Climate sensitivity of radial growth in Norway spruce (Picea abies (L.) Karst.) under different CO2 concentrations

This investigation examined the effects of two different carbon dioxide concentrations ([CO2]): Ambient (A, 385 μmol (CO2) mol−1) and elevated (E, A+385 μmol (CO2) mol−1)) on the tree-ring width and early to latewood proportion in Norway spruce for seven years (2006-2012). Further, to improve our un...

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Main Authors: Badraghi Aysan, Pokorný Radek, Novosadová Kateřina, Pietras Justina, Marek Michal V.
Format: Article
Language:English
Published: Sciendo 2016-12-01
Series:Metsanduslikud Uurimused
Subjects:
Online Access:https://doi.org/10.1515/fsmu-2016-0011
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author Badraghi Aysan
Pokorný Radek
Novosadová Kateřina
Pietras Justina
Marek Michal V.
author_facet Badraghi Aysan
Pokorný Radek
Novosadová Kateřina
Pietras Justina
Marek Michal V.
author_sort Badraghi Aysan
collection DOAJ
description This investigation examined the effects of two different carbon dioxide concentrations ([CO2]): Ambient (A, 385 μmol (CO2) mol−1) and elevated (E, A+385 μmol (CO2) mol−1)) on the tree-ring width and early to latewood proportion in Norway spruce for seven years (2006-2012). Further, to improve our understanding of the influence of climatic variables, we assessed the effects of precipitation and temperature. Our observations showed that spruce trees growing under elevated CO2 (EC) formed less early (p > 0.05) and latewood (p < 0.05) and hence smaller annual increments (p > 0.05) than trees in ambient CO2 (AC). Early to latewood proportion was nearly 73% and 75% in AC and EC, respectively. In both CO2 concentrations, the largest tree-rings and earlywood width was observed during 2009 and 2010, which is coincident with the highest precipitation in May (2010) and the highest air temperature in April (2009). Moreover, to determine the association between the latewood formation and air temperature during the second half of the growing season, and correlation between the earlywood formation and precipitation during the first half of the growing season we run Spearman’s correlation test, the determination coefficient values for latewood formation were r = 0.45 (AC) and r = 0.68 (EC), and for earlywood formation were r = 0.53 (AC) and r = 0.42 (EC), although coefficient values were not statistically significant (p > 0.05). Also, our study indicated that temperature had stonger influence than precipitation in EC, but in AC precipitation had the strongest effect on radial growth.
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spelling doaj.art-e3a8561604b7407e84e3d284337499762022-12-21T23:56:03ZengSciendoMetsanduslikud Uurimused1736-87232016-12-01651435610.1515/fsmu-2016-0011Climate sensitivity of radial growth in Norway spruce (Picea abies (L.) Karst.) under different CO2 concentrationsBadraghi Aysan0Pokorný Radek1Novosadová Kateřina2Pietras Justina3Marek Michal V.4Department of Biomass and Water Regime, Global Change Research Centre, Academy of Science of the Czech Republic, Belidla 986/4a, CZ 60300, Brno, Czech Republic CzechiaDepartment of Biomass and Water Regime, Global Change Research Centre, Academy of Science of the Czech Republic, Belidla 986/4a, CZ 60300, Brno, Czech Republic CzechiaDepartment of Biomass and Water Regime, Global Change Research Centre, Academy of Science of the Czech Republic, Belidla 986/4a, CZ 60300, Brno, Czech Republic CzechiaDepartment of Biomass and Water Regime, Global Change Research Centre, Academy of Science of the Czech Republic, Belidla 986/4a, CZ 60300, Brno, Czech Republic CzechiaDepartment of Biomass and Water Regime, Global Change Research Centre, Academy of Science of the Czech Republic, Belidla 986/4a, CZ 60300, Brno, Czech Republic CzechiaThis investigation examined the effects of two different carbon dioxide concentrations ([CO2]): Ambient (A, 385 μmol (CO2) mol−1) and elevated (E, A+385 μmol (CO2) mol−1)) on the tree-ring width and early to latewood proportion in Norway spruce for seven years (2006-2012). Further, to improve our understanding of the influence of climatic variables, we assessed the effects of precipitation and temperature. Our observations showed that spruce trees growing under elevated CO2 (EC) formed less early (p > 0.05) and latewood (p < 0.05) and hence smaller annual increments (p > 0.05) than trees in ambient CO2 (AC). Early to latewood proportion was nearly 73% and 75% in AC and EC, respectively. In both CO2 concentrations, the largest tree-rings and earlywood width was observed during 2009 and 2010, which is coincident with the highest precipitation in May (2010) and the highest air temperature in April (2009). Moreover, to determine the association between the latewood formation and air temperature during the second half of the growing season, and correlation between the earlywood formation and precipitation during the first half of the growing season we run Spearman’s correlation test, the determination coefficient values for latewood formation were r = 0.45 (AC) and r = 0.68 (EC), and for earlywood formation were r = 0.53 (AC) and r = 0.42 (EC), although coefficient values were not statistically significant (p > 0.05). Also, our study indicated that temperature had stonger influence than precipitation in EC, but in AC precipitation had the strongest effect on radial growth.https://doi.org/10.1515/fsmu-2016-0011ambient co2elevated co2wood formationradial incrementcarbon relationsconifers
spellingShingle Badraghi Aysan
Pokorný Radek
Novosadová Kateřina
Pietras Justina
Marek Michal V.
Climate sensitivity of radial growth in Norway spruce (Picea abies (L.) Karst.) under different CO2 concentrations
Metsanduslikud Uurimused
ambient co2
elevated co2
wood formation
radial increment
carbon relations
conifers
title Climate sensitivity of radial growth in Norway spruce (Picea abies (L.) Karst.) under different CO2 concentrations
title_full Climate sensitivity of radial growth in Norway spruce (Picea abies (L.) Karst.) under different CO2 concentrations
title_fullStr Climate sensitivity of radial growth in Norway spruce (Picea abies (L.) Karst.) under different CO2 concentrations
title_full_unstemmed Climate sensitivity of radial growth in Norway spruce (Picea abies (L.) Karst.) under different CO2 concentrations
title_short Climate sensitivity of radial growth in Norway spruce (Picea abies (L.) Karst.) under different CO2 concentrations
title_sort climate sensitivity of radial growth in norway spruce picea abies l karst under different co2 concentrations
topic ambient co2
elevated co2
wood formation
radial increment
carbon relations
conifers
url https://doi.org/10.1515/fsmu-2016-0011
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