Chiang Po Neng, Wang Ming Kuang, Chiu Chi Yu, King Hen Biau, Hwong Jeen Lian
Soil Laboratory, Department of Agricultural Chemistry, National Taiwan University, Taipei, Taiwan 10764, ROC.
Chemosphere. 2004 Jan;54(2):217-24. doi: 10.1016/j.chemosphere.2003.07.005.
The carbon isotope analysis [delta13C values] of organic samples can be a useful research in ecological studies because delta13C values are indicative of the plant source. This study investigated the changes in plant communities along the grassland-forest boundary in the alpine forest at Ta-Ta-Chia long term ecological research (LTER) site in central Taiwan using carbon isotope data. The aim of this study was focused on the forest fire affected the change of vegetation community. Four pedons from grassland dominated by Miscanthus transmorrisonensis (pedons 1 and 2), transition zone by Tsuga and Yushania nittakeyamensis (pedon 3), and forest zone by Tsuga and nittakeyamensis (pedon 4) were examined. Soil organic matter (SOM) delta13C values in the upper soil horizon were similar to delta13C values of the overlaying vegetation types. This indicates that the boundary between these plant communities remained the same in the past decades. The delta13C values of the grassland SOM ranged from -19.4 per thousand to -24.1 per thousand, showing decrease with soil depth. This suggests that C4 plants (transmorrisonensis) have replaced C3 plants of Tsuga and nittakeyamensis. The delta13C values of the Tsuga forest area (pedon 4) range from -27.0 per thousand to -23.5 per thousand and showed only slight change with soil depth, implying that C3 plants have remained the major species in the forest.
有机样本的碳同位素分析(δ13C值)在生态研究中可能是一项有用的研究,因为δ13C值可指示植物来源。本研究利用碳同位素数据,调查了台湾中部塔塔加长期生态研究(LTER)站点高山森林中草地 - 森林边界沿线植物群落的变化。本研究的目的聚焦于森林火灾如何影响植被群落的变化。研究了四个土样,分别来自以高山芒为主的草地(土样1和2)、以铁杉和玉山箭竹为主的过渡带(土样3)以及以铁杉和玉山箭竹为主的森林带(土样4)。上层土壤层中土壤有机质(SOM)的δ13C值与上层植被类型的δ13C值相似。这表明在过去几十年中,这些植物群落之间的边界保持不变。草地SOM的δ13C值范围为千分之 -19.4至千分之 -24.1,随土壤深度增加而降低。这表明C4植物(高山芒)已取代了铁杉和玉山箭竹的C3植物。铁杉林区(土样4)的δ13C值范围为千分之 -27.0至千分之 -23.5,且随土壤深度变化不大,这意味着C3植物仍然是森林中的主要物种。