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Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California
Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California By Paul Stone, Calvin H. Stevens, Paul Belasky, Isabel P. Montañez, Lauren G. Martin, Bruce R. Wardlaw, Charles A. Sandberg, Elmira Wan, Holly A. Olson, and Susan S. Priest Pamphlet to accompany Scientific Investigations Map 3298 2014 U.S. Department of the Interior U.S. Geological Survey Cover View of Marble Canyon area, California, showing dark rocks of Mississippian Indian Springs Formation and Pennsylvanian Bird Spring Formation overlying light rocks of Mississippian Santa Rosa Hills Limestone in middle distance. View is southeast toward Emigrant Wash and Tucki Mountain in distance. U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Stone, P., Stevens, C.H., Belasky, P., Montanez, I.P., Martin, L.G., Wardlaw, B.R., Sandberg, C.A., Wan, E., Olson, H.A., and Priest, S.S., 2014, Geologic map and upper Paleozoic stratigraphy of the Marble Canyon area, Cottonwood Canyon quadrangle, Death Valley National Park, Inyo County, California: U.S. Geological Survey Scientific Investigations Map 3298, scale 1:24,000, 59 p., http://dx.doi.org/10.3133/sim3298. -
On Some Occurrences of Diplognathodus in Carboniferous Strata of Western Europe and North Africa
v.d. Boogaard, Diplognathodus from W. Europe & N. Africa, Scripta Geol., 69 (1983) On some occurrences of Diplognathodus in Carboniferous strata of Western Europe and North Africa M. van den Boogaard Boogaard, M. van den. On some occurrences of Diplognathodus in Carboniferous strata of Western Europe and North Africa. - Scripta Geol., 69: 19-29, 1 fig., 1 pl., October 1983. The occurrence is reported of Diplognathodus coloradoensis, D. orphanus and D. ellesmerensis in some localities in Western Europe and one locality in North Afri- ca. M. van den Boogaard, Rijksmuseum van Geologie en Mineralogie, Hooglandse Kerkgracht 17, 2312 HS Leiden, The Netherlands. Introduction 19 Localities 20 Palaeontology 23 Concluding remarks 25 References 27 Introduction Species of the genus Diplognathodus may be useful for stratigraphie correlation of Carboniferous strata because some of them are probably stratigraphically short-ranging (e.g. D. coloradoensis according to Landing & Wardlaw, 1981, pp. 1255-1256). Because still little is known about the distribution of représentants of the genus outside North America I thought it useful to relate the few occur• rences of D. coloradoensis, D. orphanus and D. ellesmerensis I encountered during my investigation of Carboniferous limestones from Western Europe and North Africa. 20 v.d. Boogaard, Diplognathodus from W. Europe & N. Africa, Scripta Geol., 69 (1983) Acknowledgements Thanks for placing the samples at my disposal are due to Drs C.F. Winkler Prins, H.A. van Adrichem Boogaert, M.J.M. Bless, and A.C. van Ginkel. The informa• tion concerning the Cinderhill sample given by Dr W.H.C. Ramsbottom is much appreciated. Thanks also go to Mr J.G.M. -
Pander Society Newsletter
Pander Society Newsletter Compiled and edited by R. J. Aldridge, M. A. Purnell, and A. Thomas DEPARTMENT OF GEOLOGY UNIVERSITY OF LEICESTER LEICESTER LE1 7RH, UK Number 36 May 2004 www.conodont.net INTRODUCTORY REMARKS fter six very rewarding years, this is the last NEW CHIEF PANDERER Pander Society Newsletter to be presented by the Acurrent team. This makes it, perhaps, fitting for Dick Aldridge writes: In January 2004, I recognised that, us to begin our annual introduction by looking back to having entered my sixth year as President of the Pander see how the Society has fared over this interval. The Society ('Chief Panderer'), it was really past my time to answer is, we have certainly all been very active. The hand over to a successor. There is no stipulated length of period started with a bang (pun too bad to be intended) service in this office, but we have tried to make five in 1998 with a Pander Society meeting in Columbus, years more-or-less the norm, in order to share the Ohio, with the themes ‘Conodont evidence for impacts honour and the chore. Following traditional procedure, I and extinctions’ and ‘Hot topics in conodont asked three active members of the Society, Phil biochronology’. The same year, ECOS VII was held in Donoghue, Catherine Girard and Jeff Over, to act as a Italy, continuing the very successful pattern of these nomination committee, and asked anyone who wished events. Annual Pander Society meetings have continued to make a nomination or to contribute thoughts or in North America in each succeeding year, comments about the succession to contact them. -
