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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... -
Table 2. Element composition of the Yangla granodiorite
This dataset has no description
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Table 3. Macrofossils of invertebrate animals
r: rare, c: common, -: absent -
Oxygen isotope values from biogenic apatite (conodont elements and fish teeth...
Recovery from the end-Permian mass extinction is frequently described as delayed, with complex ecological communities typically not found in the fossil record until the Middle... -
Tab. 1+2: C14-dates cf the older and younger emergence periods
In the neighbourhood of Oobloyah Bay various phenomena ean be eneountered whieh point to a ularge-seale uplift of shorelines, i.e. to an emergence of 200 m. Delta terraces,... -
Table D.14: Microprobe analyses of garnets from sample 2119
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.18: Microprobe analysis of garnets from samples no. 2168 and 2181
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.17: Microprobe analysis of garnets from sample no. 1563
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.15+16: Microprobe analysis of garnets from sample no. 1562
Number of ions on the basis of 24 O; oxides given in weight percentage -
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... -
U-Pb age analyses on zircon grains from Mount Lawson Formation bentonites (El...
LA-ICP-MS analyses on zircon grains from Mount Lawson Formation bentonites (Ellesmere Island). Analyses listed from lowest to highest 206Pb/238U age for <1000 Ma and lowest... -
U-Pb age analyses on zircon grains from Basilika Formation bentonites (Bjørnd...
LA-ICP-MS analyses on zircon grains from Basilika Formation bentonites (Bjørndalen area). Analyses listed from lowest to highest 206Pb/238U age for <1000 Ma and lowest to... -
Major and trace element composition of whole-rock samples from the Basilika F...
This dataset has no description
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Sm-Nd isotope data of whole-rock bentonite samples from Svalbard (including C...
Initial EpsilonNd (EpsilonNd(t)) calculated with 60 Ma for Basilika Fm. bentonites and Lawson-ash 1 and 54 Ma for Lawson ash 2. -
Sm-Nd isotope data of bentonite samples (<2 µm fractions) from Svalbard and E...
Initial EpsilonNd (EpsilonNd(t)) calculated with 60 Ma for Basilika Formation bentonites and Lawson-ash 1 and 54 Ma for Lawson ash 2. -
Chemical composition of Basilika Formation (Bjørndalen area) and Mount Lawson...
This dataset has no description
