Changes in productivity partitioning induced by precipitation extremes increase inaccuracy of grassland carbon estimation

IF 10.8 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION
Jiamei Sun, Yue Yan, Bin Zhang, Wei Liu, Shande Dou, Xiaoliang Wang, Jianhui Huang, Dima Chen, Changhui Wang, Xingguo Han, Qingmin Pan
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Abstract

The fraction of net primary productivity (NPP) allocated to belowground organs (fBNPP) in grasslands is a critical parameter in global carbon cycle models; moreover, understanding the effect of precipitation changes on this parameter is vital to accurately estimating carbon sequestration in grassland ecosystems. However, how fBNPP responds to temporal precipitation changes along a gradient from extreme drought to extreme wetness, remains unclear, mainly due to the lack of long-term data of belowground net primary productivity (BNPP) and the fact that most precipitation experiments did not have a gradient from extreme drought to extreme wetness. Here, by conducting both a precipitation gradient experiment (100–500 mm) and a long-term observational study (34 years) in the Inner Mongolia grassland, we showed that fBNPP decreased linearly along the precipitation gradient from extreme drought to extreme wetness due to stronger responses in aboveground NPP to drought and wet conditions than those of BNPP. Our further meta-analysis in grasslands worldwide also indicated that fBNPP increased when precipitation decreased, and the vice versa. Such a consistent pattern of fBNPP response suggests that plants increase the belowground allocation with decreasing precipitation, while increase the aboveground allocation with increasing precipitation. Thus, the linearly decreasing response pattern in fBNPP should be incorporated into models that forecast carbon sequestration in grassland ecosystems; failure to do so will lead to underestimation of the carbon stock in drought years and overestimation of the carbon stock in wet years in grasslands.

Abstract Image

极端降水引起的生产力分配变化增加了草地碳估算的不准确性。
草地净初级生产力(NPP)中分配给地下器官的部分(fBNPP)是全球碳循环模型中的一个关键参数;此外,了解降水变化对这一参数的影响对于准确估算草地生态系统的碳封存至关重要。然而,由于缺乏地下净初级生产力(BNPP)的长期数据,而且大多数降水实验并没有从极端干旱到极端湿润的梯度,因此地下净初级生产力如何响应从极端干旱到极端湿润的降水梯度的时间变化仍不清楚。在此,我们在内蒙古草原进行了降水梯度实验(100-500 毫米)和长期观测研究(34 年),结果表明,由于地上部净初级生产力对干旱和潮湿条件的响应比地下净初级生产力的响应更强,fBNPP 在从极端干旱到极端潮湿的降水梯度上呈线性下降。我们对全球草地的进一步荟萃分析也表明,当降水减少时,fBNPP 增加,反之亦然。这种一致的 fBNPP 响应模式表明,植物会随着降水量的减少而增加地下分配,而随着降水量的增加而增加地上分配。因此,应将 fBNPP 线性递减的响应模式纳入预测草地生态系统固碳的模型中;否则将导致低估干旱年份草地的碳储量,高估潮湿年份草地的碳储量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Global Change Biology
Global Change Biology 环境科学-环境科学
CiteScore
21.50
自引率
5.20%
发文量
497
审稿时长
3.3 months
期刊介绍: Global Change Biology is an environmental change journal committed to shaping the future and addressing the world's most pressing challenges, including sustainability, climate change, environmental protection, food and water safety, and global health. Dedicated to fostering a profound understanding of the impacts of global change on biological systems and offering innovative solutions, the journal publishes a diverse range of content, including primary research articles, technical advances, research reviews, reports, opinions, perspectives, commentaries, and letters. Starting with the 2024 volume, Global Change Biology will transition to an online-only format, enhancing accessibility and contributing to the evolution of scholarly communication.
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