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New lower Permian nonmarine arthropod trace fossils from New Mexico and South Africa

Published online by Cambridge University Press:  14 July 2015

Simon J. Braddy  and
Derek E. G. Briggs
Simon J. Braddy
Affiliation:
Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdom.
Derek E. G. Briggs
Affiliation:
Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen's Road, Bristol, BS8 1RJ, United Kingdom.
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Abstract

The Lower Permian (Late Wolfcampian) marginal marine facies of the Robledo Mountains Member (Hueco Formation) of the Robledo Mountains, New Mexico, contains a diverse ichnofauna dominated by vertebrate trackways. Four new arthropod ichnotaxa are described. Tonganoxichnus robledoensis new ichnospecies, consists of repeated small traces comprising imprints of anteriorly directed legs, an elongate tapering abdomen, and a thin tail. Hedriumichnus apacheensis new ichnogenus and ichnospecies consists of isolated small traces comprising imprints of laterally-directed legs, a broad tapering abdomen, and a short tail. Rotterodichnium major new ichnospecies is a large trace with imprints of the head and thorax, a long thin abdomen and three pairs of legs, increasing in length posteriorly. Quadrispinichna parvia new ichnogenus and ichnospecies consists of four diverging or sub-parallel linear or curvilinear imprints of approximately equal length.

Tonganoxichnus, previously known from the Upper Carboniferous of eastern Kansas, is interpreted as produced by a jumping monuran (an extinct group of wingless insects). Hedriumichnus, known only from the Robledo Mountains, is interpreted as the resting trace of a nymph of a primitive Ephemeroptera or Plecoptera. Rotterodichnium, previously known from the Lower Permian of Germany, is interpreted as the resting trace of a large dragonfly-like form (Protodonata, Odonata, or Megasecoptera). Quadrispinichna, previously recorded but not named, from the Lower Permian Ecca succession of South Africa, is interpreted as a resting trace of a crustacean. These rare traces increase our understanding of the diversity and behavior of nonmarine arthropod communities in the Lower Permian.

Type
Research Article
Information
Journal of Paleontology , Volume 76 , Issue 3 , May 2002 , pp. 546 - 557
Copyright
Copyright © The Paleontological Society

