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dc.contributor.authorMagnabosco, C.
dc.contributor.authorMoore, Kelsey Reed
dc.contributor.authorWolfe, Joanna Michelle
dc.contributor.authorFournier, Gregory P.
dc.date.accessioned2018-10-01T19:40:12Z
dc.date.available2018-10-01T19:40:12Z
dc.date.issued2018-03
dc.date.submitted2017-06
dc.identifier.issn1472-4677
dc.identifier.urihttp://hdl.handle.net/1721.1/118326
dc.description.abstractPhototrophic bacteria are among the most biogeochemically significant organisms on Earth and are physiologically related through the use of reaction centers to collect photons for energy metabolism. However, the major phototrophic lineages are not closely related to one another in bacterial phylogeny, and the origins of their respective photosynthetic machinery remain obscured by time and low sequence similarity. To better understand the co-evolution of Cyanobacteria and other ancient anoxygenic phototrophic lineages with respect to geologic time, we designed and implemented a variety of molecular clocks that use horizontal gene transfer (HGT) as additional, relative constraints. These HGT constraints improve the precision of phototroph divergence date estimates and indicate that stem green non-sulfur bacteria are likely the oldest phototrophic lineage. Concurrently, crown Cyanobacteria age estimates ranged from 2.2 Ga to 2.7 Ga, with stem Cyanobacteria diverging ~2.8 Ga. These estimates provide a several hundred Ma window for oxygenic photosynthesis to evolve prior to the Great Oxidation Event (GOE) ~2.3 Ga. In all models, crown green sulfur bacteria diversify after the loss of the banded iron formations from the sedimentary record (~1.8 Ga) and may indicate the expansion of the lineage into a new ecological niche following the GOE. Our date estimates also provide a timeline to investigate the temporal feasibility of different photosystem HGT events between phototrophic lineages. Using this approach, we infer that stem Cyanobacteria are unlikely to be the recipient of an HGT of photosystem I proteins from green sulfur bacteria but could still have been either the HGT donor or the recipient of photosystem II proteins with green non-sulfur bacteria, prior to the GOE. Together, these results indicate that HGT-constrained molecular clocks are useful tools for the evaluation of various geological and evolutionary hypotheses, using the evolutionary histories of both genes and organismal lineages.en_US
dc.description.sponsorshipSimons Foundation (339603)en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (Award EAR-1615426)en_US
dc.publisherWileyen_US
dc.relation.isversionofhttp://dx.doi.org/10.1111/gbi.12273en_US
dc.rightsCreative Commons Attribution 4.0 International Licenseen_US
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en_US
dc.sourceWileyen_US
dc.titleDating phototrophic microbial lineages with reticulate gene historiesen_US
dc.typeArticleen_US
dc.identifier.citationMagnabosco, C., et al. “Dating Phototrophic Microbial Lineages with Reticulate Gene Histories.” Geobiology, vol. 16, no. 2, Mar. 2018, pp. 179–89. © 2018 The Authors.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.mitauthorMoore, Kelsey Reed
dc.contributor.mitauthorWolfe, Joanna Michelle
dc.contributor.mitauthorFournier, Gregory P.
dc.relation.journalGeobiologyen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2018-09-26T15:39:54Z
dspace.orderedauthorsMagnabosco, C.; Moore, K. R.; Wolfe, J. M.; Fournier, G. P.en_US
dspace.embargo.termsNen_US
dc.identifier.orcidhttps://orcid.org/0000-0001-7332-4098
dc.identifier.orcidhttps://orcid.org/0000-0002-2941-2514
dc.identifier.orcidhttps://orcid.org/0000-0003-1605-5455
mit.licensePUBLISHER_CCen_US


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