Water sources of dominant species in three alpine ecosystems on the Tibetan Plateau, China

Journal of Integrative Plant Biology
De-Yu DuanQi-Wu Hu

Abstract

Plant water sources were estimated by two or three compartment linear mixing models using hydrogen and oxygen isotope (deltaD and delta18O) values of different components such as plant xylem water, precipitation and river water as well as soil water on the Tibetan Plateau in the summer of 2005. Four dominant species (Quercus aquifolioides, Pinus tabulaeformis, Salix rehderiana and Nitraria tangutorum) in three typical ecosystems (forest, shrub and desert) were investigated in this study. Stable isotope ratios of the summer precipitations and the soil water presented variations in spatial and temporal scales. delta18O values of N. tangutorum xylem water were constant in the whole growth season and very similar to those of deep soil water. Water sources for all of the plants came from both precipitations and soil water. Plants switched rapidly among different water sources when environmental water conditions changed. Rainwater had different contributions to the plants, which was influenced by amounts of precipitation. The percentage of plant xylem water derived from rainwater rose with an increase in precipitation. Water sources for broad-leaved and coniferous species were different although they grew in the same environmental co...Continue Reading

References

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Mar 26, 2003·Tree Physiology·Paula C. JacksonFabio Causin
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