Species-specific transpiration responses to intermediate disturbance in a northern hardwood forest
Intermediate disturbances shape forest structure and composition, which may in turn alter carbon, nitrogen, and water cycling. We used a large‐scale experiment in a forest in northern lower Michigan where we prescribed an intermediate disturbance by stem girdling all canopy‐dominant early succession...
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Veröffentlicht in: | Journal of geophysical research. Biogeosciences 2014-12, Vol.119 (12), p.2292-2311 |
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container_title | Journal of geophysical research. Biogeosciences |
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creator | Matheny, Ashley M. Bohrer, Gil Vogel, Christoph S. Morin, Timothy H. He, Lingli Frasson, Renato Prata de Moraes Mirfenderesgi, Golnazalsadat Schäfer, Karina V. R. Gough, Christopher M. Ivanov, Valeriy Y. Curtis, Peter S. |
description | Intermediate disturbances shape forest structure and composition, which may in turn alter carbon, nitrogen, and water cycling. We used a large‐scale experiment in a forest in northern lower Michigan where we prescribed an intermediate disturbance by stem girdling all canopy‐dominant early successional trees to simulate an accelerated age‐related senescence associated with natural succession. Using 3 years of eddy covariance and sap flux measurements in the disturbed area and an adjacent control plot, we analyzed disturbance‐induced changes to plot level and species‐specific transpiration and stomatal conductance. We found transpiration to be ~15% lower in disturbed plots than in unmanipulated control plots. However, species‐specific responses to changes in microclimate varied. While red oak and white pine showed increases in stomatal conductance during postdisturbance (62.5 and 132.2%, respectively), red maple reduced stomatal conductance by 36.8%. We used the hysteresis between sap flux and vapor pressure deficit to quantify diurnal hydraulic stress incurred by each species in both plots. Red oak, a ring porous anisohydric species, demonstrated the largest mean relative hysteresis, while red maple, bigtooth aspen, and paper birch, all diffuse porous species, had the lowest relative hysteresis. We employed the Penman‐Monteith model for LE to demonstrate that these species‐specific responses to disturbance are not well captured using current modeling strategies and that accounting for changes to leaf area index and plot microclimate are insufficient to fully describe the effects of disturbance on transpiration.
Key Points
Plot level scaling of evaporation from sap flux evaluated with eddy flux
Disturbance changes intradaily transpiration dynamics
Hydraulic strategy causes species‐specific transpiration differences |
doi_str_mv | 10.1002/2014JG002804 |
format | Article |
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Key Points
Plot level scaling of evaporation from sap flux evaluated with eddy flux
Disturbance changes intradaily transpiration dynamics
Hydraulic strategy causes species‐specific transpiration differences</description><identifier>ISSN: 2169-8953</identifier><identifier>EISSN: 2169-8961</identifier><identifier>DOI: 10.1002/2014JG002804</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Birch trees ; Conductance ; Disturbance ; Disturbances ; Ecological succession ; Evaporation ; Fluctuations ; Flux ; Forests ; Herbivores ; Hydraulics ; Hysteresis ; isohydric/anisohydric ; Mathematical models ; Microclimate ; sap flux ; Stomatal conductance ; Transpiration ; Vapor pressure</subject><ispartof>Journal of geophysical research. Biogeosciences, 2014-12, Vol.119 (12), p.2292-2311</ispartof><rights>2014. American Geophysical Union. All Rights Reserved.</rights><rights>2015. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c7685-83315dc4c6de643ad1d8a47a6564c75cde4214be7c10027e00796c9c03596c2d3</citedby><cites>FETCH-LOGICAL-c7685-83315dc4c6de643ad1d8a47a6564c75cde4214be7c10027e00796c9c03596c2d3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2014JG002804$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2014JG002804$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,1433,27923,27924,45573,45574,46408,46832</link.rule.ids></links><search><creatorcontrib>Matheny, Ashley M.</creatorcontrib><creatorcontrib>Bohrer, Gil</creatorcontrib><creatorcontrib>Vogel, Christoph S.</creatorcontrib><creatorcontrib>Morin, Timothy H.