Carboniferous Onychophora from Montceau-les-Mines, France, and onychophoran terrestrialization
The geological age of the onychophoran crown-group, and when the group came onto land, have been sources of debate. Although stem-group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpr...
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| Published in | Invertebrate biology Vol. 135; no. 3; pp. 179 - 190 |
|---|---|
| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
United States
Blackwell Publishing Ltd
01.09.2016
Wiley Subscription Services, Inc John Wiley and Sons Inc |
| Subjects | |
| Online Access | Get full text |
| ISSN | 1077-8306 1744-7410 |
| DOI | 10.1111/ivb.12130 |
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| Abstract | The geological age of the onychophoran crown-group, and when the group came onto land, have been sources of debate. Although stem-group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpretations. A Late Carboniferous species from the Mazon Creek biota of the USA, Helenodora inopinata, originally interpreted as a crown-group onychophoran, has recently been allied to early Cambrian stem-group taxa. Here we describe a fossil species from the Late Carboniferous Montceau-les-Mines Lagerstätte, France, informally referred to as an onychophoran for more than 30 years. The onychophoran affinities of Antennipatus montceauensis gen. nov., sp. nov. are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem-group as a whole. Nevertheless, A. montceauensis is the most compelling candidate to date for a terrestrial Paleozoic onychophoran. |
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| AbstractList | The geological age of the onychophoran crown‐group, and when the group came onto land, have been sources of debate. Although stem‐group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpretations. A Late Carboniferous species from the Mazon Creek biota of the USA, Helenodora inopinata, originally interpreted as a crown‐group onychophoran, has recently been allied to early Cambrian stem‐group taxa. Here we describe a fossil species from the Late Carboniferous Montceau‐les‐Mines Lagerstätte, France, informally referred to as an onychophoran for more than 30 years. The onychophoran affinities of Antennipatus montceauensis gen. nov., sp. nov. are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem‐group as a whole. Nevertheless, A. montceauensis is the most compelling candidate to date for a terrestrial Paleozoic onychophoran. The geological age of the onychophoran crown‐group, and when the group came onto land, have been sources of debate. Although stem‐group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpretations. A Late Carboniferous species from the Mazon Creek biota of the USA , Helenodora inopinata , originally interpreted as a crown‐group onychophoran, has recently been allied to early Cambrian stem‐group taxa. Here we describe a fossil species from the Late Carboniferous Montceau‐les‐Mines Lagerstätte, France, informally referred to as an onychophoran for more than 30 years. The onychophoran affinities of Antennipatus montceauensis gen. nov., sp. nov. are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem‐group as a whole. Nevertheless, A. montceauensis is the most compelling candidate to date for a terrestrial Paleozoic onychophoran. The geological age of the onychophoran crown-group, and when the group came onto land, have been sources of debate. Although stem-group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpretations. A Late Carboniferous species from the Mazon Creek biota of the USA, , originally interpreted as a crown-group onychophoran, has recently been allied to early Cambrian stem-group taxa. Here we describe a fossil species from the Late Carboniferous Montceau-les-Mines Lagerstätte, France, informally referred to as an onychophoran for more than 30 years. The onychophoran affinities of gen. nov., sp. nov. are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem-group as a whole. Nevertheless, is the most compelling candidate to date for a terrestrial Paleozoic onychophoran. The geological age of the onychophoran crown-group, and when the group came onto land, have been sources of debate. Although stem-group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpretations. A