U.S. Oeoxogijcal SUB.Vklir PROFESSIONAL PAPEE AVAILABILITY of BOOKS and MAPS of the U.S

Total Page:16

File Type:pdf, Size:1020Kb

U.S. Oeoxogijcal SUB.Vklir PROFESSIONAL PAPEE AVAILABILITY of BOOKS and MAPS of the U.S f~\r/% OI U.S. OEOXOGIjCAL SUB.VKlir PROFESSIONAL PAPEE AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the cur­ rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur­ vey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month­ ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL n , OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, publications of general in- Books of the U.S. Geological Survey are available over the terest (such as leaflets, pamphlets, booklets), single copies of Earthquakes counter at the following Geological Survey Public Inquiries Offices, all & Volcanoes, Preliminary Determination of Epicenters, and some mis- of which are authorized agents of the Superintendent of Documents: cellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from WASHINGTON, D.C.-Main Interior Bldg., 2600 corridor, 18th and CSts.,NW. U.S. Geological Survey, Books and Open-File Reports DENVER, Colorado-Federal Bldg., Rm. 169,1961 Stout St. Federal Center, Box 25425 . LOS ANGELES, California-Federal Bldg., Rm. 7638,300 N. Denver, CO 80225 Los Angeles St. MENLO PARK, California-Bldg. 3 (Stop 533), Rm. 3128, Subscriptions to periodicals (Earthquakes & Volcanoes and 345 Middlefield Rd. Preliminary Determination of Epicenters) can be obtained ONLY from RESTON, Virginia-503 National Center, Rm. 1C402,12201 the Sunrise Valley Dr. SALT LAKE CITY, Utah-Federal Bldg., Rm. 8105,125 Superintendent of Documents South State St. Government Printing Office - SAN FRANCISCO, California-Customhouse, Rm. 504,555 Washington, D.C. 20402 Battery St. SPOKANE, Washington~U.S. Courthouse, Rm. 678, West (Check or money order must be payable to Superintendent of Docu- 920 Riverside Ave.. ments.) . ANCHORAGE, AIaska~Rm. 101,4230 University Dr. ANCHORAGE, Alaska-Federal Bldg, Rm. E-146, 701 C St. Maps For maps, address mail orders to U.S. Geological Survey, Map Distribution Maps Federal Center, Box 25286 Maps may ^ purchased over the counter at the U.S. Geologi- Denver, CO 80225 cal 5^^^ Offices where books are sold (all addresses in above list) and at the following Geological Survey offices: Residents of Alaska may order maps from ROLLA, Missouri-1400 Independence Rd. Alaska Distribution Section, U.S. Geological Survey, . DENVER, Colorado-Map Distribution, Bldg. 810, Federal New Federal Building - Box 12 Center 101 Twelfth Ave., Fairbanks, AK 99701 . FAIRBANKS, Alaska-New Federal Bldg., 101 Twelfth Ave. Paleontology of Late Proterozoic and Early Cambrian Rocks of East-Central Alaska By CAROL WAGNER ALLISON U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1449 A total of37 species-level taxa referable to the bacteria, cyanobacteria, algae, acritarcha, fungi, port/era, coelenterata or arthropoda, and one trace fossil from Late Proterozoic and Early Cambrian nonstromatolitic horizons in east-central Alaska are described and compared with similar fossils elsewhere UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1988 U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade names and trademarks in this publication is for descriptive purposes only and does not constitute endorsement by the U.S. Geological Survey Library of Congress Cataloging-in-Publication Data Allison, Carol Wagner. Paleontology of Late Proterozoic and Early Cambrian rocks of east-central Alaska. (Paleontology of Alaska) (Geological Survey professional paper ; 1449) Bibliography: p. Supt. of Docs.: 19.16:1449 1. Paleontology Precambrian. 2. Paleontology Cambrian. 3. Paleontology Alaska. I. Title. II. Series. HI. Series: Geological Survey professional paper ; 1449. QE724.A45 1988 560'.1'71 86-600399 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Abstract --------------------------- 1 Systematic paleontology Continued Introduction ------------------------- 1 Protista Incertae Sedis Continued Acknowledgments -------------------- 3 Type F------------------------ 27 General stratigraphy and collecting areas ---------- 3 Type G------------------------ 28 Eagle area ------------------------ 3 Fungi -------------------------- 28 Tatonduk area ---------------------- 4 Phycomycetae -------------------- 28 Nation area ----------------------- 7 ?0rder Saprolegniales -------------- 28 Woodchopper area -------------------- 9 Genus Cylindromyces ------------ 28 Correlation ------------------------ 10 Cylindromyces septatus- --------- 29 Paleontology ------------------------- 10 ?Fungi Imperfecti -------------------- 30 Sampling procedures ------------------- 11 Order Fungi Sporae Dispersae ------------ 30 Laboratory procedures ------------------ 13 Family Monocellae ---------------- 30 Interpretation ---------------------- 13 Oval Spore Type A-------------- 30 Sample repository -------------------- 13 Oval Spore Type B-------------- 31 Systematic paleontology ------------------- 14 ?Fungi -------------------------- 31 Bacteria ------------------------- 14 Type A------------------------ 31 Genus Eoastrion ------------------- 14 Type B------------------------ 32 lEoastrion sp. ------------------ 14 Porifera ------------------------- 33 Cyanobacteria ---------------------- 15 Incertae Sedis -------------------- 33 ?0rder Pleurocapsales ---------------- 15 ?Porifera ------------------------- 33 Genus Sphaerocongregus ------------- 15 Unnamed multirayed form -------------- 33 Sphaerocongregus variabilis --------- 15 Family Chancelloriidae ---------------- 34 1 Sphaerocongregus sp. ------------ 17 Genus Chancelloria --------------- 34 Genus Bavlinella ----------------- 17 Chancelloria sp. --------------- 34 Bavlinella sp., Nation area ---------- 17 IChancelloria Type A- ------------ 36 Bavlinella sp., Eagle area ---------- 18 IChancelloria Type B------------- 36 Sphaerocongregus and Bavlinella -------- 19 Coelenterata ----------------------- 36 Biologic affinity --------------- 19 Class Anthozoa ------------------- Age --------------------- 36 19 Genus Tabulaconus- --------------- 36 Order Nostocales ------------------- 19 Tabulaconus kordeae ------------- 36 Family Nostocaceae --------------- 19 ?Arthropoda ----------------------- 37 Genus Paleonostocalia ------------ 19 Type A- ----------------------- 37 Paleonostocalia irregularia -------- 20 Type B------------------------ ?Cyanobacteria ---------------------- 21 37 Filament Type A------------------- Type C------------------------ 37 21 Metazoa Incertae Sedis ----------------- Filament Type B - - - - - 37 21 Brabbinthes churkini ----------------- Filament Type C - - - - - 22 37 Incertae Sedis ---------------------- Coccoid Type A ----- 22 38 tOldhamia ---------------------- Coccoid Type B ----- 23 38 Type A------------------------ Acritarcha ---------- 23 39 Type B------------------------ Acanthomorphitae 23 39 Acanthomorph Type A 23 Type C------------------------ 39 Acanthomorph Type B-------------- 24 References Cited ----------------------- 40 Protista Incertae Sedis 24 Appendix A Locality descriptions -------------- 44 Type A------- 24 Appendix B Thin-section coordinates for specimens Type B------- 24 illustrated on plates ------------------- 46 Type C------- 25 Appendix C Coordinates for lower left corner of cover slips Type D------- 25 of thin sections --------------------- 48 Type E ------- 26 Index ---------------------------- 49 ILLUSTRATIONS [Plates follow index] PLATE 1. lEoastrion, Tatonduk area. 2. Bavlinella, Obruchevella, other cyanobacterial, protistan, and fungal(?) microfossils, Tatonduk and Eagle areas. 3. Paleonostocalia, Nation area. 4. Paleonostocalia and cyanobacterial(?) microfossils, Nation area. Ill IV CONTENTS PLATE 5. ?Fungi, Nation area. 6. Chancelloria and enigmatic thready structures, Nation area. 7. 1'Chancelloria and stauract spicules, Nation area. 8. Enigmatic thready structures, Nation area. 9. ?Arthropoda and Incertae Sedis, Nation area. 10. Brabbinthes, Nation area. 11. Protista, ?Porifera, and enigmatic microfossils, Nation area. 12. Cylindromyces, Sphaerocongregus, and protistan microfossils, Woodchopper area. 13. Sphaerocongregus, ?Fungi, Woodchopper area. 14. Sphaerocongregus, ?Fungi, Woodchopper area. 15. Sphaerocongregus, Woodchopper area. 16. Sphaerocongregus and protistan microfossils, Woodchopper area. 17. Acanthomorph acritarchs and other protistan microfossils, Woodchopper area. 18. Oldhamia, lOldhamia, Tabulaconus, and ?Arthropoda; Tatonduk, Nation, and
Recommended publications
  • Early Sponge Evolution: a Review and Phylogenetic Framework
