DOCSLIB.ORG

Kimmig CV 062018

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Kimmig CV 062018 Kimmig Curriculum vitae Julien Karl Franck Kimmig Collections Manager Division of Invertebrate Paleontology Biodiversity Institute University of Kansas Lawrence, KS 66045 email: [email protected] phone: 785-864-2747 Education Ph.D. in “Geology” 2014 University of Saskatchewan (Canada) Thesis title: “Taxonomy, taphonomy and paleocology of a new Burgess Shale-type Lagerstätte from the Mackenzie Mountains, Northwest Territories, Canada.” M.Sc. in “Biology” (Advanced Methods in Taxonomy and Biodiversity) 2009 Imperial College London & Natural History Museum London (United Kingdom) B.Sc. in “Geosciences” 2008 Georg-August-Universität Göttingen (Germany) Work experience Collections Manager (Assistant Researcher) since June 2016 Division of Invertebrate Paleontology University of Kansas Research Associate since July 2015 Supervisor: Brian Pratt University of Saskatchewan Postdoctoral Researcher October 2014–June 2015 Supervisor: Brian Pratt University of Saskatchewan Teaching Assistant September 2011–September 2014 University of Saskatchewan Adjunct Researcher September 2009 – May 2011 Supervisor: Alison Longbottom The Natural History Museum London Museum and Research Assistant December 2007 – September 2008 Supervisor: Mike Reich Geowissenschaftliches Museum Göttingen Page 1 of 8 Kimmig Recent Grants and Awards (Total Grants and Awards: 9000$) Jeanette Johnson Professional Development Award May 2018 Value: 300 $ The Association of Earth Science Clubs of Greater Kansas City, Inc. March 2018 Research Grant Value: 500 $ Emerging Scholars Program, University of Kansas, Research Grant August 2017 Value: 2500 $ Paleontological Society Arthur James Boucot Research Grant April 2017 Value: 3500 $ Emerging Scholars Program, University of Kansas, Research Grant August 2016 Value: 1250 $ Selected fieldwork (Total about 130 days) Spence Shale, Wellsville Mountains, Utah, 2017 15 days Stratigraphic Paleobiology Field Course 2014 15 days Organised by Steve Holland (UGA) and Mark Patzkowsky (Penn St) Ravens Throat River, Mackenzie Mountains, Canada, 2012 28 days PhD fieldwork Geology and Biology of the Great Barrier Reef, 2008 15 days Organised by Gert Wörheide (Munich) and Mike Reich (Göttingen) Students advised (*Undergraduate Student; **Graduate Student) Nick Rose since August 2016 Wade Leibach since August 2016 Cortney Langley August 2016 – May 2018 Jennifer Rick August – October 2017 Teaching experience University of Kansas October 2016 Biol 225: Extinction events University of Saskatchewan September 2011–September 2014 Field school in Zortman Montana, Geol 308; Paleontology, Geol 247;Sedimentology, Geol 245; 5x Introduction to Geology, Geol 121) Page 2 of 8 Kimmig Languages German – fluent Spanish and Italian – basic competence French – fluent English – fluent Computer skills Microsoft Office – literate EndNote – literate IWork – literate KE Emu – good knowledge Adobe Photoshop – literate TNT – basic competence Adobe illustrator – literate Beast – basic competence R – literate Phylip – basic competence PAUP – literate Mr Bayes – basic competence ArcGIS – literate Additional cetrifications and documents First aid certificate Laboratory safety certificate Valid driver’s license Memberships in Professional Associations Geological Society of America Society for Sedimentary Geology Paleontological Society Palaeontological Association Page 3 of 8 4 Kimmig Publications Peer reviewed Papers Lieberman, Bruce S. & Julien Kimmig (in press) Museums, Paleontology, and a Biodiversity Science Based Approach. In G. D. Rosenberg, & R. M. Clary (Eds.), Museums at the Forefront of the History and Philosophy of Geology: History Made, History in the Making. Geological Society of America Special Paper 535. Kimmig, Julien, Ronald C. Meyer & Bruce S. Lieberman (online first) Herpetogaster from the early Cambrian of Nevada (Series 2, Stage 4) and its implications for the evolution of deuterostomes. Geological Magazine. DOI://10.1017/S0016756818000389 Strotz, Luke C., Marianna Simões, Matthew Girard, Laura Breitkreuz, Julien Kimmig & Bruce S. Lieberman (2018) Getting somewhere with the Red Queen: Chasing a biologically modern definition of the hypothesis. Biology Letters 14: 20170734. Kimmig, Julien & Brian R. Pratt (2018) Coprolites in the Ravens Throat River Lagerstätte of northwestern Canada: implications for the middle Cambrian food web. Palaios 33: 125–140. Cover article Article featured in news. Kimmig, Julien, Luke C. Strotz & Bruce S. Lieberman (2017) The stalked filter feeder Siphusauctum lloydguntheri n. sp. from the middle Cambrian (Series 3: Stage 5) Spence Shale of Utah: Its biological affinities and taphonomy. Journal of Paleontology 91: 902–910. Article featured in news. Kimmig, Julien & Luke C. Strotz (2017) Coprolites in middle Cambrian (Series 2-3) Burgess Shale-type deposits of Nevada and Utah and their ecological implications. Bulletin of Geosciences 92: 297–309. Lieberman, Bruce S., Richard Kurkewicz, Heather Shinogle, Julien Kimmig & Breandán A. MacGabhann (2017) Disc-shaped fossils resembling porpitids or eldonids from the early Cambrian (Series 2: Stage 4) of western U.S.A. PeerJ 5: e3312. Kimmig, Julien & Brian R. Pratt (2016) Taphonomy of the middle Cambrian (Series 3, Drumian) Ravens Throat River Lagerstätte, Mackenzie Mountains, Northwest Territories, Canada. Lethaia 49: 150–169. Kimmig, Julien & Brian R. Pratt (2015) Soft-bodied biota from the middle Cambrian (Drumian) Rockslide Formation, Mackenzie Mountains, northwestern Canada. Journal of Paleontology 89: 51–71. Kimmig, Julien (2013) Possible secondarily terrestrial lifestyle in the European phytosaur Nicrosaurus kapffi (Late Triassic, Norian) – A preliminary study. In: Triassic Geology and Paleontology: Tanner et al. (Eds.). New Mexico Museum of Natural History and Science, Bulletin 61: 306–312. Page 4 of 8 5 Kimmig Kimmig, Julien & Justin Spielmann (2011) Biological factors influencing phytosaur (Archosauria: Phytosauridae) taxonomy: A Prospectus. In: Fossil Record 3: Sullivan et al. (Eds.). New Mexico Museum of Natural History and Science, Bulletin 53: 289– 294. Kimmig, Julien & Gernot Arp (2010) Phytosaur remains from the Norian Arnstadt Formation (Leine Valley, Germany), with reference to European phytosaur habitats. Palaeodiversity 3: 215–224. Papers in review Pratt, Brian. R. & Julien Kimmig (in review) Extensive burrowing in a middle Cambrian Burgess Shale-type fossil Lagerstätte in northwestern Canada. Strotz, Luke C., Erin E. Saupe, Julien Kimmig & Bruce S. Lieberman (in review) Metabolic rates, climate and macroevolution: A case study using Neogene molluscs. Couto, Helena & Julien Kimmig (in review) A new Burgess Shale-type deposit from the Middle Ordovician (Dapingian- Darriwilian) upper Valongo Formation, Northern Portugal. Papers in preparation (*Supervised Undergraduate Student) Kimmig, Julien & Brian R. Pratt (in prep) Silver in organic films of a middle Cambrian Lagerstätte, Mackenzie Mountains northwestern Canada. Kimmig, Julien & Brian R. Pratt (in prep) Great Canadian Lagerstätten. The middle Cambrian Ravents Throat River Lagerstätte. Kimmig, Julien et al. (in prep) Sequence stratigraphy and paleoecology of the Mississippian Lodgepole Formation. Kimmig, Julien (in prep) A new phytosaur genus from the Triassic of Morocco. Kimmig, Julien, Helena Couto, *Wade W. Leibach & Bruce S. Lieberman (in prep) Discoidal soft-bodied fossils from the upper Valongo Formation (Middle Ordovician: Dapingian-Darriwilian) of northern Portugal and their implications for the group. *Rose, Nick J., Julien Kimmig, David A. Legg, Luke C. Strotz, *Cortney B. Langley & Kenneth S. Bader (in prep) Ontogeny of the horseshoe crab Paleolimulus signatus from the Pennsylvanian Pony Creek Lagerstätte. Non peer reviewed Kimmig, Julien (2017) Book Review: Suttner, T.J. et al. 2016. Planet Earth—In Deep Time. Palaeozoic Series: Devonian and Carboniferous. The Quarterly Review of Biology 92 (3): 306–307. Page 5 of 8 6 Kimmig Kimmig, Julien (2016) Book Review: Gass, K. 2015. Solving the Mystery of the First Animals on Land: The Fossils of Blackberry Hill. Fossil News: Fall 2016: 51. Kimmig, Julien (2016) Book Review: Penney, D. and J.E. Jepson. 