Permian (Artinskian to Wuchapingian) Conodont Biostratigraphy in the Tieqiao Section, Laibin Area, South China
Permian (Artinskian to Wuchapingian) conodont biostratigraphy in the Tieqiao section, Laibin area, South China Y.D. Suna, b*, X.T. Liuc, J.X. Yana, B. Lid, B. Chene, D.P.G. Bondf, M.M. Joachimskib, P.B. Wignallg, X.L. Laia a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China b GeoZentrum Nordbayern, Universität Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen, Germany c Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China d Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Ministry of Land and Resources, Guangzhou, 510075, China e State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, 39 East Beijing Road, Nanjing, 210008, R.P. China f School of Environmental Sciences, University of Hull, Hull HU6 7RX, UK g School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK *Corresponding authors Email: [email protected] (Y.D. Sun) © 2017, Elsevier. Licensed under the Creative Commons Attribution- NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/ licenses/by-nc-nd/4.0/ 1 Abstract Permian strata from the Tieqiao section (Jiangnan Basin, South China) contain several distinctive conodont assemblages. Early Permian (Cisuralian) assemblages are dominated by the genera Sweetognathus, Pseudosweetognathus and Hindeodus with rare Neostreptognathodus and Gullodus. Gondolellids are absent until the end of the Kungurian stage—in contrast to many parts of the world where gondolellids and Neostreptognathodus are the dominant Kungurian conodonts. A conodont changeover is seen at Tieqiao and coincided with a rise of sea level in the late Kungurian to the early Roadian: the previously dominant sweetognathids were replaced by mesogondolellids. -
Permophiles Issue #58 November 2013 EXECUTIVE NOTES Notes from the SPS Secretary Museum of Natural History and Science, Albuquerque, New Mexico, USA, May 20-22, 2013
Table of Contents Notes from the SPS Secretary 1 Lucia Angiolini Notes from the SPS Chair 2 Shuzhong Shen Subcommission on Permian Stratigraphy Annual Report 2013 3 Shuzhong Shen, SPS Chairman Officers and Voting Members since August, 2012 5 The Reality of GSSPs 6 Stanley C. Finney GSSPs (Global Stratotype Section and Point) and Correlation 8 Stanley C. Finney We Need a New GSSP for the Base of the Permian 8 Spencer G. Lucas The GSSP at the Aidaralash section is solid and has no alternative 13 Vladimir I. Davydov The Aidaralash GSSP—Reply to Davydov 15 Spencer G. Lucas Proposal for the Global Stratotype Section and Point (GSSP) for the base-Sakmarian Stage (Lower Permian) 16 Valery V. Chernykh, Boris I. Chuvashov, Shuzhong Shen andCharles M. Henderson Proposal for the Global Stratotype Section and Point (GSSP) for the base-Artinskian Stage (Lower Permian) 26 Boris I. Chuvashov, Valery V. Chernykh, Shuzhong Shen and Charles M. Henderson Report of the Chinese, Iranian, Italian working group: The Permian-Triassic boundary sections of Julfa and Zal revisited 34 Lucia Angiolini, Shuzhong Shen, Maryamnaz Bahrammanesh, Syrus Abbasi, Mina Birjandi, Gaia Crippa, Dongxun Yuan and Claudio Garbelli Age assignment of section 4 of Teichert et al. (1973) at Ali Bashi Mountains (Julfa, NW Iran) 36 Abbas Ghaderi, Ali Reza Ashouri, Heinz W. Kozur and Dieter Korn Report of field excursions 2012/2013 of the “Sino-German Cooperation Group on the Late Palaeozoic Palaeobiology, Stratigraphy and Geochemistry” between Europe and China 40 Jun Wang, Shuzhong Shen, Joerg W. Schneider and Hans Kerp ANNOUNCEMENTS 42 SUBMISSION GUIDELINES FOR ISSUE 59 44 Photo 1: The Permian-Triassic succession of the Ali Bashi Mountains, Julfa, NW Iran. -
