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Thematische Bibliographien / Stable isotopes geochemistry / Zeitschriftenartikel

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Zeitschriftenartikel zum Thema „Stable isotopes geochemistry“

Autor: Grafiati

Veröffentlicht am 25. Mai 2024

Zuletzt aktualisiert am 31. Juli 2025

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1

Ogbesejana, Abiodun Busuyi, Bo Liu, and Mehdi Ostadhassan. "Stable Isotope Geochemistry of the Organic Elements within Shales and Crude Oils: A Comprehensive Review." Molecules 27, no. 1 (2021): 34. http://dx.doi.org/10.3390/molecules27010034.

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Over time, stable isotopes have proven to be a useful tool in petroleum geochemistry. However, there is currently insufficient literature on stable isotope geochemistry of the organic elements within shales and crude oils in many petroleum systems around the world. As a result, this paper critically reviews the early and recent trends in stable isotope geochemistry of organic elements in shales and crude oils. The bulk and compound-specific stable isotopes of H, C, and S, as well as their uses as source facies, depositional environments, thermal maturity, geological age, and oil–oil and oil–so

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2

Pollard, A. M. "Isotopes and impact: a cautionary tale." Antiquity 85, no. 328 (2011): 631–38. http://dx.doi.org/10.1017/s0003598x00068034.

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There can be no doubt that isotopic studies have made a huge contribution to archaeology in recent years, so much so that isotope archaeology is now seen as an essential subdiscipline of archaeology in much the same way as isotope geochemistry is a key subdiscipline of geochemistry. Ignoring for current purposes the contribution made by the measurement of a particular radioactive isotope of carbon (14C) since 1950, we can date the beginnings of isotope archaeology to the mid 1960s with the first measurements of lead isotopes in archaeological metals and slags by Brill and Wampler (1965, 1967).

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3

Corfield, Richard M., and Richard D. Norris. "Isotope Paleobiology and Paleoecology: So Why Should Paleontologists Care About Geochemistry?" Paleontological Society Papers 4 (October 1998): 1–6. http://dx.doi.org/10.1017/s1089332600000371.

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Stable isotopic techniques in geology illuminate not only variations in past climates and oceans, but also the life-histories of extinct animals, plants and protistans. This volume focuses on the ways that stable isotopes can be used as tracers of the fossil biology and ecology of long-dead organisms and ecosystems. Here, we introduce relevant aspects of stable isotope systematics and provide a summary of the papers collected in this volume. The nine contributions collected here, from some of the most eminent workers in their respective fields, explore aspects of the ecology, evolution and bio

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4

Farquhar, James. "Geochemistry of Non-Traditional Stable Isotopes." Geochimica et Cosmochimica Acta 69, no. 11 (2005): 2947–48. http://dx.doi.org/10.1016/j.gca.2004.12.016.

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5

Tissot, François L. H., and Mauricio Ibañez-Mejia. "Unlocking the Single-Crystal Record of Heavy Stable Isotopes." Elements 17, no. 6 (2021): 389–94. http://dx.doi.org/10.2138/gselements.17.6.389.

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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,

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6

Aggarwal, Jugdeep, Judith Habicht-Mauche, and Chelsey Juarez. "Application of heavy stable isotopes in forensic isotope geochemistry: A review." Applied Geochemistry 23, no. 9 (2008): 2658–66. http://dx.doi.org/10.1016/j.apgeochem.2008.05.016.

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7

Alderton, David H. M. "Oxygen isotope fractionation between cassiterite and water." Mineralogical Magazine 53, no. 371 (1989): 373–76. http://dx.doi.org/10.1180/minmag.1989.053.371.13.

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Analysis of stable isotopes in coexisting minerals has found wide application in the study of hydrothermal mineral deposits, particularly for elucidating the temperature and source of the fluid phase involved in mineralisation. For these purposes the temperature dependence of isotopic fractionation in several mineral-water systems has already been established (e.g. Friedman and O'Neil, 1977; O'Neil, 1986). Unfortunately, the oxygen isotope fractionation between cassiterite (SnO2) and water has not been adequately characterized, and this has hindered a full utilization of oxygen isotope data de

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8

Yang, Kunhua, Guilin Han, Man Liu, Xiaoqiang Li, Jinke Liu, and Qian Zhang. "Spatial and Seasonal Variation of O and H Isotopes in the Jiulong River, Southeast China." Water 10, no. 11 (2018): 1677. http://dx.doi.org/10.3390/w10111677.

