Dataset for: Nitrogen stable isotope patterns in amino acids of a metabolically versatile anoxygenic phototrophic bacterium, Rhodopseudomonas palustris (2024)

Date: 13 May, 2024

Dataset Title: Nitrogen stable isotope patterns in amino acids of a metabolically versatile anoxygenic phototrophic bacterium, Rhodopseudomonas palustris

Dataset Creators: Dr. Jenan Kharbush, jenanjk@umich.edu; Raisha Rahman, rraisha@umich.edu; Dr. Ann Pearson, apearson@eps.harvard.edu

Dataset Contact: Dr. Jenan Kharbush, jenanjk@umich.edu

Research Overview:
Amino acids are the primary nitrogen-containing compounds in cells, participating in various metabolic processes such as protein synthesis and degradation into other nitrogenous compounds. Compound-specific nitrogen isotope analysis of amino acids in environmental samples can provide insight into nitrogen sources, cycling, and tropic modifications in ecosystems. However, we lack comprehensive understanding of N utilization patterns in microorganisms, which are the site of nitrogen assimilation in biological systems, due to the varied and complex mechanisms by which microbes can acquire and metabolize nitrogen-containing compounds. δ15N measurements for free intracellular amino acids and protein-bound amino acids for environmentally-relevant microbial groups may aid in untangling the biochemical processes involved in amino acid metabolism performed by these microbial communities. Here, we report intracellular amino acid δ15N values for R. palustris, a metabolically versatile anoxygenic phototrophic bacterium.

Methodology:
The dataset contains bulk and intracellular amino acid nitrogen isotope data for two strains of the metabolically versatile anoxygenic phototrophic bacterium, Rhodopseudomonas palustris. R. palustris CGA009 was grown micro-aerobically on minimal PM media, modified from Ritchie (2013), in capped 1L culture bottles with minimal headspace. The components were as follows (in mM): (NH4)2SO4, 10; KH2PO4, 12.5; Na2HPO4, 12.5; MgSO4, 0.238; CaCl2, 0.0454; Sodium pyruvate, 10; Sodium thiosulfate, 0.1; p-aminobenzoic acid, 0.0146; Sodium bicarbonate, 10. The medium additionally contained 10 mL of the ATCC MD-VS Vitamin Supplement and 1 mL of a trace elements mix. The trace elements mix contained the following components (in mM): Citric acid H2O, 105; FeSO4 7H2O, 2.511; ZnSO4 7H2O, 38.07; MnSO4 H2O, 9.11; CuSO4 5H2O, 1.570; Co(NO3)2 6H2O,0.859; Na2MoO4 2H2O, 0.02139; H3BO3, 1.856. R. palustris TIE1 was grown in completely anoxic conditions on minimal Freshwater media, modified from Ehrenreich and Widdel (1994), in capped 1L culture bottles. The components are as follows (in mM): NH4Cl, 10; KH2PO4, 1; MgCl2 6H2O, 1.97; CaCl2 2H2O, 1.36; Sodium thiosulfate, 5; Sodium pyruvate, 10; Sodium bicarbonate, 15. The medium additionally contained 1 mL of a vitamin supplement and 1 mL of a trace elements mix. Media preparation and culture inoculation were performed in an anaerobic glovebox. All cultures were incubated at 30°C under 24-hour light while shaking at around 60 rpm. Growth rates were monitored by optical density (OD) at 600 nm on a UV-Vis spectrophotometer.

The R. palustris cultures were harvested via centrifugation at various points during the log and late-log phases of growth. The cell pellets were rinsed with nitrogen-free media between centrifugation steps. During cell collection, around 1 ml of spent media was collected, sterile filtered, and analyzed for NH4+ concentration using a Sigma-Aldrich Ammonia Assay Kit.

Cell pellets for each culture were divided for bulk biomass, free intracellular amino acid, and protein-bound amino acid nitrogen isotope analysis. The bulk nitrogen isotopic composition of lyophilized cell samples were measured via elemental analysis with isotope ratio mass spectrometry (EA-IRMS), on a Thermo Scientific Flash IRMS Elemental Analyzer with EA Isolink, coupled to a Delta V Plus IRMS through a Conflo IV universal interface. Free intracellular amino acid subsamples were first lysed through a combination of bead-beating, freeze-thawing, and sonication. The subsamples were then purified with Dowex 50WX8 (200-400 mesh) cation exchange resin according to the method outlined by Owen et al. (1999), to isolate the individual amino acids from other cellular materials. The protein-bound amino acid subsamples were first treated with 6 M HCl at 110°C for 20 hours to hydrolyze the protein peptide bonds, and then were also purified with the Dowex cation exchange resin. Prior to isotope analysis, the purified free and protein-bound amino acid subsamples were derivatized with MTBSTFA according to the procedure outlined in Molero et al. (2011). The derivatized free and protein-bound subsamples were then analyzed for 15N composition via gas chromatography isotope ratio mass spectrometer (GC-IRMS), using a Thermo Scientific GC Isolink IRMS system with a Trace 1310 and TriPlus RSH Autosampler, coupled to a Delta V Plus IRMS though a Conflo IV universal interface (Agilent J&W DB-5ms GC Column; 60 m; GC program ramp: initial temperature of 90°C, increased by 8.0°C/min to 140°C, then increased by 3.0°C/min to 280°C, and finally to 300°C by 12°C/min). Bulk, free amino acid, and protein-bound amino acid nitrogen isotope compositions were expressed in standard δ notation against atmospheric N2. δ15N values were corrected with in-house (amino acids) and authentic standards (USGS40, USGS41a, and AABA).

