Exploring cycad foliage as an archive of the isotopic composition of atmospheric nitrogen.

Molecular nitrogen (N₂ ) constitutes the majority of Earth's modern atmosphere, contributing ~0.79 bar of partial pressure (pN₂ ). However, fluctuations in pN₂ may have occurred on 10⁷ -10⁹  year timescales in Earth's past, perhaps altering the isotopic composition of atmospheric nitrogen. Here, we explore an archive that may record the isotopic composition of atmospheric N₂ in deep time: the foliage of cycads. Cycads are ancient gymnosperms that host symbiotic N₂ -fixing cyanobacteria in modified root structures known as coralloid roots. All extant species of cycads are known to host symbionts, suggesting that this N₂ -fixing capacity is perhaps ancestral, reaching back to the early history of cycads in the late Paleozoic. Therefore, if the process of microbial N₂ fixation records the δ¹⁵ N value of atmospheric N₂ in cycad foliage, the fossil record of cycads may provide an archive of atmospheric δ¹⁵ N values. To explore this potential proxy, we conducted a survey of wild cycads growing in a range of modern environments to determine whether cycad foliage reliably records the isotopic composition of atmospheric N₂ . We find that neither biological nor environmental factors significantly influence the δ¹⁵ N values of cycad foliage, suggesting that they provide a reasonably robust record of the δ¹⁵ N of atmospheric N₂ . Application of this proxy to the record of carbonaceous cycad fossils may not only help to constrain changes in atmospheric nitrogen isotope ratios since the late Paleozoic, but also could shed light on the antiquity of the N₂ -fixing symbiosis between cycads and cyanobacteria.

Duke Scholars

Author Michael Kipp Earth and Climate Sciences