Variation in the degree of coupling between δ13C of phloem sap and ecosystem respiration in two mature Nothofagus forests

被引:54
作者
Barbour, MM
Hunt, JE
Dungan, RJ
Turnbull, MH
Brailsford, GW
Farquhar, GD
Whitehead, D
机构
[1] Landcare Res, Lincoln 8152, New Zealand
[2] Univ Canterbury, Sch Biol Sci, Christchurch 1, New Zealand
[3] Natl Inst Water & Atmospher Res, Wellington, New Zealand
[4] Australian Natl Univ, Res Sch Biol Sci, Canberra, ACT 2601, Australia
关键词
carbon-13; discrimination; ecosystem respiration; Keeling plot; Nothofagus; phloem sugar delta C-13;
D O I
10.1111/j.1469-8137.2005.01329.x
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
Day-to-day variability in the carbon isotope composition of phloem sap (delta C-13(hd)) and ecosystem respiratory CO2 (delta C-13(R)) were measured to assess the tightness of coupling between canopy photosynthesis (delta C-13(hd)) and ecosystem respiration (delta C-13(R)) in two mature Nothofagus solandri (Hook. f.) forests in New Zealand. Abundant phloem-tapping scale insects allowed repeated, nondestructive access to stem phloem sap 1-2 m above ground. delta C-13(hd) was compared with delta C-13 predicted by an environmentally driven, process-based canopy photosynthesis model. Keeling plots of within-canopy CO2 were used to estimate delta C-13(R). By including a lag of 3 d, there was good agreement in the timing and direction of variation in delta C-13(hd) and predictions by the canopy photosynthesis model, suggesting that delta C-13(hd) represents a photosynthesis-weighted, integrative record of canopy photosynthesis and conductance. Significant day-to-day variability in delta C-13(R) was recorded at one of the two forests. At this site, delta C-13(R) reflected variability in delta C-13(hd) only on days with < 2 mm rain. We conclude that the degree of coupling between canopy photosynthesis and ecosystem respiration varies between sites, and with environmental conditions at a single site.
引用
收藏
页码:497 / 512
页数:16
相关论文
共 66 条
[1]  
Bailey N. T. J., 1981, Statistical methods in biology, V2nd ed.
[2]   Global carbon sinks and their variability inferred from atmospheric O2 and δ13C [J].
Battle, M ;
Bender, ML ;
Tans, PP ;
White, JWC ;
Ellis, JT ;
Conway, T ;
Francey, RJ .
SCIENCE, 2000, 287 (5462) :2467-2470
[3]  
Benecke U., 1982, CARBON UPTAKE ALLOCA, P9
[4]   Tunable diode laser absorption spectroscopy for stable isotope studies of ecosystem-atmosphere CO2 exchange [J].
Bowling, DR ;
Sargent, SD ;
Tanner, BD ;
Ehleringer, JR .
AGRICULTURAL AND FOREST METEOROLOGY, 2003, 118 (1-2) :1-19
[5]   13C content of ecosystem respiration is linked to precipitation and vapor pressure deficit [J].
Bowling, DR ;
McDowell, NG ;
Bond, BJ ;
Law, BE ;
Ehleringer, JR .
OECOLOGIA, 2002, 131 (01) :113-124
[6]   Critical evaluation of micrometeorological methods for measuring ecosystem-atmosphere isotopic exchange of CO2 [J].
Bowling, DR ;
Pataki, DE ;
Ehleringer, JR .
AGRICULTURAL AND FOREST METEOROLOGY, 2003, 116 (3-4) :159-179
[7]   CORRELATION BETWEEN THE CARBON ISOTOPE DISCRIMINATION IN LEAF STARCH AND SUGARS OF C-3 PLANTS AND THE RATIO OF INTERCELLULAR AND ATMOSPHERIC PARTIAL PRESSURES OF CARBON-DIOXIDE [J].
BRUGNOLI, E ;
HUBICK, KT ;
VONCAEMMERER, S ;
WONG, SC ;
FARQUHAR, GD .
PLANT PHYSIOLOGY, 1988, 88 (04) :1418-1424
[8]  
Brugnoli E., 1998, STABLE ISOTOPES INTE, P133
[9]  
Brugnoli Enrico, 2000, VVolume 9, P399
[10]  
BUCHMANN N, 1998, STABLE ISOTOPES INTE, P203