2014. Fossil Insects: An introduction to palaeoentomology. Priscum: Newsletter of the Paleontological Society: Winter 2016: 42–43. Invited Presentations Kimmig, Julien (2018) The Cambrian: More than just trilobites. The 57th Annual Kansas City Gem and Mineral Show, March 11th, 2018. Kimmig, Julien (2018) The Cambrian: More than just trilobites. Science on Tap, January 24th, 2018. Kimmig, Julien (2017) Cambrian Soft-bodied biotas. Kansas and Missouri Paleontological Society, May 28th, 2017. Kimmig, Julien (2016) Burgess Shale-type deposits: A window into Cambrian paleoecology. Arkansas Tech University, February 9th, 2016. Conference Sessions Chaired Kimmig, Julien & Amy Singer (2016) Lagerstätten through Time and Space. Geological Society of America, Rocky Mountain Section Meeting, Moscow, ID. Conference Presentations (*Supervised Undergraduate Student) Kimmig, Julien, Luke Strotz, Sara Kimmig, Sven Egenhoff & Bruce Lieberman (2018) The middle Cambrian Spence Shale (Series 3: Stage 5) Lagerstätte: a key Cambrian ecosystem. 5th International Palaeontological Congress, Paris. (Talk) Lieberman, Bruce & Julien Kimmig (2018) Keynote: Digitizing fossils to advance macroevolutionary research. 5th International Palaeontological Congress, Paris. (Talk) Strotz, Luke, Erin Saupe, Julien Kimmig & Bruce Lieberman (2018) Metabolic rates, climate and macroevolution: A case study
Load more

Recommended publications
  • Climate Change and the Selective Signature of the Late Ordovician Mass Extinction
    Climate change and the selective signature of the Late Ordovician mass extinction Seth Finnegana,b,1, Noel A. Heimc, Shanan E. Petersc, and Woodward W. Fischera aDivision of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125; bDepartment of Integrative Biology, University of California, 1005 Valley Life Sciences Bldg #3140, Berkeley, CA 94720; and cDepartment of Geoscience, University of Wisconsin-Madison, 1215 West Dayton Street, Madison, WI 53706 Edited by Richard K. Bambach, Smithsonian Institution, National Museum of Natural History, Washington, D.C., and accepted by the Editorial Board March 6, 2012 (received for review October 14, 2011) Selectivity patterns provide insights into the causes of ancient ex- sedimentary record (common cause hypothesis) (14). For the tinction events. The Late Ordovician mass extinction was related LOME, it is useful to split common cause into two hypotheses. to Gondwanan glaciation; however, it is still unclear whether ele- The eustatic common cause hypothesis postulates that Gondwa- vated extinction rates were attributable to record failure, habitat nan glaciation drove the extinction by lowering eustatic sea level, loss, or climatic cooling. We examined Middle Ordovician-Early thereby reducing the overall area of shallow marine habitats, Silurian North American fossil occurrences within a spatiotempo- reorganizing habitat mosaics, and disrupting larval dispersal cor- rally explicit stratigraphic framework that allowed us to quantify ridors (16–18). The climatic common cause hypothesis postulates rock record effects on a per-taxon basis and assay the interplay of that climate cooling, in addition to being ultimately responsible macrostratigraphic and macroecological variables in determining for sea-level drawdown and attendant habitat losses, had a direct extinction risk.
