Academic literature on the topic 'Isotope signature'

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Journal articles on the topic "Isotope signature"

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Emmanuel, S., J. A. Schuessler, J. Vinther, A. Matthews, and F. von Blanckenburg. "Iron isotope fractionation in marine invertebrates in near shore environments." Biogeosciences Discussions 11, no. 4 (2014): 5533–55. http://dx.doi.org/10.5194/bgd-11-5533-2014.

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Abstract. Chitons (Mollusca) are marine invertebrates that produce radula (teeth or rasping tongue) containing high concentrations of biomineralized magnetite and other iron bearing minerals. As Fe isotope signatures are influenced by redox processes and biological fractionation, Fe isotopes in chiton radula might be expected to provide an effective tracer of ambient oceanic conditions and biogeochemical cycling. Here, in a pilot study to measure Fe isotopes in marine invertebrates, we examine Fe isotopes in modern marine chiton radula collected from different locations in the Atlantic and Pac
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Emmanuel, S., J. A. Schuessler, J. Vinther, A. Matthews, and F. von Blanckenburg. "A preliminary study of iron isotope fractionation in marine invertebrates (chitons, Mollusca) in near-shore environments." Biogeosciences 11, no. 19 (2014): 5493–502. http://dx.doi.org/10.5194/bg-11-5493-2014.

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Abstract. Chitons (Mollusca) are marine invertebrates that produce radulae (teeth or rasping tongues) containing high concentrations of biomineralized magnetite and other iron-bearing minerals. As Fe isotope signatures are influenced by redox processes and biological fractionation, Fe isotopes in chiton radulae might be expected to provide an effective tracer of ambient oceanic conditions and biogeochemical cycling. Here, in a pilot study to measure Fe isotopes in marine invertebrates, we examine Fe isotopes in modern marine chiton radulae collected from different locations in the Atlantic and
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MacAvoy, Stephen E., Stephen A. Macko, and Lynne S. Arneson. "Growth versus metabolic tissue replacement in mouse tissues determined by stable carbon and nitrogen isotope analysis." Canadian Journal of Zoology 83, no. 5 (2005): 631–41. http://dx.doi.org/10.1139/z05-038.

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Stable-isotope signatures in animal tissues presumably reflect the local food web. However, that assumption may be complicated by differential nutrient routing, fractionation, and the possibility that large organisms are not in isotopic equilibrium with seasonally available food sources. Additionally, the rate at which organisms incorporate the isotopic signature of a food is largely unknown. In this study we assessed the rate of carbon- and nitrogen-isotope turnover in liver, muscle, and blood in mice (Mus musculus L., 1758) following a diet change. We report the proportion of tissue turnover
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Abiye, Tamiru A., Molla B. Demlie та Haile Mengistu. "An Overview of Aquifer Physiognomies and the δ18O and δ2H Distribution in the South African Groundwaters". Hydrology 8, № 2 (2021): 68. http://dx.doi.org/10.3390/hydrology8020068.

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A comprehensive assessment of the stable isotope distribution in the groundwater systems of South Africa was conducted in relation to the diversity in the aquifer lithology and corresponding hydraulic characteristics. The stable isotopes of oxygen (18O) and hydrogen (2H) in groundwater show distinct spatial variation owing to the recharge source and possibly mixing effect in the aquifers with the existing water, where aquifers are characterized by diverse hydraulic conductivity and transmissivity values. When the shallow aquifer that receives direct recharge from rainfall shows a similar isoto
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Meister, Patrick, and Carolina Reyes. "The Carbon-Isotope Record of the Sub-Seafloor Biosphere." Geosciences 9, no. 12 (2019): 507. http://dx.doi.org/10.3390/geosciences9120507.

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Sub-seafloor microbial environments exhibit large carbon-isotope fractionation effects as a result of microbial enzymatic reactions. Isotopically light, dissolved inorganic carbon (DIC) derived from organic carbon is commonly released into the interstitial water due to microbial dissimilatory processes prevailing in the sub-surface biosphere. Much stronger carbon-isotope fractionation occurs, however, during methanogenesis, whereby methane is depleted in 13C and, by mass balance, DIC is enriched in 13C, such that isotopic distributions are predominantly influenced by microbial metabolisms invo
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Jiménez-Rodríguez, César Dionisio, Miriam Coenders-Gerrits, Jochen Wenninger, Adriana Gonzalez-Angarita, and Hubert Savenije. "Contribution of understory evaporation in a tropical wet forest during the dry season." Hydrology and Earth System Sciences 24, no. 4 (2020): 2179–206. http://dx.doi.org/10.5194/hess-24-2179-2020.

