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Aboveground carbon sequestration of Cunninghamia lanceolata forests:Magnitude and driversOACSTPCD

中文摘要

Understanding the spatial variation,temporal changes,and their underlying driving forces of carbon sequestration in various forests is of great importance for understanding the carbon cycle and carbon management options.How carbon density and sequestration in various Cunninghamia lanceolata forests,extensively cultivated for timber production in subtropical China,vary with biodiversity,forest structure,environment,and cultural factors remain poorly explored,presenting a critical knowledge gap for realizing carbon sequestration supply potential through management.Based on a large-scale database of 449 permanent forest inventory plots,we quantified the spatial-temporal heterogeneity of aboveground carbon densities and carbon accumulation rates in Cunninghamia lanceolate forests in Hunan Province,China,and attributed the contributions of stand structure,environmental,and management factors to the heterogeneity using quantile age-sequence analysis,partial least squares path modeling(PLS-PM),and hot-spot analysis.The results showed lower values of carbon density and sequestration on average,in comparison with other forests in the same climate zone(i.e.,subtropics),with pronounced spatial and temporal variability.Specifically,quantile regression analysis using carbon accumulation rates along an age sequence showed large differences in carbon sequestration rates among underperformed and outperformed forests(0.50 and 1.80 Mg·ha^(-1)·yr^(-1)).PLS-PM demonstrated that maximum DBH and stand density were the main crucial drivers of aboveground carbon density from young to mature forests.Furthermore,species diversity and geotopographic factors were the significant factors causing the large discrepancy in aboveground carbon density change between low-and high-carbon-bearing forests.Hotspot analysis revealed the importance of culture attributes in shaping the geospatial patterns of carbon sequestration.Our work highlighted that retaining largesized DBH trees and increasing shade-tolerant tree species were important to enhance carbon sequestration in C.lanceolate forests.

Chen Wang;Shuguang Liu;Yu Zhu;Andrew R.Smith;Ying Ning;Deming Deng;

National Engineering Laboratory for Applied Technology of Forestry&Ecology in South China,Central South University of Forestry and Technology,Changsha 410004,China Technology Innovation Center for Ecological Conservation and Restoration in Dongting Lake Basin,Ministry of Natural Resources,Changsha 410007,China College of Life Science and Technology,Central South University of Forestry and Technology,Changsha 410004,ChinaNational Engineering Laboratory for Applied Technology of Forestry&Ecology in South China,Central South University of Forestry and Technology,Changsha 410004,China College of Life Science and Technology,Central South University of Forestry and Technology,Changsha 410004,China School of Ecology and Environment,Hainan University,Haikou 570228,ChinaSchool of Natural Sciences,Bangor University,Gwynedd,LL572UW,UKNational Engineering Laboratory for Applied Technology of Forestry&Ecology in South China,Central South University of Forestry and Technology,Changsha 410004,China Technology Innovation Center for Ecological Conservation and Restoration in Dongting Lake Basin,Ministry of Natural Resources,Changsha 410007,China College of Forestry,Central South University of Forestry and Technology,Changsha 410004,ChinaHunan Prospecting Designing&Research General Institute for Agriculture,Forestry&Industry,Changsha 410007,China

林学

Carbon densityCarbon accumulation rateForest ageSpatial variationCultural influence

《Forest Ecosystems》 2024 (001)

P.32-41 / 10

the National Natural Science Foundation of China(Nos.U20A2089 and 41971152);the Research Foundation of the Department of Natural Resources of Hunan Province(No.20230138ST)to SL;the open research fund of Technology Innovation Center for Ecological Conservation and Restoration in Dongting Lake Basin,Ministry of Natural Resources(No.2023005)to YZ。

10.1016/j.fecs.2024.100165

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