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LI Yuan, SUN Yuanyuan, DENG Guoshi, YUAN Feng, LIU Jun. 2022. Reconstruction of C4 plant content in Cenozoic lacustrine sediments: An example from the Dahonggou section, Qaidam Basin. Sedimentary Geology and Tethyan Geology, 42(4): 572-584. doi: 10.19826/j.cnki.1009-3850.2022.04019
Citation: LI Yuan, SUN Yuanyuan, DENG Guoshi, YUAN Feng, LIU Jun. 2022. Reconstruction of C4 plant content in Cenozoic lacustrine sediments: An example from the Dahonggou section, Qaidam Basin. Sedimentary Geology and Tethyan Geology, 42(4): 572-584. doi: 10.19826/j.cnki.1009-3850.2022.04019
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Reconstruction of C4 plant content in Cenozoic lacustrine sediments: An example from the Dahonggou section, Qaidam Basin

  • 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

More Information
  • Corresponding author: SUN Yuanyuan  
Received Date:  12 October 2021
Revised Date:  07 April 2022
    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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