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Abstract. Tropical wet forests are complex ecosystems with a large number of plant species. These environments are characterized by a high water availability throughout the whole year and a complex canopy structure. However, how the different sections of the canopy contribute to total evaporation is poorly understood. The aim of this work is to estimate the total evaporation flux and differentiate the contribution among canopy layers of a tropical wet forest in Costa Rica. The fluxes were monitored during the dry season by making use of the energy balance to quantify the fluxes and stable wate
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FELITSYN, SERGEI B., and ALEXANDER P. GUBANOV. "Nd isotope composition of early Cambrian discrete basins." Geological Magazine 139, no. 2 (2002): 159–69. http://dx.doi.org/10.1017/s0016756801006252.

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A Nd isotope map of early Cambrian epeiric basins has been inferred from the Nd isotopic signature recorded in phosphatic Small Shelly Fossils. The most radiogenic εNd(t) values characterize water reservoirs along the Avalonian and Cadomian belts, while εNd(t) values of −10 to −20 were obtained in Laurentia and East Gondwanan Australia and China. Such a distribution of Nd isotope signatures results from the different provenance of early Cambrian epeiric seas: juvenile magmatic arcs and/or cordilleran for Mongolia, Siberia, Iberia and adjacent terranes, and cratonic sources for Laurentia and Ea
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Guo, Rong, Shengjie Wang, Mingjun Zhang, et al. "Stable Hydrogen and Oxygen Isotope Characteristics of Bottled Water in China: A Consideration of Water Source." Water 11, no. 5 (2019): 1065. http://dx.doi.org/10.3390/w11051065.

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The origin of bottled water can be identified via its stable isotope signature because of the spatial variation of the stable isotope composition of natural waters. In this paper, the spatial pattern of δ2H and δ18O values were analyzed for a total of 242 bottled water samples produced at 137 sites across China that were randomly purchased during 2014–2015. The isotopic ratios of bottled water vary between −166‰ and −19‰ for δ2H, and between −21.6‰ and −2.1‰ for δ18O. Based on multiple regression analyses using meteorological and geographical parameters, an isoscape of Chinese bottled water wa
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Stevenson, R. K., X. W. Meng, and C. Hillaire-Marcel. "Impact of melting of the Laurentide Ice Sheet on sediments from the upper continental slope off southeastern Canada: evidence from Sm–Nd isotopesThis article is one of a series of papers published in this Special Issue on the theme Polar Climate Stability Network." Canadian Journal of Earth Sciences 45, no. 11 (2008): 1243–52. http://dx.doi.org/10.1139/e08-031.

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We present new Sm–Nd isotope data for sediments from a core located on the continental slope of the St. Pierre Bank of Canada’s east coast. The Nd analyses indicate that the sediments were derived from two principal sources: the North American Shield that yields an average early Proterozoic isotopic signature and a younger Proterozoic signature attributed to Appalachian crustal sources. The Appalachian-sourced sediments predominated during the last glacial maximum (LGM) and were associated with low sedimentation rates (<30 cm/ka), with the exception of a strong North American Shield signatu
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Weng, Yongbiao, Aina Johannessen, and Harald Sodemann. "High-resolution stable isotope signature of a land-falling atmospheric river in southern Norway." Weather and Climate Dynamics 2, no. 3 (2021): 713–37. http://dx.doi.org/10.5194/wcd-2-713-2021.

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Abstract. Heavy precipitation at the west coast of Norway is often connected to elongated meridional structures of high integrated water vapour transport known as atmospheric rivers (ARs). Here we present high-resolution measurements of stable isotopes in near-surface water vapour and precipitation during a land-falling AR in southwestern Norway on 7 December 2016. In our analysis, we aim to identify the influences of moisture source conditions, weather system characteristics, and post-condensation processes on the isotope signal in near-surface water vapour and precipitation. A total of 71 pr
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Dissertations / Theses on the topic "Isotope signature"

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Pérez, Moreno Rodrigo. "Stable isotope and anthropogenic tracer signature of waters in an andean geothermal system." Tesis, Universidad de Chile, 2019. http://repositorio.uchile.cl/handle/2250/170853.

