From the Late Cretaceous (Campanian) Kanguk Formation of Axel Heiberg Island, Nunavut, Canada, and Its Ecological and Geographical Implications MATTHEW J

Total Page:16

File Type:pdf, Size:1020Kb

From the Late Cretaceous (Campanian) Kanguk Formation of Axel Heiberg Island, Nunavut, Canada, and Its Ecological and Geographical Implications MATTHEW J ARCTIC VOL. 67, NO. 1 (MARCH 2014) P. 1 – 9 A Hadrosaurid (Dinosauria: Ornithischia) from the Late Cretaceous (Campanian) Kanguk Formation of Axel Heiberg Island, Nunavut, Canada, and Its Ecological and Geographical Implications MATTHEW J. VAVREK,1 LEN V. HILLS2 and PHILIP J. CURRIE3 (Received 1 October 2012; accepted in revised form 30 May 2013) ABSTRACT. A hadrosaurid vertebra was recovered during a palynological survey of the Upper Cretaceous Kanguk Formation in the eastern Canadian Arctic. This vertebra represents the farthest north record of any non-avian dinosaur to date. Although highly abraded, the fossil nonetheless represents an interesting biogeographic data point. During the Campanian, when this vertebra was deposited, the eastern Canadian Arctic was likely isolated both from western North America by the Western Interior Seaway and from more southern regions of eastern North America by the Hudson Seaway. This fossil suggests that large-bodied hadrosaurid dinosaurs may have inhabited a large polar insular landmass during the Late Cretaceous, where they would have lived year-round, unable to migrate to more southern regions during winters. It is possible that the resident herbivorous dinosaurs could have fed on non-deciduous conifers, as well as other woody twigs and stems, during the long, dark winter months when most deciduous plant species had lost their leaves. Key words: Appalachia, Arctic, Campanian, dinosaur, Laramidia, palaeobiogeography RÉSUMÉ. La vertèbre d’un hadrosauridé a été retrouvée pendant l’étude palynologique de la formation Kanguk remontant au Crétacé supérieur, dans l’est de l’Arctique canadien. Il s’agit de la vertèbre appartenant à un dinosaure non avien qui a été recueillie la plus au nord jusqu’à maintenant. Même si ce fossile est fortement abrasé, il n’en reste pas moins qu’il représente un point de donnée biogéographique intéressant. Pendant le Campanien, lorsque cette vertèbre a été déposée, l’est de l’Arctique canadien était vraisemblablement isolé de l’ouest de l’Amérique du Nord par la mer intérieure occidentale, et des régions plus au sud de l’est de l’Amérique du Nord par le bras de mer Hudson. Ce fossile suggère que de gros dinosaures hadrosauridés auraient pu habiter une grande masse terrestre insulaire polaire pendant le Crétacé tardif, où ils auraient évolué à l’année, étant incapables de migrer vers les régions plus au sud pendant l’hiver. Il est possible que les dinosaures herbivores résidents se soient nourris de conifères non décidus ainsi que d’autres tiges ou brindilles ligneuses pendant les longs mois sombres de l’hiver, lorsque la plupart des espèces végétales décidues avaient perdu leurs feuilles. Mots clés : Appalachia, Arctique, Campanien, dinosaure, Laramien, paléobiogéographie Traduit pour la revue Arctic par Nicole Giguère. INTRODUCTION et al., 2012), the Northwest Territories (Russell, 1984), and Nunavut (Russell, 1990; Núñez-Betelu et al., 2005). Addi- Since the first evidence of polar dinosaurs was discovered tional areas, such as northern Alberta (Currie et al., 2008; in Spitsbergen (Svalbard) in 1960 (de Lapparent, 1960, Fanti and Miyashita, 2009) and northern British Columbia 1962), Late Cretaceous dinosaurs have been found across (Rylaarsdam et al., 2006; Arbour and Graves, 2008), are not much of the Arctic (Rich et al., 2002; Weishampel et al., considered polar today, but would have been near or north 2004; Gangloff, 2012). These findings include remains of the Arctic Circle during the Cretaceous. from Russia (Nessov and Golovneva, 1990; Averianov and A hadrosaurid dinosaur vertebra was found on Axel Sues, 2007; Godefroit