Climatic and Edaphic Drivers of Soil Organic Carbon and Pyrogenic Carbon Stocks Across Elevation and Disturbance Gradients in Colombian Andean Forests

IF 10.8 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION
Carmen R. Montes-Pulido, Michael I. Bird, Lidiany C. da Silva Carvalho, Julieth Serrano, Carlos A. Quesada, Ted R. Feldpausch
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Abstract

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−1 (range: 67.97–1462 Mg C ha−1), while the mean PyC stock was 34.13 Mg C ha−1 (range: 2.29–305.70 Mg C ha−1), 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.

Abstract Image

哥伦比亚安第斯森林土壤有机碳和热原碳储量在海拔和扰动梯度上的气候和土壤驱动力
了解土壤有机碳(SOC)和土壤热原碳(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。在这里,我们研究了哥伦比亚安第斯山脉的36个样地的地形和环境因素对PyC的影响,这些样地跨越海拔和干扰梯度,跨越天然林和农林复合系统。在0 ~ 100 cm土壤剖面上,研究区平均有机碳储量为433.10 Mg C ha−1(范围:67.97 ~ 1462 Mg C ha−1),平均PyC储量为34.13 Mg C ha−1(范围:2.29 ~ 305.70 Mg C ha−1),约占总有机碳储量的8%。PyC的股价大约是亚马逊地区平均股价的九倍。PyC(%)随扰动梯度和土壤深度变化不显著。然而,PyC(%)和SOC(%)随海拔带变化显著(p < 0.001)。高安第斯山脉的PyC(1.3%)和SOC(14.6%)浓度最高,显著高于中安第斯山脉(PyC = 0.17%);SOC = 6.7%)和Low Andes (PyC = 0.06%;soc = 1.3%)。土壤粘粒含量和年降水量是PyC的主要驱动因素,当与pH、Ca和NDVI结合时,可以解释56%的变异。PyC与粘土含量呈正相关(估计值:0.27,p < 0.001),与年降水量负相关(估计值:- 0.18,p < 0.05)。这些因素可能影响影响土壤中PyC形成和保存的物理和化学过程。该分析提供了对安第斯森林土壤有机碳和PyC变异的深入了解,突出了土壤PyC对土壤总碳的重要贡献,以及在当前和预测的整个地区变暖条件下,它作为持续土壤碳的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Global Change Biology
Global Change Biology 环境科学-环境科学
CiteScore
21.50
自引率
5.20%
发文量
497
审稿时长
3.3 months
期刊介绍: Global Change Biology is an environmental change journal committed to shaping the future and addressing the world's most pressing challenges, including sustainability, climate change, environmental protection, food and water safety, and global health. Dedicated to fostering a profound understanding of the impacts of global change on biological systems and offering innovative solutions, the journal publishes a diverse range of content, including primary research articles, technical advances, research reviews, reports, opinions, perspectives, commentaries, and letters. Starting with the 2024 volume, Global Change Biology will transition to an online-only format, enhancing accessibility and contributing to the evolution of scholarly communication.
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