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Elastic Thickness of Oceanic Lithosphere: Tasmantid Seamounts. Tasman Sea (NERC Grant NE/L002507/1)

Elastic thickness data for Tasmantid Seamounts determined from gravity modelling. Published paper, Richards, Fred & Kalnins, Lara & Watts, A. & Cohen, Benjamin & Beaman, Robin....

3D viscosity model inferred from GLAD-M25

A model of mantle viscosity inferred from the seismic model GLAD-M25 using a method described within Lloyd et al. (2024). Model stored in NETCDF4 format with the following dimensions: depth(201),...

Cretaceous to Recent Uplift Measurements from Marine Fossil Assemblages

Cretaceous to Recent marine assemblages (total of 24,372) used to measure uplift, interpreted paleo-water depths and measured uplift. This inventory contains information about age, location,...

Carbon Isotopic Signatures of Microbial Lipids in Geothermal Deposits: Elucidating Thermophilic Ecology (NERC Grant NE/K006169/1)

Carbon Isotopic Signatures of Microbial Lipids in Geothermal Deposits: Elucidating Thermophilic Ecology. Lipid biomarkers were extracted and fractionated using standard methods. They were analysed...

A global Ediacaran-Cambrian Age Model of 130 geological successions, with radiometric ages (zircon U-Pb CA-ID-TIMS), carbon (δ13Ccarb) and strontium (87Sr/86Sr) isotope data (NERC Grant NE/T008458/1)

We present new age models for the Ediacaran-Cambrian which lacks a robust global temporal framework. This interval marks the radiation of animals, but there are major uncertainties in the...

The Geochemistry of Fossil Pigment Preservation (NERC grant NE/J023426/1)

These data represent a massive synchrotron based programme to study ancient life. Not all of these data have been processed yet, nor have we published all of the results that we intend to. These...

Geochemical results from upper Ediacaran organic-rich shales / mudstones, Yangtze Craton, South China

These data comprise geochemical results from upper Ediacaran organic-rich shales / mudstones from the Yangtze Craton (South China) from the Doushantuo Formation (member IV) and overlying lower...