Carbon and oxygen isotope analysis of small carbonate samples (20 to 100 µg) with a GasBench II preparation device

Sebastian Breitenbach; Stefano M. Bernasconi

doi:10.1002/rcm.5052

Carbon and oxygen isotope analysis of small carbonate samples (20 to 100 µg) with a GasBench II preparation device

Sebastian Breitenbach, Stefano M. Bernasconi

Research output: Contribution to journal › Letter › peer-review

126 Citations (Scopus)

Abstract

Since the pioneering work by Emiliani and Shackleton, the carbon and oxygen stable isotopes of carbonates have been of major importance in geological and environmental sciences. Palaeoceanographic and terrestrial climate research (e.g. on secondary cave carbonates or lacustrine sediments) routinely make use of the δ13C and δ18O of carbonates as climate proxies.

Original language	English
Pages (from-to)	1910-1914
Number of pages	5
Journal	Rapid Communications in Mass Spectrometry
Volume	25
Issue number	13
Early online date	3 Jun 2011
DOIs	https://doi.org/10.1002/rcm.5052 https://doi.org/10.1002/rcm.5052
Publication status	Published - 15 Jul 2011

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title = "Carbon and oxygen isotope analysis of small carbonate samples (20 to 100 µg) with a GasBench II preparation device",

abstract = "Since the pioneering work by Emiliani and Shackleton, the carbon and oxygen stable isotopes of carbonates have been of major importance in geological and environmental sciences. Palaeoceanographic and terrestrial climate research (e.g. on secondary cave carbonates or lacustrine sediments) routinely make use of the δ13C and δ18O of carbonates as climate proxies.",

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AU - Breitenbach, Sebastian

AU - Bernasconi, Stefano M.

PY - 2011/7/15

Y1 - 2011/7/15

N2 - Since the pioneering work by Emiliani and Shackleton, the carbon and oxygen stable isotopes of carbonates have been of major importance in geological and environmental sciences. Palaeoceanographic and terrestrial climate research (e.g. on secondary cave carbonates or lacustrine sediments) routinely make use of the δ13C and δ18O of carbonates as climate proxies.

AB - Since the pioneering work by Emiliani and Shackleton, the carbon and oxygen stable isotopes of carbonates have been of major importance in geological and environmental sciences. Palaeoceanographic and terrestrial climate research (e.g. on secondary cave carbonates or lacustrine sediments) routinely make use of the δ13C and δ18O of carbonates as climate proxies.

UR - https://www.scopus.com/pages/publications/79958109723

U2 - 10.1002/rcm.5052

DO - 10.1002/rcm.5052

M3 - Letter

AN - SCOPUS:79958109723

SN - 0951-4198

VL - 25

SP - 1910

EP - 1914

JO - Rapid Communications in Mass Spectrometry

JF - Rapid Communications in Mass Spectrometry

IS - 13

ER -

Carbon and oxygen isotope analysis of small carbonate samples (20 to 100 µg) with a GasBench II preparation device

Abstract

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