abiotic drivers ,medicine.disease ,Agronomy ,Soil water ,040103 agronomy & agriculture ,Land degradation ,0401 agriculture, forestry, and fisheries ,Environmental science ,010606 plant biology & botany - Abstract
[Aims]: This study investigates how precipitation, temperature and seasonality (as a proxy of plant productivity) affect the temporal and spatial variability of soil CO efflux in two dry semiarid grasslands with different degrees of land degradation. [Methods]: We measured soil CO efflux over four years under plant, biological soil crust and bare soil patches and estimated annual soil carbon losses in both, a natural and a degraded grassland, by means of generalised additive mixed models considering temporal autocorrelation in the data. [Results]: Soil CO efflux ranged from 0.08 to 3.70 and from 0.10 to 3.01 μmol CΟ m s in the natural and degraded grasslands, respectively. Daily soil CO efflux was mostly affected by moisture in the degraded grassland (25.4%), while in the natural grassland was affected jointly by seasonality, temperature and moisture (27.5%). Overall, the highest soil carbon fluxes were measured in soils covered by biological soil crusts (1.24 ± 0.02 and 1.10 ± 0.02) and the lowest in bare soils (1.11 ± 0.02 and 0.82 ± 0.02 μmol CΟ s) in the natural and degraded sites, respectively. Cumulative soil carbon fluxes were mainly driven by temperature and previous precipitation (over three months). The highest soil carbon losses were estimated in the driest year (2009) and the lowest in the wettest (2010) with almost twice the amount of rainfall. The main difference between these years was the timing of the events that mostly occurred in the moments of maximum plant activity with optimum temperatures in spring in the dry year. [Conclusions]: Changes in precipitation patterns will affect soil carbon fluxes more than rainfall amount, particularly in degraded grasslands. Therefore, considering all climate drivers together with plant activity is essential to predict how climate change will affect soil biological processes in drylands.
- Published
- 2021