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Vertebrate trackways among a stand of Supaia White plants on an early Permian floodplain, New Mexico

Published online by Cambridge University Press:  20 May 2016

William A. DiMichele
Affiliation:
Department of Paleobiology, NMNH Smithsonian Institution, Washington, DC 20560, USA,
Spencer G. Lucas
Affiliation:
New Mexico Museum of Natural History and Science, Albuquerque, NM 87104, USA,
Karl Krainer
Affiliation:
Institute of Geology and Paleontology, University of Innsbruck, Innsbruck A-6020, Austria,

Abstract

Little is known about the habit and spatial distribution of Early Permian tropical vegetation, a sharp contrast with the Pennsylvanian from which many in-situ “T0” assemblages are known. Even less is known about the potential interaction of plants and vertebrates. Here we report the discovery of a small stand of 34 probable Supaia White plants from the Abo Formation of New Mexico. The plants were growing on a mudflat, subject to periodic flooding and exposure. The same mudflat hosts trackways of vertebrates that appear to have walked around or between the Supaia plants. The stems are preserved as molds, and vary from 20 mm to 70 mm in diameter, averaging 42.4 mm, indicating heights of approximately 2.5–4 m. The plants, which may be described as small trees given their estimated height, are as close as 110 mm to their nearest neighbor and average nearly 300 mm apart. A series of lines or filled fissures, which we interpret as roots, radiates from the base of each stem. Leaves of Supaia thinfeldioides White are the only foliage found in association with these stems, on bedding planes above and at the base of the lowest expression of the stem molds. Associated vertebrate trackways either congregate around some of the stems or wend their way between the stems and include those of a single large temnospondyl amphibian (Limnopus Marsh) and many of small predatory parareptiles (Dromopus Marsh). This study demonstrates that S. thinfeldiodes were small-statured, weedy, opportunistic plants. It also shows that contemporaneous vertebrates prowled such environments, presumably either for food, shelter, or both given detectable pace and path.

