| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|
| OS-96479 | Kul-10DB-G-A1-B1-A2-composite | 0.335 | 0.345 | None | bulk sediment | Bulk Combustion AIOM | None | None | 335.0 | 40.0 | A composite 3.5 m record was compiled using a gravity core and 3 percussion cores that we are making into a single core entry |
| 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) |
|---|---|---|---|---|---|
| No calibration results available. | |||||
| Title | Author(s) | Publication | DOI | View cores |
|---|---|---|---|---|
| Glacier response to North Atlantic climate variability during the Holocene | Balascio, Nicholas L and D'Andrea, William Joseph and Bradley, Raymond S | Climate of the Past, 2015 | https://doi.org/10.5194/cp-11-1587-2015 |
|
No associated documents.
No photos found.
No photos found.
| Core name | Kul-10DB-G-A1-B1-A2-composite |
| Top depth (m) | 0.335 |
| Bottom depth (m) | 0.345 |
| Lithology | laminated sequence with frequent sandy layers. |
| Facies interpretation | glaciers grew large enough to contribute minerogenic material to the lake and retreated |
| Total organic carbon (%) | None |
| Lake name | KULUSUK LAKE |
| Preparation lab | |
| Accelerator mass spectrometer lab |