et al., 2009), Alaska (Brouwers et al., Heiberg Island, Nunavut (Fig. 1), in July 1992 during a 1987; Fiorillo and Gangloff, 2000; Gangloff et al., 2005; stratigraphic and palynological survey of the Kanguk Fiorillo, 2008; Brown and Druckenmiller, 2011), Yukon Formation in the northeastern Canadian Arctic (Núñez- (Rouse and Srivastava, 1972; Gangloff et al., 2004; Evans Betelu et al., 2005). This same expedition also recovered 1 Royal Ontario Museum, Department of Natural History, 100 Queen’s Park, Toronto, Ontario M5S 2C6, Canada; [email protected] 2 Deceased 3 Department of Biological Sciences, University of Alberta, Edmonton, Alberta T6G 2E9, Canada http://dx.doi.org/10.14430/arctic4362 © The Arctic Institute of North America 2 • M.J. VAVREK et al. capped by a rooted paleosol and is directly overlain by mud- stones of the Kanguk Formation. A similar situation exists at Strathcona Fiord (78.5472˚ N, 82.9153˚ W), but the coars- ening upward sequence is less well defined and is replaced by interbedded sandstones, which thin upwards and have interbeds of mudstone that thicken upwards. The coars- ening upward sequences gradational to the Eureka Sound Group are coarsest in the east and are thinner and finer- grained to the west. This pattern indicates that the source of the Kanguk Formation lay to the east of May Point along the axis of Ellesmere Island, and thus the dinosaur vertebra was sourced west of the axis of Ellesmere Island. Hills et al. (1994) described Scaphites depressus Reeside from the Kanguk Formation at the head of Glacier Fiord on southwestern Axel Heiberg Island, providing clear evidence of a connection with the Western Interior Seaway. Palyno- logical evidence indicates that the Kanguk Formation at Glacier Fiord is contiguous with the formation at May Point, although the sediments at May Point were deposited farther offshore. Since uplift on Axel Heiberg Island post- dates the Kanguk Formation, present-day Axel Heiberg Island was not yet above sea level when the dinosaur fossil FIG. 1. Location of Axel Heiberg Island, Nunavut, Canada. Star denotes was deposited. Therefore, the vertebra must have originated approximate discovery site of the dinosaur fossil at May Point. from a nearby terrestrial area. additional vertebrate remains of a hesperornithid bird and a large fish Xiphactinus( sp.) from nearby Ellesmere Island LOCAL GEOLOGY (Hills et al., 1999), although no non-avian dinosaurs were found on that island. This most northerly occurrence of a The hadrosaurid vertebra was found within the upper non-avian dinosaur has biologic, climatic, and geographic portion of the Kanguk Formation, at May Point on Axel implications for dinosaurs inhabiting this region during the Heiberg Island, Nunavut, Canada (Fig. 2). The local sedi- Late Cretaceous. ments also contained a large marine reptile fossil and abundant dinoflagellate cysts (Núñez-Betelu et al., 2005), indicating that the dinosaur bone was preserved in a marine GEOLOGICAL SETTING environment. The dinosaur fossil is abraded, suggesting it was likely worn in a fluvial or shoreline environment before The Sverdrup Basin is a major Carboniferous to Pale- being transported out to sea for burial. ogene depocentre within the Canadian Arctic Islands (Embry, 1991; Embry and Beauchamp, 2008), and the Cenomanian/Turonian to Campanian aged Kanguk Forma- PALYNOLOGY tion outcrops extensively within the basin (Núñez-Betelu et al., 1994). In general, the lower Kanguk Formation is com- Samples collected 8 m above the dinosaur-bearing hori- posed of dark, organic-rich mudstones that represent a low- zon yielded dinoflagellate cysts, acritarchs, spores, and pol- oxygen and low-energy environment (Núñez-Betelu et al., len (Appendix 1). In particular, the palynomorphs recovered 1994). The upper Kanguk Formation strata are composed were well preserved, and the assemblage was dominated of claystones, siltstones, and very fine-grained sandstones by the dinoflagellate Scrinodinium