2020 ESA Annual Meeting (August 3 - 6)

COS 200 Abstract - Do higher-quality plant tissue inputs promote organic matter accumulation more efficiently than lower-quality inputs? Insights from a dual-isotope pulse-chase experiment in subtropical pasture

Chris Wilson1, Michael S Strickland2, Jose Dubeux3, Lynn E. Sollenberger1, Stacy A. Smith1, Gabriel Maltais-Landry4 and Stefan Gerber5, (1)Agronomy, University of Florida, Gainesville, FL, (2)Soil and Water Systems, University of Idaho, Moscow, ID, (3)Agronomy, University of Florida, FL, (4)Soil and Water Sciences, University of Florida, Gainesville, FL, (5)Soil and Water Sciences, University of Florida IFAS, Gainesville, FL
Background/Question/Methods

Grazing lands represent a globally significant land use, account for a large portion of global soil carbon, and thus could play a critical role in climate change mitigation. Despite their global importance, the factors that regulate soil carbon in subtropical pasture systems are relatively understudied. Here, we report findings from an in situ 13C/15N pulse-chase experiment conducted in subtropical pasture in Florida, USA. We aim to study perennial legume incorporation into warm-season pasture, an agronomic practice gaining increasing attention for both production and ecosystem service benefits. Specifically, we tested whether deposition of higher-quality (lower C:N ratio) legume plant tissue increases soil C and N pools more effectively than lower-quality C4 grass tissue, as suggested by recent theoretical frameworks that emphasize the positive role of microbial growth efficiency in increasing the fraction of organic inputs stabilized over the long term (e.g. the “MEMS hypothesis”).

Results/Conclusions

Over a 16-month chase period, we found that, while legume tissue cycles more rapidly through soil and plant pools, its labelled 13C/15N content is retained ~ 25% less efficiently in our pasture soils than the C4 grass tissue, challenging the notion that greater microbial efficiency should lead to greater organic matter stabilization. While previous research indicates that mineral-associated organic matter (MAOM) is stabilized over longer timeframes than particulate organic matter (POM), our pulse-chase experiment reveals that both fractions are heterogeneous, and likely feature similar residence times for C and N. Additionally, our experiment provides novel evidence that cation-bridging may be a critical mechanism of stabilization in both fractions, with Mehlich-3 extractable calcium explaining ~ 50% of the variation in C concentrations in our soils. Overall, our findings suggest that legume addition to warm-season pasture may benefit soil organic matter indirectly via N enrichment, but do not support the notion that higher-quality inputs increase either MAOM or POM more efficiently than lower-quality inputs in our subtropical pasture system.