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The stable isotope technique of oxygen and hydrogen (δ18O and δ2H) and deuterium excess (d-excess) was used to investigate distribution characteristics in June 2017 and January 2018 in the Jiulong River, southeast China. The results revealed that (1) seasonal isotopic composition was mainly controlled by precipitation. It enriched lighter water isotopes in winter more than in summer because of the aggravating effect of low temperature and great rainfall. (2) Spatial distribution of the North, West, and South River showed increasing enrichment of heavy isotopes in that order. In the high-flow s

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Ibañez-Mejia, Mauricio, and François L. H. Tissot. "Reading the Isotopic Code of Heavy Elements." Elements 17, no. 6 (2021): 379–82. http://dx.doi.org/10.2138/gselements.17.6.379.

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The isotopic variability of the elements in our planet and Solar System is the end result of a complex mixture of processes, including variable production of isotopes in stars, ingrowth of daughter nuclides due to decay of radioactive parents, and selective incorporation of isotopes into solids, liquids, or gases as a function of their mass and/or nuclear volume. Interpreting the isotopic imprints that planetary formation and evolution have left in the rock and mineral record requires not only precise and accurate measurements but also an understanding of the drivers behind isotopic variabilit

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10

Hidayat, Hadi, Boy Yoseph та Teuku Yan Waliana Muda Iskandarsyah. "Characteristics of Groundwater Hydrochemistry and Stable Isotopes (δ18O & δ2H) in Cadasari, Banten, Indonesia". Journal of Geoscience, Engineering, Environment, and Technology 10, № 02 (2025): 154–61. https://doi.org/10.25299/jgeet.2025.10.02.21531.

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Groundwater is an essential resource for drinking and domestic use, displaying significant diversity in volcanic regions.This study focuses on Cadasari, Banten, Indonesia, and aims to determine the hydrochemical characteristics of groundwater and the stable isotopes (δ18O & δ2H). Hydrogeological mapping was employed, and analytical data were collected from 20 groundwater sources, including springs, rivers, and wells, at elevations ranging from 167 to 928 meters above sea level. The hydrochemical analysis revealed various groundwater types, such as Ca-HCO3, Ca+Mg-HCO3, Na+K+Ca-HCO3, and Na+

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11

Burgess, Ray, Mitsuru Ebihara, and Hans Eggenkamp. "Developments in Halogen Abundance and Isotope Measurements." Elements 18, no. 1 (2022): 41–46. http://dx.doi.org/10.2138/gselements.18.1.41.

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The four stable halogens (F, Cl, Br, and I) are low-abundance elements that are widely distributed in nature. Two of the halogens, Cl and Br, each have two stable isotopes showing a range in natural isotope variation of up to a few parts per thousand. A variety of analytical techniques have been developed to determine the abundance and isotopic ratios of the halogens: these include in situ techniques for high spatial resolution studies and bulk determinations, and they have been applied to a range of materials, including whole rocks, minerals, glasses, and fluid inclusions. Here, we summarise

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Liu, Zhanmin, Congqiang Liu, Guilin Han, et al. "Environmental geochemistry of calcium isotopes: Applications of a new stable isotope approach." Chinese Journal of Geochemistry 25, no. 2 (2006): 184–94. http://dx.doi.org/10.1007/bf02872181.

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13

Volkman, John K. "Future Outlook for Applications of Biomarkers and Isotopes in Organic Geochemistry." Elements 18, no. 2 (2022): 115–20. http://dx.doi.org/10.2138/gselements.18.2.115.

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Organic geochemistry continues to make important contributions to our understanding of how the biogeochemistry of our planet and its environment has changed over time and of the role of human impacts today. This article provides a brief overview of the field and a perspective on how it might develop in the near future. Particular emphasis is placed on biomarkers (compounds with a distinctive chemical structure that can be related to specific organisms) and stable isotopes of carbon, hydrogen, and nitrogen, as these are major tools used by organic geochemists. Many geochemical studies involve a

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14

Eastoe, C. J., and J. M. Guilbert. "Stable chlorine isotopes in hydrothermal processes." Geochimica et Cosmochimica Acta 56, no. 12 (1992): 4247–55. http://dx.doi.org/10.1016/0016-7037(92)90265-k.

