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1. Radon Isotopes and Stable Water Isotopes from Coal Creek Watershed, Colorado (2021)

   https://doi.org/10.15485/2283437  

   Johnson, Keira; Christensen, John; Williams, Kenneth Hurst; Gardner, William Payton; Sullivan, Pamela; Brown, Wendy; Beutler, Curtis; Thiros, Nicholas (January 2023, Environmental System Science Data Infrastructure for a Virtual Ecosystem; Watershed Function SFA)

   The radon isotope and stable water isotope data for Coal Creek Watershed, Colorado, consists of d2H, d18O, and 222Rn values from samples collected at 8 stream location along Coal Creek, samples from 7 groundwater springs within the watershed, and precipitation isotope samples collected by Next Generation Water Observing System (NGWOS) from a collector within the watershed. All stream and spring samples were collected between June and October, 2021, and precipitation isotope samples were collected between November 2020 and September 2021. These data were collected to evaluate how groundwater contributions to Coal Creek originating from a fractured hillslope and alluvial fan respond to summer monsoon rains and seasonal drying. Understanding of groundwater-surface water interactions in montane systems in critical for the future of water availability in the Western US as groundwater contributions are expected to become more important for sustaining summer stream flows. This data package contains: (1) a csv of all radon samples; (2) a csv of all stream and spring isotope samples; (3) a csv of precipitation isotope samples; and (4) a csv of locations for each sampling site. The dataset additionally includes a file-level metadata (flmd.csv) file that lists each file contained in the dataset with associated metadata; and a data dictionary (dd.csv) file that contains column/row headers used throughout the files along with a definition, units, and data type. 

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2. SIMPEL: using stable isotopes to elucidate dynamics of context specific metabolism

   https://doi.org/10.1038/s42003-024-05844-z  

   Kambhampati, Shrikaar; Hubbard, Allen H.; Koley, Somnath; Gomez, Javier D.; Marsolais, Frédéric; Evans, Bradley S.; Young, Jamey D.; Allen, Doug K. (December 2024, Communications Biology)

   Abstract The capacity to leverage high resolution mass spectrometry (HRMS) with transient isotope labeling experiments is an untapped opportunity to derive insights on context-specific metabolism, that is difficult to assess quantitatively. Tools are needed to comprehensively mine isotopologue information in an automated, high-throughput way without errors. We describe a tool, Stable Isotope-assisted Metabolomics for Pathway Elucidation (SIMPEL), to simplify analysis and interpretation of isotope-enriched HRMS datasets. The efficacy ofSIMPELis demonstrated through examples of central carbon and lipid metabolism. In the first description, a dual-isotope labeling experiment is paired withSIMPELand isotopically nonstationary metabolic flux analysis (INST-MFA) to resolve fluxes in central metabolism that would be otherwise challenging to quantify. In the second example,SIMPELwas paired with HRMS-based lipidomics data to describe lipid metabolism based on a single labeling experiment. Available as an R package,SIMPELextends metabolomics analyses to include isotopologue signatures necessary to quantify metabolic flux. 

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3. Unlocking the Single-Crystal Record of Heavy Stable Isotopes

   https://doi.org/10.2138/gselements.17.6.389  

   Tissot, François L.; Ibañez-Mejia, Mauricio (December 2021, Elements)

   Stable isotopes provide deep insights into processes across a wide range of scales, from micron- to cosmic-size systems. Here, we review how continued advances in mass-spectrometry have enabled the analysis of ever-smaller samples and brought the field of heavy stable isotope geochemistry to its next frontier: the single-crystal scale. Accessing this record can be as enlightening as it is challenging. Drawing on novel systematics at different stages of development (from well-established to nascent), we discuss how the isotopes of heavy elements, such as magnesium, iron, zirconium, or uranium, can be used at the single-crystal and subcrystal scales to reconstruct magma thermal histories, crystal growth timescales, or, possibly, magma redox conditions. 

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4. Tracing exploitation of egg boons: an experimental study using fatty acids and stable isotopes

   https://doi.org/10.1242/jeb.246247  

   Nair, Parvathi; Miller, Cambria M.; Fuiman, Lee A. (November 2023, Journal of Experimental Biology)

   ABSTRACT Coordinated spawning of marine animals releases millions of planktonic eggs into the environment, known as egg boons. Eggs are rich in essential fatty acids and may be an important lipid subsidy to egg consumers. Our aim was to validate the application of fatty acid and stable isotope tracers of egg consumption to potential egg consumers and to confirm egg consumption by the selected species. We conducted feeding experiments with ctenophores, crustaceans and fishes. We fed these animals a common diet of Artemia or a commercial feed (Otohime) and simulated egg boons for half of them by intermittently supplementing the common diet with red drum (Sciaenops ocellatus) eggs for 10–94 days. Controls did not receive eggs. Fatty acid profiles of consumers fed eggs were significantly different from those of controls 24 h after the last egg-feeding event. Consumers took on fatty acid characteristics of eggs. In fishes and ctenophores, fatty acid markers of egg consumption did not persist 2–5 days after the last egg-feeding event, but markers of egg consumption persisted in crustaceans for at least 5–10 days. Additionally, consumption of eggs, which had high values of δ15N, led to δ15N enrichment in crustaceans and a fish. We conclude that fatty acids and nitrogen stable isotope can be used as biomarkers of recent egg consumption in marine animals, validating their use for assessing exploitation of egg boons in nature. 

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5. Stable isotopes contain substantial additive information about terrestrial carbon and water cycling

   https://doi.org/10.1088/1748-9326/acf4ab  

   Li, Bonan; Good, Stephen P.; Fiorella, Richard P.; Finkenbiner, Catherine E.; Bowen, Gabriel J.; Noone, David C.; Still, Christopher J.; Anderegg, William R. L. (September 2023, Environmental Research Letters)

   Abstract Stable isotope ratios of H (δ²H), O (δ¹⁸O), and C (δ¹³C) are linked to key biogeochemical processes of the water and carbon cycles; however, the degree to which isotope-associated processes are reflected in macroscale ecosystem flux observations remains unquantified. Here through formal information assessment, new measurements ofδ¹³C of net ecosystem exchange (NEE) as well asδ²H andδ¹⁸O of latent heat (LH) fluxes across the United States National Ecological Observation Network (NEON) are used to determine conditions under which isotope measurements are informative of environmental exchanges. We find all three isotopic datasets individually contain comparable amounts of information aboutNEEandLHfluxes as wind speed observations. Such information from isotope measurements, however, is largely unique. Generally,δ¹³C provides more information aboutLHas aridity increases or mean annual precipitation decreases.δ²H provides more information aboutLHas temperatures or mean annual precipitation decreases, and also provides more information aboutNEEas temperatures decrease. Overall, we show that the stable isotope datasets collected by NEON contribute non-trivial amounts of new information about bulk environmental fluxes useful for interpreting biogeochemical and ecohydrological processes at landscape scales. However, the utility of this new information varies with environmental conditions at continental scales. This study provides an approach for quantifying the value adding non-traditional sensing approaches to environmental monitoring sites and the patterns identified here are expected to aid in modeling and data interpretation efforts focused on constraining carbon and water cycles’ mechanisms. 

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