Holocene climate variability revealed by oxygen isotope analysis of Sphagnum cellulose from Walton Moss, northern England-Reference-Cited by-同舟云学术

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Holocene climate variability revealed by oxygen isotope analysis of Sphagnum cellulose from Walton Moss, northern England

Published:2010-06 Issue:13-14 Volume:29 Page:1590-1601
ISSN:0277-3791
Container-title:Quaternary Science Reviews
language:en
Short-container-title:Quaternary Science Reviews

Author:

Daley T.J.,Barber K.E.,Street-Perrott F.A.,Loader N.J.,Marshall J.D.,Crowley S.F.,Fisher E.H.

Publisher

Elsevier BV

Subject

Geology,Archaeology,Archaeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change

Reference108 articles.

1. Model evaluation for reconstructing the oxygen isotopic composition in precipitation from tree ring cellulose over the last century;Anderson;Chemical Geology,2002

2. Deuterium and oxygen-18 isotope composition of precipitation and atmospheric moisture;Araguas-Araguas;Hydrological Processes,2000

3. Oxygen-18 composition of Sphagnum, and microenvironmental water relations;Aravena;Bryologist,1992

4. Proxy records of climate change in the UK over the last two millennia: documented change and sedimentary records from lakes and bogs;Barber;Journal of the Geological Society, London,1999

5. A sensitive high-resolution record of Late Holocene climatic change from a raised bog in Northern England;Barber;Holocene,1994

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