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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. -
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. -
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. -
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 -
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. -
The Palaeontology Newsletter
The Palaeontology Newsletter Contents 90 Editorial 2 Association Business 3 Association Meetings 11 News 14 From our correspondents Legends of Rock: Marie Stopes 22 Behind the scenes at the Museum 25 Kinds of Blue 29 R: Statistical tests Part 3 36 Rock Fossils 45 Adopt-A-Fossil 48 Ethics in Palaeontology 52 FossilBlitz 54 The Iguanodon Restaurant 56 Future meetings of other bodies 59 Meeting Reports 64 Obituary: David M. Raup 79 Grant and Bursary Reports 81 Book Reviews 103 Careering off course! 111 Palaeontology vol 58 parts 5 & 6 113–115 Papers in Palaeontology vol 1 parts 3 & 4 116 Virtual Palaeontology issues 4 & 5 117–118 Annual Meeting supplement >120 Reminder: The deadline for copy for Issue no. 91 is 8th February 2016. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 90 2 Editorial I watched the press conference for the publication on the new hominin, Homo naledi, with rising incredulity. The pomp and ceremony! The emotion! I wondered why all of these people were so invested just because it was a new fossil species of something related to us in the very recent past. What about all of the other new fossil species that are discovered every day? I can’t imagine an international media frenzy, led by deans and vice chancellors amidst a backdrop of flags and flashbulbs, over a new species of ammonite. Most other fossil discoveries and publications of taxonomy are not met with such fanfare. The Annual Meeting is a time for sharing these discoveries, many of which will not bring the scientists involved international fame, but will advance our science and push the boundaries of our knowledge and understanding. -
The Letters F and T Refer to Figures Or Tables Respectively
INDEX The letters f and t refer to figures or tables respectively "A" Marker, 312f, 313f Amherstberg Formation, 664f, 728f, 733,736f, Ashville Formation, 368f, 397, 400f, 412, 416, Abitibi River, 680,683, 706 741f, 765, 796 685 Acadian Orogeny, 686, 725, 727, 727f, 728, Amica-Bear Rock Formation, 544 Asiak Thrust Belt, 60, 82f 767, 771, 807 Amisk lowlands, 604 Askin Group, 259f Active Formation, 128f, 132f, 133, 139, 140f, ammolite see aragonite Assiniboia valley system, 393 145 Amsden Group, 244 Assiniboine Member, 412, 418 Adam Creek, Ont., 693,705f Amundsen Basin, 60, 69, 70f Assiniboine River, 44, 609, 637 Adam Till, 690f, 691, 6911,693 Amundsen Gulf, 476, 477, 478 Athabasca, Alta., 17,18,20f, 387,442,551,552 Adanac Mines, 339 ancestral North America miogeocline, 259f Athabasca Basin, 70f, 494 Adel Mountains, 415 Ancient Innuitian Margin, 51 Athabasca mobile zone see Athabasca Adel Mountains Volcanics, 455 Ancient Wall Complex, 184 polymetamorphic terrane Adirondack Dome, 714, 765 Anderdon Formation, 736f Athabasca oil sands see also oil and gas fields, Adirondack Inlier, 711 Anderdon Member, 664f 19, 21, 22, 386, 392, 507, 553, 606, 607 Adirondack Mountains, 719, 729,743 Anderson Basin, 50f, 52f, 359f, 360, 374, 381, Athabasca Plain, 617f Aftonian Interglacial, 773 382, 398, 399, 400, 401, 417, 477f, 478 Athabasca polymetamorphic terrane, 70f, Aguathuna Formation, 735f, 738f, 743 Anderson Member, 765 71-72,73 Aida Formation, 84,104, 614 Anderson Plain, 38, 106, 116, 122, 146, 325, Athabasca River, 15, 20f, 35, 43, 273f, 287f, Aklak -
Early Cambrian Tidal Sedimentary Environments, Western Victoria Island, Arctic Canada
Early Cambrian tidal sedimentary environments, western Victoria Island, Arctic Canada By Andrew Michael Durbano A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geological Sciences University of Saskatchewan Saskatoon © Andrew Michael Durbano, April 2014. All rights reserved. PERMISSION TO USE In presenting this thesis in partial fulfillment of the requirements for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Geological Sciences University of Saskatchewan Saskatoon, Saskatchewan Canada S7N 5E2 OR Dean College of Graduate Studies and Research University of Saskatchewan 107 Administration Place Saskatoon, Saskatchewan Canada S7N 5A2 i ABSTRACT The currently unnamed early Cambrian (Series 2, Stage 4) sandstone unit is exposed in the Minto Inlier of western Victoria Island, Canadian Arctic Islands, and forms the base of the Phanerozoic succession. -
Kimmigj CV 20210106.Pdf
Julien Karl Franck Kimmig Curriculum vitae Earth and Mineral Sciences Museum & Art Gallery Pennsylvania State University 116 Deike Building University Park, PA, 16802 Phone: 785-766-2386 Email: [email protected] 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 2009 Topic: Advanced Methods in Taxonomy and Biodiversity Imperial College London & Natural History Museum London (United Kingdom) B.Sc. in Geosciences 2008 Georg-August-Universität Göttingen (Germany) Professional experience Collections Manager since August 2020 Earth and Mineral Sciences Museum & Art Gallery Pennsylvania State University Research Affiliate since August 2019 Division of Invertebrate Paleontology University of Kansas Collections Manager June 2016 – July 2019 Division of Invertebrate Paleontology University of Kansas Research Associate July 2015 – June 2019 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 Kimmig | CV 1 The Natural History Museum London Museum and Research Assistant December 2007 – September 2008 Supervisor: Mike Reich Geowissenschaftliches Museum Göttingen Selected fieldwork (Total ~ 160 days) Cambrian, Utah and Idaho, 2019 10 days Spence -