crystallinum (Núñez- (Núñez-Betelu et al., 1994). These upper beds record a shal- Betelu et al., 2005). The microfossil assemblage correlates low shelf and nearshore facies and contain an abundant well with Biozone 4 of Núñez-Betelu (1994), suggesting a marine and terrestrial microfossil record, as well as inocer- middle Campanian age (Núñez-Betelu et al., 2005). amids, ammonites, and indeterminate marine vertebrates (Núñez-Betelu et al., 1994; Hills et al., 1999). The Kanguk Formation gradationally overlies the Has- PALAEOCLIMATE AND PALAEOGEOGRAPHY sel Formation and is gradationally overlain by the Eureka Sound Group on Ellesmere Island. At Cañon Fiord, Elles- The climate during the Late Cretaceous was much mere Island (79.8758˚ N, 82.2378˚ W), the upper Hassel warmer than at present (Frakes, 1979; Barron, 1983; Hal- Formation consists of a series of coarsening upward cycles lam, 1985), and Arctic regions in particular had much higher separated by marine mudstones. The last of these cycles is temperatures, which produced a smaller equator-to-pole LATE CRETACEOUS HADROSAURID • 3 temperature gradient than exists today (Barron, 1983; Amiot et al., 2004). By the Campanian, global temperatures had declined somewhat from their high in the Turonian (Parrish and Spicer, 1988a; Jenkyns et al., 2004), and Arctic regions during the Campanian may have experienced frosts and some snowfall (Wolfe and Upchurch, 1987; Amiot et al., 2004). Sea levels during the Late Cretaceous were much higher than at present (Haq et al., 1987), and large portions of North America were flooded by inland seaways (Kauffman and Caldwell, 1993; Smith et al., 1994; Hay et al., 1999). In particular, the large Western Interior Seaway extended from the Arctic Ocean to the Gulf of Mexico for most of the Late Cretaceous, dividing North America into western and eastern sub-continents, sometimes referred to as Laramidia and Appalachia, respectively. During the Late Cretaceous, North America was at approximately the same latitude as it is today, although it was rotated clockwise relative to its present orientation (Smith et al., 1994; Scotese, 2002). This rotation meant that Alaska, Yukon, northern British Columbia, and Alberta would have been farther north than they are currently, while eastern Nunavut would have been somewhat farther south. The rotation of the continent would have placed sev- eral dinosaur-bearing localities in northern British Colum- bia and Alberta near or north of the Arctic Circle; however, Axel Heiberg Island would have been farther south (at approximately 75˚ N) than it is at present (Scotese, 2002).
Recommended publications
  • Papers in Press
    Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2018PR013 Features and paleoecological significance of the shark fauna from the Upper Cretaceous Hinoshima Formation, Himenoura Group, Southwest Japan Accepted Naoshi Kitamura 4-8-7 Motoyama, Chuo-ku Kumamoto, Kumamoto 860-0821, Japan (e-mail: [email protected]) Abstract. The shark fauna of the Upper Cretaceous Hinoshima Formation (Santonian: 86.3–83.6 Ma) of the manuscriptHimenoura Group (Kamiamakusa, Kumamoto Prefecture, Kyushu, Japan) was investigated based on fossil shark teeth found at five localities: Himedo Park, Kugushima, Wadanohana, Higashiura, and Kotorigoe. A detailed geological survey and taxonomic analysis was undertaken, and the habitat, depositional environment, and associated mollusks of each locality were considered in the context of previous studies. Twenty-one species, 15 genera, 11 families, and 6 orders of fossil sharks are recognized from the localities. This assemblage is more diverse than has previously been reported for Japan, and Lamniformes and Hexanchiformes were abundant. Three categories of shark fauna are recognized: a coastal region (Himedo Park; probably a breeding site), the coast to the open sea (Kugushima and Wadanohana), and bottom-dwelling or near-seafloor fauna (Kugushima, Wadanohana, Higashiura, and Kotorigoe).
