28 results on '"Broadmeadow, M."'
Search Results
2. Photosynthetic Pathway, Chilling Tolerance and Cell Sap Osmotic Potential Values of Grasses along an Altitudinal Gradient in Papua New Guinea
- Author
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Earnshaw, M. J., Griffiths, H., and Broadmeadow, M. S. J.
- Published
- 1990
3. Short-Term Changes in Carbon-Isotope Discrimination in the C₃-CAM Intermediate Clusia minor L. Growing in Trinidad
- Author
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Borland, A. M., Griffiths, H., Broadmeadow, M. S. J., and Maxwell, C.
- Published
- 1993
4. The Carbon Isotope Ratio of Plant Organic Material Reflects Temporal and Spatial Variations in CO₂ within Tropical Forest Formations in Trinidad
- Author
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Broadmeadow, M. S. J., Griffiths, H., Maxwell, C., and Borland, A. M.
- Published
- 1992
5. On the Ecophysiology of the Clusiaceae in Trinidad: Expression of CAM in Clusia minor L. During the Transition from Wet to Dry Season and Characterization of Three Endemic Species
- Author
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Borland, A. M., Griffiths, H., Maxwell, C., Broadmeadow, M. S. J., Griffiths, N. M., and Barnes, J. D.
- Published
- 1992
6. Gas exchange and carbon isotope discrimination in lichens: Evidence for interactions between CO2-concentrating mechanisms and diffusion limitation
- Author
-
Máguas, C., Griffiths, H., and Broadmeadow, M. S. J.
- Published
- 1995
- Full Text
- View/download PDF
7. Isoprene emission potentials from European oak forests derived from canopy flux measurements: an assessment of uncertainties and inter-algorithm variability
- Author
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Langford, B., Cash, J., Acton, W. J. F., Valach, A. C., Hewitt, C. N., Fares, S., Goded, I., Gruening, C., House, E., Kalogridis, A.-C., Gros, V., Schafers, R., Thomas, R., Broadmeadow, M., Nemitz, E., Centre for Ecology and Hydrology [Edinburgh] (CEH), Natural Environment Research Council (NERC), Lancaster Environment Centre, Lancaster University, Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Chimie Atmosphérique Expérimentale (CAE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), School of Geography, Earth and Environmental Sciences [Birmingham], University of Birmingham [Birmingham], Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS), and Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)
- Subjects
Canopy ,010504 meteorology & atmospheric sciences ,Eddy covariance ,lcsh:Life ,010501 environmental sciences ,Quercus pubescens ,01 natural sciences ,7. Clean energy ,Atmospheric Sciences ,Quercus robur ,chemistry.chemical_compound ,Flux (metallurgy) ,lcsh:QH540-549.5 ,Range (statistics) ,[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment ,ComputingMilieux_MISCELLANEOUS ,Ecology, Evolution, Behavior and Systematics ,Isoprene ,0105 earth and related environmental sciences ,Earth-Surface Processes ,[SDU.OCEAN]Sciences of the Universe [physics]/Ocean, Atmosphere ,biology ,Chemistry ,lcsh:QE1-996.5 ,15. Life on land ,biology.organism_classification ,lcsh:Geology ,lcsh:QH501-531 ,Deposition (aerosol physics) ,13. Climate action ,lcsh:Ecology ,Algorithm - Abstract
Biogenic emission algorithms predict that oak forests account for ~ 70 % of the total European isoprene budget. Yet the isoprene emission potentials that underpin these model estimates are calculated from a very limited number of leaf-level observations and hence are highly uncertain. Increasingly, micrometeorological techniques such as eddy covariance are used to measure whole-canopy fluxes directly, from which isoprene emission potentials can be calculated. Here, we review five observational datasets of isoprene fluxes from a range of oak forests in the UK, Italy and France. We outline procedures to correct the measured net fluxes for losses from deposition and chemical flux divergence, which were found to be on the order of 5–8 % and 4–5 %, respectively. The corrected observational data were used to derive isoprene emission potentials at each site in a two-step process. Firstly, six commonly used emission algorithms were inverted to back out time series of isoprene emission potential, and then an average isoprene emission potential was calculated for each site with an associated uncertainty. We used these data to assess how the derived emission potentials change depending upon the specific emission algorithm used and importantly, on the particular approach adopted to derive an average site specific emission potential. Our results show that isoprene emission potentials can vary by up to a factor of four depending on the specific algorithm used and whether or not it is used in a big-leaf or canopy environment model format. When using the same algorithm, the calculated average isoprene emission potential was found to vary by as much as 34 % depending on how the average was derived. In order to best replicate the observed fluxes we propose a new weighted average method whereby the isoprene emission potential is calculated as the average of all flux observations divided by the average activity factor (γ) of the emission algorithm. This approach ensures that modelled fluxes always have the same average as the measurements. Using this new approach, with version 2.1 of the Model for Emissions of Gases and Aerosols from Nature (MEGAN), we derive new ecosystem-scale isoprene emission potentials for the five measurement sites, Alice Holt, UK (10 500 ± 2500 µg m−2 h−1), Bosco Fontana, Italy (1610 ± 420 µg