Ordovician origin and subsequent diversification of the brown algae

dc.contributor.authorChoi, Seok-Wanen
dc.contributor.authorGraf, Louisen
dc.contributor.authorChoi, Ji Wonen
dc.contributor.authorJo, Jihoonen
dc.contributor.authorBoo, Ga Hunen
dc.contributor.authorKawai, Hiroshien
dc.contributor.authorChoi, Chang Geunen
dc.contributor.authorXiao, Shuhaien
dc.contributor.authorKnoll, Andrew H.en
dc.contributor.authorAndersen, Robert A.en
dc.contributor.authorYoon, Hwan Suen
dc.date.accessioned2024-02-13T19:58:46Zen
dc.date.available2024-02-13T19:58:46Zen
dc.date.issued2024-01-19en
dc.description.abstractBrown algae are the only group of heterokont protists exhibiting complex multicellularity. Since their origin, brown algae have adapted to various marine habitats, evolving diverse thallus morphologies and gamete types. However, the evolutionary processes behind these transitions remain unclear due to a lack of a robust phylogenetic framework and problems with time estimation. To address these issues, we employed plastid genome data from 138 species, including heterokont algae, red algae, and other red-derived algae. Based on a robust phylogeny and new interpretations of algal fossils, we estimated the geological times for brown algal origin and diversification. The results reveal that brown algae first evolved true multicellularity, with plasmodesmata and reproductive cell differentiation, during the late Ordovician Period (ca. 450 Ma), coinciding with a major diversification of marine fauna (the Great Ordovician Biodiversification Event) and a proliferation of multicellular green algae. Despite its early Paleozoic origin, the diversification of major orders within this brown algal clade accelerated only during the Mesozoic Era, coincident with both Pangea rifting and the diversification of other heterokont algae (e.g., diatoms), coccolithophores, and dinoflagellates, with their red algal-derived plastids. The transition from ancestral isogamy to oogamy was followed by three simultaneous reappearances of isogamy during the Cretaceous Period. These are concordant with a positive character correlation between parthenogenesis and isogamy. Our new brown algal timeline, combined with a knowledge of past environmental conditions, shed new light on brown algal diversification and the intertwined evolution of multicellularity and sexual reproduction.en
dc.description.versionPublished versionen
dc.format.mimetypeapplication/pdfen
dc.identifier.doihttps://doi.org/10.1016/j.cub.2023.12.069en
dc.identifier.eissn1879-0445en
dc.identifier.issn0960-9822en
dc.identifier.orcidXiao, Shuhai [0000-0003-4655-2663]en
dc.identifier.otherS0960-9822(23)01769-4 (PII)en
dc.identifier.pmid38262417en
dc.identifier.urihttps://hdl.handle.net/10919/117989en
dc.language.isoenen
dc.publisherElsevieren
dc.relation.urihttps://www.ncbi.nlm.nih.gov/pubmed/38262417en
dc.rightsCreative Commons Attribution-NonCommercial 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/en
dc.subjectBayesian time estimationen
dc.subjectMesozoic Eraen
dc.subjectOrdovician Perioden
dc.subjectbrown algal originen
dc.subjectcomplex multicellularityen
dc.subjectisogamyen
dc.subjectoogamyen
dc.subjectphylogeneticsen
dc.subjectplastid genomeen
dc.titleOrdovician origin and subsequent diversification of the brown algaeen
dc.title.serialCurrent Biologyen
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten
dc.type.otherJournal Articleen
dcterms.dateAccepted2023-12-20en
pubs.organisational-group/Virginia Techen
pubs.organisational-group/Virginia Tech/Scienceen
pubs.organisational-group/Virginia Tech/Science/Geosciencesen
pubs.organisational-group/Virginia Tech/All T&R Facultyen
pubs.organisational-group/Virginia Tech/Science/COS T&R Facultyen

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