具有长期碎屑变化的土壤有机质分子组成受特定地点森林特性的控制

IF 10.8 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION Global Change Biology Pub Date : 2022-09-28 DOI:10.1111/gcb.16456
Laura Casta?eda-Gómez, Kate Lajtha, Richard Bowden, Fathima Nahidha Mohammed Jauhar, Juan Jia, Xiaojuan Feng, Myrna J. Simpson
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引用次数: 4

摘要

森林生态系统是全球重要的土壤碳(C)库,但其固碳能力容易受到气候变化因素的影响,气候变化因素会改变碳输入的数量和质量。为了更好地了解森林土壤C对改变C输入的响应,我们整合了两个落叶森林:Bousson森林(BF), Harvard森林(HF)和针叶林:H.J.安德鲁斯森林(HJA),经过20年的碎屑输入和去除处理后,矿物土壤中土壤有机质(SOM)和土壤微生物群落的三个分子组成数据集。通过放射性碳测量估算土壤C的周转时间,并与分子水平数据(基于核磁共振和植物和微生物衍生化合物的特定分析)进行比较,以更好地了解生态系统特性如何控制土壤C的生物地球化学和动力学。在所有研究的森林中,增加一倍的地上凋落物并没有增加土壤C,这可能是由于长期的土壤启动。土壤有机质的分解程度在氮有效度较高的细菌占主导地位的土壤中较高,在缺氮针叶林中较低。排除凋落物显著降低了土壤C,增加了SOM的分解状态,导致微生物群落对有效基质变化的适应。最后,虽然地上凋落物决定了针叶林(HJA)土壤碳动态及其分子组成,但地下凋落物对阔叶林(BH和HF)土壤碳动态的影响更大。这一综合表明,内在的生态系统特性在分子水平上调控着土壤C动态随凋落物的变化。在研究的森林中,20年的凋落物添加并没有提高土壤C含量,而凋落物的减少对土壤C浓度产生了负面影响。这些结果表明,这些温带森林的土壤C生物地球化学对凋落物的变化高度敏感,这是环境变化驱动因素的产物。
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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Soil organic matter molecular composition with long-term detrital alterations is controlled by site-specific forest properties

Forest ecosystems are important global soil carbon (C) reservoirs, but their capacity to sequester C is susceptible to climate change factors that alter the quantity and quality of C inputs. To better understand forest soil C responses to altered C inputs, we integrated three molecular composition published data sets of soil organic matter (SOM) and soil microbial communities for mineral soils after 20 years of detrital input and removal treatments in two deciduous forests: Bousson Forest (BF), Harvard Forest (HF), and a coniferous forest: H.J. Andrews Forest (HJA). Soil C turnover times were estimated from radiocarbon measurements and compared with the molecular-level data (based on nuclear magnetic resonance and specific analysis of plant- and microbial-derived compounds) to better understand how ecosystem properties control soil C biogeochemistry and dynamics. Doubled aboveground litter additions did not increase soil C for any of the forests studied likely due to long-term soil priming. The degree of SOM decomposition was higher for bacteria-dominated sites with higher nitrogen (N) availability while lower for the N-poor coniferous forest. Litter exclusions significantly decreased soil C, increased SOM decomposition state, and led to the adaptation of the microbial communities to changes in available substrates. Finally, although aboveground litter determined soil C dynamics and its molecular composition in the coniferous forest (HJA), belowground litter appeared to be more influential in broadleaf deciduous forests (BH and HF). This synthesis demonstrates that inherent ecosystem properties regulate how soil C dynamics change with litter manipulations at the molecular-level. Across the forests studied, 20 years of litter additions did not enhance soil C content, whereas litter reductions negatively impacted soil C concentrations. These results indicate that soil C biogeochemistry at these temperate forests is highly sensitive to changes in litter deposition, which are a product of environmental change drivers.

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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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