Stomatal behaviour, photosynthesis and transpiration under rising CO2

Definitions of the variables used and the units are given in Table 1

The literature reports enormous variation between species in the extent of stomatal responses to rising CO₂. This paper attempts to provide a framework within which some of this diversity can be explained. We describe the role of stomata in the short-term response of leaf gas exchange to increases in ambient CO₂ concentration by developing the recently proposed stomatal model of Jarvis & Davies (1998 ). In this model stomatal conductance is correlated with the functioning of the photosynthetic system so that the effects of increases in CO₂ on stomata are experienced through changes in the rate of photosynthesis in a simple and mechanistically transparent way. This model also allows us to consider the effects of evaporative demand and soil moisture availability on stomatal responses to photosynthesis and therefore provides a means of considering these additional sources of variation. We emphasize that the relationship between the rate of photosynthesis and the internal CO₂ concentration and also drought will have important effects on the relative gains to be achieved under rising CO₂.  

  Table 1 . Abbreviations     

5.

Predicting leaf gas exchange and δ¹³C responses to the past 30000 years of global environmental change     

D. J. BEERLING 《The New phytologist》1994,128(3):425-433

     

6.

Tansley Review No. 117   总被引：1，自引：0，他引：1  

KRISTIN PALMQVIST 《The New phytologist》2000,148(1):11-36

     

7.

Photosynthesis and the influence of CO₂-enrichment on δ¹³C values in a C₃ halophyte     

R. D. GUY  D. M. REID 《Plant, cell & environment》1986,9(1):65-72

Abstract Shifts in ?¹³C of the graminaceous C₃ halophyte Puccinellia nuttalliana (Schultes) Hitch. can be induced by salinization. To investigate this phenomenon, three approaches were taken: assay of carboxylases, CO₂-enrichment studies, and gas exchange analysis. Although ribulose-1,5-bisphosphate carboxylase activity decreased with salinity, phosphoenolpyruvate carboxylase activity did not increase and its levels were not atypical of C₃ plants. When plants were grown at four NaCl concentrations under atmospheres of 310 and 1300 cm³ m^?3 CO₂, the CO₂-enrichment enhanced the effects of salinity on ?¹³C. This is consistent with a biophysical explanation for salt-induced shifts in ?¹³C, whereby there is a steepening of the CO₂ diffusion gradient into the leaf. Gas exchange analysis indicated that intercellular CO₂ concentrations were depressed in the leaves of salt-affected plants. This resulted from a greatly decreased stomatal conductance coupled with only small effects on intrinsic photosynthetic capacity. Water-use efficiency was enhanced.     

8.

Elevated CO₂ concentrations and stomatal density: observations from 17 plant species growing in a CO₂ spring in central Italy     

Isabella Bettarini  Francesco P. Vaccari  Franco Miglietta 《Global Change Biology》1998,4(1):17-22

Stomatal density (SD) and stomatal conductance ( g _s) can be affected by an increase of atmospheric CO₂ concentration. This study was conducted on 17 species growing in a naturally enriched CO₂ spring and belonging to three plant communities. Stomatal conductance, stomatal density and stomatal index (SI) of plants from the spring, which were assumed to have been exposed for generations to elevated [CO₂], and of plants of the same species collected in a nearby control site, were compared. Stomatal conductance was significantly lower in most of the species collected in the CO₂ spring and this indicated that CO₂ effects on g _s are not of a transitory nature but persist in the long term and through plant generations. Such a decrease was, however, not associated with changes in the anatomy of leaves: SD was unaffected in the majority of species (the decrease was only significant in three out of the 17 species examined), and also SI values did not vary between the two sites with the exception of two species that showed increased SI in plants grown in the CO₂-enriched area. These results did not support the hypothesis that long-term exposure to elevated [CO₂] may cause adaptive modification in stomatal number and in their distribution.     

9.

Nitrogen source influences natural abundance ¹⁵N of Escherichia coli     

Jessica G. Collins  Paul Dijkstra  Stephen C. Hart  Bruce A. Hungate  Nichole M. Flood  & Egbert Schwartz 《FEMS microbiology letters》2008,282(2):246-250

     

10.

Elevated atmospheric CO₂ improved Sorghum plant water status by ameliorating the adverse effects of drought   总被引：2，自引：0，他引：2  

G. W. Wall  T. J. Brooks  N. R. Adam  A. B. Cousins  B. A. Kimball  P. J. Pinter Jr  R. L. LaMorte  J. Triggs  M. J. Ottman  S. W. Leavitt  A. D. Matthias  D. G. Williams  A. N. Webber 《The New phytologist》2001,152(2):231-248

     

11.

