an online journal jointly published by imcg and ips
About |
Editorial Board |
Volumes |
Book Reviews |
Submit a paper |
Contact |
Copyright |
Home |
by R.J. Payne and J.J. Blackford
Published online: 14.11.2008
Summary
Peatland records of Holocene palaeoclimate have been widely used in
Europe. Their potential in western North America remains largely
unexploited despite an abundance of candidate sites. Peat humification
analysis is a widely used technique for palaeoclimatic inference from
peatlands. This study attempts to demonstrate a climatic role in
determining peat humification by comparing low-resolution peat
humification records from five mires in south-east Alaska. Humification
was determined by alkali extraction and colorimetry and records dated
by radiocarbon and tephrochronology. Testate amoebae analysis was
carried out across a major humification-inferred wet shift in three of
the sites. The humification results show variability down the length of
the cores but there is only limited agreement between records from
different sites. Many general trends in the data appear to be out of
phase and periods of proxy 'complacency' are shown. This study does not
provide strong evidence for climatic forcing of humification in these
sites. Methodological issues including possible problems with the
age-depth models and the role of a peat-forming plant species signal in
the humification data are discussed. The results support previous
studies in suggesting the value of employing a multi-proxy, multi-site,
and possibly multi-core approach in peat-based palaeoclimatology.
Payne, R.J. & Blackford, J.J. (2008): Peat humification and climate change: a multi-site comparison from mires in south-east Alaska. Mires and Peat 3: Art. 9. (Online: http://www.mires-and-peat.net/map03/map_03_09.htm)
IMCG and IPS acknowledge the work of the reviewers.
| Last update: 01.01.2010 | ![]() |
www.mires-and-peat.net |
| Key title: Mires and Peat | ISSN 1819-754X | Abbreviated key title: Mires Peat |