m−2 h−1), Castelporziano, Italy (43 ± 10 µg m−2 h−1), Ispra, Italy (7590 ± 1070 µg m−2 h−1) and the Observatoire de Haute Provence, France (7990 ± 1010 µg m−2 h−1). Ecosystem-scale isoprene emission potentials were then extrapolated to the leaf-level and compared to previous leaf-level measurements for Quercus robur and Quercus pubescens, two species thought to account for 50 % of the total European isoprene budget. The literature values agreed closely with emission potentials calculated using the G93 algorithm, which were 85 ± 75 µg g−1 h−1 and 78 ± 25 µg g−1 h−1 for Q. robur and Q. pubescens respectively. By contrast, emission potentials calculated using the G06 algorithm, the same algorithm used in a previous study to derive the European budget, were significantly lower, which we attribute to the influence of past light and temperature conditions. Adopting these new G06 specific emission potentials for Q. robur (55 ± 24 µg g−1 h−1) and Q. pubescens (47 ± 16 µg g−1 h−1) reduced the projected European budget by ~ 17 %. Our findings demonstrate that calculated isoprene emission potentials vary considerably depending upon the specific approach used in their calculation. Therefore, it is our recommendation that the community now adopt a standardised approach to the way in which micrometeorological flux measurements are corrected and used to derive isoprene, and other biogenic VOC, emission potentials. Modellers who use derived emission potentials should pay particular attention to the way in which an emission potential was derived and ensure that the algorithm they are using, and the implementation thereof, is consistent with that used to derive the emission potential. Our results show that, in the worst cases, failure to account for this may result in modelled fluxes that differ from observations by up to a factor of four.
- Published
- 2017
8. Isoprene emission potentials from European oak forests derived from canopy flux measurements: An assessment of uncertainties and inter-algorithm variability
- Author
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Langford, Ben, Cash, James, Acton, William Joe Fraser, Valach, Amy, Hewitt, C N, Fares, S., Goded, Ignacio, Gruening, Carsten, House, Emily Roseanne, Kalogridis, Athina-Cerise, Gros, Valerie, Schafers, Richard, Thomas, Rick, Broadmeadow, M. S. J., Nemitz, Eiko, Langford, Ben, Cash, James, Acton, William Joe Fraser, Valach, Amy, Hewitt, C N, Fares, S., Goded, Ignacio, Gruening, Carsten, House, Emily Roseanne, Kalogridis, Athina-Cerise, Gros, Valerie, Schafers, Richard, Thomas, Rick, Broadmeadow, M. S. J., and Nemitz, Eiko
- Abstract
Biogenic emission algorithms predict that oak forests account for ∼ 70 % of the total European isoprene budget. Yet the isoprene emission potentials (IEPs) that underpin these model estimates are calculated from a very limited number of leaf-level observations and hence are highly uncertain. Increasingly, micrometeorological techniques such as eddy covariance are used to measure whole-canopy fluxes directly, from which isoprene emission potentials can be calculated. Here, we review five observational datasets of isoprene fluxes from a range of oak forests in the UK, Italy and France. We outline procedures to correct the measured net fluxes for losses from deposition and chemical flux divergence, which were found to be on the order of 5–8 and 4–5 %, respectively. The corrected observational data were used to derive isoprene emission potentials at each site in a two-step process. Firstly, six commonly used emission algorithms were inverted to back out time series of isoprene emission potential, and then an average isoprene emission potential was calculated for each site with an associated uncertainty. We used these data to assess how the derived emission potentials change depending upon the specific emission algorithm used and, importantly, on the particular approach adopted to derive an average site-specific emission potential. Our results show that isoprene emission potentials can vary by up to a factor of 4 depending on the specific algorithm used and whether or not it is used in a big-leaf or canopy environment (CE) model format. When using the same algorithm, the calculated average isoprene emission potential was found to vary by as much as 34 % depending on how the average was derived. Using a consistent approach with version 2.1 of the Model for Emissions of Gases and Aerosols from Nature (MEGAN), we derive new ecosystem-scale isoprene emission potentials for the five measurement sites: Alice Holt, UK (10 500 ± 2500 µg m−2 h−1); Bosco Fontana, Italy (1610 ± 420
- Published
- 2017
9. Terrestrial Umbrella - Effects of eutrophication and acidification on terrestrial ecosystems. Annual Report 2009
- Author
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Emmett, B., Ashmore, M., Belyazid, S, Britton, A., Broadmeadow, M., Caporn, S., Davies, O., Field, C., Dise, N., Helliwell, R., Hester, A., Hughes, S., Leake, L., Leith, I., Maskell, L., Mills, R., Mizunuma, T., Ostle, N., Phoenix, G., Power, S., Reynolds, B., Rowe, E., Scott, A., Sheppard, L., Smart, S., Sowerby, A., Tipping, E., Vanguelova, E., Vuohelainen, A., Williams, B.P., Emmett, B., Ashmore, M., Belyazid, S, Britton, A., Broadmeadow, M., Caporn, S., Davies, O., Field, C., Dise, N., Helliwell, R., Hester, A., Hughes, S., Leake, L., Leith, I., Maskell, L., Mills, R., Mizunuma, T., Ostle, N., Phoenix, G., Power, S., Reynolds, B., Rowe, E., Scott, A., Sheppard, L., Smart, S., Sowerby, A., Tipping, E., Vanguelova, E., Vuohelainen, A., and Williams, B.P.
