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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Biomarkers as proxies for plant inputs to peats: an example from a sub-boreal ombrotrophic bog
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Biomarkers as proxies for plant inputs to peats: an example from a sub-boreal ombrotrophic bog

机译:生物标志物作为泥炭植物输入的代理:来自北亚非营养性沼泽的例子

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Lipid distributions in modem peat-forming plants were determined and compared to biomarkers recovered from a ca. 2800 year old peat deposited in a Dutch ombrotrophic bog. The peat section spans a well-constrained shift in local hydrology and vegetation, and potential molecular proxies for plant inputs were directly tested against the macrofossil record. Based on the analyses of modem plants, low-molecular-weight (LMW) n-alkanes (C-23, C-25) and high-molecular-weight n-alkanes (C-33) are proposed as potential biomarkers for Sphagnum and non-Sphagnum inputs, respectively. Consistent with this, in the Bargerveen peat core, LMW n-alkane abundances increase and HMW n-alkane abundances decrease coincident with the shift to Sphagnum dominated peat. Additional potential proxies include the abundances of C-22 alpha,omega-alkanedioic acid and phytenyl phytenoate as Sphagnum indicators and the abundances of the triterpenoids taraxer-14-ene and taraxast-20-ene as biomarkers for Ericaceae rootlets. (C) 2002 Published by Elsevier Science Ltd. [References: 29]
机译:确定了在形成现代泥炭的植物中的脂质分布,并将其与从ca.ca. 2800年的泥炭沉积在荷兰的营养营养沼泽中。泥炭地段跨越了当地水文和植被的一个受约束的变化,直接根据大型化石记录测试了植物输入的潜在分子代理。在对现代植物进行分析的基础上,提出了低分子量(LMW)正构烷烃(C-23,C-25)和高分子量正构烷烃(C-33)作为潜在的生物标记。非泥炭藓输入。与此相一致,在Bargerveen泥炭岩心中,LMW正构烷烃丰度增加,而HMW正构烷烃丰度降低,而转向以泥炭藓为主的泥炭。其他潜在的替代物包括丰富的C-22α,ω-链烷二酸和植烯基肌醇六磷酸酯作为水藓指示剂,以及三萜类化合物taraxer-14-ene和taraxast-20-ene的丰富作为Ericaceae根的生物标记。 (C)2002由Elsevier Science Ltd.发布[参考:29]

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