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Photoperiod and temperature as dominant environmental drivers triggering secondary growth resumption in Northern Hemisphere conifers
JG. Huang, Q. Ma, S. Rossi, F. Biondi, A. Deslauriers, P. Fonti, E. Liang, H. Mäkinen, W. Oberhuber, CBK. Rathgeber, R. Tognetti, V. Treml, B. Yang, JL. Zhang, S. Antonucci, Y. Bergeron, JJ. Camarero, F. Campelo, K. Čufar, HE. Cuny, M. De Luis,...
Jazyk angličtina Země Spojené státy americké
Typ dokumentu časopisecké články, práce podpořená grantem, Research Support, U.S. Gov't, Non-P.H.S.
NLK
Free Medical Journals
od 1915 do Před 6 měsíci
Freely Accessible Science Journals
od 1915 do Před 6 měsíci
PubMed Central
od 1915 do Před 6 měsíci
Europe PubMed Central
od 1915 do Před 6 měsíci
Open Access Digital Library
od 1915-01-15
Open Access Digital Library
od 1915-01-01
PubMed
32759218
DOI
10.1073/pnas.2007058117
Knihovny.cz E-zdroje
- MeSH
- biologické modely MeSH
- cévnaté rostliny genetika růst a vývoj MeSH
- dřevo růst a vývoj MeSH
- ekosystém MeSH
- fotoperioda MeSH
- globální oteplování MeSH
- klimatické změny MeSH
- lesy MeSH
- podnebí MeSH
- roční období MeSH
- stromy růst a vývoj MeSH
- teplota MeSH
- xylém růst a vývoj MeSH
- Publikační typ
- časopisecké články MeSH
- práce podpořená grantem MeSH
- Research Support, U.S. Gov't, Non-P.H.S. MeSH
Wood formation consumes around 15% of the anthropogenic CO2 emissions per year and plays a critical role in long-term sequestration of carbon on Earth. However, the exogenous factors driving wood formation onset and the underlying cellular mechanisms are still poorly understood and quantified, and this hampers an effective assessment of terrestrial forest productivity and carbon budget under global warming. Here, we used an extensive collection of unique datasets of weekly xylem tissue formation (wood formation) from 21 coniferous species across the Northern Hemisphere (latitudes 23 to 67°N) to present a quantitative demonstration that the onset of wood formation in Northern Hemisphere conifers is primarily driven by photoperiod and mean annual temperature (MAT), and only secondarily by spring forcing, winter chilling, and moisture availability. Photoperiod interacts with MAT and plays the dominant role in regulating the onset of secondary meristem growth, contrary to its as-yet-unquantified role in affecting the springtime phenology of primary meristems. The unique relationships between exogenous factors and wood formation could help to predict how forest ecosystems respond and adapt to climate warming and could provide a better understanding of the feedback occurring between vegetation and climate that is mediated by phenology. Our study quantifies the role of major environmental drivers for incorporation into state-of-the-art Earth system models (ESMs), thereby providing an improved assessment of long-term and high-resolution observations of biogeochemical cycles across terrestrial biomes.
Biotechnical Faculty University of Ljubljana 1000 Ljubljana Slovenia
Center of Plant Ecology Core Botanical Gardens Chinese Academy of Sciences Guangzhou 510650 China
Department of Agricultural Sciences University of Naples Federico 2 1 80055 Portici Napoli Italy
Department of Botany Leopold Franzens University of Innsbruck 6020 Innsbruck Austria
Department of Forests Natural Resources Institute Finland 02150 Espoo Finland
Department of Physical Geography and Geoecology Charles University CZ 12843 Prague Czech Republic
Department of Wood Science and Wood Technology Mendel University in Brno 61300 Brno Czech Republic
Dipartimento di Agraria Università Mediterranea di Reggio Calabria 89122 Reggio Calabria Italy
Instituto Pirenaico de Ecología Consejo Superior de Investigaciones Científicas 50192 Zaragoza Spain
Laboratory for Dendrochronology Slovenian Forestry Institute 1000 Ljubljana Slovenia
Citace poskytuje Crossref.org
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- $a Photoperiod and temperature as dominant environmental drivers triggering secondary growth resumption in Northern Hemisphere conifers / $c JG. Huang, Q. Ma, S. Rossi, F. Biondi, A. Deslauriers, P. Fonti, E. Liang, H. Mäkinen, W. Oberhuber, CBK. Rathgeber, R. Tognetti, V. Treml, B. Yang, JL. Zhang, S. Antonucci, Y. Bergeron, JJ. Camarero, F. Campelo, K. Čufar, HE. Cuny, M. De Luis, A. Giovannelli, J. Gričar, A. Gruber, V. Gryc, A. Güney, X. Guo, W. Huang, T. Jyske, J. Kašpar, G. King, C. Krause, A. Lemay, F. Liu, F. Lombardi, E. Martinez Del Castillo, H. Morin, C. Nabais, P. Nöjd, RL. Peters, P. Prislan, A. Saracino, I. Swidrak, H. Vavrčík, J. Vieira, B. Yu, S. Zhang, Q. Zeng, Y. Zhang, E. Ziaco,
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- $a Wood formation consumes around 15% of the anthropogenic CO2 emissions per year and plays a critical role in long-term sequestration of carbon on Earth. However, the exogenous factors driving wood formation onset and the underlying cellular mechanisms are still poorly understood and quantified, and this hampers an effective assessment of terrestrial forest productivity and carbon budget under global warming. Here, we used an extensive collection of unique datasets of weekly xylem tissue formation (wood formation) from 21 coniferous species across the Northern Hemisphere (latitudes 23 to 67°N) to present a quantitative demonstration that the onset of wood formation in Northern Hemisphere conifers is primarily driven by photoperiod and mean annual temperature (MAT), and only secondarily by spring forcing, winter chilling, and moisture availability. Photoperiod interacts with MAT and plays the dominant role in regulating the onset of secondary meristem growth, contrary to its as-yet-unquantified role in affecting the springtime phenology of primary meristems. The unique relationships between exogenous factors and wood formation could help to predict how forest ecosystems respond and adapt to climate warming and could provide a better understanding of the feedback occurring between vegetation and climate that is mediated by phenology. Our study quantifies the role of major environmental drivers for incorporation into state-of-the-art Earth system models (ESMs), thereby providing an improved assessment of long-term and high-resolution observations of biogeochemical cycles across terrestrial biomes.
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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- 700 1_
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