Does leaf wax isotopic characterisation of gymnosperms and angiosperms capture environmental gradients in Himalayas?

IF 2.6 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Organic Geochemistry Pub Date : 2023-12-10 DOI:10.1016/j.orggeochem.2023.104720
Deepak Kumar Jha , Pranav Hirave , Sambit Ghosh , Bibhasvata Dasgupta , Prasanta Sanyal
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Abstract

The responses of angiosperms and gymnosperms to environmental variables (e.g., rainfall [MAP], temperature [MAT] and pCO2) remain ambiguous and require systematic investigation. This study monitored the plants' responses to changing environments and measured variations in molecular n-alkane indices, δ13Cbulk, δ13Cn-alkanes, and δ2Hn-alkanes values in woody gymnosperms (n = 36) and angiosperms (n = 17) from an altitudinal gradient (0.9 to 3.8 km) in the Himalayas The results indicate that δ13Cbulk values in angiosperms show a moderate correlation with altitude, MAP, and pCO2, while gymnosperms show no response in their δ13Cbulk. The δ13Cn-alkanes values in angiosperms remain unaffected by MAP, MAT, and pCO2, whereas gymnosperms exhibit a moderate negative correlation. The fractionations between δ13Cn-alkanes and δ13Cbulk values (ɛalk/leaf) are approximately –4.0 ± 1.6 ‰ and –5.6 ± 1.5 ‰ for gymnosperms and angiosperms, respectively. In gymnosperms, the fractionation between δ2Hn-alkane and δ2Hrain (ɛalk/rain) is –133.2 ± 39.8 ‰ and –122.8 ± 38.0 ‰ (C31), while in angiosperms, it is –88.5 ± 44.6 ‰ (C29) and –62.4 ± 22.9 ‰ (C31). The δ2Hn-alkane values in gymnosperms and angiosperms are weakly and positively influenced by MAT and MAP, respectively. We found that gymnosperms are enriched in 13C (∼1.5–3.0 ‰) and depleted in 2H (∼56–60 ‰) compared to angiosperms; this pattern is consistent throughout the latitudes sampled in this study. The species-specific isotopic response to environmental factors is primarily driven by lower stomatal conductance, smaller leaf-size, and presence of complex tracheids in gymnosperms compared to angiosperms. The statistical K-means algorithm of dual isotope analysis (δ13Cn-alkanes and δ2Hn-alkane) provided two distinct clusters with an accuracy of 70 % for angiosperms and gymnosperms, which has implications for studying past vegetation transitions.

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裸子植物和被子植物的叶蜡同位素特征是否捕捉到喜马拉雅山的环境梯度?
被子植物和裸子植物对环境变量(如降雨量[MAP]、温度[MAT]和 pCO2)的反应仍然不明确,需要进行系统研究。本研究监测了植物对环境变化的反应,并测量了海拔梯度(0.结果表明,被子植物的 δ13Cbulk 值与海拔高度、MAP 和 pCO2 呈中度相关,而裸子植物的 δ13Cbulk 值则无反应。被子植物的 δ13Cn-alkanes 值不受海拔高度、MAP 和 pCO2 的影响,而裸子植物则表现出中等程度的负相关。被子植物和裸子植物的 δ13Cn-alkanes 和 δ13Cbulk 值(ɛalk/叶)之间的分馏率分别约为 -4.0 ± 1.6 ‰ 和 -5.6 ± 1.5 ‰。在裸子植物中,δ2Hn-烷和δ2Hrain(ɛalk/rain)的分馏率分别为-133.2 ± 39.8 ‰和-122.8 ± 38.0 ‰(C31),而在被子植物中,δ2Hn-烷和δ2Hrain 的分馏率分别为-88.5 ± 44.6 ‰(C29)和-62.4 ± 22.9 ‰(C31)。裸子植物和被子植物的δ2Hn-烷值分别受到 MAT 和 MAP 的微弱和积极影响。我们发现,与被子植物相比,裸子植物的 13C 含量较高(∼1.5-3.0 ‰),而 2H 含量较低(∼56-60 ‰);这一模式在本研究采样的整个纬度都是一致的。与被子植物相比,裸子植物较低的气孔导度、较小的叶片尺寸和复杂的气管的存在是物种对环境因素的同位素特异性反应的主要驱动因素。双同位素分析(δ13Cn-烷烃和δ2Hn-烷烃)的统计K-means算法为被子植物和裸子植物提供了两个不同的聚类,准确率为70%,这对研究过去的植被过渡具有重要意义。
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来源期刊
Organic Geochemistry
Organic Geochemistry 地学-地球化学与地球物理
CiteScore
5.50
自引率
6.70%
发文量
100
审稿时长
61 days
期刊介绍: Organic Geochemistry serves as the only dedicated medium for the publication of peer-reviewed research on all phases of geochemistry in which organic compounds play a major role. The Editors welcome contributions covering a wide spectrum of subjects in the geosciences broadly based on organic chemistry (including molecular and isotopic geochemistry), and involving geology, biogeochemistry, environmental geochemistry, chemical oceanography and hydrology. The scope of the journal includes research involving petroleum (including natural gas), coal, organic matter in the aqueous environment and recent sediments, organic-rich rocks and soils and the role of organics in the geochemical cycling of the elements. Sedimentological, paleontological and organic petrographic studies will also be considered for publication, provided that they are geochemically oriented. Papers cover the full range of research activities in organic geochemistry, and include comprehensive review articles, technical communications, discussion/reply correspondence and short technical notes. Peer-reviews organised through three Chief Editors and a staff of Associate Editors, are conducted by well known, respected scientists from academia, government and industry. The journal also publishes reviews of books, announcements of important conferences and meetings and other matters of direct interest to the organic geochemical community.
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