Low resolution stable isotopes of ice core Taylor Dome

The delta 18O values were determined at the Quaternary Isotope Laboratory (M. Stuiver, Box 351360, University of Washington, Seattle WA 98195, USA). The time scale (st9507) was estimated from a correlation of delta 18O with the Vostok delta D record (Grootes et al. 1994; Steig, 1996). Between 0-340m...

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Bibliographic Details
Main Authors: Grootes, Pieter Meiert, Steig, Eric J
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 1994
Subjects:
DEPTH, ice/snow
Age model
δ18O, water
Electromechanical drill
Age model, st9507 Steig, 1996, PhD Thesis Univ Washington, Seattle
TAYLOR_DOME
Sampling/drilling ice
Taylor Dome
ice core
Online Access:https://dx.doi.org/10.1594/pangaea.473389
https://doi.pangaea.de/10.1594/PANGAEA.473389
Description
Summary:The delta 18O values were determined at the Quaternary Isotope Laboratory (M. Stuiver, Box 351360, University of Washington, Seattle WA 98195, USA). The time scale (st9507) was estimated from a correlation of delta 18O with the Vostok delta D record (Grootes et al. 1994; Steig, 1996). Between 0-340m the samples measured were of 1m cuts taken in the field. Each 1m core section was slabbed to provide a surface for ECM measurement; a thin slice was removed uniformly along the length for isotope analysis. From 340m to the bottom, sampling was done at the National Ice Core Lab at 0.5m lengths. Note that these core sections were shipped intact to NICL; they were not processed in the field.

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