Tree-ring isotopes from the Swiss Alps reveal non-climatic fingerprints of cyclic insect population outbreaks over the past 700 years
Jazyk angličtina Země Kanada Médium print
Typ dokumentu časopisecké články, práce podpořená grantem
PubMed
36738262
PubMed Central
PMC10177004
DOI
10.1093/treephys/tpad014
PII: 7026060
Knihovny.cz E-zdroje
- Klíčová slova
- Zeiraphera griseana, dendroecology, deuterium, ecophysiology, insect defoliation, insect outbreak, plant–pathogen interaction, stable isotope, tree physiology, tree-ring cellulose,
- MeSH
- izotopy kyslíku analýza MeSH
- izotopy uhlíku analýza MeSH
- modřín * fyziologie MeSH
- můry * fyziologie MeSH
- stromy MeSH
- zvířata MeSH
- Check Tag
- zvířata MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Geografické názvy
- Švýcarsko MeSH
- Názvy látek
- izotopy kyslíku MeSH
- izotopy uhlíku MeSH
- Oxygen-18 MeSH Prohlížeč
Recent experiments have underlined the potential of δ2H in tree-ring cellulose as a physiological indicator of shifts in autotrophic versus heterotrophic processes (i.e., the use of fresh versus stored non-structural carbohydrates). However, the impact of these processes has not yet been quantified under natural conditions. Defoliator outbreaks disrupt tree functioning and carbon assimilation, stimulating remobilization, therefore providing a unique opportunity to improve our understanding of changes in δ2H. By exploring a 700-year tree-ring isotope chronology from Switzerland, we assessed the impact of 79 larch budmoth (LBM, Zeiraphera griseana [Hübner]) outbreaks on the growth of its host tree species, Larix decidua [Mill]. The LBM outbreaks significantly altered the tree-ring isotopic signature, creating a 2H-enrichment and an 18O- and 13C-depletion. Changes in tree physiological functioning in outbreak years are shown by the decoupling of δ2H and δ18O (O-H relationship), in contrast to the positive correlation in non-outbreak years. Across the centuries, the O-H relationship in outbreak years was not significantly affected by temperature, indicating that non-climatic physiological processes dominate over climate in determining δ2H. We conclude that the combination of these isotopic parameters can serve as a metric for assessing changes in physiological mechanisms over time.
Department of Geography Faculty of Science Masaryk University Brno 611 37 Czech Republic
Department of Geography University of Cambridge Downing Place Cambridge CB2 3EN UK
Global Change Research Institute Czech Academy of Sciences Brno 603 00 Czech Republic
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