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Tesis para optar al grado de Magíster en Ciencias, Mención Geología<br>El presente trabajo se centra en el uso de isótopos estables y trazadores antropogénicos para investigar el origen, los tiempos de residencia y la evolución de las aguas termales en el Complejo Volcánico Lonquimay-Tolhuaca, ubicado en la parte central de la Zona Volcánica Sur. Veinte muestras de agua subterránea, surgiendo en un amplio rango de temperaturas (8-96°C), son analizadas para determinar su composición química, incluyendo elementos mayores, razones isotópicas (δ2H, δ18O, δ13CTDIC) y la concentración de clorofluoro
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Ferrio, Díaz Juan Pedro. "Reconstruction of climatic and crop conditions in the past based on the isotope signature of archaeobotanical remains." Doctoral thesis, Universitat de Lleida, 2005. http://hdl.handle.net/10803/8338.

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Reconstrucció de les condicions climàtiques i de conreu en el passat<br/>a partir de l'anàlisi isotòpica de restes arqueobotàniques<br/><br/>L'aparició i progressiu desenvolupament de l'agricultura durant els darrers 10.000 anys ha alterat radicalment<br/>l'estructura social i poblacional dels grups humans, així com la seva relació amb l'entorn. De fet, l'adopció de<br/>l'agricultura pot constituir el primer exemple en el temps d'interacció recíproca entre el medi ambient i la humanitat.<br/>Per tant, la reconstrucció de les condicions ambientals (d'origen climàtic o degudes a l'acció humana)
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Urlwin, Ben. "Carbon isotope stratigraphy of the late Proterozoic Wonoka formation of the Adelaide fold belt : diagenetic assessment and interpretation of isotopic signature and correlations with previously measured isotopic curves /." Title page, abstract and contents only, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbu77.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1993.<br>On title page : "National Grid reference : Copley 1:250,000 SH54-9 6636." Folded map in back cover pocket. Includes bibliographical references (leaves [50-65]).
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Geske, Anna-Christine [Verfasser], Adrian [Gutachter] Immenhauser, and Detlev K. [Gutachter] Richter. "Establishing the magnesium isotope signature of dolomites / Anna-Christine Geske ; Gutachter: Adrian Immenhauser, Detlev K. Richter ; Fakultät für Geowissenschaften." Bochum : Ruhr-Universität Bochum, 2014. http://d-nb.info/1212661877/34.

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Castleberry, Colette M. "Quantitative Identification of Non-coding RNAs by Isotope Labeling and LC-MS/MS." University of Cincinnati / OhioLINK, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1258474676.

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Marryanna, Lion. "Effects of spatio-temporal distribution of soil moisture on a lowland dipterocarp forest at Pasoh Forest Reserve in Peninsular Malaysia." Kyoto University, 2018. http://hdl.handle.net/2433/232153.

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Abraham, Muriel. "Spatial variation in soil organic carbon and stable carbon isotope signature in a pasture and a primary forest in central Panamá." Thesis, McGill University, 2004. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=80159.

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Soil properties and their spatial variability was measured to provide a strong database to assess the modification in soil properties associated with future changes in land use. Surface (0--10 cm) soil samples were collected from a 9 ha, 46-year-old pasture being converted to a native tree plantation and a neighboring control pasture near Sardinilla, Panama. A small-scale nested grid of surface soil samples was replicated in the future plantation and a primary forest in the region to evaluate the spatial variability of soil properties. Seven 1 m profiles were sampled in the future plant
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Romagnoli, Beatrice. "Influence of Guadalquivir estuary on aquatic biogeochemistry and isotopic signature of the saltmarshes of Doñana National Park (SW Spain)." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2018. http://amslaurea.unibo.it/15062/.

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Doñana National Park (DNP) hosts one of the most important wetlands in Europe. In 1998, the release of a toxic sludge from storage ponds at a nearby mine, led to the construction of a dyke on the natural levee of the Guadalquivir river, to protect the vast Doñana marshland against the contaminated tailings. During almost two decades, hydrology in the marshes mostly depended on the rainfall regime and to a lesser extent on an underground aquifer. Over 2014, several actions were carried out to restore connectivity with the river, allowing the entry of estuarine waters. This work presents bio
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Upton, Sally A. "Novel use of a Natural Isotope Signature to Track Recruitment and Evaluate Age Determination Methods for the 2002 Year Class of American Shad in the York River." W&M ScholarWorks, 2008. https://scholarworks.wm.edu/etd/1539617876.

