Handbook of Texas Cretaceous Fossils
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Les Vascoceratinae Et Les Pseudotissotiinae
LES VASCOCERATINAE ET LES PSEUDOTISSOTIINAE (AMMONITINA) D'ASHAKA (NE NIGERIA) : RELATIONS AVEC LEUR ENVIRONNEMENT BIOSÉDIMENTAIRE THE VASCOCERATINAEA AND PSEUDOTISSOTIINAEA (AMMONITINA) FROM ASHAKA (NE NIGERIA) : RELATIONSHIPS WlTH THE BIOSEDIMENTARY ENVIRONMENT Philippe COURVILLE COURVILLE Ph. (1992) - Les Vascoceratnae et es Pseudotssotinae (Ammonitina) d'Açhaka (NE Ngera) . relatons avec leur enviannement blosedimentare [The Vaçcoceia1,naea and Psetidotfssoti!naea jAmmon,ti.?s) fiom As,ba,ks (NE Nigeria) relationsh!ps with the biosedimentary enviionment] - Bull. Centres Rech Explof.- Prod EliAquitaine. 16. 2 407~457.8 f~y, 14 p.. Bo~ssensDecember 24, 19'32 - SSN : 0396~2687 CODEN. BCREDP A purdscpnary analyss groupng the sedtmentary yeo,ogy, the sequenta! stratgraphy. !he mcropaleonto1og;cal and nacropaeontologcal aspec!s. allows us 10 renterpret tbe marine çecton of the Gonga Formaton (hypostratotypc Ashaka sect~on).The paleartolag~cal successlonç (benthon~carganiçtrç and Ammonlte papulatons) and the sedmentary unis (ensembles mted by two d!scontinutes) cari now oe deçcrbed accurateiy A dynamc nterpretator of the seres of Ammonte papulatons s proposed for the local framework of the Ashaka ste some taxa coud beong to .. autochthonous ,, neages (Vascoceratnae and Pseudotsçatnae) others are corsdered ta be ., exo~ ric ,. elements (Fagesra and Pseodaspidoceras) The settements of the Cer,omanan and Turonan marne envronments seem to be w~th~na few steps reach. Fi'çt of a. tïe progreçslve settng of subplatycone 01 paty~spheroconetethysan Vascoceratds (Nigeiiceras and V gr cauv!ni) can be obçerved Ths ç folowed by the suaden .. appearance .. of cad-serperllcone Ammontes, whch quicky dr~fttowards cad-spherocone forms (frst morphologcal c:sls) Then a second morpnolagica crlsls occurç. -
New Species, Corallivory, in Situ Video Observations and Overview of the Goniasteridae (Valvatida, Asteroidea) in the Hawaiian Region
Zootaxa 3926 (2): 211–228 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2015 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3926.2.3 http://zoobank.org/urn:lsid:zoobank.org:pub:39FE0179-9D06-4FC2-9465-CE69D79B933F New species, corallivory, in situ video observations and overview of the Goniasteridae (Valvatida, Asteroidea) in the Hawaiian Region CHRISTOPHER L. MAH Dept. of Invertebrate Zoology, Smithsonian Institution, Washington, D.C. 20007 Abstract Two new species of Goniasteridae, Astroceramus eldredgei n. sp. and Apollonaster kelleyi n. sp. are described from the Hawaiian Islands region. Prior to this occurrence, Apollonaster was known only from the North Atlantic. The Goniasteri- dae is the most diverse family of asteroids in the Hawaiian region. Additional in situ observations of several goniasterid species, including A. eldredgei n. sp. are reported. These observations extend documentation of deep-sea corallivory among goniasterid asteroids. New species occurrences presented herein suggested further biogeographic affinities be- tween tropical Pacific and Atlantic goniasterid faunas. Key words: Goniasteridae, Valvatida, deep-sea, Hawaiian Islands, predation Introduction Recent discoveries of new genera and species from deep-sea habitats along with new in situ video observations have provided us with new ecological insight into these poorly understood and formerly inaccessible settings (e.g., Mah et al. 2010, 2014; Mah & Foltz 2014). Hawaiian deep-sea Asteroidea are taxonomically diverse and occur in an active area of oceanographic and biological research (Chave and Malahoff 1998). New data on asteroids in this area presents an opportunity to review and highlight this diverse fauna. -
