New Paleontology Gallery Exhibit Soon to Open

Total Page:16

File Type:pdf, Size:1020Kb

New Paleontology Gallery Exhibit Soon to Open The Newsletter of the Calvert Marine Museum Fossil Club Volume 22 .Number 4 D~cember2007 New Paleontology Gallery Exhibit Soon to Open ... After years of planning and months of construction and installation, a new exhibit, nearing its birth now graces' the entrance, to our Paleontology Gallery. Designed by Exhibits Curator, James Langley, this superb addition to the Museum was made possible through funding from a CMM's resident artist, Tim Scheirer National Parks Service begins to apply the spiral Earth-history Gateways Grant and the time-line to the wall. Rachel Reese, Clarissa and Lincoln Dryden another member of the CMM Exhibit's Endowment for Department, completed the computer Paleontology. CMM Fossil graphic work. The new exhibit will also Club members donated feature video presentations, some of the fossils on geoanimations, and computer terminals for display. in depth information about thefossils. Tommy Younger (left) and Skip The mural includes cast replicas. It Edwards crafted the jewel-like is my desir.e to gradually replace armature that holds an original most of the casts with original oreodont skull now on display. Scalae Naturae ... fossils as donations and/or funds become available. CALVERT MARINE MUSEUM www.calvertmarinemuseum.com '~The Ecphora December 2007 Deinosuchus: Another Maryland "SuperCroc" Figure 2 shows life drawings of crocodile and alligator heads, at approximately the same scale as By: George F. Klein Figure 1. You will note the width of the alligator's head compared to that of the crocodile. In terms of skull width, Deinosuchus resembles an alligator Deinosuchus was a large crocodilian that more than a crocodile. Having a wider snout is a lived during the Late Cretaceous. It is among the characteristic of alligators. largest crocodilians to have ever lived, with a length approaching 40 feet and a weight estimated to be 9.5 tons (1). Deinosuchus fossils have been found in Maryland, in Prince George's County (3,6). Recent work by Schwimmer (1) places Deinosuchus close to the common ancestor of the alligator family. Figure 1 shows drawings of a Deinosuchus skull (lettering on the skull refers to the individual bones). You will note that with the jaws closed, teeth from both the upper and lower jaws are visible. Especially note the notch in the jaws just behind the premaxillary bone (labeled PM in the drawing, the tip of the snout). These are characteristics of crocodiles. sa PO PRF Figure 2: The head of a crocodile (left) compared to an alligator. Recently, a new discovery has extended the geographic range of this animal to the state of New Mexico. The Deinosuchus fossils were discovered in 1999 and only recently identified. Paul Sealey, a volunteer for the New Mexico Museum of Natural History (NMMNH), found them. The fossils were found close to the town of Farmington, in the northwest comer of the state near the "Four Comers" region. The fossils consisted of a section of the lower jaw, some teeth and scutes. The fossils have been prepared and are currently on display at the NMMNH in Albuquerque (2, 5). This is the first time Deinosuchus fossil have Figure 1: Two views of a Deinosuchus skull. been found in New Mexico. According to Club website: http://www.calvertmarinemuseum.com/cmmfc/index.html Club email: [email protected] - --- --------- ----- ---- -- --------- Schwimmer (1), Deinosuchus fossils have been Deinosuchus probably lived in nearshore, .identified from ten states. My research (3) indicates estuary, and salt marsh environments the way the Schwimmer seems to have missed one state, Salt Water Crocodile (Crocodylus porosus) of Maryland (believe it or not!). Therefore, the states Australia and the Pacific region does today. It is where Deinosuchus fossils occur are now: likely that it lived all up and down the East Coast of the US and along both shores of the WIS, probably (1) New Jersey Ref. (1) as far as what would have been the Canadian border, (2) Maryland Ref. (3) although its fossils may be lacking in certain areas as (3) Delaware Ref. (1) noted above. (4) North Carolina Ref. (1) To my knowledge, Deinosuchus fossil have (5) South Carolina Ref. (1) not been found in the Campanian Age WenonahlMt. (6) Georgia Ref. (1) Laurel Formations exposed at Big Brook and (7) Alabama Ref. (1) Ramanessian Brook of New Jersey. These represent (8) Mississippi Ref. (1) deepwater sediments. Deinosuchus remains have (9) Texas Ref. (1) been found at the famous Ellisdale, NJ site, in the (10) New Mexico Ref. (2) Marshalltown Formation. The fossils from Ellisdale (11) Wyoming Ref. (1) represent a near shore environment. Virginia, an East (12) Montana Ref. (1) Coast state lacking Deinosuchus remains, has exposed only Early Cretaceous formations. As you will recall, during most of the Schwimmer found evidence of Deinosuchus Cretaceous, the Western Interior Seaway (WIS) split