Extreme isotopic depletion of nitrogen in New Zealand lithophytes and epiphytes; the result of diffusive uptake of atmospheric ammonia?

Several lichens and the terrestrial alga Trentepohlia were found to have extremely depleted ¹⁵N signatures at two sites near the Rotorua geothermal area, New Zealand. Values, typically -20‰, with several extreme cases of -24‰, are more isotopically depleted than any previously quoted δ¹⁵N signature for vegetation growing in natural environments. For Trentepohlia, distance from a geothermal source did not affect isotopic signature. A 100-km transect showed that the phenomenon is widespread and the discrimination is not related to substrate N, or to elevation. Rainfall NHx and atmospheric gaseous NH₃ (NH_3(g)) were shown to be isotopically depleted in the range -1‰ to -8‰ and could not, of themselves, be responsible for the plant values obtained. A simulation of Trentepohlia thallus was created using an acidified fiberglass mat and was allowed to absorb NH_3(g) from the atmosphere. Mats exposed at the geothermal sites and on farmland showed a significant further depletion of ¹⁵N to -17‰. We hypothesize that the extreme isotopic depletion is due to dual fractionation: firstly by the volatilization of NH _3(g) from aqueous sources into the atmosphere; secondly by the diffusive assimilation of that NH_3(g) into vegetation. We further hypothesize that lithophytes, epiphytes, and higher plants, growing on strongly N-limited substrates, will show this phenomenon more or less, depending on the proportion of diffusively assimilated NH_3(g) utilized as a N source. Many of the isotopically depleted δ¹⁵N signatures in vegetation, previously reported in the literature, especially epiphytes, may be due to this form of uptake depending on the concentration of atmospheric NH _3(g), and the degree of reliance on that form of N.