Dataset - B2FIND

Stable oxygen and carbon isotope and trace element record from Cloşani Cave (...

This dataset covers stable isotope and trace element records covering the last 20ka from two speleothems (C09-2, C09-1) from Cloşani Cave, Romania. This datasets extends the...

Uranium and Thorium in stalagmite M1-5 from Moomi Cave, Socotra Island

In this study, the dead carbon fraction (DCF) variations in stalagmite M1-5 from Socotra Island in the western Arabian Sea were investigated through a new set of high-precision...

Radiocarbon dating of stalagmite M1-5 from Moomi Cave, Socotra Island

In this study, the dead carbon fraction (DCF) variations in stalagmite M1-5 from Socotra Island in the western Arabian Sea were investigated through a new set of high-precision...

U-series and radiocarbon dating results of stalagmite M1-5 from Moomi Cave, S...

In this study, the dead carbon fraction (DCF) variations in stalagmite M1-5 from Socotra Island in the western Arabian Sea were investigated through a new set of high-precision...

Borneo stalagmite SC02 temperature reconstructions over Termination I by the ...

This dataset presents cave temperatures over the last glacial termination from stalagmite SC02 from Secret Cave in Mulu, Northern Borneo (4.063°N, 114.833°E). The temperatures...

Speleothem trace element and stable isotope data and reconstructed late Holoc...

We present the first high-resolution trace element (Mg/Ca, Sr/Ca, Ba/Ca) record from a stalagmite in southwestern Romania covering the last 3.6 ka, which provides the potential...

Speleothems and palaeoclimate variability in western Iberia during the Last G...

Large-scale and abrupt climate oscillations in the Northern Hemisphere, such as Heinrich Stadials and Dansgaard-Oeschger events, during the last glacial period have long been...

A speleothem record from Portugal reveals phases of increased winter precipit...

Two speleothems collected from the Galeria das Lâminas (GdL), in the greater Almonda Karst System (Torres Novas, Portugal). The chronology is substantiated by U-Th dates....

Last Millennium U/Th ages of MV30 stalagmite record from Mata Virgem cave

Presented here are U-Th ages derived from the MV30 stalagmite. This sample was collected from Mata Virgem cave (11°37′27.07′′S, 47°29′19.04′′W) in the eastern region of the...

Last Millennium U/Th ages of MV1 stalagmite record from Mata Virgem cave

Presented here are U-Th ages derived from the MV1 stalagmite. This sample was collected from Mata Virgem cave (11°37′27.07′′S, 47°29′19.04′′W) in the eastern region of the...

Last Millennium δ¹⁸O and δ¹³C of MV30 stalagmite record from Mata Virgem cave

Presented here are stable isotopes (δ¹⁸O, δ¹³C) derived from the MV30 stalagmite. This sample was collected from Mata Virgem cave (11°37′27.07′′S, 47°29′19.04′′W) in the eastern...

Last Millennium δ¹⁸O and δ¹³C of MV1 stalagmite record from Mata Virgem cave

Presented here are stable isotopes (δ¹⁸O, δ¹³C) derived from the MV1 stalagmite. This sample was collected from Mata Virgem cave (11°37′27.07′′S, 47°29′19.04′′W) in the eastern...

Last Millennium δ¹⁸O, δ¹³C, and U/Th ages of MV1 and MV30 stalagmite records ...

The South American Summer Monsoon (SASM) is the main driver of regional hydroclimate variability across tropical and subtropical South America. It is best recorded on...

speleothem calcite trace element data

Trace element analyses of stalagmite calcite. Samples from Scladina Cave, Belgium. The dataset is to support the Vonhof et al., 2024 publication in "Climate of the Past"

Uranium series isotopes and dating of stalagmite C09-2 from Closani Cave

Ages were calculated using the half-lives of Cheng et al. (2000). Correction for detrital contamination assumes a 232Th/238U weight ratio of 3.8 ± 1.9 and 230Th, 234U and 238U...