Late Carboniferous species from the Mazon Creek biota of the USA,Helenodora inopinata, originally interpreted as a crown-group onychophoran, has recently been allied to early Cambrian stem-group taxa. Here we describe a fossil species from the Late Carboniferous Montceau-les-Mines Lagerstätte, France, informally referred to as an onychophoran for more than 30 years. The onychophoran affinities of Antennipatus montceauensis gen. nov., sp. nov. are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem-group as a whole. Nevertheless, A. montceauensis is the most compelling candidate to date for a terrestrial Paleozoic onychophoran. The geological age of the onychophoran crown-group, and when the group came onto land, have been sources of debate. Although stem-group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpretations. A Late Carboniferous species from the Mazon Creek biota of the USA, Helenodora inopinata, originally interpreted as a crown-group onychophoran, has recently been allied to early Cambrian stem-group taxa. Here we describe a fossil species from the Late Carboniferous Montceau-les-Mines Lagerstaette, France, informally referred to as an onychophoran for more than 30 years. The onychophoran affinities of Antennipatus montceauensis gen. nov., sp. nov. are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem-group as a whole. Nevertheless, A. montceauensis is the most compelling candidate to date for a terrestrial Paleozoic onychophoran. The geological age of the onychophoran crown-group, and when the group came onto land, have been sources of debate. Although stem-group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpretations. A Late Carboniferous species from the Mazon Creek biota of the USA, Helenodora inopinata, originally interpreted as a crown-group onychophoran, has recently been allied to early Cambrian stem-group taxa. Here we describe a fossil species from the Late Carboniferous Montceau-les-Mines Lagerstätte, France, informally referred to as an onychophoran for more than 30 years. The onychophoran affinities of Antennipatus montceauensis gen. nov., sp. nov. are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem-group as a whole. Nevertheless, A. montceauensis is the most compelling candidate to date for a terrestrial Paleozoic onychophoran.The geological age of the onychophoran crown-group, and when the group came onto land, have been sources of debate. Although stem-group Onychophora have been identified from as early as the Cambrian, the sparse record of terrestrial taxa from before the Cretaceous is subject to contradictory interpretations. A Late Carboniferous species from the Mazon Creek biota of the USA, Helenodora inopinata, originally interpreted as a crown-group onychophoran, has recently been allied to early Cambrian stem-group taxa. Here we describe a fossil species from the Late Carboniferous Montceau-les-Mines Lagerstätte, France, informally referred to as an onychophoran for more than 30 years. The onychophoran affinities of Antennipatus montceauensis gen. nov., sp. nov. are indicated by the form of the trunk plicae and the shape and spacing of their papillae, details of antennal annuli, and the presence of putative slime papillae. The poor preservation of several key systematic characters for extant Onychophora, however, prohibits the precise placement of the Carboniferous fossil in the stem or crown of the two extant families, or the onychophoran stem-group as a whole. Nevertheless, A. montceauensis is the most compelling candidate to date for a terrestrial Paleozoic onychophoran. |
| Author | Garwood, Russell J. Charbonnier, Sylvain Sotty, Daniel Edgecombe, Gregory D. Chabard, Dominique Giribet, Gonzalo |
| AuthorAffiliation | 2 Department of Earth Sciences The Natural History Museum London SW7 5BD UK 5 Museum of Comparative Zoology and Department of Organismic and Evolutionary Biology Harvard University Cambridge Massachusetts 02138 USA 3 Département Histoire de la Terre Muséum national d'Histoire naturelle, Paris F‐75005 Paris France 4 Muséum d'Histoire naturelle d'Autun F‐71400 Autun France 1 School of Earth, Atmospheric and Environmental Sciences The University of Manchester Manchester M13 9PL UK 6 Department of Life Sciences The Natural History Museum London SW7 5BD UK |
