Nürnberg, Dirk; Gehre, Nadine; Fessler, Sebastian; Mirzaloo, Maryam (2025): Stable carbon and oxygen isotopes and element ratios of planktic foraminifer Globigerina bulloides from sediment core POS457_889-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.975216
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Published: 2025-02-17 • DOI registered: 2025-03-18
Abstract:
R/V POSEIDON cruise POS457 aimed at sediment coring on the Iceland-Faroe Ridge, the shelf and slope areas south of Iceland, and on Reykjanes Ridge in order to reveal paleoceanographic and paleoclimatic information. Gravity corer 889-1 was recovered from southeast of Reykjanes Ridge close to Iceland (N Atlantic, 63°03.04'N 23°23.19'W, 923.0 m water depth). We present radiocarbon datings and high-resolution XRF-scanner element compositions of bulk sediments. In addition, we provide benthic and planktic stable oxygen and carbon isotopes, as well as planktic foraminiferal element ratios.
Related to:
Mirzaloo, Maryam; Nürnberg, Dirk; Kienast, Markus; van der Lubbe, H J L (2019): Synchronous Changes in Sediment Transport and Provenance at the Iceland-Faroe Ridge Linked to Millennial Climate Variability From 55 to 6 ka BP. Geochemistry, Geophysics, Geosystems, 20(8), 4184-4201, https://doi.org/10.1029/2019GC008298
Nürnberg, Dirk; Ziegler, Martin; Karas, Cyrus; Tiedemann, Ralf; Schmidt, Matthew W (2008): Interacting Loop Current variability and Mississippi River discharge over the past 400 kyr. Earth and Planetary Science Letters, 272(1-2), 278-289, https://doi.org/10.1016/j.epsl.2008.04.051
Werner, Reinhard; Nürnberg, Dirk (2014): RV POSEIDON Fahrtbericht / Cruise Report P457: Iceland Hazards ; Volcanic risks from Iceland and climate Change: the late Quaternary to anthropogene development, Reykjavík / Iceland – Galway / Ireland, 7.-22. August 2013. GEOMAR Report (N. Ser.), 14, 88 pp, https://doi.org/10.3289/GEOMAR_REP_NS_14_2014
Coverage:
Latitude: 63.050500 * Longitude: -23.386500
Date/Time Start: 2013-08-11T12:17:00 * Date/Time End: 2013-08-11T12:17:00
Minimum DEPTH, sediment/rock: 0.005 m * Maximum DEPTH, sediment/rock: 3.905 m
Event(s):
POS457_889-1 * Latitude: 63.050500 * Longitude: -23.386500 * Date/Time: 2013-08-11T12:17:00 * Elevation: -923.4 m * IGSN: https://doi.org/10.58031/KIEL0179GE8X101 * Location: Reykjanes Ridge * Campaign: POS457 * Basis: Poseidon * Method/Device: Gravity corer (GC) * Comment: zu Wasser
Comment:
Values marked with # are uncertain.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Nürnberg, Dirk | Geocode | |
| 2 | Globigerina bulloides, δ13C | G. bulloides δ13C | ‰ PDB | Nürnberg, Dirk | Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV | VPDB; Method: Mirzaloo et al., 2019 |
| 3 | Globigerina bulloides, δ18O | G. bulloides δ18O | ‰ PDB | Nürnberg, Dirk | Mass spectrometer, Thermo Fisher Scientific, MAT 253; coupled with Carbonate preparation device, Thermo Fisher Scientific, KIEL IV | VPDB; Method: Mirzaloo et al., 2019 |
