Influence of cellulose oxygen isotope variability in sub-fossil Sphagnum and plant macrofossil components on the reliability of paleoclimate records at the Mer Bleue Bog, Ottawa, Ontario, Canada

Author:

El Bilali Hafida,Patterson R. Timothy

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference56 articles.

1. Anderson, T.W., 1988. Late Quaternary pollen stratigraphy of the Ottawa valley – Lake Ontario region and its application in dating the Champlain Sea. In: Gadd, N.R. (Ed.), The Late Quaternary Development of the Champlain Sea Basin. Geological Association of Canada, Canada. Special Paper 35, pp. 207–224.

2. Oxygen and carbon isotopic record of climatic variability in tree ring cellulose (Picea abies): an example from Central Switzerland;Anderson;Journal of Geophysical Research,1998

3. Oxygen isotopes in cellulose from modern and Quaternary intertropical peatbogs: implications for palaeohydrology;Aucour;Chemical Geology,1996

4. Auer, V., 1930. Peat bogs in Southeastern Canada. Canada Department of Mines, Ottawa. Memoir 162, 32 pp.

5. Correlations between oxygen isotope ratios of wood constituents of Quercus and Pinus samples from around the world;Barbour;Australian Journal of Plant Physiology,2001

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