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在可控环境条件和可变湿度下生长的C3禾本科植物完全成熟叶片上,次生叶蜡正构烷合成量较低。

Low secondary leaf wax n-alkane synthesis on fully mature leaves of C3 grasses grown at controlled environmental conditions and variable humidity.

作者信息

Gamarra Bruno, Kahmen Ansgar

机构信息

Department of Environmental Systems Sciences, ETH Zürich, Switzerland.

Department of Environmental Sciences - Botany, University of Basel, Switzerland.

出版信息

Rapid Commun Mass Spectrom. 2017 Jan 30;31(2):218-226. doi: 10.1002/rcm.7770.

Abstract

RATIONALE

Leaf wax n-alkanes are long-chained aliphatic compounds that are present in the cuticle of terrestrial plant leaves. Their δ H values are used for the reconstruction of past environments and for plant ecological investigations. The timing of n-alkane synthesis during leaf development and the rate of synthesis of secondary n-alkanes in fully matured leaves are still a matter of debate.

METHODS

Using a H-labeling approach we estimated secondary leaf wax n-alkane synthesis rates in mature leaf blades of six C3 grass species grown in climate chambers under controlled environmental conditions.

RESULTS

We found that mature grass leaves continue the synthesis of leaf wax n-alkanes after leaf maturation. The rate of secondary n-alkanes synthesis was, however, relatively low and varied in response to atmospheric humidity and among species from 0.09 to 1.09% per day.

CONCLUSIONS

Our investigation provides new evidence on the timing of cuticular wax synthesis in grass leaves and indicates that the majority of n-alkanes are synthesized during the initial development of the leaf. Our study will improve the interpretation of leaf wax n-alkane δ H values in environmental and geological studies as it suggests that secondary synthesis of leaf wax n-alkanes in grass leaves contributes only slightly to the geological record. Copyright © 2016 John Wiley & Sons, Ltd.

摘要

原理

叶片蜡质正构烷烃是存在于陆生植物叶片角质层中的长链脂肪族化合物。它们的δH值用于重建过去的环境以及植物生态研究。叶片发育过程中正构烷烃的合成时间以及完全成熟叶片中次生正构烷烃的合成速率仍是一个有争议的问题。

方法

我们采用氢标记法,在可控环境条件下的气候箱中,对六种C3禾本科植物成熟叶片的次生叶片蜡质正构烷烃合成速率进行了估算。

结果

我们发现成熟的禾本科植物叶片在叶片成熟后仍继续合成叶片蜡质正构烷烃。然而,次生正构烷烃的合成速率相对较低,且因大气湿度和物种不同而有所变化,每天为0.09%至1.09%。

结论

我们的研究为禾本科植物叶片角质层蜡质合成的时间提供了新的证据,并表明大多数正构烷烃是在叶片的初始发育阶段合成的。我们的研究将改进环境和地质研究中对叶片蜡质正构烷烃δH值的解释,因为这表明禾本科植物叶片蜡质正构烷烃的次生合成对地质记录的贡献很小。版权所有©2016约翰威立父子有限公司。

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