A Cambrian–Ordovician Terrestrialization of Arachnids

Understanding the temporal context of terrestrialization in chelicerates depends on whether terrestrial groups, the traditional Arachnida, have a single origin and whether or not horseshoe crabs are primitively or secondarily marine. Molecular dating on a phylogenomic tree that recovers arachnid mon...

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Main Authors: Jesus Lozano-Fernandez, Alastair R. Tanner, Mark N. Puttick, Jakob Vinther, Gregory D. Edgecombe, Davide Pisani
Format: Article
Language:English
Published: Frontiers Media S.A. 2020-03-01
Series:Frontiers in Genetics
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fgene.2020.00182/full
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author Jesus Lozano-Fernandez
Jesus Lozano-Fernandez
Alastair R. Tanner
Mark N. Puttick
Jakob Vinther
Jakob Vinther
Gregory D. Edgecombe
Davide Pisani
Davide Pisani
author_facet Jesus Lozano-Fernandez
Jesus Lozano-Fernandez
Alastair R. Tanner
Mark N. Puttick
Jakob Vinther
Jakob Vinther
Gregory D. Edgecombe
Davide Pisani
Davide Pisani
author_sort Jesus Lozano-Fernandez
collection DOAJ
description Understanding the temporal context of terrestrialization in chelicerates depends on whether terrestrial groups, the traditional Arachnida, have a single origin and whether or not horseshoe crabs are primitively or secondarily marine. Molecular dating on a phylogenomic tree that recovers arachnid monophyly, constrained by 27 rigorously vetted fossil calibrations, estimates that Arachnida originated during the Cambrian or Ordovician. After the common ancestor colonized the land, the main lineages appear to have rapidly radiated in the Cambrian–Ordovician boundary interval, coinciding with high rates of molecular evolution. The highest rates of arachnid diversification are detected between the Permian and Early Cretaceous. A pattern of ancient divergence estimates for terrestrial arthropod groups in the Cambrian while the oldest fossils are Silurian (seen in both myriapods and arachnids) is mirrored in the molecular and fossil records of land plants. We suggest the discrepancy between molecular and fossil evidence for terrestrialization is likely driven by the extreme sparseness of terrestrial sediments in the rock record before the late Silurian.
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spelling doaj.art-3d87eb49da5e4c839e9c90111886f6812022-12-21T20:30:36ZengFrontiers Media S.A.Frontiers in Genetics1664-80212020-03-011110.3389/fgene.2020.00182495961A Cambrian–Ordovician Terrestrialization of ArachnidsJesus Lozano-Fernandez0Jesus Lozano-Fernandez1Alastair R. Tanner2Mark N. Puttick3Jakob Vinther4Jakob Vinther5Gregory D. Edgecombe6Davide Pisani7Davide Pisani8School of Biological Sciences, University of Bristol, Bristol, United KingdomSchool of Earth Sciences, University of Bristol, Bristol, United KingdomSchool of Biological Sciences, University of Bristol, Bristol, United KingdomDepartment of Biology and Biochemistry, Milner Centre for Evolution, University of Bath, Bath, United KingdomSchool of Biological Sciences, University of Bristol, Bristol, United KingdomSchool of Earth Sciences, University of Bristol, Bristol, United KingdomDepartment of Earth Sciences, Natural History Museum, London, United KingdomSchool of Biological Sciences, University of Bristol, Bristol, United KingdomSchool of Earth Sciences, University of Bristol, Bristol, United KingdomUnderstanding the temporal context of terrestrialization in chelicerates depends on whether terrestrial groups, the traditional Arachnida, have a single origin and whether or not horseshoe crabs are primitively or secondarily marine. Molecular dating on a phylogenomic tree that recovers arachnid monophyly, constrained by 27 rigorously vetted fossil calibrations, estimates that Arachnida originated during the Cambrian or Ordovician. After the common ancestor colonized the land, the main lineages appear to have rapidly radiated in the Cambrian–Ordovician boundary interval, coinciding with high rates of molecular evolution. The highest rates of arachnid diversification are detected between the Permian and Early Cretaceous. A pattern of ancient divergence estimates for terrestrial arthropod groups in the Cambrian while the oldest fossils are Silurian (seen in both myriapods and arachnids) is mirrored in the molecular and fossil records of land plants. We suggest the discrepancy between molecular and fossil evidence for terrestrialization is likely driven by the extreme sparseness of terrestrial sediments in the rock record before the late Silurian.https://www.frontiersin.org/article/10.3389/fgene.2020.00182/fullArachnidaChelicerataterrestrializationCambrianmolecular clocksdiversification
spellingShingle Jesus Lozano-Fernandez
Jesus Lozano-Fernandez
Alastair R. Tanner
Mark N. Puttick
Jakob Vinther
Jakob Vinther
Gregory D. Edgecombe
Davide Pisani
Davide Pisani
A Cambrian–Ordovician Terrestrialization of Arachnids
Frontiers in Genetics
Arachnida
Chelicerata
terrestrialization
Cambrian
molecular clocks
diversification
title A Cambrian–Ordovician Terrestrialization of Arachnids
title_full A Cambrian–Ordovician Terrestrialization of Arachnids
title_fullStr A Cambrian–Ordovician Terrestrialization of Arachnids
title_full_unstemmed A Cambrian–Ordovician Terrestrialization of Arachnids
title_short A Cambrian–Ordovician Terrestrialization of Arachnids
title_sort cambrian ordovician terrestrialization of arachnids
topic Arachnida
Chelicerata
terrestrialization
Cambrian
molecular clocks
diversification
url https://www.frontiersin.org/article/10.3389/fgene.2020.00182/full
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