Chapter 307: Texas Surface Water Quality Standards (4/9/2008)
Revisions to §307 - Texas Surface Water Quality Standards (updated November 12, 2009) EPA has not approved the revised definition of “surface water in the state” in the TX WQS, which includes an area out 10.36 miles into the Gulf of Mexico. Under the CWA, Texas does not have jurisdiction to regulate water standards more than three miles from the coast. Therefore, EPA’s approval of the items in the enclosure recognizes the state’s authority under the CWA out to three miles in the Gulf of Mexico, but does not extend past that point. Beyond three miles, EPA retains authority for CWA purposes EPA’s approval also does not include the application the TX WQS for the portions of the Red River and Lake Texoma that are located within the state of Oklahoma. Finally, EPA is not approving the TX WQS for those waters or portions of waters located in Indian Country, as defined in 18 U.S.C. 1151. The following sections have been approved by EPA and are therefore effective for CWA purposes: • §307.1. General Policy Statement • §307.2. Description of Standards • §307.3. Definitions and Abbreviations (see item under “no action” section below) • §307.4. General Criteria • §307.5. Antidegradation • §307.6. Toxic Materials. (see item under “no action” section below) • §307.7. Site-specific Uses and Criteria (see item under “no action” section below) • §307.8. Application of Standards • §307.9. Determination of Standards Attainment • Appendix C - Segment Descriptions • Appendix D - Site-specific Receiving Water Assessments The following sections have been partially approved by EPA: • Appendix A. -
Natural Communities of Michigan: Classification and Description
Natural Communities of Michigan: Classification and Description Prepared by: Michael A. Kost, Dennis A. Albert, Joshua G. Cohen, Bradford S. Slaughter, Rebecca K. Schillo, Christopher R. Weber, and Kim A. Chapman Michigan Natural Features Inventory P.O. Box 13036 Lansing, MI 48901-3036 For: Michigan Department of Natural Resources Wildlife Division and Forest, Mineral and Fire Management Division September 30, 2007 Report Number 2007-21 Version 1.2 Last Updated: July 9, 2010 Suggested Citation: Kost, M.A., D.A. Albert, J.G. Cohen, B.S. Slaughter, R.K. Schillo, C.R. Weber, and K.A. Chapman. 2007. Natural Communities of Michigan: Classification and Description. Michigan Natural Features Inventory, Report Number 2007-21, Lansing, MI. 314 pp. Copyright 2007 Michigan State University Board of Trustees. Michigan State University Extension programs and materials are open to all without regard to race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, marital status or family status. Cover photos: Top left, Dry Sand Prairie at Indian Lake, Newaygo County (M. Kost); top right, Limestone Bedrock Lakeshore, Summer Island, Delta County (J. Cohen); lower left, Muskeg, Luce County (J. Cohen); and lower right, Mesic Northern Forest as a matrix natural community, Porcupine Mountains Wilderness State Park, Ontonagon County (M. Kost). Acknowledgements We thank the Michigan Department of Natural Resources Wildlife Division and Forest, Mineral, and Fire Management Division for funding this effort to classify and describe the natural communities of Michigan. This work relied heavily on data collected by many present and former Michigan Natural Features Inventory (MNFI) field scientists and collaborators, including members of the Michigan Natural Areas Council. -
Late Cretaceous-Early Palaeogene Echinoderms and the K/T Boundary in the Southeast Netherlands and Northeast Belgium — Part 6: Conclusions
