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Bottjer DJ. Analysis of ancient mass extinction recoveries in marine environments: generating strategies for managing outcomes of the current mass extinction. Natl Sci Rev 2024; 11:nwad240. [PMID: 38116096 PMCID: PMC10727839 DOI: 10.1093/nsr/nwad240] [Citation(s) in RCA: 1] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/27/2023] [Revised: 09/05/2023] [Accepted: 09/08/2023] [Indexed: 12/21/2023] Open
Affiliation(s)
- David J Bottjer
- Department of Earth Sciences, University of Southern California, USA
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Mongiardino Koch N, Thompson JR, Hiley AS, McCowin MF, Armstrong AF, Coppard SE, Aguilera F, Bronstein O, Kroh A, Mooi R, Rouse GW. Phylogenomic analyses of echinoid diversification prompt a re-evaluation of their fossil record. eLife 2022; 11:72460. [PMID: 35315317 PMCID: PMC8940180 DOI: 10.7554/elife.72460] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/24/2021] [Accepted: 03/03/2022] [Indexed: 12/25/2022] Open
Abstract
Echinoids are key components of modern marine ecosystems. Despite a remarkable fossil record, the emergence of their crown group is documented by few specimens of unclear affinities, rendering their early history uncertain. The origin of sand dollars, one of its most distinctive clades, is also unclear due to an unstable phylogenetic context. We employ 18 novel genomes and transcriptomes to build a phylogenomic dataset with a near-complete sampling of major lineages. With it, we revise the phylogeny and divergence times of echinoids, and place their history within the broader context of echinoderm evolution. We also introduce the concept of a chronospace - a multidimensional representation of node ages - and use it to explore methodological decisions involved in time calibrating phylogenies. We find the choice of clock model to have the strongest impact on divergence times, while the use of site-heterogeneous models and alternative node prior distributions show minimal effects. The choice of loci has an intermediate impact, affecting mostly deep Paleozoic nodes, for which clock-like genes recover dates more congruent with fossil evidence. Our results reveal that crown group echinoids originated in the Permian and diversified rapidly in the Triassic, despite the relative lack of fossil evidence for this early diversification. We also clarify the relationships between sand dollars and their close relatives and confidently date their origins to the Cretaceous, implying ghost ranges spanning approximately 50 million years, a remarkable discrepancy with their rich fossil record.
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Affiliation(s)
- Nicolás Mongiardino Koch
- Department of Earth & Planetary Sciences, Yale University, New Haven, United States.,Scripps Institution of Oceanography, University of California San Diego, La Jolla, United States
| | - Jeffrey R Thompson
- Department of Earth Sciences, Natural History Museum, London, United Kingdom.,University College London Center for Life's Origins and Evolution, London, United Kingdom
| | - Avery S Hiley
- Scripps Institution of Oceanography, University of California San Diego, La Jolla, United States
| | - Marina F McCowin
- Scripps Institution of Oceanography, University of California San Diego, La Jolla, United States
| | - A Frances Armstrong
- Department of Invertebrate Zoology and Geology, California Academy of Sciences, San Francisco, United States
| | - Simon E Coppard
- Bader International Study Centre, Queen's University, Herstmonceux Castle, East Sussex, United Kingdom
| | - Felipe Aguilera
- Departamento de Bioquímica y Biología Molecular, Facultad de Ciencias Biológicas, Universidad de Concepción, Concepción, Chile
| | - Omri Bronstein
- School of Zoology, Faculty of Life Sciences, Tel Aviv University, Tel Aviv, Israel.,Steinhardt Museum of Natural History, Tel-Aviv, Israel
| | - Andreas Kroh
- Department of Geology and Palaeontology, Natural History Museum Vienna, Vienna, Austria
| | - Rich Mooi
- Department of Invertebrate Zoology and Geology, California Academy of Sciences, San Francisco, United States
| | - Greg W Rouse
- Scripps Institution of Oceanography, University of California San Diego, La Jolla, United States
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Mongiardino Koch N, Thompson JR. A Total-Evidence Dated Phylogeny of Echinoidea Combining Phylogenomic and Paleontological Data. Syst Biol 2020; 70:421-439. [PMID: 32882040 DOI: 10.1093/sysbio/syaa069] [Citation(s) in RCA: 19] [Impact Index Per Article: 4.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/12/2020] [Revised: 08/14/2020] [Accepted: 08/23/2020] [Indexed: 12/13/2022] Open
