Comprehensive data dump for sample OS-96454
Sample
| 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-96454 | Kul-10DB-G-A1-B1-A2-composite | 0.945 | 0.955 | None | bulk sediment | Bulk Combustion AIOM | None | None | 1290.0 | 25.0 | 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 results for Sample OS-96454
| 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) | 194.0 | 299.0 to 73.0 | 267.0 to 137.0 |
| Intcal20 | default - Terrestrial 0.0 | IOSACal (v.0.6.0) | 1226.0 | 1283.0 to 1242.0 | 1275.0 to 1246.0 |
| Marine20 | default - Southern Ocean 1141.0 | IOSACal (v.0.6.0) | 69.0 | 235.0 to 1.0 | 105.0 to 1.0 |
| Marine20 | default - S. Baffin Island (Bay ?) 150.0 | IOSACal (v.0.6.0) | 562.0 | 708.0 to 418.0 | 633.0 to 498.0 |
| Marine20 | default - N. Baffin Island (Bay?) 220.0 | IOSACal (v.0.6.0) | 508.0 | 621.0 to 410.0 | 556.0 to 449.0 |
Associated publications
| 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 |
|
Associated documents
No associated documents.
Field photographs
No photos found.
Lab photographs
No photos found.
Complete dump of sample & measurement data
Sample-related information| Core name | Kul-10DB-G-A1-B1-A2-composite |
| Top depth (m) | 0.945 |
| Bottom depth (m) | 0.955 |
| 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 |