- Published
- 2009
10. Terrestrial Umbrella - Effects of eutrophication and acidification on terrestrial ecosystems. Annual Report 2008
- Author
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Emmett, B., Cooper, J. R., Ashmore, M., Belyazid, S, Britton, A., Broadmeadow, M., Caporn, S., Carroll, J., Davies, O., Dise, N., Field, C., Helliwell, R., Hester, A., Hughes, S., Leake, L., Leith, I., Maskell, L., Mills, R., Mizunuma, T., Ostle, N., Phoenix, G., Power, S., Reynolds, B., Rowe, E., Scott, A., Sheppard, L., Smart, S., Sowerby, A., Tipping, E., Vanguelova, E., Vuohelainen, A., Emmett, B., Cooper, J. R., Ashmore, M., Belyazid, S, Britton, A., Broadmeadow, M., Caporn, S., Carroll, J., Davies, O., Dise, N., Field, C., Helliwell, R., Hester, A., Hughes, S., Leake, L., Leith, I., Maskell, L., Mills, R., Mizunuma, T., Ostle, N., Phoenix, G., Power, S., Reynolds, B., Rowe, E., Scott, A., Sheppard, L., Smart, S., Sowerby, A., Tipping, E., Vanguelova, E., and Vuohelainen, A.
- Published
- 2008
11. Terrestrial Umbrella: effects of eutrophication and acidification on terrestrial ecosystems. Final report
- Author
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Emmett, B., Ashmore, M., Britton, A., Broadmeadow, M., Bullock, J., Cape, N., Caporn, S. J. M., Carroll, J. A., Cooper, J. R., Cresser, M. S., Crossley, A., d'Hooghe, P., De Lange, I., Edmondson, J., Evans, C. D., Field, C., Fowler, D., Grant, H., Green, E., Griffiths, B., Haworth, B., Helliwell, R., Hicks, K., Hinton, C., Holding, H., Hughes, S., James, M., Jones, A., Jones, M., Jones, M. L. M., Leake, J., Leith, I., Maskell, L., McNamara, N., Moy, I., Oakley, S., Ostle, N., Pilkington, M., Power, S., Prendergast, M., Ray, N., Reynolds, B., Rowe, E., Roy, D., Scott, A., Sheppard, L., Smart, S., Sowerby, A., Sutton, M., Terry, A., Tipping, E., van den Berg, L., van Dijk, N., van Zetten, E., Vanguelova, E., Williams, B., Williams, D., Williams, W., Emmett, B., Ashmore, M., Britton, A., Broadmeadow, M., Bullock, J., Cape, N., Caporn, S. J. M., Carroll, J. A., Cooper, J. R., Cresser, M. S., Crossley, A., d'Hooghe, P., De Lange, I., Edmondson, J., Evans, C. D., Field, C., Fowler, D., Grant, H., Green, E., Griffiths, B., Haworth, B., Helliwell, R., Hicks, K., Hinton, C., Holding, H., Hughes, S., James, M., Jones, A., Jones, M., Jones, M. L. M., Leake, J., Leith, I., Maskell, L., McNamara, N., Moy, I., Oakley, S., Ostle, N., Pilkington, M., Power, S., Prendergast, M., Ray, N., Reynolds, B., Rowe, E., Roy, D., Scott, A., Sheppard, L., Smart, S., Sowerby, A., Sutton, M., Terry, A., Tipping, E., van den Berg, L., van Dijk, N., van Zetten, E., Vanguelova, E., Williams, B., Williams, D., and Williams, W.
- Published
- 2007
12. Inter-annual variation of carbon uptake by a plantation oak woodland in south-eastern England
- Author
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Wilkinson, M., primary, Eaton, E. L., additional, Broadmeadow, M. S. J., additional, and Morison, J. I. L., additional
- Published
- 2012
- Full Text
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13. UK emissions by sources and removals by sinks due to land use, land use change and forestry activities. Report, April 2006
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Milne, R., Mobbs, D. C., Thomson, A. M., Matthews, R. W., Broadmeadow, M. S. J., Mackie, E., Wilkinson, M., Benham, S., Harris, K., Grace, J., Quegan, S., Coleman, K., Powlson, D. S., Whitmore, A. P., Sozanska-Stanton, M., Smith, P., Levy, P. E., Ostle, N., Murray, T. D., Van Oijen, M., Brown, T., Milne, R., Mobbs, D. C., Thomson, A. M., Matthews, R. W., Broadmeadow, M. S. J., Mackie, E., Wilkinson, M., Benham, S., Harris, K., Grace, J., Quegan, S., Coleman, K., Powlson, D. S., Whitmore, A. P., Sozanska-Stanton, M., Smith, P., Levy, P. E., Ostle, N., Murray, T. D., Van Oijen, M., and Brown, T.
