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Geology Department N e w s l e t t e r Group photo taken at the Fall 2015 Geology Bonding Night held at Pizza Hut. Hello Alumni! On behalf of the Geology Department, I hope 2016 is starting out well for you. There have been a lot of changes during the past twelve months, as you’ll see by reading the remainder of this newsletter. Most of the changes are driven by the ongoing budget crisis in the state of Illinois so it is completely out of our hands. We expect even more changes in the coming year, but rest assured that we will be here in some form for the foreseeable future and our commitment to our students is as strong as ever. Despite these lean budgetary times we continue to bring students on field trips, involve them in undergraduate research, and bring them to research conferences to present their results. We are able to continue these activities because you, our alumni, generously contribute to our Geology Foundation account. We can’t thank you enough for your past and your continuing monetary support of the Geology Department. I hope you enjoy reading this year’s edition of the Geology Alumni Newsletter. Steve Bennett Alumni Newsletter Editor Artwork on the 2016 WIU Geology t-shirt features Bob Johnson’s vision of a wrestling match between Lincoln and an oversized Tully Monster. Finished Diprotodon skull. This was in the process of printing last year at this time. Bob assembled, painted, and made a stand for the skull. Dr. Hegna has it on display in the Geol 112 - History of the Earth lab room. Geology Department Newsletter P a g e 2 Leslie Melim I spent most of Spring 2015 Semester on sabbatical in Albuquerque, NM working on the scanning electron microscope at the University of New Mexico. Much as I love teaching, it was a nice change to just work on research for awhile. I missed Macomb and my friends here, but really enjoyed spending time with my friends there. I had planned on spending two months, but stayed an extra month after a riding accident left me with a broken ankle (it’s fine now) and unable to drive my manual-transmission Subaru. The extra time was very productive, as I collected hundreds of additional images and completed most of a detailed survey of recrystallization fabrics in cave pearls from the Huber Limestone Mine in Quincy, IL and from Carlsbad Cavern, NM. In addition, I worked some more on the living pool fingers from the Herbstlabyrinth/Adventhöhle Cave System, Germany, which produced a quick paper and a talk. Summer was fairly quiet with no field camp. I did get to Denver, Colorado for the American Association of Petroleum Geologists Annual Meeting as part of editor duties for Journal of Sedimentary Research. I also managed a nice visit with my sister in the Seattle area: July has much nicer weather than my usual December visit. In between trips, I found time for lots of horseback riding and woodworking. In August, I got back into teaching with the largest Geol 340 Strat. Sed. class ever: 22 students! It made for a very busy semester, particularly when grading the WID papers came around. As usual, I went back to UNM over Thanksgiving Break, taking two geology majors, Nick Liming and Justin Christensen, to finish up the cave pearl recrystallization study. Coming home, there was a huge ice storm over the Texas Panhandle that closed the interstate. To go around, we drove up through Colorado but it still got us. We encountered freezing drizzle on I-70 and so had to slow down. Unfortunately, the idiot behind us left her cruise control on (in ice?!) and rear ended my car. No one was hurt, but we ended up staying an extra two days in Colorado before I could get a rental car from her insurance company. Nick and Justin were great company in the little tiny town of Limon in eastern Colorado. I ended up taking the little Ford rent- al on a long odyssey over winter break from Illinois to Seattle to Albuquerque and finally back to Colorado to pick up my car in January. I’d much rather have done it with my all-wheel drive Subaru! Presentations: Melim, L.A., Spilde, M.N., Northup, D.E., 2015, Geomicrobiology of cave pearls: New evidence from Carlsbad Cavern. Geological Society of America Abstracts with Programs, Vol. 47, No. 7, p. 57, Presented November 1, 2015. Melim, L.A. Northup, D.E., Hughes, K.J., Spilde, M.N., and Boston, P.J., 2015, An SEM and molecular study of the living pool fingers in the Herbstlabyrinth/Adventhöhle Cave System, Hess, Germany. 2015 NSS Convention, Waynesville, MO, July 13-17, 2015. Presented July 15, 2015. Publications: Meyer, S., Melim, L., and Scholz, D., 2015, Morphologie der Pool-Fingers in der Riesenberghöhle (Süntel, Niedersachsen), Die Höhle, v. 66, p. 80-95 (in German, English abstract). Melim, L.A., Northup, D.E., Spilde, M.N., and Boston, P.J., 2015, Update: Living reticulated filaments from Herbstlabyrinth-Adventhöhle Cave System, Germany, Journal of Cave and Karst Studies, v. 77, p. 87-90. Preston, L.J., Melim, L.A., Polyak, V.J., Asmerom, Y., Southam, G., 2014, Infrared spectroscopic biosignatures from Hidden Cave, New Mexico: Possible applications for remote life detection, Geomicrobiology Journal, v. 31, p. 929-941. Geology Department Newsletter P a g e 3 Peter Calengas Greetings to all of the friends of the Department! The past year has been a very eventful one for everyone. Although our overall enrollments are similar to recent years, we currently have a large group of students taking our upper division courses (Geologic Field Methods, Stratigraphy and Sedimentology, Structural Geology) producing the largest enrollments we have had in these courses in 30 years. That is the good news. The bad news is that we once again have a “bare-bones” budget, and next year does not look any better! Fortunately, your generous financial support has made a difference. We will be offering Geology Field Camp this summer and have been able to continue to support our in-class field trips, trips for field work, and travel to present research at conferences. Without your generous donations to our foundation this would not be possible. In fact, half of our expenses during the last fiscal year were paid using our Geology Foundation account. Your continued support helps defray the cost for these important activities and allows us to continue to offer a high-quality Geology program for our majors. With Dr. Mayborn serving as an Interim Associate Dean in the College of Arts and Sciences, we were allowed to hire a visiting lecturer, Dr. Petr Yakovlev, for the Spring 2016 semester to teach Structural Geology. Although the geomorphology faculty position remains unfilled, we have asked Dr. Yakovlev to teach Geomorphology this spring to give our students an additional upper-division course option. I continue to teach my online Environmental Geology class and to serve as a consultant to a variety of Industrial Mineral enterprises. Keep in touch. It’s always great to hear from you. Diane Edwards Hi Everyone, As always, it’s a pleasure to submit a “blurb” for the annual Geology newsletter. That means I’m still vertical and working with some of the best folks on campus. There is a lot of uncertainty here at WIU and throughout the state of Illinois. Nonetheless we keep moving forward and coming to work each day to do the best we can for our students. Our major count is holding steady, which is great news! We have a large group of students signed up for Geology Summer Field Camp 2016. Right now the count is 23 which matches the count from 1984’s field camp. We’re very humbled by the Paul Wagner Memorial contributions received this past year. These funds went to the Geology Foundation and have been earmarked for field camp. We’ve had really great turnouts the past few years for Bonding Night, the annual Geology Club Holiday Party, and the spring picnic. It’s very heart-warming to see our students interested in these Geology-related social events. On a personal note, my entire family met for a week of fun in the sun and on the water at Lake of the Ozarks, Missouri. We had beautiful weather, amazing accommodations and a ton of fun. I feel truly blessed! The photo was taken at “Wobbly Boots” Restaurant, Osage Beach. Those of you that have visited this area are probably familiar with it. Please keep in touch & wishing you all a healthy, happy year! Geology Department Newsletter P a g e 4 To m H e g n a 2015 proved to be a busy year in the “Hegna Lab”. In the spring, I had the privilege of taking the Paleontology class on a trip to Iowa City to see the paleontology collections at the University of Iowa (my alma mater), the MAPS fossil show, and the Devonian fossil gorge. I helped out with the Structural Geology field trip to Wisconsin—seeing some sights that I had not seen since I was an undergraduate and did a similar trip, as well as some that I had never seen before. I was even able to convince Dr. Mayborn to make a brief stop at a spectacular Ordovician-age outcrop in southern Wisconsin to see some fossils. At the end of the spring semester, I took several stu- dents to the North Central Geological Society of America Meeting, where several presented their research.
Recommended publications
  • Exceptionally Preserved Fossil Assemblages Through Geologic Time and Space