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References

Abel, O. 1935. Vorzeitliche Lebensspuren. Gustav Fischer, Jena, 644 p.Google Scholar
Anderson, A. M. 1974. Arthropod trackways and other trace fossils from the Early Permian Lower Karroo Beds of South Africa. Unpublished Ph.D. dissertation, University of Witwatersrand, 172 p.Google Scholar
Anderson, A. M. 1981. The Umfolozia arthropod trackways in the Permian Dwyka and Ecca Series of South Africa. Journal of Paleontology, 55:84–108.Google Scholar
Anderson, L. I. 1996. Taphonomy and taxonomy of the Palaeozoic Xiphosura. Unpublished Ph.D. dissertation, University of Manchester, 413 p.Google Scholar
Braddy, S. J. 1995. A new arthropod trackway and associated invertebrate ichnofauna from the Lower Permian Hueco Formation of the Robledo Mountains, southern New Mexico. New Mexico Museum of Natural History and Science Bulletin, 6:101–105.Google Scholar
Braddy, S. J. 1998. An overview of the invertebrate ichnotaxa from the Robledo Mountains ichnofauna (Lower Permian), southern New Mexico. New Mexico Museum of Natural History and Science Bulletin, 12:93–98.Google Scholar
Braddy, S. J. 1999. Terrestrial trace fossils from the Robledo Mountains Ichnofauna (Lower Permian) of southern New Mexico. Geoscientist, 9(7):5–6.Google Scholar
Braddy, S. J., Morrissey, L. B., and Yates, A. In review. Amphibian traces from the Lower Permian of southern New Mexico. Palaeontology.Google Scholar
Chamberlain, C. K. 1975. Recent Lebensspuren in nonmarine aquatic environments, p. 431–458. In Frey, R. W. (ed.), The Study of Trace Fossils. Springer Verlag, New York.CrossRefGoogle Scholar
Debriette, P., and Gand, G. 1990. Conséquences stratigraphiques et paléoenvironnementales de nouvelles observations paléontologiques dans le Permien de la partie occidentale du bassin de Lodève (sud du Massif central). Géologie de la France, 1:19–34.Google Scholar
Devera, J. A. 1989. Ichnofossil assemblages and associated lithofacies of the Lower Pennsylvanian (Caseyville and Tradewater Formations), southern Illinois, p. 57–83. In Cobb, J. C. (coord.), Geology of the Lower Pennsylvanian in Kentucky, Indiana, and Illinois. Illinois Basin Studies, 1.Google Scholar
Evans, M. E. G. 1975. The jump of Petrobius (Thysanura: Machilidae). Journal of Zoology, London, 176:49–65.CrossRefGoogle Scholar
Fürsich, F. T. 1974. Ichnogenus Rhizocorallium . Paläontologische Zeitschrift, 48:16–28.CrossRefGoogle Scholar
Gand, G. 1994. Ichnocoenoses à Isopodichnus furcosus nov. ichnosp. dans le Permien du Bassin de Lodève (Massif Central, France). Geobios, 27:73–86.CrossRefGoogle Scholar
Guerra-Sommer, M., Mendez-Piccoli, A. E., and Dias-Fabricio, M. E. 1984. Ichnofosseis em varvitos do Grupo Itararé, Permiano Inferio, Bacia do Paraná, RS, Brasil. Memoria III Congreso Latinoamericano de Paleontologia, 130–139.Google Scholar
Haubold, H., Hunt, A. P., Lucas, S. G., and Lockley, M. G. 1995. Wolfcampian (Early Permian) vertebrate tracks from Arizona and New Mexico. New Mexico Museum of Natural History and Science Bulletin, 6:135–165.Google Scholar
Haughton, S. H. 1919. A review of the reptilian fauna of the Karroo System of South Africa. Transactions of the Geological Society of South Africa, 22:1–25.Google Scholar
Haughton, S. H. 1925. Exhibit: tracks of animals preserved in the Ecca Shales of Cape Province. Transactions of the Royal Society of South Africa, 13:28–29.Google Scholar
Holub, V., and Kozur, H. 1981. Arthropodenfährten aus dem Rotliegenden der CSSR. Geologisch-Paläontologische Mitteilungen Innsbruck, 11:95–148.Google Scholar
Hunt, A. P., Lockley, M. G., Lucas, S. G., MacDonald, J. P., Hotton, N., and Kramer, J. 1993. Early Permian tracksites in the Robledo Mountains, south-central New Mexico. New Mexico Museum of Natural History and Science Bulletin, 2:23–31.Google Scholar
Jarzembowski, E. A., and Ross, A. J. 1996. Insect origination and extinction in the Phanerozoic. p. 65–78. In Hart, M. B. (ed.), Biotic Recovery from Mass Extinction Events. Geological Society Special Publication, 102.Google Scholar
Keighley, D. G., and Pickerill, R. K. 1998. Systematic ichnology of the Mabou and Cumberland groups (Carboniferous) of western Cape Breton Islands, eastern Canada, 2: surface markings. Atlantic Geology, 34:83–112.CrossRefGoogle Scholar
