Ecosystem CO2/H2O fluxes are explained by hydraulically limited gas exchange during tree mortality from spruce bark beetles

Disturbances are increasing globally due to anthropogenic changes in land use and climate. This study determines whether a disturbance that affects the physiology of individual trees can be used to predict the response of the ecosystem by weighing two competing hypothesis at annual time scales: (a)...

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Veröffentlicht in:Journal of geophysical research. Biogeosciences 2014-06, Vol.119 (6), p.1195-1215
Hauptverfasser: Frank, John M., Massman, William J., Ewers, Brent E., Huckaby, Laurie S., Negrón, José F.
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container_end_page 1215
container_issue 6
container_start_page 1195
container_title Journal of geophysical research. Biogeosciences
container_volume 119
creator Frank, John M.
Massman, William J.
Ewers, Brent E.
Huckaby, Laurie S.
Negrón, José F.
description Disturbances are increasing globally due to anthropogenic changes in land use and climate. This study determines whether a disturbance that affects the physiology of individual trees can be used to predict the response of the ecosystem by weighing two competing hypothesis at annual time scales: (a) changes in ecosystem fluxes are proportional to observable patterns of mortality or (b) to explain ecosystem fluxes the physiology of dying trees must also be incorporated. We evaluate these hypotheses by analyzing 6 years of eddy covariance flux data collected throughout the progression of a spruce beetle (Dendroctonus rufipennis) epidemic in a Wyoming Engelmann spruce (Picea engelmannii)–subalpine fir (Abies lasiocarpa) forest and testing for changes in canopy conductance (gc), evapotranspiration (ET), and net ecosystem exchange (NEE) of CO2. We predict from these hypotheses that (a) gc, ET, and NEE all diminish (decrease in absolute magnitude) as trees die or (b) that (1) gc and ET decline as trees are attacked (hydraulic failure from beetle‐associated blue‐stain fungi) and (2) NEE diminishes both as trees are attacked (restricted gas exchange) and when they die. Ecosystem fluxes declined as the outbreak progressed and the epidemic was best described as two phases: (I) hydraulic failure caused restricted gc, ET (28 ± 4% decline, Bayesian posterior mean ± standard deviation), and gas exchange (NEE diminished 13 ± 6%) and (II) trees died (NEE diminished 51 ± 3% with minimal further change in ET to 36 ± 4%). These results support hypothesis b and suggest that model predictions of ecosystem fluxes following massive disturbances must be modified to account for changes in tree physiological controls and not simply observed mortality. Key Points The dynamics of spruce beetle disturbance takes years from attack to mortality Conductance and evapotranspiration decline dramatically from blue‐stain fungus CO2 flux is restricted after beetle attack then plummets with spruce mortality
doi_str_mv 10.1002/2013JG002597
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This study determines whether a disturbance that affects the physiology of individual trees can be used to predict the response of the ecosystem by weighing two competing hypothesis at annual time scales: (a) changes in ecosystem fluxes are proportional to observable patterns of mortality or (b) to explain ecosystem fluxes the physiology of dying trees must also be incorporated. We evaluate these hypotheses by analyzing 6 years of eddy covariance flux data collected throughout the progression of a spruce beetle (Dendroctonus rufipennis) epidemic in a Wyoming Engelmann spruce (Picea engelmannii)–subalpine fir (Abies lasiocarpa) forest and testing for changes in canopy conductance (gc), evapotranspiration (ET), and net ecosystem exchange (NEE) of CO2. We predict from these hypotheses that (a) gc, ET, and NEE all diminish (decrease in absolute magnitude) as trees die or (b) that (1) gc and ET decline as trees are attacked (hydraulic failure from beetle‐associated blue‐stain fungi) and (2) NEE diminishes both as trees are attacked (restricted gas exchange) and when they die. Ecosystem fluxes declined as the outbreak progressed and the epidemic was best described as two phases: (I) hydraulic failure caused restricted gc, ET (28 ± 4% decline, Bayesian posterior mean ± standard deviation), and gas exchange (NEE diminished 13 ± 6%) and (II) trees died (NEE diminished 51 ± 3% with minimal further change in ET to 36 ± 4%). These results support hypothesis b and suggest that model predictions of ecosystem fluxes following massive disturbances must be modified to account for changes in tree physiological controls and not simply observed mortality. 