Weldeab, Syee; Emeis, Kay-Christian; Hemleben, Christoph; Vennemann, Torsten W; Schulz, Hartmut (2002): (Table 1) Stable oxygen isotope ratios of Globigerinoides ruber of sediment core M40/4_KL51 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.735756, In supplement to: Weldeab, S et al. (2002): Sr and Nd isotope composition of Late Pleistocene sapropels and nonsapropelic sediments from the Eastern Mediterranean Sea: implications for detrital influx and climatic conditions of the source areas. Geochimica et Cosmochimica Acta, 66(20), 3585-3598, https://doi.org/10.1016/S0016-7037(02)00954-7
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Coverage:
Latitude: 34.808300 * Longitude: 27.287700
Date/Time Start: 1998-01-23T00:00:00 * Date/Time End: 1998-01-23T00:00:00
Minimum DEPTH, sediment/rock: 4.60 m * Maximum DEPTH, sediment/rock: 5.84 m
Event(s):
M40/4_KL51 (67) * Latitude: 34.808300 * Longitude: 27.287700 * Date/Time: 1998-01-23T00:00:00 * Elevation: -2157.0 m * Recovery: 7 m * Location: E of Crete * Campaign: M40/4 * Basis: Meteor (1986) * Method/Device: Piston corer Meischner large (KL_Mg)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Globigerinoides ruber white, δ18O | G. ruber w δ18O | ‰ PDB | Weldeab, Syee | Mass spectrometer Finnigan MAT 251 | size fraction >250 ¬µm |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
31 data points
Data
1 Depth sed [m] | 2 G. ruber w δ18O [‰ PDB] |
---|---|
4.60 | 3.72 |
4.70 | 3.74 |
4.80 | 2.98 |
4.90 | 2.70 |
4.98 | 1.95 |
5.08 | 2.41 |
5.12 | 2.34 |
5.14 | 2.06 |
5.16 | 3.40 |
5.18 | 3.46 |
5.20 | 3.61 |
5.22 | 3.46 |
5.24 | 3.25 |
5.26 | 2.95 |
5.28 | 2.67 |
5.30 | 2.68 |
5.32 | 2.49 |
5.40 | 1.30 |
5.44 | 0.65 |
5.46 | 0.60 |
5.51 | 1.07 |
5.58 | 0.81 |
5.62 | 1.04 |
5.64 | 0.90 |
5.66 | 0.72 |
5.72 | 0.50 |
5.74 | -0.10 |
5.78 | 2.11 |
5.80 | 2.22 |
5.82 | 2.14 |
5.84 | 2.27 |