Montes-Pulido Carmen R, Bird Michael I, da Silva Carvalho Lidiany C, Serrano Julieth, Quesada Carlos A, Feldpausch Ted R
School of Agricultural, Livestock, and Environmental Sciences, Universidad Nacional Abierta y a Distancia (UNAD), Bogota, Colombia.
College of Science and Engineering and ARC Centre of Excellence for Indigenous and Environmental Histories and Futures, James Cook University, Smithfield, Queensland, Australia.
Glob Chang Biol. 2025 Jul;31(7):e70135. doi: 10.1111/gcb.70135.
Understanding the drivers of soil organic carbon (SOC) and soil pyrogenic carbon (PyC) variation and their role in natural and managed ecosystems is increasingly important. However, PyC stocks in tropical Andean soils remain understudied. Here, we examined how edaphic and environmental factors affect PyC across elevation and disturbance gradients in 36 plots spanning natural forests and agrosilvopastoral systems in the Colombian Andes. Across the 0-100 cm soil profile, the mean SOC stock in the study region was 433.10 Mg C ha (range: 67.97-1462 Mg C ha), while the mean PyC stock was 34.13 Mg C ha (range: 2.29-305.70 Mg C ha), accounting for approximately ~8% of the total SOC. This PyC stock is approximately nine times greater than the Amazon-wide average. PyC (%) did not vary significantly with disturbance gradients or soil depths. However, both PyC (%) and SOC (%) varied significantly with elevation zonation (p < 0.001). The High Andes had the highest concentrations of PyC (1.3%) and SOC (14.6%), which were substantially higher than the Medium Andes (PyC = 0.17%; SOC = 6.7%) and Low Andes (PyC = 0.06%; SOC = 1.3%). Soil clay content and annual precipitation were the primary drivers of PyC, explaining 56% of the variability when combined with pH, Ca, and NDVI. PyC was positively associated with clay content (Estimate: 0.27, p < 0.001) and negatively associated with annual precipitation (Estimate: -0.18, p < 0.05). These factors may influence the physical and chemical processes that affect PyC formation and preservation in soils. This analysis provides insight into SOC and PyC variability in Andean forest soils, highlighting the substantial contribution of soil PyC to total soil carbon and its importance as persistent soil carbon under current and predicted warming conditions across the region.
了解土壤有机碳(SOC)和土壤热解碳(PyC)变化的驱动因素及其在自然和人工管理生态系统中的作用变得越来越重要。然而,热带安第斯土壤中的PyC储量仍未得到充分研究。在此,我们研究了土壤和环境因素如何影响哥伦比亚安第斯山脉跨越天然林和农林牧系统的36个样地中不同海拔和干扰梯度下的PyC。在0 - 100厘米的土壤剖面中,研究区域的平均SOC储量为433.10 Mg C ha(范围:67.97 - 1462 Mg C ha),而平均PyC储量为34.13 Mg C ha(范围:2.29 - 305.70 Mg C ha),约占总SOC的8%。这一PyC储量大约是整个亚马逊地区平均水平的九倍。PyC(%)随干扰梯度或土壤深度没有显著变化。然而,PyC(%)和SOC(%)均随海拔分区有显著变化(p < 0.001)。高安第斯地区的PyC(1.3%)和SOC(1 + 4.6%)浓度最高,显著高于中山地区(PyC = 0.17%;SOC = 6.7%)和低山地区(PyC = 0.06%;SOC = 1.3%)。土壤粘土含量和年降水量是PyC的主要驱动因素,与pH、Ca和归一化植被指数(NDVI)结合时可解释56%的变异性。PyC与粘土含量呈正相关(估计值:0.27,p < 0.001),与年降水量呈负相关(估计值: - 0.18,p < 0.05)。这些因素可能会影响影响土壤中PyC形成和保存的物理和化学过程。该分析深入了解了安第斯森林土壤中SOC和PyC的变异性,突出了土壤PyC对土壤总碳的重大贡献及其在该地区当前和预测的变暖条件下作为持久性土壤碳的重要性。