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Hydrogen isotope data from speleothem WB-21-5-A used for the paleotemperature...
The dataset includes speleothem fluid inlcusion hydrogen isotopes used to reconstruct climate in southeastern Alaska during the past ~3,500 years. Speleothem WB-21-5-A was... -
MIS 5 speleothem growth phases in the central Eastern Desert of Egypt
This data set presents Th/U ages from a speleothem deposit in the Eastern Desert of Egypt at Saqia Cave and mean values of δ13C and δ18O for the respective speleothem growth... -
Thorium / uranium dating of stalagmite PR-LA-1 (Cueva Larga, Puerto Rico)
Activity ratios were corrected for initial Th assuming an detrital weight ratio 232Th/238U = 0.13 ± 0.04 (corresponding to an activity ratio of the detritus in secular... -
(Supplementary Table 1) 230Th/U results for stalagmite Cuba Grande (CG) from ...
We present 22 U-series ages for a stalagmite from north-western Cuba based on multi-collector inductively coupled plasma mass spectrometry (MC-ICPMS) and thermal ionisation mass... -
Measured SC02 U/Th isotope activity ratios, calculated ages and monte-carlo d...
U-Th ages were calculated using the initial detrital 230Th/232Th value of 111 ± 41 ppm, which was previously calculated for SC02 based on two isochrons measured in separate... -
δ18O and δ13C at distance-from-top of stalagmite and Oxcal deposition model i...
Here are presented Mulu, Borneo (4°6'N, 114°53'E) Secret Cave stalagmite SC02 d18O and d13C values over Termination 1, published in Buckingham et al. (2022). This study reports... -
⁸⁷Sr/⁸⁶Sr stalagmite records from Northeastern Brazil
This dataset has no description
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Age model and d13C of TRA 7 speleothem
This dataset has no description
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U/Th results of TRA 7 speleothem
U decay constants: λ238 = 1.55125x10-10 (Jaffey et al., 1971) and λ234 = 2.82206x10-6 (Cheng et al., 2013). Th decay constant: λ230 = 9.1705x10-6 (Cheng et al., 2013). d234U =... -
Hendy test of stable carbon and oxygen isotope ratios of Speleothem M37-1-16A
This dataset has no description
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Percentiles of global mean sea level during Pliocene warmth
GMSL is the ice-equivalent value; i.e. thermal expansion has been corrected for. -
(Table 1) Growth rates of stalagmites of the Okshola cave
Minimum and maximum gives the subsamples along the growth axis, whereas the distance is the midpoint of two subsamples. -
(Table 1) TIMS U-Th results from stalagmites and stalactites of the Okshola cave
Distance gives the central position of TIMS subsamples along the groth axis of stalagmites. For stalactites from Fata Morgana minimum and maximum refere to cm interval from the... -
Trace element and stable isotope data of subaqueous grown speleothems (Hells ...
This dataset provides geochemical data (trace elements and stable isotopes) of subaqueous grown speleothems (Hells Bells) from the north-eastern Yucatán Peninsula. These... -
Paleovegetation seesaw in Brazil since the Late Pleistocene: A multiproxy stu...
Paleovegetation studies in Brazil have been mostly based on pollen analysis and geochemical proxies in lacustrine and soil records. These records, however, are sparsely located... -
Fluid inclusion oxygen and hydrogen stable isotopes in a speleothem from Susa...
Fluid inclusion isotopes for a speleothem from Libya Supplement to: Rogerson, Mike; Dublyansky, Yuri; Hoffmann, Dirk L; Luetscher, Marc; Spötl, Christoph; Töchterle, Paul... -
(Table 1) Age determination of stalagmites of the Marcello Arévalo Cave in Chile
Stalagmites are important palaeo-climatic archives since their chemical and isotopic signatures have the potential to record high-resolution changes in temperature and... -
Trace element concent of Stagamite MF-3 from Schafsloch Cave
This dataset has no description
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Chronology and stable isotopes of Stagamite MF-3 from Schafsloch Cave
This dataset has no description
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Age-depth model with δ13Cca and δ18Oca isotope profiles for stalagmite Y99 gr...
The Arabian Peninsula was one key area for H. sapiens dispersals out of Africa. Current dispersal models advocate that dispersals via the "southern route" into Arabia occurred...