    [Show full text]
  • New Constraints on the Age, Geochemistry
    New constraints on the age, geochemistry, and environmental impact of High Arctic Large Igneous Province magmatism: Tracing the extension of the Alpha Ridge onto Ellesmere Island, Canada T.V. Naber1,2, S.E. Grasby1,2, J.P. Cuthbertson2, N. Rayner3, and C. Tegner4,† 1 Geological Survey of Canada–Calgary, Natural Resources Canada, Calgary, Canada 2 Department of Geoscience, University of Calgary, Calgary, Canada 3 Geological Survey of Canada–Northern, Natural Resources Canada, Ottawa, Canada 4 Centre of Earth System Petrology, Department of Geoscience, Aarhus University, Aarhus, Denmark ABSTRACT Island, Nunavut, Canada. In contrast, a new Province (HALIP), is one of the least studied U-Pb age for an alkaline syenite at Audhild of all LIPs due to its remote geographic lo- The High Arctic Large Igneous Province Bay is significantly younger at 79.5 ± 0.5 Ma, cation, and with many exposures underlying (HALIP) represents extensive Cretaceous and correlative to alkaline basalts and rhyo- perennial arctic sea ice. Nevertheless, HALIP magmatism throughout the circum-Arctic lites from other locations of northern Elles- eruptions have been commonly invoked as a borderlands and within the Arctic Ocean mere Island (Audhild Bay, Philips Inlet, and potential driver of major Cretaceous Ocean (e.g., the Alpha-Mendeleev Ridge). Recent Yelverton Bay West; 83–73 Ma). We propose anoxic events (OAEs). Refining the age, geo- aeromagnetic data shows anomalies that ex- these volcanic occurrences be referred to col- chemistry, and nature of these volcanic rocks tend from the Alpha Ridge onto the northern lectively as the Audhild Bay alkaline suite becomes critical then to elucidate how they coast of Ellesmere Island, Nunavut, Canada.
    [Show full text]
  • Mesocyparis Rosanovii</Emphasis> Sp. Nov
    ISSN 0031-0301, Paleontological Journal, 2006, Vol. 40, No. 3, pp. 328–338. © Pleiades Publishing, Inc., 2006. Original Russian Text © T.M. Kodrul, M.V. Tekleva, V.A. Krassilov, 2006, published in Paleontologicheskii Zhurnal, 2006, No. 3, pp. 93–102. A New Conifer Species, Mesocyparis rosanovii sp. nov. (Cupressaceae, Coniferales), and Transberingian Floristic Connections T. M. Kodrula, M. V. Teklevab, and V. A. Krassilovc aGeological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 109017 Russia e-mail: [email protected] bPaleontological Institute of Russian Academy of Sciences, ul. Profsoyuznaya 123, Moscow, 117997 Russia cInstitute of Evolution, University of Haifa, Mount Carmel 31905, Haifa, Israel Received October 25, 2005 Abstract—A new species, Mesocyparis rosanovii sp. nov. from the Lower Paleocene of the Amur Region, Rus- sia, is characterized by a combination of advanced and primitive features: mixed opposite-alternate branching of vegetative shoots, leafy microsporophylls, as well as a relatively high number of sporangia per microsporo- phyll and seeds per cone scale. The Late Cretaceous–Early Paleogene genus Mesocyparis McIver et Basinger, which obviously embraces a natural group of closely related species, was a significant component of the vege- tation in the middle and high latitudes of eastern Asia and western North America. The range of the genus tes- tifies to terrestrial Transberingian connections between the continents during the Cretaceous warming phases. DOI: 10.1134/S0031030106030142 Key words: conifers, Cupressaceae, Paleocene, Amur Region, Beringia, phytogeography. INTRODUCTION from each other, which would have virtually excluded the possibility of migration. The problem of floristic exchanges between eastern In this context, phytogeographic relations between Asia and western regions of North America has long Asia and North America should be revised using mod- attracted the attention of phytogeographers.
