TY - JOUR
T1 - Woody biomass production lags stem-girth increase by over one month in coniferous forests
AU - Cuny, Henri E.
AU - Rathgeber, Cyrille B.K.
AU - Frank, David
AU - Fonti, Patrick
AU - Makinen, Harri
AU - Prislan, Peter
AU - Rossi, Sergio
AU - Del Castillo, Edurne Martinez
AU - Campelo, Filipe
AU - Vavrčík, Hanuš
AU - Camarero, Jesus Julio
AU - Bryukhanova, Marina V.
AU - Jyske, Tuula
AU - Gricar, Jozica
AU - Gryc, Vladimir
AU - De Luis, Martin
AU - Vieira, Joana
AU - Cufar, Katarina
AU - Kirdyanov, Alexander V.
AU - Oberhuber, Walter
AU - Treml, Vaclav
AU - Huang, Jian Guo
AU - Li, Xiaoxia
AU - Swidrak, Irene
AU - Deslauriers, Annie
AU - Liang, Eryuan
AU - Nojd, Pekka
AU - Gruber, Andreas
AU - Nabais, Cristina
AU - Morin, Hubert
AU - Krause, Cornelia
AU - King, Gregory
AU - Fournier, Meriem
PY - 2015/10/26
Y1 - 2015/10/26
N2 - Wood is the main terrestrial biotic reservoir for long-term carbon sequestration, and its formation in trees consumes around 15% of anthropogenic carbon dioxide emissions each year. However, the seasonal dynamics of woody biomass production cannot be quantified from eddy covariance or satellite observations. As such, our understanding of this key carbon cycle component, and its sensitivity to climate, remains limited. Here, we present high-resolution cellular based measurements of wood formation dynamics in three coniferous forest sites in northeastern France, performed over a period of 3 years. We show that stem woody biomass production lags behind stem-girth increase by over 1 month. We also analyse more general phenological observations of xylem tissue formation in Northern Hemisphere forests and find similar time lags in boreal, temperate, subalpine and Mediterranean forests. These time lags question the extension of the equivalence between stem size increase and woody biomass production to intra-annual time scales. They also suggest that these two growth processes exhibit differential sensitivities to local environmental conditions. Indeed, in the well-watered French sites the seasonal dynamics of stem-girth increase matched the photoperiod cycle, whereas those of woody biomass production closely followed the seasonal course of temperature. We suggest that forecasted changes in the annual cycle of climatic factors may shift the phase timing of stem size increase and woody biomass production in the future.
AB - Wood is the main terrestrial biotic reservoir for long-term carbon sequestration, and its formation in trees consumes around 15% of anthropogenic carbon dioxide emissions each year. However, the seasonal dynamics of woody biomass production cannot be quantified from eddy covariance or satellite observations. As such, our understanding of this key carbon cycle component, and its sensitivity to climate, remains limited. Here, we present high-resolution cellular based measurements of wood formation dynamics in three coniferous forest sites in northeastern France, performed over a period of 3 years. We show that stem woody biomass production lags behind stem-girth increase by over 1 month. We also analyse more general phenological observations of xylem tissue formation in Northern Hemisphere forests and find similar time lags in boreal, temperate, subalpine and Mediterranean forests. These time lags question the extension of the equivalence between stem size increase and woody biomass production to intra-annual time scales. They also suggest that these two growth processes exhibit differential sensitivities to local environmental conditions. Indeed, in the well-watered French sites the seasonal dynamics of stem-girth increase matched the photoperiod cycle, whereas those of woody biomass production closely followed the seasonal course of temperature. We suggest that forecasted changes in the annual cycle of climatic factors may shift the phase timing of stem size increase and woody biomass production in the future.
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U2 - 10.1038/nplants.2015.160
DO - 10.1038/nplants.2015.160
M3 - Article
AN - SCOPUS:84945133014
SN - 2055-026X
VL - 1
SP - 1
EP - 6
JO - Nature plants
JF - Nature plants
M1 - 15160
ER -