pp 507-580 15-01-2007 14:51 Pagina 505 Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 6: Conclusions John W.M. Jagt Jagt, J.W.M. Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 6: Conclusions. — Scripta Geol., 121: 505-577, 8 figs., 9 tables, Leiden, December 2000. John W.M. Jagt, Natuurhistorisch Museum Maastricht, Postbus 882, NL-6200 AW Maastricht, The Netherlands, E-mail: [email protected] Key words: Echinodermata, Late Cretaceous, Early Palaeogene, palaeobiology, K/T boundary, extinc- tion. The palaeobiology of echinoderms occurring in the Meerssen and Geulhem members is discussed and changes in diversity across the K/T boundary are documented. Using literature data on the ecology of extant faunas, the various echinoderm groups are considered. Naturally, such data can only be applied with due caution to fossil forms, whose skeletal morphology is often incompletely known. This holds especially true for asteroids, ophiuroids, and crinoids, which, upon death, rapidly disinte- grate into jumbles of dissociated ossicles. Bioturbation, scavenging, and current winnowing all con- tribute to blurring the picture still further. However, data on extant forms do allow a preliminary sub- division of fossil species into various ecological groups, which are discussed herein. Combining recently published data on K/T boundary sections in Jylland and Sjælland (Denmark) with the pic- ture drawn here for the Maastricht area results in the following best constrained scenario. The demise of the highly diverse latest Maastrichtian echinoderm faunas, typical of shallow-water settings with local palaeorelief and associated unconsolidated bottoms, was rapid, suggestive of a catastrophic event (e.g. -
Starfish Saponins, 19
3 266 STARFISH SAPONINS, 19. ‘ A NOVEL STEROIDAL GLYCOSIDE SULFATE FROM THE STARFISHES PROTOREASTER NODOSUS AND PENTACERASTER ALVEOLATUS2 RAFFAELERICCIO, FRANCO ZOLLO, ESTERFINAMORE, LUIGIhfINALE* Dipartitnetlin di CbitnicL~dtlle Sostanze ì%ttirali, Uiiivcrsiiù~ Via L. Rodimi 22. 80138 Napoli, Itufy. ---DOhïINImE3T, - GEORGESBAKGIB ANT, Cetitre ORSTOM, BP AS, Noimia, Ntw Cdrdoniu and JACQUE PUSSET Laboratoire dus Plunta h.Ii&irzalus, CNRS, B P 643, Not~t~éa,Neu, Cal&niLr ABSTRACT.-A new sulfated asterosaponin (l),containing the unprecedented (20R,22S)- Sa-cholesta-9(1 l), 24(25)-diene-3ß,Ga 20,22-tetraol aglycone, has been isolated from the Pacific starfishes Platmastw tiodosus and Pmtawu.ster alceolntm. The sulfate residue is at C-3 and the oligosaccharide chain, ß-D-fucopyranosyl(11+2)-ß-D-quinovopyranosyl(l++4) [-ß-D- quinovopyranosyl( 11+2)1-ß-D-xylopyranosyl( 1~3)-ß-D-quinovopyranosyl,is at C-6. We have reported previously the occurrence of a novel type of steroidal glycoside, nodososide, (24S)-24-0-E2-0-methyl-ß-D-xylopyranosyl-(1~2)-a-L-arabino-furano- syl)-5a-cholestane-3ß, 5,6ß,8,15a,24-hexol, along with several polyhydroxylated sterols, from the Pacific starfish Protoreaster nodosils L. (order Phanerozonia, family Oreasteridae) (1-3). We have now examined the more polar components and have iso- lated a new sulfated asterosaponin (11, which we named protoreasteroside, along with R -13 & H OH 2 R= ‘v ’For Part 18, seel Nat Pivd , 48, 97 1985) of the Progetto Finalizzato “Chimica Fine e Secondana” del GN O 10001373 thte g - -. - - - OH 1 268 Journal of Natural Products {Vol. -
Classification of Ammonitic Sutures Using Gis
