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Astrochronological age model (silicon) from the Contessa Road (Italy)
Ages are presented in kyr relative to the PETM onset (0 kyr). -
Astrochronological age model (calcium) from the Contessa Road (Italy)
Ages are presented in kyr relative to the PETM onset (0 kyr). -
Astrochronological age model (iron) from the Contessa Road (Italy)
Ages are presented in kyr relative to the PETM onset (0 kyr). -
Replicate X-ray fluorescence measurements from the Contessa Road (Italy)
This dataset has no description
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X-ray fluorescence measurements from Contessa Road (Italy)
This dataset has no description
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Updated ages for the McMurdo erratics and basis for age changes
LAD: last appearance datum, FAD: first appearance datum, LO: Last occurrence, LCO: Last common occurrence, FO: First occurrenceAntarctica New Zealand Sir Robin Irvine PhD... -
GDGT abundances and indices for Ross Sea sample sites
Note for AND1-1B (ANDRILL-1B): in samples with BIT values but no brGDGT values, the BIT has been taken from McKay et al. (2012).Antarctica New Zealand Sir Robin Irvine PhD... -
X-ray fluorescence data from Contessa Road (Italy), Paleocene-Eocene Thermal ...
The Paleocene-Eocene Thermal Maximum (PETM) is the most studied global warming event of a series of Paleocene-Eocene carbon cycle perturbations called hyperthermals. PETM... -
(Table S2) Elemental data raw results and internal standard errors for hardgr...
9 = bellow detection limit -
(Table S1) Laser ablation strontium isotope analysis for hardgrounds
This dataset has no description
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Appendix 1. Single-zircon Pb evaporation ages from the Djupkilsodden granitoi...
This dataset has no description
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Tab. 3: Pb-Pb analytical primary data
This dataset has no description
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U-Pb, trace element, and Hf isotope analysis for Macquarie Island detrital zi...
Oceanic zircon trace element and Hf-isotope geochemistry offers a means to assess the magmatic evolution of a dying spreading ridge and provides an independent evaluation of the... -
Table A1 LA-ICP-MS zircon U-Pb data of Laoniushan granitoids
The NWW-striking Qinling Orogen formed in the Triassic by collision between the North China and Yangtze Cratons. Triassic granitoid intrusions, mostly middle- to high-K,... -
Anisotropy of magnetic susceptibility (AMS) of small scale marble shear zone,...
This dataset has no description
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(Table 6) Carbon and oxygen isotopic compositions of carbonate material from ...
This dataset has no description
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(Table 3) K-Ar dating of trachybasalts from the Sinii Utes Depression, Southe...
This dataset has no description
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Geochemical analyses of microbial carbonates deposited during the Holocene in...
The data refer to the geochemical and isotopic characterization of microbial carbonate in the shallow platform of the South Atlantic Ocean, Espírito Santo - Brazil. Geochemical... -
δ13C and δ18O isotopic analyses of microbial carbonates deposited during the ...
The data refer to the geochemical and isotopic characterization of microbial carbonate in the shallow platform of the South Atlantic Ocean, Espírito Santo - Brazil. Carbon and... -
Age determination of microbial carbonates deposited during the Holocene in th...
The data refer to the geochemical and isotopic characterization of microbial carbonate in the shallow platform of the South Atlantic Ocean, Espírito Santo - Brazil. The...