    [Show full text]
  • FALL 2017 President’S Reflections
    PriscumPriscum NEWSLETTER OF THE VOLUME 24, ISSUE 1 President’s Reflections Paleobiology, the finances of both journals appear secure for INSIDE THIS ISSUE: the foreseeable future, and with a much-improved online presence for both journals. To be sure, more work lies ahead, Report on Student but we are collaborating with Cambridge to expand our au- 3 Diversity and Inclusion thor and reader bases, and, more generally, to monitor the ever-evolving publishing landscape. Our partnership with The Dry Dredgers of 10 Cambridge is providing additional enhancements for our Cincinnati, Ohio members, including the digitization of the Society’s entire archive of special publications; as of this writing, all of the PS Embraces the 13 Hydrologic Cycle Society’s short course volumes are now available through the member’s portal, and all remaining Society publications will be made available soon. We are also exploring an exciting PS Events at 2017 GSA 14 new outlet through Cambridge for all future Special Publica- By Arnie Miller (University of tions. Stay tuned! Book Reviews 15 Cincinnati), President In my first year as President, the Society has continued to These are challenging times for move forward on multiple fronts, as we actively explore and Books Available for 28 scientists and for the profes- pursue new means to carry out our core missions of enhanc- Review Announcement sional societies that represent ing and broadening the reach of our science and of our Socie- them. In the national political ty, and providing expanded developmental opportunities for arena, scientific findings, policies, and funding streams that all of our members.
    [Show full text]
  • Carbonate-Hosted Zn-Pb Mineralization in the Lower
    Carbonate-hosted Zn-Pb mineralization in the Lower Cambrian Sekwi Formation, Mackenzie Mountains, NWT: Stratigraphic, structural, and lithologic controls, and constraints on ore fluid characteristics by Beth J. Fischer Thesis submitted in partial fulfillment of the requirements for the degree of Master of Science (M.Sc.) in Geology School of Graduate Studies Laurentian University Sudbury, Ontario © Beth Fischer, 2012 Library and Archives Bibliotheque et Canada Archives Canada Published Heritage Direction du 1+1 Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-87713-5 Our file Notre reference ISBN: 978-0-494-87713-5 NOTICE: AVIS: The author has granted a non­ L'auteur a accorde une licence non exclusive exclusive license allowing Library and permettant a la Bibliotheque et Archives Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par I'lnternet, preter, telecommunication or on the Internet, distribuer et vendre des theses partout dans le loan, distrbute and sell theses monde, a des fins commerciales ou autres, sur worldwide, for commercial or non­ support microforme, papier, electronique et/ou commercial purposes, in microform, autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in this et des droits moraux qui protege cette these. Ni thesis. Neither the thesis nor la these ni des extraits substantiels de celle-ci substantial extracts from it may be ne doivent etre imprimes ou autrement printed or otherwise reproduced reproduits sans son autorisation.
    [Show full text]
  • The Ordovician Succession Adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen
    1 2 The Ordovician succession adjacent to Hinlopenstretet, Ny Friesland, Spitsbergen 3 4 Björn Kröger1, Seth Finnegan2, Franziska Franeck3, Melanie J. Hopkins4 5 6 Abstract: The Ordovician sections along the western shore of the Hinlopen Strait, Ny 7 Friesland, were discovered in the late 1960s and since then prompted numerous 8 paleontological publications; several of them are now classical for the paleontology of 9 Ordovician trilobites, and Ordovician paleogeography and stratigraphy. Our 2016 expedition 10 aimed in a major recollection and reappraisal of the classical sites. Here we provide a first 11 high-resolution lithological description of the Kirtonryggen and Valhallfonna formations 12 (Tremadocian –Darriwilian), which together comprise a thickness of 843 m, a revised bio-, 13 and lithostratigraphy, and an interpretation of the depositional sequences. We find that the 14 sedimentary succession is very similar to successions of eastern Laurentia; its Tremadocian 15 and early Floian part is composed of predominantly peritidal dolostones and limestones 16 characterized by ribbon carbonates, intraclastic conglomerates, microbial laminites, and 17 stromatolites, and its late Floian to Darriwilian part is composed of fossil-rich, bioturbated, 18 cherty mud-wackestone, skeletal grainstone and shale, with local siltstone and glauconitic 19 horizons. The succession can be subdivided into five third-order depositional sequences, 20 which are interpreted as representing the SAUK IIIB Supersequence known from elsewhere 21 on the Laurentian
    [Show full text]
  • Insights Into the Role of Redox State in Burgess 1 Shale-Type Taphonomic
    University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Geography, Earth and Environmental Sciences 2018-09 On the edge of exceptional preservation: insights into the role of redox state in Burgess Shale-type taphonomic windows from the Mural Formation, Alberta, Canada Sperling, EA http://hdl.handle.net/10026.1/11604 10.1042/ETLS20170163 Emerging Topics in Life Sciences All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. 1 On the edge of exceptional preservation: insights into the role of redox state in Burgess 2 Shale-type taphonomic windows from the Mural Formation, Alberta, Canada 3 4 5 6 Erik A. Sperling1*, Uwe Balthasar2, Christian B. Skovsted3 7 8 1 Department of Geological Sciences, Stanford University, Stanford, CA, USA 94305 9 10 2 School of Geography, Earth and Environmental Sciences, University of Plymouth, PL4 8AA, 11 Plymouth, United Kingdom 12 13 3 Department of Palaeobiology, Swedish Museum of Natural History, Box 50007, SE-104 05 14 Stockholm, Sweden 15 16 17 18 19 20 21 22 23 * Corresponding author: 24 Dr. Erik A. Sperling 25 Department of Geological Sciences 26 Stanford University 27 Stanford, CA, USA 94305 28 650-736-0852 (v) 29 [email protected] 30 31 32 Keywords: Cambrian; Mural Formation; Burgess Shale-type preservation; Oxygen; 33 taphonomy; iron reduction 34 35 36 1 37 Abstract 38 39 Animals originated in the Neoproterozoic and ‘exploded’ into the fossil record in the 40 Cambrian.
    [Show full text]
  • GEOLOGIC TIME SCALE V
    GSA GEOLOGIC TIME SCALE v. 4.0 CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST HIST. ANOM. (Ma) ANOM. CHRON. CHRO HOLOCENE 1 C1 QUATER- 0.01 30 C30 66.0 541 CALABRIAN NARY PLEISTOCENE* 1.8 31 C31 MAASTRICHTIAN 252 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 Lopin- 254 32 C32 72.1 635 2A C2A PIACENZIAN WUCHIAPINGIAN PLIOCENE 3.6 gian 33 260 260 3 ZANCLEAN CAPITANIAN NEOPRO- 5 C3 CAMPANIAN Guada- 265 750 CRYOGENIAN 5.3 80 C33 WORDIAN TEROZOIC 3A MESSINIAN LATE lupian 269 C3A 83.6 ROADIAN 272 850 7.2 SANTONIAN 4 KUNGURIAN C4 86.3 279 TONIAN CONIACIAN 280 4A Cisura- C4A TORTONIAN 90 89.8 1000 1000 PERMIAN ARTINSKIAN 10 5 TURONIAN lian