- Published
- 2006
14. Terrestrial Umbrella Annual Report. July 2006
- Author
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Emmett, B. A., Williams, B. L., Ashmore, M., Britton, A., Broadmeadow, M., Bullock, J., Cape, J. N., Caporn, S. J. M., Carroll, J. A., Cresser, M. S., Crossley, A. C., de Lange, I., Edmondson, J., Evans, C., Fowler, D., Grant, H., Green, E. R., Green, S., Griffiths, B., Hall, J., Helliwell, R., Hinton, C., Hughes, S., Jones, A. G., Jones, M., Leake, J. R., Leith, I. D., Maskell, L., McNamara, N., Moy, I., Oakley, S., Ostle, N., Power, S. A., Prendergast, M., Price, E. A. C., Reynolds, B., Rowe, E., Roy, D., Scott, A., Sheppard, L. J., Smart, S., Sowerby, A., Sutton, M. A., Thacker, S. A., Tipping, E., van Dijk, N., Vanguelova, E., van Zetten, E., Williams, D., Wilson, D., Wright, S., Emmett, B. A., Williams, B. L., Ashmore, M., Britton, A., Broadmeadow, M., Bullock, J., Cape, J. N., Caporn, S. J. M., Carroll, J. A., Cresser, M. S., Crossley, A. C., de Lange, I., Edmondson, J., Evans, C., Fowler, D., Grant, H., Green, E. R., Green, S., Griffiths, B., Hall, J., Helliwell, R., Hinton, C., Hughes, S., Jones, A. G., Jones, M., Leake, J. R., Leith, I. D., Maskell, L., McNamara, N., Moy, I., Oakley, S., Ostle, N., Power, S. A., Prendergast, M., Price, E. A. C., Reynolds, B., Rowe, E., Roy, D., Scott, A., Sheppard, L. J., Smart, S., Sowerby, A., Sutton, M. A., Thacker, S. A., Tipping, E., van Dijk, N., Vanguelova, E., van Zetten, E., Williams, D., Wilson, D., and Wright, S.
- Published
- 2006
15. UK emissions by sources and removals by sinks due to land use, land use change and forestry activities. Report, June 2005
- Author
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Milne, R., Mobbs, D. C., Thomson, A. M., Skiba, U., Matthews, R. W., Broadmeadow, M. S. J., Mackie, E., Wilkinson, M., Benham, S., Harris, K., Grace, J., Coleman, K., Whitmore, A. P., Zhang, C., Sozanska-Stanton, M., Smith, P., Levy, P. E., Ostle, N., Murray, T. D., Van Oijen, M., Brown, T. A. W., Milne, R., Mobbs, D. C., Thomson, A. M., Skiba, U., Matthews, R. W., Broadmeadow, M. S. J., Mackie, E., Wilkinson, M., Benham, S., Harris, K., Grace, J., Coleman, K., Whitmore, A. P., Zhang, C., Sozanska-Stanton, M., Smith, P., Levy, P. E., Ostle, N., Murray, T. D., Van Oijen, M., and Brown, T. A. W.
- Published
- 2005
16. Chemical fluxes in time through forest ecosystems in the UK – Soil response to pollution recovery
- Author
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Vanguelova, E.I., primary, Benham, S., additional, Pitman, R., additional, Moffat, A.J., additional, Broadmeadow, M., additional, Nisbet, T., additional, Durrant, D., additional, Barsoum, N., additional, Wilkinson, M., additional, Bochereau, F., additional, Hutchings, T., additional, Broadmeadow, S., additional, Crow, P., additional, Taylor, P., additional, and Durrant Houston, T., additional
- Published
- 2010
- Full Text
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17. Risk assessments for forest trees: The performance of the ozone flux versus the AOT concepts
- Author
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Karlsson, P.E., primary, Braun, S., additional, Broadmeadow, M., additional, Elvira, S., additional, Emberson, L., additional, Gimeno, B.S., additional, Le Thiec, D., additional, Novak, K., additional, Oksanen, E., additional, Schaub, M., additional, Uddling, J., additional, and Wilkinson, M., additional
- Published
- 2007
- Full Text
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18. Environmental Limitations to O3 Uptake - Some Key Results from Young Trees Growing at Elevated Co2 Concentrations.
- Author
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Broadmeadow, M. S. J., Heath, J., Randle, T. J., Broadmeadow, M. S. J., Heath, J., and Randle, T. J.
- Abstract
Elevated carbon dioxide concentrations and limited water supply have been shown to reduce the impact of ozone pollution on the growth and physiology of Quercus petraea in a long-term factorial experiment. These responses can be explained by observed reductions in stomatal conductance, and thus potential ozone exposure of 28% and 40% for CO2 and drought treatments respectively. However, parameterisation of a stomatal conductance model for Quercus robur and Fagus sylvatica grown under ambient and elevated CO2 concentrations in a separate experiment has demonstrated that elevated CO2 also reduces the responsiveness of stomata to both saturation deficit (LAVPD) and soil moisture deficit () in beech, and to a lesser extent, in oak. Season-long model simulations of ozone fluxes suggest that LAVPD and conductance parameters derived at ambient CO2 concentrations will lead to these fluxes being underestimated by 24% and 2% for beech and oak respectively at 615 ppm CO2.