predation on dinosaurs. A private collector in the Big North America from the Gulf of Mexico to the Bend area of Texas found hadrosaur vertebrae with Arctic. Occurrences of Deinosuchus fossils west of blunt bite marks on them. These big marks are the current Mississippi River are from what would probably too large to have been made by the other be the east facing shore of the WIS. The only crocodilians alive during the Cretaceous. occurrence of Deinosuchus from the west facing Photographs of these vertebrae are shown in shore is that from the state of Mississippi. reference 1. At 9.5 tons, Deinosuchus was heavier Interestingly, Deinosuchus and crocodilian than a T rex and any hadrosaur. fossils in general are lacking from the terrific marine Cretaceous formations of Kansas. I find the paucity of crocodile fossils from this state somewhat perplexing, as dinosaurs have been found in these marine exposures. Some of the dinosaurs found in Kansas are undoubtedly due to "float and bloat"-that is a dinosaur dies, was washed into a river and eventually into the WIS, floating due to bloating of its carcass as a result of internal bacterial decay. Then marine predators like sharks and mosasaurs probably scavenged it following which, the carcass sank to the bottom where it became fossilized. You would think that a crocodile would also become fossilized in Kansas by the same process. Deinosuchus fossils are found in late Cretaceous exposures (Campanian and possibly Maastrichtian Age, 83.0 - 65.4 million years old). Figure 3: Deinosuchus posterior tooth, basal The youngest formations in Kansas are 82 -83 diameter approx. 1.5". million years old (4) so this may explain the lack of Deinosuchus fossils from that state. Club website: http://www.calvertmarinemuseum.comlcmmfc/index.html Club email: [email protected] ¥k.'The-ill Ecphora December 2007 Thanks to Dewayne Varnum, President of the Stingray crusher plate from East Coast Fossil Club of Fayetteville, North Carolina (www.megalodon.net). Above is a Purse State Park photograph of a very large posterior Deinosuchus tooth, found at Elizabethtown, NC. Elizabethtown I found a nearly complete ray crusher plate has been the source of some of the most significant on Nov. 8, 2007 on the Potomac shoreline at Purse Deinosuchus finds on the East Coast. State Park. The plate was actually embedded in a In addition to the very large Miocene layer of Aquia Formation sediment about six inches crocodile Gavialosuchus (or Thecachampsa) found below the surface of the water when I stumbled upon at Calvert Cliffs,. during the Cretaceous, Maryland it. I'm kind of sorry that I didn't walk back to the was home to another, even larger crocodilian, truck to retrieve a shovel to remove a slab of Deinosuchus. sediment so that it could be uncovered "in situ." In stead I hacked it out in four pieces with my wire References mesh scoop-on-a-handle. (1) King 0/ the Crocodylians by: D. R. Schwimmer Indiana University press, Bloomington, IN 2002 (2) http://www.abqtrib.com/newsI2006/janl03/bo na- fide-bony- find! (3) Hartstein, E, L. Decina and R. Keil "A Late Cretaceous (Severn Formation) Vertebrate Assemblage from Bowie, Maryland" The Mosasaur, Vol. 6, p. 17 (May 1999) (4) Oceans o/Kansas by: MJ. Everhart Indiana University Press, Bloomington, IN 2005 (5) www.nmnaturalhistory.org/science!geoscienc e/collecting fossils/disp1ay1.html (6) Collecting Fossils in Maryland by: J. D. Glaser Johns Hopkins University Press, Baltimore, MD 1995 ?Oldest Record of Multicellular The plate (Myliobatis copeanus) measures 3.25 Life, Named Fracto/usus misrai inches long by 2.25 inches wide and contains 10 rows o/plates! Photo by B. Hargreaves. A fossil found in Canada believed to be 565 Submitted by Bruce Hargreaves -P million years old has been named after the Indian geologist, Shiva Balak Misra, who found it. http://news.bbc.co.uk/2/hi/south asia17000829.stm Submitted by Yasemin Tulu -P Club website: http://www.calvertmarinemuseum.comlcmmfc/index.html Club email: CMMFossilclub@hotmaiLcom ~~\::The-s""· Ecphora December 2007 Locals know the area around the Bear Valley The Carboniferous Challenge: mine as a recreation site for off-road vehicles and a Seed Fems, Scale Trees, and place to swim in some of the water-filled pits. Horsetails Geologists know it as the site of "Whaleback", an exposed example of the Allegheny orogeny (mountain building) and a famous natural structure By: Tom Farrell & Bruce Hargreaves that is visited by college geology students from' around the globe. In fact, it's "paradise lost" for While most field trips sponsored by the many geologists because it contains examples of CMMFC focus on the hunt for extinct marine life three types of faults, plus folds, joints, cleavage, associated with the Miocene epoch, occasionally we lineations, and slickenlines, not to mention numerous explore areas along the Eastern seaboard containing varieties of terrestrial and marine sediments, all fossil-bearing sediments from other eras.