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15

Abudeif, Abdelbaset M., Gamal Z. Abdel Aal, Nessreen F. Abdelbaky, Mohamed H. Ali, and Mohammed A. Mohammed. "An Integrated Geophysics and Isotope Geochemistry to Unveil the Groundwater Paleochannel in Abydos Historical Site, Egypt." Minerals 13, no. 1 (2022): 64. http://dx.doi.org/10.3390/min13010064.

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The scientific controversy among archaeologists about the existence of paleochannels under the Abydos archaeological site, Sohag, Egypt connecting the Osirion (cenotaph of Seti I) with the Nile River has been explained in this study. This study is an attempt to address this issue using integrating a near-surface geophysical approach with stable isotopic geochemistry on this site. Particularly, the stable oxygen and hydrogen isotopes on the water samples collected from the surface and the groundwater in the study area were analyzed and interpreted. The isotopes result showed that the Osirion wa

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16

Nurgaliev, D. K., I. Yu Chernova, D. I. Khassanov, B. I. Gareev, G. A. Batalin, and D. Ya Khabibullin. "Comparing the results of lineament analysis with isotope geochemistry data." SOCAR Proceedings, SI2 (December 30, 2021): 110–18. http://dx.doi.org/10.5510/ogp2021si200562.

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This article presents the results of a geochemical survey carried out in the southwestern part of the Siberian platform, within the Sayan-Yenisei (Angara) syneclise (a superorder Riphean-Middle Paleozoic structure). The object of research was hydrocarbon gases contained in the subsoil rocks (clays). The subsoil samples were taken from the bottom of boreholes (40 mm in diameter) made with an electric drill. The sampling depth was 0.6–1 m. Further laboratory studies included chromatographic and isotope analysis. Lineament analysis of the digital elevation model was carried out as a complementary

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17

Baumgartner, L. P., and D. Rumble. "Transport of stable isotopes: I: Development of a kinetic continuum theory for stable isotope transport." Contributions to Mineralogy and Petrology 98, no. 4 (1988): 417–30. http://dx.doi.org/10.1007/bf00372362.

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18

West, Catherine F. "Islands, Coastlines, and Stable Isotopes: Advances in Archaeology and Geochemistry." Journal of Island and Coastal Archaeology 8, no. 2 (2013): 149–51. http://dx.doi.org/10.1080/15564894.2013.803895.

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19

Feineman, Maureen, Sarah Penniston-Dorland, Franck Poitrasson, and Stefan Weyer. "Applications of non-traditional stable isotopes in high-temperature geochemistry." Chemical Geology 258, no. 1-2 (2009): 1–4. http://dx.doi.org/10.1016/j.chemgeo.2008.08.008.

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20

Pang, Zhonghe, Jie Li, and Jiao Tian. "Noble gas geochemistry and chronology of groundwater in an active rift basin in central China." E3S Web of Conferences 98 (2019): 01040. http://dx.doi.org/10.1051/e3sconf/20199801040.

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Stable noble gas isotopes are excellent groundwater tracers. Radioactive noble gases are emerging new tools in the study of groundwater circulation dynamics. Among these, the 85Kr and 81Kr, and 39Ar have advanced very fast in recent years and exhibit strong potential in the reconstruction of the history of groundwater recharge and evolution in sedimentary basins at different scales. Here, we report the findings in groundwater circulation dynamics as relative to intensive water-rock interactions, heat transfer and He gas flux in Guanzhong Basin located in Xi’an, the geographical centre of China

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21

Ghosh, Santanu, Tushar Adsul, Balram Tiwari, Dinesh Kumar, and Atul Kumar Varma. "Exploring Geochemical Signatures in Production Water: Insights from Coal Bed Methane and Shale Gas Exploration—A Brief Review." Methane 3, no. 1 (2024): 172–90. http://dx.doi.org/10.3390/methane3010011.

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This article furnishes a brief review of the geochemistry of waters produced during coal bed methane and shale gas exploration. Stable deuterium and oxygen isotopes of produced waters, as well as the stable carbon isotope of dissolved inorganic carbon in these waters, are influenced by groundwater recharge, methanogenic pathways, the mixing of formation water with saline water, water–rock interactions, well completion, contamination from water from adjacent litho-units, and coal bed dewatering, among many others. Apart from the isotopic fingerprints, significant attention should be given to th

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22

Huber, Miłosz A., Stanisław Hałas, Yuri N. Neradovsky, Tamara B. Bayanova, Artem W. Mokrushin, and Lesia Lata. "Stable isotope geochemistry of sulfides from intrusion in Monchegorsk, northern part of Baltic Shield." Geochronometria 43, no. 1 (2016): 96–101. http://dx.doi.org/10.1515/geochr-2015-0034.

