Arctic, Antarctic, and Alpine Research 41(4):426-433. 2009
doi: http://dx.doi.org/10.1657/1938-4246-41.4.426

Determination of Leaf Area Index, Total Foliar N, and Normalized Difference Vegetation Index for Arctic Ecosystems Dominated by Cassiope tetragona

Matteo Campioli*,$, Lorna E. Street, Anders Michelsen, Gaius R. Shaver§, Thomas Maere#, Roeland Samson@, and Raoul Lemeur*

*Department of Applied Ecology and Environmental Biology, Ghent University, B-9000 Ghent, Belgium

School of GeoSciences, University of Edinburgh, Edinburgh, EH9 3JN, U.K

Department of Biology, University of Copenhagen, DK-1353 Copenhagen K, Denmark

§The Ecosystems Center, Marine Biological Laboratory, Woods Hole, Massachusetts 02543, U.S.A

#BIOMATH, Ghent University, B-9000 Ghent, Belgium

@Department of Bioscience Engineering, University of Antwerp, B-2020 Antwerp, Belgium

$Corresponding author. Present address: Research Group of Plant and Vegetation Ecology, University of Antwerp, Universiteitsplein 1, B-2610 Wilrijk, Belgium

Abstract

Leaf area index (LAI) and total foliar nitrogen (TFN) are important canopy characteristics and crucial variables needed to simulate photosynthesis and ecosystem CO2 fluxes. Although plant communities dominated by Cassiope tetragona are widespread in the Arctic, LAI and TFN for this vegetation type have not been accurately quantified. We address this knowledge gap by (i) direct measurements of LAI and TFN for C. tetragona, and (ii) determining TFN-LAI and LAI–normalized difference vegetation index (NDVI) relationships for typical C. tetragona tundras in the subarctic (Sweden) and High Arctic (Greenland and Svalbard).

Leaves of C. tetragona are 2–6 mm long and closely appressed to their stems forming parallelepiped shoots. We determined the LAI of C. tetragona by measuring the area of the leaves while still attached to the stem, then doubling the resulting one-sided area. TFN was determined from leaf N and biomass. The LAI-NDVI and TFN-LAI relationships showed high correlation and can be used to estimate indirectly LAI and TFN. The LAI-NDVI relationship for C. tetragona vegetation differed from a generic LAI-NDVI relationship for arctic tundra, whereas the TFN-LAI relationship did not. Overall, the LAI of C. tetragona tundra ranged from 0.4 to 1.1 m2 m−2 and TFN from 1.4 to 1.7 g N m−2.

