New chemical and microbial perspectives on vitamin B1 and vitamer dynamics of a coastal system

Author:

Bittner Meriel J12ORCID,Bannon Catherine C3ORCID,Rowland Elden3ORCID,Sundh John4ORCID,Bertrand Erin M3ORCID,Andersson Anders F5ORCID,Paerl Ryan W67ORCID,Riemann Lasse12ORCID

Affiliation:

1. Marine Biological Section , Department of Biology, , 3000 Helsingør , Denmark

2. University of Copenhagen , Department of Biology, , 3000 Helsingør , Denmark

3. Department of Biology, Dalhousie University , Halifax, B3H 4R2, Nova Scotia , Canada

4. Department of Biochemistry and Biophysics, National Bioinformatics Infrastructure Sweden, Science for Life Laboratory, Stockholm University , Box 1031, 17121 Solna , Sweden

5. Department of Gene Technology, Science for Life Laboratory, School of Engineering Sciences in Chemistry, Biotechnology and Health, KTH Royal Institute of Technology , 17165 Stockholm , Sweden

6. Department of Marine , Earth and Atmospheric Sciences, , Raleigh, NC 2769 , United States

7. North Carolina State University , Earth and Atmospheric Sciences, , Raleigh, NC 2769 , United States

Abstract

Abstract Vitamin B1 (thiamin, B1) is an essential micronutrient for cells, yet intriguingly in aquatic systems most bacterioplankton are unable to synthesize it de novo (auxotrophy), requiring an exogenous source. Cycling of this valuable metabolite in aquatic systems has not been fully investigated and vitamers (B1-related compounds) have only begun to be measured and incorporated into the B1 cycle. Here, we identify potential key producers and consumers of B1 and gain new insights into the dynamics of B1 cycling through measurements of B1 and vitamers (HMP: 4-amino-5-hydroxymethyl-2-methylpyrimidine, HET: 4-methyl-5-thiazoleethanol, FAMP: N-formyl-4-amino-5-aminomethyl-2-methylpyrimidine) in the particulate and dissolved pool in a temperate coastal system. Dissolved B1 was not the primary limiting nutrient for bacterial production and was relatively stable across seasons with concentrations ranging from 74–117 pM, indicating a balance of supply and demand. However, vitamer concentration changed markedly with season as did transcripts related to vitamer salvage and transport suggesting use of vitamers by certain bacterioplankton, e.g. Pelagibacterales. Genomic and transcriptomic analyses showed that up to 78% of the bacterioplankton taxa were B1 auxotrophs. Notably, de novo B1 production was restricted to a few abundant bacterioplankton (e.g. Vulcanococcus, BACL14 (Burkholderiales), Verrucomicrobiales) across seasons. In summer, abundant picocyanobacteria were important putative B1 sources, based on transcriptional activity, leading to an increase in the B1 pool. Our results provide a new dynamic view of the players and processes involved in B1 cycling over time in coastal waters, and identify specific priority populations and processes for future study.

Funder

Independent Research Fund Denmark

European Union’s Horizon 2020

NSF OCE

NSERC

Simons Foundation

Publisher

Oxford University Press (OUP)

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