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Title: Area and Carbon Content of Sphagnum Since Last Glacial Maximum

Abstract

The distribution and abundance of Sphagnum spores in North America and Eurasia are mapped for the past 21ka, as described in Gajewski et al. (2002). In summary, spore data were taken from existing pollen data bases, as were radiocarbon chronologies. The abundance of Sphagnum spores was mapped at 2000-year intervals beginning 21000 years BP (before present). The present-day distribution of abundant Sphagnum spores corresponds closely to areas with peatland development, with maximum Sphagnum abundance between 630 and 1300 mm annual precipitation and between -2° and 60°C mean annual air temperature. Carbon content of peatlands was generated from estimated peatland area, calculated values of peat thickness, and specified values of bulk density (112 × 103-3) and fraction of carbon (51.7%).To access the older version of this data package see: http://cdiac.ess-dive.lbl.gov/trends/ecosystems/gajewski2.html

Authors:
; ; ; ;
  1. University of Ottawa, Laboratory for Paleoclimatology and Climatology
Publication Date:
Other Number(s):
cdiac:doi 10.3334/CDIAC/vrc.001; doi:10.3334/CDIAC/VRC.001; osti:1389531
Research Org.:
Environmental System Science Data Infrastructure for a Virtual Ecosystem (ESS-DIVE) (United States)
Subject:
54 ENVIRONMENTAL SCIENCES
Keywords:
Carbon; Sphagnum; Peatland; North America; Europe; Asia; Eurasia; Carbon Dioxide; peatland carbon; peatland area
OSTI Identifier:
1389531
DOI:
https://doi.org/10.3334/CDIAC/VRC.001

Citation Formats

Gajewski, K., Viau, A., Sawada, M., Atkinson, D., and Wilson, S. Area and Carbon Content of Sphagnum Since Last Glacial Maximum. United States: N. p., 2002. Web. doi:10.3334/CDIAC/VRC.001.
Gajewski, K., Viau, A., Sawada, M., Atkinson, D., & Wilson, S. Area and Carbon Content of Sphagnum Since Last Glacial Maximum. United States. doi:https://doi.org/10.3334/CDIAC/VRC.001
Gajewski, K., Viau, A., Sawada, M., Atkinson, D., and Wilson, S. 2002. "Area and Carbon Content of Sphagnum Since Last Glacial Maximum". United States. doi:https://doi.org/10.3334/CDIAC/VRC.001. https://www.osti.gov/servlets/purl/1389531. Pub date:Tue Oct 01 00:00:00 EDT 2002
@article{osti_1389531,
title = {Area and Carbon Content of Sphagnum Since Last Glacial Maximum},
author = {Gajewski, K. and Viau, A. and Sawada, M. and Atkinson, D. and Wilson, S.},
abstractNote = {The distribution and abundance of Sphagnum spores in North America and Eurasia are mapped for the past 21ka, as described in Gajewski et al. (2002). In summary, spore data were taken from existing pollen data bases, as were radiocarbon chronologies. The abundance of Sphagnum spores was mapped at 2000-year intervals beginning 21000 years BP (before present). The present-day distribution of abundant Sphagnum spores corresponds closely to areas with peatland development, with maximum Sphagnum abundance between 630 and 1300 mm annual precipitation and between -2° and 60°C mean annual air temperature. Carbon content of peatlands was generated from estimated peatland area, calculated values of peat thickness, and specified values of bulk density (112 × 103-3) and fraction of carbon (51.7%).To access the older version of this data package see: http://cdiac.ess-dive.lbl.gov/trends/ecosystems/gajewski2.html},
doi = {10.3334/CDIAC/VRC.001},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Tue Oct 01 00:00:00 EDT 2002},
month = {Tue Oct 01 00:00:00 EDT 2002}
}