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Millet, Marc-Alban. "Interactions de faibles profondeurs et géochimie des basaltes d'îles océaniques : implications sur les modes d'acquisition de la signature isotopique et sur la topogique mantellique." Phd thesis, Université Blaise Pascal - Clermont-Ferrand II, 2007. http://tel.archives-ouvertes.fr/tel-00718419.

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Les compositions isotopiques de Sr, Nd et Pb des basaltes d'îles océaniques ont été mesurées de manière systématique depuis 30 ans. Les variations de ces compositions sont classiquement interprétées comme la signature du mélange entre des composants présents au sein des panaches mantelliques. Cependant elles peuvent aussi représenter des interactions entre les magmas et les réservoirs qu'ils traversent au cours de leurs remontées vers la surface. Après avoir mis en évidence les processus pouvant altérer la composition initiale d'un magma et proposer des moyens de s'en affranchir, 2 études loca
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Books on the topic "Isotope signature"

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Mauro, Brilli, and Ogle Neil, eds. The isotopic signature of classical marbles. "L'Erma" di Bretschneider, 2006.

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Clauer, Norbert, and Sambhu Chaudhuri, eds. Isotopic Signatures and Sedimentary Records. Springer-Verlag, 1992. http://dx.doi.org/10.1007/bfb0009858.

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Oschmann, Lynn A. Global isotopic signatures of oceanic island basalts. Available from the National Technical Information Service, 1991.

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Kallenbach, R., T. Encrenaz, J. Geiss, K. Mauersberger, T. C. Owen, and F. Robert, eds. Solar System History from Isotopic Signatures of Volatile Elements. Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-010-0145-8.

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ISSI Workshop (2002 Bern, Switzerland). Solar system history from isotopic signatures of volatile elements: Volume resulting from an ISSI workshop, 14-18 January 2002, Bern, Switzerland. Kluwer Academic Publishers, 2003.

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Vintró, Luis León. The determination of transuranium isotopic signatures in environmental materials and their application to the study of marine processes. University College Dublin, 1997.

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O'Rourke, Dennis, Justin Tackney, Joan Coltrain, and Jennifer Raff. Ancient DNA and Stable Isotopes. Edited by Max Friesen and Owen Mason. Oxford University Press, 2016. http://dx.doi.org/10.1093/oxfordhb/9780199766956.013.3.

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Genetic diversity in modern Arctic communities provides a baseline from which to assess population history. This is augmented by documenting patterns of genetic variation in prehistoric populations using ancient DNA methods, and inferring dietary resource information and adaptive strategies derived from stable isotope analyses. This chapter uses this multidisciplinary approach to examine population history and colonization events in the Aleutians of South Alaska, and the origin and population history of Paleoeskimo and Neoeskimo populations of the North American Arctic. The power to identify p
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Norbert, Clauer, and Chaudhuri Sambhu 1938-, eds. Isotopic signatures and sedimentary records. Springer-Verlag, 1992.

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(Editor), Norbert Clauer, and Sambhu Chaudhuri (Editor), eds. Isotopic Signatures & Sedimentary Records (Lecture Notes in Earth Sciences). Springer, 1992.

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Heinrich, Wilhelm, and Rainer Abart, eds. Mineral reaction kinetics: Microstructures, textures, chemical and isotopic signatures. Mineralogical Society of Great Britain & Ireland, 2017. http://dx.doi.org/10.1180/emu-notes.16.

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Book chapters on the topic "Isotope signature"

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Moriya, Kazuyoshi. "Isotope Signature of Ammonoid Shells." In Topics in Geobiology. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9630-9_19.

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Ogrinc, N., H. Hintelmann, C. Eckley, and S. Lojen. "Biogeochemical influence on carbon isotope signature in boreal lake sediments." In The Interactions between Sediments and Water. Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-017-3366-3_28.

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Tanaka, Yu-ki, Kohshiro Takata, Takahiro Kawasaki, Atsuko Shinohara, Kazuko Ishikawa-Takata, and Takafumi Hirata. "Iron Isotope Signature in Red Blood Cell Samples from Japanese Female Donors of Various Ages." In Metallomics. Springer Japan, 2017. http://dx.doi.org/10.1007/978-4-431-56463-8_12.

