2021
DOI: 10.1007/s00442-021-04940-9
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Dew water-uptake pathways in Negev desert plants: a study using stable isotope tracers

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Cited by 8 publications
(11 citation statements)
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“…As a result of this dependency on the third layer, epiphytic biomass and diversity are frequently higher in humid montane forests characterised by frequent occult precipitation events and relatively low evaporative demand (Zotz, 2016). Another example of segregation along the atmospheric resource‐axis comes from hyper‐arid areas, such as the Atacama and Namib deserts, where rainfall events are sporadic and may wet plant canopies, but rarely result in a substantial increase in soil moisture (Hill et al, 2015, 2021). Many ground‐rooted plant species growing in such environments appear to obtain both water and nutrients primarily from fog and dew rather than from rainwater (e.g.…”
Section: How Does Accessing Atmospheric Resources Contribute To Hydro...mentioning
confidence: 99%
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“…As a result of this dependency on the third layer, epiphytic biomass and diversity are frequently higher in humid montane forests characterised by frequent occult precipitation events and relatively low evaporative demand (Zotz, 2016). Another example of segregation along the atmospheric resource‐axis comes from hyper‐arid areas, such as the Atacama and Namib deserts, where rainfall events are sporadic and may wet plant canopies, but rarely result in a substantial increase in soil moisture (Hill et al, 2015, 2021). Many ground‐rooted plant species growing in such environments appear to obtain both water and nutrients primarily from fog and dew rather than from rainwater (e.g.…”
Section: How Does Accessing Atmospheric Resources Contribute To Hydro...mentioning
confidence: 99%
“…Another example of segregation along the atmospheric resourceaxis comes from hyper-arid areas, such as the Atacama and Namib deserts, where rainfall events are sporadic and may wet plant canopies, but rarely result in a substantial increase in soil moisture (Hill et al, 2015(Hill et al, , 2021. Many ground-rooted plant species growing in such environments appear to obtain both water and nutrients primarily from fog and dew rather than from rainwater (e.g.…”
Section: Spatial Hydrological Niche Segregationmentioning
confidence: 99%
“…However, we established that for F. bungeana, the percentage utilization of soil water was highest in the 0-30 cm soil layer, and was not restricted by either root hydraulic conductivity or the soil water potential of this layer, which consequently posed the question as to which absorption path is operational under these conditions. The findings of numerous studies have revealed that dew uptake by plants occurs in most deserts where water is limited by the scarcity of precipitation (Hill et al, 2015;Dawson and Goldsmith, 2018;Berry et al, 2019;Hill et al, 2021). For example, Hill et al (2015) found that some dominant desert plants derive approximately 50% of their water requirements from dew (Hill et al, 2015), and several studies have provided evidence to indicate direct entry of dew water into leaves (Cavallaro et al, 2020), water uptake pathways into leaves through the cuticle (Gouvra and Grammatikopoulos, 2003;Goldsmith et al, 2017), and water uptake through stems (Breshears et al, 2008;Mason et al, 2016).…”
Section: Discussion Variation In Water Sourcesmentioning
confidence: 99%
“…For example, Hill et al (2015) found that some dominant desert plants derive approximately 50% of their water requirements from dew (Hill et al, 2015), and several studies have provided evidence to indicate direct entry of dew water into leaves (Cavallaro et al, 2020), water uptake pathways into leaves through the cuticle (Gouvra and Grammatikopoulos, 2003;Goldsmith et al, 2017), and water uptake through stems (Breshears et al, 2008;Mason et al, 2016). Hill et al (2021) also demonstrated that desert plants utilize dew on leaves (including direct absorption of dew by leaves and root absorption of dew falling onto the surface soil), transfer this water to the roots, and subsequent transport the water to the stems via different routes (Hill et al, 2021). It is thus conceivable that the input of dew with the same isotopic values as the upper soil causes a negative correlation between the proportion of water absorbed from the 0-30 cm soil layer and the soil potential of this layer, whereas the direct absorption of water via the leaves would account for the lack of correlation between the water source and hydraulic conductivity of the root system.…”
Section: Discussion Variation In Water Sourcesmentioning
confidence: 99%
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