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High‐precision oxygen and carbon isotope analysis of very small (10–30 µg) amounts of carbonates using continuous flow isotope ratio mass spectrometry
Author(s) -
Fiebig Jens,
Schöne Bernd R.,
Oschmann Wolfgang
Publication year - 2005
Publication title -
rapid communications in mass spectrometry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.528
H-Index - 136
eISSN - 1097-0231
pISSN - 0951-4198
DOI - 10.1002/rcm.2060
Subject(s) - chemistry , mass spectrometry , analytical chemistry (journal) , continuous flow , art history , art , physics , environmental chemistry , chromatography , mechanics
One of the major applications of stable isotope geochemistry is the estimation of palaeoenvironmental parameters from O/O and C/C ratios (commonly expressed as dO and dC versus VPDB) of calcareous hard parts of fossil marine organisms. One of these parameters is ocean temperature. Past variations are compared to instrumental records in order to understand present day and, possibly, future climatic change. Isotopic analysis of carbonates greatly benefited from the development of continuous flow isotope ratio mass spectrometry (CF-IRMS, e.g., Matthews and Hayes and Merritt and Hayes). For the purpose of CFIRMS, new automatic carbonate preparation techniques such as the Gas Bench II (Thermoquest) were designed that helped to significantly improve the daily sample throughput, with sample size as small as 50 mg. An effective sampling and correction strategy for isotopic analysis of carbonates using the Gas Bench II has recently been described by Spoetl and Vennemann. Following their procedure, external precision (1s) is better than 0.07% for dC and 0.08% for dO for sample sizes >50 mg. For lower amounts (20–50 mg), external precision drops drastically with decreasing sample size (T. Vennemann, personal communication) and averages to 0.12% for dC and 0.16% for dO, respectively. Considering that a temperature difference of 18C corresponds to a dO variation of approximately 0.2%, only temperature variations >18C can be reliably identified utilizing sample amounts <50mg. However, the decrease in precision for sample sizes <50 mg is caused by the fact that the major amount of analyte CO2 is discarded during isotopic analysis. In what follows, we describe a new cryofocus setup of the Gas Bench II that enables isotopic analyses of carbonate quantities as small as 10–30mg with external precisions indistinguishable from those of the ‘‘routine’’ setup of Spoetl and Vennemann with sample sizes >50mg. Our analytical setup equals that described by Spoetl and Vennemann with the following major modifications: (1) we use a Thermoquest MAT 253 dynamic range mass spectrometer and (2) the sample loop at the 8-way Valco valve is replaced by a cryofocusing unit, that is commercially available from Thermoquest. It consists of a Ushaped 1/1600 stainless steel tube with Ni-wire inside (cryofocus) and a 2l Dewar for storage of liquid nitrogen. The tube is fixed to a pneumatically operated lifting unit and placed above the Dewar. The Isodat software supports vertical movement of the lifting unit such that the cryofocus can be