Uptake of ¹⁵NO₂ by sunflower (Helianthus annum) during exposures in light and darkness: quantities, relationship to stomatal aperture and incorporation into different nitrogen pools within the plant     

HANS-JOSEF SEGSCHNEIDER  JÜRGEN WILDT AND  HILMAR FÖRSTEL 《The New phytologist》1995,131(1):109-119

     

12.

Quantifying foliar uptake of gaseous nitrogen dioxide using enriched foliar δ¹⁵N values     

Dena M. Vallano  Jed P. Sparks 《The New phytologist》2008,177(4):946-955

     

13.

Species level patterns in ¹³C and ¹⁵N abundance of ectomycorrhizal and saprotrophic fungal sporocarps     

Andy F. S. Taylor  Petra M. Fransson  Peter Högberg  Mona N. Högberg  Agneta H. Plamboeck 《The New phytologist》2003,159(3):757-774

     

14.

Temporal changes in root growth and ¹⁵N uptake and water relations of two tussock grass species recovering from water stress     

Hormoz BassiriRad  Martyn M. Caldwell 《Physiologia plantarum》1992,86(4):525-531

Physiological responses of Agropyron desertorum and Pseudoroegneria spicata , two common cold desert perennial tussock grass species of the North American Great Basin, were evaluated during and after a period of imposed drought in a pot study. The timing and the pattern of response of leaf water potential (Ψ₁), stomatal conductance (g_s), and root growth were strikingly similar in both species during and after drought. The severity of stress influenced the magnitude of Ψ₁ and g_s, but had little effect on the timing of these responses. Although drought inhibited total root length in prestressed plants, within 4 days after relief of drought both species showed similar increases in root growth which exceeded those of the control. Despite similarities in their root growth responses to increased soil water availability, the two grasses differed in their capacity to restore N uptake following drought. By 14 days after rewatering, N uptake in the prestressed Agropyron had recovered to levels of control plants, although both root biomass and root lenght were much less than those of the controls. This is attributed to elevated root uptake kinetics. Restoration of N uptake by prestressed Pseudoregneria was much less effective during the same period.     

15.

¹⁵N natural abundance of vascular rainforest epiphytes: implications for nitrogen source and acquisition     

G. R. STEWART  S. SCHMIDT  L.L. HANDLEY  M. H. TURNBULL  P. D. ERSKINE  C. A. JOLY 《Plant, cell & environment》1995,18(1):85-90

The foliar natural abundance of ¹⁵N was analysed to compare the potential nitrogen sources of vascular rainforest epiphytes and associated soil-rooted trees. Leaves of epiphytes collected from six rainforest communities in Brazil, Australia and the Solomon Islands were depleted in ¹⁵N relative to the trees at each site. Epiphyte δ¹⁵N was as low as -6.4%_o, while trees were generally enriched in ¹⁵N (0.7 to 3.5%_o). These results indicate either that epiphytes use nitrogen sources depleted in ¹⁵N or that discrimination against ¹⁵N is an intrinsic function of epiphyte physiology. At three sites, epiphytes could be grouped into those having both low δ¹⁵N and low leaf-nitrogen content and those possessing both high δ¹⁵N and high leaf-nitrogen content. The second group had δ¹⁵N values in the range sometimes attributable to N₂ fixation (-2 to 0%o). There was no correlation between growth form and δ¹⁵N. It is concluded that epiphytes may utilize ¹⁵N-depleted nitrogen from atmospheric deposition and N₂ fixation.     

16.

Uptake of nitrogen and carbon from double-labelled (¹⁵N and ¹³C) glycine by mycorrhizal pine seedlings     

A. F. S. Taylor  G. Gebauer  D. J. Read 《The New phytologist》2004,164(2):383-388

     

17.

Effects of elevated CO₂, water and nutrients on Picea sitchensis (Bong.) Carr seedlings   总被引：1，自引：0，他引：1  

JOHN TOWNEND 《The New phytologist》1995,130(2):193-206

     

18.