Recommended publications
  • Skempton's Poroelastic Relaxation
    Datashare 129 Skempton’s poroelastic relaxation: The mechanism that accounts for the distribution of pore pressure and exhumation-related fractures in black shale of the Appalachian Basin Terry Engelder and Rose-Anna Behr AAPG Bulletin, v. 105, no. 4 (April 2021), pp. 669–694 Copyright ©2021. The American Association of Petroleum Geologists. All rights reserved. EXPLANATIONS FOR TABLE 2: In an expansion of work by Sheldon (1912) on COMPARATIVE TERMINOLOGIES FROM the Appalachian Plateau, east-northeast fractures were SELECTED JOINT STUDIES IN THE mapped across a region large enough to sample rocks APPALACHIAN BASIN through a 20° swing of the Appalachian oroclinal bend (Parker, 1942). Parker (1942) relabeled the strike fi The rst depictions of Appalachian Basin fractures joints in Sheldon (1912) as set III (accompanying paper were in wood block prints by Sarah Hall as they appear Table 2 and in this Datashare). This was necessary ’ in her husband s paper from the geological survey of because the azimuth of these set III joints (i.e., the east- the fourth district of New York (Hall, 1843). A print northeast set) did not follow around the oroclinal of Taughannock Falls cascading over the Geneseo bend as defined by fold axes. Parker (1942, p. 406) black shale a few kilometers north of Ithaca, New York, writes, “Their different character and constant strike shows two major joint sets that are not quite orthogonal. over the whole region point definitely to an indepen- The artist even captured a hint of lithological control dent origin, perhaps simultaneous or perhaps much of the black shale on joint development.
    [Show full text]
  • Smithsonian Contributions and Studies
    Thecachampsa antiqua (Leidy, 1852) (Crocodylidae: Thoracosaurinae) from Fossil Marine Deposits at Lee Creek Mine, Aurora, North Carolina, USA Albert C. Myrick, Jr. Formation (early Pliocene; Gibson, 1983; Hazel, 1983). It ABSTRACT provides a first opportunity to study the Lee Creek crocodilian materials in relation to other similar forms of comparable geo- Fossil remains of crocodilians at Lee Creek Mine have been few and fragmentary. Nevertheless, isolated teeth and dermal plates logic age. The purpose of this paper is to describe the Lee from the spoil piles are identifiable as Thecachampsa antiqua Creek Mine crocodilian specimens and to comment on the (Leidy). This species was established by Leidy on characters of taxonomic status and paleozoogeographic implications related teeth presumably from the Calvert Formation of Virginia (late to the Lee Creek Mine occurrence and to occurrences of early to early middle Miocene), but the species is now validated by skulls and numerous elements from the middle Miocene forma- closely related forms elsewhere. tions of the Chesapeake Group. The same form is common in the ACKNOWLEDGMENTS.•The Lee Creek Mine specimens cit- Florida early Pliocene, where it is represented by several fairly ed in this report were collected and donated by P.J. Harmatuk, complete skeletons known as Gavialosuchus americanus (Sell- F. Hyne, and B. Hyne. I thank L.G. Barnes (Los Angeles arás). It also is known from numerous skulls from early and mid- County Museum of Natural History) for providing refresher dle Miocene formations near Lisbon, Portugal, as Tomistoma lusitanica (Vianna and Moraes). Teeth and a dermal scute indicat- information on the California specimens.
