Interpreting paleoclimate from l8 O and 2 H in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern Ontario
The oxygen-isotope content of terrestrial plant cellulose is related to that of the source waters by a two-step process involving evapotranspirative leaf-water enrichment and equilibrium isotopic exchange between leaf water and atmospheric carbon dioxide. A combination of two models that describe th...
Published in: | Canadian Journal of Earth Sciences |
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1985
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crcansciencepubl:10.1139/e85-180 2024-03-03T08:47:55+00:00 Interpreting paleoclimate from l8 O and 2 H in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern Ontario Edwards, T. W. D. Aravena, R. O. Fritz, P. Morgan, A. V. 1985 http://dx.doi.org/10.1139/e85-180 http://www.nrcresearchpress.com/doi/pdf/10.1139/e85-180 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 22, issue 11, page 1720-1726 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1985 crcansciencepubl https://doi.org/10.1139/e85-180 2024-02-07T10:53:41Z The oxygen-isotope content of terrestrial plant cellulose is related to that of the source waters by a two-step process involving evapotranspirative leaf-water enrichment and equilibrium isotopic exchange between leaf water and atmospheric carbon dioxide. A combination of two models that describe these steps yields consistent agreement between measured and predicted climatic and isotopic data. Humidity is the dominant influence on variations in the cellulose 18 O enrichment relative to the source water. A good first-order approximation of the average daytime relative humidity during the growth season at a site can be based on the linear correlation that exists between humidity and cellulose enrichment, without explicit consideration of factors such as temperature, δ 18 O of atmospheric vapour, and leaf boundary-layer dynamics.The value of the combined model for paleoclimatic reconstruction has been tested using fossil wood from a late glacial site at Brampton, Ontario. Estimates of the past relative humidity were derived from the divergence between measured δ 18 O values of fossil wood cellulose and environmental water isotopic compositions inferred from the carbon-bound deuterium contents of the cellulose. Growing conditions were apparently substantially drier than those at present between about 11 500 and 8700 years BP, at a time when coniferous forests predominated in southwestern Ontario. A shift in the inferred meteoric water composition over this period suggests a gradual increase in mean annual temperature of about 2 or 3 °C, in agreement with estimates of temperature change based on paleoentomological data. Article in Journal/Newspaper permafrost Canadian Science Publishing Canadian Journal of Earth Sciences 22 11 1720 1726 |
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Open Polar |
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Canadian Science Publishing |
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crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
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General Earth and Planetary Sciences Edwards, T. W. D. Aravena, R. O. Fritz, P. Morgan, A. V. Interpreting paleoclimate from l8 O and 2 H in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern Ontario |
topic_facet |
General Earth and Planetary Sciences |
description |
The oxygen-isotope content of terrestrial plant cellulose is related to that of the source waters by a two-step process involving evapotranspirative leaf-water enrichment and equilibrium isotopic exchange between leaf water and atmospheric carbon dioxide. A combination of two models that describe these steps yields consistent agreement between measured and predicted climatic and isotopic data. Humidity is the dominant influence on variations in the cellulose 18 O enrichment relative to the source water. A good first-order approximation of the average daytime relative humidity during the growth season at a site can be based on the linear correlation that exists between humidity and cellulose enrichment, without explicit consideration of factors such as temperature, δ 18 O of atmospheric vapour, and leaf boundary-layer dynamics.The value of the combined model for paleoclimatic reconstruction has been tested using fossil wood from a late glacial site at Brampton, Ontario. Estimates of the past relative humidity were derived from the divergence between measured δ 18 O values of fossil wood cellulose and environmental water isotopic compositions inferred from the carbon-bound deuterium contents of the cellulose. Growing conditions were apparently substantially drier than those at present between about 11 500 and 8700 years BP, at a time when coniferous forests predominated in southwestern Ontario. A shift in the inferred meteoric water composition over this period suggests a gradual increase in mean annual temperature of about 2 or 3 °C, in agreement with estimates of temperature change based on paleoentomological data. |
format |
Article in Journal/Newspaper |
author |
Edwards, T. W. D. Aravena, R. O. Fritz, P. Morgan, A. V. |
author_facet |
Edwards, T. W. D. Aravena, R. O. Fritz, P. Morgan, A. V. |
author_sort |
Edwards, T. W. D. |
title |
Interpreting paleoclimate from l8 O and 2 H in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern Ontario |
title_short |
Interpreting paleoclimate from l8 O and 2 H in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern Ontario |
title_full |
Interpreting paleoclimate from l8 O and 2 H in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern Ontario |
title_fullStr |
Interpreting paleoclimate from l8 O and 2 H in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern Ontario |
title_full_unstemmed |
Interpreting paleoclimate from l8 O and 2 H in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern Ontario |
title_sort |
interpreting paleoclimate from l8 o and 2 h in plant cellulose: comparison with evidence from fossil insects and relict permafrost in southwestern ontario |
publisher |
Canadian Science Publishing |
publishDate |
1985 |
url |
http://dx.doi.org/10.1139/e85-180 http://www.nrcresearchpress.com/doi/pdf/10.1139/e85-180 |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Canadian Journal of Earth Sciences volume 22, issue 11, page 1720-1726 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e85-180 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
22 |
container_issue |
11 |
container_start_page |
1720 |
op_container_end_page |
1726 |
_version_ |
1792504213046034432 |