PP010-0009
Histidine Intramolecular Nitrogen Isotope Analysis - A Potential New Tracer of Ecosystem Nitrogen Sources

Tuesday, 8 December 2020
Poster
Charlotte Wing Man Lee1, Lydia Hayes1, Ava Kreider-Mueller2, Evelyn Kuhnel1, Jesus Baca1, Catherine Shaw1, Roslyn Swonke1, Mark A Altabet3 and Lin Zhang1, (1)Texas A&M University Corpus Christi, Corpus Christi, TX, United States, (2)University of Massachusetts Dartmouth, SMAST, New Bedford, MA, United States, (3)University of Massachusetts Dartmouth, New Bedford, MA, United States
Abstract:
In nitrogen (N) isotope studies of ecosystem structure, Phenylalanine (Phe) is considered the canonical source amino acid (AA) as its δ15N value is thought to reflect the δ15N of N sources. However, the α-amino group, containing Phe’s only N atom, is subject to degradation reactions such as transamination and deamination, which may incur isotope fractionation. The molecular structure of Histidine (His) contains 3 N atoms, two of which are in the imidazole side chain and are synthesized from ATP and glutamine respectively. The side chain is less prone to transamination and deamination and is likely re-used by consuming organisms due to the expensive cost of metabolic synthesis. Thus, we hypothesize that the δ15N of the His side chain (δ15NHis-side) retains the δ15N of the inorganic N source with high fidelity, serving as a new tracer to identify N sources and utilization patterns. Both Phe and His are found at low mol% (< 5%) in sediments, but the higher N content in His makes δ15N analysis more feasible.

δ15NHis-side analysis is made possible by a new method in which, after hydrolysis, AAs are first separated and collected by Ion-exchange Chromatography with the His fraction divided in 2. One sub-fraction is oxidized by hypochlorite, converting the α-N to nitrite; and the other one reacted with persulfate, oxidizing all three Ns into nitrate. Both nitrite and nitrate are then converted to nitrous oxide and analyzed using Purge-and-Trap Isotope Ratio Mass Spectrometry. The δ15NHis α-N and δ15NPhe are determined using a previously published method while δ15NHis-side could be calculated by the mass balance equation. We will compare the δ15NHis-side in cyanobacteria, zooplankton, and sediment with the δ15NPhe in the same samples and the δ15N of their corresponding inorganic N sources. This study will provide new insights into key AA biosynthesis and degradation in biota and natural environments.