Core 11PRM-2 (Sub-basin in the North Western corner of the lake)
Associated publications
| Title | Author(s) | Publication | DOI | View cores |
|---|---|---|---|---|
| The deglaciation and neoglaciation of Upernavik Isstr{\o}m, Greenland | Briner, Jason P and H{\aa}kansson, Lena and Bennike, Ole | Quaternary Research, 2013 | (no DOI) |
|
Core information
| Core name | Region | Collection date | IGSN ID | Core type | Latitude (DD) | Longitude (DD) | Water depth (m) |
Core length (m) |
Comments |
|---|---|---|---|---|---|---|---|---|---|
| 11PRM-2 | Arctic, Greenland - Avannaata Municipality, terrestrial | None | None | 70.03422 | -54.78827 | 7.3 | 1.05 |
Lake information
| Lake name | Lake description | Catchment area (m2) | Open vs closed | Mictic state |
|---|---|---|---|---|
| UPERNAVIK-PRM | Proglacial threshold lake | True | None |
Samples in this core
| Sample ID | Core depth (m) |
Lithology | Facies interpretation | Carbon type | Sample preparation type | Age (14C yr ± 1σ) | Calibrated age, median probability (cal. yr BP) | Calibrated age, 2σ range (cal. yr BP) | Comments |
|---|---|---|---|---|---|---|---|---|---|
| OS-96910 | 0.035 - 0.038 | Mixture of Mineral- and organic-rich sediment | The ice margin was no more extensive than its current (2008-2012) position until the latest holocene | Sediment–organic carbon | Bulk Combustion | 1110.0 ± 35.0 | Calibrated age for default reservoir correction not available | Calibrated age for default reservoir correction not available | None |
| OS-97071 | 0.062 - 0.065 | Organic-rich Sediment | The ice margin was no more extensive than its current (2008-2012) position until the latest holocene | Sediment–organic carbon | Bulk Combustion | 7450.0 ± 23.0 | 6562.0 | 7004.0-6160.0 | None |
| OS-92415 | 1.013 - 1.016 | Organic-rich Sediment | The ice margin was no more extensive than its current (2008-2012) position until the latest holocene | Scorpidium scorpioides | Bulk Combustion | 8360.0 ± 40.0 | 7514.0 | 7906.0-7153.0 | None |
Associated documents
No associated documents.