海岸泥质风暴沉积物研究现状与展望
收稿日期: 2023-12-08
修回日期: 2024-02-16
网络出版日期: 2024-04-01
基金资助
广东省自然科学基金资助
Research Progress and Prospect of the Coastal Muddy Storm Deposit
Received date: 2023-12-08
Revised date: 2024-02-16
Online published: 2024-04-01
Supported by
the Natural Science Foundation of Guangdong Province, China
从前寒武纪至今，各年代地层中普遍存在风暴沉积物，它们记录了地史时期曾经发生的极端气象事件。古风暴沉积物研究被认为能在预测未来极端气象事件演变趋势方面提供关键的长时间尺度信息，而准确识别风暴沉积物是这项研究的重要基础。在先前的研究中，学者们主要关注相对容易识别的砂质风暴沉积物、碳酸盐（钙质）风暴沉积物、风暴砾石与巨砾以及风暴贝壳层，而对较难识别的泥质风暴沉积物缺乏深入研究。近年来，国内外研究人员在海岸泥质风暴沉积物的判识方法和指标、沉积过程以及古风暴历史重建等方面取得了不少重要进展。这对于完善对风暴沉积记录类型的认识以及进行高分辨率的古风暴活动历史重建十分重要。为此，着重回顾了近年来有关海岸泥质风暴沉积物判识方法体系的研究进展，发现综合运用元素地球化学、同位素地球化学和有机地球化学的敏感指标是准确识别泥质风暴沉积物的关键，但仍需深入探究泥质风暴沉积物地球化学判识指标与风暴沉积动力过程的响应机理，建议优先关注不同沉积环境泥质风暴沉积物的系统性对比研究、野外原位观测及室内沉积模拟，并强化跨学科交叉合作。
江凯禧 , 苏明 , 林春明 , 刘佳威 , 雷亚平 , 王策 , 陈慧 , 马文斌 . 海岸泥质风暴沉积物研究现状与展望[J]. 地球科学进展, 2024 , 39(3) : 279 -291 . DOI: 10.11867/j.issn.1001-8166.2024.024
Storm deposits ranging from the Precambrian era to the present day are found extensively in stratigraphic layers spanning almost all ages. These deposits serve as good records preserving information on paleo-extreme weather events that transpired throughout this extensive timeframe. Research on palaeostorm deposits is crucial for supplying vital long-term information for forecasting the evolutionary trends of future extreme weather events. The precise recognition of storm deposits is the pivotal foundation of this research. In previous research, the primary emphasis has been placed on easily discernible sandy storm deposits, carbonate (calcareous) storm deposits, storm pebbles, cobbles, and shell beds associated with storms because of their relative ease of identification. However, there has been a notable absence of investigations on muddy storm deposits, which presents challenges for identification. In recent years, significant progress has been made by researchers in refining the methods and indicators for identifying coastal muddy storm deposits, understanding depositional processes, and reconstructing paleostorm history. These advancements have played a crucial role in enhancing our comprehension of storm sediment classifications and in reconstructing the detailed history of paleostorm activity at high resolution. This study focuses on reviewing the recent advances in identification indices for coastal muddy storm deposits. We found that the integrated use of elemental, isotopic, and organic geochemistry serves as a sensitive indicator critical for the identification of muddy storm deposits. However, further research is required on the response mechanisms between the geochemical identification indicators of muddy storm sediments and the dynamics of storm deposition processes. It is emphasized that systematic comparative studies of muddy storm sedimentation in different sedimentary environments, field in situ observations, and laboratory simulations, as well as the strengthening of interdisciplinary collaboration, are worthy of priority as research focuses and directions for the future.
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