    [Show full text]
  • Mannville Group of Saskatchewan
    Saskatchewan Report 223 Industry and Resources Saskatchewan Geological Survey Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan J.E. Christopher 2003 19 48 Printed under the authority of the Minister of Industry and Resources Although the Department of Industry and Resources has exercised all reasonable care in the compilation, interpretation, and production of this report, it is not possible to ensure total accuracy, and all persons who rely on the information contained herein do so at their own risk. The Department of Industry and Resources and the Government of Saskatchewan do not accept liability for any errors, omissions or inaccuracies that may be included in, or derived from, this report. Cover: Clearwater River Valley at Contact Rapids (1.5 km south of latitude 56º45'; latitude 109º30'), Saskatchewan. View towards the north. Scarp of Middle Devonian Methy dolomite at right. Dolomite underlies the Lower Cretaceous McMurray Formation outcrops recessed in the valley walls. Photo by J.E. Christopher. Additional copies of this digital report may be obtained by contacting: Saskatchewan Industry and Resources Publications 2101 Scarth Street, 3rd floor Regina, SK S4P 3V7 (306) 787-2528 FAX: (306) 787-2527 E-mail: [email protected] Recommended Citation: Christopher, J.E. (2003): Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan; Sask. Industry and Resources, Report 223, CD-ROM. Editors: C.F. Gilboy C.T. Harper D.F. Paterson RnD Technical Production: E.H. Nickel M.E. Opseth Production Editor: C.L. Brown Saskatchewan Industry and Resources ii Report 223 Foreword This report, the first on CD to be released by the Petroleum Geology Branch, describes the geology of the Success Formation and the Mannville Group wherever these units are present in Saskatchewan.
    [Show full text]
  • TGI Strat Column 2009.Cdr
    STRATIGRAPHIC CORRELATION CHART TGI II: Williston Basin Architecture and Hydrocarbon Potential in Eastern Saskatchewan and Western Manitoba EASTERN MANITOBA PERIOD MANITOBA SUBSURFACE SASKATCHEWAN OUTCROP ERA glacial drift glacial drift glacial drift Quaternary Wood Mountain Formation Peace Garden Peace Garden Member Tertiary Member Ravenscrag Formation CENOZOIC Formation Goodlands Member Formation Goodlands Member Turtle Mountain Turtle Mountain Turtle Frenchman Formation Whitemud Formation Boissevain Formation Boissevain Formation Eastend Formation Coulter Member Coulter Member Bearpaw Formation Odanah Member Belly River “marker” Odanah Member Belly River Formation “lower” Odanah Member Millwood Member Lea Park Formation Millwood Member MONTANA GROUP Pembina Member Pembina Member Pierre Shale Pierre Shale Milk River Formation Gammon Ferruginous Member Gammon Ferruginous Member Niobrara Formation Chalky Unit Boyne Member Boyne Member Boyne Calcareous Shale Unit Member Carlile Morden Member Carlile upper Formation Morden Member Formation Morden Member Carlile Formation Assiniboine Marco Calcarenite Assiniboine Member Member CRETACEOUS Second White Specks Laurier Limestone Beds Favel Favel Keld Keld Member Member Formation Formation Belle Fourche Formation Belle Fourche Member MESOZOIC COLORADO GROUP Belle Fourche Member upper Fish Scale Formation Fish Scale Zone upper Base of Fish Scale marker Base of Fish Scale marker Westgate Formation Westgate Member lower Westgate Member Newcastle Formation Newcastle Member lower Viking Sandstone
    [Show full text]
  • Late Pleistocene Birds from Kingston Saltpeter Cave, Southern Appalachian Mountains, Georgia
    Bull. Fla. Mus. Nat. Hist. (2005) 45(4):231-248 231 LATE PLEISTOCENE BIRDS FROM KINGSTON SALTPETER CAVE, SOUTHERN APPALACHIAN MOUNTAINS, GEORGIA David W. Steadman1 Kingston Saltpeter Cave, Bartow County, Georgia, has produced late Quaternary fossils of 38 taxa of birds. The presence of extinct species of mammals, and three radiocarbon dates on mammalian bone collagen ranging from approximately 15,000 to 12,000 Cal B.P., indicate a late Pleistocene age for this fauna, although a small portion of the fossils may be Holocene in age. The birds are dominated by forest or woodland species, especially the Ruffed Grouse (Bonasa umbellus) and Passenger Pigeon (Ectopistes migratorius). Species indicative of brushy or edge habitats, wetlands, and grasslands also are present. They include the Greater Prairie Chicken (Tympanuchus cupido, a grassland indicator) and Black-billed Magpie (Pica pica, characteristic of woody edges bordering grasslands). Both of these species reside today no closer than 1000+ km to the west (mainly northwest) of Georgia. An enigmatic owl, perhaps extinct and undescribed, is represented by two juvenile tarsometatarsi. The avifauna of Kingston Saltpeter Cave suggests that deciduous or mixed deciduous/coniferous forests and woodlands were the dominant habitats in the late Pleistocene of southernmost Appalachia, with wetlands and grasslands present as well. Key Words: Georgia; late Pleistocene; southern Appalachians; Aves; extralocal species; faunal change INTRODUCTION dates have been determined from mammal bones at Numerous late Pleistocene vertebrate faunas have been KSC. The first (10,300 ± 130 yr B.P.; Beta-12771, un- recovered from caves and other karst features of the corrected for 13C/12C; = 12,850 – 11,350 Cal B.P.) is Appalachian region (listed in Lundelius et al.