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Abstract The sulfide minerals from old mafic intrusion rocks from the Kola Peninsula were analyzed on stable sulfur isotopes. These samples were already dated by the Sm-Nd method. These sulfide samples were evaluated upon a geochemical composition by ICP-MS. The sulfide mineral samples were selected from the main ore-bearing rocks of the Monchetundra layered intrusion. The analyzed sulfides formed several generations of mineralization associated with primary and hydrothermal stage of formation of the deposits. Isotopic studies confirm a few consecutive stages of mineralization. These data were

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23

Hatzinger, Paul B., John Karl Böhlke, Neil C. Sturchio, Baohua Gu, Linnea J. Heraty, and Robert C. Borden. "Fractionation of stable isotopes in perchlorate and nitrate during in situ biodegradation in a sandy aquifer." Environmental Chemistry 6, no. 1 (2009): 44. http://dx.doi.org/10.1071/en09008.

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Environmental context. Perchlorate (ClO4–) and nitrate (NO3–) are common co-contaminants in groundwater, with both natural and anthropogenic sources. Each of these compounds is biodegradable, so in situ enhanced bioremediation is one alternative for treating them in groundwater. Because bacteria typically fractionate isotopes during biodegradation, stable isotope analysis is increasingly used to distinguish this process from transport or mixing-related decreases in contaminant concentrations. However, for this technique to be useful in the field to monitor bioremediation progress, isotope frac

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Clarke, W. B., J. H. Crocket, R. J. Gillespie, H. R. Krouse, D. M. Shaw, and H. P. Schwarcz. "Henry George Thode, M.B.E. 10 September 1910 — 22 March 1997." Biographical Memoirs of Fellows of the Royal Society 46 (January 2000): 499–514. http://dx.doi.org/10.1098/rsbm.1999.0098.

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Henry George Thode was one of Canada's most distinguished physical scientists, internationally known for his work in the fields of geochemistry and nuclear chemistry. He did much of the pioneering work on the separation and concentration of stable isotopes, and made seminal studies of the natural variations in the isotopic composition of the elements in nature, particularly sulphur. Morever, he was the principal force behind the development of McMaster University in Hamilton, Ontario, from a small church-affiliated liberal arts college with 600 students to one of Canada's leading universities

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Druhan, Jennifer L., and Matthew J. Winnick. "Reactive Transport of Stable Isotopes." Elements 15, no. 2 (2019): 107–10. http://dx.doi.org/10.2138/gselements.15.2.107.

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26

Mueller, M. H., R. Weingartner, and C. Alewell. "Importance of vegetation, topography and flow paths for water transit times of base flow in alpine headwater catchments." Hydrology and Earth System Sciences 17, no. 4 (2013): 1661–79. http://dx.doi.org/10.5194/hess-17-1661-2013.

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Abstract. The mean transit time (MTT) of water in a catchment gives information about storage, flow paths, sources of water and thus also about retention and release of solutes in a catchment. To our knowledge there are only a few catchment studies on the influence of vegetation cover changes on base flow MTTs. The main changes in vegetation cover in the Swiss Alps are massive shrub encroachment and forest expansion into formerly open habitats. Four small and relatively steep headwater catchments in the Swiss Alps (Ursern Valley) were investigated to relate different vegetation cover to water

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Kyser, T. K. "Stable isotopes and fractionations in the mantle." Chemical Geology 70, no. 1-2 (1988): 184. http://dx.doi.org/10.1016/0009-2541(88)90742-5.

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28

Aarons, Sarah M., Aleisha C. Johnson, and Shelby T. Rader. "Forming Earth’s Continental Crust: A Nontraditional Stable Isotope Perspective." Elements 17, no. 6 (2021): 413–18. http://dx.doi.org/10.2138/gselements.17.6.413.

