Stephanie P. George-Chacon, T. Luke Smallman, Juan Manuel Dupuy, José Luis Hernández-Stefanoni, David T. Milodowski, Mathew Williams
{"title":"分离全球变化下土地利用和功能变化对Yucatán森林生物量的影响","authors":"Stephanie P. George-Chacon, T. Luke Smallman, Juan Manuel Dupuy, José Luis Hernández-Stefanoni, David T. Milodowski, Mathew Williams","doi":"10.3389/ffgc.2023.1204596","DOIUrl":null,"url":null,"abstract":"Tropical forests hold large stocks of carbon in biomass and face pressures from changing climate and anthropogenic disturbance. Forests' capacity to store biomass under future conditions and accumulate biomass during regrowth after clearance are major knowledge gaps. Here we use chronosequence data, satellite observations and a C-cycle model to diagnose woody C dynamics in two dry forest ecotypes (semi-deciduous and semi-evergreen) in Yucatán, Mexico. Woody biomass differences between mature semi-deciduous (90 MgC ha −1 ) and semi-evergreen (175 MgC ha −1 ) forest landscapes are mostly explained by differences in climate (c. 60%), particularly temperature, humidity and soil moisture effects on production. Functional variation in foliar phenology, woody allocation, and wood turnover rate explained c. 40% of biomass differences between ecotypes. Modeling experiments explored varied forest clearance and regrowth cycles, under a range of climate and CO 2 change scenarios to 2100. Production and steady state biomass in both ecotypes were reduced by forecast warming and drying (mean biomass 2021–2100 reduced 16–19% compared to 2001–2020), but compensated by fertilisation from rising CO 2 . Functional analysis indicates that trait adjustments amplify biomass losses by 70%. Experiments with disturbance and recovery across historically reported levels indicate reductions to mean forest biomass stocks over 2021–2100 similar in magnitude to climate impacts (10–19% reductions for disturbance with recovery). Forest disturbance without regrowth amplifies biomass loss by three- or four-fold. We conclude that vegetation functional differences across the Yucatán climate gradient have developed to limit climate risks. Climate change will therefore lead to functional adjustments for all forest types. These adjustments are likely to magnify biomass reductions caused directly by climate change over the coming century. However, the range of impacts of land use and land use change are as, or more, substantive than the totality of direct and indirect climate impacts. Thus the carbon storage of Yucatan's forests is highly vulnerable both to climate and land use and land use change. Our results here should be used to test and enhance land surface models use for dry forest carbon cycle assessment regionally and globally. A single plant functional type approach for modeling Yucatán's forests is not justified.","PeriodicalId":12538,"journal":{"name":"Frontiers in Forests and Global Change","volume":"21 1","pages":"0"},"PeriodicalIF":2.7000,"publicationDate":"2023-09-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Isolating the effects of land use and functional variation on Yucatán's forest biomass under global change\",\"authors\":\"Stephanie P. George-Chacon, T. Luke Smallman, Juan Manuel Dupuy, José Luis Hernández-Stefanoni, David T. Milodowski, Mathew Williams\",\"doi\":\"10.3389/ffgc.2023.1204596\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Tropical forests hold large stocks of carbon in biomass and face pressures from changing climate and anthropogenic disturbance. Forests' capacity to store biomass under future conditions and accumulate biomass during regrowth after clearance are major knowledge gaps. Here we use chronosequence data, satellite observations and a C-cycle model to diagnose woody C dynamics in two dry forest ecotypes (semi-deciduous and semi-evergreen) in Yucatán, Mexico. Woody biomass differences between mature semi-deciduous (90 MgC ha −1 ) and semi-evergreen (175 MgC ha −1 ) forest landscapes are mostly explained by differences in climate (c. 60%), particularly temperature, humidity and soil moisture effects on production. Functional variation in foliar phenology, woody allocation, and wood turnover rate explained c. 40% of biomass differences between ecotypes. Modeling experiments explored varied forest clearance and regrowth cycles, under a range of