Subcommission on Cambrian Stratigraphy
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Diversity Partitioning During the Cambrian Radiation
Diversity partitioning during the Cambrian radiation Lin Naa,1 and Wolfgang Kiesslinga,b aGeoZentrum Nordbayern, Paleobiology and Paleoenvironments, Friedrich-Alexander-Universität Erlangen-Nürnberg, 91054 Erlangen, Germany; and bMuseum für Naturkunde, Leibniz Institute for Research on Evolution and Biodiversity at the Humboldt University Berlin, 10115 Berlin, Germany Edited by Douglas H. Erwin, Smithsonian National Museum of Natural History, Washington, DC, and accepted by the Editorial Board March 10, 2015 (received for review January 2, 2015) The fossil record offers unique insights into the environmental and Results geographic partitioning of biodiversity during global diversifica- Raw gamma diversity exhibits a strong increase in the first three tions. We explored biodiversity patterns during the Cambrian Cambrian stages (informally referred to as early Cambrian in this radiation, the most dramatic radiation in Earth history. We as- work) (Fig. 1A). Gamma diversity dropped in Stage 4 and de- sessed how the overall increase in global diversity was partitioned clined further through the rest of the Cambrian. The pattern is between within-community (alpha) and between-community (beta) robust to sampling standardization (Fig. 1B) and insensitive to components and how beta diversity was partitioned among environ- including or excluding the archaeocyath sponges, which are po- ments and geographic regions. Changes in gamma diversity in the tentially oversplit (16). Alpha and beta diversity increased from Cambrian were chiefly driven by changes in beta diversity. The the Fortunian to Stage 3, and fluctuated erratically through the combined trajectories of alpha and beta diversity during the initial following stages (Fig. 2). Our estimate of alpha (and indirectly diversification suggest low competition and high predation within beta) diversity is based on the number of genera in published communities. -
Wright and Cherns Supplementary Data Flat
Wright and Cherns Supplementary Data Flat pebble conglomerates from subtidal settings (Fig. 2) PROPOSE SHELF D AGE LOCATION FORMATION SETTING PROCESS AUTHOR(S) Subtidal within Mesoproteroz China, Hebei Gaoyuzhuang storm wave oic Province Formation base storms Luo et al. 2014 Proterozoic, NW Canada, Pre-Marinoan Mackenzie mid to outer glaciation Mountains Keele Fm ramp storms Day et al. 2004 Bertrand-Sarfati Gourma, bottom & Moussine- Vendian West Africa slope currents' Pouchkine 1983 Low energy Narbonne et al. Ediacaran South Africa Swartpunt Fm deeper ramp storm 1997 Canadian MacNaughton et Ediacaran Arctic Gametrail Fm subtidal ramp storms al. 2008 shallow Kyrshabakty carbonate high energy Heubeck et al. Ediacaran Kazakhstan Formation platform events 2013 Ediacaran - Lower carbonate Grotzinger & Cambrian Oman Ara Group platform Al-Rawahi 2014 Lower South Sellick Hill Mount & Kidder Cambrian Australia Formation subtidal storms 1993 Lower Bayan Gol Fm, shallow Cambrian W Mongolia Zavkhan Basin subtidal storms Kruse et al. 1996 Lower Shuijingtuo Ishikawa et al. Cambrian South China Fm subtidal 2008 Middle Canadian Dewing & Cambrian Arctic ramp Nowlan 2012 British Middle Columbia, Cambrian Canada Jubilee Fm Pope 1990 1 Middle Pratt & Cambrian Argentina La Laja Fm subtidal shelf tsunamis Bordonaro 2007 low energy Middle shallow Cambrian Australia Ranken Lst subtidal storms Kruse 1996 Middle Wyoming, Upper Gros Cambrian USA Ventre Shale Csonka 2009 middle upper Middle W Utah, upper Wheeler, carbonate belt - Cambrian USA Marjum fms subtidal shelf Robison 1964 Middle- Upper Supratidal to Cambrian NW China subtidal fpc storms Liang et al. 1993 Ust’- Brus,Labaz, Middle Orakta, Cambrian - Kulyumbe, Lower Ujgur and Iltyk Kouchinsky et Ordovician Siberia fms al. -
Appendix 3.Pdf