- Published
- 1999
19. The development of an approach to assess critical loads of acidity for woodland habitats in Great Britain
- Author
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Langan, S. J., primary, Hall, J., additional, Reynolds, B., additional, Broadmeadow, M., additional, Hornung, M., additional, and Cresser, M. S., additional
- Published
- 2004
- Full Text
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20. New critical levels for ozone effects on young trees based on AOT40 and simulated cumulative leaf uptake of ozone
- Author
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Karlsson, P.E., primary, Uddling, J., additional, Braun, S., additional, Broadmeadow, M., additional, Elvira, S., additional, Gimeno, B.S., additional, Le Thiec, D., additional, Oksanen, E., additional, Vandermeiren, K., additional, Wilkinson, M., additional, and Emberson, L., additional
- Published
- 2004
- Full Text
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21. Short-term changes in carbon-isotope discrimination in the C3-CAM intermediate Clusia minor L. growing in Trinidad
- Author
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Borland, A. M., Griffiths, H., Broadmeadow, M. S. J., Fordham, M. C., and Maxwell, C.
- Abstract
On-line instantaneous carbon isotope discrimination was measured in conjunction with net uptake of CO
2 in leaves of exposed and shaded plants of the C3 -CAM intermediate Clusia minor growing under natural conditions in Trinidad. At the end of the rainy season (late January-early February, 1992) C3 photosynthesis predominated although exposed leaves recaptured a small proportion of respiratory CO2 at night for the synthesis of malic acid. Citric acid was the major organic acid accumulated by exposed leaves at this time with a citric: malic acid ratio of 11:1. Values of instantaneous discrimination (?) in exposed leaves during the wet season rose from 17.1‰ shortly after dawn to 22.7‰ around mid-day just before stomata closed, suggesting that most CO2 was fixed by Rubisco at this time. During the late afternoon, instantaneous ? declined from 22.2‰ to 17‰, probably reflecting the limited contribution from PEPc activity and an increase in diffusional resistance to CO2 in exposed leaves. Shaded leaves showed no CAM activity and CO2 uptake proceeded throughout the day in the wet season. The decrease in instantaneous ? from 27‰ in the morning to 19.2‰ in the late afternoon was therefore entirely due to diffusional limitation. Leaves sampled in the dry season (mid-March, 1992) had by now induced full CAM activity with both malic and citric acids accumulated overnight and stomata closed for 4–5 h over the middle of the day. Values of instantaneous ? measured over the first 3 h after dawn (6.4–9.1‰) indicated that C4 carboxylation dominated CO2 uptake for most of the morning when rates of photosynthesis were maximal, implying that under natural conditions, the down regulation of PEPc in phase II occurs much more slowly than laboratory-based studies have suggested. The contribution from C3 carboxylation to CO2 uptake during phase II was most marked in leaves which accumulated lower quantities of organic acids overnight. In exposed leaves, measurements of instantaneous ? during the late afternoon illustrated the transition from C3 to C4 carboxylation with stomata remaining open during the transition from dusk into the dark period. Uptake of CO2 by shaded leaves during the late afternoon however appeared to be predominantly limited by decreased stomatal conductance. The short-term measurements of instantaneous ? were subsequently integrated over 24 h in order to predict the leaf carbon isotope ratios (dp ) and to compare this with the dp measured for leaf organic material. Whilst there was close agreement between predicted and measured dp for plants sampled in the wet season, during the dry season the predicted carbon isotope ratios were 5–9‰ higher than the measured isotope ratios. During the annual cycle of leaf growth most carbon was fixed via the C3 pathway although CAM clearly plays an important role in maintaining photochemical integrity in the dry season.- Published
- 1993
- Full Text
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22. Gas exchange and carbon isotope discrimination in lichens: Evidence for interactions between CO2-concentrating mechanisms and diffusion limitation
- Author
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Máguas, C., Griffiths, H., and Broadmeadow, M. S. J.