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    Gondwana Research 48 (2017) 164–188 Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr GR Focus Review Exceptionally preserved fossil assemblages through geologic time and space A.D. Muscente a,⁎, James D. Schiffbauer b, Jesse Broce b, Marc Laflamme c, Kenneth O'Donnell d,ThomasH.Boage, Michael Meyer f, Andrew D. Hawkins g,JohnWarrenHuntleyb, Maria McNamara h, Lindsay A. MacKenzie i, George D. Stanley Jr. j, Nancy W. Hinman j, Michael H. Hofmann j, Shuhai Xiao g a Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA b Department of Geological Sciences, University of Missouri, Columbia, MO 65211, USA c Department of Chemical and Physical Sciences, University of Toronto Mississauga, Mississauga, ON L5L 1C6, Canada d AECOM, Germantown, MD 20876, USA e Department of Geological Sciences, Stanford University, Stanford, CA 94305, USA f Geophysical Laboratory, Carnegie Institution for Science, Washington, DC 20015, USA g Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, USA h School of Biological, Earth, and Environmental Sciences, University College Cork, Cork, T23 TK30, Ireland i Department of Geological Sciences, SUNY Geneseo, Geneseo, NY 14454, USA j Department of Geosciences, University of Montana, Missoula, MT 59812, USA article info abstract Article history: Geologic deposits containing fossils with remains of non-biomineralized tissues (i.e. Konservat-Lagerstätten) Received 23 February 2017 provide key insights into ancient organisms and ecosystems. Such deposits are not evenly distributed through Received in revised form 13 April 2017 geologic time or space, suggesting that global phenomena play a key role in exceptional fossil preservation.
  • Reinterpretation of the Enigmatic Ordovician Genus Bolboporites (Echinodermata)