Accepted: April 2009



References Cited

ACIA 2004. Impact of a Warming Arctic: Arctic Climate Impact Assessment. Cambridge and New York Cambridge University Press. 140 pp.
Baddeley, J. A., S. J. Woodin, and I. J. Alexander. 1994. Effects of increased nitrogen and phosphorus availability on the photosynthesis and nutrient relations of three arctic dwarf shrubs from Svalbard. Functional Ecology 8:676685. CrossRef, CSA
Bay, C. 1998. Vegetation mapping of Zackenberg valley, Northeast Greenland Danish Polar Center and Botanical Museum, University of Copenhagen. 29 pp. http://www.dpc.dk/sw13186.asp.
Berg, A., S. Kjelvik, and F. E. Wielgolaski. 1975. Measurements of leaf areas and leaf angles of plants in Hardangervidda, Norway. In Wielgolaski, F. E. Fennoscandian Tundra Ecosystems. Part 1: Plants and Microorganisms. Springer-Verlag. Berlin. 103110.
Berglund, B. E., L. Barnekow, D. Hammarlund, P. Sandgren, and I. F. Snowball. 1996. Holocene forest dynamics and climate changes in the Abisko area, northern Sweden—The Sonesson model of vegetation history reconsidered and confirmed. Ecological Bulletins 45:1530.
Bliss, L. C., J. Kerik, and W. Peterson. 1987. Primary production of dwarf shrub heath communities, Truelove Lowland. In Bliss, L. C. Truelove Lowland, Devon Island, Canada: a High Arctic Ecosystem. Edmonton University of Alberta Press. 217224.
Callaghan, T. V., B. A. Carlsson, and N. J. C. Tyler. 1989. Historical records of climate-related growth in Cassiope tetragona from the Arctic. Journal of Ecology 77:823837. CrossRef, CSA
Campioli, M. 2008. Carbon allocation in ecosystems: an experimental and modelling approach for tundra and forest vegetations. PhD thesis. Ghent, Belgium Ghent University. 177 pp.
Campioli, M., A. Michelsen, A. Demey, A. Vermeulen, R. Samson, and R. Lemeur. 2009. Net primary production and carbon stocks for subarctic mesic-dry tundras with contrasting microtopography, altitude, and dominant species. Ecosystems 12:760776. CrossRef
Chen, J. M. and T. A. Black. 1992. Defining leaf area index for non-flat leaves. Plant Cell and Environment 15:421429. CrossRef
Christiansen, H. H. and O. Humlum. 1993. Glacial history and periglacial landforms of the Zackenberg area, Northeast Greenland: Preliminary results. Geografisk Tidsskrift 93:1929.
Graglia, E., S. Jonasson, A. Michelsen, I. K. Schmidt, M. Havström, and L. Gustavsson. 2001. Effects of environmental perturbations on abundance of subarctic plants after three, seven and ten years of treatments. Ecography 24:512. CrossRef, CSA
Groendahl, L., T. Friborg, and H. Soegaard. 2007. Temperature and snow-melt controls on interannual variability in carbon exchange in the High Arctic. Theoretical and Applied Climatology 88:111125. CrossRef
Grogan, P. and S. Jonasson. 2005. Temperature and substrate controls on intra-annual variation in ecosystem respiration in two subarctic vegetation types. Global Change Biology 11:465475. CrossRef
Havström, M., T. V. Callaghan, and S. Jonasson. 1993. Differential growth-responses of Cassiope tetragona, an arctic dwarf shrub, to environmental perturbations among three contrasting high sites and sub-arctic sites. Oikos 66:389402. CrossRef
Illeris, L., S. M. König, P. Grogan, S. Jonasson, A. Michelsen, and H. Ro-Poulsen. 2004. Growing-season carbon dioxide flux in a dry subarctic heath: responses to long-term manipulations. Arctic Antarctic, and Alpine Research 36:456463. BioOne
Jonasson, S. 1989. Implications of leaf longevity, leaf nutrient reabsorption and translocation for the resource economy of five evergreen plant species. Oikos 56:121131. CrossRef, CSA
Jonasson, S., A. Michelsen, and I. K. Schmidt. 1999a. Coupling of nutrient cycling and carbon dynamics in the Arctic; integration of soil microbial and plant processes. Applied Soil Ecology 11:135146. CrossRef
Jonasson, S., A. Michelsen, I. K. Schmidt, and E. V. Nielsen. 1999b. Responses in microbes and plants to changed temperature, nutrient, and light regimes in the Arctic. Ecology 80:18281843. CrossRef, CSA
Jonckheere, I., S. Fleck, K. Nackaerts, B. Muys, P. Coppin, M. Weiss, and F. Baret. 2004. Review of methods for in situ leaf area index determination—Part I. Theories, sensors and hemispherical photography. Agricultural and Forest Meteorology 121:1935. CrossRef
Kudo, G., U. Nordenhall, and U. Molau. 1999. Effects of snowmelt timing on leaf traits, leaf production, and shoot growth of alpine plants: comparisons along a snowmelt gradient in northern Sweden. Ecoscience 6:439450.
Lønne, I. and W. Nemec. 2004. High-arctic fan delta recording deglaciation and environment disequilibrium. Sedimentology 51:553589. CrossRef
