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青藏高原高寒草甸植物的表皮蜡质:基于纬度梯度推断的气候效应

Cuticular waxes in alpine meadow plants: climate effect inferred from latitude gradient in Qinghai-Tibetan Plateau.

作者信息

Guo Yanjun, Guo Na, He Yuji, Gao Jianhua

机构信息

College of Agronomy and Biotechnology Southwest University Chongqing 400716 China.

出版信息

Ecol Evol. 2015 Aug 25;5(18):3954-68. doi: 10.1002/ece3.1677. eCollection 2015 Sep.

Abstract

Alpine meadow ecosystems are susceptible to climate changes. Still, climate impact on cuticular wax in alpine meadow plants is poorly understood. Assessing the variations of cuticular wax in alpine meadow plants across different latitudes might be useful for predicting how they may respond to climate change. We studied nine alpine meadows in a climate gradient in the east side of Qinghai-Tibetan Plateau, with mean annual temperature ranging from -7.7 to 3.2°C. In total, 42 plant species were analyzed for cuticular wax, averaged 16 plant species in each meadow. Only four plant species could be observed in all sampling meadows, including Kobresia humilis,Potentilla nivea,Anaphalis lacteal, and Leontopodium nanum. The amounts of wax compositions and total cuticular wax in the four plant species varied among sampling meadows, but no significant correlation could be observed between them and temperature, precipitation, and aridity index based on plant species level. To analyze the variations of cuticular wax on community level, we averaged the amounts of n-alkanes, aliphatic acids, primary alcohols, and total cuticular wax across all investigated plant species in each sampling site. The mean annual temperature, mean temperature in July, and aridity index were significantly correlated with the averaged amounts of wax compositions and total cuticular wax. The average chain length of n-alkanes in both plant and soil linearly increased with increased temperature, whereas reduced with increased aridity index. No significant correlation could be observed between mean annual precipitation and mean precipitation from June to August and the cuticular wax amounts and average chain length. Our results suggest that the survival of some alpine plants in specific environments might be depended on their abilities in adjusting wax deposition on plant leaves, and the alpine meadow plants as a whole respond to climate change, benefiting the stability of alpine meadow ecosystem.

摘要

高山草甸生态系统易受气候变化影响。然而,气候对高山草甸植物表皮蜡质的影响仍知之甚少。评估不同纬度高山草甸植物表皮蜡质的变化,可能有助于预测它们对气候变化的响应。我们研究了青藏高原东侧气候梯度上的9个高山草甸,年平均温度范围为-7.7至3.2°C。总共分析了42种植物的表皮蜡质,每个草甸平均有16种植物。在所有采样草甸中仅能观察到4种植物,包括矮嵩草、雪白委陵菜、乳白香青和小垫状点地梅。这4种植物的蜡质成分含量和总表皮蜡质在采样草甸间存在差异,但基于植物物种水平,未观察到它们与温度、降水和干旱指数之间存在显著相关性。为了分析群落水平上表皮蜡质的变化,我们对每个采样点所有调查植物物种的正构烷烃、脂肪酸、伯醇和总表皮蜡质含量进行了平均。年平均温度、7月平均温度和干旱指数与蜡质成分平均含量和总表皮蜡质显著相关。植物和土壤中正构烷烃的平均链长均随温度升高呈线性增加,而随干旱指数增加而降低。未观察到年平均降水量以及6月至8月平均降水量与表皮蜡质含量和平均链长之间存在显著相关性。我们的结果表明,一些高山植物在特定环境中的生存可能取决于它们调节叶片蜡质沉积的能力,并且高山草甸植物作为一个整体对气候变化做出响应,这有利于高山草甸生态系统的稳定性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fc7f/4588662/e20d6223cfd7/ECE3-5-3954-g001.jpg

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