</creatorcontrib><creatorcontrib>He, Lingli</creatorcontrib><creatorcontrib>Frasson, Renato Prata de Moraes</creatorcontrib><creatorcontrib>Mirfenderesgi, Golnazalsadat</creatorcontrib><creatorcontrib>Schäfer, Karina V. R.</creatorcontrib><creatorcontrib>Gough, Christopher M.</creatorcontrib><creatorcontrib>Ivanov, Valeriy Y.</creatorcontrib><creatorcontrib>Curtis, Peter S.</creatorcontrib><title>Species-specific transpiration responses to intermediate disturbance in a northern hardwood forest</title><title>Journal of geophysical research. Biogeosciences</title><addtitle>J. Geophys. Res. Biogeosci</addtitle><description>Intermediate disturbances shape forest structure and composition, which may in turn alter carbon, nitrogen, and water cycling. We used a large‐scale experiment in a forest in northern lower Michigan where we prescribed an intermediate disturbance by stem girdling all canopy‐dominant early successional trees to simulate an accelerated age‐related senescence associated with natural succession. Using 3 years of eddy covariance and sap flux measurements in the disturbed area and an adjacent control plot, we analyzed disturbance‐induced changes to plot level and species‐specific transpiration and stomatal conductance. We found transpiration to be ~15% lower in disturbed plots than in unmanipulated control plots. However, species‐specific responses to changes in microclimate varied. While red oak and white pine showed increases in stomatal conductance during postdisturbance (62.5 and 132.2%, respectively), red maple reduced stomatal conductance by 36.8%. We used the hysteresis between sap flux and vapor pressure deficit to quantify diurnal hydraulic stress incurred by each species in both plots. Red oak, a ring porous anisohydric species, demonstrated the largest mean relative hysteresis, while red maple, bigtooth aspen, and paper birch, all diffuse porous species, had the lowest relative hysteresis. We employed the Penman‐Monteith model for LE to demonstrate that these species‐specific responses to disturbance are not well captured using current modeling strategies and that accounting for changes to leaf area index and plot microclimate are insufficient to fully describe the effects of disturbance on transpiration.
Key Points
Plot level scaling of evaporation from sap flux evaluated with eddy flux
Disturbance changes intradaily transpiration dynamics
Hydraulic strategy causes species‐specific transpiration differences</description><subject>Birch trees</subject><subject>Conductance</subject><subject>Disturbance</subject><subject>Disturbances</subject><subject>Ecological succession</subject><subject>Evaporation</subject><subject>Fluctuations</subject><subject>Flux</subject><subject>Forests</subject><subject>Herbivores</subject><subject>Hydraulics</subject><subject>Hysteresis</subject><subject>isohydric/anisohydric</subject><subject>Mathematical models</subject><subject>Microclimate</subject><subject>sap flux</subject><subject>Stomatal conductance</subject><subject>Transpiration</subject><subject>Vapor pressure</subject><issn>2169-8953</issn><issn>2169-8961</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqNkU1LJDEQhhtxQVFv_oCAFw-25qvzcVTR3hVxYXX1GDJJDUZnkjbpYfTfb4YREQ-yubxF6nkrVZWm2Sf4mGBMTygm_KqvkcJ8o9mmROhWaUE2P-KObTV7pTzhelS9ImS7mdwO4AKUtqx0Ghwas41lCNmOIUWUoQwpFihoTCjEEfIcfLAjIB_KuMgTGx3UBLIopjw-Qo7o0Wa_TMmjaar2cbf5MbWzAnvvutP8vby4O__ZXv_uf52fXrdOCtW1ijHSeced8CA4s554Zbm0ohPcyc554JTwCUi3GlcCxlILpx1mXVXq2U5zuK475PSyqA-beSgOZjMbIS2KIUJUDyGE_wfacaGU1qKiB1_Qp7TIsQ5SKS6p0IKySh2tKZdTKRmmZshhbvObIdis-jWfv6fibI0vwwzevmXNVf-np7juprratatuHl4_XDY_GyGZ7MzDTW_Uvdb92R01t-wf7NifXA</recordid><startdate>201412</startdate><enddate>201412</enddate><creator>Matheny, Ashley M.</creator><creator>Bohrer, Gil</creator><creator>Vogel, Christoph S.</creator><creator>Morin, Timothy H.</creator><creator>He, Lingli</creator><creator>Frasson, Renato Prata de Moraes</creator><creator>Mirfenderesgi, Golnazalsadat</creator><creator>Schäfer, Karina V. R.</creator><creator>Gough, Christopher M.</creator><creator>Ivanov, Valeriy Y.</creator><creator>Curtis, Peter S.