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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... -
Data from: Combined effects of land use and hunting on distributions of tropi...
In our paper “Combined effects of land use and hunting on distributions of tropical mammals.” (Conservation Biology, Available from:... -
Mulu Borneo stalagmite SC02 U/Th dating and oxygen and carbon stable isotopes...
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). U-Th ages were... -
In situ Be-10, Al-26, and Ne-21 measurements of detrital river sediment in ce...
We measured the concentration of in situ Be-10 and Al-26 in quartz separated from medium (250-850 micron) detrital river sand collected from 22 watersheds in central Cuba.... -
Mg/Ca and oxygen isotope data from the Indo-Pacific
Across the middle Miocene, Earth's climate underwent a major cooling and expansion of the Antarctic ice sheet. However, the associated response and development of the tropical... -
Marine Isotope Stage 5 low-latitude data and model comparisons
This dataset includes planktic foraminifera (Globigerinoides ruber sensu-stricto) stable oxygen isotope and Mg/Ca data from IODP Expedition 353, Sites U1446 and U1448 across... -
12 year Northern Borneo cave drip water oxygen isotopic time series
We present ~twelve year-long time series of biweekly cave drip water (oxygen isotope) variations from three sites from Gunung Mulu National Park in Northern Sarawak, Borneo.... -
Annual change in precipitation across 6 regions throughout Marine Isotope Sta...
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Mg/Ca and δ¹⁸O records of Globigerinoides ruber (sensu-stricto) from IODP Sit...
This dataset has no description
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Mg/Ca and δ¹⁸O records of Globigerinoides ruber (sensu-stricto) from IODP Sit...
This dataset has no description
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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... -
Neon processing and analysis data
(1) Computed by comparison to 20Ne signal in air pipettes. 1-sigma uncertainty includes measurement uncertainty of 20Ne signal in this analysis and the reproducibility of the... -
Beryllium blank sensitivity analysis from the detrital river sediment in cent...
Beryllium blank sensitivity analysis showing comparison between using individual batch blanks and average blanks. -
Aluminium-26 and Beryllium-10 derived erosion rate from the detrital river se...
Note: * Where the 26Al/10Be ratio is significantly below 7 (see Table S7), the erosion rates are overestimes.* The CU-016 Be data are only from the duplicate sample. -
Aluminum and beryllium isotope concentrations and ratios from the detrital ri...
= We used only the DUP Be-10 measurement because we re-leached the sample and concluded the first one was not clean enough. -
Aluminum isotope measurements from the detrital river sediment in central Cuba
This dataset has no description
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Beryllium isotope measurements from the detrital river sediment in central Cuba
Isotopic analysis was conducted at PRIME Laboratory; ratios were normalized against standard 07KNSTD3110 with an assumed ratio of 2850 x 10^-15 (Nishiizumi et al., 2007). -
Blank data for aluminum measurements
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Blank data for beryllium measurements
This dataset has no description
