Francey R J Farquhar G D A n ex plan at ion of .3 C/.2C variat ions in t ree ring s N at ure,1982,297:28~3.
[2]
L eavit t S W,Long A S ampin g st rategy f or st abl e carb on isot ope analysis of t ree ring s in pin e N atu re,1984,311:145~147
[3]
S heu D D,K ou P,Chiu C H,e t al V ariabilit y of tr ee ring .3C in Taiw an fi r:growt h ef f ect and response t o M ayO ct ober t emperat ures G eochemi ca et Cosm ochimica A ct a,1996,60(1):171~177
[4]
N gu yen Q uey rens A,Ferhi A,Loust au D,e t al W it hin ring .3 C s pat ial variabilit y an d in t erannual variat ions inw ood cel lulose of tw o cont rast ing provenances of P i nus p inast er Canada Journ al of Forest R es earch,1998,28:766~773
[5]
Panek J A,W arin g R H Carbon i sot op e variati on in Douglas fir f ol iage:im provin g t he cl imat e relat ions hip TreePhys iology,1995,15(10):657~663
S aur er M,Sigent h aler U The climat e carbon isot ope r elat ion ship in t ree ring s and t h e signif icance of si te condit ions T ell us,1995,(46B):320~330
[8]
M cCarroll D,Paw el lek F S tabl e carb on isot ope rati os of P inus syl v est ri s f rom nort hern Fin lan d and t he pot en tialf or ext ract ing a clim at e si gnal f rom long Fennoscandian chr on ol ogi es T he H ol ocen e,2001,11:517~526
[9]
K eel ing C D,M ook W G,T an s P P R ecent t rends in t he .3C/.2 C rat io of at mosph eric carb on diox ide N atu re,1979,277:121~123
X u H L,Wang R,G au t hier L,et al T om at o l eaf phot os ynt het ic responses t o h umidit y and t emperat ure under s alin ity and w at er def icit Pedosph ere,1999,9(2):105~112
[13]
K e S Z,Liu Z R,Q ian J L,et al A ngular di st ribut ion of elem ent cont ent s in t ree rings and t h e environment al inf ormati on Pedos pher e,1999,9(1):6~76
[14]
Q ian J L,K e S Z,H uang J S,et a l Correlati on bet w een chemical element s cont ent s in t ree rings an d soils Pedos pher e,1993,3(4):309~319
[15]
T ans P P,M ook W G Past at mos pheri c CO 2 levels an d t he.3C/.2 C rat ions in t ree rings T el lus,1980,32(3):268~283
[16]
Francey R J Tasmanian t ree rings belie su gg est ed ant hropogeni c 13C/12C t rend s N at ure,1981,297:232~235
[17]
S chl eser G H,H el le G,L cke A,et al Is ot ope signals as cl imate proxies:t he rol e of t ran sfer f unct ions in t hes tu dy of t erres t rial archives Quat er nar y S ci ence Re v ie w s,1999,18(7):927~943
M cCarroll D,Loader N J St able is ot opes in t ree rings Q uat ernary Science R eview s,2004,23:771~80.
[24]
Farquhar G D,O/l eary M H,Berry J A O n th e relat ionsh ip bet w een carbon isot ope discriminat ion and t h e i nt ercellu lar carbon dioxide con cen trat ion in l eaves A ust ralian Journal of Plan t Physiol ogy,1982,9:121~137
[25]
Farquhar G D,Wong S C A n empiri cal m odel of st omat a conduct ance A ust ralian Journal of Plant Physiology,#1984,..:.9.~.20
[26]
Zimm erman J K,Eh lerin ger J R Carbon isot ope rat ios are correl at ed w it h ir radiance level s in t he Panamanian orchid Cat aset um viridif lavu m O ecologia,1990,83:247~249
[27]
K rn er C,Farquh ar G D,W ong S C Carbon is ot ope discrim inat ion b y plan t s f ol low s lat itu dinal and alt it udinalt rends Oec ol ogi a(B erl),1991,88:30~40
[28]
Reindl D T,Beckm ann W A,D uff ie J A E valuat ion of hourly t ilt ed surf ace radiat ion model s Sol ar En ergy,1990,45:9~17
[29]
查良松我国太阳辐射量区域性变化特征研究地理研究,1996,15(2):21~27
[30]
Waring R H,S ilvest er W B V ariat ion in foliar .3 C values w it hin t he crow ns of P i nus radiat e t rees T ree Physiology,1994,14:1203~1213
[31]
Zhang H,Sharit i M R,N ob el P S Phot osynt het ic charact eris ti cs of s un vs shade plant s of Encel i a f ar inosa asaf fect ed by phot osynt heti c p hot on f lux den sit y,int ercellul ar CO 2 con cent rat ion,l eaf w at er pot en ti al an d leaf temperat u re A ust ralian J ou rnal of Plant Ph ysiology,1995,22:833~84.