Abstract
In the ongoing debates about eukaryogenesis—the series of evolutionary events leading to the emergence of the eukaryotic cell from prokaryotic ancestors—members of the Asgard archaea play a key part as the closest archaeal relatives of eukaryotes1. However, the nature and phylogenetic identity of the last common ancestor of Asgard archaea and eukaryotes remain unresolved2–4. Here we analyse distinct phylogenetic marker datasets of an expanded genomic sampling of Asgard archaea and evaluate competing evolutionary scenarios using state-of-the-art phylogenomic approaches. We find that eukaryotes are placed, with high confidence, as a well-nested clade within Asgard archaea and as a sister lineage to Hodarchaeales, a newly proposed order within Heimdallarchaeia. Using sophisticated gene tree and species tree reconciliation approaches, we show that analogous to the evolution of eukaryotic genomes, genome evolution in Asgard archaea involved significantly more gene duplication and fewer gene loss events compared with other archaea. Finally, we infer that the last common ancestor of Asgard archaea was probably a thermophilic chemolithotroph and that the lineage from which eukaryotes evolved adapted to mesophilic conditions and acquired the genetic potential to support a heterotrophic lifestyle. Our work provides key insights into the prokaryote-to-eukaryote transition and a platform for better understanding the emergence of cellular complexity in eukaryotic cells.
Original language | English |
---|---|
Pages (from-to) | 992-999 |
Number of pages | 8 |
Journal | Nature |
Volume | 618 |
Issue number | 7967 |
DOIs | |
Publication status | Published - 29 Jun 2023 |
Externally published | Yes |
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In: Nature, Vol. 618, No. 7967, 29.06.2023, p. 992-999.
Research output: Contribution to journal › Article › Research › peer-review
TY - JOUR
T1 - Inference and reconstruction of the heimdallarchaeial ancestry of eukaryotes
AU - Eme, Laura
AU - Tamarit, Daniel
AU - Caceres, Eva F.
AU - Stairs, Courtney W.
AU - De Anda, Valerie
AU - Schön, Max E.
AU - Seitz, Kiley W.
AU - Dombrowski, Nina
AU - Lewis, William H.
AU - Homa, Felix
AU - Saw, Jimmy H.
AU - Lombard, Jonathan
AU - Nunoura, Takuro
AU - Li, Wen Jun
AU - Hua, Zheng Shuang
AU - Chen, Lin Xing
AU - Banfield, Jillian F.
AU - John, Emily St
AU - Reysenbach, Anna Louise
AU - Stott, Matthew B.
AU - Schramm, Andreas
AU - Kjeldsen, Kasper U.
AU - Teske, Andreas P.
AU - Baker, Brett J.
AU - Ettema, Thijs J.G.
N1 - Funding Information: We thank S. Köstlbacher, L. Hederstedt, A. Spang and A. J. Roger for discussions; staff at the Uppsala Multidisciplinary Center for Advanced Computational Science (UPPMAX) at Uppsala University and the Swedish National Infrastructure for Computing (SNIC) at the PDC Center for High-Performance Computing for providing computational resources; staff at the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) for taking sediment samples from the Taketomi shallow submarine hydrothermal system; and the crew of the RV Roger Revelle for assisting with the sampling of the ABE and Mariner vent fields along the Eastern Lau Spreading Center during the RR1507 Expedition. The Ngāti Tahu–Ngāti Whaoa Runanga Trust is acknowledged as mana whenua of Radiata Pool and associated samples, and we thank them for their assistance in access and sampling of the Ngatamariki geothermal features. We thank the Kingdom of Tonga for access to the deep-sea hydrothermal vent sites along the ELSC. Sampling in the Eastern Lau Spreading Center and Guaymas Basin (Gulf of California) was supported by the US-National Science Foundation (NSF-OCE-1235432 to A.-L.R. and NSF-OCE-0647633 to A.P.T.). A subset of Guaymas sediments were sequenced by the US Department of Energy Joint Genome Institute, a DOE Office of Science User Facility under contract number DE-AC02-05CH11231 granted to N.D. We thank the captain and crew of RV Aurora for assistance during sampling at Aarhus Bay. Sampling at Aarhus Bay was supported by the VILLUM Experiment project “FISHing for the ancestors of the eukaryotic cell” (grant number 17621 to A.S. and K.U.K.). This work was supported by grants of the European Research Council (ERC Starting and Consolidator grants 310039 and 817834, respectively), the Swedish Research Council (VR grant 2015-04959), the Dutch Research Council (NWO-VICI grant VI.C.192.016), Marie Skłodowska-Curie ITN project SINGEK (H2020-MSCA-ITN-2015-675752) and the Wellcome Trust foundation (Collaborative award 203276/K/16/Z) awarded to T.J.G.E. L.E. was supported by a Marie Skłodowska-Curie IEF (grant 704263) and by funding from the European Research Council (ERC Starting grant 803151). T.N. was supported by JSPS KAKENHI JP19H05684 within JP19H05679. W.