Beyond bulk: Density fractions explain heterogeneity in global soil carbon abundance and persistence
Autor: | Susan E. Crow, Erika Marin-Spiotta, Carlos A. Sierra, Casey McGrath, Katherine Heckman, J. Grey Monroe, Sophie F. von Fromm, Alain F. Plante, Zheng Shi, Jeffrey Beem-Miller, Aaron Thompson, Marco Keiluweit, Shane Stoner, Caitlin E. Hicks Pries, Alison M. Hoyt, Corey R. Lawrence, Craig Rasmussen, Joseph C. Blankinship, Joshua P. Schimel, Asmeret Asefaw Berhe, Rota Wagai |
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Rok vydání: | 2021 |
Předmět: | |
Zdroj: | Global Change Biology. 28:1178-1196 |
ISSN: | 1365-2486 1354-1013 |
DOI: | 10.1111/gcb.16023 |
Popis: | Understanding the controls on the amount and persistence of soil organic carbon (C) is essential for predicting its sensitivity to global change. The response may depend on whether C is unprotected, isolated within aggregates, or protected from decomposition by mineral associations. Here, we present a global synthesis of the relative influence of environmental factors on soil organic C partitioning among pools, abundance in each pool (mg C g-1 soil), and persistence (as approximated by radiocarbon abundance) in relatively unprotected particulate and protected mineral-bound pools. We show that C within particulate and mineral-associated pools consistently differed from one another in degree of persistence and relationship to environmental factors. Soil depth was the best predictor of C abundance and persistence, though it accounted for more variance in persistence. Persistence of all C pools decreased with increasing mean annual temperature (MAT) throughout the soil profile whereas persistence increased with increasing wetness index (MAP/PET) in subsurface soils (30-176 cm). The relationship of C abundance (mg C g-1 soil) to climate varied among pools and with depth. Mineral-associated C in surface soils ( |
Databáze: | OpenAIRE |
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