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Biogeosciences</title><addtitle>J. Geophys. Res. Biogeosci</addtitle><description>Disturbances are increasing globally due to anthropogenic changes in land use and climate. This study determines whether a disturbance that affects the physiology of individual trees can be used to predict the response of the ecosystem by weighing two competing hypothesis at annual time scales: (a) changes in ecosystem fluxes are proportional to observable patterns of mortality or (b) to explain ecosystem fluxes the physiology of dying trees must also be incorporated. We evaluate these hypotheses by analyzing 6 years of eddy covariance flux data collected throughout the progression of a spruce beetle (Dendroctonus rufipennis) epidemic in a Wyoming Engelmann spruce (Picea engelmannii)–subalpine fir (Abies lasiocarpa) forest and testing for changes in canopy conductance (gc), evapotranspiration (ET), and net ecosystem exchange (NEE) of CO2. We predict from these hypotheses that (a) gc, ET, and NEE all diminish (decrease in absolute magnitude) as trees die or (b) that (1) gc and ET decline as trees are attacked (hydraulic failure from beetle‐associated blue‐stain fungi) and (2) NEE diminishes both as trees are attacked (restricted gas exchange) and when they die. Ecosystem fluxes declined as the outbreak progressed and the epidemic was best described as two phases: (I) hydraulic failure caused restricted gc, ET (28 ± 4% decline, Bayesian posterior mean ± standard deviation), and gas exchange (NEE diminished 13 ± 6%) and (II) trees died (NEE diminished 51 ± 3% with minimal further change in ET to 36 ± 4%). These results support hypothesis b and suggest that model predictions of ecosystem fluxes following massive disturbances must be modified to account for changes in tree physiological controls and not simply observed mortality. Key Points The dynamics of spruce beetle disturbance takes years from attack to mortality Conductance and evapotranspiration decline dramatically from blue‐stain fungus CO2 flux is restricted after beetle attack then plummets with spruce mortality</description><subject>Anthropogenic factors</subject><subject>Bark</subject><subject>Carbon dioxide</subject><subject>disturbance</subject><subject>Ecosystems</subject><subject>eddy covariance</subject><subject>Environmental changes</subject><subject>Epidemics</subject><subject>Evapotranspiration</subject><subject>Gas exchange</subject><subject>Land use</subject><subject>Mortality</subject><subject>net ecosystem exchange</subject><subject>Physiology</subject><subject>Trees</subject><issn>2169-8953</issn><issn>2169-8961</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNpNUE1PwzAMrRBITLAbPyAS50E-2rQ5wgQd02ASAu0YpakzAuk6klas4s8TNDThiy37vWf7JckFwVcEY3pNMWHzMlaZyI-SESVcTArByfGhzthpMg7hHccoYouQUfJ9p9swhA4aNF3S6xldIuP6HQSkPCDYbZ2yG6hRNaC3ofaqd1Yr5wbkbGO7OFirEGH6TW3WgOre280adR4ANa3vlLPdgIxvGxS2vteAKuU_UAXQOQjnyYlRLsD4L58lr_d3L9PZZLEsH6Y3i4lmaTycFbVKM4pzpgXGRhvDGeN1RSClNalIahg2meEgTKEZp4YJU_NKM0qVyLViZ8nlXnfr288eQiff295v4kpJOCtSKgqeRxTbo76sg0FuvW2UHyTB8tde-d9eOS-fS4opEZE12bNs9HB3YMUvZdTMM7l6KiUpFhm5Xd3LR_YD_Hl-1Q</recordid><startdate>201406</startdate><enddate>201406</enddate><creator>Frank, John M.</creator><creator>Massman, William J.</creator><creator>Ewers, Brent E.</creator><creator>Huckaby, Laurie S.</creator><creator>Negrón, José F.</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>201406</creationdate><title>Ecosystem CO2/H2O fluxes are explained by hydraulically limited gas exchange during tree mortality from spruce bark beetles</title><author>Frank, John M. ; Massman, William J. ; Ewers, Brent E. ; Huckaby, Laurie S. ; Negrón, José F.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3469-38da452073c900fcff6336db1e42d1b14f30f5f6e9f8c362f39fd6bc322a97ca3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Anthropogenic factors</topic><topic>Bark</topic><topic>Carbon dioxide</topic><topic>disturbance</topic><topic>Ecosystems</topic><topic>eddy covariance</topic><topic>Environmental changes</topic><topic>Epidemics</topic><topic>Evapotranspiration</topic><topic>Gas exchange</topic><topic>Land use</topic><topic>Mortality</topic><topic>net ecosystem exchange</topic><topic>Physiology</topic><topic>Trees</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Frank, John M.</creatorcontrib><creatorcontrib>Massman, William J.</creatorcontrib><creatorcontrib>Ewers, Brent E.</creatorcontrib><creatorcontrib>Huckaby, Laurie S.</creatorcontrib><creatorcontrib>Negrón, José F.</creatorcontrib><collection>Istex</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of geophysical research. 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subjects Anthropogenic factors
Bark
Carbon dioxide
disturbance
Ecosystems
eddy covariance
Environmental changes
Epidemics
Evapotranspiration
Gas exchange
Land use
Mortality
net ecosystem exchange
Physiology
Trees
title Ecosystem CO2/H2O fluxes are explained by hydraulically limited gas exchange during tree mortality from spruce bark beetles
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