2021
DOI: 10.1007/s00027-021-00811-w
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Seedling adaptive characteristics of Phragmites australis to nutrient heterogeneity under salt stress using a split-root approach

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Cited by 7 publications
(5 citation statements)
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“…For seedlings, increasing salinity resulted in decreased growth rate, but the growth of rhizome-derived plants was optimum at 5 g L −1 salinity. Moreover, high soil nutrient heterogeneity can increase the negative effect of salinity on plant growth, as found in the study under controlled conditions [216]. In another study, 1.5 g L −1 NaCl did not result in growth inhibition, but all plants died at 35 g L −1 salinity [217].…”
Section: Phargmites Australismentioning
confidence: 62%
“…For seedlings, increasing salinity resulted in decreased growth rate, but the growth of rhizome-derived plants was optimum at 5 g L −1 salinity. Moreover, high soil nutrient heterogeneity can increase the negative effect of salinity on plant growth, as found in the study under controlled conditions [216]. In another study, 1.5 g L −1 NaCl did not result in growth inhibition, but all plants died at 35 g L −1 salinity [217].…”
Section: Phargmites Australismentioning
confidence: 62%
“…Although more research is needed to identify what limits native species plasticity, one possible explanation is that native P. australis need to limit unsustainable phenotypic responses to maintain resistance to some other abiotic and biotic stresses (Power et al., 2019; Valladares et al., 2007), such as salt pressure and predation pressure from native herbivores. For example, salt pressure was found to constrain the growth plasticity of native P. australis in response to N heterogeneity (Guan et al., 2021). Moreover, under herbivory pressure, native plant species should maintain a stable anti‐herbivore defence with low trait plasticity in response to variation in soil nutrient availability (Dawson et al., 2004; Shan et al., 2022).…”
Section: Discussionmentioning
confidence: 99%
“…Therefore, our study further improved the zonation method of a tidal flat on the basis of the principle of tidal correction [44], as shown in Figure 3. The specific steps of tidal correction in the coastal wetlands of the LRE are as follows: (1) our study calculated the tidal information at the scene center time of the RS images using the tide gauge data (see Table 1); the tide levels (h) of RS images received on 29 May 2021 and 20 October 2021 were 1.449 m and 1.265 m, respectively and the tide level difference (∆h) between the two images was 0.185 m. (2) The shoreline of the study area was divided into three sections due to the intricate terrains of the coastal wetlands in the LRE, as shown in Figure 4. Our study selected the instantaneous waterline (29 May 2021) as the baseline of the tide correction model, set the vertical line from the baseline to another instantaneous waterline every 300 m as the division line, and then calculated the average length of the division line in each shoreline to obtain the distance of two instantaneous waterlines in the same region (∆l).…”
Section: Tidal Flat Zonationmentioning
confidence: 99%
“…As the most vulnerable and economically important ecosystem in the world, coastal wetlands can provide sufficient nutrients and organic matter for marine animals and salt marsh plants living on a tidal flat, also playing a crucial role in ecological protection, biodiversity maintenance, flood prevention, and water purification [1][2][3]. One of the most active micro-geomorphology units of the tidal flat, tidal creeks are widely distributed in the coastal wetlands and connect to a bay or an estuary to transport nutrients, deliver sediments, and help in vegetation colonization and diffusion [4,5].…”
Section: Introductionmentioning
confidence: 99%