20 Years of Speleothem Paleoluminescence Records of Environmental Changes: An Overview

TL;DR

This paper reviews 20 years of research on speleothem paleoluminescence, highlighting its high-resolution potential for reconstructing past environmental and climatic changes, supported by international collaborative efforts.

Contribution

It provides a comprehensive overview of advancements, potential, and limitations of speleothem luminescence records in environmental and paleoclimatic studies over two decades.

Findings

Speleothems offer extremely high-resolution climate records.

They can serve as natural climatic stations with annual resolution.

The field has progressed significantly through international collaboration.

Abstract

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.