2013
DOI: 10.1111/nph.12284
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Ammonium first: natural mosses prefer atmospheric ammonium but vary utilization of dissolved organic nitrogen depending on habitat and nitrogen deposition

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Cited by 69 publications
(63 citation statements)
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“…Moreover, plant dissolved organic nitrogen (DON) use was often demonstrated experimentally by the uptake of one or a few 15 N‐labelled amino acids, which cannot elucidate the real availability of the whole soil DON pool to plants (Kahmen, Livesley, & Arndt, ), so that substantial uncertainties existed in the source contributions estimated by using the δ 15 N of the whole DON pool (e.g. Liu et al., ). Consequently, we assume NH 4 + and NO 3 − to be the dominant N sources for plants in tropical ecosystems (e.g.…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…Moreover, plant dissolved organic nitrogen (DON) use was often demonstrated experimentally by the uptake of one or a few 15 N‐labelled amino acids, which cannot elucidate the real availability of the whole soil DON pool to plants (Kahmen, Livesley, & Arndt, ), so that substantial uncertainties existed in the source contributions estimated by using the δ 15 N of the whole DON pool (e.g. Liu et al., ). Consequently, we assume NH 4 + and NO 3 − to be the dominant N sources for plants in tropical ecosystems (e.g.…”
Section: Methodsmentioning
confidence: 99%
“…Plant NH 4 + preference over NO 3 − (βnormalNH4+) was evaluated by using the fnormalNH4+ minus corresponding proportional contributions of soil NH 4 + in soil DIN (Equation ).normalβNH4+=fNH4+false([NH4+]false/[DIN]false)where fnormalNH4+ values were calculated from Equation , [NH 4 + ] and [DIN] were mean concentrations of NH 4 + and DIN in soil of corresponding plots. Positive βnormalNH4+ values indicate plant NH 4 + preference over soil NO 3 − , 0 values indicate no preference, and negative βnormalNH4+ indicate a plant preference for NO 3 − over NH 4 + (more details in Liu et al., ).…”
Section: Methodsmentioning
confidence: 99%
“…Scenarios 3–4 are expected to be true for mosses because atmospheric NO − 3 has been assumed as the sole source (Liu et al, 2012a). Nevertheless, isotopic partitioning of N sources (Liu et al, 2013b) and further Δ 17 O analysis (Figure 5) suggests that moss NO − 3 , even at epilithic habitats, is actually a mixture of atmospheric NO − 3 and soil-derived NO − 3 . Thus, it is becoming clear that mosses can acquire substantial N from substrates; and moss NO − 3 is a valid atmospheric bio-monitor only for species growing on rare N-free substrates.…”
Section: Isotopic Systematics Of No−3 In Plantsmentioning
confidence: 96%
“…Pore water that has passed through the Sphagnum filter may differ in terms of 103 water quality including pH (Manninen et al, 2011;Sheppard et al, 2014) (Krupa, 2003;Staelens et al, 2008;Stevens et al, 2011) and hydrogen 108 ion (H + ) leaching (Krupa, 2003;Liu et al, 2013;Manninen et al, 2011;Paulissen et al, 109 2004; Stevens et al, 2011;Tomassen et al, 2003). In contrast, NO3 -uptake is 110 accompanied by hydroxyl ion (OH -) loss generated by nitrate reduction (Manninen et al,111 2011; Stevens et al, 2011).…”
mentioning
confidence: 99%