Modeling C-13 discrimination in tree rings

Citation
F. Berninger et al., Modeling C-13 discrimination in tree rings, GLOBAL BIOG, 14(1), 2000, pp. 213-223
Citations number
59
Categorie Soggetti
Earth Sciences
Journal title
GLOBAL BIOGEOCHEMICAL CYCLES
ISSN journal
08866236 → ACNP
Volume
14
Issue
1
Year of publication
2000
Pages
213 - 223
Database
ISI
SICI code
0886-6236(200003)14:1<213:MCDITR>2.0.ZU;2-E
Abstract
Annual variations from 1877 to 1995 in tree-ring alpha-cellulose C-13/C-12 isotopic ratios for four subarctic Pinus sylvestris trees were determined, and, in conjunction with a recent record of atmospheric (CO2)-C-13/(CO2)-C- 12 ratios, the historical pattern of photosynthetic isotope discrimination, Delta(13)C, was evaluated. Year-to-year variability in Delta(13)C has been as much as 1.5 parts per thousand with the period 1900-1920 showing an ext ended period of unusually high photosynthetic discriminations. The summers during these years were, on average, unusually cold. Since 1920 a long term trend of increasing Delta(13)C of similar to 0.016 parts per thousand yr(- 1) is inferred. We compared measured Delta(13)C with those predicted on the basis of the theoretical relationship between Delta(13)C and the ratio of substomatal to ambient CO2 concentration, C-i/C-a using mechanistic equatio ns for chloroplast biochemistry coupled with a stomatal conductance model. Two variations of a nonlinear optimal-regulation stomatal conductance model were compared. Although both models were based on the assumption that stom ata serve to minimize the average transpiration rate for a given average ra te of CO2 assimilation, one version of the model incorporated reductions in stomatal conductance in response to recent increases in atmospheric CO2 co ncentrations and the other did not. The CO2 sensitive stomatal model failed to describe the long-term increase in C-13 discrimination, especially afte r 1950. The insensitive model gave good agreement, suggesting that an obser ved increase in subarctic Pinus sylvestris Delta(13)C since 1920 is attribu table to recent increases in atmospheric CO2 concentrations with subsequent increases in the ratio of substomatal to ambient CO2 concentrations. The m odel was also capable of accounting for high frequency (year-to-year) varia tions in Delta(13)C, these differences being attributable to year-to-year f luctuations in the average leaf-to-air vapor pressure difference affecting stomatal conductance and hence C-i/C-a.