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气候变暖引起的物候变化对生态系统碳交换的影响受半干旱草原降水的调节。

The effects of warming-shifted plant phenology on ecosystem carbon exchange are regulated by precipitation in a semi-arid grassland.

机构信息

State Key Laboratory of Vegetation and Environmental Change, Institute of Botany, The Chinese Academy of Sciences, Xiangshan, Beijing, China.

出版信息

PLoS One. 2012;7(2):e32088. doi: 10.1371/journal.pone.0032088. Epub 2012 Feb 16.

DOI:10.1371/journal.pone.0032088
PMID:22359660
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3281109/
Abstract

BACKGROUND

The longer growing season under climate warming has served as a crucial mechanism for the enhancement of terrestrial carbon (C) sink over the past decades. A better understanding of this mechanism is critical for projection of changes in C cycling of terrestrial ecosystems.

METHODOLOGY/PRINCIPAL FINDINGS: A 4-year field experiment with day and night warming was conducted to examine the responses of plant phenology and their influences on plant coverage and ecosystem C cycling in a temperate steppe in northern China. Greater phenological responses were observed under night than day warming. Both day and night warming prolonged the growing season by advancing phenology of early-blooming species but without changing that of late-blooming species. However, no warming response of vegetation coverage was found for any of the eight species. The variances in species-level coverage and ecosystem C fluxes under different treatments were positively dependent upon the accumulated precipitation within phenological duration but not the length of phenological duration.

CONCLUSIONS/SIGNIFICANCE: These plants' phenology is more sensitive to night than day warming, and the warming effects on ecosystem C exchange via shifting plant phenology could be mediated by precipitation patterns in semi-arid grasslands.

摘要

背景

在过去几十年中,气候变暖导致的生长季延长是增强陆地碳(C)汇的关键机制。更好地理解这一机制对于预测陆地生态系统的碳循环变化至关重要。

方法/主要发现:本研究在中国北方的温带草原进行了为期 4 年的日夜间增温野外实验,以检验植物物候对植物覆盖度和生态系统 C 循环的影响。夜间增温比日间增温引起更大的物候响应。日夜间增温都通过提前早期开花物种的物候来延长生长季,但不改变晚期开花物种的物候。然而,在八种物种中,没有发现任何一种植被覆盖度有增温响应。不同处理下物种水平覆盖度和生态系统 C 通量的方差与物候持续时间内的累积降水量呈正相关,而与物候持续时间的长度无关。

结论/意义:这些植物的物候对夜间增温比对日间增温更敏感,通过改变植物物候来影响生态系统 C 交换的增温效应可能受到半干旱草原降水模式的调节。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/ea29cab29ca7/pone.0032088.g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/80304de18c65/pone.0032088.g001.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/088fd132b817/pone.0032088.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/954507a5b25b/pone.0032088.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/b5dfbd432ef2/pone.0032088.g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/a7633f931b77/pone.0032088.g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/ea29cab29ca7/pone.0032088.g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/80304de18c65/pone.0032088.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/a44ae3adae57/pone.0032088.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/088fd132b817/pone.0032088.g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/954507a5b25b/pone.0032088.g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/b5dfbd432ef2/pone.0032088.g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/a7633f931b77/pone.0032088.g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bcf6/3281109/ea29cab29ca7/pone.0032088.g007.jpg

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