Compound‐specific stable carbon isotope ratios (δ 13 C values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1)

Abstract Compound‐specific isotope analysis using gas chromatography interfaced to isotope ratio mass spectrometry (GC/IRMS) was applied for the determination of δ 13 C values of the marine halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1). The δ 13 C value of a...

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Published in:Rapid Communications in Mass Spectrometry
Main Authors: Vetter, Walter, Gleixner, Gerd
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2006
Subjects:
Online Access:http://dx.doi.org/10.1002/rcm.2686
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spelling crwiley:10.1002/rcm.2686 2024-06-02T07:57:46+00:00 Compound‐specific stable carbon isotope ratios (δ 13 C values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1) Vetter, Walter Gleixner, Gerd 2006 http://dx.doi.org/10.1002/rcm.2686 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Frcm.2686 https://onlinelibrary.wiley.com/doi/full/10.1002/rcm.2686 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Rapid Communications in Mass Spectrometry volume 20, issue 20, page 3018-3022 ISSN 0951-4198 1097-0231 journal-article 2006 crwiley https://doi.org/10.1002/rcm.2686 2024-05-03T11:04:41Z Abstract Compound‐specific isotope analysis using gas chromatography interfaced to isotope ratio mass spectrometry (GC/IRMS) was applied for the determination of δ 13 C values of the marine halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1). The δ 13 C value of a lab‐made Q1 standard (−34.20 ± 0.27‰) was depleted in 13 C by more than 11‰ relative to the residues of Q1 in dolphin blubber from Australia and skua liver from Antarctica. This clarified that the synthesized Q1 was not the source for Q1 in the biota samples. However, two Australian marine mammals showed a large variation in the δ 13 C value, which, in our experience, was implausible. Since the GC/IRMS system was connected to a conventional ion trap mass spectrometer by a post‐column splitter, we were able to closely inspect the peak purity of Q1 in the respective samples. While the mass spectra of Q1 did not indicate any impurity, a fronting peak of PCB 101 was identified in one sample. This interference falsified the δ 13 C value of the respective sample. Once this sample was excluded, we found that the δ 13 C values of the remaining samples, i.e. liver of Antarctic brown skua (−21.47 ± 1.47‰) and blubber of Australian melon‐headed whale (−22.80 ± 0.33‰), were in the same order. The standard deviation for Q1 was larger in the skua samples than in the standard and the whale blubber sample. This was due to lower amounts of skua sample available. It remained unclear if the Q1 residues originate from the same producer and location. Copyright © 2006 John Wiley & Sons, Ltd. Article in Journal/Newspaper Antarc* Antarctic Antarctica Brown Skua Wiley Online Library Antarctic Rapid Communications in Mass Spectrometry 20 20 3018 3022
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract Compound‐specific isotope analysis using gas chromatography interfaced to isotope ratio mass spectrometry (GC/IRMS) was applied for the determination of δ 13 C values of the marine halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1). The δ 13 C value of a lab‐made Q1 standard (−34.20 ± 0.27‰) was depleted in 13 C by more than 11‰ relative to the residues of Q1 in dolphin blubber from Australia and skua liver from Antarctica. This clarified that the synthesized Q1 was not the source for Q1 in the biota samples. However, two Australian marine mammals showed a large variation in the δ 13 C value, which, in our experience, was implausible. Since the GC/IRMS system was connected to a conventional ion trap mass spectrometer by a post‐column splitter, we were able to closely inspect the peak purity of Q1 in the respective samples. While the mass spectra of Q1 did not indicate any impurity, a fronting peak of PCB 101 was identified in one sample. This interference falsified the δ 13 C value of the respective sample. Once this sample was excluded, we found that the δ 13 C values of the remaining samples, i.e. liver of Antarctic brown skua (−21.47 ± 1.47‰) and blubber of Australian melon‐headed whale (−22.80 ± 0.33‰), were in the same order. The standard deviation for Q1 was larger in the skua samples than in the standard and the whale blubber sample. This was due to lower amounts of skua sample available. It remained unclear if the Q1 residues originate from the same producer and location. Copyright © 2006 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Vetter, Walter
Gleixner, Gerd
spellingShingle Vetter, Walter
Gleixner, Gerd
Compound‐specific stable carbon isotope ratios (δ 13 C values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1)
author_facet Vetter, Walter
Gleixner, Gerd
author_sort Vetter, Walter
title Compound‐specific stable carbon isotope ratios (δ 13 C values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1)
title_short Compound‐specific stable carbon isotope ratios (δ 13 C values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1)
title_full Compound‐specific stable carbon isotope ratios (δ 13 C values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1)
title_fullStr Compound‐specific stable carbon isotope ratios (δ 13 C values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1)
title_full_unstemmed Compound‐specific stable carbon isotope ratios (δ 13 C values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (Q1)
title_sort compound‐specific stable carbon isotope ratios (δ 13 c values) of the halogenated natural product 2,3,3′,4,4′,5,5′‐heptachloro‐1′‐methyl‐1,2′‐bipyrrole (q1)
publisher Wiley
publishDate 2006
url http://dx.doi.org/10.1002/rcm.2686
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Frcm.2686
https://onlinelibrary.wiley.com/doi/full/10.1002/rcm.2686
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
Brown Skua
genre_facet Antarc*
Antarctic
Antarctica
Brown Skua
op_source Rapid Communications in Mass Spectrometry
volume 20, issue 20, page 3018-3022
ISSN 0951-4198 1097-0231
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op_doi https://doi.org/10.1002/rcm.2686
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