- Abstract
The characteristics of gas exchange and carbon isotope discrimination were determined for a number of lichen species, representing contrasting associations between fungal (mycobiont) and photosynthetic (photobiont) organism. These parameters were evaluated with regard to the occurrence of any CO
2 -concentrating mechanism (CCM) expressed specifically by the green algal (phycobiont) or cyanobacterial (cyanobiont) partner. Carbon isotope discrimination (?) fell into three categories. The highest ?, found in lichens comprising a phycobiont plus cyanobacteria limited to pockets in the thallus (known as cephalodia), ranged from 24 to 28‰, equivalent to a carbon isotope ratio (d13 C) of around -32 to-36‰ vs. Pee Dee Belemnite (PDB) standard. Further evidence was consistent with CO2 supply to the carboxylating system entirely mediated by diffusion rather than a CCM, in that thallus CO2 compensation point and online instantaneous ? were also high, in the range normally associated with C3 higher plants. For lichens consisting of phycobiont or cyanobiont alone, organic material ? formed two distinct ranges around 15‰ (equivalent to a d13 C of -23%.). Thallus compensation point and instantaneous ? were lower in the cyanobiont group, which also showed higher maximum rates of net photosynthesis, whether expressed on the basis of thallus dry weight, chlorophyll content or area. These data provide additional evidence for the activity of a CCM in cyanobiont lichens, which only show photosynthetic activity when reactivated with liquid water. Rates of net CO2 uptake were lower in both phycobiont associations, but were relatively constant across a wide working range of thallus water contents, usually in parallel with on-line ?. The phycobiont response was consistent whether photosynthesis had been reactivated with liquid water or water vapour. The effect of diffusion limitation could generally be seen with a 3–4‰ decrease in instantaneous ? at the highest water contents. The expression of a CCM in phycobiont algae, although reduced compared with that in cyanobacteria, has already been related to the occurrence of pyrenoids in chloroplasts. In view of the inherent requirement of cyanobacteria for some form of CCM, and the smaller pools of dissolved inorganic carbon (DIC = CO2 + HCOinf3 su- + COinf3 su2- ) associated with phycobiont lichens, it appears that ? characteristics provide a good measure of the magnitude of any CCM, albeit tempered by diffusion limitation at the highest thallus water contents.- Published
- 1995
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23. The carbon isotope ratio of plant organic material reflects temporal and spatial variations in CO2 within tropical forest formations in Trinidad
- Author
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Broadmeadow, M. S. J., Griffiths, H., Maxwell, C., and Borland, A. M.
- Abstract
A method of monitoring and collecting CO
2 samples in the field has been developed which has been used to study both temporal and spatial variations in canopy CO2 isotopic signatures in two contrasting tropical forest formations in Trinidad. These have been related to vertical gradients in the carbon isotope ratio (d13 C) of organic material in conjunction with measurements of other environmental parameters. The d13 C of leaf material from two canopies showed a gradient with respect to height, more negative values being found low in the understorey. The deciduous secondary forest, (Simla) showed a difference of 4.6‰ and the semi-evergreen seasonal canopy (Aripo), 2.8‰. The range of d13 C values at Simla was 4‰ less negative than those at Aripo. In order to relate these measurements to the interaction between diffusion or carboxylation limitation, and source CO2 effects, variations in environmental parameters through the canopy have been compared with changes in CO2 partial pressure (Pa ) and isotopic composition d13 C throughout the day during the dry season. Values of Pa 20 m above the ground at Aripo varied from 380 vpm at dawn to 340 vpm at midday, at which time the partial pressure 15 cm above the ground was 375 vpm. The CO2 partial pressure did not stabilise during the course of the day, and there was good correlation (r2 =0.82) between da and Pa , with more negative values of da occuring in the understorey. Diuraal changes of 2‰ were evident at all canopy positions. In the more open canopy at Simla, these gradients were similar, but less marked. Leaf-air vapour pressure deficit (VPD) showed no relationship with height, possibly as a result of minimal water flux from both the soil and the canopy due to low soil water content; VPD was 1.5 kPa higher at midday than dawn. A 3° C temperature gradient between the understorey and upper canopy was observed at Aripo but not in the more open Simla canopy. CO2 partial pressure stabilised for only 4 h in the middle of the day, while other parameters showed no stable period. The proportion of floor respired CO2 reassimilated at Aripo has been calculated as 26%, 19%, and 8% for the periods 0600–1000, 1000–1400, and 1400–1800 hours. In order to quantify source CO2 effects, measurements of the environmental parameters and assimilation rate must be made at all canopy positions and throughout the day.- Published
- 1992
- Full Text
- View/download PDF
24. Elevated CO 2 and tree root growth: contrasting responses in Fraxinus excelsior, Quercus petraea and Pinus sylvestris.