Parameterization of the CO₂ and H₂O gas exchange of several temperate deciduous broad-leaved trees at the leaf scale considering seasonal changes   总被引：4，自引：3，他引：1  

Y. KOSUGI  S. SHIBATA  & S. KOBASHI 《Plant, cell & environment》2003,26(2):285-301

A combined model to simulate CO₂ and H₂O gas exchange at the leaf scale was parameterized using data obtained from in situ leaf‐scale observations of diurnal and seasonal changes in the CO₂ and H₂O gas exchange of four temperate deciduous broad‐leaved trees using a porometric method. The model consists of a Ball et al. type stomatal conductance submodel [Ball, Woodrow & Berry, pp. 221–224 in Progress in Photosynthesis Research (ed. I. Biggins), Martinus‐Nijhoff Publishers, Dordrecht, The Netherlands, 1987] and a Farquhar et al. type biochemical submodel of photosynthesis (Farquhar, von Caemmerer & Berry, Planta 149, 78–90, 1980). In these submodels, several parameters were optimized for each tree species as representative of the quantitative characteristics related to gas exchange. The results show that the seasonal physiological changes of V_cmax25 in the biochemical model of photosynthesis should be used to estimate the long‐term CO₂ gas exchange. For R_d25 in the biochemical model of photosynthesis and m in the Ball et al. type stomatal conductance model, the difference should be counted during the leaf expansion period.     

19.

¹⁵N natural abundance during early and late succession in a middle-European dry acidic grassland     

W. Beyschlag  S. Hanisch  S. Friedrich  A. Jentsch  & C. Werner 《Plant biology (Stuttgart, Germany)》2009,11(5):713-724

δ¹⁵N and total nitrogen content of above- and belowground tissues of 13 plant species from two successional stages (open pioneer community and ruderal grass stage) of a dry acidic grassland in Southern Germany were analysed, in order to evaluate whether resource use partitioning by niche separation and N input by N₂-fixing legumes are potential determinants for species coexistence and successional changes. Within each stage, plants from plots with different legume cover were compared. Soil inorganic N content, total plant biomass and δ¹⁵N values of bulk plant material were significantly lower in the pioneer stage than in the ruderal grass community. The observed δ¹⁵N differences were rather species- than site-specific. Within both stages, there were also species-specific differences in isotopic composition between above- and belowground plant dry matter. Species-specific δ¹⁵N signatures may theoretically be explained by (i) isotopic fractionation during microbial-mediated soil N transformations; (ii) isotopic fractionation during plant N uptake or fractionation during plant–mycorrhiza transfer processes; (iii) differences in metabolic pathways and isotopic fractionation within the plant; or (iv) partitioning of available N resources (or pools) among plant groups or differential use of the same resources by different species, which seems to be the most probable route in the present case. A significant influence of N₂-fixing legumes on the N balance of the surrounding plant community was not detectable. This was confirmed by the results of an independent in situ removal experiment, showing that after 3 years there were no measurable differences in the frequency distribution between plots with and without N₂-fixing legumes.     

20.

Soil ¹³C–¹⁵N dynamics in an N₂-fixing clover system under long-term exposure to elevated atmospheric CO₂     

Kees-Jan Van Groenigen  Johan Six  David Harris‡  Herbert Blum§  Chris Van Kessel 《Global Change Biology》2003,9(12):1751-1762

Reduced soil N availability under elevated CO₂ may limit the plant's capacity to increase photosynthesis and thus the potential for increased soil C input. Plant productivity and soil C input should be less constrained by available soil N in an N₂‐fixing system. We studied the effects of Trifolium repens (an N₂‐fixing legume) and Lolium perenne on soil N and C sequestration in response to 9 years of elevated CO₂ under FACE conditions. ¹⁵N‐labeled fertilizer was applied at a rate of 140 and 560 kg N ha^?1 yr^?1 and the CO₂ concentration was increased to 60 Pa pCO₂ using ¹³C‐depleted CO₂. The total soil C content was unaffected by elevated CO₂, species and rate of ¹⁵N fertilization. However, under elevated CO₂, the total amount of newly sequestered soil C was significantly higher under T. repens than under L. perenne. The fraction of fertilizer‐N (f_N) of the total soil N pool was significantly lower under T. repens than under L. perenne. The rate of N fertilization, but not elevated CO₂, had a significant effect on f_N values of the total soil N pool. The fractions of newly sequestered C (f_C) differed strongly among intra‐aggregate soil organic matter fractions, but were unaffected by plant species and the rate of N fertilization. Under elevated CO₂, the ratio of fertilizer‐N per unit of new C decreased under T. repens compared with L. perenne. The L. perenne system sequestered more ¹⁵N fertilizer than T. repens: 179 vs. 101 kg N ha^?1 for the low rate of N fertilization and 393 vs. 319 kg N ha^?1 for the high N‐fertilization rate. As the loss of fertilizer‐¹⁵N contributed to the ¹⁵N‐isotope dilution under T. repens, the input of fixed N into the soil could not be estimated. Although N₂ fixation was an important source of N in the T. repens system, there was no significant increase in total soil C compared with a non‐N₂‐fixing L. perenne system. This suggests that N₂ fixation and the availability of N are not the main factors controlling soil C sequestration in a T. repens system.     

