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Late-glacial and early Holocene variations in atmospheric CO2 concentration indicated by high-resolution stomatal index data

Rundgren, Mats LU and Björck, Svante LU (2003) In Earth and Planetary Science Letters 213(3-4). p.191-204
Abstract
Data from ice cores suggest that Late-glacial and early Holocene atmospheric CO2 variations were rather conservative, the most important change being a gradual Younger Dryas increase. By contrast, palaeo-CO2 records based on the inverse relationship between CO2 Partial pressure and stomatal frequency of terrestrial plant leaves reflect a more dynamic CO2 evolution, including an abrupt decrease at the Allerod/Younger Dryas transition. Here we present a Late-glacial and early Holocene CO2 record based on stomatal index data from leaves preserved in the sediments of a small lake in southwestern Sweden. Three independent records constructed from stomatal index data of Salix polaris, Salix herbacea and Betula nana leaves were combined to form a... (More)
Data from ice cores suggest that Late-glacial and early Holocene atmospheric CO2 variations were rather conservative, the most important change being a gradual Younger Dryas increase. By contrast, palaeo-CO2 records based on the inverse relationship between CO2 Partial pressure and stomatal frequency of terrestrial plant leaves reflect a more dynamic CO2 evolution, including an abrupt decrease at the Allerod/Younger Dryas transition. Here we present a Late-glacial and early Holocene CO2 record based on stomatal index data from leaves preserved in the sediments of a small lake in southwestern Sweden. Three independent records constructed from stomatal index data of Salix polaris, Salix herbacea and Betula nana leaves were combined to form a high-resolution CO2 reconstruction for the period 12 800-10 800 cal yr BP. Atmospheric CO2 concentrations were found to have decreased rapidly from c. 260 ppmv to 210-215 ppmv within 200 years during the Allerod (GI-1)/Younger Dryas (GS-1) transition. After 100-200 years, CO2 concentration started to gradually increase to 270-290 ppmv at the end of the Younger Dryas stadial (GS-1). CO2 concentrations were relatively stable during the early Holocene, except for a short-lived period of lower (240-250 ppmv) values c. 11350-11200 cal yr BP. This Late-glacial and early Holocene CO2 evolution partly resembles previous stomatal-based CO2 reconstructions, and the overall trend is almost identical to that seen in ice-core records. The amplitude of change is, however, markedly higher in the Swedish stomatal-based record compared to the ice cores. This difference may partly be accounted for by the inherent smoothing of ice-core CO2 records caused by diffusion, but a major part of the difference in amplitude between ice-core and stomatal-based records still remains to be explained. Based on our reconstruction, atmospheric CO2 may have played an important role in climate dynamics during the last deglaciation. (C) 2003 Elsevier B.V. All rights reserved. (Less)
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author
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Betula, Salix, early Holocene, atmospheric CO2, late-glacial, stomata
in
Earth and Planetary Science Letters
volume
213
issue
3-4
pages
191 - 204
publisher
Elsevier
external identifiers
  • wos:000185060100003
  • scopus:0041361908
ISSN
1385-013X
DOI
10.1016/S0012-821X(03)00324-8
language
English
LU publication?
yes
id
1e43eca7-7085-4969-8925-27e934b27195 (old id 302290)
date added to LUP
2007-09-20 19:13:17
date last changed
2018-01-07 05:49:28
@article{1e43eca7-7085-4969-8925-27e934b27195,
  abstract     = {Data from ice cores suggest that Late-glacial and early Holocene atmospheric CO2 variations were rather conservative, the most important change being a gradual Younger Dryas increase. By contrast, palaeo-CO2 records based on the inverse relationship between CO2 Partial pressure and stomatal frequency of terrestrial plant leaves reflect a more dynamic CO2 evolution, including an abrupt decrease at the Allerod/Younger Dryas transition. Here we present a Late-glacial and early Holocene CO2 record based on stomatal index data from leaves preserved in the sediments of a small lake in southwestern Sweden. Three independent records constructed from stomatal index data of Salix polaris, Salix herbacea and Betula nana leaves were combined to form a high-resolution CO2 reconstruction for the period 12 800-10 800 cal yr BP. Atmospheric CO2 concentrations were found to have decreased rapidly from c. 260 ppmv to 210-215 ppmv within 200 years during the Allerod (GI-1)/Younger Dryas (GS-1) transition. After 100-200 years, CO2 concentration started to gradually increase to 270-290 ppmv at the end of the Younger Dryas stadial (GS-1). CO2 concentrations were relatively stable during the early Holocene, except for a short-lived period of lower (240-250 ppmv) values c. 11350-11200 cal yr BP. This Late-glacial and early Holocene CO2 evolution partly resembles previous stomatal-based CO2 reconstructions, and the overall trend is almost identical to that seen in ice-core records. The amplitude of change is, however, markedly higher in the Swedish stomatal-based record compared to the ice cores. This difference may partly be accounted for by the inherent smoothing of ice-core CO2 records caused by diffusion, but a major part of the difference in amplitude between ice-core and stomatal-based records still remains to be explained. Based on our reconstruction, atmospheric CO2 may have played an important role in climate dynamics during the last deglaciation. (C) 2003 Elsevier B.V. All rights reserved.},
  author       = {Rundgren, Mats and Björck, Svante},
  issn         = {1385-013X},
  keyword      = {Betula,Salix,early Holocene,atmospheric CO2,late-glacial,stomata},
  language     = {eng},
  number       = {3-4},
  pages        = {191--204},
  publisher    = {Elsevier},
  series       = {Earth and Planetary Science Letters},
  title        = {Late-glacial and early Holocene variations in atmospheric CO2 concentration indicated by high-resolution stomatal index data},
  url          = {http://dx.doi.org/10.1016/S0012-821X(03)00324-8},
  volume       = {213},
  year         = {2003},
}