| 4 | Globigerina bulloides, Magnesium/Calcium ratio | G. bulloides Mg/Ca | mmol/mol | Nürnberg, Dirk | Method: Nürnberg et al., 2008 | |
| 5 | Globigerina bulloides, Strontium/Calcium ratio | G. bulloides Sr/Ca | mmol/mol | Nürnberg, Dirk | Method: Nürnberg et al., 2008 | |
| 6 | Globigerina bulloides, Aluminium/Calcium ratio | G. bulloides Al/Ca | mmol/mol | Nürnberg, Dirk | Method: Nürnberg et al., 2008 | |
| 7 | Globigerina bulloides, Iron/Calcium ratio | G. bulloides Fe/Ca | mmol/mol | Nürnberg, Dirk | Method: Nürnberg et al., 2008 | |
| 8 | Globigerina bulloides, Manganese/Calcium ratio | G. bulloides Mn/Ca | mmol/mol | Nürnberg, Dirk | Method: Nürnberg et al., 2008 |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
189 data points
Data
| 1 Depth sed [m] | 2 G. bulloides δ13C [‰ PDB] | 3 G. bulloides δ18O [‰ PDB] | 4 G. bulloides Mg/Ca [mmol/mol] | 5 G. bulloides Sr/Ca [mmol/mol] | 6 G. bulloides Al/Ca [mmol/mol] | 7 G. bulloides Fe/Ca [mmol/mol] | 8 G. bulloides Mn/Ca [mmol/mol] |
|---|---|---|---|---|---|---|---|
| 0.005 | -0.378 | 1.624 | 2.374 | 1.362 | 0.444 | 0.417 | 0.021 |
| 0.105 | -0.125 | 2.034 | 2.325 | 1.344 | 0.421 | 0.370 | 0.051 |
| 0.205 | -0.212 | 1.912 | 2.380 | 1.372 | 0.262 | 0.347 | 0.050 |
| 0.305 | -0.571 | 1.669 | 2.932 | 1.365 | 1.498 | 1.923 | 0.081 |
| 0.405 | -0.421 | 1.640 | 2.207 | 1.372 | 0.068 | 0.172 | 0.069 |
| 0.505 | -0.187 | 1.488 | 2.420 | 1.366 | 0.161 | 0.370 | 0.057 |
| 0.605 | -0.242 | 1.751 | 2.586 | 1.360 | 0.513 | 0.561 | 0.053 |
| 0.605 | -0.242 | 1.751 | |||||
| 0.705 | -0.048 | 1.653 | 2.348 | 1.351 | 0.621 | 0.599 | 0.057 |
| 0.805 | -0.125 | 1.443 | 2.611 | 1.382 | 0.292 | 0.364 | 0.052 |
| 0.905 | -0.047 | 1.638 | 2.639 | 1.343 | 1.352 | 1.067 | 0.088 |
| 1.005 | -0.493 | 1.634 | 2.215 | 1.420 | 0.165 | 0.250 | 0.033 |
| 1.105 | -0.197 | 1.871 | 2.118 | 1.361 | 0.253 | 0.284 | 0.048 |
| 1.205 | -0.184 | 1.867 | 2.208 | 1.366 | 0.234 | 0.302 | 0.052 |
| 1.305 | -0.316 | 1.558 | 1.996 | 1.362 | 0.161 | 0.161 | 0.044 |
| 1.405 | -0.449 | 1.733 | 3.937 | 1.366 | #3.433 | 2.744 | 0.076 |
| 1.505 | -0.420 | 1.751 | 3.039 | 1.378 | 1.574 | 1.520 | 0.048 |
| 1.605 | -0.992 | 2.017 | 2.221 | 1.370 | 0.168 | 0.246 | 0.040 |
| 1.705 | -0.716 | 1.969 | 2.195 | 1.437 | 0.115 | 0.144 | 0.032 |
| 1.805 | -1.007 | 2.199 | 2.676 | 1.408 | 0.962 | 1.022 | 0.073 |
| 1.905 | -1.018 | 2.717 | 2.343 | 1.474 | 0.540 | 0.504 | 0.066 |
| 2.005 | -0.885 | 3.047 | 2.176 | 1.431 | 0.240 | 0.324 | 0.068 |
| 2.105 | -0.564 | 3.094 | 2.290 | 1.401 | 0.704 | 0.649 | 0.083 |
| 2.305 | -1.063 | 2.924 | 2.617 | 1.418 | 0.661 | 0.727 | 0.105 |
| 2.405 | -0.892 | 2.937 | 2.162 | 1.430 | 0.345 | 0.173 | 0.102 |
| 2.505 | -0.221 | 1.836 | |||||
| 2.605 | -0.643 | 2.874 | |||||
| 2.905 | -1.389 | 2.173 | |||||
| 3.005 | -1.393 | 2.110 | |||||
| 3.105 | -1.195 | 3.089 | 2.135 | 1.401 | 0.407 | 0.386 | 0.101 |
| 3.505 | -1.110 | 1.740 | |||||
| 3.905 | -0.716 | 2.150 |