C5 93.9 290 SAKMARIAN STENIAN 11.6 CENOMANIAN 296 SERRAVALLIAN 34 C34 ASSELIAN 299 5A 100 100 300 GZHELIAN 1200 C5A 13.8 LATE 304 KASIMOVIAN 307 1250 MESOPRO- 15 LANGHIAN ECTASIAN 5B C5B ALBIAN MIDDLE MOSCOVIAN 16.0 TEROZOIC 5C C5C 110 VANIAN 315 PENNSYL- 1400 EARLY 5D C5D MIOCENE 113 320 BASHKIRIAN 323 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 1500 CALYMMIAN 6 C6 APTIAN LATE 20 120 331 6A C6A 20.4 EARLY 1600 M0r 126 6B C6B AQUITANIAN M1 340 MIDDLE VISEAN MISSIS- M3 BARREMIAN SIPPIAN STATHERIAN C6C 23.0 6C 130 M5 CRETACEOUS 131 347 1750 HAUTERIVIAN 7 C7 CARBONIFEROUS EARLY TOURNAISIAN 1800 M10 134 25 7A C7A 359 8 C8 CHATTIAN VALANGINIAN M12 360 140 M14 139 FAMENNIAN OROSIRIAN 9 C9 M16 28.1 M18 BERRIASIAN 2000 PROTEROZOIC 10 C10 LATE
    [Show full text]
  • Guidebookguidebook A.L
    ROCKSLIDESROCKSLIDES ANDAND ROCKROCK AVALANCHESAVALANCHES OFOF THETHE KOKOMERENKOKOMEREN RIVERRIVER BASINBASIN (CENTRAL(CENTRAL TIENTIEN SHAN)SHAN) ICL SUMMER SCHOOL ON ROCKSLIDES AND RELATED PHENOMENA GUIDEBOOKGUIDEBOOK A.L. Strom & K.E. Abdrakhmatov Moscow–Bishkek, 2009 2 CONTENT 1 INTRODUCTION...............................................................................................................................................................11 2 GEOLOGICAL BACKGROUND (FACTORS GOVERNING BEDROCK SLOPE FAILURES)............................13 2.1 GEOLOGY........................................................................................................................................................................13 2.2 GEOMORPHOLOGY AND NEOTECTONICS.................................................................................................................................13 2.3 SEISMICITY ......................................................................................................................................................................20 2.4 HYDROGEOLOGICAL CONDITIONS..........................................................................................................................................26 3 ROCKSLIDE CASE STUDIES.........................................................................................................................................26 3.1 THE SNAKE-HEAD ROCK AVALANCHE...................................................................................................................................26
    [Show full text]
  • International Chronostratigraphic Chart
    INTERNATIONAL CHRONOSTRATIGRAPHIC CHART www.stratigraphy.org International Commission on Stratigraphy v 2018/08 numerical numerical numerical Eonothem numerical Series / Epoch Stage / Age Series / Epoch Stage / Age Series / Epoch Stage / Age GSSP GSSP GSSP GSSP EonothemErathem / Eon System / Era / Period age (Ma) EonothemErathem / Eon System/ Era / Period age (Ma) EonothemErathem / Eon System/ Era / Period age (Ma) / Eon Erathem / Era System / Period GSSA age (Ma) present ~ 145.0 358.9 ± 0.4 541.0 ±1.0 U/L Meghalayan 0.0042 Holocene M Northgrippian 0.0082 Tithonian Ediacaran L/E Greenlandian 152.1 ±0.9 ~ 635 Upper 0.0117 Famennian Neo- 0.126 Upper Kimmeridgian Cryogenian Middle 157.3 ±1.0 Upper proterozoic ~ 720 Pleistocene 0.781 372.2 ±1.6 Calabrian Oxfordian Tonian 1.80 163.5 ±1.0 Frasnian Callovian 1000 Quaternary Gelasian 166.1 ±1.2 2.58 Bathonian 382.7 ±1.6 Stenian Middle 168.3 ±1.3 Piacenzian Bajocian 170.3 ±1.4 Givetian 1200 Pliocene 3.600 Middle 387.7 ±0.8 Meso- Zanclean Aalenian proterozoic Ectasian 5.333 174.1 ±1.0 Eifelian 1400 Messinian Jurassic 393.3 ±1.2 7.246 Toarcian Devonian Calymmian Tortonian 182.7 ±0.7 Emsian 1600 11.63 Pliensbachian Statherian Lower 407.6 ±2.6 Serravallian 13.82 190.8 ±1.0 Lower 1800 Miocene Pragian 410.8 ±2.8 Proterozoic Neogene Sinemurian Langhian 15.97 Orosirian 199.3 ±0.3 Lochkovian Paleo- 2050 Burdigalian Hettangian 201.3 ±0.2 419.2 ±3.2 proterozoic 20.44 Mesozoic Rhaetian Pridoli Rhyacian Aquitanian 423.0 ±2.3 23.03 ~ 208.5 Ludfordian 2300 Cenozoic Chattian Ludlow 425.6 ±0.9 Siderian 27.82 Gorstian
