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Photoperiod and temperature as dominant environmental drivers triggering secondary growth resumption in Northern Hemisphere conifers.
Huang, Jian-Guo; Ma, Qianqian; Rossi, Sergio; Biondi, Franco; Deslauriers, Annie; Fonti, Patrick; Liang, Eryuan; Mäkinen, Harri; Oberhuber, Walter; Rathgeber, Cyrille B K; Tognetti, Roberto; Treml, Václav; Yang, Bao; Zhang, Jiao-Lin; Antonucci, Serena; Bergeron, Yves; Camarero, J Julio; Campelo, Filipe; Cufar, Katarina; Cuny, Henri E; De Luis, Martin; Giovannelli, Alessio; Gricar, Jozica; Gruber, Andreas; Gryc, Vladimír; Güney, Aylin; Guo, Xiali; Huang, Wei; Jyske, Tuula; Kaspar, Jakub; King, Gregory; Krause, Cornelia; Lemay, Audrey; Liu, Feng; Lombardi, Fabio; Martinez Del Castillo, Edurne; Morin, Hubert; Nabais, Cristina; Nöjd, Pekka; Peters, Richard L; Prislan, Peter; Saracino, Antonio; Swidrak, Irene; Vavrcík, Hanus; Vieira, Joana; Yu, Biyun; Zhang, Shaokang; Zeng, Qiao; Zhang, Yaling; Ziaco, Emanuele.
Afiliación
  • Huang JG; Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China; huangjg@scbg.ac.cn.
  • Ma Q; Center of Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou 510650, China.
  • Rossi S; Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China.
  • Biondi F; Center of Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou 510650, China.
  • Deslauriers A; Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China.
  • Fonti P; Département des Sciences Fondamentales, Université du Québec à Chicoutimi, Chicoutimi, QC G7H 2B1, Canada.
  • Liang E; DendroLab, Department of Natural Resources and Environmental Science, University of Nevada, Reno, NV 89557.
  • Mäkinen H; Département des Sciences Fondamentales, Université du Québec à Chicoutimi, Chicoutimi, QC G7H 2B1, Canada.
  • Oberhuber W; Dendrosciences, Swiss Federal Research Institute for Forest, Snow and Landscape, CH-8903 Birmensdorf, Switzerland.
  • Rathgeber CBK; Key Laboratory of Alpine Ecology and Biodiversity, Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China.
  • Tognetti R; Department of Forests, Natural Resources Institute Finland, 02150 Espoo, Finland.
  • Treml V; Department of Botany, Leopold-Franzens University of Innsbruck, 6020 Innsbruck, Austria.
  • Yang B; AgroParisTech, Institut National de Recherche pour l'Agriculture, l'Alimentation et l'Environnement, Université de Lorraine, Silva, F-54000 Nancy, France.
  • Zhang JL; Dipartimento di Agricoltura, Ambiente e Alimenti, Università degli Studi del Molise, 86100 Campobasso, Italy.
  • Antonucci S; Department of Physical Geography and Geoecology, Charles University, CZ-12843 Prague, Czech Republic.
  • Bergeron Y; Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China.
  • Camarero JJ; Center of Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou 510650, China.
  • Campelo F; Chinese Academy of Sciences Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, Yunnan 666303, China.
  • Cufar K; Dipartimento di Agricoltura, Ambiente e Alimenti, Università degli Studi del Molise, 86100 Campobasso, Italy.
  • Cuny HE; Forest Research Institute, Université du Quebec en Abitibi-Témiscamingue, Rouyn-Noranda, QC J9X5E4, Canada.
  • De Luis M; Instituto Pirenaico de Ecología, Consejo Superior de Investigaciones Científicas, 50192 Zaragoza, Spain.
  • Giovannelli A; Centre for Functional Ecology, Department of Life Sciences, University of Coimbra, 3000-456 Coimbra, Portugal.
  • Gricar J; Biotechnical Faculty, University of Ljubljana, 1000 Ljubljana, Slovenia.
