Megapezia longipes Willard and Cleaves 1930 from the Pennsylvanian Rhode Island Formation of Massachusetts: ichnotaxonomic status.
Matthew (1903) established the ichnogenus Megapezia for tracks from the Mississippian Horton Group of Parrsboro, Nova Scotia, Canada. Later, Willard and Cleaves (1930) erected a new ichnospecies, Megapezia longipes, for a vertebrate trace that was found in the Pennsylvanian Rhode Island Formation of Plainville, Massachusetts, USA. These authors described and figured the fossil, which made the name available according to Article 12 of the International Code of Zoological Nomenclature (Ride et al. 1999); but the description did not include justification for assigning the fossil to Megapezia. Additionally, Willard and Cleaves (1930) provided a photograph of Megapezia longipes but no interpretive drawing, which makes the written description difficult to follow.
No additional specimens have been assigned to Megapezia longipes in the nearly 90 years since it was described, and thus the taxon is based entirely on the holotype. Haubold (1970, 1971) questioned the assignment of the species to Megapezia. To address Haubold's concern about the ichnogeneric status of Megapezia longipes, this paper presents the results of a reexamination of the holotype, including a more detailed description and interpretation, together with new photographs accompanied by interpretive line drawings. The evidence presented indicates that the specimen does not belong to Megapezia, but is better assigned, at least provisionally, to the ichnogenus Matthewichnus.
GEOLOGICAL AND PALEONTOLOGICAL CONTEXT
The fossil described by Willard and Cleaves (1930) was collected from rocks of the Rhode Island Formation, which is an approximately 3000 m thick sedimentary unit within the Narragansett Basin (Fig. 1). There are two hypotheses regarding the origin of the basin. Mosher (1983) proposed that it formed during sinistrai motion as Laurentia and Avalonia collided, whereas Wintsch and Sutter (1986) argued that the basin formed during late Paleozoic thrust faulting in south-central New England. Most researchers (e.g., Shaler et al. 1899; Towe 1959; Quinn and Oliver 1962; Skehan et al. 1979; Mosher 1983) consider the basin to be of Pennsylvanian age based on plant fossils, but radiometric dating of rhyolite near the base of the basin fill suggests that extension began in the Devonian (Maria and Hermes 2001; Thompson and Hermes 2003; Fig. 2).
Towe (1959) argued that the sedimentary rocks of the basin were formed in an alluvial fan system with meandering streams, floodplains, and swamps. Fossiliferous rocks near Plainville include fine-grained sandstone, siltstone, shale, and coal, and are considered low-energy interchannel, swamp, and floodplain deposits (Towe, 1959; S. Voigt, personal communication, 2010). The slab on which the tracks were preserved is composed of dark-grey shale and lacks desiccation cracks or any other indicator of subaerial exposure, which suggests that the sediment was deposited in an aquatic environment.
Narragansett Basin rocks were deformed and metamorphosed to differing degrees during the Alleghanian orogeny (Skehan et al. 1979; Mosher 1983; Murray et al. 2004; Hatcher 2010). The northern part of the basin, where Megapezia longipes was collected, experienced low grade, sub-greenschist-facies metamorphism, as evidenced by mineral assemblages and coal rank (Skehan et al. 1979; Murray et al. 2004; Connell 2006; Kirkwood 2006). Trace fossils collected in Plainville are visibly deformed (Willard and Cleaves 1930; Fichman et al. 2015).
The flora and fauna in Carboniferous strata around Plainville are quite diverse. Oleksyshyn (1976) reported a Westphalian C flora of 27 species from a quarry near where Megapezia longipes was found. Animal fossils from this quarry are restricted to traces. Invertebrate traces include Cochlichnus anguineus, Diplichnites cuithensis, Diplichnites gouldi, Diplopodichnus biformis, Gordia carickensis, Helminthoidichites tenuis, Lockeia isp., Planolites isp., Siskemia elegans, Stiallia pilosa, Stiaria intermedia, Tonganoxichnus buildexensis and Umfolozia sinuosa (Getty et al. 2013; personal observations). Vertebrates are represented by Undichna unisulca, Undichna isp., Batrachichnus plainvillensis, and Characichnos tridactylus, and Notalacerta missouriensis (Woodworth 1900; Fichman et al. 2015).
MATERIALS AND METHODS
The holotype of Megapezia longipes was originally housed at Brown University (Willard and Cleaves 1930), but it is now at the Museum of Comparative Zoology at Harvard University, where it bears specimen number MCZ 140. The specimen was examined and photographed for the present study under low-angle light. The photographs were imported into the public-domain image processing and analysis program ImageJ (Rasband 1997-2004) in order to obtain track measurements, including length, width and angle of divarication. Due to deformation, however, the track measurements reported herein are approximations of those of the original track.