Type
Research Article
Copyright
Copyright © The Paleontological Society 

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References

Baird, D. 1965. Footprints from the Cutler Formation. U. S. Geological Survey Professional Paper, 503C:C47C50.Google Scholar
Booi, M., van Waveren, I. M., and van Konijnenburg-van Cittert, J. H. A. 2009. Comia and Rhachiphyllum from the Early Permian of Sumatra, Indonesia. Review of Palaeobotany and Palynology, 156:418435.Google Scholar
Buatois, L. A. and Mángano, M. G. 2007. Invertebrate ichnology of continental freshwater environments, p. 285323. InMiller, W. III(ed.), Trace Fossils: Concepts, Problems, Prospects. Elsevier, Amsterdam.CrossRefGoogle Scholar
Buatois, L. A., Mángano, M. G., Genise, J. F., and Taylor, T. N. 1998. The ichnological record of the continental invertebrate invasion: evolutionary trends in environmental expansion, ecospace utilization, and behavioral complexity. Palaios, 13:217240.CrossRefGoogle Scholar
Carpenter, K. 1992. Behavior of hadrosaurs as interpreted from footprints in the “Mesaverde” Group (Campanian) of Colorado, Utah, and Wyoming. Rocky Mountain Geology, 29:8196.Google Scholar
Deng, S.-H., Wan, C.-B., and Yang, J.-G. 2009. Discovery of a Late Permian Angara-Cathaysia mixed flora from Acheng of Heilongjiang, China, with discussions on the closure of the Paleoasian Ocean. Science in China Series D, Earth Sciences, 52:17461755.CrossRefGoogle Scholar
DiMichele, W. A. and Falcon-Lang, H. J. 2011. Pennsylvanian ‘fossil forests’ in growth position (T0 assemblages): origin, taphonomic bias and palaeoecological insights. Journal of the Geological Society, 168:585605.Google Scholar
DiMichele, W. A., Kerp, H., Krings, M., and Chaney, D. S. 2005. The Permian peltasperm radiation: evidence from the southwestern United States. New Mexico Museum of Natural History and Science Bulletin, 30:6779.Google Scholar
DiMichele, W. A., Chaney, D. S., Nelson, W. J., Lucas, S. G., Looy, C. V., Quick, K., and Wang, J. 2007. A low diversity, seasonal tropical landscape dominated by conifers and peltasperms: Early Permian Abo Formation, New Mexico. Review of Palaeobotany and Palynology, 145:249273.Google Scholar
DiMichele, W. A., Nelson, W. J., Elrick, S., and Ames, P. R. 2009. Catastrophically buried Middle Pennsylvanian Sigillaria and calamitean sphenopsids from Indiana, U.S.A.: what kind of vegetation was this? Palaios, 24:159166.Google Scholar
Eberth, D. A. and Miall, A. D. 1991. Stratigraphy, sedimentology and evolution of a vertebrate-bearing, braided to anastomosed fluvial system, Cutler Formation (Permian–Pennsylvanian), north-central New Mexico. Sedimentary Geology, 72:225252.CrossRefGoogle Scholar
Falcon-Lang, H. J. 2009. A Macroneuropteris scheuchzeri tree preserved in growth position in the Middle Pennsylvanian Sydney Mines Formation, Nova Scotia, Canada. Atlantic Geology, 45:7480.Google Scholar
Falcon-Lang, H. J., Jud, N. A., Nelson, W. J., DiMichele, W. A., Chaney, D. S., and Lucas, S. G. 2011. Pennsylvanian coniferopsid forests in sabkha facies reveal the nature of seasonal tropical biome. Geology, 39:371374.Google Scholar
Galtier, J. and Broutin, J. 2008. Floras from red beds of the Permian Basin of Lodève (Southern France). Journal of Iberian Geology, 34:5772.Google Scholar
Gand, G., Kerp, H., Parsons, C., and Martínez-García, E. 1997. Palaeoenvironmental and stratigraphic aspects of animal traces and plant remains in Spanish Permian red beds (Peña Sagra, Cantabrian Mountains, Spain). Geobios, 30:295318.Google Scholar
Gastaldo, R. A., Stevanovic-Walls, I. M., and Ware, W. N. 2004. Erect forests are evidence for coseismic base-level changes in Pennsylvanian cyclothems of the Black Warrior Basin, U.S.A., p. 219238. InPashin, J. C. and Gastaldo, R. A.(eds.), Sequence Stratigraphy, Paleoclimate, and Tectonics of Coal-Bearing Strata. A.A.P.G. Studies in Geology, 51.Google Scholar
Haubold, H. 1971. Ichnia Amphibiorum et Reptiliorum fossilium. Encyclopedia of Paleoherpetology, 18:1124.Google Scholar
Haubold, H. 1984. Saurierfährten. Neue Brehm-Bucherei, 231 p.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, 6:135165.Google Scholar
Hunt, A. 1983. Plant fossils and lithostratigraphy of the Abo Formation (lower Permian) in the Socorro area and plant biostratigraphy of Abo red beds in New Mexico. New Mexico Geological Society Guidebook, 34th Field Conference, Socorro Region II, 157163.Google Scholar
Hunt, A. P. and Lucas, S. G. 2006. Permian tetrapod ichnofacies. Geological Society of London, Special Publication, 265:137156.Google Scholar
Hunt, A. P., Lucas, S. G., Haubold, H., and Lockley, M. G. 1995. Early Permian (late Wolfcampian) tetrapod tracks from the Robledo Mountains, south-central New Mexico. New Mexico Museum of Natural History and Science Bulletin, 6:167180.Google Scholar
Johnson, K. R. 2007. Palaeobotany: forests frozen in time. Nature, 447:786787.Google Scholar
Krainer, K. and Lucas, S. G. 2009. Cyclic sedimentation of the upper Carboniferous Bursum Formation, central New Mexico: tectonics versus glacioeustasy. New Mexico Geological Society Guidebook, 60:167182.Google Scholar
Krainer, K. and Lucas, S. G. 2010. Sedimentology of the Pennsylvanian–Permian Cutler Group and Lower Permian Abo Formation, Northern New Mexico, p. 2536. InLucas, S. G., Schneider, J. W., and Spielmann, J. A.(eds.), Carboniferous–Permian Transition in Cañon del Cobre, northern New Mexico. New Mexico Museum of Natural History and Science Bulletin, 49.Google Scholar
