CH4 and δ18O of O2 records from Antarctic and Greenland ice: A clue for stratigraphic disturbance in the bottom part of the Greenland Ice Core Project and the Greenland Ice Sheet Project 2 ice cores
- 30 November 1997
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 102 (C12) , 26547-26557
- https://doi.org/10.1029/97jc00164
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- An interlaboratory comparison of techniques for extracting and analyzing trapped gases in ice coresJournal of Geophysical Research: Oceans, 1997
- Changes in the atmospheric CH4 gradient between Greenland and Antarctica during the HoloceneJournal of Geophysical Research: Atmospheres, 1997
- δ18O of atmospheric oxygen measured on the GRIP Ice Core Document Stratigraphic disturbances in the lowest 10% of the coreGeophysical Research Letters, 1996
- International effort helps decipher mysteries of paleoclimate from Antarctic ice coresEos, 1995
- The Dole Effect and its variations during the last 130,000 years as measured in the Vostok Ice CoreGlobal Biogeochemical Cycles, 1994
- The growth rate and distribution of atmospheric methaneJournal of Geophysical Research: Atmospheres, 1994
- Air content paleo record in the Vostok ice core (Antarctica): A mixed record of climatic and glaciological parametersJournal of Geophysical Research: Atmospheres, 1994
- A 135,000‐year Vostok‐Specmap Common temporal frameworkPaleoceanography and Paleoclimatology, 1993
- Atmospheric methane, record from a Greenland Ice Core over the last 1000 yearGeophysical Research Letters, 1993
- The δ18O of atmospheric O2 from air inclusions in the Vostok Ice Core: Timing of CO2 and ice volume changes during the penultimate deglaciationPaleoceanography and Paleoclimatology, 1991