Files contained here:
r_palustris_nitrogen_isotope_data.csv
This file contains 35 rows and 17 columns. Rows 2 to 13 contain data on R. palustris samples grown in N-replete conditions. Rows 15 to 17 contain data on R. palustris samples grown in N-limited conditions. The columns contain the following information:
B. Sample identifier, with each sample designated by experiment date, strain, and a letter. Samples with the same year-month designation were part of the same culture experiment.
C. Initial NH4 concentration
D. Raw OD600 measurement at time of culture harvest
E. Normalized OD, calculated relative to highest OD600 measurement for each set of culture experiments
F. Optimized OD, calculated by multiplying Normalized OD/column (5) by a factor
G. Fraction of NH4 remaining in sample, calculated from NH4 concentration measurements on spent media
H. Fractional Yield (f), calculated as (1-Optimized OD/Column (6))
I. Ln(f), or Ln(Fractional Yield)
J. Substrate δ15N, or nitrogen isotopic composition of NH4+ used in media preparation
K. Bulk Biomass δ15N
L-W. Free Intracellular Amino Acid δ15N values for the following amino acids, in order: glutamate/glutamine, aspartate/asparagine, alanine, isoleucine, leucine, valine, proline, glycine, serine, lysine, phenylalanine, tyrosine. Each column is labelled as "Free" followed by the three-letter code for the given amino acid.
X-AI. Protein-bound Amino Acid δ15N values for the following amino acids, in order: glutamate/glutamine, aspartate/asparagine, alanine, isoleucine, leucine, valine, proline, glycine, serine, lysine, phenylalanine, tyrosine. Each column is labelled as "Prot" followed by the three-letter code for the given amino acid. For the columns for glutamate/glutamine and aspartate/asparagine, Glx and Asx are used, respectively.

Use and Access:
This data set is made available under a Creative Commons Public Domain license (CC0 1.0).

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Dataset for: Nitrogen stable isotope patterns in amino acids of a metabolically versatile anoxygenic phototrophic bacterium, Rhodopseudomonas palustris (2024)

FAQs

Which two amino acids stable isotope values can be used to assess an organism's trophic position? ›

The majority of studies have used the difference between two amino acids, glutamate and phenylalanine (Glu and Phe), as the two 'canonical' 'trophic' and 'source' amino acids, but some have suggested using a different combination, or a multiple amino acid approach (Popp et al.

How is protein metabolized in the body? ›

This process begins in the stomach and continues in the small intestine. Large protein chains are disassembled to eventually leave free amino acids that can be taken up into the blood and transported to various cells around the body for further breakdown.

What are the stable isotopes of amino acids? ›

The stable isotope composition of amino acids refers to the abundance of heavy and light non-radioactive isotopes of carbon (13C and 12C), nitrogen (15N and 14N), and other elements within these molecules. Amino acids are the building blocks of proteins.

Which amino acid plays a most significant role in nitrogen metabolism? ›

The amino acids Glutamate and glutamine are the products of absorbed ammonia. And compound serves as a large nitrogen source for various metabolic processes in the plant body. Amino acid Glutamine plays important role in nitrogen metabolism.

What are the trophic amino acids? ›

'Trophic' amino acids are those whose amino-nitrogens are interchangeable, part of a metabolic amino-nitrogen pool, and 'source' amino acids are those whose amino-nitrogens are not interchangeable with the metabolic pool.

What is a stable isotope analysis can be used to analyze? ›

Stable isotope analysis can be used in ecological studies to trace chemical movement through the environment. A common application is to use the isotopic composition of a mixture to determine the proportions of various sources in the mixture, using mathematical mixing models.

What are the two main types of isotopes stable and unstable? ›

There are two main types of isotopes: stable and unstable (radioactive). There are 254 known stable isotopes. All artificial (lab-made) isotopes are unstable and therefore radioactive; scientists call them radioisotopes. Some elements can only exist in an unstable form (for example, uranium).

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