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    Reinterpretation of the enigmatic Ordovician genus Bolboporites (Echinodermata). Emeric Gillet, Bertrand Lefebvre, Véronique Gardien, Emilie Steimetz, Christophe Durlet, Frédéric Marin To cite this version: Emeric Gillet, Bertrand Lefebvre, Véronique Gardien, Emilie Steimetz, Christophe Durlet, et al.. Reinterpretation of the enigmatic Ordovician genus Bolboporites (Echinodermata).. Zoosymposia, Magnolia Press, 2019, 15 (1), pp.44-70. 10.11646/zoosymposia.15.1.7. hal-02333918 HAL Id: hal-02333918 https://hal.archives-ouvertes.fr/hal-02333918 Submitted on 13 Nov 2020 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. 1 Reinterpretation of the Enigmatic Ordovician Genus Bolboporites 2 (Echinodermata) 3 4 EMERIC GILLET1, BERTRAND LEFEBVRE1,3, VERONIQUE GARDIEN1, EMILIE 5 STEIMETZ2, CHRISTOPHE DURLET2 & FREDERIC MARIN2 6 7 1 Université de Lyon, UCBL, ENSL, CNRS, UMR 5276 LGL-TPE, 2 rue Raphaël Dubois, F- 8 69622 Villeurbanne, France 9 2 Université de Bourgogne - Franche Comté, CNRS, UMR 6282 Biogéosciences, 6 boulevard 10 Gabriel, F-2100 Dijon, France 11 3 Corresponding author, E-mail: [email protected] 12 13 Abstract 14 Bolboporites is an enigmatic Ordovician cone-shaped fossil, the precise nature and systematic affinities of 15 which have been controversial over almost two centuries.
  • (Drumian, Miaolingian) Marjum Formation of Western Utah, USA

    (Drumian, Miaolingian) Marjum Formation of Western Utah, USA

    First palaeoscolecid from the Cambrian (Drumian, Miaolingian) Marjum Formation of western Utah, USA WADE W. LEIBACH, RUDY LEROSEY-AUBRIL, ANNA F. WHITAKER, JAMES D. SCHIFFBAUER, and JULIEN KIMMIG Leibach, W.W., Lerosey-Aubril, R., Whitaker, A.F., Schiffbauer, J.D., and Kimmig, J. 2021. First palaeoscolecid from the Cambrian (Drumian, Miaolingian) Marjum Formation of western Utah, USA. Acta Palaeontologica Polonica 66 (X): xxx–xxx. The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It preserves a diverse non-biomineralized fossil assemblage, which is dominated by panarthropods and sponges. Infaunal components are particularly rare, and are best exemplified by the poorly diverse scalidophoran fauna and the uncertain presence of palaeoscolecids amongst it. To date, only a single Marjum Formation fossil has been tentatively assigned to the palaeoscolecid taxon Scathascolex minor. This specimen and two recently collected worm fragments were analysed in this study using scanning electron microscopy and energy dispersive X-ray spectrometry. The previous occurrence of a Marjum Formation palaeoscolecid is refuted based on the absence of sclerites in the specimen, which we tentatively assign to an unidentified species of Ottoia. The two new fossils, however, are identified as a new palaeoscolecid taxon, Arrakiscolex aasei gen. et sp. nov., characterized by the presence of hundreds of size-constrained (20–30 µm), smooth- rimmed, discoid plates on each annulus. This is the first indisputable evidence for the presence of palaeoscolecids in the Marjum biota, and a rare occurrence of the group in the Cambrian of Laurentia. Palaeoscolecids are now known from nine Cambrian Stage 3–Guzhangian localities in Laurentia, but they typically represent rare components of the biotas.
  • The Weeks Formation Konservat-Lagerstätte and the Evolutionary Transition of Cambrian Marine Life