Ichnogenus Matthewichnus Haubold 1970 type SPECIES: Matthewichnus velox Matthew 1905
DIAGNOSIS: Quadrupedal, plantigrade tetrapod trackway with tetradactyl manus and pentadactyl pes imprints. Manus is approximately as wide as long and is much smaller than pes. Manus digits II and III approximately equal in length and elongate, slightly more than half the length of the entire print. Digits I and IV of manus approximately one third the length of the entire print. Pes digits increase in length from I to IV, with digits III and V being approximately equal in length. (Modified from Haubold et al. 2005.).
REMARKS: Matthewichnus is similar in gross morphology to the ichnogenera Batrachichnus and Limnopus. Voigt and Lucas (2015), for example, noted that Matthewichnus caudifer is indistinguishable from Batrachichnus salamandroides based solely on the morphology of the tracks. Fillmore et al. (2012), however, noted that Matthewichnus can be differentiated from Batrachichnus and Limnopus by the much smaller manus track than pes track. Further morphological differences between Matthewichnus and Batrachichnus include the presence of elongate digits II and III on the manus and a more irregular placement of manus and pes imprints within the trackway (Kohl and Bryan 1994; Haubold et al. 2005; Fillmore et al. 2012; Voigt and Haubold 2015; Voigt and Lucas 2015).
cf. Matthewichnus longipes Willard and Cleaves 1930 comb. nov. (Figures 3-4) 1930 Megapezia longipes; Willard and Cleaves, p. 324, pi. 4, fig. 1. 1970 ? Megapezia longipes; Haubold, p. 94. 1971 ? Megapezia longipes; Haubold, p. 14. 1995 Megapezia longipes; Cotton et al., p. 201, fig. 8B, table 1. 2007 Megapezia; Lucas, p. 9.
MATERIAL: Holotype--MCZ 140, housed at the Museum of Comparative Zoology at Harvard University.
OCCURRENCE: Late Carboniferous (Pennsylvanian), Rhode Island Formation.
DESCRIPTION: Two tracks are preserved side by side in concave epirelief on the slab. They are separated by a nearly continuous area of rock at the same elevation as the rest of the slab. The track on the right is smaller, tetradactyl, and slightly longer than wide. It exhibits a long, rectangular imprint proximal to the digit imprints. The track measures 40 mm long (26 mm without the proximal rectangular imprint) by 22 mm wide. The digit imprints, which are counted from right to left, are in general straight, although the third digit exhibits a bend along its length. All have rounded distal terminations. Digits I and IV measure 5 mm long, or about one-fifth the length of the track. Digits II and III 10 mm and 12 mm, or 38-46% the length of the track. The total angle of divarication between the digits is 113[degrees], and the angles of divarication between the successive digits are as follows: I-II = 54[degrees], II-III = 33[degrees], and III-IV = 28[degrees]. The track exhibits a pronounced transverse wrinkling that is especially well developed in the region between the digits and the rectangular imprint.
The larger track, on the left, is pentadactyl and is nearly twice the length of the tetradactyl track. It measures 50 mm long by 20 mm wide. A broad, ovate imprint measuring 23 mm long by 18 mm wide is located proximal to the digit imprints, which are less well defined than those in the other track. Digit imprints are counted from right to left. Digits I and V are short, measuring approximately 5 and 4 mm long, respectively. Both appear as small, subtly rounded projections on the sides of the track. Imprints of digits II, III and IV are relatively long, measuring 11 mm, 15 mm, and 16 mm, respectively. The imprint of digit II is approximately straight, whereas those of digits III and IV curve and are concave to the left. All of the digits are of relatively uniform thickness and have rounded terminations. The total angle of divarication is 60[degrees]; the angles of divarication between the successive digits are as follows: I-II = 28[degrees]; II-III = 21[degrees]; III-IV = 10[degrees]; and IV-V= 9[degrees].
REMARKS: The two tracks on MCZ 140 are here interpreted as having been made by a manus and pes. The smaller, tetradactyl track is inferred to be that of the manus, whereas the larger pentadactyl track is that of the pes. The serial increase in length from right to left in the first four digits of the pes track indicates that it was made by a left foot. Considering the close proximity of the tracks, along with their similar orientation, it seems likely that they were made by the same animal as a manus-pes set. If that were true, then the tetradactyl track would be that of the left manus. It is possible, however, that the tracks were made by two different individuals traveling in the same direction. The tracks were probably made in wet mud, as is evidenced by the presence of the rectangular imprint (which was likely made by the antebrachium, or forearm) associated with that of the manus, the deep digit imprints of the manus, and the poorly defined and strongly curved digits of the pes imprint. Similar tracks from Argentina have also been interpreted as being produced in saturated sediment (Melchor and Sarjeant 2004).
