Authors

Cindy De Jonge, Swiss Federal Institute of Technology Zurich
BrGDGTs Round Robin
Francien Peterse, Utrecht University
Klaas G.J. Nierop, Utrecht University
Thomas M. Blattmann, Swiss Federal Institute of Technology Zurich
Marcelo Alexandre, Brown University
Salome Ansanay-Alex, UMR 5276 LGL-TPE
Thomas Austin, GNS Science
Mathieu Babin, Université du Québec à Rimouski
Edouard Bard, Aix-Marseille University
Thorsten Bauersachs, Kiel University
Jerome Blewett, Harvard University
Brenna Boehman, Woods Hole Oceanographic Institution
Isla S. Castañeda, University of Massachusetts
Junhui Chen, Ministry of Natural Resources of the People's Republic of China
Martina L.G. Conti, University of York
Sergio Contreras, Universidad Católica de la Santísima Concepción
Julia Cordes, University of Bremen
Nina Davtian, Autonomous University of Barcelona
Bart van Dongen, University of Manchester
Bella Duncan, Victoria University of Wellington
Felix J. Elling, Kiel University
Valier Galy, Woods Hole Oceanographic Institution
Shaopeng Gao, Chinese Academy of Sciences
Jens Hefter, Alfred Wegener Institute - Helmholtz Centre for Polar and Marine Research
Kai Uwe Hinrichs, University of Bremen
Mitchell R. Helling, University of Wyoming
Mariska Hoorweg, Utrecht University
Ellen Hopmans, Royal Netherlands Institute for Sea Research - NIOZ
Juzhi Hou, Chinese Academy of Sciences
Arnaud Huguet
Guodong Jia
Cornelia Karger
Brendan J. Keely
Stephanie Kusch
Hui Li
Jie Liang
Julius S. Lipp
Weiguo Liu
Hongxuan Lu
Kai Mangelsdorf
Hayley Manners, School of Geography, Earth and Environmental Sciences
Alfredo Martinez Garcia
Guillemette Menot
Gesine Mollenhauer
B. David A. Naafs
Sebastian Naeher
Lauren K. O'Connor
Ethan M. Pearce
Ann Pearson

ORCID

Abstract

Ratios of glycerol dialkyl glycerol tetraethers (GDGT), which are membrane lipids of bacteria and archaea, are at the base of several paleoenvironmental proxies. They are frequently applied to soils as well as lake- and marine sediments to generate records of past temperature and soil pH. To derive meaningful environmental information from these reconstructions, high analytical reproducibility is required. Based on submitted results by 39 laboratories from across the world, which employ a diverse range of analytical and quantification methods, we explored the reproducibility of brGDGT-based proxies (MBT′5ME, IR, and #ringstetra) measured on four soil samples and four soil lipid extracts. Correct identification and integration of 5- and 6-methyl brGDGTs is a prerequisite for the robust calculation of proxy values, but this can be challenging as indicated by the large inter-interlaboratory variation. The exclusion of statistical outliers improves the reproducibility, where the remaining uncertainty translates into a temperature offset from median proxy values of 0.3–0.9°C and a pH offset of 0.05–0.3. There is no apparent systematic impact of the extraction method and sample preparation steps on the brGDGT ratios. Although reported GDGT concentrations are generally consistent within laboratories, they vary greatly between laboratories. This large variability in brGDGT quantification may relate to variations in ionization efficiency or specific mass spectrometer settings possibly impacting the response of brGDGTs masses relative to that of the internal standard used. While ratio values of GDGT are generally comparable, quantities can currently not be compared between laboratories.

DOI

10.1029/2024GC011583

Publication Date

2024-06-26

Publication Title

Geochemistry, Geophysics, Geosystems

Volume

25

Issue

7

ISSN

1525-2027

Keywords

GDGT, interlaboratory comparison, round robin

Creative Commons License

Creative Commons Attribution 4.0 International License
This work is licensed under a Creative Commons Attribution 4.0 International License.

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