    [Show full text]
  • International Chronostratigraphic Chart
    INTERNATIONAL CHRONOSTRATIGRAPHIC CHART www.stratigraphy.org International Commission on Stratigraphy v 2014/02 numerical numerical numerical Eonothem numerical Series / Epoch Stage / Age Series / Epoch Stage / Age Series / Epoch Stage / Age Erathem / Era System / Period GSSP GSSP age (Ma) GSSP GSSA EonothemErathem / Eon System / Era / Period EonothemErathem / Eon System/ Era / Period age (Ma) EonothemErathem / Eon System/ Era / Period age (Ma) / Eon GSSP age (Ma) present ~ 145.0 358.9 ± 0.4 ~ 541.0 ±1.0 Holocene Ediacaran 0.0117 Tithonian Upper 152.1 ±0.9 Famennian ~ 635 0.126 Upper Kimmeridgian Neo- Cryogenian Middle 157.3 ±1.0 Upper proterozoic Pleistocene 0.781 372.2 ±1.6 850 Calabrian Oxfordian Tonian 1.80 163.5 ±1.0 Frasnian 1000 Callovian 166.1 ±1.2 Quaternary Gelasian 2.58 382.7 ±1.6 Stenian Bathonian 168.3 ±1.3 Piacenzian Middle Bajocian Givetian 1200 Pliocene 3.600 170.3 ±1.4 Middle 387.7 ±0.8 Meso- Zanclean Aalenian proterozoic Ectasian 5.333 174.1 ±1.0 Eifelian 1400 Messinian Jurassic 393.3 ±1.2 7.246 Toarcian Calymmian Tortonian 182.7 ±0.7 Emsian 1600 11.62 Pliensbachian Statherian Lower 407.6 ±2.6 Serravallian 13.82 190.8 ±1.0 Lower 1800 Miocene Pragian 410.8 ±2.8 Langhian Sinemurian Proterozoic Neogene 15.97 Orosirian 199.3 ±0.3 Lochkovian Paleo- Hettangian 2050 Burdigalian 201.3 ±0.2 419.2 ±3.2 proterozoic 20.44 Mesozoic Rhaetian Pridoli Rhyacian Aquitanian 423.0 ±2.3 23.03 ~ 208.5 Ludfordian 2300 Cenozoic Chattian Ludlow 425.6 ±0.9 Siderian 28.1 Gorstian Oligocene Upper Norian 427.4 ±0.5 2500 Rupelian Wenlock Homerian
    [Show full text]
  • 2009 Geologic Time Scale Cenozoic Mesozoic Paleozoic Precambrian Magnetic Magnetic Bdy
    2009 GEOLOGIC TIME SCALE CENOZOIC MESOZOIC PALEOZOIC PRECAMBRIAN MAGNETIC MAGNETIC BDY. AGE POLARITY PICKS AGE POLARITY PICKS AGE PICKS AGE . N PERIOD EPOCH AGE PERIOD EPOCH AGE PERIOD EPOCH AGE EON ERA PERIOD AGES (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) (Ma) HIST. HIST. ANOM. ANOM. (Ma) CHRON. CHRO HOLOCENE 65.5 1 C1 QUATER- 0.01 30 C30 542 CALABRIAN MAASTRICHTIAN NARY PLEISTOCENE 1.8 31 C31 251 2 C2 GELASIAN 70 CHANGHSINGIAN EDIACARAN 2.6 70.6 254 2A PIACENZIAN 32 C32 L 630 C2A 3.6 WUCHIAPINGIAN PLIOCENE 260 260 3 ZANCLEAN 33 CAMPANIAN CAPITANIAN 5 C3 5.3 266 750 NEOPRO- CRYOGENIAN 80 C33 M WORDIAN MESSINIAN LATE 268 TEROZOIC 3A C3A 83.5 ROADIAN 7.2 SANTONIAN 271 85.8 KUNGURIAN 850 4 276 C4 CONIACIAN 280 4A 89.3 ARTINSKIAN TONIAN C4A L TORTONIAN 90 284 TURONIAN PERMIAN 10 5 93.5 E 1000 1000 C5 SAKMARIAN 11.6 CENOMANIAN 297 99.6 ASSELIAN STENIAN SERRAVALLIAN 34 C34 299.0 5A 100 300 GZELIAN C5A 13.8 M KASIMOVIAN 304 1200 PENNSYL- 306 1250 15 5B LANGHIAN ALBIAN MOSCOVIAN MESOPRO- C5B VANIAN 312 ECTASIAN 5C 16.0 110 BASHKIRIAN TEROZOIC C5C 112 5D C5D MIOCENE 320 318 1400 5E C5E NEOGENE BURDIGALIAN SERPUKHOVIAN 326 6 C6 APTIAN 20 120 1500 CALYMMIAN E 20.4 6A C6A EARLY MISSIS- M0r 125 VISEAN 1600 6B C6B AQUITANIAN M1 340 SIPPIAN M3 BARREMIAN C6C 23.0 345 6C CRETACEOUS 130 M5 130 STATHERIAN CARBONIFEROUS TOURNAISIAN 7 C7 HAUTERIVIAN 1750 25 7A M10 C7A 136 359 8 C8 L CHATTIAN M12 VALANGINIAN 360 L 1800 140 M14 140 9 C9 M16 FAMENNIAN BERRIASIAN M18 PROTEROZOIC OROSIRIAN 10 C10 28.4 145.5 M20 2000 30 11 C11 TITHONIAN 374 PALEOPRO- 150 M22 2050 12 E RUPELIAN