When Willard and Cleaves (1930) described Megapezia longipes, they interpreted the fossil to include only a single, pentadactyl imprint that they thought was made by the left hind foot. These authors clearly stated that they thought the manus imprint was lacking. Considering that the ichnogenus Megapezia was established for a trackway with tetradactyl pedal imprints (Matthew 1903), Willard and Cleaves' specimen should not have been assigned to Megapezia. The reinterpretation of the specimen here as being composed of both manus and pes imprints does nothing to change this assessment since the correctly identified pes is also pentadactyl.
Rather than Megapezia, the tracks on MCZ 140 are more similar in morphology to the ichnogenera Batrachichnus, Limnopus, and Matthewichnus, all of which have tetradactyl manus tracks and pentadactyl pes tracks (Marsh 1894; Woodworth 1900; Baird 1952; Haubold 1970; Kohl and Bryan 1994; Tucker and Smith 2004). Various features of the tracks, however, suggest that they are more appropriately assigned to Matthewichnus. For example, the manus track is much smaller than the pes track. Furthermore, digit impressions II and III of the manus are relatively long, although not as long as is often cited for Matthewichnus. Finally, as in some specimens of Matthewichnus (e.g., Voigt and Lucas 2015, fig. 2B), the pes imprint on MCZ 140 is situated anterolaterally to that of the manus. The poor definition of the tracks and the lack of a complete trackway, however, argue against a definitive ichnogeneric reassignment (Bertling et al. 2006). Consequently, the tracks on MCZ 140 are provisionally reassigned to Matthewichnus. The ichnospecies cf. Matthewichnus longipes is, however, not synonymized with any other ichnospecies within Matthewichnus pending the collection of additional material that can be compared with other species with in the ichnogenus.
Considering that MCZ 140 was until now the only specimen assigned to Megapezia from New England, the reassignment of the tracks to Matthewichnus, albeit tentatively, means that Megapezia is no longer recognized in this region (cf. Cotton et al. 1995; Lucas 2007). Furthermore, since Megapezia longipes was the only valid ichnospecies of Megapezia other than the type, the ichnogenus is now restricted to the type species, Megapezia pineoi, from the Mississippian of Nova Scotia.
Haubold (1970) reassigned Lull's (1920) species Dromopus?. woodworthi, also from the Narragansett Basin, to Matthewichnus. This reassignment would make MCZ 140 the second occurrence of Matthewichnus within the Narragansett Basin. Fillmore et al. (2012), however, were skeptical of including Dromopus? woodworthi in Matthewichnus. Unlike typical Matthewichnus tracks, which have rounded tips to the digit imprints (Voigt and Lucas 2015), Dromopus? woodworthi has distinctive toe-pad and claw imprints. Thus the inclusion of Dromopus? woodworthi in Matthewichnus is not accepted herein and MCZ 140 is considered the first tentative occurrence of Matthewichnus within the Narragansett Basin.
I thank Jessica Cundiff, Acting Collection Manager at the Museum of Comparative Zoology, for granting me permission to study MCZ 140 and other specimens in her care. I also thank Meredith Fichman, Richard Knecht, and Robert Sproule for assistance at the museum. Thanks are due to Andrew Bush for lending his camera for photography. Robert Sproule is also acknowledged for providing comments on early drafts of the manuscript. Reviews by Matt Stimson and Spencer Lucas, along with editorial comments by Rob Fensome, greatly improved the final draft.
Baird, D. 1952. Revision of the Pennsylvanian and Permian footprints Limnopus, Allopus, and Baropus. Journal of Paleontology, 26, pp. 832-840.
Bertling, M., Braddy, S.J., Bromley, R.G., Demathieu, G.R., Genise, J., Mikulas, R., Nielsen, J.K., Nielsen, S.S., Rindsberg, A.K., Schlirf, M., and Uchman, A. 2006. Names for trace fossils: a uniform approach. Lethaia, 39, pp. 265-286. http://dx.doi. org/10.1080/00241160600787890
Connell, E. 2006. Microstructural analysis of the Rhode Island Formation, Narragansett Basin, MA. Undergraduate Review (Bridgewater State University), 2, pp. 224-230.
