What is the relationship between changes in canopy leaf area and changes in photosynthetic CO2 flux in arctic ecosystems?

被引:188
作者
Street, L. E. [1 ]
Shaver, G. R.
Williams, M.
Van Wijk, M. T.
机构
[1] Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA
[2] Univ Edinburgh, Sch Geosci, Inst Atmospher & Environm Sci, Edinburgh EH9 3JN, Midlothian, Scotland
[3] Univ Wageningen & Res Ctr, Plant Prod Syst, NL-6709 RZ Wageningen, Netherlands
基金
英国自然环境研究理事会;
关键词
Alaska; Arctic tundra; carbon balance; CO2; flux; gross primary productivity; landscape heterogeneity; leaf area index; light response; normalized difference vegetation index; Sweden;
D O I
10.1111/j.1365-2745.2006.01187.x
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
1 The arctic environment is highly heterogeneous in terms of plant distribution and productivity. If we are to make regional scale predictions of carbon exchange it is necessary to find robust relationships that can simplify this variability. One such potential relationship is that of leaf area to photosynthetic CO2 flux at the canopy scale. 2 In this paper we assess the effectiveness of canopy leaf area in explaining variation in gross primary productivity (GPP): (i) across different vegetation types; (ii) at various stages of leaf development; and (iii) under enhanced nutrient availability. To do this we measure net CO2 flux light response curves with a 1 x 1 m chamber, and calculate GPP at a photosynthetic photon flux density (PPFD) of 600 mu mol m(-2) s(-1). 3 At a subarctic site in Sweden, we report 10-fold variation in GPP among natural vegetation types with leaf area index (LAI) values of 0.05-2.31 m(2) m(-2). At a site of similar latitude in Alaska we document substantially elevated rates of GPP in fertilized vegetation. 4 We can explain 80% of the observed variation in GPP in natural vegetation (including vegetation measured before deciduous leaf bud burst) by leaf area alone, when leaf area is predicted from measurements of normalized difference vegetation index (NDVI). 5 In fertilized vegetation the relative increase in leaf area between control and fertilized treatments exceeds the relative increase in GPP. This suggests that higher leaf area causes increased self-shading, or that lower leaf nitrogen per unit leaf area causes a reduction in the rate of photosynthesis. 6 The results of this study indicate that canopy leaf area is an excellent predictor of GPP in diverse low arctic tundra, across a wide range of plant functional types.
引用
收藏
页码:139 / 150
页数:12
相关论文
共 35 条
[1]  
[Anonymous], 2004, IMPACTS WARMING ARCT
[2]   Inter-annual variability of NDVI in response to long-term warming and fertilization in wet sedge and tussock tundra [J].
Boelman, NT ;
Stieglitz, M ;
Griffin, KL ;
Shaver, GR .
OECOLOGIA, 2005, 143 (04) :588-597
[3]   Response of NDVI, biomass, and ecosystem gas exchange to long-term warming and fertilization in wet sedge tundra [J].
Boelman, NT ;
Stieglitz, M ;
Rueth, HM ;
Sommerkorn, M ;
Griffin, KL ;
Shaver, GR ;
Gamon, JA .
OECOLOGIA, 2003, 135 (03) :414-421
[4]   RESPONSES OF ARCTIC TUNDRA TO EXPERIMENTAL AND OBSERVED CHANGES IN CLIMATE [J].
CHAPIN, FS ;
SHAVER, GR ;
GIBLIN, AE ;
NADELHOFFER, KJ ;
LAUNDRE, JA .
ECOLOGY, 1995, 76 (03) :694-711
[5]   Responses of moist non-acidic arctic tundra to altered environment: productivity, biomass, and species richness [J].
Gough, L ;
Hobbie, SE .
OIKOS, 2003, 103 (01) :204-216
[6]   Dry heath arctic tundra responses to long-term nutrient and light manipulation [J].
Gough, L ;
Wookey, PA ;
Shaver, GR .
ARCTIC ANTARCTIC AND ALPINE RESEARCH, 2002, 34 (02) :211-218
[7]   Carbon and nitrogen cycling in soils from acidic and nonacidic tundra with different glacial histories in Northern Alaska [J].
Hobbie, SE ;
Miley, TA ;
Weiss, MS .
ECOSYSTEMS, 2002, 5 (08) :761-774
[8]   Species compositional differences on different-aged glacial landscapes drive contrasting responses of tundra to nutrient addition [J].
Hobbie, SE ;
Gough, L ;
Shaver, GR .
JOURNAL OF ECOLOGY, 2005, 93 (04) :770-782
[9]   Corrected calculations for soil and ecosystem measurements of CO2 flux using the LI-COR 6200 portable photosynthesis system [J].
Hooper, DU ;
Cardon, ZG ;
Chapin, FS ;
Durant, M .
OECOLOGIA, 2002, 132 (01) :1-11
[10]  
Johnson LC, 2000, ECOLOGY, V81, P453, DOI 10.1890/0012-9658(2000)081[0453:PCNICC]2.0.CO