Palaeontologia Electronica http://palaeo-electronica.org PATTERN MATCHING: CLASSIFICATION OF AMMONITIC SUTURES USING GIS Lori L. Manship ABSTRACT Geographic Information Systems (GIS) is utilized to apply spatial analysis tech- niques to visually and quantitatively match ammonoid suture patterns for classification. The Turonian ammonite family Coilopoceratidae was chosen as the basis for this project, because the similar suture patterns within the family make species-level identi- fication a challenge. A Coilopoceras springeri suture template was created by overlay- ing 10 different Coilopoceras springeri suture patterns, using the right holotype suture pattern as the basal or designation guide. Templates for Coilopoceras colleti and Hopli- toides sandovalensis sutures were constructed in the same manner. Sutures of known and unknown specimens were tested within the templates in order to identify species. The sutures of known specimens matched with the correct templates and did not com- pare well with other species’ templates. Sutures of unknown specimens clearly fit within one template better than within others and, hence, could be reliably classified to the species level. In addition to species classification, the GIS method provides a mechanism for both visual and quantitative comparisons of individual sutures. This GIS method will aid professional and avocational paleontologists, biostratigraphers, and geologists in classifying ammonite species, and may help further our understanding of suture morphogenesis and function by providing a standard basis for morphological comparison of complex sutural patterns. Department of Geosciences, Texas Tech University, Lubbock, Texas, 79409-1053, USA. [email protected] KEY WORDS: ammonite; Geographic Information Systems (GIS); suture pattern; Turonian; Cretaceous PE Article Number: 7.2.5A Copyright: Paleontological Society. -
12. Lower Cretaceous Ammonites from the South Atlantic Leg 40 (Dsdp), Their Stratigraphic Value and Sedimentologic Properties
12. LOWER CRETACEOUS AMMONITES FROM THE SOUTH ATLANTIC LEG 40 (DSDP), THEIR STRATIGRAPHIC VALUE AND SEDIMENTOLOGIC PROPERTIES Jost Wiedmann and Joachim Neugebauer, Geol.-palaont. Institut der Universitat Tubingen, BRD ABSTRACT Eleven ammonites have been cored during Leg 40. They were found concentrated in the lower parts of the drilled section at Sites 363 (Walvis Ridge) and 364 (Angola Basin), and permit recognition of upper Albian, middle Albian, and upper Aptian. So far, no lower Albian could be recognized. A high ammonite density can be assumed for the South Atlantic Mid-Cretaceous. In contrast to data available so far, the Walvis Ridge associations consisting of phylloceratids and desmoceratids show more open- basin relationships than those of the Angola Basin, which are composed of mortoniceratids, desmoceratids, and heteromorphs. Paleobiogeographically, the South Atlantic fauna can be related to the well-known onshore faunas of Angola, South Africa, and Madagascar as well as to the European Mid-Cretaceous. This means that the opening of the South Atlantic and its connection with the North Atlantic occurred earlier as was generally presumed, i.e., in the middle Albian. Records of lower Aptian ammonite faunas from Gabon and Brazil remain doubtful. High rates of sedimentation prevailed especially in the Aptian and Albian, in connection with the early deepening of the South Atlantic basins. The mode of preservation of the ammonites suggests that they were deposited on the outer shelf or on the upper continental slope and were predominantly buried under sediments of slightly reducing conditions. In spite of a certain variability of the depositional environment, the ammonites show a uniform and particular mode of preservation. -
Field Summary Report Mapping Conventions for Texas PI and Draft