Photosynthesis and the influence of CO2-enrichment on δ13C values in a C3 halophyte

Abstract Shifts in ?¹³C of the graminaceous C₃ halophyte Puccinellia nuttalliana (Schultes) Hitch. can be induced by salinization. To investigate this phenomenon, three approaches were taken: assay of carboxylases, CO₂-enrichment studies, and gas exchange analysis. Although ribulose-1,5-bisphosphate carboxylase activity decreased with salinity, phosphoenolpyruvate carboxylase activity did not increase and its levels were not atypical of C₃ plants. When plants were grown at four NaCl concentrations under atmospheres of 310 and 1300 cm³ m^?3 CO₂, the CO₂-enrichment enhanced the effects of salinity on ?¹³C. This is consistent with a biophysical explanation for salt-induced shifts in ?¹³C, whereby there is a steepening of the CO₂ diffusion gradient into the leaf. Gas exchange analysis indicated that intercellular CO₂ concentrations were depressed in the leaves of salt-affected plants. This resulted from a greatly decreased stomatal conductance coupled with only small effects on intrinsic photosynthetic capacity. Water-use efficiency was enhanced.     

Elevated CO2 concentrations and stomatal density: observations from 17 plant species growing in a CO2 spring in central Italy

Stomatal density (SD) and stomatal conductance ( g _s) can be affected by an increase of atmospheric CO₂ concentration. This study was conducted on 17 species growing in a naturally enriched CO₂ spring and belonging to three plant communities. Stomatal conductance, stomatal density and stomatal index (SI) of plants from the spring, which were assumed to have been exposed for generations to elevated [CO₂], and of plants of the same species collected in a nearby control site, were compared. Stomatal conductance was significantly lower in most of the species collected in the CO₂ spring and this indicated that CO₂ effects on g _s are not of a transitory nature but persist in the long term and through plant generations. Such a decrease was, however, not associated with changes in the anatomy of leaves: SD was unaffected in the majority of species (the decrease was only significant in three out of the 17 species examined), and also SI values did not vary between the two sites with the exception of two species that showed increased SI in plants grown in the CO₂-enriched area. These results did not support the hypothesis that long-term exposure to elevated [CO₂] may cause adaptive modification in stomatal number and in their distribution.     

Temporal changes in root growth and 15N uptake and water relations of two tussock grass species recovering from water stress

Physiological responses of Agropyron desertorum and Pseudoroegneria spicata , two common cold desert perennial tussock grass species of the North American Great Basin, were evaluated during and after a period of imposed drought in a pot study. The timing and the pattern of response of leaf water potential (Ψ₁), stomatal conductance (g_s), and root growth were strikingly similar in both species during and after drought. The severity of stress influenced the magnitude of Ψ₁ and g_s, but had little effect on the timing of these responses. Although drought inhibited total root length in prestressed plants, within 4 days after relief of drought both species showed similar increases in root growth which exceeded those of the control. Despite similarities in their root growth responses to increased soil water availability, the two grasses differed in their capacity to restore N uptake following drought. By 14 days after rewatering, N uptake in the prestressed Agropyron had recovered to levels of control plants, although both root biomass and root lenght were much less than those of the controls. This is attributed to elevated root uptake kinetics. Restoration of N uptake by prestressed Pseudoregneria was much less effective during the same period.     

15N natural abundance of vascular rainforest epiphytes: implications for nitrogen source and acquisition

The foliar natural abundance of ¹⁵N was analysed to compare the potential nitrogen sources of vascular rainforest epiphytes and associated soil-rooted trees. Leaves of epiphytes collected from six rainforest communities in Brazil, Australia and the Solomon Islands were depleted in ¹⁵N relative to the trees at each site. Epiphyte δ¹⁵N was as low as -6.4%_o, while trees were generally enriched in ¹⁵N (0.7 to 3.5%_o). These results indicate either that epiphytes use nitrogen sources depleted in ¹⁵N or that discrimination against ¹⁵N is an intrinsic function of epiphyte physiology. At three sites, epiphytes could be grouped into those having both low δ¹⁵N and low leaf-nitrogen content and those possessing both high δ¹⁵N and high leaf-nitrogen content. The second group had δ¹⁵N values in the range sometimes attributable to N₂ fixation (-2 to 0%o). There was no correlation between growth form and δ¹⁵N. It is concluded that epiphytes may utilize ¹⁵N-depleted nitrogen from atmospheric deposition and N₂ fixation.     

