East Asian Paleoenvironmental Science Database

Stalagmite

High-resolution geological and biological records >> Stalagmite

Stalagmite is one kind of secondary carbonates formed in limestone caves (speleothem). After cave water droplets containing Ca2+ and HCO3- drip onto floor, carbonate in the water might become supersaturated due to CO2 degassing under certain conditions, resulting in the formation of stalagmite in a process year after year. Stalagmite is one of important geological archives for paleoclimate research. The advantages include wide spatial distribution, suitable for U-Th and U-Pb dating, enriched in climate proxies, continuity, long time span, comparability and lower sampling cost etc. This database contain all published records which can be applied by all related researchers.

The Holocene stalagmite trace element and Sr isotope records from central C... 29-Sep-2024
Speleothem records from southwest China during the last deglaciation 19-Sep-2024
Stalagmite F11 and F2 U-series Dates and F11 proxy dataset of Talisman cave... 25-Jun-2024
Carbon and oxygen isotope data set of stalagmite XRY24 in XRY Cave (1951-20... 17-Jun-2024
Seasonal to decadal variations of precipitation oxygen isotopes in northern... 25-Dec-2023
Holocene Speleothem 14C ages from Longfeng, Jiuxian and Shennong Cave 27-Oct-2022
Stalagmite data sets of Kesang cave in Xinjiang 10-May-2021
Stalagmite data sets of Magou cave in Henan 10-May-2021
Holocene stalagmite δ18O and δ13C records from Wuya Cave, south margin of... 21-Oct-2020
Rainfall variations in central Indo-Pacific dataset (over the past 2700 y) 18-Nov-2019
Suozi Cave, China speleothem stable isotope dataset (during MIS 5d-c) 05-Mar-2019

Data number：11
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