    [Show full text]
  • Prootic Anatomy of a Juvenile Tyrannosauroid from New Jersey and Its Implications for the Morphology and Evolution of the Tyrannosauroid Braincase
    Prootic anatomy of a juvenile tyrannosauroid from New Jersey and its implications for the morphology and evolution of the tyrannosauroid braincase Chase D Brownstein Corresp. 1 1 Collections and Exhibitions, Stamford Museum & Nature Center, Stamford, Connecticut, United States Corresponding Author: Chase D Brownstein Email address: [email protected] Among the most recognizable theropods are the tyrannosauroids, a group of small to large carnivorous coelurosaurian dinosaurs that inhabited the majority of the northern hemisphere during the Cretaceous and came to dominate large predator niches in North American and Asian ecosystems by the end of the Mesozoic era. The clade is among the best-represented of dinosaur groups in the notoriously sparse fossil record of Appalachia, the Late Cretaceous landmass that occupied the eastern portion of North America after its formation from the transgression of the Western Interior Seaway. Here, the prootic of a juvenile tyrannosauroid collected from the middle-late Campanian Marshalltown Formation of the Atlantic Coastal Plain is described, remarkable for being the first concrete evidence of juvenile theropods in that plain during the time of the existence of Appalachia and the only portion of theropod braincase known from the landmass. Phylogenetic analysis recovers the specimen as an “intermediate” tyrannosauroid of similar grade to Dryptosaurus and Appalachiosaurus. Comparisons with the corresponding portions of other tyrannosauroid braincases suggest that the Ellisdale prootic is more similar to Turonian forms in morphology than to the derived tyrannosaurids of the Late Cretaceous, thus supporting the hypothesis that Appalachian tyrannosauroids and other vertebrates were relict forms surviving in isolation from their derived counterparts in Eurasia.
    [Show full text]
  • Fordyce, RE 2006. New Light on New Zealand Mesozoic Reptiles
    Fordyce, R. E. 2006. New light on New Zealand Mesozoic reptiles. Geological Society of New Zealand newsletter 140: 6-15. The text below differs from original print format, but has the same content. P 6 New light on New Zealand Mesozoic reptiles R. Ewan Fordyce, Associate Professor, Otago University ([email protected]) Jeff Stilwell and coauthors recently (early 2006) published the first report of dinosaur bones from Chatham Island. The fossils include convincing material, and the occurrence promises more finds. Questions remain, however, about the stratigraphic setting. This commentary summarises the recent finds, considers earlier reports of New Zealand Mesozoic vertebrates, and reviews some broader issues of Mesozoic reptile paleobiology relevant to New Zealand. The Chatham Island finds A diverse team reports on the Chathams finds. Jeff Stilwell (fig. 1 here) is an invertebrate paleontologist with research interests on Gondwana breakup and Southern Hemisphere Cretaceous-early Cenozoic molluscs (e.g. Stilwell & Zinsmeister 1992), including Chatham Islands (1997). Several authors are vertebrate paleontologists – Chris Consoli, Tom Rich, Pat Vickers-Rich, Steven Salisbury, and Phil Currie – with diverse experience of dinosaurs. Rupert Sutherland and Graeme Wilson (GNS) are well-known for their research on tectonics and biostratigraphy. The Chathams article describes a range of isolated bones attributed to theropod (“beast-footed,” carnivorous) dinosaurs, including a centrum (main part or body of a vertebra), a pedal phalanx (toe bone), the proximal head of a tibia (lower leg bone, at the knee joint), a manual phalanx (finger bone) and a manual ungual (terminal “claw” of a finger). On names of groups, fig.
