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Temperature-sensitive biochemical 18O-fractionation and humidity-dependent attenuation factor are needed to predict δ18O of cellulose from leaf water in a grassland ecosystem
by
Hirl, Regina T.
, Zhu, Jianjun
, Schleip, Inga
, Ogée, Jérôme
, Schäufele, Rudi
, Wingate, Lisa
, Ostler, Ulrike
, Schnyder, Hans
, Cabrera, Juan C. Baca
in
18O‐enrichment of cellulose oxygen isotope composition of cellulose
/ air
/ Air temperature
/ Aquatic plants
/ Attenuation
/ canopy
/ canopy conductance
/ Cellulose
/ Climate effects
/ Conductance
/ Drought
/ ecosystems
/ Environmental Sciences
/ Fractionation
/ grassland
/ Grasslands
/ Growth models
/ Humidity
/ Isotope composition
/ isotope‐enabled soil–vegetation–atmosphere transfer model (MuSICA)
/ Leaves
/ Life span
/ longevity
/ Oxygen
/ Oxygen enrichment
/ Oxygen isotopes
/ perennial ryegrass (Lolium perenne)
/ Physiological effects
/ Physiology
/ Plant cover
/ Relative humidity
/ Resistance
/ Seedlings
/ Substrates
/ temperature
/ wheat
2021
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Temperature-sensitive biochemical 18O-fractionation and humidity-dependent attenuation factor are needed to predict δ18O of cellulose from leaf water in a grassland ecosystem
by
Hirl, Regina T.
, Zhu, Jianjun
, Schleip, Inga
, Ogée, Jérôme
, Schäufele, Rudi
, Wingate, Lisa
, Ostler, Ulrike
, Schnyder, Hans
, Cabrera, Juan C. Baca
in
18O‐enrichment of cellulose oxygen isotope composition of cellulose
/ air
/ Air temperature
/ Aquatic plants
/ Attenuation
/ canopy
/ canopy conductance
/ Cellulose
/ Climate effects
/ Conductance
/ Drought
/ ecosystems
/ Environmental Sciences
/ Fractionation
/ grassland
/ Grasslands
/ Growth models
/ Humidity
/ Isotope composition
/ isotope‐enabled soil–vegetation–atmosphere transfer model (MuSICA)
/ Leaves
/ Life span
/ longevity
/ Oxygen
/ Oxygen enrichment
/ Oxygen isotopes
/ perennial ryegrass (Lolium perenne)
/ Physiological effects
/ Physiology
/ Plant cover
/ Relative humidity
/ Resistance
/ Seedlings
/ Substrates
/ temperature
/ wheat
2021
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Temperature-sensitive biochemical 18O-fractionation and humidity-dependent attenuation factor are needed to predict δ18O of cellulose from leaf water in a grassland ecosystem
by
Hirl, Regina T.
, Zhu, Jianjun
, Schleip, Inga
, Ogée, Jérôme
, Schäufele, Rudi
, Wingate, Lisa
, Ostler, Ulrike
, Schnyder, Hans
, Cabrera, Juan C. Baca
in
18O‐enrichment of cellulose oxygen isotope composition of cellulose
/ air
/ Air temperature
/ Aquatic plants
/ Attenuation
/ canopy
/ canopy conductance
/ Cellulose
/ Climate effects
/ Conductance
/ Drought
/ ecosystems
/ Environmental Sciences
/ Fractionation
/ grassland
/ Grasslands
/ Growth models
/ Humidity
/ Isotope composition
/ isotope‐enabled soil–vegetation–atmosphere transfer model (MuSICA)
/ Leaves
/ Life span
/ longevity
/ Oxygen
/ Oxygen enrichment
/ Oxygen isotopes
/ perennial ryegrass (Lolium perenne)
/ Physiological effects
/ Physiology
/ Plant cover
/ Relative humidity
/ Resistance
/ Seedlings
/ Substrates
/ temperature
/ wheat
2021
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Temperature-sensitive biochemical 18O-fractionation and humidity-dependent attenuation factor are needed to predict δ18O of cellulose from leaf water in a grassland ecosystem
Journal Article
Temperature-sensitive biochemical 18O-fractionation and humidity-dependent attenuation factor are needed to predict δ18O of cellulose from leaf water in a grassland ecosystem
2021
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Overview
• We explore here our mechanistic understanding of the environmental and physiological processes that determine the oxygen isotope composition of leaf cellulose (δ18Ocellulose) in a drought-prone, temperate grassland ecosystem.
• A new allocation-and-growth model was designed and added to an 18O-enabled soil–vegetation–atmosphere transfer model (MuSICA) to predict seasonal (April–October) and multi-annual (2007–2012) variation of δ18Ocellulose and 18O-enrichment of leaf cellulose (Δ18Ocellulose) based on the Barbour–Farquhar model.
• Modelled δ18Ocellulose agreed best with observations when integrated over c. 400 growing-degree-days, similar to the average leaf lifespan observed at the site. Over the integration time, air temperature ranged from 7 to 22°C and midday relative humidity from 47 to 73%. Model agreement with observations of δ18Ocellulose (R² = 0.57) and Δ18Ocellulose (R² = 0.74), and their negative relationship with canopy conductance, was improved significantly when both the biochemical 18O-fractionation between water and substrate for cellulose synthesis (ϵbio, range 26–30‰) was temperature-sensitive, as previously reported for aquatic plants and heterotrophically grown wheat seedlings, and the proportion of oxygen in cellulose reflecting leaf water 18O-enrichment (1 – p
ex
pₓ, range 0.23–0.63) was dependent on air relative humidity, as observed in independent controlled experiments with grasses.
• Understanding physiological information in δ18Ocellulose requires quantitative knowledge of climatic effects on p
ex
pₓ and ϵ
bio.
Publisher
Wiley,Wiley Subscription Services, Inc
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