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Olsson, Pål Axel. "Using Stable Carbon Isotope Labelling in Signature Fatty Acids to Track Carbon Allocation in Arbuscular Mycorrhiza." In Soil Biology. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-95894-9_16.

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Hu, Lingzhi, Hua Pan, and Samuel A. Wickline. "Fluorine (19F) MRI to Measure Renal Oxygen Tension and Blood Volume: Experimental Protocol." In Methods in Molecular Biology. Springer US, 2021. http://dx.doi.org/10.1007/978-1-0716-0978-1_31.

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AbstractFluorinated compounds feature favorable toxicity profile and can be used as a contrast agent for magnetic resonance imaging and spectroscopy. Fluorine nucleus from fluorinated compounds exhibit well-known advantages of being a high signal nucleus with a natural abundance of its stable isotope, a convenient gyromagnetic ratio close to that of protons, and a unique spectral signature with no detectable background at clinical field strengths. Perfluorocarbon core nanoparticles (PFC NP) are a class of clinically approved emulsion agents recently applied in vivo for ligand-targeted molecular imaging. The objective of this chapter is to outline a multinuclear 1H/19F MRI protocol for functional kidney imaging in rodents for mapping of renal blood volume and oxygenation (pO2) in renal disease models.This chapter is based upon work from the COST Action PARENCHIMA, a community-driven network funded by the European Cooperation in Science and Technology (COST) program of the European Union, which aims to improve the reproducibility and standardization of renal MRI biomarkers. This experimental protocol chapter is complemented by a separate chapter describing the basic concept of functional imaging using fluorine (19F) MR methods.
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Kumar, Bhishm. "Isotopic Signatures." In Encyclopedia of Earth Sciences Series. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_311.

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Das, Supriyo Kumar, Ujan Karmakar, Arunabha Dey, Sandip Agrahari, and Alf Ekblad. "Carbon Stable Isotope Source Signature of Bulk Organic Matter in Middle Bengal Fan Sediment Collected During IODP Expedition 354." In Dynamics of the Earth System: Evolution, Processes and Interactions. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40659-2_5.

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Kreuzer, Helen W. "Stable Isotope Signatures for Microbial Forensics." In Chemical and Physical Signatures for Microbial Forensics. Springer New York, 2011. http://dx.doi.org/10.1007/978-1-60327-219-3_7.

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Mauersberger, K., D. Krankowsky, and C. Janssen. "Oxygen Isotope Processes and Transfer Reactions." In Solar System History from Isotopic Signatures of Volatile Elements. Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-010-0145-8_17.

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Craw, Dave, and Doug MacKenzie. "Fluid Inclusions and Isotopic Signatures." In SpringerBriefs in World Mineral Deposits. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-35158-2_7.

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Conference papers on the topic "Isotope signature"

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Stehmeier, Lester, Brad Magyar, Karlis Muehlenbachs, Xiaosu Lang, and Ajay Dalai. "Use of Stable Isotope Ratios to Determine the Origin of Coke Formed in Gas Turbines." In 2002 4th International Pipeline Conference. ASMEDC, 2002. http://dx.doi.org/10.1115/ipc2002-27115.

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Coke deposits can form in compression equipment on natural gas transmission lines. These deposits are a result of incomplete combustion due to poor fuel gas quality or incorrect equipment design and/or operation. There is an isotopic “signature” which is carried over from the fuel gas into the coke if incomplete combustion occurs, allowing the origin of the coke deposit to be identified. The use of a continuous flow gas chromatograph isotope ratio mass spectrometer (GC/IRMS) provides a convenient method for determining the isotopic composition of the components in the fuel gas. These ratios ca
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Chang, Sae Jung, and Ruth Blake. "Oxygen Isotope Signature during Phosphite Oxidation by Bacterial Alkaline Phosphatase." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.359.

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Hammerli, Johannes, Tony I. S. Kemp, John Craven, et al. "INSIGHTS INTO THE SULFUR ISOTOPE SIGNATURE OF THE LOWER CRUST: IN SITU S ISOTOPE ANALYSIS OF S-RICH SCAPOLITE VIA SIMS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284982.

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Schilling, Kathrin, Alexander Halliday, Alastair Lamb, Tatjana Cronogorac-Jurcevic, and Fiona Larner. "Urinary Zinc Stable Isotope Signature as Indicator for Cancer Types with Disrupted Zinc Metabolism." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2305.

