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干旱化加剧和干旱土地扩张对碳储存能力、生物多样性丧失和生态系统服务的影响。

Impact of aridity rise and arid lands expansion on carbon-storing capacity, biodiversity loss, and ecosystem services.

机构信息

Xinjiang Key Laboratory of Desert Plant Roots Ecology and Vegetation Restoration, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, China.

State Key Laboratory of Desert and Oasis Ecology, Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, China.

出版信息

Glob Chang Biol. 2024 Apr;30(4):e17292. doi: 10.1111/gcb.17292.

Abstract

Drylands, comprising semi-arid, arid, and hyperarid regions, cover approximately 41% of the Earth's land surface and have expanded considerably in recent decades. Even under more optimistic scenarios, such as limiting global temperature rise to 1.5°C by 2100, semi-arid lands may increase by up to 38%. This study provides an overview of the state-of-the-art regarding changing aridity in arid regions, with a specific focus on its effects on the accumulation and availability of carbon (C), nitrogen (N), and phosphorus (P) in plant-soil systems. Additionally, we summarized the impacts of rising aridity on biodiversity, service provisioning, and feedback effects on climate change across scales. The expansion of arid ecosystems is linked to a decline in C and nutrient stocks, plant community biomass and diversity, thereby diminishing the capacity for recovery and maintaining adequate water-use efficiency by plants and microbes. Prolonged drought led to a -3.3% reduction in soil organic carbon (SOC) content (based on 148 drought-manipulation studies), a -8.7% decrease in plant litter input, a -13.0% decline in absolute litter decomposition, and a -5.7% decrease in litter decomposition rate. Moreover, a substantial positive feedback loop with global warming exists, primarily due to increased albedo. The loss of critical ecosystem services, including food production capacity and water resources, poses a severe challenge to the inhabitants of these regions. Increased aridity reduces SOC, nutrient, and water content. Aridity expansion and intensification exacerbate socio-economic disparities between economically rich and least developed countries, with significant opportunities for improvement through substantial investments in infrastructure and technology. By 2100, half the world's landmass may become dryland, characterized by severe conditions marked by limited C, N, and P resources, water scarcity, and substantial loss of native species biodiversity. These conditions pose formidable challenges for maintaining essential services, impacting human well-being and raising complex global and regional socio-political challenges.

摘要

旱地包括半干旱、干旱和极干旱地区,覆盖了地球陆地表面的大约 41%,并且在最近几十年中已经大幅扩张。即使在更乐观的情景下,例如到 2100 年将全球升温限制在 1.5°C 以内,半干旱土地的面积可能仍会增加高达 38%。本研究概述了干旱地区变干的最新进展,特别关注其对植物-土壤系统中碳(C)、氮(N)和磷(P)积累和可用性的影响。此外,我们总结了干旱加剧对生物多样性、服务提供以及跨尺度气候变化反馈的影响。干旱生态系统的扩张与 C 和养分储量、植物群落生物量和多样性的下降有关,从而降低了植物和微生物的恢复能力和维持充足水分利用效率的能力。长期干旱导致土壤有机碳(SOC)含量减少 3.3%(基于 148 项干旱处理研究),植物凋落物输入减少 8.7%,绝对凋落物分解减少 13.0%,凋落物分解速率降低 5.7%。此外,由于反照率增加,与全球变暖存在实质性的正反馈循环。丧失关键生态系统服务,包括粮食生产能力和水资源,对这些地区的居民构成了严峻挑战。干旱加剧会降低 SOC、养分和水分含量。旱地的扩张和强化加剧了经济富裕和最不发达国家之间的社会经济差距,通过对基础设施和技术的大量投资,有很大的改善机会。到 2100 年,世界一半的陆地可能会变成旱地,其特征是 C、N 和 P 资源有限、水资源短缺和大量本地物种生物多样性丧失等严峻条件。这些条件对维持基本服务构成了巨大挑战,影响人类福祉并引发复杂的全球和区域社会政治挑战。

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