    [Show full text]
  • Black Lives and Whitened Stories: from the Lowcountry to the Mountains?
    National Park Service <Running Headers> <E> U.S. Department of the Interior Historic Resource Study of Black History at Rock Hill/Connemara Carl Sandburg Home NHS BLACK LIVES AND WHITENED STORIES: From the Lowcountry to the Mountains David E. Whisnant and Anne Mitchell Whisnant CULTURAL RESOURCES SOUTHEAST REGION BLACK LIVES AND WHITENED STORIES: From the Lowcountry to the Mountains By David E. Whisnant, Ph.D. Anne Mitchell Whisnant, Ph.D. Primary Source History Services A HISTORIC RESOURCE STUDY OF BLACK HISTORY AT ROCK HILL/CONNEMARA Presented to Carl Sandburg Home National Historic Site In Partnership with the Organization of American Historians/National Park Service Southeast Region History Program NATIONAL PARK SERVICE U.S. DEPARTMENT OF THE INTERIOR NOVEMBER 2020 Cultural Resources Division Southeast Regional Office National Park Service 100 Alabama Street, SW Atlanta, Georgia 30303 (404) 507-5847 Black Lives and Whitened Stories: From the Lowcountry to the Mountains By David E. Whisnant and Anne Mitchell Whisnant http://www.nps.gov Cover Photos: Smyth Servants: Black female servant rolling children in stroller. Photograph, Carl Sandburg National Historic Site archives, (1910; Sadie “Boots” & Rosana [?]). Smyth Servants: Swedish House HSR, p. 22; (Collection of William McKay, great-grandson of the Smyths). Also Barn Complex HSR Fig. 11, p. 7: Figure 11. The Smyths’ servants in front of the kitchen building, ca. 1910. (Collection of Smyth great-grandson William McKay). Sylvene: From HSR, Main House, pp. 10, 37: Collection of Juliane Heggoy. Man and 3: Swedish House HSR, p. 22; (Collection of William McKay, great-grandson of the Smyths). Also Barn Complex HSR Fig.
    [Show full text]
  • A Tyrannosauroid Metatarsus from the Merchantville Formation of Delaware Increases the Diversity of Non-Tyrannosaurid Tyrannosauroids on Appalachia
    A tyrannosauroid metatarsus from the Merchantville Formation of Delaware increases the diversity of non-tyrannosaurid tyrannosauroids on Appalachia Chase D. Brownstein Collections and Exhibitions, Stamford Museum & Nature Center, Stamford, CT, USA ABSTRACT During the Late Cretaceous, the continent of North America was divided into two sections: Laramidia in the west and Appalachia in the east. Although the sediments of Appalachia recorded only a sparse fossil record of dinosaurs, the dinosaur faunas of this landmass were different in composition from those of Laramidia. Represented by at least two taxa (Appalachiosaurus montgomeriensis and Dryptosaurus aquilunguis), partial and fragmentary skeletons, and isolated bones, the non-tyrannosaurid tyrannosauroids of the landmass have attracted some attention. Unfortunately, these eastern tyrants are poorly known compared to their western contemporaries. Here, one specimen, the partial metatarsus of a tyrannosauroid from the Campanian Merchantville Formation of Delaware, is described in detail. The specimen can be distinguished from A. montgomeriensis and D. aquilunguis by several morphological features. As such, the specimen represents a potentially previously unrecognized taxon of tyrannosauroid from Appalachia, increasing the diversity of the clade on the landmass. Phylogenetic analysis and the morphology of the bones suggest the Merchantville specimen is a tyrannosauroid of “intermediate” grade, thus supporting the notion that Appalachia was a refugium Submitted 18 July 2017 for relict dinosaur
    [Show full text]
  • Late Cretaceous) Cephalopods from the L´Opez De Bertodano Formation, Seymour Island, Antarctica