Cotton, W.D. Hunt, A.P., and Cotton, J.E. 1995. Paleozoic vertebrate tracksites in eastern North America. In Early Permian footprints and facies. Edited by S.G. Lucas and A.B. Heckert. New Mexico Museum of Natural History and Science Bulletin 6, pp. 189-211.
Fichman, J.H., Crespi, J., Getty, P.R., and Bush, A.M. 2015. Retrodeformation of Carboniferous trace fossils from the Narragansett Basin, U.S.A., using raindrop imprints and bedding-cleavage intersection lineation as strain markers. Palaios, 30, pp. 574-588. http:// dx.doi.org/10.2110/palo.2014.092
Fillmore, D.L., Lucas, S.G., and Simpson, E.L. 2012. Ichnology of the Mississippian Mauch Chunk Formation, eastern Pennsylvania. New Mexico Museum of Natural History and Science Bulletin, 54, pp. 1-136.
Getty, P.R., Sproule, R, Wagner, D., and Bush, A.M. 2013. Variation in wingless insect trace fossils: insights from neoichnology and the Pennsylvanian of Massachusetts. Palaios, 28, pp. 243-258. http://dx.doi.org/10.2110/ palo.2012.pl2-108r
Hatcher, R.D. 2010. The Appalachian orogen: a brief summary. In From Rodinia to Pangea: the lithotectonic record of the Appalachian region. Geological Society of America, Memoir 206, pp. 1-19. http://dx.doi. org/10.1130/2010.1206(01)
Haubold, H. 1970. Versuch einer Revision der Amphibien-Fahrten des Karbon und Perm. Freiberger Forschungshafte, 260, pp. 83-117.
Haubold, H. 1971. Ichnia amphibiorum et reptiliorum fossilium. In Encyclopedia of Paleoherpetology, Gustav Fischer Verlag, Portland, USA, pp. 1-124.
Haubold, H., Allen, A., Atkinson, T.P., Buta, R.J., Lacefield, J.A., Minkin, S.C., and Relihan, B.A. 2005. Interpretation of the tetrapod footprints from the Early Pennsylvanian of Alabama. In Pennsylvanian footprints in the Black Warrior Basin of Alabama. Edited by R.J. Buta, A.K.Rindsberg, and D.C. Kopaska-Merkel. Alabama Paleontological Society Monograph 1, pp. 75-111.
Kirkwood, A. 2006. Microstructural analysis of a drill core from the Rhode Island Formation: upper 750 feet. Undergraduate Review (Bridgewater State University), 2, pp. 159-164.
Kohl, M.S. and Bryan, J.R. 1994. A new Middle Pennsylvanian (Westphalian) amphibian trackway from the Cross Mountain Formation, east Tennessee Cumberlands. Journal of Paleontology, 68, pp. 655-663.
Lucas, S.G. 2007. Tetrapod footprint biostratigraphy and biochronology. Ichnos, 14, pp. 5-38. http://dx.doi. org /10.1080/10420940601006792
Lull, R.S. 1920. An Upper Carboniferous footprint from Attleboro, Massachusetts. American Journal of Science, 50, pp. 234-236. http://dx.doi.org/10.2475/ajs. s4-50.297.234
Maria, A. and Hermes, O.D. 2001. Volcanic rocks in the Narragansett Basin, southeastern New England: petrology and significance to early basin formation. American Journal of Science, 301, pp. 286-312. http:// dx.doi.org/10.2475/ajs.301.3.286
Marsh, O.C. 1894. Footprints of vertebrates in the Coal-measures of Kansas. Geological Magazine, 8, pp. 337-339. http://dx.doi.org/10.1017/S0016756800184262
Matthew, G.F. 1903. New genera of batrachian footprints of the Carboniferous system in eastern Canada. Canadian Record of Science, 9, pp. 99-111.
Matthew, G.F. 1905. New species and a new genus of batrachian footprints of the Carboniferous system in eastern Canada. Transactions of the Royal Society of Canada, 10, pp. 77-122.
Melchor, R.N. and Sarjeant, W.A.S. 2004. Small amphibian and reptile footprints from the Permian Carapacha Basin, Argentina. Ichnos, 11, pp. 57-78. http://dx.doi. org/10.1080/10420940490428814
Mosher, S. 1983. Kinematic history of the Narragansett Basin, Massachusetts and Rhode Island: constraints on late Paleozoic plate reconstructions. Tectonics, 2, pp. 327-344. http://dx.doi.org/10.1029/TC002i004p00327
Murray, D.P., Skehan, J.W., and Raben, J. 2004. Tectonostratigraphic relationships and coalification trends in the Narragansett and Norfolk basins, New England. Journal of Geodynamics, 37, pp. 583-611. http://dx.doi.org/10.1016/j.jog.2004.02.006
Oleksyshyn, J. 1976. Fossil plants of Pennsylvanian age from northwestern Narragansett Basin. In Studies in New England Geology. Geological Society of America Memoir 146, pp. 143-179.
