Forest carbon storage along the north-south transect of eastern China: Spatial patterns, allocation, and influencing factors

被引:57
|
作者
Wen, Ding [1 ,2 ]
He, Nianpeng [1 ]
机构
[1] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Carbon storage; Carbon allocation; NSTEC; Forest; Pattern; Scale; SOIL CARBON; ORGANIC-CARBON; TEMPERATURE SENSITIVITY; DECOMPOSITION RATES; CLIMATE-CHANGE; BIOMASS; SCALE; DENSITY; POOLS; SEQUESTRATION;
D O I
10.1016/j.ecolind.2015.10.054
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Forests play an important role in sequestrating atmospheric CO2; therefore, understanding the spatial variations and controlling mechanisms of forest carbon (C) storage is important. In this study, we collected data on forest C storage along a north-south transect of eastern China from literature published between 2004 and 2014. The collected data, which were from over 2000 plots, allowed us to explore the latitudinal patterns in forest C storage. The results showed that vegetation C storage decreased with increasing latitude, while soil C storage increased. This spatial pattern of vegetation C storage was more apparent for mature forests (forest age >80 years). Furthermore, latitudinal patterns in forest C storage, both in vegetation and in soil, became stronger with increasing statistical scale, increasing from plot scale to latitudinal scale (2-5). However, total forest C storage (vegetation + soil) had no apparent latitudinal pattern. Interestingly, the allocation ratios of forest C storage between vegetation and soil had a negative logarithmic relationship with latitude. These results suggest that in eastern China, climatic factors control latitudinal patterns in the forest C storage of vegetation and soil, albeit in different ways (positive for vegetation and negative for soil), and also control the allocation ratios of forest C storage between vegetation and soil. Furthermore, the latitudinal patterns of forest C storage were opposite for vegetation and soil, resulting from the different climatic controlling mechanism. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:960 / 967
页数:8
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