20年来洞穴沉积物的古发光记录及其环境变化
20 Years of Speleothem Paleoluminescence Records of Environmental Changes: An Overview
摘要：
本文介绍了洞穴沉积物古发光记录环境变化研究20年来的进展。研究结果表明，洞穴矿物发光研究的进展主要是由于联合国教科文组织统计研究所岩溶物理化学和水文地质学委员会的洞穴矿物发光国际计划的实施。高分辨率发光洞穴沉积物代用记录的潜力、分辨率和局限性：古温度、太阳日射、太阳亮度、冰川、海平面上升、过去降水、植物种群、古土壤、过去岩溶剥蚀、化学污染、地磁场和宇宙射线通量变化、过去宇宙成因同位素生产和超新星爆发、热液水的进展、和构造隆升。它表明，洞穴沉积物允许极高的分辨率（高于任何其他古气候陆地档案）和长时间的记录。某些洞穴沉积物可作为自然气候站，获得具有年分辨率的第四纪气候定量代用记录。
英文摘要：
This paper discusses advance of the research on Speleothem Paleoluminescence Records of Environmental Changes after it have been first introduced by the author 20 years ago. It is demonstrated that most of the progress in this field was made in result of the operation of the International Program Luminescence of Cave Minerals of the commission on Physical Chemistry and Hydrogeology of Karst of UIS of UNESCO. Potential, resolution and limitations of high resolution luminescence speleothem proxy records of Paleotemperature, Solar Insolation, Solar Luminosity, Glaciations, Sea Level advances, Past Precipitation, Plants Populations, Paleosoils, Past Karst Denudation, Chemical Pollution, Geomagnetic field and Cosmic Rays Flux variations, Cosmogenic Isotopes production and Supernova Eruptions in the Past, Advances of Hydrothermal Waters, and Tectonic Uplift are discussed. It is demonstrated that speleothems allow extremely high resolution (higher than in any other paleoclimatic terrestrial archives) and long duration of records. Some speleothems can be used as natural climatic stations for obtaining of quantitative proxy records of Quaternary climates with annual resolution.
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