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The formation of continental crust via plate tectonics strongly influences the physical and chemical characteristics of Earth’s surface and may be the key to Earth’s long-term habitability. However, continental crust formation is difficult to observe directly and is even more difficult to trace through time. Nontraditional stable isotopes have yielded significant insights into this process, leading to a new view both of Earth’s earliest continental crust and of what controls modern crustal generation. The stable isotope systems of titanium (Ti), zirconium (Zr), molybdenum (Mo), and thallium (T

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Magette, Evan, Adam Turner, Yongbo Peng, and Achim D. Herrmann. "Syndepositional Uptake of Uranium, Molybdenum and Vanadium into Modern Bahamian Carbonate Sediments during Early Diagenesis." Geosciences 13, no. 3 (2023): 66. http://dx.doi.org/10.3390/geosciences13030066.

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Syndepositional diagenesis is a complicating factor when interpreting geochemical proxies in carbonate sedimentary environments. Previous studies have suggested that carbonate deposits may preserve the geochemical and isotopic signatures of seawater that can be used for paleo-redox reconstructions. However, more work is necessary to understand how these trace metals are preserved. The present study examines shallow marine carbonate sediments from the Bahamas to better understand diagenetic effects on trace metal uptake and sequestration. Analysis of diagenetic effects and trace metal uptake fo

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Pracht, Hilde, Brett Metcalfe, and Frank J. C. Peeters. "Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth." Biogeosciences 16, no. 2 (2019): 643–61. http://dx.doi.org/10.5194/bg-16-643-2019.

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Abstract. The translation of the original seawater signal (i.e. ambient temperature and δ18Osw) into distinct chambers of a single shell of a foraminifer during calcification can influence our interpretation of surface ocean conditions of the past, when based upon oxygen and carbon stable isotope geochemistry. In this study three different hypotheses were tested to gain more insight into biological and ecological processes that influence the resultant composition of stable isotopes of oxygen (δ18O) in the shells of planktonic foraminifera. These hypotheses were related to the shell size; the d

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Cameron, Eion M. "Stable isotopes in high temperature geological processes." Journal of Geochemical Exploration 30, no. 1-3 (1988): 323–24. http://dx.doi.org/10.1016/0375-6742(88)90067-2.

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32

Chela-Flores, J. "A case for landing on the moon's farside to test nitrogen abundances." International Journal of Astrobiology 11, no. 1 (2011): 61–69. http://dx.doi.org/10.1017/s1473550411000334.

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AbstractA high research priority in astrobiology is the search and eventual identification of biomarkers in the Solar System. In spite of numerous steps forward, lunar science remains largely disjoint from the main stream of astrobiology, but in recent years the Moon has begun to emerge as a novel target for astrobiologists. We discuss an overlap between lunar geology and terrestrial geomicrobiology that arises from analysis of lunar soils and some uncertainties in chemical evolution and the origin of life scenarios. Unexpected isotopic heterogeneity of nitrogen (N) was found to be remarkable

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Pack, Andreas, Stephan Hoernes, Matthias Göbbels, Rainer Bross, and Andreas Buhr. "Stable oxygen isotopes - A new approach for tracing the origin of oxide inclusions in steels." European Journal of Mineralogy 17, no. 3 (2005): 483–93. http://dx.doi.org/10.1127/0935-1221/2005/0017-0483.

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Anbar, A. D. "Iron stable isotopes: beyond biosignatures." Earth and Planetary Science Letters 217, no. 3-4 (2004): 223–36. http://dx.doi.org/10.1016/s0012-821x(03)00572-7.

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Aléon, Jérôme, Marc Chaussidon, Michel Champenois, and Denis Mangin. "Quantitative Imaging of Stable Isotopes by Ion Microprobe." Geostandards and Geoanalytical Research 25, no. 2-3 (2001): 417–29. http://dx.doi.org/10.1111/j.1751-908x.2001.tb00998.x.

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HARLEY, S. L., and C. M. GRAHAM. "Stable isotopes as tracers of metamorphic processes: introduction." Journal of Metamorphic Geology 12, no. 3 (1994): 209–10. http://dx.doi.org/10.1111/j.1525-1314.1994.tb00016.x.

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Clark, Ian D., and Bernard Lauriol. "Kinetic enrichment of stable isotopes in cryogenic calcites." Chemical Geology 102, no. 1-4 (1992): 217–28. http://dx.doi.org/10.1016/0009-2541(92)90157-z.

