A timeline of bacterial and archaeal diversification in the ocean

dc.contributor.authorMartinez-Gutierrez, Carolina A.en
dc.contributor.authorUyeda, Josef C.en
dc.contributor.authorAylward, Frank O.en
dc.date.accessioned2023-12-13T20:30:11Zen
dc.date.available2023-12-13T20:30:11Zen
dc.date.issued2023-12en
dc.description.abstractMicrobial plankton play a central role in marine biogeochemical cycles, but the timing in which abundant lineages diversified into ocean environments remains unclear. Here, we reconstructed the timeline in which major clades of bacteria and archaea colonized the ocean using a high-resolution benchmarked phylogenetic tree that allows for simultaneous and direct comparison of the ages of multiple divergent lineages. Our findings show that the diversification of the most prevalent marine clades spans throughout a period of 2.2 Ga, with most clades colonizing the ocean during the last 800 million years. The oldest clades - SAR202, SAR324, <i>Ca</i>. Marinimicrobia, and Marine Group II - diversified around the time of the Great Oxidation Event, during which oxygen concentration increased but remained at microaerophilic levels throughout the Mid-Proterozoic, consistent with the prevalence of some clades within these groups in oxygen minimum zones today. We found the diversification of the prevalent heterotrophic marine clades SAR11, SAR116, SAR92, SAR86, and Roseobacter as well as the Marine Group I to occur near to the Neoproterozoic Oxygenation Event (0.8-0.4 Ga). The diversification of these clades is concomitant with an overall increase of oxygen and nutrients in the ocean at this time, as well as the diversification of eukaryotic algae, consistent with the previous hypothesis that the diversification of heterotrophic bacteria is linked to the emergence of large eukaryotic phytoplankton. The youngest clades correspond to the widespread phototrophic clades <i>Prochlorococcus, Synechococcus,</i> and <i>Crocosphaera</i>, whose diversification happened after the Phanerozoic Oxidation Event (0.45-0.4 Ga), in which oxygen concentrations had already reached their modern levels in the atmosphere and the ocean. Our work clarifies the timing at which abundant lineages of bacteria and archaea colonized the ocean, thereby providing key insights into the evolutionary history of lineages that comprise the majority of prokaryotic biomass in the modern ocean.en
dc.description.versionPublished versionen
dc.format.mimetypeapplication/pdfen
dc.identifier.doihttps://doi.org/10.7554/elife.88268en
dc.identifier.eissn2050-084Xen
dc.identifier.issn2050-084Xen
dc.identifier.orcidAylward, Frank [0000-0002-1279-4050]en
dc.identifier.orcidUyeda, Josef [0000-0003-4624-9680]en
dc.identifier.otherPMC10703444en
dc.identifier.other88268 (PII)en
dc.identifier.pmid38059790en
dc.identifier.urihttps://hdl.handle.net/10919/117186en
dc.identifier.volume12en
dc.language.isoenen
dc.publishereLife Sciencesen
dc.relation.urihttps://www.ncbi.nlm.nih.gov/pubmed/38059790en
dc.rightsCreative Commons Attribution 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en
dc.subjectGreat Oxidation Eventen
dc.subjectarchaeaen
dc.subjectevolutionary biologyen
dc.subjectgeneticsen
dc.subjectgenomicsen
dc.subjectmarine bacteriaen
dc.subjectmolecular datingen
dc.titleA timeline of bacterial and archaeal diversification in the oceanen
dc.title.serialeLifeen
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten
dc.type.otherresearch-articleen
dc.type.otherJournal Articleen
pubs.organisational-group/Virginia Techen
pubs.organisational-group/Virginia Tech/Scienceen
pubs.organisational-group/Virginia Tech/Science/Biological Sciencesen
pubs.organisational-group/Virginia Tech/Faculty of Health Sciencesen
pubs.organisational-group/Virginia Tech/All T&R Facultyen
pubs.organisational-group/Virginia Tech/Science/COS T&R Facultyen

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