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Foliar pH, an emerging plant functional trait: Biogeography and variability across northern China

机译:叶面pH,一种新兴植物功能性状:中国北方的生物地理和变异性

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Aims Plant pH is a functional trait deserving more attention than the current few studies at local scales, given its roles in nutrient cycling and physiological processes. How plant pH varies and is regulated at large scales remain unclear. Here we explore the biogeography of foliar pH and the potential drivers. Location East-west transect of northern China with increasing aridity westward. Time period 2016-2017. Major taxa Spermatophytes. Methods We analysed foliar pH of plants from 22 sites across northern China, and investigated its spatial pattern and relationships with climate, soil, and plant functional type (PFT). Results Foliar pH was generally acidic (5.33 +/- .04) in northern China, showing distinct geographical variability: foliar pH decreased significantly westward at an average rate of 0.25 units per 10 degrees longitude. Climate, soil and PFT explained 11, 17 and 59% of the variance in foliar pH, respectively. Foliar pH decreased (about 0.16) with mean annual precipitation (per 100 mm), soil stress coefficient (per 10%) and aridity index (per 0.14), but increased with mean annual temperature (per 2 degrees C). Across PFTs, herbs exhibited higher foliar pH than woody plants (6.0 vs. 4.9); gymnosperms relative to angiosperms had lower foliar pH (3.7 vs. 5.6); and monocotyledons showed higher foliar pH compared with dicotyledons (6.0 vs. 5.5). Main conclusions This study provides the first comprehensive analysis of the evident pattern of foliar pH over a large spatial scale. Foliar pH is higher in warm-arid northwestern relative to cold-humid northeastern China and in later- than earlier-evolved plants. Similar to leaf mineral elements, foliar-pH biogeography is shaped by the joint effects of climate, soil and PFT; PFT and moisture are the most influential factors. Our findings provide a new impetus for understanding functional biogeography, and lay the groundwork for research on the linkage of foliar pH to ecological functions and macroevolutionary implications.
机译:鉴于营养循环和生理过程的角色,目前植物pH值得比当前鳞片的目前的研究更加关注。植物pH如何变化,并在大尺度上调节仍然不清楚。在这里,我们探索叶面pH和潜在司机的生物地理。北方北方的东西部横断面随着旱灾的增加。 2016-2017的时间段。主要的分类杀菌精菌。方法从中国北方的22个站点分析了植物的叶面pH,并调查了其气候,土壤和植物功能型(PFT)的空间模式和关系。结果叶酸通常在中国酸性(5.33 +/- .04),显示出明显的地理变异性:叶面pH值下降,平均速度为0.25单位经度0.25单位。气候,土壤和PFT分别解释了叶面pH的差异的11,17和59%。叶酸下降(约0.16),平均年降水量(每100毫米),土壤应激系数(每10%)和干燥指数(每0.14),但随着平均年度温度(每2摄氏度)增加。跨PFT,草药表现出比木质植物更高的叶面pH(6.0与4.9);裸子植物相对于高血管植物具有较低的叶酸pH(3.7与5.6);与双子叶(6.0对5.5)相比,单子叶和单圈子均显示出更高的叶酸。本研究主要结论本研究规定了对大型空间尺度的叶面叶pH的明显模式的第一次综合分析。叶面pH在温暖干旱的西北相对于中国冷漠的东北部和早期进化的植物较高。类似于叶矿物元素,叶酸-PH生物地理成形为气候,土壤和PFT的关节效应; PFT和水分是最有影响力的因素。我们的调查结果为了解功能性生物地理学提供了一种新的推动力,并为叶面pH的联系的研究奠定了基础,对生态功能和宏观调整的影响。

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