Species-Specific Shifts in Diurnal Sap Velocity Dynamics and Hysteretic Behavior of Ecophysiological Variables During the 2015–2016 El Niño Event in the Amazon Forest
Current climate change scenarios indicate warmer temperatures and the potential for more extreme droughts in the tropics, such that a mechanistic understanding of the water cycle from individual trees to landscapes is needed to adequately predict future changes in forest structure and function. In t...
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Published in | Frontiers in plant science Vol. 10; p. 830 |
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Main Authors | , , , , , , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
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Frontiers Research Foundation
28.06.2019
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Abstract | Current climate change scenarios indicate warmer temperatures and the potential for more extreme droughts in the tropics, such that a mechanistic understanding of the water cycle from individual trees to landscapes is needed to adequately predict future changes in forest structure and function. In this study, we contrasted physiological responses of tropical trees during a normal dry season with the extreme dry season due to the 2015-2016 El Niño-Southern Oscillation (ENSO) event. We quantified high resolution temporal dynamics of sap velocity (V
), stomatal conductance (g
) and leaf water potential (Ψ
) of multiple canopy trees, and their correlations with leaf temperature (T
) and environmental conditions [direct solar radiation, air temperature (T
) and vapor pressure deficit (VPD)]. The experiment leveraged canopy access towers to measure adjacent trees at the ZF2 and Tapajós tropical forest research (near the cities of Manaus and Santarém). The temporal difference between the peak of g
(late morning) and the peak of VPD (early afternoon) is one of the major regulators of sap velocity hysteresis patterns. Sap velocity displayed species-specific diurnal hysteresis patterns reflected by changes in T
. In the morning, T
and sap velocity displayed a sigmoidal relationship. In the afternoon, stomatal conductance declined as T
approached a daily peak, allowing Ψ
to begin recovery, while sap velocity declined with an exponential relationship with T
. In Manaus, hysteresis indices of the variables T
-T
and Ψ
-T
were calculated for different species and a significant difference (
< 0.01, α = 0.05) was observed when the 2015 dry season (ENSO period) was compared with the 2017 dry season ("control scenario"). In some days during the 2015 ENSO event, T
approached 40°C for all studied species and the differences between T
and T
reached as high at 8°C (average difference: 1.65 ± 1.07°C). Generally, T
was higher than T
during the middle morning to early afternoon, and lower than T
during the early morning, late afternoon and night. Our results support the hypothesis that partial stomatal closure allows for a recovery in Ψ
during the afternoon period giving an observed counterclockwise hysteresis pattern between Ψ
and T
. |
---|---|
AbstractList | Current climate change scenarios indicate warmer temperatures and the potential for more extreme droughts in the tropics, such that a mechanistic understanding of the water cycle from individual trees to landscapes is needed to adequately predict future changes in forest structure and function. In this study, we contrasted physiological responses of tropical trees during a normal dry season with the extreme dry season due to the 2015–2016 El Niño-Southern Oscillation (ENSO) event. We quantified high resolution temporal dynamics of sap velocity (V
s
), stomatal conductance (g
s
) and leaf water potential (Ψ
L
) of multiple canopy trees, and their correlations with leaf temperature (T
leaf
) and environmental conditions [direct solar radiation, air temperature (T
air
) and vapor pressure deficit (VPD)]. The experiment leveraged canopy access towers to measure adjacent trees at the ZF2 and Tapajós tropical forest research (near the cities of Manaus and Santarém). The temporal difference between the peak of g
s
(late morning) and the peak of VPD (early afternoon) is one of the major regulators of sap velocity hysteresis patterns. Sap velocity displayed species-specific diurnal hysteresis patterns reflected by changes in T
leaf
. In the morning, T
leaf
and sap velocity displayed a sigmoidal relationship. In the afternoon, stomatal conductance declined as T
leaf
approached a daily peak, allowing Ψ
L
to begin recovery, while sap velocity declined with an exponential relationship with T
leaf
. In Manaus, hysteresis indices of the variables T
leaf
-T
air
and Ψ
L
-T
leaf
were calculated for different species and a significant difference (
p
< 0.01, α = 0.05) was observed when the 2015 dry season (ENSO period) was compared with the 2017 dry season (“control scenario”). In some days during the 2015 ENSO event, T
leaf
approached 40°C for all studied species and the differences between T
