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Journal Article

Differences between tree stem CO2 efflux and O2 influx rates cannot be explained by internal CO2 transport or storage in large beech trees

MPS-Authors
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Helm,  Juliane
Department Biogeochemical Processes, Prof. S. E. Trumbore, Max Planck Institute for Biogeochemistry, Max Planck Society;
IMPRS International Max Planck Research School for Global Biogeochemical Cycles, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Hilman,  Boaz
Department Biogeochemical Processes, Prof. S. E. Trumbore, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Muhr,  Jan
Tree Reserve Carbon Pools, Dr. J. Muhr, Department Biogeochemical Processes, Prof. S. E. Trumbore, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Hartmann,  Henrik
Tree Mortality Mechanisms, Dr. H. Hartmann, Department Biogeochemical Processes, Prof. S. E. Trumbore, Max Planck Institute for Biogeochemistry, Max Planck Society;

External Resource

https://doi.org/10.1111/pce.14614
(Publisher version)

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Fulltext (public)

BGC4457.pdf
(Publisher version), 4MB

Supplementary Material (public)

BGC4457s1.pdf
(Supplementary material), 227KB

Citation

Helm, J., Salomón, R. L., Hilman, B., Muhr, J., Knohl, A., Steppe, K., et al. (2023). Differences between tree stem CO2 efflux and O2 influx rates cannot be explained by internal CO2 transport or storage in large beech trees. Plant, Cell and Environment, 46(9), 2680-2693. doi:10.1111/pce.14614.


Cite as: https://hdl.handle.net/21.11116/0000-000E-16A7-D
Abstract
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