A Geoconservation perspective on the trace fossil record associated with the end – Ordovician mass extinction and glaciation in the Welsh Basin Item Type Thesis or dissertation Authors Nicholls, Keith H. Citation Nicholls, K. (2019). A Geoconservation perspective on the trace fossil record associated with the end – Ordovician mass extinction and glaciation in the Welsh Basin. (Doctoral dissertation). University of Chester, United Kingdom. Publisher University of Chester Rights Attribution-NonCommercial-NoDerivatives 4.0 International Download date 26/09/2021 02:37:15 Item License http://creativecommons.org/licenses/by-nc-nd/4.0/ Link to Item http://hdl.handle.net/10034/622234 International Chronostratigraphic Chart v2013/01 Erathem / Era System / Period Quaternary Neogene C e n o z o i c Paleogene Cretaceous M e s o z o i c Jurassic M e s o z o i c Jurassic Triassic Permian Carboniferous P a l Devonian e o z o i c P a l Devonian e o z o i c Silurian Ordovician s a n u a F y r Cambrian a n o i t u l o v E s ' i k s w o Ichnogeneric Diversity k p e 0 10 20 30 40 50 60 70 S 1 3 5 7 9 11 13 15 17 19 21 n 23 r e 25 d 27 o 29 M 31 33 35 37 39 T 41 43 i 45 47 m 49 e 51 53 55 57 59 61 63 65 67 69 71 73 75 77 79 81 83 85 87 89 91 93 Number of Ichnogenera (Treatise Part W) Ichnogeneric Diversity 0 10 20 30 40 50 60 70 1 3 5 7 9 11 13 15 17 19 21 n 23 r e 25 d 27 o 29 M 31 33 35 37 39 T 41 43 i 45 47 m 49 e 51 53 55 57 59 61 c i o 63 z 65 o e 67 a l 69 a 71 P 73 75 77 79 81 83 n 85 a i r 87 b 89 m 91 a 93 C Number of Ichnogenera (Treatise Part W) -
PROGRAMME ABSTRACTS AGM Papers
The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important. -
Proposed Global Standard Stratotype-Section And
PROPOSED GLOBAL STANDARD STRATOTYPE-SECTION AND POINT FOR THE DRUMIAN STAGE (CAMBRIAN) Prepared for the International Subcommission on Cambrian Stratigraphy by: Loren E. Babcock School of Earth Sciences The Ohio State University, 125 South Oval Mall Columbus, OH 43210, USA [email protected] Richard A. Robison Department of Geology, University of Kansas Lawrence, KS 66045, USA [email protected] Margaret N. Rees Department of Geoscience University of Nevada, Las Vegas Las Vegas, NV 89145, USA [email protected] Peng Shanchi Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences 39 East Beijing Road, Nanjing 210008, China [email protected] Matthew R. Saltzman School of Earth Sciences The Ohio State University, 125 South Oval Mall Columbus, OH 43210, USA [email protected] 31 July 2006 CONTENTS Introduction …………………………………………………………………………. 2 Proposal: Stratotype Ridge, Drum Mountains (Millard County, Utah, USA) as the GSSP for the base of the Drumian Stage ……………………………………………………. 3 1. Stratigraphic rank of the boundary …………………..…………………………… 3 2. Proposed GSSP – geography and physical geology ……………………………… 3 2.1. Geographic location …………………………………………………...….. 3 2.2. Geological location ………………..……………………...…………...….. 4 2.3. Location of level and specific point ……………………..……………...… 4 2.4. Stratigraphic completeness ………………...……………………………… 5 2.5. Thickness and stratigraphic extent …………………...……………...……. 5 2.6. Provisions for conservation, protection, and accessibility ……………..…. 5 3. Motivation for selection of the boundary level and of the potential stratotype section ………………………………………………………………………………. 6 3.1. Principal correlation event (marker) at GSSP level ………...…………..… 6 3.2. Potential stratotype section …………………………………………....….. 7 3.3. Demonstration of regional and global correlation ………………………... 8 3.3.1. Agnostoid trilobite biostratigraphy ………………………………… 9 3.3.2. Polymerid trilobite biostratigraphy …………....…………….……. -
Lee-Riding-2018.Pdf