| AuthorAffiliation_xml | – name: 1 School of Earth, Atmospheric and Environmental Sciences The University of Manchester Manchester M13 9PL UK – name: 5 Museum of Comparative Zoology and Department of Organismic and Evolutionary Biology Harvard University Cambridge Massachusetts 02138 USA – name: 6 Department of Life Sciences The Natural History Museum London SW7 5BD UK – name: 4 Muséum d'Histoire naturelle d'Autun F‐71400 Autun France – name: 3 Département Histoire de la Terre Muséum national d'Histoire naturelle, Paris F‐75005 Paris France – name: 2 Department of Earth Sciences The Natural History Museum London SW7 5BD UK |
| Author_xml | – sequence: 1 givenname: Russell J. surname: Garwood fullname: Garwood, Russell J. email: russell.garwood@manchester.ac.uk, russell.garwood@manchester.ac.uk organization: School of Earth, Atmospheric and Environmental Sciences, The University of Manchester, M13 9PL, Manchester, UK – sequence: 2 givenname: Gregory D. surname: Edgecombe fullname: Edgecombe, Gregory D. organization: Department of Earth Sciences, The Natural History Museum, SW7 5BD, London, UK – sequence: 3 givenname: Sylvain surname: Charbonnier fullname: Charbonnier, Sylvain organization: Département Histoire de la Terre, Muséum national d'Histoire naturelle, Paris, F-75005, Paris, France – sequence: 4 givenname: Dominique surname: Chabard fullname: Chabard, Dominique organization: Muséum d'Histoire naturelle d'Autun, F-71400, Autun, France – sequence: 5 givenname: Daniel surname: Sotty fullname: Sotty, Daniel organization: Muséum d'Histoire naturelle d'Autun, F-71400, Autun, France – sequence: 6 givenname: Gonzalo surname: Giribet fullname: Giribet, Gonzalo organization: Museum of Comparative Zoology and Department of Organismic and Evolutionary Biology, Harvard University, 02138, Cambridge, Massachusetts, USA |
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| Keywords | velvet worms Ecdysozoa Antennipatus montceauensis gen. nov. sp. nov Carboniferous fossils Onychophora terrestrialization |
| Language | English |
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| Notes | ark:/67375/WNG-KZRF3X5V-N Appendix S1. A zip file containing 3D models of Antennipatus montceauensis gen. nov., sp. nov., in the VAXML interchange format. The file can be downloaded from Zenodo data archive (10.5281/zenodo.50828). This can be opened with the freely available software SPIERS (spiers-software.org). Video S1. A recording showing the hand specimens of Antennipatus montceauensis gen. nov., sp. nov., as well as static low lighting renders, and animated multicolor lighting rigs, to emphasize the surface relief of the specimens. EPSRC - No. EP/F007906/1; No. EP/F001452/1; No. EP/I02249X/1 istex:93423BB58E63237469E2740154F64D7DC5BD3113 ArticleID:IVB12130 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
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Oliveira IdS, Franke FA, Hering L, Schaffer S, Rowell DM, Weck-Haimann A, Monge-Nájera J, Morera-Brenes B, & Mayer G 2012a. Unexplored character diversity in Onychophora (velvet worms): a comparative study of three peripatid species. PLoS ONE 7: e51220. Oliveira IdS, Schaffer S, Kvartalnov PV, Galoyan EA, Plako IV, Weck-Heimann A, Geissler P, Ruhberg H, & Mayer G 2013. A new species of Eoperipatus (Onychophora) from Vietnam reveals novel morphological characters for the South-East Asian Peripatidae. Zool. Anz. 252: 495-510. Haug JT, Mayer G, Haug C, & Briggs DEG 2012. A Carboniferous non-onychophoran lobopodian reveals long-term survival of a Cambrian morphotype. Curr. Biol. 22: 1673-1675. Sutton MD, Rahman I, & Garwood R 2014. Techniques for Virtual Palaeontology. Wiley-Blackwell, Hoboken, New Jersey. Monge-Nájera J 1995. Phylogeny, biogeography and reproductive trends in the Onychophora. Zool. J. Linn. Soc. 114: 21-60. Morera-Brenes B & Monge-Nájera J 2010. A new giant species of placented worm and the mechanism by which onychophorans weave their nets (Onychophora: Peripatidae). Rev. Biol. Trop. 58: 1127-1142. Garwood RJ, Dunlop JA, Giribet G, & Sutton MD 2011. Anatomically modern Carboniferous harvestmen demonstrate early cladogenesis and stasis in Opiliones. Nat. Commun. 