- Author
-
Crookshanks M, Taylor G, and Broadmeadow M
- Abstract
Root growth and respiration in elevated CO
2 (700 μmol mol-1 ) was studied in three tree species, Fraxinus excelsior L., Quercus petraea. L. and Pinus sylvestris L. grown in open-top chambers (OTCs) during a long-term exposure (20 months), during which root systems were allowed to develop without restriction imposed by pots. Root growth, measured as root length using root in-growth bags was increased significantly in trees exposed to elevated CO2 , although the magnitude of the response differed considerably between species and with time of sampling, the greatest effect observed after 6 months in ash (ratio of elevated: ambient, e∶a; 3·40) and the smallest effect observed in oak (e∶a; 1·95). This was accompanied by changes in specific root length, with a significant decrease in all species after 6 months, suggesting that root diameter or root density were increased in elevated CO2 . Increases in root length might have resulted from an acceleration in root cell expansion, since epidermal cell size was significantly increased in the zone of elongation in ash root tips (P<0·05). Contrasting effects of elevated CO2 were observed for root carbohydrates, with significant increases in soluble sugars for all species (P<0·05), but both increases and decreases in starch content were observed, depending on species, and producing a significant interaction between species and CO2 (P<0·001). Exposure to elevated CO2 increased the total root d. wt for whole trees of all three species after 8 months of exposure, although the magnitude of this effect, in contrast to the root in-growth study, was greatest in Scots pine and smallest in ash. No significant effect of elevated CO2 was observed on the root∶shoot ratio. Further detailed analysis of whole root systems after 20 months confirmed that species differences in root responses to elevated CO2 were apparent, with increased coarse and fine root production in elevated CO2 for Scots pine and ash respectively. Lateral root number was increased in elevated CO2 for all species, as was mean root diameter. Root respiration rates were significantly reduced in elevated CO2 for all three species. These results provide firm evidence that exposure of trees to future CO2 concentrations will have large effects on root system development, growth, carbohydrate status and respiration. The magnitude and direction of such effects will differ, depending on species. The consequences of such responses for the three species studied are discussed.- Published
- 1998
- Full Text
- View/download PDF
25. Carbon-Isotope Composition of Biochemical Fractions and the Regulation of Carbon Balance in Leaves of the C3-Crassulacean Acid Metabolism Intermediate Clusia minor L. Growing in Trinidad.
- Author
-
Borland AM, Griffiths H, Broadmeadow M, Fordham MC, and Maxwell C
- Abstract
Carbon-isotope ratios ([delta]13Cs) were measured for various bio-chemical fractions quantitatively extracted from naturally exposed and shaded leaves of the C3-Crassulacean acid metabolism (CAM) intermediate Clusia minor, sampled at dawn and dusk on days during the wet and dry seasons in Trinidad. As the activity of CAM increased in response to decreased availability of water and higher photon flux density, organic acids and soluble sugars were enriched in 13C by approximately 3.5 to 4%[per mille (thousand) sign] compared to plants sampled during the wet season. The induction of CAM was accompanied by a doubling in size of the reserve carbohydrate pools. Moreover, stoichiometric measurements indicated that degradation of both chloroplastic reserves and soluble sugars were necessary to supply phosphoenolpyruvate for the synthesis of organic acids at night. Results also suggest that two pools of soluble sugars exist in leaves of C. minor that perform CAM, one a vacuolar pool enriched in 13C and the second a transport pool depleted in 13C. Estimates of carbon-isotope discrimination expressed during CAM, derived from the trafficking among inorganic carbon, organic acids, and carbohydrate pools overnight, ranged from 0.9 to 3.1%[per mille (thousand) sign]. The [delta]13C of structural material did not change significantly between wet and dry seasons, indicating that most of the carbon used in growth was derived from C3 carboxylation.
- Published
- 1994
- Full Text
- View/download PDF
26. Short-term changes in carbon-isotope discrimination in the C 3 -CAM intermediate Clusia minor L. growing in Trinidad.
- Author
-
Borland AM, Griffiths H, Broadmeadow MS, Fordham MC, and Maxwell C
- Abstract
On-line instantaneous carbon isotope discrimination was measured in conjunction with net uptake of CO
2 in leaves of exposed and shaded plants of the C3 -CAM intermediate Clusia minor growing under natural conditions in Trinidad. At the end of the rainy season (late January-early February, 1992) C3 photosynthesis predominated although exposed leaves recaptured a small proportion of respiratory CO2 at night for the synthesis of malic acid. Citric acid was the major organic acid accumulated by exposed leaves at this time with a citric: malic acid ratio of 11:1. Values of instantaneous discrimination (Δ) in exposed leaves during the wet season rose from 17.1‰ shortly after dawn to 22.7‰ around mid-day just before stomata closed, suggesting that most CO2 was fixed by Rubisco at this time. During the late afternoon, instantaneous Δ declined from 22.2‰ to 17‰, probably reflecting the limited contribution from PEPc activity and an increase in diffusional resistance to CO2 in exposed leaves. Shaded leaves showed no CAM activity and CO2 uptake proceeded throughout the day in the wet season. The decrease in instantaneous Δ from 27‰ in the morning to 19.2‰ in the late afternoon was therefore entirely due to diffusional limitation. Leaves sampled in the dry season (mid-March, 1992) had by now induced full CAM activity with both malic and citric acids accumulated overnight and stomata closed for 4-5 h over the middle of the day. Values of instantaneous Δ measured over the first 3 h after dawn (6.4-9.1‰) indicated that C4 carboxylation dominated CO2 uptake for most of the morning when rates of photosynthesis were maximal, implying that under natural conditions, the down regulation of PEPc in phase II occurs much more slowly than laboratory-based studies have suggested. The contribution from C3 carboxylation to CO2 uptake during phase II was most marked in leaves which accumulated lower quantities of organic acids overnight. In exposed leaves, measurements of instantaneous Δ during the late afternoon illustrated the transition from C3 to C4 carboxylation with stomata remaining open during the transition from dusk into the dark period. Uptake of CO2 by shaded leaves during the late afternoon however appeared to be predominantly limited by decreased stomatal conductance. The short-term measurements of instantaneous Δ were subsequently integrated over 24 h in order to predict the leaf carbon isotope ratios (δp ) and to compare this with the δp measured for leaf organic material. Whilst there was close agreement between predicted and measured δp for plants sampled in the wet season, during the dry season the predicted carbon isotope ratios were 5-9‰ higher than the measured isotope ratios. During the annual cycle of leaf growth most carbon was fixed via the C3 pathway although CAM clearly plays an important role in maintaining photochemical integrity in the dry season.- Published
- 1993
- Full Text
- View/download PDF
27. The carbon isotope ratio of plant organic material reflects temporal and spatial variations in CO 2 within tropical forest formations in Trinidad.