Kozur, H., and Lemone, D. V. 1995. New terrestrial arthropod trackways from the Abo Member (Sterlitamakian, Late Sakmarian, Late Wolfcampian) of the Shalem Colony Section, Robledo Mountains, New Mexico. New Mexico Museum of Natural History and Science Bulletin, 6:107–113.Google Scholar
Kukalová-Peck, J. 1987. New Carboniferous Diplura, Monura, and Thysanura, the hexapod ground plan, and the role of thoracic side lobes in the origin of wings (Insecta). Canadian Journal of Zoology, 65:2327–2345.CrossRefGoogle Scholar
Kukalová-Peck, J. 1994. Fossil history and the evolution of hexapod structures, p. 141–179. In Naumann, T. D. (ed.), Insects of Australia (second edition). CSIRO, Melbourne University Press, Melbourne.Google Scholar
Labandeira, C. C., and Sepkoski, J. J. Jr. 1993. Insect diversity in the fossil record. Science, 261:310–315.CrossRefGoogle ScholarPubMed
Lucas, S. G., Anderson, O. J., Heckert, A. B., and Hunt, A. P. 1995. Geology of Early Permian tracksites, Robledo Mountains, South-Central New Mexico. New Mexico Museum of Natural History and Science Bulletin, 6:13–32.Google Scholar
MacDonald, J. 1992. Footprints from the dawn of time. Science Probe, 2(3):32–47.Google Scholar
MacDonald, J. 1994. Earth's First Steps. Johnson Books, Boulder, Colorado, 190 p.Google Scholar
Mack, G. H., and James, W. C. 1986. Cyclic sedimentation in the mixed siliciclastic- carbonate Abo-Hueco transitional zone (Lower Permian), south-western New Mexico. Journal of Sedimentary Petrology, 56:635–647.Google Scholar
Mángano, M. G., Buatois, L. A., Maples, C. G., and Lanier, W. P. 1997. Tonganoxichnus, a new insect trace from the Upper Carboniferous of eastern Kansas. Lethaia, 30:113–125.CrossRefGoogle Scholar
Miller, M. F. 1982. Limulicubichnus: a new ichnogenus of limulid resting traces. Journal of Paleontology, 56:429–433.Google Scholar
Osgood, R. G. 1970. Trace fossils of the Cincinnati area. Palaeontographica Americana, 6(41):281–444.Google Scholar
Packard, A. S. 1886. On the Carboniferous xiphosurous fauna of North America. Memoirs of the National Academy of Sciences, 3:143–157.Google Scholar
Pollard, J. E. 1985. Isopodichnus, related arthropod trace fossils and notostracans from Triassic fluvial sediments. Transactions of the Royal Society of Edinburgh: Earth Sciences, 76:273–285.CrossRefGoogle Scholar
Romano, M., and Whyte, M. A. 1987. A limulid trace fossil from the Scarborough Formation (Jurassic) of Yorkshire: its occurrence, taxonomy and interpretation. Proceedings of the Yorkshire Geological Society, 46:85–95.CrossRefGoogle Scholar
Rowland, J. M. 1997. The late Paleozoic insect assemblage at Carrizo Arroyo, New Mexico. New Mexico Museum of Natural History and Science Bulletin, 11:1–7.Google Scholar
Savage, N. M. 1971. A varvite ichnocoenosis from the Dwyka Series of Natal. Lethaia, 4:217–233.CrossRefGoogle Scholar
Scott, A. C., and Taylor, T. N. 1983. Plant/animal interactions during the Upper Carboniferous. The Botanical Review, 49:259–307.CrossRefGoogle Scholar
Shear, W. A., and Kukalová-Peck, J. 1990. The ecology of Palaeozoic terrestrial arthropods: the fossil evidence. Canadian Journal of Zoology, 68:1807–1834.CrossRefGoogle Scholar
Theron, A. C. 1967. The sedimentology of the Koup Subgroup near Laingsburg. Unpublished M.Sc. dissertation, University of Stellenbosch, 25 p.Google Scholar
Trewin, N. H. 1994. A draft system for the identification and description of arthropod trackways. Palaeontology, 37:811–823.Google Scholar
Trewin, N. H., and McNamara, K. J. 1995. Arthropods invade the land: trace fossils and palaeoenvironments of the Tumblagooda Sandstone (?late Silurian) of Kalbarri, Western Australia. Transactions of the Royal Society of Edinburgh: Earth Sciences, 85:177–210.CrossRefGoogle Scholar
Walter, H. 1982. Zur Ichnologie der Oberen Hornburger Schichten des östlichen Harzvorlandes. Freiberger Forschungshefte C, 366:45–63.Google Scholar
Walter, H. 1983. Zur Taxonomie, ökologie und biostratigraphie der ichnia limnisch- terrestrischer arthropoden des mitteleuropäischen jung-paläozoikums. Freiberger Forschungshefte C, 382:146–193.Google Scholar
Whalley, P. E. S., and Jarzembowski, E. A. 1986. A new assessment of Rhyniella, the earliest known insect, from the Devonian of Rhynie, Scotland. Nature, 291:317.CrossRefGoogle Scholar