Associated publications

Title Author(s) Publication DOI View cores
Early Holocene history of the west Greenland Ice Sheet and the GH-8.2 event Long A.J. and Roberts D.H. and Dawson S. Quaternary Science Reviews, 2006 https://doi.org/10.1016/j.quascirev.2005.07.002
Isolation basins, sea-level changes and the Holocene history of the Greenland Ice Sheet Long, Antony J and Woodroffe, Sarah A and Roberts, David H and Dawson, Sue Quaternary Science Reviews, 2011 https://doi.org/10.1016/j.quascirev.2011.10.013
A model of Greenland ice sheet deglaciation constrained by observations of relative sea level and ice extent Lecavalier, B.S. and Milne G. A. and Simpson M.J.R. and Wake L. and Huybrechts P. and Tarasov L. and Kjeldsen K. and Funder S. and Long A.J. and Woodroffe S. and Dyke A. and Larsen N.K. Quaternary Science Reviews, 2014 https://doi.org/10.1016/j.quascirev.2014.07.018
Paleo sea-level indicators and proxies from Greenland in the GAPSLIP database and comparison with modelled sea level from the PaleoMIST ice-sheet reconstruction Gowan, E. GEUS Bulletin, https://doi.org/10.34194/geusb.v53.8355

Core information

Core name Region Collection date IGSN ID Core type Latitude (DD) Longitude (DD) Water depth
(m)
Core length
(m)
Comments
T0-6 Arctic, Greenland - Avannaata Municipality, terrestrial None Piston corer 69.12000 -50.67600 9.0 3.0 Assigned 'Lake Name' based on Figure 5: Lake name + the number core they kept from the lake. Water depth from Figure 5 schematic (when shown). Core length from Figure 5 schematic (when shown). Lat/Long not given in paper, using Gowan (2023) which has accurate lat long for the lakes. ; Depths are HIGHLY uncertain! Combination of text and assumptions from Fig. 5.; Depths are HIGHLY uncertain! Combination of text and assumptions from Fig. 5.; Depths are HIGHLY uncertain! Combination of text and assumptions from Fig. 5.; Depths are HIGHLY uncertain! Combination of text and assumptions from Fig. 5.; Top/bottom depth reported in paper in m below water surface. I've converted that to m in sediment section by subtracting the water depth.; Top/bottom depth reported in paper in m below water surface. I've converted that to m in sediment section by subtracting the water depth.

Expedition information

Expedition name Ship Start date End date Report DOI
Upernivik Unnamed personal coring platform July 1, 2005 July 1, 2005 https://doi.org/10.1016/j.quascirev.2005.07.002

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
T0-6 96-97 cm 0.96 - 0.97 black gyttja that’s highly humified with traces of silt that transitions to dark gray silt and sand with organic matter Lake has been isolated from the ocean and is a freshwater lake was collecting and forming gyttja Bulk gyttja Bulk combustion 1750.0 ± 40.0 162.0 421.0-1.0 Top/bottom depth reported in paper in m below water surface. I've converted that to m in sediment section by subtracting the water depth.
T0-6 121-122 cm 1.21 - 1.22 soft brown gyttja with laminations of silty gyttja at the base Lake has been isolated from the ocean and is a freshwater lake was collecting and forming gyttja Bulk gyttja Bulk combustion 3540.0 ± 40.0 1865.0 2319.0-1411.0 Top/bottom depth reported in paper in m below water surface. I've converted that to m in sediment section by subtracting the water depth.

Associated documents

No associated documents.