Pattern of xylem phenology in conifers of cold ecosystems at the Northern Hemisphere

© 2016 John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 22(2016), 11 vom: 06. Nov., Seite 3804-3813
1. Verfasser: Rossi, Sergio (VerfasserIn)
Weitere Verfasser: Anfodillo, Tommaso, Čufar, Katarina, Cuny, Henri E, Deslauriers, Annie, Fonti, Patrick, Frank, David, Gričar, Jožica, Gruber, Andreas, Huang, Jian-Guo, Jyske, Tuula, Kašpar, Jakub, King, Gregory, Krause, Cornelia, Liang, Eryuan, Mäkinen, Harri, Morin, Hubert, Nöjd, Pekka, Oberhuber, Walter, Prislan, Peter, Rathgeber, Cyrille B K, Saracino, Antonio, Swidrak, Irene, Treml, Václav
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2016
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article cambium cell differentiation cell production climate change conifers growth meristem secondary wall formation
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245 1 0 |a Pattern of xylem phenology in conifers of cold ecosystems at the Northern Hemisphere 
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520 |a The interaction between xylem phenology and climate assesses forest growth and productivity and carbon storage across biomes under changing environmental conditions. We tested the hypothesis that patterns of wood formation are maintained unaltered despite the temperature changes across cold ecosystems. Wood microcores were collected weekly or biweekly throughout the growing season for periods varying between 1 and 13 years during 1998-2014 and cut in transverse sections for assessing the onset and ending of the phases of xylem differentiation. The data set represented 1321 trees belonging to 10 conifer species from 39 sites in the Northern Hemisphere and covering an interval of mean annual temperature exceeding 14 K. The phenological events and mean annual temperature of the sites were related linearly, with spring and autumnal events being separated by constant intervals across the range of temperature analysed. At increasing temperature, first enlarging, wall-thickening and mature tracheids appeared earlier, and last enlarging and wall-thickening tracheids occurred later. Overall, the period of wood formation lengthened linearly with the mean annual temperature, from 83.7 days at -2 °C to 178.1 days at 12 °C, at a rate of 6.5 days °C-1 . April-May temperatures produced the best models predicting the dates of wood formation. Our findings demonstrated the uniformity of the process of wood formation and the importance of the environmental conditions occurring at the time of growth resumption. Under warming scenarios, the period of wood formation might lengthen synchronously in the cold biomes of the Northern Hemisphere 
650 4 |a Journal Article 
650 4 |a cambium 
650 4 |a cell differentiation 
650 4 |a cell production 
650 4 |a climate change 
650 4 |a conifers 
650 4 |a growth 
650 4 |a meristem 
650 4 |a secondary wall formation 
700 1 |a Anfodillo, Tommaso  |e verfasserin  |4 aut 
700 1 |a Čufar, Katarina  |e verfasserin  |4 aut 
700 1 |a Cuny, Henri E  |e verfasserin  |4 aut 
700 1 |a Deslauriers, Annie  |e verfasserin  |4 aut 
700 1 |a Fonti, Patrick  |e verfasserin  |4 aut 
700 1 |a Frank, David  |e verfasserin  |4 aut 
700 1 |a Gričar, Jožica  |e verfasserin  |4 aut 
700 1 |a Gruber, Andreas  |e verfasserin  |4 aut 
700 1 |a Huang, Jian-Guo  |e verfasserin  |4 aut 
700 1 |a Jyske, Tuula  |e verfasserin  |4 aut 
700 1 |a Kašpar, Jakub  |e verfasserin  |4 aut 
700 1 |a King, Gregory  |e verfasserin  |4 aut 
700 1 |a Krause, Cornelia  |e verfasserin  |4 aut 
700 1 |a Liang, Eryuan  |e verfasserin  |4 aut 
700 1 |a Mäkinen, Harri  |e verfasserin  |4 aut 
700 1 |a Morin, Hubert  |e verfasserin  |4 aut 
700 1 |a Nöjd, Pekka  |e verfasserin  |4 aut 
700 1 |a Oberhuber, Walter  |e verfasserin  |4 aut 
700 1 |a Prislan, Peter  |e verfasserin  |4 aut 
700 1 |a Rathgeber, Cyrille B K  |e verfasserin  |4 aut 
700 1 |a Saracino, Antonio  |e verfasserin  |4 aut 
700 1 |a Swidrak, Irene  |e verfasserin  |4 aut 
700 1 |a Treml, Václav  |e verfasserin  |4 aut 
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