    The Weeks Formation Konservat-Lagerstätte and the Evolutionary Transition of Cambrian Marine Life

    Downloaded from http://jgs.lyellcollection.org/ by guest on October 1, 2021 Review focus Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2018-042 The Weeks Formation Konservat-Lagerstätte and the evolutionary transition of Cambrian marine life Rudy Lerosey-Aubril1*, Robert R. Gaines2, Thomas A. Hegna3, Javier Ortega-Hernández4,5, Peter Van Roy6, Carlo Kier7 & Enrico Bonino7 1 Palaeoscience Research Centre, School of Environmental and Rural Science, University of New England, Armidale, NSW 2351, Australia 2 Geology Department, Pomona College, Claremont, CA 91711, USA 3 Department of Geology, Western Illinois University, 113 Tillman Hall, 1 University Circle, Macomb, IL 61455, USA 4 Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK 5 Museum of Comparative Zoology and Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, MA 02138, USA 6 Department of Geology, Ghent University, Krijgslaan 281/S8, B-9000 Ghent, Belgium 7 Back to the Past Museum, Carretera Cancún, Puerto Morelos, Quintana Roo 77580, Mexico R.L.-A., 0000-0003-2256-1872; R.R.G., 0000-0002-3713-5764; T.A.H., 0000-0001-9067-8787; J.O.-H., 0000-0002- 6801-7373 * Correspondence: [email protected] Abstract: The Weeks Formation in Utah is the youngest (c. 499 Ma) and least studied Cambrian Lagerstätte of the western USA. It preserves a diverse, exceptionally preserved fauna that inhabited a relatively deep water environment at the offshore margin of a carbonate platform, resembling the setting of the underlying Wheeler and Marjum formations. However, the Weeks fauna differs significantly in composition from the other remarkable biotas of the Cambrian Series 3 of Utah, suggesting a significant Guzhangian faunal restructuring.
  • Exceptional Fossil Preservation During CO2 Greenhouse Crises? Gregory J

    Exceptional Fossil Preservation During CO2 Greenhouse Crises? Gregory J

    Palaeogeography, Palaeoclimatology, Palaeoecology 307 (2011) 59–74 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Exceptional fossil preservation during CO2 greenhouse crises? Gregory J. Retallack Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA article info abstract Article history: Exceptional fossil preservation may require not only exceptional places, but exceptional times, as demonstrated Received 27 October 2010 here by two distinct types of analysis. First, irregular stratigraphic spacing of horizons yielding articulated Triassic Received in revised form 19 April 2011 fishes and Cambrian trilobites is highly correlated in sequences in different parts of the world, as if there were Accepted 21 April 2011 short temporal intervals of exceptional preservation globally. Second, compilations of ages of well-dated fossil Available online 30 April 2011 localities show spikes of abundance which coincide with stage boundaries, mass extinctions, oceanic anoxic events, carbon isotope anomalies, spikes of high atmospheric carbon dioxide, and transient warm-wet Keywords: Lagerstatten paleoclimates. Exceptional fossil preservation may have been promoted during unusual times, comparable with fi Fossil preservation the present: CO2 greenhouse crises of expanding marine dead zones, oceanic acidi cation, coral bleaching, Trilobite wetland eutrophication, sea level rise, ice-cap melting, and biotic invasions. Fish © 2011 Elsevier B.V. All rights reserved. Carbon dioxide Greenhouse 1. Introduction Zeigler, 1992), sperm (Nishida et al., 2003), nuclei (Gould, 1971)and starch granules (Baxter, 1964). Taphonomic studies of such fossils have Commercial fossil collectors continue to produce beautifully pre- emphasized special places where fossils are exceptionally preserved pared, fully articulated, complex fossils of scientific(Simmons et al., (Martin, 1999; Bottjer et al., 2002).
  • Th TRILO the Back to the Past Museum Guide to TRILO BITES

