Meteorological observations, and 210Pb and 14C ages of peat profiles from subarctic Canada
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2010
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| _version_ | 1867169506237874176 |
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| author | Kaislahti Tillman, Päivi Holzkämper, Steffen Kuhry, Peter Sannel, A Britta K Loader, Neil J Robertson, Iain |
| author_facet | Kaislahti Tillman, Päivi Holzkämper, Steffen Kuhry, Peter Sannel, A Britta K Loader, Neil J Robertson, Iain |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Stable carbon and oxygen isotope ratios in single plant components in Sphagnum peat have a good potential to reveal environmental changes in peat archives. Two peat profiles, covering the past ~6000 years, and a Sphagnum hummock from a discontinuous permafrost area in west central Canada were studied in order to evaluate the effect of decomposition rate on isotope records and to assess which plant components are most suitable for climate reconstructions. The stable isotope values from the most recently forming Sphagnum tissues were compared with observational climate data to study the impact of variations in temperature and precipitation on the peat isotopes. Our results show that there is high correlation between d13C values in alpha-cellulose isolated from Sphagnum fuscum stems and summer temperatures, whereas d18O in the plant tissues is controlled by several factors, such as summer precipitation, summer temperature and evaporation. According to our results, decomposition as derived from C/N values and colorimetry does not seem to affect the oxygen and carbon isotope values of alpha-cellulose from Sphagnum fuscum peat significantly. There is, however, a (quasi-) constant offset between the isotope values of branches and stems and between whole plant material and alpha-cellulose, which makes it crucial to select single moss-fractions when past climate and environmental changes are to be derived from the isotope record. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_786145 |
| institution | PANGAEA |
| language | en |
| publishDate | 2010 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Meteorological observations, and 210Pb and 14C ages of peat profiles from subarctic Canada Kaislahti Tillman, Päivi Holzkämper, Steffen Kuhry, Peter Sannel, A Britta K Loader, Neil J Robertson, Iain International Polar Year (2007-2008); ipy; IPY Stable carbon and oxygen isotope ratios in single plant components in Sphagnum peat have a good potential to reveal environmental changes in peat archives. Two peat profiles, covering the past ~6000 years, and a Sphagnum hummock from a discontinuous permafrost area in west central Canada were studied in order to evaluate the effect of decomposition rate on isotope records and to assess which plant components are most suitable for climate reconstructions. The stable isotope values from the most recently forming Sphagnum tissues were compared with observational climate data to study the impact of variations in temperature and precipitation on the peat isotopes. Our results show that there is high correlation between d13C values in alpha-cellulose isolated from Sphagnum fuscum stems and summer temperatures, whereas d18O in the plant tissues is controlled by several factors, such as summer precipitation, summer temperature and evaporation. According to our results, decomposition as derived from C/N values and colorimetry does not seem to affect the oxygen and carbon isotope values of alpha-cellulose from Sphagnum fuscum peat significantly. There is, however, a (quasi-) constant offset between the isotope values of branches and stems and between whole plant material and alpha-cellulose, which makes it crucial to select single moss-fractions when past climate and environmental changes are to be derived from the isotope record. |
| title | Meteorological observations, and 210Pb and 14C ages of peat profiles from subarctic Canada |
| topic | International Polar Year (2007-2008); ipy; IPY |
| url | https://doi.org/10.1594/PANGAEA.786145 |