Loughborough Research Repository + GRANTS Data + UP Research Data Repository2026 · Crystal structure
Datasets generated for O'Mara et al. (2026), Fire biomarkers in marine sediments record terrestrial fire activity. <i>AGU Advances</i><p dir="ltr">Dataset of organic fire proxy measurements from a transect of marine sediment core tops from the Iberian through Western African margins (40°N-34°S). Measurements include concentrations and <sup>230</sup>Th<sub>XS</sub>-normalized mass accumulation rates of a suite of polycyclic aromatic hydrocarbons (PAHs) and anhydrosugars. Core samples were provided by the Lamont-Doherty Core Repos
ZivaHub + HKU DataHub + figshare + Loughborough Research Repository + UP Research Data Repository2025 · Astronomical catalogue
<b>Evaluating the Behavior of </b><sup><strong>230</strong></sup><b>Th and </b><sup><strong>3</strong></sup><b>He Constant-Flux Proxies Across a Carbonate Preservation Gradient in the Cocos Ridge</b> DataSet<p dir="ltr">This dataset contains all the data for paper "Evaluating the Behavior of <sup>230</sup>Th and <sup>3</sup>He Constant-Flux Proxies Across a Carbonate Preservation Gradient in the Cocos Ridge". This includes <sup>14</sup>C dates and constructed age model, thorium isotope measurements, all replicate helium isotope measurements and averages and reproducibility, and focusing factors for a
RADAR + RADAR4Memory2025 · dataset
The influence of albedo on Mesoarchaean climate - global tas temperatureClimate change in the Mesoarchaean potentially played a pivotal role in facilitating gold mobilisation and deposition, ultimately contributing to the formation of the Witwatersrand gold province in the Kaapvaal Craton (South Africa) – the world’s largest known gold province. Almost all of the gold there occurs in the 2.90 – 2.79 Ga Central Rand Group, whereas the underlying 2.95 - 2.91 Ga West Ran
RADAR + RADAR4Memory2025 · dataset
The influence of land distribution and areal extent on Mesoarchaean climate - global tas temperaturesClimate change in the Mesoarchaean potentially played a pivotal role in facilitating gold mobilisation and deposition, ultimately contributing to the formation of the Witwatersrand gold province in the Kaapvaal Craton (South Africa) – the world’s largest known gold province. Almost all of the gold there occurs in the 2.90 – 2.79 Ga Central Rand Group, whereas the underlying 2.95 - 2.91 Ga West Ran