-J.L. was supported by the National Natural Science Foundation of China (grant number 91951205 and 92251302). D.T. was supported by the Swedish Research Council (International Postdoc grant 2018-06609). C.W.S. was supported by a Science for Life Laboratory postdoctoral fellowship (awarded to T.J.G.E.) and funding from the Swedish research council (Vetenskaprådet Starting grant 2020-05071 to C.W.S.). J.L. was supported by the Wenner-Gren Foundation (fellowship 2016-0072). J.H.S. was supported by a Marie Skłodowska-Curie IIF grant (331291). This work was also supported by the Moore-Simons Project on the Origin of the Eukaryotic Cell, Simons Foundation 73592LPI to T.J.G.E. and B.J.B. ( https://doi.org/10.46714/735925LPI ) and Simons Foundation 812811 to L.E. ( https://doi.org/10.46714/735923LPI ), and NSF Division of Biological Science SBS Biodiversity: Discovery and Analysis program (1753661) to B.J.B. This work made use of the Dutch national e-infrastructure with the support of the SURF Cooperative using grant no. EINF-2953. to T.E. Funding Information: We thank S. Köstlbacher, L. Hederstedt, A. Spang and A. J. Roger for discussions; staff at the Uppsala Multidisciplinary Center for Advanced Computational Science (UPPMAX) at Uppsala University and the Swedish National Infrastructure for Computing (SNIC) at the PDC Center for High-Performance Computing for providing computational resources; staff at the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) for taking sediment samples from the Taketomi shallow submarine hydrothermal system; and the crew of the RV Roger Revelle for assisting with the sampling of the ABE and Mariner vent fields along the Eastern Lau Spreading Center during the RR1507 Expedition. The Ngāti Tahu–Ngāti Whaoa Runanga Trust is acknowledged as mana whenua of Radiata Pool and associated samples, and we thank them for their assistance in access and sampling of the Ngatamariki geothermal features. We thank the Kingdom of Tonga for access to the deep-sea hydrothermal vent sites along the ELSC. Sampling in the Eastern Lau Spreading Center and Guaymas Basin (Gulf of California) was supported by the US-National Science Foundation (NSF-OCE-1235432 to A.-L.R. and NSF-OCE-0647633 to A.P.T.). A subset of Guaymas sediments were sequenced by the US Department of Energy Joint Genome Institute, a DOE Office of Science User Facility under contract number DE-AC02-05CH11231 granted to N.D. We thank the captain and crew of RV Aurora for assistance during sampling at Aarhus Bay. Sampling at Aarhus Bay was supported by the VILLUM Experiment project “FISHing for the ancestors of the eukaryotic cell” (grant number 17621 to A.S. and K.U.K.). This work was supported by grants of the European Research Council (ERC Starting and Consolidator grants 310039 and 817834, respectively), the Swedish Research Council (VR grant 2015-04959), the Dutch Research Council (NWO-VICI grant VI.C.192.016), Marie Skłodowska-Curie ITN project SINGEK (H2020-MSCA-ITN-2015-675752) and the Wellcome Trust foundation (Collaborative award 203276/K/16/Z) awarded to T.J.G.E. L.E. was supported by a Marie Skłodowska-Curie IEF (grant 704263) and by funding from the European Research Council (ERC Starting grant 803151). T.N. was supported by JSPS KAKENHI JP19H05684 within JP19H05679. W.-J.L. was supported by the National Natural Science Foundation of China (grant number 91951205 and 92251302). D.T. was supported by the Swedish Research Council (International Postdoc grant 2018-06609). C.W.S. was supported by a Science for Life Laboratory postdoctoral fellowship (awarded to T.J.G.E.) and funding from the Swedish research council (Vetenskaprådet Starting grant 2020-05071 to C.W.S.). J.L. was supported by the Wenner-Gren Foundation (fellowship 2016-0072). J.H.S. was supported by a Marie Skłodowska-Curie IIF grant (331291). This work was also supported by the Moore-Simons Project on the Origin of the Eukaryotic Cell, Simons Foundation 73592LPI to T.J.G.E. and B.J.B. (https://doi.org/10.46714/735925LPI) and Simons Foundation 812811 to L.E. (https://doi.org/10.46714/735923LPI), and NSF Division of Biological Science SBS Biodiversity: Discovery and Analysis program (1753661) to B.J.B. This work made use of the Dutch national e-infrastructure with the support of the SURF Cooperative using grant no. EINF-2953. to T.E. Publisher Copyright: © 2023, The Author(s).