    Th TRILO the Back to the Past Museum Guide to TRILO BITES

    With regard to human interest in fossils, trilobites may rank second only to dinosaurs. Having studied trilobites most of my life, the English version of The Back to the Past Museum Guide to TRILOBITES by Enrico Bonino and Carlo Kier is a pleasant treat. I am captivated by the abundant color images of more than 600 diverse species of trilobites, mostly from the authors’ own collections. Carlo Kier The Back to the Past Museum Guide to Specimens amply represent famous trilobite localities around the world and typify forms from most of the Enrico Bonino Enrico 250-million-year history of trilobites. Numerous specimens are masterpieces of modern professional preparation. Richard A. Robison Professor Emeritus University of Kansas TRILOBITES Enrico Bonino was born in the Province of Bergamo in 1966 and received his degree in Geology from the Depart- ment of Earth Sciences at the University of Genoa. He currently lives in Belgium where he works as a cartographer specialized in the use of satellite imaging and geographic information systems (GIS). His proficiency in the use of digital-image processing, a healthy dose of artistic talent, and a good knowledge of desktop publishing software have provided him with the skills he needed to create graphics, including dozens of posters and illustrations, for all of the displays at the Back to the Past Museum in Cancún. In addition to his passion for trilobites, Enrico is particularly inter- TRILOBITES ested in the life forms that developed during the Precambrian. Carlo Kier was born in Milan in 1961. He holds a degree in law and is currently the director of the Azul Hotel chain.
  • First Occurrence of the Problematic Vetulicolian Skeemella Clavula in the Cambrian Marjum Formation of Utah, USA

    First Occurrence of the Problematic Vetulicolian Skeemella Clavula in the Cambrian Marjum Formation of Utah, USA

    Carnets Geol. 20 (10) E-ISSN 1634-0744 DOI 10.4267/2042/70836 First occurrence of the problematic vetulicolian Skeemella clavula in the Cambrian Marjum Formation of Utah, USA Julien KIMMIG 1, 2 Wade W. LEIBACH 1, 3 Bruce S. LIEBERMAN 1, 4 Abstract: The Cambrian Marjum Formation of western Utah (USA) preserves a diverse soft-bodied fauna from the upper Drumian that is slightly younger than the well-known Burgess Shale. While the Marjum is dominated by arthropods, animals belonging to a variety of phyla have been found. Here, we document the second occurrence of the rare, enigmatic taxon Skeemella clavula, which was pre- viously thought to be restricted to the Pierson Cove Formation of the Drum Mountains. The occurrence in the Marjum represents a new preservational setting, as well as a slightly younger deposit. The new specimens also expand the number of known specimens to three. In addition, they improve understan- ding of the morphology of this representative of the problematic phylum Vetulicolia. Key-words: • Burgess Shale-type preservation; • Great Basin; • Vetulicolia; • Miaolingian; • Drumian; • Problematica Citation: KIMMIG J., LEIBACH W.W. & LIEBERMAN B.S. (2020).- First occurrence of the problematic vetuli- colian Skeemella clavula in the Cambrian Marjum Formation of Utah, USA.- Carnets Geol., Madrid, vol. 20, no. 10, p. 215-221. Résumé : Première occurrence du Vetulicolia problématique Skeemella clavula dans la For- mation cambrienne de Marjum Formation d'Utah, É.U.A.- Dans l'ouest de l'Utah (É.U.A.), la For- mation cambrienne de Marjum préserve une faune diversifiée d'animaux à corps mou dans le Drumien supérieur, une faune légèrement plus jeune que celle des fameux Schistes de Burgess.
  • The Stratigraphic Section in the Vicinity of Eureka, Nevada

