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碳酸盐岩风化碳汇对喀斯特生态系统服务功能权衡协同的影响

邓群群 李阳兵 白晓永

生态学报2026,Vol.46Issue(4):1724-1736,13.
生态学报2026,Vol.46Issue(4):1724-1736,13.DOI:10.20103/j.stxb.202506151510

碳酸盐岩风化碳汇对喀斯特生态系统服务功能权衡协同的影响

The impact of carbonate rock weathering carbon sink on the synergy of karst ecosystem service functions

邓群群 1李阳兵 2白晓永3

作者信息

  • 1. 贵州师范大学地理与环境科学学院,贵阳 550001||中国科学院地球化学研究所环境地球化学国家重点实验室,贵阳 550081
  • 2. 贵州师范大学地理与环境科学学院,贵阳 550001
  • 3. 贵州大学,贵阳 550025||中国科学院地球化学研究所环境地球化学国家重点实验室,贵阳 550081
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摘要

Abstract

The carbonate rock weathering carbon sink is a fundamental and dynamic component of the karst carbon cycle,playing a crucial yet often overlooked role in regional carbon budgets.A deep understanding of its impact mechanisms on ecosystem services(ES)is therefore essential for achieving sustainable ecosystem management in karst regions,which are among the world's most ecologically fragile landscapes.However,prevailing research paradigms have predominantly focused on evaluating single ES in isolation.This approach has created a significant knowledge gap regarding how the carbonate rock weathering carbon sink influences the complex,long-term trade-offs and synergistic relationships between multiple pairs of ES over time.To address this critical gap,our study focuses on the extensive karst terrain of Southwest China,the largest contiguous karst area globally,as an exemplary case.By leveraging a comprehensive,long-term dataset from 2000 to 2020,which integrates multi-source remote sensing imagery and meteorological reanalysis data,we employed a coupled methodological framework.This framework combines a process-based thermodynamic dissolution model,specifically calibrated for karst environments,with advanced spatial statistics and correlation analysis.The primary objective was to quantitatively unravel the dynamic evolution of trade-offs and synergies among three critical ESs—soil conservation,water yield,and carbon storage—as they are influenced by the spatiotemporal variations in the carbonate rock weathering carbon sink flux.Our results reveal several key findings.The average carbonate rock weathering carbon sink flux in the Southwest karst region was 7.04 t C km-2 a-1,exhibiting a significant and persistent annual increase of 40 kg C/km2.Concurrently,all three ESs showed widespread and marked improvement,with over 75%of the area displaying statistically significant positive trends for each service.The pairwise relationships between these ESs were overwhelmingly synergistic,dominating more than 69%of the study area.Notably,a simultaneous enhancement of all three services—a"win-win-win"scenario—was achieved in 52.4%of the region.A pivotal discovery was that the strength of these synergies positively correlated with the magnitude of the carbonate weathering carbon sink,intensifying as the carbon sink increased.In conclusion,our findings underscore the critical importance of integrating geological carbon sink processes into the assessment and management of ecosystem services.By explicitly accounting for the influence of carbonate rock weathering,our study provides a more mechanistic and nuanced understanding.This refined knowledge is indispensable for informing and optimizing the efficacy of regional ecological restoration projects and policy decisions,ultimately supporting the synergistic achievement of ecological sustainability and carbon neutrality goals in vulnerable karst landscapes.

关键词

碳酸盐岩风化/生态系统服务功能/权衡协同/岩溶碳汇/喀斯特地区

Key words

carbonate rock weathering/ecosystem service functions/trade-offs and synergies/karst carbon sink/karst region

引用本文复制引用

邓群群,李阳兵,白晓永..碳酸盐岩风化碳汇对喀斯特生态系统服务功能权衡协同的影响[J].生态学报,2026,46(4):1724-1736,13.

基金项目

国家自然科学基金(U24A20579,U22A20619) (U24A20579,U22A20619)

贵州省科技创新人才团队建设项目(黔科合人才CXTD[2025]057号) (黔科合人才CXTD[2025]057号)

贵州省科技计划项目(黔科合支撑[2024]重点014) (黔科合支撑[2024]重点014)

生态学报

OACHSSCD

1000-0933

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