| 湖泊沉积物C4植物含量重建方法的讨论——以新生代柴达木盆地大红沟剖面为例 |
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| 引用本文： | 李元,孙媛媛,邓国仕,袁峰,刘俊. 湖泊沉积物C4植物含量重建方法的讨论——以新生代柴达木盆地大红沟剖面为例[J]. 沉积与特提斯地质, 2022, 42(4): 572-584. DOI: 10.19826/j.cnki.1009-3850.2022.04019 |
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| 作者姓名： | 李元 孙媛媛 邓国仕 袁峰 刘俊 |
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| 作者单位： | 1.合肥工业大学资源与环境工程学院,安徽 合肥 230009; 2.中国地质调查局成都地质调查中心,四川 成都 610081; 3.自然资源部沉积盆地与油气资源重点实验室,四川 成都 610081 |
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| 基金项目： | 第二次青藏高原综合科学考察(2019QZKK0704, 2019QZKK0708)；国家自然科学基金青年基金(41807333)；国家自然科学基金面上项目(42172026, 41772003)，中央高校基本科研业务费专项资金(PA2020GDKC0022)；中国地质调查局地质调查项目(DD20190080, DD20211381) |
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| 摘 要： | 当前气候变暖是一个全球面临的重大问题，它对人类赖以生存的植被生态系统造成的影响已经在全球各地逐步显现出来。为了深入了解植物生态系统对环境和气候变化的响应机制，我们需要更好地借鉴地质历史时期气候环境和植物协同演化的重要事件。C4植物作为陆地生产力较强的植物，在植物生态演化中占举足轻重的地位。目前研究表明C4植物可能最晚起源于始新世-渐新世之交，但从它早期起源到随后在生态系统中的大规模扩张时间间隔长达20多个百万年。是什么因素导致了C4植物的起源和扩张是一个悬而未决的重要问题，需要开展大量的调查研究来评估和重建C4植物在过去生态系统中的相对生物量变化。重建C4植物的含量目前主要的方法是建立在C3/C4植物碳同位素和植物内部结构形态差异基础之上。最常运用的研究材料包括(古)土壤有机质、成壤碳酸盐、陆地食草动物体组织、沉积物生物标志物、孢粉、植硅体等。这些方法在重建现代以及地质历史时期C4植物相对生物量变化的研究中发挥了重要作用，但同时也存在很多无法避免的问题。本文介绍了C4植物起源和扩张机制的主流观点以及不同研究材料的碳同位素所推算C4植物生物量的基本原理，并以柴达木盆地大红沟剖面为例，针对新生代湖泊沉积物中陆生高等植物的长链正构烷烃特征和单体烃碳同位素的研究结果，详细讨论C4植物含量重建的方法与缺点，为探讨C4植物起源、演化及控制因素提供参考。我们通过分析前人研究的大红沟剖面长链正构烷烃及单体烃 δ13Calk 值特征，推测在30~24 Ma、20~17 Ma和13~7 Ma期间δ13Calk值显示相对正偏的原因，可能是干旱和C4植物在当地生态系统中出现的双重因素叠加造成的。但这一推断还需要借助于新的研究方法，即单颗粒孢粉碳同位素的方法来提供C4植物的确凿证据。
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| 关 键 词： | C4植物 碳同位素 (古)土壤 成壤碳酸盐 牙釉质 植硅体 长链正构烷烃 单颗粒孢粉碳同位素 |
| 收稿时间： | 2021-10-12 |
| 修稿时间： | 2022-04-07 |
Reconstruction of C4 plant content in Cenozoic lacustrine sediments: An example from the Dahonggou section, Qaidam Basin |
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| LI Yuan,SUN Yuanyuan,DENG Guoshi,YUAN Feng,LIU Jun. Reconstruction of C4 plant content in Cenozoic lacustrine sediments: An example from the Dahonggou section, Qaidam Basin[J]. Sedimentary Geology and Tethyan Geology, 2022, 42(4): 572-584. DOI: 10.19826/j.cnki.1009-3850.2022.04019 |
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| Authors: | LI Yuan SUN Yuanyuan DENG Guoshi YUAN Feng LIU Jun |
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| Affiliation: | 1.School of Resources and Environmental Engineering,Hefei University of Technology,Hefei 230009,China; 2.Chengdu Center,China Geological Survey,Chengdu 610081,China; 3.Key Laboratory of Sedimentary Basin and Oil and Gas Resources,Ministry of Natural Resources,Chengdu 610081,China |
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| Abstract: | Global climate change has posed serious effect on the vegetation of our ecosystem. In order to understand the response of plant ecosystems to environmental and climate changes,we need to learn well from the earth’s past. C4 plants play a pivotal role in the modern ecosystems. Previous studies have shown that C4 plants originated prior to the Eocene-Oligocene transition,but the expansion of C4 grasses had not happened until the Middle to Late Miocene. What caused the origin and expansion of C4 plants is important in understanding the ecosystem evolution. The current method for estimating C4 contribution is mainly based on the differences in C3/C4 plant carbon isotopes and their structures. The commonly used samples include (paleo-) soil organic matters,pedogenic carbonates,terrestrial herbivore tissues,biomarkers,pollen and phytolith. The application of isotopic difference in these different samples has played an important role in the reconstruction of the relative biomass of C4 plants in modern ecosystems and geological records. This article summarizes the mainstream views related to the driving forces that triggered the origin and expansion of C4 plants,and briefly introduces the basic principles of various materials archiving the biomass of C4 plants evolution history. Finally,taking the Dahonggou section in the Cenozoic Qaidam Basin as an example,the methods and shortcomings of the reconstruction of C4 plant content in lacustrine sediments are discussed in detail based on the long-chain n-alkanes and carbon isotope analysis of Cenozoic terrestrial higher plants. The δ13Calk values of long-chain alkanes vary from~-30‰ to~-26‰,and the δ13Calk values are positive. We believe that the double superposition effect of drought and C4 plant expansion leads to the positive excursions of δ13Calk values. The expansion of C4 vegetation in the Cenozoic Qaidam Basin may be controlled by dry and wet conditions and climate change. But this hypothesis needs to be tested by carbon isotope analysis from single pollen grains. |
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| Keywords: | C4 plants carbon isotopes (fossil) soil pedogenic carbonate tooth enamel phytolith N-alkanes carbon isotopes of the single pollen grain |
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