PY - 2023/6/29
Y1 - 2023/6/29
N2 - In the ongoing debates about eukaryogenesis—the series of evolutionary events leading to the emergence of the eukaryotic cell from prokaryotic ancestors—members of the Asgard archaea play a key part as the closest archaeal relatives of eukaryotes1. However, the nature and phylogenetic identity of the last common ancestor of Asgard archaea and eukaryotes remain unresolved2–4. Here we analyse distinct phylogenetic marker datasets of an expanded genomic sampling of Asgard archaea and evaluate competing evolutionary scenarios using state-of-the-art phylogenomic approaches. We find that eukaryotes are placed, with high confidence, as a well-nested clade within Asgard archaea and as a sister lineage to Hodarchaeales, a newly proposed order within Heimdallarchaeia. Using sophisticated gene tree and species tree reconciliation approaches, we show that analogous to the evolution of eukaryotic genomes, genome evolution in Asgard archaea involved significantly more gene duplication and fewer gene loss events compared with other archaea. Finally, we infer that the last common ancestor of Asgard archaea was probably a thermophilic chemolithotroph and that the lineage from which eukaryotes evolved adapted to mesophilic conditions and acquired the genetic potential to support a heterotrophic lifestyle. Our work provides key insights into the prokaryote-to-eukaryote transition and a platform for better understanding the emergence of cellular complexity in eukaryotic cells.
AB - In the ongoing debates about eukaryogenesis—the series of evolutionary events leading to the emergence of the eukaryotic cell from prokaryotic ancestors—members of the Asgard archaea play a key part as the closest archaeal relatives of eukaryotes1. However, the nature and phylogenetic identity of the last common ancestor of Asgard archaea and eukaryotes remain unresolved2–4. Here we analyse distinct phylogenetic marker datasets of an expanded genomic sampling of Asgard archaea and evaluate competing evolutionary scenarios using state-of-the-art phylogenomic approaches. We find that eukaryotes are placed, with high confidence, as a well-nested clade within Asgard archaea and as a sister lineage to Hodarchaeales, a newly proposed order within Heimdallarchaeia. Using sophisticated gene tree and species tree reconciliation approaches, we show that analogous to the evolution of eukaryotic genomes, genome evolution in Asgard archaea involved significantly more gene duplication and fewer gene loss events compared with other archaea. Finally, we infer that the last common ancestor of Asgard archaea was probably a thermophilic chemolithotroph and that the lineage from which eukaryotes evolved adapted to mesophilic conditions and acquired the genetic potential to support a heterotrophic lifestyle. Our work provides key insights into the prokaryote-to-eukaryote transition and a platform for better understanding the emergence of cellular complexity in eukaryotic cells.
UR - http://www.scopus.com/inward/record.url?scp=85161898060&partnerID=8YFLogxK
U2 - 10.1038/s41586-023-06186-2
DO - 10.1038/s41586-023-06186-2
M3 - Article
C2 - 37316666
AN - SCOPUS:85161898060
SN - 0028-0836
VL - 618
SP - 992
EP - 999
JO - Nature
JF - Nature
IS - 7967
ER -