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38

Xia, Di, Han Ye, Yingying Xie, et al. "Isotope geochemistry, hydrochemistry, and mineralogy of a river affected by acid mine drainage in a mining area, South China." RSC Advances 7, no. 68 (2017): 43310–18. http://dx.doi.org/10.1039/c7ra07809a.

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Hansen, Hans Jørgen. "Stable isotopes of carbon from basaltic rocks and their possible relation to atmospheric isotope excursions." Lithos 92, no. 1-2 (2006): 105–16. http://dx.doi.org/10.1016/j.lithos.2006.03.029.

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40

Ray, Jyotiranjan S., and R. Ramesh. "Rayleigh fractionation of stable isotopes from a multicomponent source." Geochimica et Cosmochimica Acta 64, no. 2 (2000): 299–306. http://dx.doi.org/10.1016/s0016-7037(99)00181-7.

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41

Youke, Han, and An Na. "An approach to analysis of stable isotopes in microsamples." Chinese Journal of Geochemistry 10, no. 4 (1991): 372–78. http://dx.doi.org/10.1007/bf02841098.

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42

Green, Daniel R., Tanya M. Smith, Gregory M. Green, Felicitas B. Bidlack, Paul Tafforeau, and Albert S. Colman. "Quantitative reconstruction of seasonality from stable isotopes in teeth." Geochimica et Cosmochimica Acta 235 (August 2018): 483–504. http://dx.doi.org/10.1016/j.gca.2018.06.013.

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Crumpton-Banks, Jessica G. M., Thomas Tanner, Ivan Hernández Almeida, James W. B. Rae, and Heather Stoll. "Technical note: No impact of alkenone extraction on foraminiferal stable isotope, trace element and boron isotope geochemistry." Biogeosciences 19, no. 24 (2022): 5633–44. http://dx.doi.org/10.5194/bg-19-5633-2022.

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Abstract. Recent advances in geochemical techniques mean that several robust proxies now exist to determine the past carbonate chemistry of the oceans. Foraminiferal δ11B and alkenone carbon isotopes allow us to reconstruct sea-surface pH and pCO2, respectively, and the ability to apply both proxies to the same sediment sample would give strongly paired datasets and reduce sample waste. However, no studies to date have examined whether the solvents and extraction techniques used to prepare alkenones for analysis also impact the geochemistry of foraminifera within those sediments. Here we exami

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Laeter, John R. "The Role of Isotopic Reference Materials for the Analysis of "Non-Traditional" Stable Isotopes." Geostandards and Geoanalytical Research 29, no. 1 (2005): 53–61. http://dx.doi.org/10.1111/j.1751-908x.2005.tb00655.x.

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Ibrahim, Khalil, Issa Makhlouf, Ali El Naqah, and Sana’ Al-Thawabteh. "Geochemistry and Stable Isotopes of Travertine from Jordan Valley and Dead Sea Areas." Minerals 7, no. 5 (2017): 82. http://dx.doi.org/10.3390/min7050082.

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Garnit, Hechmi, Maria Boni, Giuliana Buongiovanni, et al. "C–O Stable Isotopes Geochemistry of Tunisian Nonsulfide Zinc Deposits: A First Look." Minerals 8, no. 1 (2018): 13. http://dx.doi.org/10.3390/min8010013.

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Gammons, C. H., D. M. Snyder, S. R. Poulson, and K. Petritz. "Geochemistry and Stable Isotopes of the Flooded Underground Mine Workings of Butte, Montana." Economic Geology 104, no. 8 (2009): 1213–34. http://dx.doi.org/10.2113/gsecongeo.104.8.1213.

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Philp, R. Paul. "The emergence of stable isotopes in environmental and forensic geochemistry studies: a review." Environmental Chemistry Letters 5, no. 2 (2006): 57–66. http://dx.doi.org/10.1007/s10311-006-0081-y.

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Albarède, Francis. "Metal Stable Isotopes in the Human Body: A Tribute of Geochemistry to Medicine." Elements 11, no. 4 (2015): 265–69. http://dx.doi.org/10.2113/gselements.11.4.265.

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Meyer, H., and R. S. Sletten. "Preface to the special issue on stable isotopes and geochemistry of ground ice." Permafrost and Periglacial Processes 22, no. 1 (2011): 1–2. http://dx.doi.org/10.1002/ppp.718.

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