leaf
and T
air
reached as high at 8°C (average difference: 1.65 ± 1.07°C). Generally, T
leaf
was higher than T
air
during the middle morning to early afternoon, and lower than T
air
during the early morning, late afternoon and night. Our results support the hypothesis that partial stomatal closure allows for a recovery in Ψ
L
during the afternoon period giving an observed counterclockwise hysteresis pattern between Ψ
L
and T
leaf
. Current climate change scenarios indicate warmer temperatures and the potential for more extreme droughts in the tropics, such that a mechanistic understanding of the water cycle from individual trees to landscapes is needed to adequately predict future changes in forest structure and function. In this study, we contrasted physiological responses of tropical trees during a normal dry season with the extreme dry season due to the 2015–2016 El Niño-Southern Oscillation (ENSO) event. We quantified high resolution temporal dynamics of sap velocity (Vs), stomatal conductance (gs) and leaf water potential (ΨL) of multiple canopy trees, and their correlations with leaf temperature (Tleaf) and environmental conditions [direct solar radiation, air temperature (Tair) and vapor pressure deficit (VPD)]. The experiment leveraged canopy access towers to measure adjacent trees at the ZF2 and Tapajós tropical forest research (near the cities of Manaus and Santarém). The temporal difference between the peak of gs (late morning) and the peak of VPD (early afternoon) is one of the major regulators of sap velocity hysteresis patterns. Sap velocity displayed species-specific diurnal hysteresis patterns reflected by changes in Tleaf. In the morning, Tleaf and sap velocity displayed a sigmoidal relationship. In the afternoon, stomatal conductance declined as Tleaf approached a daily peak, allowing ΨL to begin recovery, while sap velocity declined with an exponential relationship with Tleaf. In Manaus, hysteresis indices of the variables Tleaf-Tair and ΨL-Tleaf were calculated for different species and a significant difference (p < 0.01, α = 0.05) was observed when the 2015 dry season (ENSO period) was compared with the 2017 dry season (“control scenario”). In some days during the 2015 ENSO event, Tleaf approached 40°C for all studied species and the differences between Tleaf and Tair reached as high at 8°C (average difference: 1.65 ± 1.07°C). Generally, Tleaf was higher than Tair during the middle morning to early afternoon, and lower than Tair during the early morning, late afternoon and night. Our results support the hypothesis that partial stomatal closure allows for a recovery in ΨL during the afternoon period giving an observed counterclockwise hysteresis pattern between ΨL and Tleaf. Current climate change scenarios indicate warmer temperatures and the potential for more extreme droughts in the tropics, such that a mechanistic understanding of the water cycle from individual trees to landscapes is needed to adequately predict future changes in forest structure and function. In this study, we contrasted physiological responses of tropical trees during a normal dry season with the extreme dry season due to the 2015-2016 El Niño-Southern Oscillation (ENSO) event. We quantified high resolution temporal dynamics of sap velocity (Vs), stomatal conductance (gs) and leaf water potential (ΨL) of multiple canopy trees, and their correlations with leaf temperature (Tleaf) and environmental conditions [direct solar radiation, air temperature (Tair) and vapor pressure deficit (VPD)]. The experiment leveraged canopy access towers to measure adjacent trees at the ZF2 and Tapajós tropical forest research (near the cities of Manaus and Santarém). The temporal difference between the peak of gs (late morning) and the peak of VPD (early afternoon) is one of the major regulators of sap velocity hysteresis patterns. Sap velocity displayed species-specific diurnal hysteresis patterns reflected by changes in Tleaf. In the morning, Tleaf and sap velocity displayed a sigmoidal relationship. In the afternoon, stomatal conductance declined as Tleaf approached a daily peak, allowing ΨL to begin recovery, while sap velocity declined with an exponential relationship with Tleaf. In Manaus, hysteresis indices of the variables Tleaf-Tair and ΨL-Tleaf were calculated for different species and a significant difference (p < 0.01, α = 0.05) was observed when the 2015 dry season (ENSO period) was compared with the 2017 dry season ("control scenario"). In some days during the 2015 ENSO event, Tleaf approached 40°C for all studied species and the differences between Tleaf and Tair reached as high at 8°C (average difference: 1.65 ± 1.07°C). Generally, Tleaf was higher than Tair during the middle morning to early afternoon, and lower than Tair during the early morning, late afternoon and night. Our results support the hypothesis that partial stomatal closure allows for a recovery in ΨL during the afternoon period giving an observed counterclockwise hysteresis pattern between ΨL and