    The Stratigraphic Section in the Vicinity of Eureka, Nevada

    The Stratigraphic Section in the Vicinity of Eureka, Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 276 The Stratigraphic Section in the Vicinity of Eureka, Nevada By T. B. NOLAN, C. W. MERRIAM, and J. S. WILLIAMS GEOLOGICAL SURVEY PROFESSIONAL PAPER 276 Revision of the pre- Tertiary stratigraphy of east-central Nevada UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1956 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.00 (paper cover) CONTENTS Page Page Abstract_ _____________________ 1 Silurian system.___________________________ 36 Introduction. _--___-______--___- 2 Roberts Mountains formation.__________ 36 Acknowledgments- --.-_---___-_-. 3 Lone Mountain dolomite__________... 37 Structural setting._______________ 3 Devonian system.__________-_-_-__--_____. 40 Economic significance. _-__._. 5 Nevada formation_________--______--. 40 Cambrian system.________________ 5 Beacon Peak dolomite member. 42 Prospect Mountain quartzite.. 6 Oxyoke Canyon sandstone member... 43 Pioche shale_______--_-_-_.__. 7 Sentinel Mountain dolomite member. 43 Eldorado dolomite___________ 9 Woodpecker limestone member. 44 Geddes limestone.___________ 11 Bay State dolomite member.--...--. 45 Secret Canyon shale._________ 12 Devils Gate limestone._________________ 48 Lower shale member. .... 13 Meister member.__________________ 49 Hayes Canyon member.____________ 49 Clarks Spring member.._ 14 Devonian and Mississippian systems. ________ 52 Hamburg dolomite.___-_.____ 16 Pilot shale________-__-_-___--__---_-_. 52 Dunderberg shale.___________ 18 Carboniferous systems_.____-__-______-__- 54 Windfall formation.__________ 19 Mississippian system._________--,___-_- 54 Catlin member._________ 20 Joana limestone,___________________ 54 Bullwhacker member.
  • Retallack 2011 Lagerstatten

    Retallack 2011 Lagerstatten

    This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Palaeogeography, Palaeoclimatology, Palaeoecology 307 (2011) 59–74 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Exceptional fossil preservation during CO2 greenhouse crises? Gregory J. Retallack Department of Geological Sciences, University of Oregon, Eugene, Oregon 97403, USA article info abstract Article history: Exceptional fossil preservation may require not only exceptional places, but exceptional times, as demonstrated Received 27 October 2010 here by two distinct types of analysis. First, irregular stratigraphic spacing of horizons yielding articulated Triassic Received in revised form 19 April 2011 fishes and Cambrian trilobites is highly correlated in sequences in different parts of the world, as if there were Accepted 21 April 2011 short temporal intervals of exceptional preservation globally. Second, compilations of ages of well-dated fossil Available online 30 April 2011 localities show spikes of abundance which coincide with stage boundaries, mass extinctions, oceanic anoxic events, carbon isotope anomalies, spikes of high atmospheric carbon dioxide, and transient warm-wet Keywords: Lagerstatten paleoclimates.
  • Resolving Details of the Nonbiomineralized Anatomy of Trilobites Using Computed

    Resolving Details of the Nonbiomineralized Anatomy of Trilobites Using Computed

    Resolving Details of the Nonbiomineralized Anatomy of Trilobites Using Computed Tomographic Imaging Techniques Thesis Presented in Partial Fulfillment of the Requirements for the Master of Science in the Graduate School of The Ohio State University By Jennifer Anita Peteya, B.S. Graduate Program in Earth Sciences The Ohio State University 2013 Thesis Committee: Loren E. Babcock, Advisor William I. Ausich Stig M. Bergström Copyright by Jennifer Anita Peteya 2013 Abstract Remains of two trilobite species, Elrathia kingii from the Wheeler Formation (Cambrian Series 3), Utah, and Cornuproetus cornutus from the Hamar Laghdad Formation (Middle Devonian), Alnif, Morocco, were studied using computed tomographic (CT) and microtomographic (micro-CT) imaging techniques for evidence of nonbiomineralized alimentary structures. Specimens of E. kingii showing simple digestive tracts are complete dorsal exoskeletons preserved with cone-in-cone concretions on the ventral side. Inferred stomach and intestinal structures are preserved in framboidal pyrite, likely resulting from replication by a microbial biofilm. C. cornutus is preserved in non- concretionary limestone with calcite spar lining the stomach ventral to the glabella. Neither species shows sediment or macerated sclerites of any kind in the gut, which tends to rule out the possibilities that they were sediment deposit-feeders or sclerite-ingesting durophagous carnivores. Instead, the presence of early diagenetic minerals in the guts of E. kingii and C. cornutus favors an interpretation of a carnivorous feeding strategy involving separation of skeletal parts of prey prior to ingestion. ii Dedication This manuscript is dedicated to my parents for encouraging me to go into the field of paleontology and to Lee Gray for inspiring me to continue.
  • Zootaxa, the Marjuman Trilobite Cedarina Lochman: Thoracic

