02848naa a2200349 a 450000100080000000500110000800800410001902400540006010000270011424501020014126000090024352018460025265000150209865000160211365000140212965000240214365000230216765000090219065300160219965300320221565300320224770000210227970000170230070000160231770000230233370000200235670000200237670000190239670000240241570000200243977300390245921685102024-10-25       2024    bl uuuu     u00u1 u    #d7 ahttps://doi.org/10.1016/j.catena.2024.1084512DOI1 aPINHEIRO JUNIOR, C. R.  aDrivers of carbon stabilization and sequestration in Brazil's black soils.h[electronic resource]  c2024  aClimate and land use are recognized as two of the main drivers of changes in soil organic carbon (SOC) on a global scale. Both factors play an important role in understanding SOC sequestration and mitigation of climate change. Particularly important, black soils are mineral soils with high SOC contents and high natural fertility and play an important role in national and global food and climate security. Here, we used a database of 90 black soils in Brazil − under different climate and land use conditions across the country − to test the hypothesis that C stock is richer in wetter climate conditions and that agricultural land use reduces C stock and the percentage of carbon saturation (PCS%). Climate data were obtained from the National Oceanic Atmospheric Administration (NOAA) and used to classify Thornthwaite’s climate. The land use information was obtained in the MapBiomas platform and was grouped into three major types: cropland, pasture, and native vegetation. The nonparametric Kruskal-Wallis test showed no differences for C stock, C/N ratio, and PCS% for both land use and climate. The low C/N ratio and the strong correlation between Ca2+, CEC, clay, and SOC suggest that organo-mineral interactions − which are stronger in soils with high-activity clays (e.g., Chernozems, Kastanozems, and Phaeozems) − promotes greater stabilization of the SOC and its long-term persistence and, thus being less sensitive to variations in climate and land use. Considering the total area of approximately 3.7 × 106 ha and the average value of C stock of 93.2 Mg/ha, the total SOC stored in Brazil’s black soils is in the order of 0.35 Gt, and the carbon stock stabilization potential is 0.25 Gt. Our results highlight the potential of Brazil’s black soils to promote carbon sequestration and climate change mitigation.  aChernozems  aKastanozems  aPhaeozems  aSoil organic matter  aMatéria Orgânica  aSolo  aChernossolo  aInterações organominerais  aOrgano-mineral interactions1 aCANISARES, L. P.1 aABREU, M. C.1 aLYRA, G. B.1 aOLIVEIRA, A. P. de1 aGRESCHUK, L. T.1 aFERREIRA, T. O.1 aPEREIRA, M. G.1 aANJOS, L. H. C. dos1 aCHERUBIN, M. R.  tCatenagv. 246, 108451, Nov. 2024.