    [Show full text]
  • Ordovician Stratigraphy and Benthic Community Replacements in the Eastern Anti-Atlas, Morocco J
    Ordovician stratigraphy and benthic community replacements in the eastern Anti-Atlas, Morocco J. Javier Alvaro, Mohammed Benharref, Jacques Destombes, Juan Carlos Gutiérrez-Marco, Aaron Hunter, Bertrand Lefebvre, Peter van Roy, Samuel Zamora To cite this version: J. Javier Alvaro, Mohammed Benharref, Jacques Destombes, Juan Carlos Gutiérrez-Marco, Aaron Hunter, et al.. Ordovician stratigraphy and benthic community replacements in the eastern Anti- Atlas, Morocco. The Great Ordovician Biodiversification Event: Insights from the Tafilalt Biota, Morocco, 485, The Geological Society of London, pp.SP485.20, In press, Geological Society, London, Special Publication, 10.1144/SP485.20. hal-02405970 HAL Id: hal-02405970 https://hal.archives-ouvertes.fr/hal-02405970 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. The Geological Society Special Publications Ordovician stratigraphy and benthic community replacements in the eastern Anti-Atlas, Morocco --Manuscript Draft-- Manuscript Number: GSLSpecPub2019-17R1 Article Type: Research article Full Title: Ordovician stratigraphy and benthic community replacements in the eastern Anti-Atlas, Morocco Short Title: Ordovician stratigraphy of the Anti-Atlas Corresponding Author: Javier Alvaro Instituto de Geociencias SPAIN Corresponding Author E-Mail: [email protected] Other Authors: MOHAMMED BENHARREF JACQUES DESTOMBES JUAN CARLOS GUTIÉRREZ-MARCO AARON W.
    [Show full text]
  • 1 Rrh: Middle Cambrian Coprolites Lrh: J. Kimmig And
    RRH: MIDDLE CAMBRIAN COPROLITES LRH: J. KIMMIG AND B.R. PRATT Research Article DOI: http://dx.doi.org/10.2110/palo.2017.038 COPROLITES IN THE RAVENS THROAT RIVER LAGERSTÄTTE OF NORTHWESTERN CANADA: IMPLICATIONS FOR THE MIDDLE CAMBRIAN FOOD WEB 1 2 JULIEN KIMMIG AND BRIAN R. PRATT 1Biodiversity Institute, University of Kansas, Lawrence, Kansas 66045, USA 2Department of Geological Sciences, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5E2, Canada e-mail: [email protected] ABSTRACT: The Rockslide Formation (middle Cambrian, Drumian, Bolaspidella Zone) of the Mackenzie Mountains, northwestern Canada, hosts the Ravens Throat River Lagerstätte, which consists of two, 1-m thick intervals of greenish, thinly laminated, locally burrowed, slightly calcareous mudstone yielding a low-diversity and low-abundance fauna of bivalved arthropods, ‘worms’, hyoliths, and trilobites. Also present are flattened, circular, black carbonaceous objects averaging 15 mm in diameter, interpreted as coprolites preserved in either dorsal or ventral view. Many consist of aggregates of ovate carbonaceous flakes 0.5–2 mm long, which are probably compacted fecal pellets. Two-thirds contain a variably disarticulated pair of arthropod valves, and many also contain coiled to fragmented, corrugated ‘worm’ cuticle, either alone or together with valves. A few contain an enrolled agnostoid. In rare cases a ptychoparioid cranidium, agnostoid shield, bradoriid valve, or hyolith conch or operculum is present; these are taken to be due to capture and ingestion of bioclasts from the adjacent seafloor. Many of the coprolites are associated with semi-circular spreiten produced by movement of the worm-like predator while it occupied a vertical burrow. Its identity is unknown but it clearly exhibited prey selectivity.
    [Show full text]