Michelsen, A., S. Jonasson, D. Sleep, M. Havström, and T. V. Callaghan. 1996. Shoot biomass, delta C13, nitrogen and chlorophyll responses of two arctic dwarf shrubs to in situ shading, nutrient application and warming simulating climatic change. Oecologia 105:112. CrossRef, CSA
Molau, U. 1997. Responses to natural climatic variation and experimental warming in two tundra plant species with contrasting life forms: Cassiope tetragona and Ranunculus nivalis. Global Change Biology 3:97107. CrossRef, CSA
Nams, M. L. N. and B. Freedman. 1987a. Ecology of heath communities dominated by Cassiope tetragona at Alexandra Fiord, Ellesmere Island, Canada. Ecography 10:2232. CrossRef
Nams, M. L. N. and B. Freedman. 1987b. Phenology and resource allocation in a high arctic evergreen dwarf shrub, Cassiope tetragona. Ecography 10:128136. CrossRef
Rennermalm, A. K., H. Soegaard, and C. Nordstroem. 2005. Interannual variability in carbon dioxide exchange from a high arctic fen estimated by measurements and modeling. Arctic, Antarctic, and Alpine Research 37:545556. BioOne
Shaver, G. R., L. E. Street, E. B. Rastetter, M. T. van Wijk, and M. Williams. 2007. Functional convergence in regulation of net CO2 flux in heterogeneous tundra landscapes in Alaska and Sweden. Journal of Ecology 95:802817. CrossRef
Sigsgaard, C., D. Petersen, L. Groendahl, K. Thorsøe, H. Meltofte, M. Tamstorf, and B. U. Hansen. 2006. The Climate Basis and GeoBasis programmes. In Klitgaard, A. B., M. Rasch, and K. Caning. Zackenberg Ecological Research Operations, 11th Annual Report, 2006. Copenhagen Danish Polar Center. 1135.
Soegaard, H., C. Nordstroem, T. Friborg, B. U. Hansen, T. R. Christensen, and C. Bay. 2000. Trace gas exchange in a high-arctic valley 3. Integrating and scaling CO2 fluxes from canopy to landscape using flux data, footprint modeling, and remote sensing. Global Biogeochemical Cycles 14:725744. CrossRef, CSA
Steltzer, H. and J. M. Welker. 2006. Modeling the effect of photosynthetic vegetation properties on the NDVI-LAI relationship. Ecology 87:27652772. CrossRef, PubMed
Street, L. E., G. R. Shaver, M. Williams, and M. T. van Wijk. 2007. What is the relationship between changes in canopy leaf area and changes in photosynthetic CO2 flux in arctic ecosystems? Journal of Ecology 95:139150. CrossRef
Svoboda, J. 1987. Ecology and primary production of raised beach communities, Truelove Lowland. In Bliss, L. C. Truelove Lowland, Devon Island, Canada: a High Arctic Ecosystem. Edmonton University of Alberta Press. 185216.
van Wijk, M. T. and M. Williams. 2005. Optical instruments for measuring leaf area index in low vegetation: application in arctic ecosystems. Ecological Applications 15:14621470. CrossRef
van Wijk, M. T., M. Williams, and G. R. Shaver. 2005. Tight coupling between leaf area index and foliage N content in arctic plant communities. Oecologia 142:421427. CrossRef, PubMed
Watson, D. J. 1947. Comparative physiological studies in the growth of field crops. I. Variation in net assimilation rate and leaf area between species and varieties, and within and between years. Annals of Botany 11:4176.
Wielgolaski, F. E., S. Kjelvik, and P. Kallio. 1975. Mineral content of tundra and forest plants in Fennoscandia. In Wielgolaski, F. E. Fennoscandian Tundra Ecosystems. Part 1: Plants and Microorganisms. Berlin Springer-Verlag. 316332.
Williams, M. and E. B. Rastetter. 1999. Vegetation characteristics and primary productivity along an arctic transect: implications for scaling-up. Journal of Ecology 87:885898. CrossRef
Williams, M., W. Eugster, E. B. Rastetter, J. P. McFadden, and F. S. Chapin. 2000. The controls on net ecosystem productivity along an arctic transect: a model comparison with flux measurements. Global Change Biology 6:116126. CrossRef, CSA
Williams, M., L. E. Street, M. T. van Wijk, and G. R. Shaver. 2006. Identifying differences in carbon exchange among arctic ecosystem types. Ecosystems 9:288304. CrossRef

1Wind-exposed site with sparse vegetation (less than 20% of the total cover) and very dry soil.

Cited by

Terry V. Callaghan, Torben R. Christensen, Elin J. Jantze. (2011) Plant and Vegetation Dynamics on Disko Island, West Greenland: Snapshots Separated by Over 40 Years. AMBIO: A Journal of the Human Environment 40:6, 624-637
Online publication date: 1-Sep-2011.

Abstract & References : Full Text : PDF (736 KB) : Rights & Permissions 

 
BioOne is the product of innovative collaboration between scientific societies, libraries, academe and the private sector.
 
21 Dupont Circle NW, Suite 800, Washington, DC 20036 • Phone 202.296.1605 • Fax 202.872.0884
 
Copyright © 2012 BioOne All rights reserved