{"title":"Does leaf wax isotopic characterisation of gymnosperms and angiosperms capture environmental gradients in Himalayas?","authors":"Deepak Kumar Jha , Pranav Hirave , Sambit Ghosh , Bibhasvata Dasgupta , Prasanta Sanyal","doi":"10.1016/j.orggeochem.2023.104720","DOIUrl":null,"url":null,"abstract":"<div><p>The responses of angiosperms and gymnosperms to environmental variables (e.g., rainfall [MAP], temperature [MAT] and <em>p</em>CO<sub>2</sub>) remain ambiguous and require systematic investigation. This study monitored the plants' responses to changing environments and measured variations in molecular <em>n</em>-alkane indices, δ<sup>13</sup>C<sub>bulk</sub>, δ<sup>13</sup>C<em><sub>n</sub></em><sub>-alkanes</sub>, and δ<sup>2</sup>H<em><sub>n</sub></em><sub>-alkanes</sub> 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 δ<sup>13</sup>C<sub>bulk</sub> values in angiosperms show a moderate correlation with altitude, MAP, and <em>p</em>CO<sub>2</sub>, while gymnosperms show no response in their δ<sup>13</sup>C<sub>bulk</sub>. The δ<sup>13</sup>C<em><sub>n</sub></em><sub>-alkanes</sub> values in angiosperms remain unaffected by MAP, MAT, and <em>p</em>CO<sub>2</sub>, whereas gymnosperms exhibit a moderate negative correlation. The fractionations between δ<sup>13</sup>C<em><sub>n</sub></em><sub>-alkanes</sub> and δ<sup>13</sup>C<sub>bulk</sub> values (<em>ɛ<sub>alk/leaf</sub></em>) are approximately –4.0 ± 1.6 ‰ and –5.6 ± 1.5 ‰ for gymnosperms and angiosperms, respectively. In gymnosperms, the fractionation between δ<sup>2</sup>H<em><sub>n</sub></em><sub>-alkane</sub> and δ<sup>2</sup>H<sub>rain</sub> (<em>ɛ<sub>alk/rain</sub></em>) is –133.2 ± 39.8 ‰ and –122.8 ± 38.0 ‰ (C<sub>31</sub>), while in angiosperms, it is –88.5 ± 44.6 ‰ (C<sub>29</sub>) and –62.4 ± 22.9 ‰ (C<sub>31</sub>). The δ<sup>2</sup>H<em><sub>n</sub></em><sub>-alkane</sub> values in gymnosperms and angiosperms are weakly and positively influenced by MAT and MAP, respectively. We found that gymnosperms are enriched in <sup>13</sup>C (∼1.5–3.0 ‰) and depleted in <sup>2</sup>H (∼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 (δ<sup>13</sup>C<em><sub>n</sub></em><sub>-alkanes</sub> and δ<sup>2</sup>H<em><sub>n</sub></em><sub>-alkane</sub>) provided two distinct clusters with an accuracy of 70 % for angiosperms and gymnosperms, which has implications for studying past vegetation transitions.</p></div>","PeriodicalId":400,"journal":{"name":"Organic Geochemistry","volume":"187 ","pages":"Article 104720"},"PeriodicalIF":2.6000,"publicationDate":"2023-12-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S0146638023001663/pdfft?md5=ac46addba4004f1314d25c8fc4afda05&pid=1-s2.0-S0146638023001663-main.pdf","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Organic Geochemistry","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0146638023001663","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
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.
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.