| 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-115691 | DA17-NG-ST03-039G | 3.08 | 3.13 | None | Mixed benthic foraminifera | Carbonate hydrolysis | None | None | 10480.0 | 70.0 |
| 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) | 10785.0 | 11066.0 to 10533.0 | 10939.0 to 10640.0 |
| Intcal20 | default - Terrestrial 0.0 | IOSACal (v.0.6.0) | 12463.0 | 12679.0 to 12418.0 | 12621.0 to 12449.0 |
| Marine20 | default - Southern Ocean 1141.0 | IOSACal (v.0.6.0) | 9958.0 | 10483.0 to 9470.0 | 10208.0 to 9683.0 |
| Marine20 | default - S. Baffin Island (Bay ?) 150.0 | IOSACal (v.0.6.0) | 11330.0 | 11671.0 to 11663.0 | 11468.0 to 11177.0 |
| Marine20 | default - N. Baffin Island (Bay?) 220.0 | IOSACal (v.0.6.0) | 11229.0 | 11519.0 to 10998.0 | 11333.0 to 11111.0 |
| 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 |