BIASES in INTERPRETATION of the FOSSIL RECORD of CONODONTS by MARK A
[Special Papers in Palaeontology, 73, 2005, pp. 7–25] BETWEEN DEATH AND DATA: BIASES IN INTERPRETATION OF THE FOSSIL RECORD OF CONODONTS by MARK A. PURNELL* and PHILIP C. J. DONOGHUE *Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK; e-mail: [email protected] Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK; e-mail: [email protected] Abstract: The fossil record of conodonts may be among and standing generic diversity. Analysis of epoch ⁄ stage-level the best of any group of organisms, but it is biased nonethe- data for the Ordovician–Devonian interval suggests that less. Pre- and syndepositional biases, including predation there is generally no correspondence between research effort and scavenging of carcasses, current activity, reworking and and generic diversity, and more research is required to bioturbation, cause loss, redistribution and breakage of ele- determine whether this indicates that sampling of the cono- ments. These biases may be exacerbated by the way in which dont record has reached a level of maturity where few genera rocks are collected and treated in the laboratory to extract remain to be discovered. One area of long-standing interest elements. As is the case for all fossils, intervals for which in potential biases and the conodont record concerns the there is no rock record cause inevitable gaps in the strati- pattern of recovery of different components of the skeleton graphic distribution of conodonts, and unpreserved environ- through time. We have found no evidence that the increas- ments lead to further impoverishment of the recorded ing abundance of P elements relative to S and M elements spatial and temporal distributions of taxa. -
Paper Number: 4008
Paper Number: 4008 Characterization of conodont biostratigraphy in the basal Moscovian boundary interval at the Naqing section, Loudian, Guizhou, South China Lambert, L. L.1, Qi, Y. P.2, Nemyrovska, T. I.3, Wang, X. D.2, Hu, K. Y.2, and Wang, Q. L.2 1Geological Sciences, University of Texas at San Antonio, One UTSA Circle, San Antonio, TX 78249, USA [email protected] 2State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, PR China 3Institute of Geological Sciences, National Academy of Sciences of Ukraine, O. Gonchar Str. 55-b, 01601 Kiev, Ukraine ___________________________________________________________________________ A major criterion for selecting a Global Stratotype Section and Point (GSSP) is to demonstrate depositional continuity. Depositional continuity is most often accepted where there is a transitional morphocline from an ancestral species to its descendent. The GSSP is then selected to correspond with the phylogenetic first occurrence of the descendent species. Ideally, strata elsewhere are subsequently correlated with the GSSP using the local first appearance of the descendent species, or by other taxa associated with the GSSP providing supplementary biostratigraphic data. Any other stratigraphic methods can be used for correlation once the GSSP has been ratified by the International Union of Geological Sciences Commission on Stratigraphy. Multiple conodont lineages with complete transitional morphologies characterize the Bashkirian- Moscovian boundary interval in the Naqing section. The presence of all these chronoclines through the section demonstrates depositional continuity at Naqing, and provides numerous possible conodont- based levels available for selecting a basal Moscovian GSSP. -
Ian, and the Early Upper Devonian Some Icriodus Species Such As
