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New insights into the mechanisms of plant isotope fractionation from combined analysis of intramolecular
13
C and deuterium abundances in
Pinus nigra
tree-ring glucose
Wieloch, Thomas
Umeå University, Faculty of Science and Technology, Umeå Plant Science Centre (UPSC). Department of Forest Genetics and Plant Physiology, Swedish University of Agricultural Sciences, Umeå, Sweden; Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA.
ORCID iD:
0000-0001-9162-2291
Holloway-Phillips, Meisha
Research Unit of Forest Dynamics, Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmendsorf, Switzerland.
Yu, Jun
Umeå University, Faculty of Science and Technology, Department of Mathematics and Mathematical Statistics.
(Mathematical Statistics)
ORCID iD:
0000-0001-5673-620X
Niittylä, Totte
Umeå University, Faculty of Science and Technology, Umeå Plant Science Centre (UPSC). Department of Forest Genetics and Plant Physiology, Swedish University of Agricultural Sciences, Umeå, Sweden.
2024 (English)
In:
New Phytologist, ISSN 0028-646X, E-ISSN 1469-8137
Article in journal (Refereed) Epub ahead of print
Abstract [en]
Understanding isotope fractionation mechanisms is fundamental for analyses of plant ecophysiology and paleoclimate based on tree-ring isotope data.
To gain new insights into isotope fractionation, we analysed intramolecular
13
C discrimination in tree-ring glucose (
Δ
i
', i
= C-1 to C-6) and metabolic deuterium fractionation at H
1
and H
2
(ε
met
) combinedly. This dual-isotope approach was used for isotope-signal deconvolution.
We found evidence for metabolic processes affecting Δ
1
' and Δ
3
', which respond to air vapour pressure deficit (VPD), and processes affecting
Δ
1
'
and
Δ
3
'
, and ε
met
, which respond to precipitation but not VPD. These relationships exhibit change points dividing a period of homeostasis (1961–1980) from a period of metabolic adjustment (1983–1995). Homeostasis may result from sufficient groundwater availability. Additionally, we found Δ
5
' and Δ
6
' relationships with radiation and temperature, which are temporally stable and consistent with previously proposed isotope fractionation mechanisms.
Based on the multitude of climate covariables, intramolecular carbon isotope analysis has a remarkable potential for climate reconstruction. While isotope fractionation beyond leaves is currently considered to be constant, we propose significant parts of the carbon and hydrogen isotope variation in tree-ring glucose originate in stems (precipitation-dependent signals). As basis for follow-up studies, we propose mechanisms introducing Δ
1
', Δ
2
', Δ
3
', and ε
met
variability.
Place, publisher, year, edition, pages
John Wiley & Sons, 2024.
Keywords [en]
carbon stable isotopes, hydrogen stable isotopes, intramolecular isotope analysis, isotope fractionation mechanisms, leaf water status, plant–environment interactions, stem water status, tree rings
National Category
Botany
Identifiers
URN:
urn:nbn:se:umu:diva-230106
DOI:
10.1111/nph.20113
ISI:
001318897800001
PubMedID:
39314055
Scopus ID:
2-s2.0-85204714005
OAI: oai:DiVA.org:umu-230106
DiVA, id:
diva2:1901673
Funder
Swedish Research Council Formas, 2022-02833
Available from:
2024-09-29
Created:
2024-09-29
Last updated:
2024-10-16
Open Access in DiVA
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Wieloch, Thomas
Yu, Jun
Niittylä, Totte
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Yu, Jun
Niittylä, Totte
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Department of Mathematics and Mathematical Statistics
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