Tree physiological monitoring of the 2018 larch budmoth outbreak: preference for leaf recovery and carbon storage over stem wood formation in Larix decidua.

Zeiraphera griseana cell wall thickness European Alps insect outbreak non-structural carbohydrates (NSC) stable isotopes tree rings wood formation

Journal

Tree physiology
ISSN: 1758-4469
Titre abrégé: Tree Physiol
Pays: Canada
ID NLM: 100955338

Informations de publication

Date de publication:
05 12 2020
Historique:
received: 24 11 2019
revised: 17 05 2020
accepted: 06 07 2020
pubmed: 30 7 2020
medline: 9 2 2021
entrez: 30 7 2020
Statut: ppublish

Résumé

Insect defoliation impacts forest productivity worldwide, highlighting the relevance of plant-insect interactions. The larch budmoth (Zeiraphera griseana Hübner) is one of the most extensively studied defoliators, where numerous tree ring-based analyses on its host (Larix decidua Mill.) have aided in identifying outbreak dynamics over the past millennia. Yet, outbreaks have been widely absent after the early 1980s, and little is known about the in situ tree physiological responses and the allocation of carbon resources during and after defoliation. In summer 2018, we tracked an ongoing larch budmoth outbreak in a well-studied larch forest in the Swiss Alps. We performed biweekly monitoring on an affected and unaffected site using a unique combination of xylogenesis observations, measurements of non-structural carbohydrates, isotopic analysis of needle assimilates and ground-based and remote-sensed leaf trait observations. The budmoth induced a defoliation that lasted 40 days and could be detected by satellite observations. Soluble sugars significantly decreased in needles and stem phloem of the defoliated trees, while starch levels remained stable in the stem and root xylem compared to the control. Carbon and oxygen isotope ratios in needle assimilates indicated that neither photosynthetic assimilation rates nor stomatal conductance was different between sites before, during and after the outbreak. Defoliated trees ceased cell wall thickening 17 days earlier than unaffected trees, showing the earliest halt of ring formation recorded from 2007 untill 2013 and causing significant thinner cell walls, particularly in the latewood. No significant differences were found for cell enlargement rates and ring width. Our study revealed that an outbreak causes a downregulation of cell wall thickening first, while no starch is mobilized or leaf physiology is adjusted to compensate for the reduced carbon source due to defoliation. Our observations suggest that affected larch trees prioritize leaf recovery and carbon storage over wood biomass development.

Identifiants

pubmed: 32722795
pii: 5876819
doi: 10.1093/treephys/tpaa087
doi:

Substances chimiques

Carbon 7440-44-0

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

1697-1711

Informations de copyright

© The Author(s) 2020. Published by Oxford University Press. All rights reserved. For permissions, please e-mail: journals.permissions@oup.com.

Auteurs

Richard L Peters (RL)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.
Department of Plants and Crops, Faculty of Bioscience Engineering, Laboratory of Plant Ecology, Ghent University, Coupure links 653, Ghent B-9000, Belgium.

Jose Carlos Miranda (JC)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.
Forest Genetics and Ecophysiology Research Group, School of Forestry Engineering, Universidad Politécnica de Madrid, Ciudad Universitaria s/n, Madrid 28040, Spain.

Leonie Schönbeck (L)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.

Daniel Nievergelt (D)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.

Marina V Fonti (MV)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.
Institute of Ecology and Geography, Siberian Federal University, 79 Svobodny pr., Krasnoyarsk 660041, Russia.

Matthias Saurer (M)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.

Ana Stritih (A)

ETH Zurich, Institute for Landscape and Spatial Development, Planning of Landscape and Urban Systems (PLUS), Stefano-Franscini Platz 5, Zürich 8093, Switzerland.
WSL Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, Davos Dorf 7260, Switzerland.

Patrick Fonti (P)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.

Beat Wermelinger (B)

Forest Health and Biotic Interactions, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.

Georg von Arx (G)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.

Marco M Lehmann (MM)

Forest Dynamics, Swiss Federal Research Institute for Forest, Snow and Landscape Research (WSL), Zürcherstrasse 111, Birmensdorf CH-8903, Switzerland.

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