Tleaf.Current climate change scenarios indicate warmer temperatures and the potential for more extreme droughts in the tropics, such that a mechanistic understanding of the water cycle from individual trees to landscapes is needed to adequately predict future changes in forest structure and function. In this study, we contrasted physiological responses of tropical trees during a normal dry season with the extreme dry season due to the 2015-2016 El Niño-Southern Oscillation (ENSO) event. We quantified high resolution temporal dynamics of sap velocity (Vs), stomatal conductance (gs) and leaf water potential (ΨL) of multiple canopy trees, and their correlations with leaf temperature (Tleaf) and environmental conditions [direct solar radiation, air temperature (Tair) and vapor pressure deficit (VPD)]. The experiment leveraged canopy access towers to measure adjacent trees at the ZF2 and Tapajós tropical forest research (near the cities of Manaus and Santarém). The temporal difference between the peak of gs (late morning) and the peak of VPD (early afternoon) is one of the major regulators of sap velocity hysteresis patterns. Sap velocity displayed species-specific diurnal hysteresis patterns reflected by changes in Tleaf. In the morning, Tleaf and sap velocity displayed a sigmoidal relationship. In the afternoon, stomatal conductance declined as Tleaf approached a daily peak, allowing ΨL to begin recovery, while sap velocity declined with an exponential relationship with Tleaf. In Manaus, hysteresis indices of the variables Tleaf-Tair and ΨL-Tleaf were calculated for different species and a significant difference (p < 0.01, α = 0.05) was observed when the 2015 dry season (ENSO period) was compared with the 2017 dry season ("control scenario"). In some days during the 2015 ENSO event, Tleaf approached 40°C for all studied species and the differences between Tleaf and Tair reached as high at 8°C (average difference: 1.65 ± 1.07°C). Generally, Tleaf was higher than Tair during the middle morning to early afternoon, and lower than Tair during the early morning, late afternoon and night. Our results support the hypothesis that partial stomatal closure allows for a recovery in ΨL during the afternoon period giving an observed counterclockwise hysteresis pattern between ΨL and Tleaf. Current climate change scenarios indicate warmer temperatures and the potential for more extreme droughts in the tropics, such that a mechanistic understanding of the water cycle from individual trees to landscapes is needed to adequately predict future changes in forest structure and function. In this study, we contrasted physiological responses of tropical trees during a normal dry season with the extreme dry season due to the 2015-2016 El Niño-Southern Oscillation (ENSO) event. We quantified high resolution temporal dynamics of sap velocity (V ), stomatal conductance (g ) and leaf water potential (Ψ ) of multiple canopy trees, and their correlations with leaf temperature (T ) and environmental conditions [direct solar radiation, air temperature (T ) and vapor pressure deficit (VPD)]. The experiment leveraged canopy access towers to measure adjacent trees at the ZF2 and Tapajós tropical forest research (near the cities of Manaus and Santarém). The temporal difference between the peak of g (late morning) and the peak of VPD (early afternoon) is one of the major regulators of sap velocity hysteresis patterns. Sap velocity displayed species-specific diurnal hysteresis patterns reflected by changes in T . In the morning, T and sap velocity displayed a sigmoidal relationship. In the afternoon, stomatal conductance declined as T approached a daily peak, allowing Ψ to begin recovery, while sap velocity declined with an exponential relationship with T . In Manaus, hysteresis indices of the variables T -T and Ψ -T were calculated for different species and a significant difference ( < 0.01, α = 0.05) was observed when the 2015 dry season (ENSO period) was compared with the 2017 dry season ("control scenario"). In some days during the 2015 ENSO event, T approached 40°C for all studied species and the differences between T and T reached as high at 8°C (average difference: 1.65 ± 1.07°C). Generally, T was higher than T during the middle morning to early afternoon, and lower than T during the early morning, late afternoon and night. Our results support the hypothesis that partial stomatal closure allows for a recovery in Ψ during the afternoon period giving an observed counterclockwise hysteresis pattern between Ψ and T . |
Author | Sampaio-Filho, Israel de Jesus Cobello, Leticia O. Higuchi, Niro Newman, Brent D. Koven, Charles D. Negrón-Juárez, Robinson I. Chambers, Jeffrey Q. Dawson, Todd E. McDowell, Nate G. Gimenez, Bruno O. Varadharajan, Charuleka Holm, Jennifer A. Araújo, Alessandro C. Spanner, Gustavo C. Jardine, Kolby J. Fontes, Clarissa G. Christianson, Danielle S. Warren, Jeffrey M. |
