2018
DOI: 10.1007/s40333-018-0069-z
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Stable isotope analysis of water sources for Tamarix laxa in the mega-dunes of the Badain Jaran Desert, China

Abstract: The complex interactions in desert ecosystems between functional types and environmental conditions could be reflected by plant water use patterns. However, the mechanisms underlying the water use patterns as well as the water sources of Tamarix laxa in the mega-dunes of the Badain Jaran Desert, China, remain unclear. This study investigated the water sources and water use patterns of T. laxa using the stable oxygen isotope method. The δ 18 O values of xylem water, soil water in different layers (0-200 cm), ra… Show more

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Cited by 13 publications
(19 citation statements)
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“…Previous studies have demonstrated the enrichment of the heavy isotopes in the shallow soil water relative to the deep soil water and groundwater because of soil surface evaporation (Gat et al, 2007;Zhang et al, 2018). It should be noted that soil water was not extracted from the 0-80 cm soil depth in the Tazhong site and from the 0-20 cm soil depth in the Aral site due to the extreme low SWC in these soil layers.…”
Section: Figmentioning
confidence: 97%
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“…Previous studies have demonstrated the enrichment of the heavy isotopes in the shallow soil water relative to the deep soil water and groundwater because of soil surface evaporation (Gat et al, 2007;Zhang et al, 2018). It should be noted that soil water was not extracted from the 0-80 cm soil depth in the Tazhong site and from the 0-20 cm soil depth in the Aral site due to the extreme low SWC in these soil layers.…”
Section: Figmentioning
confidence: 97%
“…Water is an indispensable factor for plant growth, vegetation distribution and community composition (Rosenthal et al, 2005;Zhou et al, 2013;Zhang et al, 2018). In the desert ecosystem, water is extraordinarily valuable and has a decisive impact on the survival and distribution of plants.…”
Section: Introductionmentioning
confidence: 99%
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“…Based on the δ 13 C value, which is often used to distinguish carbon assimilation or water use strategy, T. ramosissima is traditionally regarded as a C 3 plant ( Zhang et al 2017 ). However, variations in the δ 13 C value caused by the influence of temperature, wind speed, precipitation and relative humidity (RH) ( Zhang et al 2018 ) also reflect conversion of water use strategy. In addition, a complete set of core genes of C 4 carbon fixation were found not only in the two Tamarix species, namely, T. ramosissima and Tamarix chinensis ( Swaminathan et al 2020 ), but also in Reaumuria soongorica , which belongs to the same family as Tamarix spp.…”
Section: Introductionmentioning
confidence: 99%