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Published on: February 9, 2019
Global ecological predictors of the soil priming effect
Felipe Bastida1, Carlos García2, Noah Fierer3,4
1CEBAS-CSIC, Department of Soil and Water Conservation, Campus Universitario de Espinardo, 30100, Murcia, Spain. fbastida@cebas.csic.es.
Soil priming effects, which influence carbon cycling, are driven by soil organic carbon (SOC) content. Positive priming occurs in arid soils with low SOC, while negative priming is observed in mesic soils with high SOC.
Area of Science:
- Soil Science
- Ecology
- Biogeochemistry
Background:
- Understanding soil priming is crucial for modeling terrestrial carbon (C) cycling.
- Soil priming describes the change in soil organic matter decomposition due to the addition of fresh organic matter.
Purpose of the Study:
- To identify the global drivers of apparent soil priming effects.
- To investigate the relationship between soil properties and the soil priming effect.
Main Methods:
- Surveyed soils from 86 globally distributed locations.
- Utilized 13C-glucose labeling to measure apparent soil priming effects.
- Employed statistical modeling to analyze relationships between priming and environmental factors.
Main Results:
- Positive apparent priming effects (increased CO2 release) were negatively associated with soil organic carbon (SOC) content and microbial respiration.
- Apparent priming effects were generally negative in mesic sites with high SOC content.
- Positive apparent priming effects were observed in arid sites with low SOC content after labile carbon addition.
Conclusions:
- Soil organic carbon content is a critical regulator of apparent soil priming effects globally.
- Findings have significant implications for refining carbon cycling models under changing global conditions.
- The study highlights the context-dependency of soil priming, influenced by climate and soil properties.
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