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Goodge, John W., and C. Mark Fanning. "ORIGIN AND PROVENANCE SIGNATURE OF MESOPROTEROZOIC A-TYPE GRANITES IN LAURENTIA BASED ON O-ISOTOPE COMPOSITIONS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-335091.

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Li, Jiangyan, and Jiasong Fang. "Clumped Isotope Signature of H2S, New Insights into the Process of Sulfate Reduction by the Various Microbial Mediators." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1485.

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Burch, Sara J., David A. Gonzales, Benjamin D. Holt, et al. "A COMPARISON OF GEOCHEMICAL AND HELIUM ISOTOPE SIGNATURE OF THERMAL FLUIDS, RICO AND DUNTON SPRINGS, SAN JUAN MOUNTAINS, COLORADO." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314156.

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Zambito, James J., Troy Rasbury, Kathleen C. Benison, and Gerilyn S. Soreghan. "STRONTIUM ISOTOPE RATIOS AND BORON ISOTOPIC COMPOSITION OF PERMIAN STRATA IN THE U.S. MID-CONTINENT: INTERPRETING A MARINE GEOCHEMICAL SIGNATURE IN NON-MARINE ENVIRONMENTS OF THE BLAINE FORMATION." In 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343855.

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Sauer, Kirsten B., Stacia M. Gordon, Robert B. Miller, Jeffrey D. Vervoort, and Christopher M. Fisher. "U-PB AND HF ISOTOPE SIGNATURE OF DETRITAL ZIRCONS FROM THE SWAKANE GNEISS OF THE NORTH CASCADES, WASHINGTON: IMPLICATIONS FOR RAPID BURIAL AND MARGIN-PARALLEL TRANSLATION." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274527.

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Koster, Olivia, Todd A. LaMaskin, Chad S. Lane, and Andrea D. Hawkes. "STABLE CARBON ISOTOPE SIGNATURE OF THE LATE DEVONIAN (FRASNIAN) ALAMO IMPACT AT DEVILS GATE, NEVADA: GEOLOGICALLY INSTANTANEOUS TRANSFER OF 13C-ENRICHED CARBON FROM THE LITHOSPHERE TO THE DISSOLVED INORGANIC CARBON POOL." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-320594.

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Reports on the topic "Isotope signature"

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Efurd, D. W., and D. J. Rokop. Isotopic signatures by bulk analyses. Office of Scientific and Technical Information (OSTI), 1997. http://dx.doi.org/10.2172/554812.

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2

Matthews, Murray, Pascal Achim, M. Auer, et al. WOSMIP II- Workshop on Signatures of Medical and Industrial Isotope Production. Office of Scientific and Technical Information (OSTI), 2011. http://dx.doi.org/10.2172/1062519.

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3

Dresel, P. Evan, John C. Evans, and Orville T. Farmer. Investigation of Isotopic Signatures for Sources of Groundwater Contamination at the Hanford Site. Office of Scientific and Technical Information (OSTI), 2002. http://dx.doi.org/10.2172/15001172.

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4

Moran, J. E., and G. B. Hudson. Using groundwater age and other isotopic signatures to delineate groundwater flow and stratification. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/221890.

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5

King, R. D., S. J. Piercey, R. C. Paulen, S. J. A. Day, I R Smith, and J. A. Petrus. Isotopic and geochemical signatures of base-metal indicator minerals in the southern Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2019. http://dx.doi.org/10.4095/315440.

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6

Hess, Emily. Strontium, Lead, and Oxygen Isotopic Signatures of Mid-Miocene Silicic Volcanism in Eastern Oregon. Portland State University Library, 2000. http://dx.doi.org/10.15760/etd.2077.

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7

Gaffney, Jeffrey. Natural Radionuclides and Isotopic Signatures for Determining Carbonaceous Aerosol Sources, Aerosol Lifetimes, and Washout Processes. Office of Scientific and Technical Information (OSTI), 2012. http://dx.doi.org/10.2172/1172299.

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8

Paradis, S., W. A. Turner, M. Coniglio, N. Wilson, and J L Nelson. Stable and radiogenic isotopic signatures of mineralized Devonian carbonate rocks of the northern Rocky Mountains and the Western Canada Sedimentary Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/222922.

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