Ordovician origin and subsequent diversification of the brown algae

Brown 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...

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Veröffentlicht in:Current biology 2024-02, Vol.34 (4), p.740-754.e4
Hauptverfasser: Choi, Seok-Wan, Graf, Louis, Choi, Ji Won, Jo, Jihoon, Boo, Ga Hun, Kawai, Hiroshi, Choi, Chang Geun, Xiao, Shuhai, Knoll, Andrew H., Andersen, Robert A., Yoon, Hwan Su
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container_end_page 754.e4
container_issue 4
container_start_page 740
container_title Current biology
container_volume 34
creator Choi, Seok-Wan
Graf, Louis
Choi, Ji Won
Jo, Jihoon
Boo, Ga Hun
Kawai, Hiroshi
Choi, Chang Geun
Xiao, Shuhai
Knoll, Andrew H.
Andersen, Robert A.
Yoon, Hwan Su
description Brown 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. •Brown algal phylogeny and evolutionary timeline were established with plastid genomes•Brown algae originated during the late Ordovician Period (ca. 450 Ma)•The major diversification of brown algae occurred during the Mesozoic Era•Isogamy reappearances correlate with gametic parthenogenesis Brown algae exhibit complex multicellularity and diverse gamete types; however, the timing and mechanisms of the evolution remain unclear. Choi et al. show that brown algae emerged with diversification of marine invertebrates during the Ordovician Period. Further diversification and transitions in gamete types occurred during the Mesozoic Era.
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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. 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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. 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subjects Bayesian time estimation
brown algal origin
complex multicellularity
isogamy
Mesozoic Era
oogamy
Ordovician Period
phylogenetics
plastid genome
title Ordovician origin and subsequent diversification of the brown algae
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