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青藏高原草原光合作用的气候限制因素由温度转为水分。

Climatic limitations on grassland photosynthesis over the Tibetan Plateau shifted from temperature to water.

机构信息

Faculty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 610031, China.

Faculty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 610031, China.

出版信息

Sci Total Environ. 2024 Jan 1;906:167663. doi: 10.1016/j.scitotenv.2023.167663. Epub 2023 Oct 7.

Abstract

Plant photosynthesis plays an essential role in regulating the global carbon cycle. Therefore, it is essential to understand the limitations imposed by climate on plant photosynthesis to comprehend the impacts of climate change on land carbon dynamics. In this study, taking gross primary productivity as a direct representation of photosynthesis, we employed a light use efficiency model (i.e., the revised EC-LUE) and factorial analysis method to quantify the spatiotemporal variation of temperature- and water-limitations on plant photosynthesis over the Tibetan Plateau (TP) grasslands during growing season (May to October) in 1983-2018. Results revealed a clear spatiotemporal pattern of the temperature- and water-limitations: temperature is the primary climatic limiting factor in the eastern TP, while water is the primary climatic limiting factor in the western TP; the water- and temperature-limitations prevail in summer and spring/autumn, respectively. The water- and temperature-limitations intensified and alleviated, respectively, during 1983 through 2018. There also was a widespread shift from temperature-limitation to water-limitation in the TP, particularly in midsummer (August). Our findings demonstrated the shifting relative importance of climatic limitations on plant photosynthesis under changing climate, which is crucial for predicting future terrestrial carbon cycle dynamics.

摘要

植物光合作用在调节全球碳循环中起着至关重要的作用。因此,了解气候对植物光合作用的限制作用对于理解气候变化对陆地碳动态的影响至关重要。在本研究中,我们以总初级生产力(Gross Primary Productivity,GPP)作为光合作用的直接代表,利用光能利用效率模型(即修正后的 EC-LUE)和因子分析方法,量化了 1983 年至 2018 年青藏高原(TP)草原生长季(5 月至 10 月)期间温度和水分对植物光合作用的时空变化限制。结果揭示了温度和水分限制的明显时空格局:在青藏高原东部,温度是主要的气候限制因素,而在青藏高原西部,水分是主要的气候限制因素;水分和温度限制分别在夏季和春/秋季占主导地位。在 1983 年至 2018 年期间,水分和温度限制分别加剧和缓解。TP 地区也出现了从温度限制到水分限制的广泛转变,尤其是在盛夏(8 月)。本研究结果表明,在气候变化下,气候限制对植物光合作用的相对重要性发生了变化,这对于预测未来陆地碳循环动态至关重要。

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