    [Show full text]
  • (Squamata: Mosasauridae) from the Late Cretaceous Of
    C. R. Palevol 14 (2015) 483–493 Contents lists available at ScienceDirect Comptes Rendus Palevol www.sci encedirect.com General Palaeontology, Systematics and Evolution (Vertebrate Palaeontology) An halisaurine (Squamata: Mosasauridae) from the Late Cretaceous of Patagonia, with a preserved tympanic disc: Insights into the mosasaur middle ear Un halisauriné (Squamata : Mosasauridae) du Crétacé supérieur de Patagonie, à disque tympanique conservé : un aperc¸ u de l’oreille moyenne des mosasaures a,∗ b Marta S. Fernández , Marianella Talevi a CONICET - División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentina b CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Isidro Lobo y Belgrano, 8332 General Roca, Río Negro, Argentina a b s t r a c t a r t i c l e i n f o Article history: Halisaurinae is a subfamily of enigmatic, small- to medium-sized mosasauroids, which Received 15 September 2014 retain a mosaic of primitive and derived features. The first record of a South American Hal- Accepted after revision 13 May 2015 isaurus with precise stratigraphic information includes a quadrate carrying a tympanic disc together with twelve vertebrae, collected in the Late Maastrichtian of Jagüel Formation Handled by Nathalie Bardet in northern Patagonia (Argentina). The preservation of a tympanic disc allows exploring and discussing the mechanisms of sound transmission in these mosasauroids. The loca- Keywords: tion of the tympanic disc resembles that one formed by the extracolumella of aquatic Halisaurus turtles and at least one extant lizard. Based on morphological comparison of the middle Patagonia ear we discuss previous hypotheses on the modification of the tympanic middle ear system Late Maastrichtian of mosasauroids for underwater hearing, in a manner similar to that observed in aquatic Cretaceous turtles.
    [Show full text]
  • View Preprint
    A peer-reviewed version of this preprint was published in PeerJ on 11 June 2018. View the peer-reviewed version (peerj.com/articles/4973), which is the preferred citable publication unless you specifically need to cite this preprint. Brownstein CD. 2018. Trace fossils on dinosaur bones reveal ecosystem dynamics along the coast of eastern North America during the latest Cretaceous. PeerJ 6:e4973 https://doi.org/10.7717/peerj.4973 Theropod hindlimbs with feeding and other traces reveal ecosystem dynamics in the Maastrichtian of eastern North America Chase Brownstein Corresp. Corresponding Author: Chase Brownstein Email address: [email protected] Direct documentation of the ecology of past life is often rare when the fossil record is comparatively poor, as in the case of the terrestrial fauna of the Maastrichtian of eastern North America. Here, I describe a femur and partial tibia shaft assignable to theropods from the Maastrichtian Big Brook locality of New Jersey. The former, identifiable to a previously undetected morphotype of large ornithomimosaur, bears several scrapes identifiable as the feeding traces of sharks, adding to the collection of terrestrial vertebrate remains bearing such marks from the state. The latter is littered with tooth marks and punctures from possibly multiple crocodyliform individuals, the first documented occurrence of such traces on dinosaur bone from the Maastrichtian of the Atlantic Coastal Plain. Additionally, its surface is dotted with likely traces of invertebrates, revealing a microcosm of biological interaction from the Maastrichtian New Jersey shoreline. Previously, the massive Campanian crocodylian taxon Deinosuchus rugosus and the slightly smaller Cenomanian-age Texas crocodyliform Deltasuchus motherali have been shown as important drivers of terrestrial vertebrate taphonomy in eastern North America.
