Paleo-peatlands as organic carbon pools in geological history
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摘要
Peatlands, as one of the important ecosystems, have the ability of long-term carbon sequestration, and are an extremely important carbon pool, which play a vital role in the global carbon cycle. Paleo-peatlands are the main storage for terrestrial carbon, and they are also important records of paleoclimate. Net primary productivity (NPP) of the paleo-peatland refers to the fixed carbon of peatland in the primary production process, and studying the NPP in paleo-peatlands is of great significance for understanding the generation, development, and evolution of paleo-peatlands.
Geologists read the stratigraphic cycles using paleoclimate proxy records and link the recognized sedimentary oscillations to the Milankovitch cycles. Information recorded by the geophysical logs can be an ideal paleoclimate proxy which has been commonly used in the study of cyclostratigraphy. The logging response of gamma-ray, density, and resistivity can reflect the variation in ash yield and the V/I (vitrinite to inertinite) ratio in a coal seam. Spectral analyses of geophysical data from thick coal seams can help identify the significant signals of Milankovitch period parameters, and then the period of coal deposition can be calculated. Further considering the carbon loss during coalification, the long-term average carbon accumulation rate and net primary productivity (NPP) of paleo-peatlands in coal seam can be estimated.
The source of carbon in vegetation including paleo-peatlands is atmospheric CO2, fixed through photosynthesis. Therefore, the different atmospheric CO2 levels in different geological ages should result in different NPP values of paleo-peatlands. Several case studies for the Late Permian, Middle Jurassic, Early Cretaceous and Holocene showed that the NPPs of paleo-peatlands are mainly controlled by the atmospheric CO2 contents. The higher NPP values are associated with the higher atmospheric CO2 contents. Therefore, it can be suggested that NPP values could be a possible proxy of global atmospheric CO2 during geological periods.
 
关键词
paleo-peatlands,carbon pool,Milankovitch cycle,carbon accumulation rate,net primary productivity (NPP)
报告人
Longyi Shao
Professor China University of Mining and Technology (Beijing)

稿件作者
Longyi Shao China University of Mining and Technology (Beijing)
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重要日期
  • 会议日期

    06月10日

    2025

    06月13日

    2025

  • 04月15日 2025

    初稿截稿日期

主办单位
National Natural Science Foundation of China
Geobiology Society
National Committee of Stratigraphy of China
Ministry of Science and Technology
Geological Society of China
Paleontological Society of China
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (CAS)
Institute of Vertebrate Paleontology and Paleoanthropology, CAS
International Commission on Stratigraphy
International Paleontological Association
承办单位
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (CUG, Wuhan)
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