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Mechanisms of a coniferous woodland persistence under drought and heat

Bibliographic Data

ID15550685
AuthorsNate G McDowell (0000-0002-2178-2254, Pacific Northwest National Laboratory, corresponding author), Charlotte Grossiord (0000-0002-9113-3671, Los Alamos National Laboratory), Henry D Adams (0000-0001-9630-4305, Oklahoma State University), Sara Pinzón‐Navarro (Universidad de Panamá), D S Mackay (0000-0003-0477-9755, University at Buffalo, State University of New York), David D Breshears (0000-0001-6601-0058, University of Arizona), Craig D Allen (0000-0002-8777-5989, United States Geological Survey), Isaac Borrego (0000-0003-1007-8963, Los Alamos National Laboratory), L Turin Dickman (0000-0003-3876-7058, Los Alamos National Laboratory), Adam Collins (0000-0003-2617-516X, Los Alamos National Laboratory), Monica L Gaylord (0000-0003-3487-063X, US Forest Service), Natalie McBranch (Los Alamos National Laboratory), William T Pockman (0000-0002-3286-0457, University of New Mexico), Alberto Vilagrosa (0000-0002-1432-1214, University of Alicante), Brian H Aukema (0000-0003-4370-0499, University of Minnesota), Devin W Goodsman (0000-0003-1935-5779, Canadian Forest Service), Chonggang Xu (0000-0002-0937-5744, Los Alamos National Laboratory)
Year2019
Volume14
Issue4
Pages045014-045014
Publication date2019-02-21
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ab0921
OpenAlexW2917087592
LanguageEN
Citations received3
References cited4

Predictions of warmer droughts causing increasing forest mortality are becoming abundant, yet few studies have investigated the mechanisms of forest persistence. To examine the resistance of forests to warmer droughts, we used a five-year precipitation reduction (45% removal), heat (+4 C above ambient) and combined drought and heat experiment in an isolated stand of mature Pinus edulis-Juniperus monosperma. Despite severe experimental drought and heating, no trees died, and we observed only minor evidence of hydraulic failure or carbon starvation. Two mechanisms promoting survival were supported. First, access to bedrock water, or 'hydraulic refugia' aided trees in their resistance to the experimental conditions. Second, the isolation of this stand amongst a landscape of dead trees precluded ingress by Ips confusus, frequently the ultimate biotic mortality agent of pion. These combined abiotic and biotic landscape-scale processes can moderate the impacts of future droughts on tree mortality by enabling tree avoidance of hydraulic failure, carbon starvation, and exposure to attacking abiotic agents

Abiotic component · Bedrock · Biology · Disturbance (geology · Geography · Persistence (discontinuity · Precipitation · Resistance (ecology · Woodland · Environmental Science · Fire effects on ecosystems · Plant Water Relations and Carbon Dynamics · Tree-ring climate responses · Ecology · Geology

  • Tree mortality in a warming world

    Open Access•Chuixiang Yi, George R Hendrey et al.•Environmental Research Letters•2022

  • Lateral subsurface flow modulates forest mortality risk to future climate and elevated CO 2

    Open Access•Xiaonan Tai, Martín Venturas et al.•Environmental Research Letters•2021

  • Changing climate sensitivity of secondary growth following extreme drought events in forest ecosystems

    Open Access•Christopher Leifsson, Allan Buras et al.•Environmental Research Letters•2022

  • Temperature response surfaces for mortality risk of tree species with future drought

    Open Access•Henry D Adams, Greg A Barron‐gafford et al.•Environmental Research Letters•2017

Unique citing works3
Citations per year0,6
Citation span2021 - 2022 (2)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 3

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