Quinn, A.W. and Oliver, W.A. Jr. 1962. Pennsylvanian rocks in New England. In Pennsylvanian System in the United States, a symposium. American Association of Petroleum Geologists, Tulsa, Oklahoma, pp. 60-73.
Rasband, W.S. 1997-2014. ImageJ: U.S. National Institutes of Health, Bethesda, Maryland, USA. URL <http:// imagej.nih.gov/ij/> March 2015.
Ride WDL, Cogger, HG, Dupuis C, Kraus, O, Minelli A, Thompson FC, Tubbs PK. 1999. International Code of Zoological Nomenclature Fourth Edition. The International Trust for Zoological Nomenclature: online http://iczn.org/iczn/index.jsp. (incorporating 2012 amendments).
Shaler, N.S., Woodworth, J.B., and Foerste, A.F. 1899. Geology of the Narragansett Basin. Government Printing Office, Washington, D.C., 402 p. http://dx.doi. org/10.5962/bhl.title.66965
Skehan, J.W., Murray, D.P., Hepburn, J.C., Billings, M.P., Lyons, P.C., and Doyle, R.G. 1979. The Mississippian and Pennsylvanian (Carboniferous) systems in the United States-Massachusetts, Rhode Island, and Maine. U.S. Geological Survey Professional Paper, 1110, pp. A1-A30.
Thompson, M.D. and Hermes, O.D. 2003. Early rifting in the Narragansett Basin, Massachusetts-Rhode Island: evidence from Late Devonian bimodal volcanic rocks. The Journal of Geology, 111, pp. 597-604. http://dx.doi. org/10.1086/376768
Towe, K.M. 1959. Petrology and source of sediments in the Narragansett Basin of Rhode Island and Massachusetts. Journal of Sedimentary Petrology, 29, pp. 503-512.
Tucker, L. and Smith, M.P. 2004. A multivariate taxonomic analysis of the Late Carboniferous vertebrate ichnofauna of Alveley, southern Shropshire, England. Palaeontology, 47, pp. 679-710. http://dx.doi. org/10.111 l/j.0031 -0239.2004.00377.x
Voigt, S. and Haubold, H. 2015. Permian tetrapod footprints from the Spanish Pyrenees. Palaeogeography, Palaeoclimatology, Palaeoecology, 417, pp. 112-120. http://dx.doi.org/10.1016/j.palaeo.2014.10.038
Voigt, S. and Lucas, S.G. 2015. Permian tetrapod ichnodiversity of the Prehistoric Trackways National Monument (south-central New Mexico, U.S.A.). In Carboniferous-Permian transition in the Robledo Mountains, southern New Mexico. Edited by S.G. Lucas and W.A. DiMichele. New Mexico Museum of Natural History and Science Bulletin 65, pp. 153-167.
Walker, J.D. Geissman, J.W., Bowring, S.A., and Babcock, L.E. 2012, compilers, GSA Geologic Time Scale, v. 4.0: The Geological Society of America. http://www. geosociety.org/science/timescale/timescl.pdf.
Willard, B. and Cleaves, A.B. 1930. Amphibian footprints from the Pennsylvanian of the Narragansett Basin. Bulletin of the Geological Society of America, 41, pp. 321-327. http://dx.doi.org/10.1130/GSAB-41-321
Wintsch, R.P. and Sutter, J.F. 1986. A tectonic model for the late Paleozoic of southeastern New England. The Journal of Geology, 94, pp. 459-472. http://dx.doi. org/10.1086/629051
Woodworth, J.B. 1900. Vertebrate footprints on Carboniferous shales of Plainville, Massachusetts. Bulletin of the Geological Society of America, 11, pp. 449-454. http://dx.doi.org/10.1130/GSAB-11-449
PATRICK R. GETTY
Center for Integrative Geosciences, University of Connecticut, 354 Mansfield Road, Storrs Connecticut 06269, USA
Corresponding author <firstname.lastname@example.org>
Date received: 05 January 2016 [paragraph] Date accepted: 23 February 2016
Please note: Some tables or figures were omitted from this article.
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