</creator><general>Blackwell Publishing Ltd</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>201412</creationdate><title>Species-specific transpiration responses to intermediate disturbance in a northern hardwood forest</title><author>Matheny, Ashley M. ; Bohrer, Gil ; Vogel, Christoph S. ; Morin, Timothy H. ; He, Lingli ; Frasson, Renato Prata de Moraes ; Mirfenderesgi, Golnazalsadat ; Schäfer, Karina V. R. ; Gough, Christopher M. ; Ivanov, Valeriy Y. ; Curtis, Peter S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c7685-83315dc4c6de643ad1d8a47a6564c75cde4214be7c10027e00796c9c03596c2d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Birch trees</topic><topic>Conductance</topic><topic>Disturbance</topic><topic>Disturbances</topic><topic>Ecological succession</topic><topic>Evaporation</topic><topic>Fluctuations</topic><topic>Flux</topic><topic>Forests</topic><topic>Herbivores</topic><topic>Hydraulics</topic><topic>Hysteresis</topic><topic>isohydric/anisohydric</topic><topic>Mathematical models</topic><topic>Microclimate</topic><topic>sap flux</topic><topic>Stomatal conductance</topic><topic>Transpiration</topic><topic>Vapor pressure</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Matheny, Ashley M.</creatorcontrib><creatorcontrib>Bohrer, Gil</creatorcontrib><creatorcontrib>Vogel, Christoph S.</creatorcontrib><creatorcontrib>Morin, Timothy H.</creatorcontrib><creatorcontrib>He, Lingli</creatorcontrib><creatorcontrib>Frasson, Renato Prata de Moraes</creatorcontrib><creatorcontrib>Mirfenderesgi, Golnazalsadat</creatorcontrib><creatorcontrib>Schäfer, Karina V. 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Biogeosciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Matheny, Ashley M.</au><au>Bohrer, Gil</au><au>Vogel, Christoph S.</au><au>Morin, Timothy H.</au><au>He, Lingli</au><au>Frasson, Renato Prata de Moraes</au><au>Mirfenderesgi, Golnazalsadat</au><au>Schäfer, Karina V. R.</au><au>Gough, Christopher M.</au><au>Ivanov, Valeriy Y.</au><au>Curtis, Peter S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Species-specific transpiration responses to intermediate disturbance in a northern hardwood forest</atitle><jtitle>Journal of geophysical research. Biogeosciences</jtitle><addtitle>J. Geophys. Res. Biogeosci</addtitle><date>2014-12</date><risdate>2014</risdate><volume>119</volume><issue>12</issue><spage>2292</spage><epage>2311</epage><pages>2292-2311</pages><issn>2169-8953</issn><eissn>2169-8961</eissn><abstract>Intermediate disturbances shape forest structure and composition, which may in turn alter carbon, nitrogen, and water cycling. We used a large‐scale experiment in a forest in northern lower Michigan where we prescribed an intermediate disturbance by stem girdling all canopy‐dominant early successional trees to simulate an accelerated age‐related senescence associated with natural succession. Using 3 years of eddy covariance and sap flux measurements in the disturbed area and an adjacent control plot, we analyzed disturbance‐induced changes to plot level and species‐specific transpiration and stomatal conductance. We found transpiration to be ~15% lower in disturbed plots than in unmanipulated control plots. However, species‐specific responses to changes in microclimate varied. While red oak and white pine showed increases in stomatal conductance during postdisturbance (62.5 and 132.2%, respectively), red maple reduced stomatal conductance by 36.8%. We used the hysteresis between sap flux and vapor pressure deficit to quantify diurnal hydraulic stress incurred by each species in both plots. Red oak, a ring porous anisohydric species, demonstrated the largest mean relative hysteresis, while red maple, bigtooth aspen, and paper birch, all diffuse porous species, had the lowest relative hysteresis. We employed the Penman‐Monteith model for LE to demonstrate that these species‐specific responses to disturbance are not well captured using current modeling strategies and that accounting for changes to leaf area index and plot microclimate are insufficient to fully describe the effects of disturbance on transpiration.
Key Points
Plot level scaling of evaporation from sap flux evaluated with eddy flux
Disturbance changes intradaily transpiration dynamics
Hydraulic strategy causes species‐specific transpiration differences</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2014JG002804</doi><tpages>20</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Birch trees Conductance Disturbance Disturbances Ecological succession Evaporation Fluctuations Flux Forests Herbivores Hydraulics Hysteresis isohydric/anisohydric Mathematical models Microclimate sap flux Stomatal conductance Transpiration Vapor pressure |
title | Species-specific transpiration responses to intermediate disturbance in a northern hardwood forest |
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