.. ,Field summary Report-Mapping Conventions for Texas PI and Draft Project Date of field trip: 1/12-1/16/87 Personnel: Warren Hagenbuck USFWS Curtis Carley USFWS Frank Spague SCS Frank J. sargent Martel Lynn Ashby Hartel 1:100,000 Hap Names: Sherman NW (16 quads), SW; Dallas NW, SW Co~lateral Data: USGS topographical quads- 1:24,100, 1:250,000 SOil survey for all maps where available. Rainfall data for all maps where available. Photography The CrR photography being used is produced by NHAP at a scale of 1:58,000 with flight dates of.september to December 1981. The quality \. is good for both resolution and emulsion. Climate conditions at the time of photography appear to be typical. All photo signatures reviewed during field reconnaissance reflect emulsion and resolution qualities consistently throughout the project area. ".Ecoregion and Physiography '. The project area is located· primarily within the Prairie Parkland Province, oak-Bluestem Sec-l:ion. This region is characterized by 23" to 40" of precipitation annually-with yearly average temperatures between e 47-F-83 F. ~he topography of the maps' northern and eastern sections are comprised of irregular plains (gently rolling) wiu{ relief upwards of 100-300 feet. In the remaining western half of the work area the relief may vary from 300-500 feet with tableland features. Within this western section , in the very southwest corner of Dallas SW, is the Prairie Bushland Province, Juniper-Oak-MesquitJ Section. / The Prairie Bushland Province also has an ar~a of irregUlar plains, yet the relief is 300-500' in elevation. -
Upper Cretaceous Crustacea from Mexico and Colombia: Similar Faunas and Environments During Turonian Times
Revista Mexicana de Ciencias Geológicas, Turonianv. 24, núm. Crustacea 3, 2007, p.from 403-422 Mexico and Colombia 403 Upper Cretaceous Crustacea from Mexico and Colombia: similar faunas and environments during Turonian times Francisco J. Vega1,*, Torrey Nyborg2, Alexis Rojas-Briceño3, Pedro Patarroyo3, Javier Luque4, Héctor Porras-Múzquiz5, and Wolfgang Stinnesbeck6 1 Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, Coyoacán, 04510 México, D.F., Mexico. 2 Department of of Earth and Biological Sciences, Loma Linda University, Loma Linda CA, 92350, USA. 3 Departamento de Geociencias, Universidad Nacional de Colombia, A. A. 14490, Bogotá, Colombia. 4 Smithsonian Tropical Research Institute. Apartado Postal 0843-03092, Balboa, Ancon, Panama. 5 Museo de Múzquiz A. C., Zaragoza 209, 26340, Múzquiz, Coahuila, Mexico. 6 Geologisch-Paläontologisches Institut, Im Neuenheimer Feld 234, 69120 Heidelberg, Germany. * [email protected] ABSTRACT Nine taxa represent the crustacean component of the Turonian fauna from the Eagle Ford Group limestones and marls that crop out in several quarries, northwest of Múzquiz, Coahuila, Mexico. Three crustacean taxa are found in common with deposits of similar age and paleoenvironment of the San Rafael Formation of Colombia. Planktic foraminifera, ammonoids, inoceramid bivalves, shes, marine reptiles, a pterosaur and plant remains were preserved in the Múzquiz quarries, in what has been interpreted as an anoxic, low energy bottom at a water depth of no less than 50 m. The cirriped Stramentum preserved on the ammonite Forresteria is described. Stomatopod remains of the family Pseudosculdidae are described, their incompleteness and poor preservation prevent their detailed identi cation. One species of scyllarid lobster is included. -
Phylogeny, Diversity, and Ecology of the Ammonoid Superfamily Acanthoceratoidea Through the Cenomanian and Turonian
