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Journal ArticleDOI

Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide

Harmon Craig
- 01 Jan 1957 - 
- Vol. 12, Iss: 1, pp 133-149
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TLDR
In this paper, Niee's and Solenhofen standards were compared to the Chicago PDB standard for carbon and oxygen isotope ratios, and the correction factors for instrumental effects and for the nature of the mass spectra were derived.
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This article is published in Geochimica et Cosmochimica Acta.The article was published on 1957-01-01. It has received 4071 citations till now. The article focuses on the topics: Carbon & Carbon dioxide.

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Citations
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Dissolved organic carbon chemistry and dynamics in contrasting forest and grassland soils

TL;DR: In this paper, the authors examined changes in isotopic (13C and 14C) and spectroscopic (UV and 13C NMR) properties of dissolved organic carbon (DOC) in relation to soil organic matter (SOM) to elucidate the sources and sinks of DOC as water percolates through the soils of two contrasting upland coastal California ecosystems.
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Differential water resource use by herbaceous and woody plant life-forms in a shortgrass steppe community.

TL;DR: The findings support the two-layer model in a broad sense, but indicate a relatively flexible strategy of water acquisition by shrubs in the shortgrass steppe of northeastern Colorado.
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Late Quaternary Vegetation and Climate Changes in Central Texas Based on the Isotopic Composition of Organic Carbon

TL;DR: Stable carbon isotope analysis of organic carbon in alluvial deposits and soils of three streams in central Texas reveals significant shifts in the ratio of C3 to C4 plant biomass production during the past 15,000 yr as mentioned in this paper.
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Methane production in aerobic oligotrophic surface water in the central Arctic Ocean

TL;DR: In this article, it was shown that methylated compounds may serve as precursors for methane and thermodynamic calculations show that methylotrophic methanogenesis can provide energy in aerobic environments.
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Carbon isotope fractionation in the Fischer-tropsch synthesis and in meteorites.

TL;DR: Carbon dioxide and organic compounds made by a Fischer-Tropsch reaction at 400�K show a kinetic isotope fractionation of 50 to 100 per mil, similar to that observed in carbonaceous chondrites, which supports the view that organic compounds in meteorites were produced by catalytic reactions between carbon monoxide and hydrogen in the solar nebula.
References
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Journal ArticleDOI

On the Isotopic Chemistry of Carbonates and a Paleotemperature Scale

TL;DR: In this paper, the temperature variation of the fractionation of oxygen in exchange reactions between dissolved carbonate and water and between calcite and water was calculated on theoretical grounds, and checked experimentally.
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Variation of O18 content of waters from natural sources

TL;DR: A number of marine water and fresh water samples were examined for the relative O18O16 ratio, and the variation of this ratio was determined to a precision of ± 1% as mentioned in this paper.
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Revised carbonate-water isotopic temperature scale

TL;DR: The relationship between temperature and O(18) content relative to that for a Cretaceous belemnite of the Pee Dee formation previously reported (Epstein, Buchsbaum, Lowenstam, and Urey, 1951) has been re-determined using modified procedures for removing organic matter from shells, and is found to be 16.5 - 4.3 δ + 0.14 δ^2
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The geochemistry of the stable carbon isotopes

TL;DR: A survey of the variation of the ratio C13/C12 in nature can be found in this paper, where Urey and his co-workers used two complete feed systems with magnetic switching to determine small differences in isotope ratios between samples and a standard gas.