    ÔØ ÅÒÙ×Ö ÔØ Evolution and extinction of Maastrichtian (Late Cretaceous) cephalopods from the L´opez de Bertodano Formation, Seymour Island, Antarctica James D. Witts, Vanessa C. Bowman, Paul B. Wignall, J. Alistair Crame, Jane E. Francis, Robert J. Newton PII: S0031-0182(14)00560-4 DOI: doi: 10.1016/j.palaeo.2014.11.002 Reference: PALAEO 7081 To appear in: Palaeogeography, Palaeoclimatology, Palaeoecology Received date: 23 February 2014 Revised date: 3 November 2014 Accepted date: 12 November 2014 Please cite this article as: Witts, James D., Bowman, Vanessa C., Wignall, Paul B., Al- istair Crame, J., Francis, Jane E., Newton, Robert J., Evolution and extinction of Maas- trichtian (Late Cretaceous) cephalopods from the L´opez de Bertodano Formation, Sey- mour Island, Antarctica, Palaeogeography, Palaeoclimatology, Palaeoecology (2014), doi: 10.1016/j.palaeo.2014.11.002 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. ACCEPTED MANUSCRIPT Evolution and extinction of Maastrichtian (Late Cretaceous) cephalopods from the López de Bertodano Formation, Seymour Island, Antarctica James D. Witts a,* Vanessa C. Bowman b, Paul B. Wignall a, J. Alistair Crame b, Jane E. Francis a,b, Robert J. Newton a a School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, United Kingdom b British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, United Kingdom * Corresponding author: [email protected] ACCEPTED MANUSCRIPT 1 ACCEPTED MANUSCRIPT ABSTRACT One of the most expanded records to contain the final fortunes of ammonoid cephalopods is within the López de Bertodano Formation of Seymour Island, James Ross Basin, Antarctica.
    [Show full text]
  • Memoir of the Fukui Prefectural Dinosaur Museum 16: 29–38 (2017) ARTICLE © by the Fukui Prefectural Dinosaur Museum
    Memoir of the Fukui Prefectural Dinosaur Museum 16: 29–38 (2017) ARTICLE © by the Fukui Prefectural Dinosaur Museum FIRST OCCURRENCE OF A TYRANNOSAUROID DINOSAUR FROM THE LOWER CAMPANIAN MERCHANTVILLE FORMATION OF DELAWARE, USA Sebastian G. DALMAN1, Steven E. JASINSKI2,3 and Spencer G. LUCAS1 1 New Mexico Museum of Natural History and Science, 1801 Mountain Road N. W. Albuquerque, NM 87104 USA 2 The State Museum of Pennsylvania, Section of Paleontology and Geology, 300 North Street, Harrisburg, PA 17120-0024 USA 3 University of Pennsylvania, Department of Earth and Environmental Science, Philadelphia, PA 19104-6316 USA ABSTRACT This study provides a detailed osteological description of an isolated proximal caudal centrum and two nearly complete isolated metatarsals II and IV of the left foot of a gracile theropod dinosaur from the Lower Campanian of the Merchantville Formation in northern Delaware, USA. The caudal centrum and the metatarsals are referred to Tyrannosauroidea. The centrum is not well preserved, and thus not diagnostic; however, both metatarsals are diagnostic. The referral to Tyrannosauroidea is supported by several morphological features, including extensive surfaces on metatarsals II and IV for the articulation with metatarsal III, and a characteristic low, slightly convex muscle scar on metatarsal IV developed as a thin low ridge located on the posterior surface between the M. gastrocnemius pars lateralis insertion scar and the metatarsal III articular surface. This ridge has been previously interpreted as the plantar ridge, which is present in some derived Late Campanian tyrannosauroid taxa. Additionally, metatarsal IV has a deep medial notch for the accommodation of an“ L”– shaped proximal articulation of metatarsal III, and a“ U”– shaped proximal articular end.
    [Show full text]