Articles | Volume 23, issue 1
https://doi.org/10.5194/bg-23-21-2026
https://doi.org/10.5194/bg-23-21-2026
Research article
 | 
05 Jan 2026
Research article |  | 05 Jan 2026

Archaeal lipostratigraphy of the Scotian Slope shallow sediments, Atlantic Canada

Narges Ahangarian, Unyime U. Umoh, Natasha MacAdam, Adam MacDonald, Patricia Granados, Jeremy N. Bentley, Elish Redshaw, Martin G. Fowler, Venus Baghalabadi, and G. Todd Ventura

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Cited articles

Arndt, S., Jørgensen, B. B., LaRowe, D. E., Middelburg, J. J., Pancost, R. D., and Regnier, P.: Quantifying the degradation of organic matter in marine sediments: A review and synthesis, Earth-Sci. Rev., 123, 53–86, https://doi.org/10.1016/j.earscirev.2013.02.008, 2013. 
Bauersachs, T., Weidenbach, K., Schmitz, R. A., and Schwark, L.: Distribution of glycerol ether lipids in halophilic, methanogenic and hyperthermophilic archaea, Org. Geochem., 83–84, 101–108, https://doi.org/10.1016/j.orggeochem.2015.03.009, 2015. 
Bennett, R. and Desiage, P.-A.: Expedition report 21CONDOR: Scotian Slope, 14–29 August 2021 (Open File 8889, Geological Survey of Canada, 2022), https://doi.org/10.4095/329977, 2022. 
Bentley, J. N., Ventura, G. T., Walters, C. C., Sievert, S. M., and Seewald, J. S.: The influence of near-surface sediment hydrothermalism on the TEX86 tetraether-lipid-based proxy and a new correction for ocean bottom lipid overprinting, Biogeosciences, 19, 4459–4477, https://doi.org/10.5194/bg-19-4459-2022, 2022. 
Berner, R. A.: Early Diagenesis: A theoretical Approach. Princeton University Press, Princeton, 241 pp., ISBN 9780691082608, 1980. 
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This study documents previously unknown, shallow sediment stratigraphic archaeal zones that extend over a large section of the Scotian Slope of Northeastern Canada. These zones appear to be geochemically and not lithologically controlled. They are also not detectable by using traditional lipid biomarker ratios. They indicate subsurface microbial community structures to be more complex and tractable over large expanses of the continental margins.
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