PHYLOGENY, DIVERSITY, AND ECOLOGY OF THE AMMONOID SUPERFAMILY ACANTHOCERATOIDEA THROUGH THE CENOMANIAN AND TURONIAN DAVID A.A. MERTZ A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE August 2017 Committee: Margaret Yacobucci, Advisor Andrew Gregory Keith Mann © 2017 David Mertz All Rights Reserved iii ABSTRACT Margaret Yacobucci Both increased extinction and decreased origination, caused by rising oceanic anoxia and decreased provincialism, respectively, have been proposed as the cause of the Cenomanian Turonian (C/T) extinction event for ammonoids. Conflicting evidence exists for whether diversity actually dropped across the C/T. This study used the ammonoid superfamily Acanthoceratoidea as a proxy for ammonoids as a whole, particularly focusing on genera found in the Western Interior Seaway (WIS) of North America, including Texas. Ultimately, this study set out to determine 1) whether standing diversity decreased across the C/T boundary in the WIS, 2) whether decreased speciation or increased extinction in ammonoids led to a drop in diversity in the C/T extinction event, 3) how ecology of acanthoceratoid genera changed in relation to the C/T extinction event, and 4) whether these ecological changes indicate rising anoxia as the cause of the extinction. In answering these questions, three phylogenetic analyses were run that recovered the families Acanthoceratidae, Collignoniceratidae, and Vascoceratidae. Pseudotissotiidae was not recovered at all, while Coilopoceratidae was recovered but reclassified as a subfamily of Vascoceratidae. Seven genera were reclassified into new families and one genus into a new subfamily. After calibrating the trees with stratigraphy, I was able to determine that standing diversity dropped modestly across the C/T boundary and the Early/Middle Turonian boundary. -
Mid-Cretaceous Ammonite Sequence for Western New Mexico Iv
iii Contents ABSTRACT 5 Genus Morrowites Cobban and Hook, n. gen. 9 Morrowites wingi (Morrow) 9 INTRODUCTION 5 M. depressus (Powell) 11 COMPOSITION OF MOLLUSCAN FAUNA 5 M. subdepressus Cobban and Hook, n. sp. 11 OCCURRENCE AND PRESERVATION OF FOSSILS 6 M. cf. M. dixeyi (Reyment) 12 STRATIGRAPHIC POSITION OF FOSSILS 6 Subfamily Euomphaloceratinae Cooper 13 COLLECTION LOCALITIES 7 Genus Kamerunoceras Reyment 13 Kamerunoceras turoniense (d'Orbigny) 13 FAMILY VASCOCERATIDAE H. Douvillé 14 SYSTEMATIC PALEONTOLOGY 7 Subfamily Vascoceratinae H. Douvillé 14 FAMILY BACULITIDAE GILL 7 Genus Neoptychites Kossmat 14 Genus Baculites Lamarck 7 Neoptychites cephalotus (Courtiller) 14 Baculites yokoyamai Tokunaga and Shimizu 7 Genus Fagesia Pervinquière 15 FAMILY MUNIERICERATIDAE WRIGHT 7 Fagesia superstes (Kossmat) 16 Genus Tragodesmoceras Spath 7 FAMILY C OLLIGNONICERATIDAE WRIGHT AND WRIGHT 16 Tragodesmoceras socorroense Cobban and Hook 7 Subfamily Barroisiceratinae Basse 16 FAMILY PLACENTICERATIDAE HYATT 8 Genus Cibolaites Cobban and Hook, n. gen. 16 Genus Placenticeras Spath 8 Cibolaites molenaari Cobban and Hook, n. sp. 16 Placenticeras cumminsi Cragin 8 REFERENCES 18 FAMILY ACANTHOCERATIDAE DE GROSSOUVRE 8 Subfamily Mammitinae Hyatt 8 Genus Mammites PLATES 1-14 21 Laube and Bruder 8 INDEX 50 Mammites nodosoides (Schluter) 8 TABLE 1—Mid-Cretaceous ammonite sequence for western New Mexico iv FIGURES 1—Location of study area 5 9—Histogram of size and body chambers of Neoptychites 2—External sutures of Mammites nodosoides (Schluter) 9 3— cephalotus (Courtiller) 14 Whorl sections of Morrowites wingi (Morrow) 10 4—External 10—Scatter diagram of breadth to diameter ratio of Neop- suture of Morrowites wingi (Morrow) 10 5—Whorl section and tychites 14 suture of Morrowites depressus 11—External sutures of Neoptychites cephalotus (Cour-tiller) 15 (Powell) 11 12—External suture of Fagesia superstes (Kossmat) 16 13— 6—External sutures of Morrowites subdepressus Cobban and Histogram of size of body chambers of Cibolaites molenaari Hook, n.