2023
DOI: 10.3389/fpls.2022.1060686
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C:N:P stoichiometry in plant, soil and microbe in Sophora moorcroftiana shrubs across three sandy dune types in the middle reaches of the Yarlung Zangbo River

Abstract: The alpine sandy dune ecosystem is highly vulnerable to global climate change. Ecological stoichiometry in plants and soils plays a crucial role in biogeochemical cycles, energy flow and functioning in ecosystems. The alpine sandy dune ecosystem is highly vulnerable to global climate change. However, the stoichiometric changes and correlations of plants and soils among different types of sandy dunes have not been fully explored. Three sandy dune types (moving dune, MD; semifixed dune, SFD; and fixed dune, FD) … Show more

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Cited by 4 publications
(2 citation statements)
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“…Considerable nutrient variation can be observed both among the same organs of different plants and among different organs of the individual plant (Figure 2). This finding is consistent with previous studies conducted on vegetation types in western alpine swamp wetlands (Wu et al, 2023), and typical dune vegetation in the Yarlung Tsangpo River (Dong, Yang, et al, 2023). The driving factor behind this phenomenon is the different N and P demands across various halophytes, which consequently influence photosynthesis and carbon allocation capacities, thereby leading to nutrient content and ratio variations among these plants (Li, Sun, & Fu, 2021).…”
Section: Discussionsupporting
confidence: 93%
“…Considerable nutrient variation can be observed both among the same organs of different plants and among different organs of the individual plant (Figure 2). This finding is consistent with previous studies conducted on vegetation types in western alpine swamp wetlands (Wu et al, 2023), and typical dune vegetation in the Yarlung Tsangpo River (Dong, Yang, et al, 2023). The driving factor behind this phenomenon is the different N and P demands across various halophytes, which consequently influence photosynthesis and carbon allocation capacities, thereby leading to nutrient content and ratio variations among these plants (Li, Sun, & Fu, 2021).…”
Section: Discussionsupporting
confidence: 93%
“…The dried soil samples (5.0 g) were added to 25 mL of distilled water in a stomacher to homogenize at 10,000 r/min and were kept for 30 min at room temperature to obtain clear supernatant for pH determination [36]. The soil samples were collected in five volumetric soil rings (volume 100 cm 3 ) to determine the soil bulk density [36]. Soil organic carbon content was determined with K 2 Cr 2 O 7 oxidation and FeSO 4 titration methods [37].…”
Section: Analysis Of Plant and Soil Physicochemical Propertiesmentioning
confidence: 99%