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ian, and the early Upper Devonian some Icriodus species such as /. fusiformis, I. culicellus, I. rectiro- stratus, I. retrodepressus, I. regularicrescens, I. obliquimarginatus and /. subterminus have a wide or so metimes nearly cosmopolite dispersion in different magnafacies areas (type Ardenno-Rhenish and Her- cynian-Bohemian) and there is no marked difference in the earliest occurrence of each species. This means that the geographical dispersion of at least some Icriodus species was due primarily to good com munication seaways which could be modified in the course of time and not to very specialised local fa des factors. Having in mind the SEDDON and SWEET model for conodonts, the dominance of Icrio dus in shallow water shelf environment implies no restriction in geographical dispersion. Particularly in this environment, anomalies in the vertical distribution ofPolygnathus taxa, e. g.,-P. serotinus, P. lingui- formis div. subspecies, P. cooperi cooperi can be noticed. Reexamination of Late Pennsylvanian and Early Permian Conodont Apparatuses Using Clustering Techniques. By T. R. CARR Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706, USA. Conodont faunas containing easily identified Pa elements assignable to the genera Diplognathodus and Hindeodus have been reported from Upper Pennsylvanian and Lower Permian strata of North Ame rica. If the seximembrate model for the apparatus of each genus is correct, the remaining elements should also be present. However, previous investigators have normally considered ramiform elements which might be assignable to the two genera as attributable to species of either the Idiognathodus— Streptognathodus plexus or Adetognathus. -
Pander Society Newsletter
Pander Society Newsletter S O E R C D I E N T A Y P 1 9 6 7 Compiled and edited by P.H. von Bitter and J. Burke PALAEOBIOLOGY DIVISION, DEPARTMENT OF NATURAL HISTORY, ROYAL ONTARIO MUSEUM, TORONTO, ON, CANADA M5S 2C6 Number 41 May 2009 www.conodont.net Webmaster Mark Purnell, University of Leicester 2 Chief Panderer’s Remarks May 1, 2009 Dear Colleagues: It is again spring in southern Canada, that very positive time of year that allows us to forget our winter hibernation & the climatic hardships endured. It is also the time when Joan Burke and I get to harvest and see the results of our winter labours, as we integrate all the information & contributions sent in by you (Thank You) into a new and hopefully ever better Newsletter. Through the hard work of editor Jeffrey Over, Paleontographica Americana, vol. no. 62, has just been published to celebrate the 40th Anniversary of the Pander Society and the 150th Anniversary of the first conodont paper by Christian Pander in 1856; the titles and abstracts are here reproduced courtesy of the Paleontological Research Institution in Ithica, N.Y. Glen Merrill and others represented the Pander Society at a conference entitled “Geologic Problem Solving with Microfossils”, sponsored by NAMS, the North American Micropaleontology Section of SEPM, in Houston, Texas, March 15-18, 2009; the titles of papers that dealt with or mentioned conodonts, are included in this Newsletter. Although there have been no official Pander Society meetings since newsletter # 40, a year ago, there were undoubtedly many unofficial ones; many of these would have been helped by suitable refreshments, the latter likely being the reason I didn’t get to hear about the meetings. -
A Database of Triassic Conodonts from a Comprehensive Revision of Literature
SPANISH JOURNAL OF PALAEONTOLOGY A database of Triassic conodonts from a comprehensive revision of literature Pablo PLASENCIA1,2*, Ana MÁRQUEZ-ALIAGA2 & Jingeng SHA1 1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology (CAS), Nanjing, 39 East Beijing Road, Nanjing, 210008, People’s Republic of China; [email protected]; [email protected] 2 Departamento de Geología, Universitat de Valencia, Dr. Moliner, 50, 46100 Burjassot, Valencia, Spain; [email protected] * Corresponding author Plasencia, P., Márquez-Aliaga, A. & Sha, J. 2013. A data base of Triassic conodonts from a comprehensive revision of literature. [Una base de datos de conodontos triásicos a partir de una completa revisión de la literatura]. Spanish Journal of Palaeontology, 28 (2), 215-226. Manuscript received 08 September 2012 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 19 December 2012 ABSTRACT RESUMEN The revision of a comprehensive amount of bibliography La revisión de una amplia cantidad de bibliografía ha hecho has made possible the development of a database containing posible el desarrollo de una base de datos en la que fi guran los the stratigraphic ranges of the conodont species from the rangos estratigráfi cos de las especies de conodontos presentes uppermost Permian and the Triassic, with a total of 336 species desde el Pérmico superior y el Triásico, con un total de 336 in 52 genera. This database is aimed at biostratigraphy and especies y 52 géneros. Esta base de datos está dirigida a la studies related to biological, evolutional and palaeodiversity bioestratigrafía y a estudios relacionados con las dinámicas dynamics. -