    [Show full text]
  • Phylogenetic Taphonomy: a Statistical and Phylogenetic
    Drumheller and Brochu | 1 1 PHYLOGENETIC TAPHONOMY: A STATISTICAL AND PHYLOGENETIC 2 APPROACH FOR EXPLORING TAPHONOMIC PATTERNS IN THE FOSSIL 3 RECORD USING CROCODYLIANS 4 STEPHANIE K. DRUMHELLER1, CHRISTOPHER A. BROCHU2 5 1. Department of Earth and Planetary Sciences, The University of Tennessee, Knoxville, 6 Tennessee, 37996, U.S.A. 7 2. Department of Earth and Environmental Sciences, The University of Iowa, Iowa City, Iowa, 8 52242, U.S.A. 9 email: [email protected] 10 RRH: CROCODYLIAN BITE MARKS IN PHYLOGENETIC CONTEXT 11 LRH: DRUMHELLER AND BROCHU Drumheller and Brochu | 2 12 ABSTRACT 13 Actualistic observations form the basis of many taphonomic studies in paleontology. 14However, surveys limited by environment or taxon may not be applicable far beyond the bounds 15of the initial observations. Even when multiple studies exploring the potential variety within a 16taphonomic process exist, quantitative methods for comparing these datasets in order to identify 17larger scale patterns have been understudied. This research uses modern bite marks collected 18from 21 of the 23 generally recognized species of extant Crocodylia to explore statistical and 19phylogenetic methods of synthesizing taphonomic datasets. Bite marks were identified, and 20specimens were then coded for presence or absence of different mark morphotypes. Attempts to 21find statistical correlation between trace types, marking animal vital statistics, and sample 22collection protocol were unsuccessful. Mapping bite mark character states on a eusuchian 23phylogeny successfully predicted the presence of known diagnostic, bisected marks in extinct 24taxa. Predictions for clades that may have created multiple subscores, striated marks, and 25extensive crushing were also generated. Inclusion of fossil bite marks which have been positively 26associated with extinct species allow this method to be projected beyond the crown group.
    [Show full text]
  • An Eocene Tomistomine from Peninsular Thailand Jérémy Martin, Komsorn Lauprasert, Haiyan Tong, Varavudh Suteethorn, Eric Buffetaut
    An Eocene tomistomine from peninsular Thailand Jérémy Martin, Komsorn Lauprasert, Haiyan Tong, Varavudh Suteethorn, Eric Buffetaut To cite this version: Jérémy Martin, Komsorn Lauprasert, Haiyan Tong, Varavudh Suteethorn, Eric Buffetaut. An Eocene tomistomine from peninsular Thailand. Annales de Paléontologie, Elsevier Masson, 2019, 10.1016/j.annpal.2019.03.002. hal-02121886 HAL Id: hal-02121886 https://hal.archives-ouvertes.fr/hal-02121886 Submitted on 6 May 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. An Eocene tomistomine from peninsular Thailand Un tomistominé éocène de la peninsule Thaïlandaise Jeremy E. Martin1, Komsorn Lauprasert2, Haiyan Tong2, Varavudh Suteethorn2 and Eric Buffetaut3 1Laboratoire de Géologie de Lyon: Terre, Planète et Environnement, UMR CNRS 5276 (CNRS, ENS, Université Lyon 1), Ecole Normale Supérieure de Lyon, 69364 Lyon Cedex 07, France, email: [email protected] 2Palaeontological Research and Education Centre, Mahasarakham University, Khamrieng, 44150 Thailand 3Laboratoire de Géologie de l’Ecole Normale Supérieure, CNRS (UMR 8538), 24 rue Lhomond, Paris Cedex 05, 75231, France Abstract Skull and mandibular elements of a tomistomine crocodilian are described from the late Eocene to early Oligocene lignite seams of Krabi, peninsular Thailand.
    [Show full text]
  • Joint Loading Configurations Inferred from Propagation Paths
    Journal of Structural Geology 21 (1999) 1637±1652 www.elsevier.nl/locate/jstrugeo Joint interaction with embedded concretions: joint loading con®gurations inferred from propagation paths David T. McConaughy 1, Terry Engelder* Department of Geosciences, The Pennsylvania State University, University Park, PA 16802, USA Received 16 December 1997; accepted 18 May 1999 Abstract The interaction between propagating joints and embedded concretions in a Devonian black shale near Seneca Lake, NY, permits identi®cation of the loading con®gurations responsible for two joint sets of dierent ages striking at nearly the same orientation. The earlier set consists of systematic joints cut by later Alleghanian joints of the Appalachian Plateau. The later set consists of non-systematic curving cross joints that abut these same Alleghanian joints. Field evidence shows that concretions functioned as sti inclusions in a compliant black shale. As a consequence of this elastic contrast, local perturbations in the remote stress ®eld persisted around the concretions during burial, tectonic deformation, and exhumation. These stress perturbations in¯uenced joint propagation paths of both joint sets. Our conclusions about loading con®gurations are based on ®nite-element modeling of the eect of the local stress perturbation on concretion-modi®ed joint propagation. Modeling shows that the local stress perturbation from a thermoelastic loading was responsible for de¯ecting cross joints away from concretions in a curved propagation path near the concretion. This load con®guration also led to arrest of cross joints before they penetrated the shale±concretion interface. At greater distances from the concretion, the propagation path of cross joints was controlled by the contemporary tectonic stress ®eld.