2: 444. Perrier V & Charbonnier S 2014. The Montceau-les-Mines Lagerstätte (Late Carboniferous, France). C.R. Palevol 13: 353-367. Ruhberg H 1985. Die Peripatopsidae (Onychophora). Systematik, Ökologie. Chorologie und phylogenetische Aspekte. Zoologica 137: 1-183. Concha A, Mellado P, Morera-Brenes B, Sampaio Costa C, Mahadevan L, & Monge-Nájera J 2015. Oscillation of the velvet worm slime jet by passive hydrodynamic instability. Nat. Commun. 6: 6292. Poinar G Jr 1996. Fossil velvet worms in Baltic and Dominican amber: onychophoran evolution and biogeography. Science 273: 1370-1371. Sutton MD, Garwood RJ, Siveter DJ, & Siveter DJ 2012. SPIERS and VAXML; A software toolkit for tomographic visualisation and a format for virtual specimen interchange. Palaeontol. Electron. 15(2): 5T. Selden PA 1996. First fossil mesothele spider, from the Carboniferous of France. Rev. Suisse Zool. hors série 585-596. Garwood RJ, Sharma PP, Dunlop JA, & Giribet G 2014. A Paleozoic stem group to mite harvestmen revealed through integration of phylogenetics and development. Curr. Biol. 24: 1017-1023. Oliveira IdS, Read VMSJ, & Mayer G 2012b. A world checklist of Onychophora (velvet worms), with notes on nomenclature and status of names. ZooKeys 211: 1-70. Rolfe WDI, Schram FR, Pacaud G, Sotty D, & Secretan S 1982. A remarkable Stephanian biota from Montceau-les-Mines, France. J. Paleontol. 56: 426-428. Smith MR & Ortega-Hernández J 2014. Hallucigenia's onychophoran-like claws and the case for Tactopoda. Nature 514: 363-366. Garwood RJ & Dunlop JA 2014. 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Autun 97: 37-43. 2012a; 7 1982; 56 2014; 514 2015; 6 2002; 3361 2011; 2 2010; 58 2007; 446 2010; 2493 2015; 523 2007; 1440 2000; 119 2015; 10 1997 1905; 2 1996 2014; 24 1994 1995; 114 2008; 99 1999; 1 2012; 15 2014; 133 2016; 16 2014; 88 1986; 1 2012; 3 2004; 18 2006; 49 2002; 45 2012b; 211 2015; 112 2004; 78 1980; 54 1994; 12 2008; 23 2014; 13 1985; 137 2016 2014 2014; 281 2013; 252 1996; 273 2012; 7 2012; 22 1981; 97 1988; 259 Langiaux J (e_1_2_7_19_1) 1994 e_1_2_7_5_1 Rolfe WDI (e_1_2_7_42_1) 1982; 56 e_1_2_7_9_1 e_1_2_7_15_1 e_1_2_7_13_1 e_1_2_7_11_1 Giribet G (e_1_2_7_14_1) 2016 e_1_2_7_45_1 e_1_2_7_47_1 Garwood RJ (e_1_2_7_10_1) 2012; 15 e_1_2_7_26_1 Brusca RC (e_1_2_7_4_1) 2016 e_1_2_7_28_1 Ruhberg H (e_1_2_7_43_1) 1985; 137 Selden PA (e_1_2_7_44_1) 1996 Bouvier E‐L (e_1_2_7_3_1) 1905; 2 Sutton MD (e_1_2_7_48_1) 2012; 15 e_1_2_7_25_1 e_1_2_7_31_1 e_1_2_7_33_1 e_1_2_7_21_1 e_1_2_7_35_1 e_1_2_7_37_1 e_1_2_7_39_1 e_1_2_7_6_1 Morera‐Brenes B (e_1_2_7_23_1) 2010; 58 Hay AA (e_1_2_7_17_1) 1997 e_1_2_7_18_1 e_1_2_7_16_1 e_1_2_7_40_1 e_1_2_7_2_1 e_1_2_7_12_1 e_1_2_7_46_1 Poplin C (e_1_2_7_38_1) 1994; 12 e_1_2_7_27_1 e_1_2_7_29_1 Thompson I (e_1_2_7_50_1) 1980; 54 Sutton MD (e_1_2_7_49_1) 2014 Pacaud G (e_1_2_7_32_1) 1981; 97 e_1_2_7_51_1 e_1_2_7_30_1 Dunlop JA (e_1_2_7_8_1) 1999; 1 e_1_2_7_24_1 e_1_2_7_22_1 e_1_2_7_34_1 e_1_2_7_20_1 e_1_2_7_36_1 Courel L (e_1_2_7_7_1) 1994 Racheboeuf PR (e_1_2_7_41_1) 2008; 99 |
| References_xml | – reference: Perrier V & Charbonnier S 2014. The Montceau-les-Mines Lagerstätte (Late Carboniferous, France). C.R. Palevol 13: 353-367. – reference: Garwood RJ & Sutton MD 2012. The enigmatic arthropod Camptophyllia. Palaeontol. Electron. 15(2): 15A. – reference: Poplin C & Heyler D, eds. 1994. Quand le massif central était sous l'Équateur-Un écosystème carbonifère à Montceau-les-Mines. Mém. Sect. Sci. 12: 328. – reference: Racheboeuf PR, Vannier J, & Anderson LI 2002. A new three-dimensionally preserved xiphosuran chelicerate from the Montceau-Les-Mines Lagerstätte (Carboniferous, France). Palaeontology 45: 125-147. – reference: Baird GC, Sroka SD, Shabica CW, & Kuecher GJ 1986. Taphonomy of Middle Pennsylvanian Mazon Creek area fossil localities, Northeast Illinois: significance of exceptional fossil preservation in syngenetic concretions. Palaios 1: 271-285. – reference: Morera-Brenes B & Monge-Nájera J 2010. 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| SubjectTerms | Antennipatus montceauensis gen. nov. sp. nov Biota Cambrian Cambrian period Carboniferous Carboniferous period Cretaceous Cretaceous period Ecdysozoa fossils France Mines new genus new species Onychophora Original Paleozoic streams Taxa terrestrialization United States velvet worms |
| Title | Carboniferous Onychophora from Montceau-les-Mines, France, and onychophoran terrestrialization |
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