TY - JOUR
T1 - Patterns of woody plant-derived soil carbon losses and persistence after brush management in a semi-arid grassland
AU - DeMarco, Jennie
AU - Filley, Timothy
AU - Throop, Heather
N1 - Funding Information:
This research was supported by US National Science Foundation grant DEB 0953864. Thanks to J.G. Smith for help with soil collection and M. R. Bravo-Garza, K. Slown, and C. Elam for help with sample processing. D. Gamblin and N. Louden helped with the CuO oxidation analyses. We appreciate constructive comments on a previous version of the manuscript from J. Schafer and two anonymous reviewers.
Publisher Copyright:
© 2016, Springer International Publishing Switzerland.
PY - 2016/9/1
Y1 - 2016/9/1
N2 - Aims: Woody encroachment and subsequent brush management aimed at reducing woody plant cover can alter soil organic carbon (SOC) pools. However, brush management influences on the sources and stability of SOC is unknown. Using a space-for-time approach in a site with closely co-located patches representing unencroached grassland, woody encroachment, and brush management, we coupled stable isotopes and plant-derived biomarkers to quantify how woody encroachment alters input sources and stability of SOC and how these patterns change with brush management. Methods: Stable isotopes, lignin-derived phenols, substituted fatty acids, and carbon content of density fractions were measured in soils collected in shrub canopy interspaces, under live shrubs, and under shrubs killed 8 or 52 y previously. Results: Bulk SOC and C3-derived SOC were higher in shallow soil (0–5 cm) under live shrubs than in interspace soil. Long-term brush management showed a decline in total SOC stocks, substituted fatty acids, and C3-derived SOC that were associated with the soil light fraction. Despite declines in bulk SOC following brush management, accumulated C3-derived SOC pools in the dense fraction remained largely stable following brush management. Conclusions: Woody encroachment increases the proportion of poorly-protected light fraction and loosely-mineral associated SOC derived from leaf litter, which is lost within several decades after brush management. However, woody encroachment produced a stabilized mineral-bound pool of C3- and C4-derived SOC that remained 52 years after brush management, suggesting that woody encroachment has the potential for long-term SOC stabilization.
AB - Aims: Woody encroachment and subsequent brush management aimed at reducing woody plant cover can alter soil organic carbon (SOC) pools. However, brush management influences on the sources and stability of SOC is unknown. Using a space-for-time approach in a site with closely co-located patches representing unencroached grassland, woody encroachment, and brush management, we coupled stable isotopes and plant-derived biomarkers to quantify how woody encroachment alters input sources and stability of SOC and how these patterns change with brush management. Methods: Stable isotopes, lignin-derived phenols, substituted fatty acids, and carbon content of density fractions were measured in soils collected in shrub canopy interspaces, under live shrubs, and under shrubs killed 8 or 52 y previously. Results: Bulk SOC and C3-derived SOC were higher in shallow soil (0–5 cm) under live shrubs than in interspace soil. Long-term brush management showed a decline in total SOC stocks, substituted fatty acids, and C3-derived SOC that were associated with the soil light fraction. Despite declines in bulk SOC following brush management, accumulated C3-derived SOC pools in the dense fraction remained largely stable following brush management. Conclusions: Woody encroachment increases the proportion of poorly-protected light fraction and loosely-mineral associated SOC derived from leaf litter, which is lost within several decades after brush management. However, woody encroachment produced a stabilized mineral-bound pool of C3- and C4-derived SOC that remained 52 years after brush management, suggesting that woody encroachment has the potential for long-term SOC stabilization.
KW - Carbon isotopes
KW - Cupric oxide oxidation
KW - Lignin-derived phenols
KW - Sonoran Desert
KW - Woody encroachment
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U2 - 10.1007/s11104-016-2880-7
DO - 10.1007/s11104-016-2880-7
M3 - Article
AN - SCOPUS:84964088536
SN - 0032-079X
VL - 406
SP - 277
EP - 293
JO - Plant and Soil
JF - Plant and Soil
IS - 1-2
ER -