Parameterization of the CO2 and H2O gas exchange of several temperate deciduous broad-leaved trees at the leaf scale considering seasonal changes

A combined model to simulate CO₂ and H₂O gas exchange at the leaf scale was parameterized using data obtained from in situ leaf‐scale observations of diurnal and seasonal changes in the CO₂ and H₂O gas exchange of four temperate deciduous broad‐leaved trees using a porometric method. The model consists of a Ball et al. type stomatal conductance submodel [Ball, Woodrow & Berry, pp. 221–224 in Progress in Photosynthesis Research (ed. I. Biggins), Martinus‐Nijhoff Publishers, Dordrecht, The Netherlands, 1987] and a Farquhar et al. type biochemical submodel of photosynthesis (Farquhar, von Caemmerer & Berry, Planta 149, 78–90, 1980). In these submodels, several parameters were optimized for each tree species as representative of the quantitative characteristics related to gas exchange. The results show that the seasonal physiological changes of V_cmax25 in the biochemical model of photosynthesis should be used to estimate the long‐term CO₂ gas exchange. For R_d25 in the biochemical model of photosynthesis and m in the Ball et al. type stomatal conductance model, the difference should be counted during the leaf expansion period.     

15N natural abundance during early and late succession in a middle-European dry acidic grassland

δ¹⁵N and total nitrogen content of above- and belowground tissues of 13 plant species from two successional stages (open pioneer community and ruderal grass stage) of a dry acidic grassland in Southern Germany were analysed, in order to evaluate whether resource use partitioning by niche separation and N input by N₂-fixing legumes are potential determinants for species coexistence and successional changes. Within each stage, plants from plots with different legume cover were compared. Soil inorganic N content, total plant biomass and δ¹⁵N values of bulk plant material were significantly lower in the pioneer stage than in the ruderal grass community. The observed δ¹⁵N differences were rather species- than site-specific. Within both stages, there were also species-specific differences in isotopic composition between above- and belowground plant dry matter. Species-specific δ¹⁵N signatures may theoretically be explained by (i) isotopic fractionation during microbial-mediated soil N transformations; (ii) isotopic fractionation during plant N uptake or fractionation during plant–mycorrhiza transfer processes; (iii) differences in metabolic pathways and isotopic fractionation within the plant; or (iv) partitioning of available N resources (or pools) among plant groups or differential use of the same resources by different species, which seems to be the most probable route in the present case. A significant influence of N₂-fixing legumes on the N balance of the surrounding plant community was not detectable. This was confirmed by the results of an independent in situ removal experiment, showing that after 3 years there were no measurable differences in the frequency distribution between plots with and without N₂-fixing legumes.     

Soil 13C–15N dynamics in an N2-fixing clover system under long-term exposure to elevated atmospheric CO2

Reduced soil N availability under elevated CO₂ may limit the plant's capacity to increase photosynthesis and thus the potential for increased soil C input. Plant productivity and soil C input should be less constrained by available soil N in an N₂‐fixing system. We studied the effects of Trifolium repens (an N₂‐fixing legume) and Lolium perenne on soil N and C sequestration in response to 9 years of elevated CO₂ under FACE conditions. ¹⁵N‐labeled fertilizer was applied at a rate of 140 and 560 kg N ha^?1 yr^?1 and the CO₂ concentration was increased to 60 Pa pCO₂ using ¹³C‐depleted CO₂. The total soil C content was unaffected by elevated CO₂, species and rate of ¹⁵N fertilization. However, under elevated CO₂, the total amount of newly sequestered soil C was significantly higher under T. repens than under L. perenne. The fraction of fertilizer‐N (f_N) of the total soil N pool was significantly lower under T. repens than under L. perenne. The rate of N fertilization, but not elevated CO₂, had a significant effect on f_N values of the total soil N pool. The fractions of newly sequestered C (f_C) differed strongly among intra‐aggregate soil organic matter fractions, but were unaffected by plant species and the rate of N fertilization. Under elevated CO₂, the ratio of fertilizer‐N per unit of new C decreased under T. repens compared with L. perenne. The L. perenne system sequestered more ¹⁵N fertilizer than T. repens: 179 vs. 101 kg N ha^?1 for the low rate of N fertilization and 393 vs. 319 kg N ha^?1 for the high N‐fertilization rate. As the loss of fertilizer‐¹⁵N contributed to the ¹⁵N‐isotope dilution under T. repens, the input of fixed N into the soil could not be estimated. Although N₂ fixation was an important source of N in the T. repens system, there was no significant increase in total soil C compared with a non‐N₂‐fixing L. perenne system. This suggests that N₂ fixation and the availability of N are not the main factors controlling soil C sequestration in a T. repens system.