LI Xiang bo, CHEN Jian fa, ZHANG Ping zhong, LIU Guang xiu. The Characteristics of Carbon Isotope Composition of Modern Plants over Qinghai-Tibet Plateau (NE) and Its Climatic Information[J]. Acta Sedimentologica Sinica, 1999, 17(2): 325-329.
Citation:
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LI Xiang bo, CHEN Jian fa, ZHANG Ping zhong, LIU Guang xiu. The Characteristics of Carbon Isotope Composition of Modern Plants over Qinghai-Tibet Plateau (NE) and Its Climatic Information[J]. Acta Sedimentologica Sinica, 1999, 17(2): 325-329.
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The Characteristics of Carbon Isotope Composition of Modern Plants over Qinghai-Tibet Plateau (NE) and Its Climatic Information
- 1.
Northwest Institute of Geology, CUNPE Lanzhou 730020;
- 2.
Lanzhou Institute of Geology Chinnse Academy of Sciences Lanzhou 730000
- Received Date: 1998-03-04
- Rev Recd Date:
1998-07-30
- Publish Date:
1999-06-10
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Abstract
Global change become a world wide concerned problem in the recent years. The study of plant carbon isotopic composition become an important field in the research of global change,in which a fundamental goal is to determine the contro ling factors of plant carbon isotope discrimination and composition. The paper gives an analysis on the carbon isotope composition of modern plants ( all are C3 species) in Qinghai-Tibet plateau(NE)and a detailed discussion on t he various factors that can influence it. The value of δ13C of 61 samples varies from -23.5‰ to -30.8‰,with an average of -26.6‰. Analysis shows that with the same plant the δ13C value increases with the increase of altitu de and decresases with the increase of latitude.The result of this study shows t hat precipitation,air moisture and pressure are the most important environmental factors to the change of δ13C. The less the amount of precipitation, the more positive the plant δ13C values are. On the other hand,the higher th e air pressure the more negative the δ13C values are. It is now clear tha t plant δ13C value relates directly to the assimilation of leaf to CO2( A),leaf stomatic conductance(g) and intercellular/ambient partial pressure ratio (Pi/Pa). A(cording to) their effect on A, g and Pi/Pa,it is clear that the precipitation, air moisture and pressure cause the change of plant δ13C value. The study suggests that a lot of information reflecting the change of nature env ironmental can be recorded in plants.So it is completely possible to extract cli matic information from plant δ13C.
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References
[1]
|
王富葆,阎革,林本海等.若尔盖高原泥炭δ13C的初步研究[ J] .科学通报,1993,38(1):65~67 |
[2]
|
张平中,王先彬,陈践发等.湖相有机质的氢指数及碳同位素组成—湖面波动评 价的指标—以RH孔为例[J] .科学通报,1995,40(18):1682~1685 |
[3]
|
CerLing T E, Quade J, Wang Y, Bowman J R. Carbon isotopes i n Soils and Palaeosoils as ecology and palaeoecology indicators[J] . Nature, 19 89,341:138~139 |
[4]
|
Humphrey J D,Ferring C R. Stable isotopic evidence for latest pleistocene and holocene climatic change in North-Central Texas[J] . Quaterna ry Research, 1994, 41:200~213 |
[5]
|
K?rner Ch, Farquhar G D. Roksandic Z. A global survey of carbon isotope discrimination in plants from high altitude[J] . Oecologia, 198 8,74:623~632 |
[6]
|
K?rner Oh, Farquhar G D, Wang S C. Carbon isotope discriminat e by pants follows latitudinal and altitudinal trends[J] . Oecologia, 199 1,88:30~40 |
[7]
|
Balesdent J. Site-Related δ13C of tree leaves and soil orga nic matter in a temperate forest[J] . Ecology, 1993,74(6):1 713~1 721 |
[8]
|
Saurer M, Sigenthaler U. The climate-carbon isotope relationship in tree rings and the significance of site conditions[J] . Tellus,1995,46B:32 0~330 |
[9]
|
Farquhar G D, Ehleringer J R, Hubick K T. Carbon isotope discri mination and photosynthesis[J] . Ann Rev Plant physiol 1989,40:503~537 |
[10]
|
Farquhar G D, O′leary M H, Berry J A. On the relationship betwe en carbon isotope discrimination and intercellalar carbon dioxide concentration in leaves[J] . Aust. J. Plant Physiol, 1982,9:121~137 |
[11]
|
Francey R J, Farquhar G D. An explanation of 13C/12C variations in tree rings[J] . Nature, 1982, 295:28-31 |
[12]
|
Vogel J C. Recycling of carbon in a forest environment[J] . Oecol. P lant, 1978, 13:89~94 |
[13]
|
Stuiver M, Braziunas T F, Tree cellulose 13C/12 C isotope ratios and climatic change[J] . Nature,1987, 328:58~60 |
[14]
|
Farquhar G D, Wong S C. An empirical model of stomatal conducta nce[J] . Aust. J. Plant Physiol, 1984,11:191~210 |
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Proportional views
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