Earth-Science Reviews 181 (2018) 98–121 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Marine oxygenation, lithistid sponges, and the early history of Paleozoic T skeletal reefs ⁎ Jeong-Hyun Leea, , Robert Ridingb a Department of Geology and Earth Environmental Sciences, Chungnam National University, Daejeon 34134, Republic of Korea b Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996, USA ARTICLE INFO ABSTRACT Keywords: Microbial carbonates were major components of early Paleozoic reefs until coral-stromatoporoid-bryozoan reefs Cambrian appeared in the mid-Ordovician. Microbial reefs were augmented by archaeocyath sponges for ~15 Myr in the Reef gap early Cambrian, by lithistid sponges for the remaining ~25 Myr of the Cambrian, and then by lithistid, calathiid Dysoxia and pulchrilaminid sponges for the first ~25 Myr of the Ordovician. The factors responsible for mid–late Hypoxia Cambrian microbial-lithistid sponge reef dominance remain unclear. Although oxygen increase appears to have Lithistid sponge-microbial reef significantly contributed to the early Cambrian ‘Explosion’ of marine animal life, it was followed by a prolonged period dominated by ‘greenhouse’ conditions, as sea-level rose and CO2 increased. The mid–late Cambrian was unusually warm, and these elevated temperatures can be expected to have lowered oxygen solubility, and to have promoted widespread thermal stratification resulting in marine dysoxia and hypoxia. Greenhouse condi- tions would also have stimulated carbonate platform development, locally further limiting shallow-water cir- culation. Low marine oxygenation has been linked to episodic extinctions of phytoplankton, trilobites and other metazoans during the mid–late Cambrian. -
Abstract Volume
https://doi.org/10.3301/ABSGI.2019.04 Milano, 2-5 July 2019 ABSTRACT BOOK a cura della Società Geologica Italiana 3rd International Congress on Stratigraphy GENERAL CHAIRS Marco Balini, Università di Milano, Italy Elisabetta Erba, Università di Milano, Italy - past President Società Geologica Italiana 2015-2017 SCIENTIFIC COMMITTEE Adele Bertini, Peter Brack, William Cavazza, Mauro Coltorti, Piero Di Stefano, Annalisa Ferretti, Stanley C. Finney, Fabio Florindo, Fabrizio Galluzzo, Piero Gianolla, David A.T. Harper, Martin J. Head, Thijs van Kolfschoten, Maria Marino, Simonetta Monechi, Giovanni Monegato, Maria Rose Petrizzo, Claudia Principe, Isabella Raffi, Lorenzo Rook ORGANIZING COMMITTEE The Organizing Committee is composed by members of the Department of Earth Sciences “Ardito Desio” and of the Società Geologica Italiana Lucia Angiolini, Cinzia Bottini, Bernardo Carmina, Domenico Cosentino, Fabrizio Felletti, Daniela Germani, Fabio M. Petti, Alessandro Zuccari FIELD TRIP COMMITTEE Fabrizio Berra, Mattia Marini, Maria Letizia Pampaloni, Marcello Tropeano ABSTRACT BOOK EDITORS Fabio M. Petti, Giulia Innamorati, Bernardo Carmina, Daniela Germani Papers, data, figures, maps and any other material published are covered by the copyright own by the Società Geologica Italiana. DISCLAIMER: The Società Geologica Italiana, the Editors are not responsible for the ideas, opinions, and contents of the papers published; the authors of each paper are responsible for the ideas opinions and con- tents published. La Società Geologica Italiana, i curatori scientifici non sono responsabili delle opinioni espresse e delle affermazioni pubblicate negli articoli: l’autore/i è/sono il/i solo/i responsabile/i. ST3.2 Cambrian stratigraphy, events and geochronology Conveners and Chairpersons Per Ahlberg (Lund University, Sweden) Loren E. -
The Ediacaran–Cambrian Transition: the Emerging Record from Small Carbonaceous Fossils (Scfs)
38 The Ediacaran–Cambrian transition: the emerging record from Small Carbonaceous Fossils (SCFs) Ben J. Slater1, Thomas H.P. Harvey2, Romain Guilbaud3, Sebastian Willman1, Graham E. Budd1, Nicholas J. Butterfield4. 1Department of Earth Sciences (Palaeobiology), Uppsala University, Villavägen 16, SE-75236 Uppsala, Sweden ([email protected]) 2School of Geography, Geology and the Environment, University of Leicester, Leicester LE1 7RH, UK 3Lancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, UK. 4Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK Abstract.