climate and CO 2 change scenarios to 2100. Production and steady state biomass in both ecotypes were reduced by forecast warming and drying (mean biomass 2021–2100 reduced 16–19% compared to 2001–2020), but compensated by fertilisation from rising CO 2 . Functional analysis indicates that trait adjustments amplify biomass losses by 70%. Experiments with disturbance and recovery across historically reported levels indicate reductions to mean forest biomass stocks over 2021–2100 similar in magnitude to climate impacts (10–19% reductions for disturbance with recovery). Forest disturbance without regrowth amplifies biomass loss by three- or four-fold. We conclude that vegetation functional differences across the Yucatán climate gradient have developed to limit climate risks. Climate change will therefore lead to functional adjustments for all forest types. These adjustments are likely to magnify biomass reductions caused directly by climate change over the coming century. 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引用次数: 0
摘要
热带森林拥有大量的生物质碳储量,面临着气候变化和人为干扰的压力。森林在未来条件下储存生物量和在砍伐后的再生过程中积累生物量的能力是主要的知识空白。本文利用时序数据、卫星观测和C循环模型对墨西哥Yucatán两种干林生态型(半落叶和半常绿)的木材C动态进行了诊断。成熟半落叶(90 MgC ha - 1)和半常绿(175 MgC ha - 1)森林景观之间的木质生物量差异主要由气候差异(约60%),特别是温度、湿度和土壤水分对生产的影响来解释。叶面物候、木材分配和木材周转率的功能差异解释了生态型间约40%的生物量差异。模拟实验探索了到2100年一系列气候和二氧化碳变化情景下不同的森林砍伐和再生周期。两种生态型的产量和稳态生物量都因预测的增温和干燥而减少(2021-2100年的平均生物量比2001-2020年减少16-19%),但因二氧化碳浓度上升而产生的肥料补偿了产量和稳态生物量。功能分析表明,性状调整使生物量损失增加了70%。在历史报告水平上对干扰和恢复进行的实验表明,2021-2100年期间平均森林生物量储量的减少幅度与气候影响相似(干扰与恢复减少10-19%)。没有再生的森林干扰会使生物量损失增加三到四倍。我们得出结论,Yucatán气候梯度上的植被功能差异已经发展到限制气候风险。因此,气候变化将导致所有森林类型的功能调整。在未来一个世纪,这些调整可能会加剧气候变化直接导致的生物量减少。然而,土地利用和土地利用变化的影响范围与直接和间接气候影响的总和一样大,甚至更大。因此,尤卡坦森林的碳储量极易受到气候和土地利用以及土地利用变化的影响。我们的研究结果应该用于测试和增强用于区域和全球干旱森林碳循环评估的陆地表面模型。用单一植物功能类型方法对Yucatán的森林进行建模是不合理的。
Isolating the effects of land use and functional variation on Yucatán's forest biomass under global change
Tropical forests hold large stocks of carbon in biomass and face pressures from changing climate and anthropogenic disturbance. Forests' capacity to store biomass under future conditions and accumulate biomass during regrowth after clearance are major knowledge gaps. Here we use chronosequence data, satellite observations and a C-cycle model to diagnose woody C dynamics in two dry forest ecotypes (semi-deciduous and semi-evergreen) in Yucatán, Mexico. Woody biomass differences between mature semi-deciduous (90 MgC ha −1 ) and semi-evergreen (175 MgC ha −1 ) forest landscapes are mostly explained by differences in climate (c. 60%), particularly temperature, humidity and soil moisture effects on production. Functional variation in foliar phenology, woody allocation, and wood turnover rate explained c. 40% of biomass differences between ecotypes. Modeling experiments explored varied forest clearance and regrowth cycles, under a range of climate and CO 2 change scenarios to 2100. Production and steady state biomass in both ecotypes were reduced by forecast warming and drying (mean biomass 2021–2100 reduced 16–19% compared to 2001–2020), but compensated by fertilisation from rising CO 2 . Functional analysis indicates that trait adjustments amplify biomass losses by 70%. Experiments with disturbance and recovery across historically reported levels indicate reductions to mean forest biomass stocks over 2021–2100 similar in magnitude to climate impacts (10–19% reductions for disturbance with recovery). Forest disturbance without regrowth amplifies biomass loss by three- or four-fold. We conclude that vegetation functional differences across the Yucatán climate gradient have developed to limit climate risks. Climate change will therefore lead to functional adjustments for all forest types. These adjustments are likely to magnify biomass reductions caused directly by climate change over the coming century. However, the range of impacts of land use and land use change are as, or more, substantive than the totality of direct and indirect climate impacts. Thus the carbon storage of Yucatan's forests is highly vulnerable both to climate and land use and land use change. Our results here should be used to test and enhance land surface models use for dry forest carbon cycle assessment regionally and globally. A single plant functional type approach for modeling Yucatán's forests is not justified.