    [Show full text]
  • Unraveling the Central Appalachian Fold-Thrust Belt, Pennsylvania: the Power of Sequentially Restored Balanced Cross Sections for a Blind Fold-Thrust Belt
    Unraveling the central Appalachian fold-thrust belt, Pennsylvania: The power of sequentially restored balanced cross sections for a blind fold-thrust belt Peter B. Sak1, Nadine McQuarrie2,*, Benjamin P. Oliver2,*, Natasha Lavdovsky2, and Margaret S. Jackson1,* 1Department of Earth Sciences, Dickinson College, Carlisle, Pennsylvania 17013, USA 2Department of Geosciences, Princeton University, Princeton, New Jersey 08540, USA ABSTRACT Anticlinorium, the northernmost structure of example of a blind thrust system. At its north- the fold-thrust belt that cuts upsection from ernmost end, the fold-thrust belt sweeps east- We present a kinematic model for the the Cambrian Waynesboro Formation to the ward, creating the broad arc of the Pennsylvania sequential development of the Appalachian Silurian Salina décollement. Because the fault salient (Fig. 1). Although previous research in fold-thrust belt (eastern U.S.) across a clas- that cores the Nittany Anticlinorium can only the central Appalachians has made considerable sic transect through the Pennsylvania salient. facilitate 10 km of shortening on the plateau, progress toward quantifying how shortening New map and strain data are used to create an early history of Appalachian Plateau LPS is distributed among microscopic (e.g., Smart a balanced geologic cross section from the in Silurian and younger rocks is required to et al., 1997; Thorbjornsen and Dunne, 1997), southern edge of the Valley and Ridge Prov- balance the section. We propose that the addi- mesoscopic (e.g., Smart et al., 1997; Hogan
    [Show full text]
  • Who's Got the Biggest?
    WHO’S GOT THE BIGGEST? Rom Whitaker and Nik Whitaker [Adapted by inclusion of additional images from article in Crocodile Specialist Group Newsletter 27(4): 26-30] The fascination for ‘fi nding the biggest’ is deeply engrained, and when fi lm producer Harry Marshall at Icon Films (UK) offered a chance to search for the world’s largest crocodilian - who could refuse? Claims of giant crocodiles are as wild as those for outsize fi sh and snakes. “It was longer than the boat”, has been earnestly related in a dozen languages, from the Rift Valley lakes of Figure 2. Alistair Graham with skull of 6.2 m (20’) long C. Ethiopia to the mighty Fly River in Papua New Guinea. And porosus from the Fly River, Papua New Guinea (see Fig. the Fly River is where this ‘skull quest’ (for that’s what it’s 1). Photograph: Rom Whitaker. become) began. Largest Crocodile with Photographic Documentation The note that Jerome published on this fi nd (Montague 1983) didn’t exactly shake the world. People were (and still are) quite In 1980 I (RW) was working for the United Nations crocodile convinced that C. porosus well over 20’ long are on record. program in Papua New Guinea as ‘Production Manager’; the But when the quest for the biggest started to get serious, it second author (NW) was also there, see illustration. Along was soon obvious that these ‘records’ are mostly anecdotes with UN volunteer Jerome Montague, also a biologist, we with no solid evidence. Some colleagues are ready to accept went off on patrol down the Fly River, checking on the anecdotal total lengths - we are much more skeptical.
    [Show full text]
  • Hunt-Et-Al-2017.Pdf
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/319237612 Sexual dimorphism and sexual selection in cytheroidean ostracodes from the Late Cretaceous of the U.S. Coastal Plain Article in Paleobiology · August 2017 DOI: 10.1017/pab.2017.19 CITATION READS 1 107 7 authors, including: Gene Hunt Maria João Fernandes Martins Smithsonian Institution Smithsonian Institution 94 PUBLICATIONS 1,829 CITATIONS 27 PUBLICATIONS 242 CITATIONS SEE PROFILE SEE PROFILE Mark Puckett Rowan Lockwood University of Southern Mississippi College of William and Mary 38 PUBLICATIONS 366 CITATIONS 40 PUBLICATIONS 812 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Taxonomy, paleoecology and biostratigraphy of ostracodes from the Riachuelo Formation, Sergipe-Alagoas Basin, northeastern Brazil View project Dinosaur body-size evolution View project All content following this page was uploaded by Mark Puckett on 18 October 2017. The user has requested enhancement of the downloaded file. Paleobiology, page 1 of 22 DOI: 10.1017/pab.2017.19 Sexual dimorphism and sexual selection in cytheroidean ostracodes from the Late Cretaceous of the U.S. Coastal Plain Gene Hunt, M. João Fernandes Martins, T. Markham Puckett, Rowan Lockwood, John P. Swaddle, Christine M. S. Hall, and James Stedman Abstract.—Sexual dimorphism is common in many extant animals, but it is difficult to demonstrate in fossil species. Working with material from the Late Cretaceous of the U.S. Coastal Plain, we herein analyze sexual dimorphism in ostracodes from the superfamily Cytheroidea, a group whose extant members have males that are relatively more elongate than females.