––The most profound change in the fossil record is centered on the Ediacaran–Cambrian transition. Sediments deposited near to this boundary record the first complex trace fossils, the first animal biomineralizers and the earliest fossils of the major animal groups that came to define the subsequent Phanerozoic fossil record. Here we discuss how the emerging record of small carbonaceous fossils (SCFs) is shedding new light on unmineralized aspects of the biota from this critical evolutionary transition. The new SCFs record complements currently established records from trace fossils and biomineralized shelly-remains in reconstructing the broader scale macroevolutionary patterns of this transition, but via an entirely different taphonomic window. SCFs extend the record of multiple major animal groups, improve our picture of protistan diversity from this interval, and reveal new data on elements of the biota that span the Ediacaran–Cambrian boundary. Key words: small carbonaceous fossils; bilateria; Burgess Shale-type preservation; Ediacaran; Terreneuvian. The dramatic changes in the fossil record across subsequent Cambrian radiation (Butterfield, the Ediacaran–Cambrian transition seemingly 2003; Slater et al., 2018a). -
Ediacaran and Cambrian Stratigraphy in Estonia: an Updated Review
Estonian Journal of Earth Sciences, 2017, 66, 3, 152–160 https://doi.org/10.3176/earth.2017.12 Ediacaran and Cambrian stratigraphy in Estonia: an updated review Tõnu Meidla Department of Geology, Institute of Ecology and Earth Sciences, Faculty of Science and Technology, University of Tartu, Ravila 14a, 50411 Tartu, Estonia; [email protected] Received 18 December 2015, accepted 18 May 2017, available online 6 July 2017 Abstract. Previous late Precambrian and Cambrian correlation charts of Estonia, summarizing the regional stratigraphic nomenclature of the 20th century, date back to 1997. The main aim of this review is updating these charts based on recent advances in the global Precambrian and Cambrian stratigraphy and new data from regions adjacent to Estonia. The term ‘Ediacaran’ is introduced for the latest Precambrian succession in Estonia to replace the formerly used ‘Vendian’. Correlation with the dated sections in adjacent areas suggests that only the latest 7–10 Ma of the Ediacaran is represented in the Estonian succession. The gap between the Ediacaran and Cambrian may be rather substantial. The global fourfold subdivision of the Cambrian System is introduced for Estonia. The lower boundary of Series 2 is drawn at the base of the Sõru Formation and the base of Series 3 slightly above the former lower boundary of the ‘Middle Cambrian’ in the Baltic region, marked by a gap in the Estonian succession. The base of the Furongian is located near the base of the Petseri Formation. Key words: Ediacaran, Cambrian, correlation chart, biozonation, regional stratigraphy, Estonia, East European Craton. INTRODUCTION The latest stratigraphic chart of the Cambrian System in Estonia (Mens & Pirrus 1997b, p. -
The Auxiliary Boundary Stratotype Section and Point (ASSP) of the Jiangshanian Stage (Cambrian: Furongian Series) in the Kyrshabakty Section
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/261721078 The Auxiliary boundary Stratotype Section and Point (ASSP) of the Jiangshanian Stage (Cambrian: Furongian Series) in the Kyrshabakty section Article in Episodes · March 2014 DOI: 10.18814/epiiugs/2014/v37i1/005 CITATION READS 1 238 7 authors, including: Leonid E. Popov Michael G. Bassett National Museum Wales National Museum of Wales 296 PUBLICATIONS 3,956 CITATIONS 46 PUBLICATIONS 557 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Early Palaeozoic brachiopods and associated faunas of CAOB. View project Cambrian-Ordovician Boundary View project All content following this page was uploaded by Leonid E. Popov on 21 April 2014. The user has requested enhancement of the downloaded file. 41 by Gappar Kh. Ergaliev1, Vyacheslav (Slava) G. Zhemchuzhnikov2, Leonid E. Popov3, Michael G. Bassett3 and Farkhat G. Ergaliev4 The Auxiliary boundary Stratotype Section and Point (ASSP) of the Jiangshanian Stage (Cambrian: Furongian Series) in the Kyrshabakty section, Kazakhstan 1 K.I.Satpaev Institute of Geological Sciences, Kabanbai Batyra Street, 69-a, 050010 Almaty, Kazakhstan. E-mail: [email protected] 2 North Caspian Oil Development LLP, Almaty, Kazakhstan. E-mail: [email protected] 3 Department of Geology, National Museum of Wales, Cathays Park, Cardiff CF10 3NP, Wales, United Kingdom. E-mail: [email protected] 4 Dala Mining (TMM International), Koshek-Batyra Street, 5, 050010 Almaty Kazakhstan. E-mail: [email protected] The Kyrshabakty section in the Malyi Karatau Range, Union of Geological Sciences (IUGS). The GSSP for the stage, now southern Kazakhstan, has been approved as the Auxiliary known as the Jiangshanian (formerly provisional Stage 9) is located in the Duibian B section, Zhejiang, China (Peng et al., 2012). -