  • Gruber A; Department of Forest and Carbon Resources, Institut National de Information Géographique et Forestière (IGN), 54250 Champigneulles, France.
  • Gryc V; Department of Geography and Regional Planning, Environmental Science Institute, University of Zaragoza, 50009 Zaragoza, Spain.
  • Güney A; Istituto di Ricerca sugli Ecosistemi Terrestri, Consiglio Nazionale delle Ricerche, 50019 Sesto Fiorentino, Italy.
  • Guo X; Laboratory for Dendrochronology, Slovenian Forestry Institute, 1000 Ljubljana, Slovenia.
  • Huang W; Department of Botany, Leopold-Franzens University of Innsbruck, 6020 Innsbruck, Austria.
  • Jyske T; Department of Wood Science and Wood Technology, Mendel University in Brno, 61300 Brno, Czech Republic.
  • Kaspar J; Institute of Botany, University of Hohenheim, 70593 Stuttgart, Germany.
  • King G; Department of Biology, Southwest Anatolia Forest Research Institute, 07010 Antalya, Turkey.
  • Krause C; Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou 510650, China.
  • Lemay A; Center of Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou 510650, China.
  • Liu F; State Key Laboratory for Conservation and Utilization of Subtropical Agro-bioresources, College of Life Sciences, South China Agricultural University, Guangzhou 510642, China.
  • Lombardi F; Department of Forests, Natural Resources Institute Finland, 02150 Espoo, Finland.
  • Martinez Del Castillo E; Department of Physical Geography and Geoecology, Charles University, CZ-12843 Prague, Czech Republic.
  • Morin H; Dendrosciences, Swiss Federal Research Institute for Forest, Snow and Landscape, CH-8903 Birmensdorf, Switzerland.
  • Nabais C; Department of Sciences, University of Alberta, Camrose, AB T4V 2R3, Canada.
  • Nöjd P; Département des Sciences Fondamentales, Université du Québec à Chicoutimi, Chicoutimi, QC G7H 2B1, Canada.
  • Peters RL; Département des Sciences Fondamentales, Université du Québec à Chicoutimi, Chicoutimi, QC G7H 2B1, Canada.
  • Prislan P; Center of Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou 510650, China.
  • Saracino A; Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan 430074, China.
  • Swidrak I; Dipartimento di Agraria, Università Mediterranea di Reggio Calabria, 89122 Reggio Calabria, Italy.
  • Vavrcík H; Department of Geography and Regional Planning, Environmental Science Institute, University of Zaragoza, 50009 Zaragoza, Spain.
  • Vieira J; Département des Sciences Fondamentales, Université du Québec à Chicoutimi, Chicoutimi, QC G7H 2B1, Canada.
  • Yu B; Centre for Functional Ecology, Department of Life Sciences, University of Coimbra, 3000-456 Coimbra, Portugal.
  • Zhang S; Department of Forests, Natural Resources Institute Finland, 02150 Espoo, Finland.
  • Zeng Q; Dendrosciences, Swiss Federal Research Institute for Forest, Snow and Landscape, CH-8903 Birmensdorf, Switzerland.
  • Zhang Y; Laboratory of Plant Ecology, Department of Plants and Crops, Faculty of Bioscience Engineering, Ghent University, B-9000 Ghent, Belgium.
  • Ziaco E; Biotechnical Faculty, University of Ljubljana, 1000 Ljubljana, Slovenia.
Proc Natl Acad Sci U S A ; 117(34): 20645-20652, 2020 08 25.
Article en En | MEDLINE | ID: mdl-32759218
ABSTRACT
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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Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Asunto principal: Madera / Xilema / Tracheophyta Tipo de estudio: Prognostic_studies Idioma: En Revista: Proc Natl Acad Sci U S A Año: 2020 Tipo del documento: Article

Texto completo: 1 Colección: 01-internacional Banco de datos: MEDLINE Asunto principal: Madera / Xilema / Tracheophyta Tipo de estudio: Prognostic_studies Idioma: En Revista: Proc Natl Acad Sci U S A Año: 2020 Tipo del documento: Article