Cnidaria: Hydrozoa) Or Eldonids from the Early Cambrian (Series 2: Stage 4) of Western U.S.A
A peer-reviewed version of this preprint was published in PeerJ on 6 June 2017. View the peer-reviewed version (peerj.com/articles/3312), which is the preferred citable publication unless you specifically need to cite this preprint. Lieberman BS, Kurkewicz R, Shinogle H, Kimmig J, MacGabhann BA. 2017. Disc-shaped fossils resembling porpitids or eldonids from the early Cambrian (Series 2: Stage 4) of western USA. PeerJ 5:e3312 https://doi.org/10.7717/peerj.3312 Disc-shaped fossils resembling porpitids (Cnidaria: Hydrozoa) or eldonids from the early Cambrian (Series 2: Stage 4) of western U.S.A. Bruce S Lieberman Corresp., 1, 2 , Richard Kurkewicz 3 , Heather Shinogle 4 , Julien Kimmig 2 , Breandán Anraoi MacGabhann 5 1 Department of Ecology & Evolutionary Biology, University of Kansas, Lawrence, Kansas, United States 2 Biodiversity Institute, University of Kansas, Lawrence, Kansas, United States 3 Pangaea Fossils, San Francisco, California, United States 4 Microscopy and Analytical Imaging Laboratory, University of Kansas, Lawrence, Kansas, United States 5 Department of Geography, Edge Hill University, Ormskirk, United Kingdom Corresponding Author: Bruce S Lieberman Email address: [email protected] The morphology and affinities of newly discovered disc-shaped soft-bodied fossils from the early Cambrian (Series 2: Stage 4, Dyeran) Carrara Formation are discussed. These specimens show some similarity to the Ordovician Discophyllum Hall, 1847; traditionally this taxon had been treated as a fossil porpitid. However, recently it has instead been referred to another clade, the eldonids, which includes the enigmatic Eldonia Walcott, 1911 that was originally described from the Cambrian Burgess Shale. The status of various Proterozoic and Phanerozoic taxa previously referred to porpitids and eldonids is also briefly considered. -
Newsletter Number 91
The Palaeontology Newsletter Contents 91 Editorial 2 Association Business 3 Association Meetings 20 News 25 From our correspondents Legends of Rock: Charles Lapworth 34 Behind the scenes at the Museum 38 Mystery Fossil 23 43 Marvellous Mistakes 44 Fossil tree site deteriorating 49 “Science without barriers” 50 0–5 in 3 billion years 55 Tim Palmer steps down 58 Future meetings of other bodies 62 Meeting Reports 68 Obituary: Peter Forey 78 Obituary: Walter Sweet 82 Grant and Bursary Reports 84 Book Reviews 106 Careering off course! 111 Palaeontology vol 59 parts 1 & 2 114–115 Papers in Palaeontology vol 2 part 1 116 Reminder: The deadline for copy for Issue no. 92 is 6th June 2016. On the Web: <http://www.palass.org/> ISSN: 0954-9900 Newsletter 91 2 Editorial The PalAss Newsletter has been a cardinal feature of the Association’s publishing remit for nearly thirty years, and over its lifetime it has evolved in response to trends in palaeontology, science and society. Today the Newsletter features a mixture of long-established content relating to meetings, grant reports, methodologies and book reviews, and more recent additions such as media coverage of palaeontology, virtual visits to collections and biographies of notable palaeontologists (current and historical). I am honoured to take up the role of Newsletter Editor for 2016 and am hugely grateful to the outgoing Editor, Jo Hellawell, for invaluable help during the transition period. I hope that under my stewardship, the Newsletter continues to deliver thought-provoking material of interest to all of the Association’s members. One aspect of palaeontology – and the scientific realm more broadly – that has been highlighted recently is the role of women. -
Earth Science Week 2019 Highlights Report
Earth Science Week 2020: Earth Materials in Our Lives October 11–17, 2020 Highlights Report Earth Materials in Our Lives EARTH SCIENCE WEEK www.earthsciweek.org Earth Science Week 2020: Earth Materials in Our Lives October 11–17, 2020 Highlights Report Copyright ©2021 by Contents American Geosciences Institute. 2 Highlights Report: Earth Science Week 2020 ISBN: __ 2 Introduction 4 Summary of Activities American Geosciences Institute 4220 King Street 4 Key Partnerships and Efforts Alexandria, VA 22302 U.S.A. 10 Earth Science Week Toolkits www.americangeosciences.org 11 Web Resources 703-379-2480 13 Newsletter If you have comments concerning this report, please contact: 13 Contests Ed Robeck, Ph.D. 15 Earth Science Teaching Award Director of Education and Outreach 15 Focus Days American Geosciences Institute 16 AGI Promotions 703-379-2480 x245 [email protected] 17 State Proclamations 17 Publicity and Media Coverage 19 Earth Science Week Sponsors See Our News Coverage 19 Global Sponsors Because of the large and increasing number of news clip- 19 Earth Science Week Program Partners pings citing Earth Science Week activities and resources, the 20 Earth Science Week 2020 Events and Activities by print edition of the print report no longer includes clippings. State and Territory To view the hundreds of press releases and news items pro- 32 International Events moting awareness of Earth Science Week each year, please visit online at www.earthsciweek.org/highlights. Thank you for helping us in our efforts to conserve resources and protect the environment. Published and printed in the United States of America. All rights reserved.