PHYLOGENY and DISTRIBUTION by LARS E
[Papers in Palaeontology, 2019, pp. 1–17] CAMBRIAN RHYNCHONELLIFORM NISUSIOID BRACHIOPODS: PHYLOGENY AND DISTRIBUTION by LARS E. HOLMER1,2 , MOHAMMAD-REZA KEBRIA-EE ZADEH3, LEONID E. POPOV4, MANSOUREH GHOBADI POUR2,4,5,J.JAVIERALVARO 6, VACHIK HAIRAPETIAN7 and ZHIFEI ZHANG1 1Shaanxi Key Laboratory of Early Life & Environments, State Key Laboratory for Continental Dynamics, Northwest University, Xi’an, 710069, China 2Department of Earth Sciences, Palaeobiology, SE-752 36, Uppsala, Sweden; [email protected] 3Department of Geology, Payame Noor University, Semnan, Iran; [email protected] 4Department of Earth Sciences, National Museum of Wales, Cathays Park, Cardiff, CF10 3NP, UK; [email protected] 5Department of Geology, Faculty of Sciences, Golestan University, Gorgan, 49138-15739, Iran; [email protected] 6Instituto de Geociencias (CSIC-UCM), Dr. Severo Ochoa 7, Madrid, 28040, Spain; [email protected] 7Department of Geology, Khorasgan (Isfahan) Branch, Islamic Azad University, PO Box 81595-158, Isfahan, Iran; [email protected] Typescript received 18 July 2018; accepted in revised form 6 November 2018 Abstract: A comprehensive review and phylogenetic analy- an early separation of the lineages of spinose and non-spi- sis of genera and species presently assigned to the rhyn- nose nisusiids. The non-spinose nisusiids probably evolved chonelliform superfamily Nisusioidea and family Nisusiidae in Laurentia by the end of Cambrian Series 4. The new suggests that this short-lived but important group of bra- nisusiid genus Bellistrophia is described. The new species chiopods first appeared in peri-Gondwana during the second Nisusia multicostata represents the first documented rhyn- half of the Cambrian Series 2, before going extinct by the chonelliform (kutorginide) brachiopod from the Miaolingian end of Drumian times. -
Systematics, Biogeography and Palaeoecology of Cambrian Series 3 Trilobites and Agnostids from East Gondwana
University of New England SYSTEMATICS, BIOGEOGRAPHY AND PALAEOECOLOGY OF CAMBRIAN SERIES 3 TRILOBITES AND AGNOSTIDS FROM EAST GONDWANA by Lee Ann Hally B. Ed (Charles Sturt Uni., Bathurst. July 1977) B. Sc (Macquarie Uni., Sydney. March 1984) M. Sc (Macquarie Uni., Sydney. March 1989) This thesis is submitted to fulfill the requirements for the degree of Doctor of Philosophy from the University of New England. October 2015 Declaration All work submitted is solely for a PhD at University of New England, Armidale. NSW. All assistance for this PhD and all sources used in its preparation are duly acknowledged. Signature Lee Ann Hally October 2015 i Acknowledgements I am ever grateful to my supervisor, Dr. J.R. Paterson, for his phronesis in the art of palaeontology and his love of teaching his craft. He has been an inspiration and his guidance always caused me to reflect and grow in my own way. I am forever grateful for his support and guidance, as well as his friendship. I thank my assistant supervisor, Dr. I. Metcalfe, for his valuable comments and discussions and Dr. N. Vickery for her support in many ways over the four years of my PhD. I owe the initial inspiration for this research to my undergraduate and postgraduate lecturers at Macquarie University, Prof. John Talent and A. Prof. Ruth Mawson. They created a passion in me which drove me to greater heights and I am forever grateful. I owe much of my development over the period of undertaking my PhD, to my husband Steve’s tolerance, humour and good cooking! His knowledge of all animals, even agnostids, is amazing! I thank Drs.