The Archean origin of assimilatory sulfate metabolisms provides novel insight into redox conditions of early Earth environments

Dissimilatory sulfur metabolisms recording differing biological isotopic fractionation are well studied, important components of sulfur cycling (Mateos et al., 2023). Assimilatory sulfur metabolisms and genes across life provide a complementary window into sulfur biogeochemistry with individual pathways having specific isotopic fractionations acting on distinct redox states (e.g. sulfate, sulfide, sulfite) for anabolism (Liu et al., 2012). An assimilation pathway exists, which starts with sulfate adenylyltransferase (sat/ATP sulfurylase) catalyzing a reaction of adenosine triphosphate (ATP) and sulfate (SO42-) resulting in adenosine 5’-phosphosulfate (APS), and incorporation of more reduced sulfur into biomolecules. This sat/ATP sulfurylase enzyme represents the first step required by life to incorporate sulfate and informs our understanding of biological processes performing this fundamental chemical reaction. A phylogenetic and molecular clock analysis of the sat/ATP sulfurylase protein family (E.C. 2.7.7.4) was performed to determine the age of sulfate assimilation proteins. Extant diversity of sat proteins was estimated to have a last common ancestor ~3.24 Ga (95% CI 3.52–3.06 Ga) using relaxed molecular clocks calibrated with eukaryotic and cyanobacteria age ranges from previously published fossil calibrated investigations. These results suggest sulfate cycling in Paleoarchean environments, despite extensive evidence of low marine sulfate concentrations (Crowe & Canfield et al., 2014). Archean sulfate biogeochemical cycling could result from microbial sulfur oxidation and sources could include abiotic oxidation of volcanic sulfur, hydrothermal processes or pyrite (Canfield, 2001, Lyons et al., 2024). This phylogenomic evidence of sulfate during Archean times provides an independent complement to geochemical records and indicates that sulfur redox chemistry during the Archean was likely more complex than previously described.

Name thesis:degree_name

Master

Department dc:contributor.department

Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences

Grantor dc:publisher

Massachusetts Institute of Technology

Year dc:date.issued

2025

Author dc:creator

• Payette, Jack G.

Advisor dc:contributor.advisor

• Fournier, Gregory P.

Statement dc:rights

• In Copyright - Educational Use Permitted
• Copyright retained by author(s)

Licence dc:rights.uri

• https://rightsstatements.org/page/InC-EDU/1.0/

Handle dc:identifier.uri

https://hdl.handle.net/1721.1/158898

OAI identifier oai:identifier

oai:dspace.mit.edu:1721.1/158898