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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... -
Table 2. Element composition of the Yangla granodiorite
This dataset has no description
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(Table 3) Diatom deposits in the Kurisches Haff, Baltic Sea
This dataset has no description
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(Table 2) Diatom deposits in the Frische Nehrung, Baltic Sea
This dataset has no description
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(Table 1) Diatom deposits in the Frische Haff, Baltic Sea
This dataset has no description
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Table 3. Macrofossils of invertebrate animals
r: rare, c: common, -: absent -
(Fig. 5) Stratigraphic distribution of middle Paleogene calcareous nannofossi...
Point distance is the sample level (m). Species abundance: A = abundant (>10 %), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = not present -
(Fig. 4) Stratigraphic distribution of lower Paleogene calcareous nannofossil...
Point distance is the sample level (m). Species abundance: A = abundant (>10 %), C = common (1-10 %), F = few (0.1-1 %), R = rare (<0.1 %), - = not present -
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
