Journal
PLANT CELL AND ENVIRONMENT
Volume 37, Issue 2, Pages 315-326Publisher
WILEY
DOI: 10.1111/pce.12197
Keywords
carbon and oxygen isotopes; carbon cycle; down-regulation; isotopic fractionation; photosynthesis; stomatal conductance; stomatal sensitivity; vapour pressure deficit; water-use efficiency
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Funding
- Swiss Secretariat for Educational Research, COST Action 639 Gas budget of soils' [C07.0033]
- Swiss National Science Foundation, REQUIP [206021_128761]
- Swiss National Science Foundation (SNF) [206021_128761] Funding Source: Swiss National Science Foundation (SNF)
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Alpine treelines are temperature-limited vegetation boundaries. Understanding the effects of elevated [CO2] and warming on CO2 and H2O gas exchange may help predict responses of treelines to global change. We measured needle gas exchange of Larix deciduaMill. and Pinus mugo ssp. uncinataDC trees after 9 years of free air CO2 enrichment (575 mu molmol(-1)) and 4 years of soil warming (+4 degrees C) and analysed C-13 and O-18 values of needles and tree rings. Tree needles under elevated [CO2] showed neither nitrogen limitation nor end-product inhibition, and no down-regulation of maximal photosynthetic rate (A(max)) was found. Both tree species showed increased net photosynthetic rates (A(n)) under elevated [CO2] (L.decidua: +39%; P.mugo: +35%). Stomatal conductance (g(H2O)) was insensitive to changes in [CO2], thus transpiration rates remained unchanged and intrinsic water-use efficiency (iWUE) increased due to higher A(n). Soil warming affected neither A(n) nor g(H2O). Unresponsiveness of g(H2O) to [CO2] and warming was confirmed by O-18 needle and tree ring values. Consequently, under sufficient water supply, elevated [CO2] induced sustained enhancement in A(n) and lead to increased C inputs into this ecosystem, while soil warming hardly affected gas exchange of L.decidua and P.mugo at the alpine treeline.
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