First Occurrence of Ellisonia, Gondolella and Ubinates (Conodonts) in Itaituba Formation, Pennsylvanian of Amazonas Basin, Brazil
6(2):56-62, jul/dez 2010 © Copyright 2010 by Unisinos - doi: 10.4013/gaea.2010.62.01 First occurrence of Ellisonia, Gondolella and Ubinates (Conodonts) in Itaituba Formation, Pennsylvanian of Amazonas Basin, Brazil Sara Nascimento, Valesca Brasil Lemos Universidade Federal do Rio Grande do Sul. Av. Bento Gonçalves, 9500, Prédio 43.127, sala 211, 91501-470, Porto Alegre, RS, Brasil. [email protected], [email protected] Ana Karina Scomazzon Universidade Federal de Pelotas. Rua Domingos Rodrigues, 2, 96010-440, Pelotas, RS, Brasil. [email protected] Nilo Siguehiko Matsuda PETROBRAS/E&P-EXP/GEO/ES. Av. Chile, 330, Edifício Ventura, 13º andar, 20031-170, Rio de Janeiro, RJ, Brasil. [email protected] Cristiane Pakulski da Silva Universidade Federal do Rio Grande do Sul. Av. Bento Gonçalves, 9500. Prédio 43.127, sala 211, 91501-470, Porto Alegre, RS, Brasil. [email protected] ABSTRACT This paper analyzes and describes a fi rst occurrence of the conodonts Ellisonia, Gondolella and Ubinates in Amazonas Basin, North of Brazil. The recovered material comes from two outcrops along the Tapajos River and from a limestone quarry of Itaituba Formation, whose levels are in- cluded in the Itaituba Formation, with a Pennsylvanian age. Those conodonts are relevant paleoecological indicators of water depth, salinity and environmental energy and have implications in the Late Carboniferous to Triassic biostratigraphy. The fossil remains represent M and S conodont elements, associated to Pa elements of the Idiognathodus, Idiognathoides, Neognathodus, Adetognathus, Hindeodus and Diplognathodus genus. Key words: conodonts, Amazonas Basin, Itaituba Formation, Pennsylvanian. RESUMO PRIMEIRA OCORRÊNCIA DOS GÊNEROS ELLISONIA, GONDOLELLA E UBINATES (CONODONTS) PARA A FORMAÇÃO ITAITUBA, PENSILVANIANO DA BACIA DO AMAZONAS, BRASIL. -
Pander Society Newsletter
Pander Society Newsletter Compiled and edited by P.H. von Bitter and J. Burke DEPARTMENT OF NATURAL HISTORY (PALAEOBIOLOGY SECTION), ROYAL ONTARIO MUSEUM, TORONTO, ONTARIO, CANADA M5S 2C6 Number 38 June 2006 www.conodont.net CHIEF PANDERER’S REMARKS Dear Conodont Colleagues: A year has gone by since I last communicated like this, and I’m pleased (and relieved) that another Pander Society Newsletter is ready to ‘go’. Thank you for having sent in your reports and questionnaires; without your willingness to going through a bit of pain there would be no Pander Society Newsletter, and our communications would be the poorer. I am very grateful to compiler and editor Joan Burke (Toronto) and webmaster Mark Purnell (Leicester) for their dedication and ongoing interest; they have helped me greatly and continue to make me look better than I really am, particularly in a time of personal and professional transition. You, the Pander Society membership, continue to ‘re-invent’ and apply conodonts in startling new ways. Some of this re-invention was seen at the Pander Society Symposium in Harrisburg, Pennsylvania, where on March 20-22, 2006 our (mostly) North American members focused on Conodonts & Sequence Stratigraphy. Looking ahead, the programme of ICOS 2006 on July 12-30/ 2006 in Leicester, England, promises not only to surprise and delight, but looks remarkably diverse and imaginative. Christian Pander, would, on the 150th anniversary of the publication of his major conodont study, no doubt be enormously impressed and pleased with the innovativeness and progress of his intellectual grandchildren. My best wishes to all of you.