Abstract
Phylogenomic and paleontological data constitute complementary resources for unraveling the phylogenetic relationships and divergence times of lineages, yet few studies have attempted to fully integrate them. Several unique properties of echinoids (sea urchins) make them especially useful for such synthesizing approaches, including a remarkable fossil record that can be incorporated into explicit phylogenetic hypotheses. We revisit the phylogeny of crown group Echinoidea using a total-evidence dating approach that combines the largest phylogenomic data set for the clade, a large-scale morphological matrix with a dense fossil sampling, and a novel compendium of tip and node age constraints. To this end, we develop a novel method for subsampling phylogenomic data sets that selects loci with high phylogenetic signal, low systematic biases, and enhanced clock-like behavior. Our results demonstrate that combining different data sources increases topological accuracy and helps resolve conflicts between molecular and morphological data. Notably, we present a new hypothesis for the origin of sand dollars, and restructure the relationships between stem and crown echinoids in a way that implies a long stretch of undiscovered evolutionary history of the crown group in the late Paleozoic. Our efforts help bridge the gap between phylogenomics and phylogenetic paleontology, providing a model example of the benefits of combining the two. [Echinoidea; fossils; paleontology; phylogenomics; time calibration; total evidence.].
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Affiliation(s)
| | - Jeffrey R Thompson
- Department of Genetics, Evolution and Environment, University College London, Darwin Building, Gower Street, London WC1E 6BT, UK
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Thompson JR, Posenato R, Bottjer DJ, Petsios E. Echinoids from the Tesero Member (Werfen Formation) of the Dolomites (Italy): implications for extinction and survival of echinoids in the aftermath of the end-Permian mass extinction. PeerJ 2019; 7:e7361. [PMID: 31531267 PMCID: PMC6718154 DOI: 10.7717/peerj.7361] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/17/2019] [Accepted: 06/27/2019] [Indexed: 12/02/2022] Open
Abstract
The end-Permian mass extinction (∼252 Ma) was responsible for high rates of extinction and evolutionary bottlenecks in a number of animal groups. Echinoids, or sea urchins, were no exception, and the Permian to Triassic represents one of the most significant intervals of time in their macroevolutionary history. The extinction event was responsible for significant turnover, with the Permian–Triassic representing the transition from stem group echinoid-dominated faunas in the Palaeozoic to Mesozoic faunas dominated by crown group echinoids. This turnover is well-known, however, the environmental and taxonomic distribution of echinoids during the latest Permian and Early Triassic is not. Here we report on an echinoid fauna from the Tesero Member, Werfen Formation (latest Permian to Early Triassic) of the Dolomites (northern Italy). The fauna is largely known from disarticulated ossicles, but consists of both stem group taxa, and a new species of crown group echinoid, Eotiaris teseroensis n. sp. That these stem group echinoids were present in the Tesero Member indicates that stem group echinoids did not go extinct in the Dolomites coincident with the onset of extinction, further supporting other recent work indicating that stem group echinoids survived the end-Permian extinction. Furthermore, the presence of Eotiaris across a number of differing palaeoenvironments in the Early Triassic may have had implications for the survival of cidaroid echinoids during the extinction event.
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Affiliation(s)
- Jeffrey R Thompson
- Department of Genetics, Evolution and Environment, University College London, University of London, London, United Kingdom.,Department of Earth Sciences, University of Southern California, Los Angeles, CA, United States of America.,Department of Geosciences, Baylor University, Waco, TX, United States of America
| | - Renato Posenato
- Dipartimento di Fisica e Scienze della Terra, Università di Ferrara, Ferrara, Italy
| | - David J Bottjer
- Department of Earth Sciences, University of Southern California, Los Angeles, CA, United States of America
| | - Elizabeth Petsios
- Department of Geosciences, Baylor University, Waco, TX, United States of America
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