全土壤变暖对高寒草地生态系统碳通量的影响

IF 2.3
Ying Chen, Mengguang Han, Qi Shen, Wenkuan Qin, Zhenhua Zhang, Jin-Sheng He, Biao Zhu
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引用次数: 0

摘要

全球变暖影响了生态系统碳交换,从而改变了陆地生态系统的碳汇能力。然而,生态系统碳通量对整个土壤剖面变暖的响应尚不清楚。我们还编制了一个包含48篇文章的数据库,使用全球元分析来检验这些通量的实验变暖效应的一般模式。结果全土壤升温使高寒草地生态系统总生产力(GEP)提高14%,生态系统呼吸(ER)提高11%,但对生态系统净碳交换(NEE)影响较小。在荟萃分析中,变暖也增加了GEP(10%-11%)和ER(13%),但没有改变NEE。增温引起的植物群落变化和生长期延长可能是增温条件下植物GEP和ER较高的主要原因,两者的抵消可能导致NEE对增温的响应较小。结论应重视生态系统碳通量对全土壤或全生态系统全年变暖的长期响应。这些新发现可能有助于我们更好地预测和减轻现实变暖情景下未来的气候-碳反馈。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Effects of whole-soil warming on ecosystem carbon fluxes in an alpine grassland

Effects of whole-soil warming on ecosystem carbon fluxes in an alpine grassland

Background

Global warming impacts ecosystem carbon exchange, thus altering the carbon sink capacity of terrestrial ecosystems. However, the response of ecosystem carbon fluxes to whole-soil-profile warming remains unclear.

Methods

We first investigated the effect of whole-soil warming on ecosystem carbon fluxes in an alpine grassland ecosystem on the Qinghai-Tibet Plateau. We also compiled a database of 48 articles to examine the general patterns of experimental warming effects on these fluxes using a global meta-analysis.

Results

Our results showed that whole-soil warming elevated gross ecosystem productivity (GEP) by 14% and ecosystem respiration (ER) by 11%, but had a minor impact on net ecosystem carbon exchange (NEE) in the alpine grassland. In the meta-analysis, warming also enhanced GEP (10%–11%) and ER (13%), but did not alter NEE. Warming-induced shifts in plant community and extension of growing season may be the main reasons for the higher GEP and ER under warming, and the offset of both fluxes likely caused the minor response of NEE to warming.

Conclusions

More attention should be paid to the long-term response of ecosystem carbon fluxes to whole-soil or whole-ecosystem warming throughout the year. These novel findings may help us better predict and mitigate future climate-carbon feedback under realistic warming scenarios.

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