Kues, B. S. and Giles, K. A. 2004. The late Paleozoic ancestral Rocky Mountains system in New Mexico, p. 95136. InMack, G. H. and Giles, K. A.(eds.), The Geology of New Mexico: A Geologic History. New Mexico Geological Society Special Publication 11.Google Scholar
Lucas, S. G. and Krainer, K. 2004. The Red Tanks Member of the Bursum Formation in the Lucero uplift and regional stratigraphy of the Bursum Formation in New Mexico. New Mexico Museum of Natural History and Science Bulletin, 25:4352.Google Scholar
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, 6:1332.Google Scholar
Lucas, S. G., Heckert, A. B., Estep, J. W., and Cook, C. W. 1998. Stratigraphy of the Lower Permian Hueco Group in the Robledo Mountains, Doña Ana County, New Mexico. New Mexico Museum of Natural History and Science Bulletin, 12:4354.Google Scholar
Lucas, S. G., Krainer, K., and Colpitts, R. M. 2005a. Abo-Yeso (Lower Permian) stratigraphy in central New Mexico, p. 101115. InLucas, S. G., Zeigler, K. E., and Spielmann, J. A.(eds.), The Permian of Central New Mexico. New Mexico Museum of Natural History and Science Bulletin 31.Google Scholar
Lucas, S. G., Minter, N. J., Spielmann, J. A., Hunt, A. P., and Braddy, S. J. 2005b. Early Permian ichnofossil assemblage from the Fra Cristobal Mountains, southern New Mexico, p. 140150. InLucas, S. G., Zeigler, K. E., and Spielmann, J. A.(eds.), The Permian of Central New Mexico. New Mexico, Museum of Natural History and Science Bulletin 31.Google Scholar
Lucas, S. G., Minter, N. J., Spielmann, J. A., Smith, J. A., and Braddy, S. J. 2005c. Early Permian ichnofossils from the northern Caballo Mountains, Sierra County, New Mexico, p. 151162. InLucas, S. G., Zeigler, K. E., and Spielmann, J. A.(eds.), The Permian of Central New Mexico,. New Mexico, Museum of Natural History and Science Bulletin 31.Google Scholar
Lucas, S. G., Krainer, K., Corbitt, L., Dibenedetto, J., and Vachard, D. 2011. The Trans Mountain Road Member, a new stratigraphic unit of the Lower Permian Hueco Group, northern Franklin Mountains, Texas, p. 93109. InSullivan, R. M., Lucas, S. G., and Spielmann, J. A.(eds.), Fossil Record 3: New Mexico Museum of Natural History and Science Bulletin.Google Scholar
Macdonald, J. 1994. Earth's First Steps: Tracking Life Before the Dinosaurs. Johnson Books, Boulder, Colorado, 290 p.Google Scholar
Marsh, O. C. 1894. Footprints of vertebrates in the Coal Measures of Kansas. American Journal of Science, 3rd Series, 283:8184.Google Scholar
Miall, A. D. 1996. The Geology of Fluvial Deposits. Sedimentary Facies, Basin Analysis, and Petroleum Geology. Springer, Berlin, 582 p.Google Scholar
Minter, N. J. and Braddy, S. J. 2009. Ichnology of an Early Permian tidal flat: the Robledo Mountains Formation of the Robledo Mountains, Southern New Mexico, U.S.A. Special Papers in Palaeontology, 82:1107.Google Scholar
Naiman, R. J. and Décamps, H. 1997. The ecology of interfaces: riparian zones. Annual Review of Ecology and Systematics, 28:621658.Google Scholar
Niklas, K. J. and Spatz, H.-C. 2004. Growth and hydraulic (not mechanical) constraints govern the scaling of tree height and mass. Proceedings of the National Academy of Sciences of the United States of America, 101:1566115663.Google Scholar
Opluštil, S., Pšenička, J., Libertín, M., Bashforth, A. R., Šimůnek, Z., and Dašková, J. 2009. A Middle Pennsylvanian (Bolsovian) peat-forming forest preserved in situ in volcanic ash of the Whetstone Horizon in the Radnice Basin, Czech Republic. Review of Palaeobotany and Palynology, 155:234274.Google Scholar
Parker, L. R. and Balsley, J. K. 1989. Coal mines as localities for studying dinosaur trace fossils, p. 353360. InGillette, D. D. and Lockley, M. G.(eds.), Dinosaur Tracks and Traces, Cambridge University Press, Cambridge, U.K.Google Scholar
Pfefferkorn, H. W. and Wang, J. 2007. Early Permian coal-forming floras preserved as compressions from the Wuda District (Inner Mongolia, China). International Journal of Coal Geology, 69:90102.Google Scholar
Pfefferkorn, H. W., Gillespie, W. H., Resnick, D. A., and Scheihing, M. H. 1984. Reconstruction and architecture of medullosan pteridosperms (Pennsylvanian). The Mosasaur (Delaware Valley Paleontological Society), 2:18.Google Scholar
Pohlig, H. 1892. Altpermische Saurierfährten, Fische und Medusen der Gegend von Friedrichroda i. Thüringen, p. 5964. InAnonymous (ed.), Festschrift zum 70. Geburtstag von Rudolf Leuckardt, Engelmann, Leipzig, Germany.Google Scholar
Read, C. B. and Mamay, S. H. 1964. Upper Paleozoic floral zones and floral provinces of the United States. U.S. Geological Survey Professional Paper, 454K:135.Google Scholar
Stidd, B. M. 1981. The current status of medullosan seed ferns. Review of Palaeobotany and Palynology, 32:63101.Google Scholar
Voigt, S. and Haubold, H. 2000. Analyse zur Variabilität der Tetrapodenfährte Ichniotherium cottae aus dem Tambacher Sandstein (Rotliegend, U-Perm, Thüringen). Hallesches Jahrbuch Geowissenschat B, 22:1758.Google Scholar
Voigt, S., Berman, D. S., and Henrici, A. C. 2007. First well-established track-trackmaker association of Paleozoic tetrapods based on Ichniotherium trackways and diadectid skeletons from the lower Permian of Germany. Journal of Vertebrate Paleontology, 27:553570.Google Scholar
Wang, Z. Q. 1997. Permian Supaia fronds and an associated Autunia fructification from Shanxi, China. Palaeontology, 40:245277.Google Scholar
White, D. 1929. Flora of the Hermit Shale, Grand Canyon, Arizona. Carnegie Institution of Washington Bulletin, 405:1221.Google Scholar
Wing, S. L., Hickey, L. J., and Swisher, C. C. 1993. Implications of an exceptional fossil flora for Late Cretaceous vegetation. Nature, 363:342344.CrossRefGoogle Scholar