RAD-CI: ARCTIC TERRESTRIAL

Associated publications

Title	Author(s)	Publication	DOI	View cores
Isolation basin stratigraphy and Holocene relative sea-level change on Arveprinsen Ejland, Disko Bugt, West Greenland	Long, Antony J. and Roberts, David H. and Wright, Matthew R.	Journal of Quaternary Science,	https://doi.org/10.1002/(SICI)1099-1417(199907)14:4<323::AID-JQS442>3.0.CO;2-0
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
V8-5	Arctic, Greenland - Avannaata Municipality, terrestrial	None		Russian peat corer	69.76741	-51.26006	1.5	1.8	Core name created from lake name + core kept for analysis. Lat/Long redetermined in Google Earth. Water depths estimated from Fig. 8; Converted from depth below water to m in sediment section by subtracting the water depth. Erosion between these units! The contact is sharp in this core and a thin sand bed is found in other cores from the basin. Occurred before organic-rich gyttja deposition; Converted from depth below water to m in sediment section by subtracting the water depth. The contact is sharp in this core and a thin sand bed is found in other cores from the basin. Occurred before organic-rich gyttja deposition; Top/bottom depth reported in paper in m below water surface. Converted that to m in sediment section by subtracting the water depth. ; Sample name created from lake name + core kept for analysis + number of radiocarbon samples from the same core.

Lake information

Lake name	Lake description	Catchment area (m²)	Open vs closed	Mictic state
V8	Elongate basin with an outlet to the south. Lowest lake in the study.		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
V8-5-1	1.77 - 1.78	None	None	bulk gyttja	bulk combustion	4510.0 ± 50.0	3052.0	3534.0-2603.0	Top/bottom depth reported in paper in m below water surface. Converted that to m in sediment section by subtracting the water depth.

Associated documents

No associated documents.