    [Show full text]
  • Significance of the Deformation History Within the Hinge Zone of the Pennsylvania Salient, Appalachian Mountains
    Bucknell University Bucknell Digital Commons Faculty Journal Articles Faculty Scholarship 2014 Significance of the Deformation History within the Hinge Zone of the Pennsylvania Salient, Appalachian Mountains Mary Beth Gray Bucknell University, [email protected] Peter B. Sak [email protected] Zeshan Ismat Follow this and additional works at: https://digitalcommons.bucknell.edu/fac_journ Part of the Tectonics and Structure Commons Recommended Citation Sak, P.B., Gray, M.B., and Ismat, Z., 2014, Significance of the Juniata culmination in the deformation history of the Pennsylvania salient, Appalachian Mountains. Journal of Geology 122, 367-380 This Article is brought to you for free and open access by the Faculty Scholarship at Bucknell Digital Commons. It has been accepted for inclusion in Faculty Journal Articles by an authorized administrator of Bucknell Digital Commons. For more information, please contact [email protected]. Significance of the Deformation History within the Hinge Zone of the Pennsylvania Salient, Appalachian Mountains Peter B. Sak,1,* Mary Beth Gray,2 and Zeshan Ismat3 1. Department of Earth Sciences, Dickinson College, Carlisle, Pennsylvania 17013, USA; 2. Department of Geology, Bucknell University, Lewisburg, Pennsylvania 17837, USA; 3. Department of Earth and Environment, Franklin and Marshall College, Lancaster, Pennsylvania 17603, USA ABSTRACT Two competing models exist for the formation of the Pennsylvania salient, a widely studied area of pronounced curvature in the Appalachian mountain belt. The viability of these models can be tested by compiling and analyzing the patterns of structures within the general hinge zone of the Pennsylvania salient. One end-member model suggests a NW-directed maximum shortening direction and no rotation through time in the culmination.
    [Show full text]
  • THE BIBLIOGRAPHY of HADROSAURIAN DINOSAURS the First 150 Years: 1856 - 2006
    THE BIBLIOGRAPHY OF HADROSAURIAN DINOSAURS The First 150 Years: 1856 - 2006. complied by M.K. Brett-Surman © Smithsonian Institution 1985-2008 The Department of Paleobiology of the National Museum of Natural History, Smithsonian Institution, currently houses approximately 44 million fossil plant, invertebrate, and vertebrate fossils in more than 480 separate collections. In addition, Paleobiology also maintains a reference collection of over 120,000 stratigraphic and sediment samples. This listing represents a service provided to the public as part of our Outreach Program and as part of the Smithsonian Institution’s mission "for the increase and diffusion of knowledge...". Papers are listed by author and year. Author's names are capitalized. The viewer should be aware of any searches that are case sensitive. The papers listed here, in a majority of instances, do NOT contain abstracts, papers on ichnites, or popular articles or books, unless they present new information or cover an aspect of the history of dinosaur paleontology. At present, some of the legacy software that was used to maintain this list only allowed basic ASCII characters, therefore foreign accents (such as in French and Spanish) did not translate. This will be fixed at a later date. The Bibliography of Hadrosaurian Dinosaurs was written, compiled, and maintained by M.K. Brett-Surman, (Museum Specialist), P.O. Box 37012, Department of Paleobiology, National Museum of Natural History, MRC-121, Washington, DC 20013-7012. He can be reached electronically at: [email protected]., and by FAX at 202-786-2832. Please send all corrections and additions to the e-mail address. This file will be no longer be updated, except for entries prior to 2007.
    [Show full text]