AuthorAffiliation | 3 Department of Integrative Biology, University of California, Berkeley , Berkeley, CA , United States 4 Embrapa Amazônia Oriental , Belém , Brazil 6 Earth and Environmental Sciences Division, Los Alamos National Laboratory , Los Alamos, NM , United States 7 Pacific Northwest National Laboratory , Richland, WA , United States 1 National Institute of Amazonian Research (INPA) , Manaus , Brazil 8 Department of Geography, University of California, Berkeley , Berkeley, CA , United States 2 Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory , Berkeley, CA , United States 5 Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory , Oak Ridge, TN , United States |
AuthorAffiliation_xml | – name: 8 Department of Geography, University of California, Berkeley , Berkeley, CA , United States – name: 5 Environmental Sciences Division and Climate Change Science Institute, Oak Ridge National Laboratory , Oak Ridge, TN , United States – name: 4 Embrapa Amazônia Oriental , Belém , Brazil – name: 7 Pacific Northwest National Laboratory , Richland, WA , United States – name: 2 Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory , Berkeley, CA , United States – name: 6 Earth and Environmental Sciences Division, Los Alamos National Laboratory , Los Alamos, NM , United States – name: 3 Department of Integrative Biology, University of California, Berkeley , Berkeley, CA , United States – name: 1 National Institute of Amazonian Research (INPA) , Manaus , Brazil |
Author_xml | – sequence: 1 givenname: Bruno O. surname: Gimenez fullname: Gimenez, Bruno O. – sequence: 2 givenname: Kolby J. surname: Jardine fullname: Jardine, Kolby J. – sequence: 3 givenname: Niro surname: Higuchi fullname: Higuchi, Niro – sequence: 4 givenname: Robinson I. surname: Negrón-Juárez fullname: Negrón-Juárez, Robinson I. – sequence: 5 givenname: Israel de Jesus surname: Sampaio-Filho fullname: Sampaio-Filho, Israel de Jesus – sequence: 6 givenname: Leticia O. surname: Cobello fullname: Cobello, Leticia O. – sequence: 7 givenname: Clarissa G. surname: Fontes fullname: Fontes, Clarissa G. – sequence: 8 givenname: Todd E. surname: Dawson fullname: Dawson, Todd E. – sequence: 9 givenname: Charuleka surname: Varadharajan fullname: Varadharajan, Charuleka – sequence: 10 givenname: Danielle S. surname: Christianson fullname: Christianson, Danielle S. – sequence: 11 givenname: Gustavo C. surname: Spanner fullname: Spanner, Gustavo C. – sequence: 12 givenname: Alessandro C. surname: Araújo fullname: Araújo, Alessandro C. – sequence: 13 givenname: Jeffrey M. surname: Warren fullname: Warren, Jeffrey M. – sequence: 14 givenname: Brent D. surname: Newman fullname: Newman, Brent D. – sequence: 15 givenname: Jennifer A. surname: Holm fullname: Holm, Jennifer A. – sequence: 16 givenname: Charles D. surname: Koven fullname: Koven, Charles D. – sequence: 17 givenname: Nate G. surname: McDowell fullname: McDowell, Nate G. – sequence: 18 givenname: Jeffrey Q. surname: Chambers fullname: Chambers, Jeffrey Q. |
BackLink | https://www.ncbi.nlm.nih.gov/pubmed/31316536$$D View this record in MEDLINE/PubMed https://www.osti.gov/biblio/1530001$$D View this record in Osti.gov |
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ContentType | Journal Article |
Copyright | Copyright © 2019 Gimenez, Jardine, Higuchi, Negrón-Juárez, Sampaio-Filho, Cobello, Fontes, Dawson, Varadharajan, Christianson, Spanner, Araújo, Warren, Newman, Holm, Koven, McDowell and Chambers. 2019 Gimenez, Jardine, Higuchi, Negrón-Juárez, Sampaio-Filho, Cobello, Fontes, Dawson, Varadharajan, Christianson, Spanner, Araújo, Warren, Newman, Holm, Koven, McDowell and Chambers |
Copyright_xml | – notice: Copyright © 2019 Gimenez, Jardine, Higuchi, Negrón-Juárez, Sampaio-Filho, Cobello, Fontes, Dawson, Varadharajan, Christianson, Spanner, Araújo, Warren, Newman, Holm, Koven, McDowell and Chambers. 2019 Gimenez, Jardine, Higuchi, Negrón-Juárez, Sampaio-Filho, Cobello, Fontes, Dawson, Varadharajan, Christianson, Spanner, Araújo, Warren, Newman, Holm, Koven, McDowell and Chambers |
CorporateAuthor | Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States) Pacific Northwest National Laboratory (PNNL), Richland, WA (United States) Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States) |
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Keywords | sap velocity stomatal conductance direct solar radiation tropical forests vapor pressure deficit leaf temperature hysteresis |
Language | English |
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SubjectTerms | BASIC BIOLOGICAL SCIENCES direct solar radiation ENVIRONMENTAL SCIENCES hysteresis leaf temperature Plant Science sap velocity stomatal conductance tropical forests tropical forests, sap velocity, stomatal conductance, direct solar radiation, vapor pressure deficit, leaf temperature vapor pressure deficit |
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Title | Species-Specific Shifts in Diurnal Sap Velocity Dynamics and Hysteretic Behavior of Ecophysiological Variables During the 2015–2016 El Niño Event in the Amazon Forest |
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