    Zootaxa, the Marjuman Trilobite Cedarina Lochman: Thoracic

    Zootaxa 2218: 35–58 (2009) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2009 · Magnolia Press ISSN 1175-5334 (online edition) The Marjuman trilobite Cedarina Lochman: thoracic morphology, systematics, and new species from western Utah and eastern Nevada, USA JONATHAN M. ADRAIN1, SHANAN E. PETERS2 & STEPHEN R. WESTROP3 1Department of Geoscience, 121 Trowbridge Hall, University of Iowa, Iowa City, Iowa 52242, USA. E-mail: [email protected] 2Department of Geology & Geophysics, University of Wisconsin-Madison, 1215 W. Dayton St., Madison, Wisconsin 53706, USA. E-mail:[email protected] 3Oklahoma Museum of Natural History and School of Geology and Geophysics, University of Oklahoma, Norman, Oklahoma 73072, USA. E-mail:[email protected] Abstract Cedarina schachti n. sp. from the Marjuman (Cedaria Zone) Weeks Formation of western Utah, USA, provides the first information on thoracic morphology within the genus. Its thorax is radically different from those of species of Cedaria Walcott, with which Cedarina Lochman has been classified in Cedariidae Raymond, but strikingly similar to those of plesiomorphic remopleuridoideans grouped in the paraphyletic Richardsonellinae Raymond. If Cedarina and the remopleuridoideans are genuinely related it follows that 1) Cedariidae as traditionally conceived is paraphyletic; 2) Cedarina is a plesiomorphic sister taxon of the remopleuridoideans; and 3) the remopleuridoideans are not a component of the Order Asaphida. Silicified material of a second new species, C. clevensis from the Marjuman (Crepicephalus Zone) Lincoln Peak Formation of eastern Nevada, confirms the presence of a long thoracic axial spine and provides the first information on ontogenetic development and ventral morphology within the genus.
  • 2 Paleontology and Taphonomy of the Upper Weeks Formation (Cambrian, Upper Marjuman, Cedaria Zone) of Western Utah

    2 Paleontology and Taphonomy of the Upper Weeks Formation (Cambrian, Upper Marjuman, Cedaria Zone) of Western Utah

    2 PALEONTOLOGY AND TAPHONOMY OF THE UPPER WEEKS FORMATION (CAMBRIAN, UPPER MARJUMAN, CEDARIA ZONE) OF WESTERN UTAH 2.1 Abstract Twelve species of trilobites belonging to as many genera, one lingulide brachiopod species, Lingulella sp., one aglaspid species, Beckwithia typa, and an undetermined lightly scleritized or soft-bodied arthropod-like animal were recovered in a quantitative collection from the upper Weeks Formation (Marjuman) in the House Range of western Utah. Previously described trilobite genera include, in order of abundance in the collection, Cedaria, Modocia, Menomonia, Genevievella, Ammagnostus, Dresbachia, Norwoodia, Tricrepicephalus, and Weeksina. Two new ptychopariid genera and species, Nephalicephalus beebei and Selenocoryphe platyura, were also recovered in the collection, as were two new ptychopariid species, Modocia weeksensis and Norwoodia bellaspina. Additionally the new ptychopariid genus and species Gerospina schachti is described from supplemental material. At least 12 other genera, mostly trilobites, are known to occur in the Weeks Formation but were not recovered in the quantitative sample. The Weeks Formation fauna is very well preserved. Fossil orientation data and overall taphonomic state indicate little out-of-habitat transport of skeletal elements; 79 percent of the specimens recovered in an in situ collection consisted of articulated molts and complete exoskeletons. Sedimentary structures in the sample interval suggest episodic siliciclastic deposition in a carbonate mud-dominated environment located