植物生态学报 ›› 2009, Vol. 33 ›› Issue (6): 1208-1219.DOI: 10.3773/j.issn.1005-264x.2009.06.022
徐振锋1,2, 尹华军1, 赵春章1, 曹刚1, 万名利1, 刘庆1,*()
收稿日期:
2009-04-02
接受日期:
2009-07-13
出版日期:
2009-11-30
发布日期:
2021-04-29
通讯作者:
刘庆
作者简介:
*(liuqing@cib.ac.cn)基金资助:
XU Zhen-Feng1,2, YIN Hua-Jun1, ZHAO Chun-Zhang1, CAO Gang1, WAN Ming-Li1, LIU Qing1,*()
Received:
2009-04-02
Accepted:
2009-07-13
Online:
2009-11-30
Published:
2021-04-29
Contact:
LIU Qing
摘要:
陆地生态系统凋落物分解是全球碳收支的一个重要组成部分, 主要受气候、凋落物质量和土壤生物群落的综合控制。科学家们普遍认为全球气候变化将对陆地生态系统凋落物分解产生复杂而深远的影响。该文结合凋落物分解试验的常用方法——缩微试验、原位模拟实验和自然环境梯度实验, 归纳现有研究结果, 意在揭示全球气候变化对陆地生态系统凋落物分解的直接影响(温度对凋落物分解速率的影响)和间接影响(温度对凋落物质量、土壤微生物群落及植被型的影响)的普遍规律。各种研究方法都表明: 在水分条件理想的情况下, 温度升高往往能加快凋落物的分解速率; 原位模拟实验中, 凋落物分解速率因物种、增温方法和地理方位而异; 全球气候变化能改变凋落物质量, 但可能不会在短期内影响凋落物的分解速率; 凋落物质量和可分解性的种间差异远大于增温所引发的表型响应差异, 那么, 气候变化所引发的植物群落结构和物种组成的变化将对陆地生态系统凋落物分解产生更强烈的影响; 土壤生物群落如何响应全球气候变化, 进而怎样影响凋落物分解过程, 这些都还存在着极大的不确定性。
徐振锋, 尹华军, 赵春章, 曹刚, 万名利, 刘庆. 陆地生态系统凋落物分解对全球气候变暖的响应. 植物生态学报, 2009, 33(6): 1208-1219. DOI: 10.3773/j.issn.1005-264x.2009.06.022
XU Zhen-Feng, YIN Hua-Jun, ZHAO Chun-Zhang, CAO Gang, WAN Ming-Li, LIU Qing. A REVIEW OF RESPONSES OF LITTER DECOMPOSITION IN TERRESTRIAL ECOSYSTEMS TO GLOBAL WARMING. Chinese Journal of Plant Ecology, 2009, 33(6): 1208-1219. DOI: 10.3773/j.issn.1005-264x.2009.06.022
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[14] | 宋小艳, 王根绪, 冉飞, 杨燕, 张莉, 肖瑶. 东北大兴安岭演替初期泰加林灌草层典型植物开花物候与生长对模拟暖干化气候的响应[J]. 植物生态学报, 2018, 42(5): 539-549. |
[15] | 武启骞, 王传宽. 控雪处理下红松和蒙古栎凋落叶分解动态[J]. 植物生态学报, 2018, 42(2): 153-163. |
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