Huang Chunju, Ogg James G, Kemp David B
State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China.
Hubei Key Laboratory of Critical Zone Evolution, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China.
Palaeogeogr Palaeoclimatol Palaeoecol. 2020 Dec 15;560:110017. doi: 10.1016/j.palaeo.2020.110017. Epub 2020 Sep 11.
A high-precision geologic time scale is the essential key for understanding the Earth's evolutionary history and geologic processes. Astronomical tuning of orbitally forced stratigraphic records to construct high-resolution Astronomical Time Scales (ATS) has led to a progressive refinement of the geologic time scale over the past two decades. In turn, these studies provide new insights regarding the durations and rates of major Earth events, evolutionary processes, and climate changes, all of which provide a scientific basis for contextualizing and predicting future global change trends. South China hosts some of the best-exposed and well-dated Neoproterozoic through Mesozoic stratigraphic sections in the world; many of which are suitable for cyclostratigraphy and calibrating the geologic time scale. In North China, several Cenozoic oil-bearing basins have deep boreholes with continuous sampling and/or well logging that enable derivation of astronomically tuned time scales for an improved understanding of basin evolution and hydrocarbon generation. This Special Issue focuses on case studies of astrochronology and applied cyclostratigraphy research using reference sections within China. In this introductory overview, we: (1) summarize all existing astrochronology studies of the Neoproterozoic through Cenozoic sections within China that have been used to enhance the international geologic time scale, (2) examine briefly the astronomically forced paleoclimate information recorded in various depositional systems and the modern techniques employed to analyze the periodicity of these signals encoded within the sedimentary record, and (3) summarize the 20 contributions to this Special Issue of on 'Cyclostratigraphy and Astrochronology: Case studies from China'.
高精度地质年代表是理解地球演化历史和地质过程的关键要素。通过对轨道强迫地层记录进行天文调谐以构建高分辨率天文年代表(ATS),在过去二十年中使得地质年代表不断完善。反过来,这些研究为重大地球事件的持续时间和速率、演化过程以及气候变化提供了新的见解,所有这些都为将未来全球变化趋势置于背景中并进行预测提供了科学依据。华南拥有世界上一些出露最好且年代测定良好的新元古代至中生代地层剖面;其中许多适合进行旋回地层学研究和校准地质年代表。在华北,几个新生代含油盆地有深钻孔,可进行连续采样和/或测井,从而能够推导天文调谐年代表,以更好地理解盆地演化和油气生成。本期特刊聚焦于利用中国境内参考剖面进行天文年代学和应用旋回地层学研究的案例。在本引言综述中,我们:(1)总结中国境内用于完善国际地质年代表的新元古代至新生代剖面的所有现有天文年代学研究,(2)简要审视各种沉积体系中记录的天文强迫古气候信息以及用于分析沉积记录中编码的这些信号周期性的现代技术,(3)总结本期关于“旋回地层学与天文年代学:来自中国的案例研究”特刊的20篇投稿。