- Author
-
Broadmeadow MS, Griffiths H, Maxwell C, and Borland AM
- Abstract
A method of monitoring and collecting CO
2 samples in the field has been developed which has been used to study both temporal and spatial variations in canopy CO2 isotopic signatures in two contrasting tropical forest formations in Trinidad. These have been related to vertical gradients in the carbon isotope ratio (δ13 C) of organic material in conjunction with measurements of other environmental parameters. The δ13 C of leaf material from two canopies showed a gradient with respect to height, more negative values being found low in the understorey. The deciduous secondary forest, (Simla) showed a difference of 4.6‰ and the semi-evergreen seasonal canopy (Aripo), 2.8‰. The range of δ13 C values at Simla was 4‰ less negative than those at Aripo. In order to relate these measurements to the interaction between diffusion or carboxylation limitation, and source CO2 effects, variations in environmental parameters through the canopy have been compared with changes in CO2 partial pressure (Pa ) and isotopic composition δ13 C throughout the day during the dry season. Values of Pa 20 m above the ground at Aripo varied from 380 vpm at dawn to 340 vpm at midday, at which time the partial pressure 15 cm above the ground was 375 vpm. The CO2 partial pressure did not stabilise during the course of the day, and there was good correlation (r2 =0.82) between δa and Pa , with more negative values of δa occuring in the understorey. Diuraal changes of 2‰ were evident at all canopy positions. In the more open canopy at Simla, these gradients were similar, but less marked. Leaf-air vapour pressure deficit (VPD) showed no relationship with height, possibly as a result of minimal water flux from both the soil and the canopy due to low soil water content; VPD was 1.5 kPa higher at midday than dawn. A 3° C temperature gradient between the understorey and upper canopy was observed at Aripo but not in the more open Simla canopy. CO2 partial pressure stabilised for only 4 h in the middle of the day, while other parameters showed no stable period. The proportion of floor respired CO2 reassimilated at Aripo has been calculated as 26%, 19%, and 8% for the periods 0600-1000, 1000-1400, and 1400-1800 hours. In order to quantify source CO2 effects, measurements of the environmental parameters and assimilation rate must be made at all canopy positions and throughout the day.- Published
- 1992
- Full Text
- View/download PDF
28. Short-term changes in carbon-isotope discrimination identify transitions between C3 and C 4 carboxylation during Crassulacean acid metabolism.
- Author
-
Griffiths H, Broadmeadow MS, Borland AM, and Hetherington CS
- Abstract
Short-term measurements of instantaneous carbon-isotope discrimination have been determined from mass-spectrometric analyses of CO2 collected online during gas exchange for the epiphytic bromeliad Tillandsia utriculata L. Using this technique, the isotopic signature of CO2 exchange for each phase of Crassulacean acid metabolism (CAM) has been characterised. During night-time fixation of CO2 (Phase I), discrimination (Δ) ranged from 4.4 to 6.6‰, equivalent to an effective carbon-isotope ratio (δ(13)C) of -12.3 to -14.5‰ versus Pee Dee Belemnite (PDB). These values reflected the gross photosynthetic balance between net CO2 uptake and refixation of respiratory CO2, characteristic of CAM in the Bromeliaceae. When Δ for the relative proportion of external (p a ) and internal (p i) CO2 is taken into account, calculated p i/p a decreased during the later part of the dark period from 0.68 to 0.48. Measurements of Δ during Phase II, early in the light period, showed the transition between C4 and C3 pathways, with carboxylation being increasingly dominated by ribulose bisphosphate carboxylase (Rubisco) as Δ increased from 10.5 to 21.2‰ During decarboxylation in the light period (Phase III), CO2 leaked out of the leaf and the inherent discrimination of Rubisco was expressed. The value of Δ calculated from on-line measurements (64.4‰) showed that the CO2 lost was considerably enriched in (13)C, and this was confirmed by direct analysis of the CO2 diffusing out into a CO2-free atmosphere (δ (13)C = + 51.6‰ versus PDB). Instantaneous discrimination was characteristic of the C3 pathway during Phase IV (late in the light period), but a reduction in Δ showed an increasing contribution from phosphoenolpyruvate carboxylase. The results from this non-invasive technique confirm the observations that "double carboxylation" involving both phosphoenolpyruvate carboxylase and Rubisco occurs during the transient phases of CAM (II and IV) in the light period.
- Published
- 1990
- Full Text
- View/download PDF
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