| Sample name | Core name | Top depth (m) | Bottom depth (m) | Total organic carbon (%) | Carbon type | Sample preparation method | Fraction modern | δ13C (‰, PDB) | Age (14C yr) | Age uncertainty (14C yr; 1σ) | Comments |
|---|---|---|---|---|---|---|---|---|---|---|---|
| ETH-115692 | DA17-NG-ST03-039G | 3.08 | 3.13 | None | Mixed planktonic foraminifera | Carbonate hydrolysis | None | None | 10190.0 | 60.0 |
| Calibration curve | Reservoir correction (14C yr) | Calibration software | Calibrated age, median probability (cal. yr BP) | Calibrated age, 95.45% probability range (2σ; cal. yr BP) | Calibrated age, 68.2% probability range (1σ; cal. yr BP) |
|---|---|---|---|---|---|
| Marine20 | default - Global Ocean 550.0 | IOSACal (v.0.6.0) | 10361.0 | 10569.0 to 10175.0 | 10461.0 to 10453.0 |
| Intcal20 | default - Terrestrial 0.0 | IOSACal (v.0.6.0) | 11850.0 | 12421.0 to 12408.0 | 11942.0 to 11749.0 |
| Marine20 | default - Southern Ocean 1141.0 | IOSACal (v.0.6.0) | 9607.0 | 10134.0 to 9125.0 | 9876.0 to 9367.0 |
| Marine20 | default - S. Baffin Island (Bay ?) 150.0 | IOSACal (v.0.6.0) | 10930.0 | 11188.0 to 10651.0 | 11081.0 to 10787.0 |
| Marine20 | default - N. Baffin Island (Bay?) 220.0 | IOSACal (v.0.6.0) | 10845.0 | 11086.0 to 10590.0 | 10989.0 to 10716.0 |
| Title | Author(s) | Publication | DOI | View cores |
|---|---|---|---|---|
| Deglacial to Mid Holocene environmental conditions on the northeastern Greenland shelf, western Fram Strait | Elnegaard Hansen, Katrine and Lorenzen, Jesper and Davies, Joanna and Wacker, Lukas and Pearce, Christof and Seidenkrantz, Marit-Solveig | Quaternary Science Reviews, 2022 | https://doi.org/10.1016/j.quascirev.2022.107704 |
|
No associated documents.
No photos found.
No photos found.
| Core name | DA17-NG-ST03-039G |
| Top depth (m) | 3.08 |
| Bottom depth (m) | 3.13 |
| Lithology | highest absolute concentrations of both benthic and planktonic foraminifer |
| Facies interpretation | same distal claciomarine conditions with the Atlantic water influence as recorded in the outer peterman Fjord from c. 7.0 cal ka BP. Cold conditions accompanied by heavy sea-ice concentrations implied by high abundance of S. horvathi at the beginning of 13.3 cal ka BP |
| Total organic carbon (%) | None |
| Preparation lab | |
| Accelerator mass spectrometer lab |