    Available online at www.sciencedirect.com ScienceDirect Palaeoworld 27 (2018) 1–29 Review Early sponge evolution: A review and phylogenetic framework a,b,∗ a Joseph P. Botting , Lucy A. Muir a Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, China b Department of Natural Sciences, Amgueddfa Cymru — National Museum Wales, Cathays Park, Cardiff CF10 3LP, UK Received 27 January 2017; received in revised form 12 May 2017; accepted 5 July 2017 Available online 13 July 2017 Abstract Sponges are one of the critical groups in understanding the early evolution of animals. Traditional views of these relationships are currently being challenged by molecular data, but the debate has so far made little use of recent palaeontological advances that provide an independent perspective on deep sponge evolution. This review summarises the available information, particularly where the fossil record reveals extinct character combinations that directly impinge on our understanding of high-level relationships and evolutionary origins. An evolutionary outline is proposed that includes the major early fossil groups, combining the fossil record with molecular phylogenetics. The key points are as follows. (1) Crown-group sponge classes are difficult to recognise in the fossil record, with the exception of demosponges, the origins of which are now becoming clear. (2) Hexactine spicules were present in the stem lineages of Hexactinellida, Demospongiae, Silicea and probably also Calcarea and Porifera; this spicule type is not diagnostic of hexactinellids in the fossil record. (3) Reticulosans form the stem lineage of Silicea, and probably also Porifera. (4) At least some early-branching groups possessed biminerallic spicules of silica (with axial filament) combined with an outer layer of calcite secreted within an organic sheath.
    [Show full text]
  • Skeletonized Microfossils from the Lower–Middle Cambrian Transition of the Cantabrian Mountains, Northern Spain
    Skeletonized microfossils from the Lower–Middle Cambrian transition of the Cantabrian Mountains, northern Spain SÉBASTIEN CLAUSEN and J. JAVIER ÁLVARO Clausen, S. and Álvaro, J.J. 2006. Skeletonized microfossils from the Lower–Middle Cambrian transition of the Cantabrian Mountains, northern Spain. Acta Palaeontologica Polonica 51 (2): 223–238. Two different assemblages of skeletonized microfossils are recorded in bioclastic shoals that cross the Lower–Middle Cambrian boundary in the Esla nappe, Cantabrian Mountains. The uppermost Lower Cambrian sedimentary rocks repre− sent a ramp with ooid−bioclastic shoals that allowed development of protected archaeocyathan−microbial reefs. The shoals yield abundant debris of tube−shelled microfossils, such as hyoliths and hyolithelminths (Torellella), and trilobites. The overlying erosive unconformity marks the disappearance of archaeocyaths and the Iberian Lower–Middle Cambrian boundary. A different assemblage occurs in the overlying glauconitic limestone associated with development of widespread low−relief bioclastic shoals. Their lowermost part is rich in hyoliths, hexactinellid, and heteractinid sponge spicules (Eiffelia), chancelloriid sclerites (at least six form species of Allonnia, Archiasterella, and Chancelloria), cambroclaves (Parazhijinites), probable eoconchariids (Cantabria labyrinthica gen. et sp. nov.), sclerites of uncertain af− finity (Holoplicatella margarita gen. et sp. nov.), echinoderm ossicles and trilobites. Although both bioclastic shoal com− plexes represent similar high−energy conditions, the unconformity at the Lower–Middle Cambrian boundary marks a drastic replacement of microfossil assemblages. This change may represent a real community replacement from hyolithelminth−phosphatic tubular shells to CES (chancelloriid−echinoderm−sponge) meadows. This replacement coin− cides with the immigration event based on trilobites previously reported across the boundary, although the partial infor− mation available from originally carbonate skeletons is also affected by taphonomic bias.
    [Show full text]
  • Constraints on the Timescale of Animal Evolutionary History
    Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J.
    [Show full text]
  • Smithsonian Miscellaneous Collections
    SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 67, NUMBER 6 CAMBRIAN GEOLOGY AND PALEONTOLOGY IV No. 6.—MIDDLE CAMBRIAN SPONGIAE (With Plates 60 to 90) BY CHARLES D. WALCOTT (Publication 2580) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION 1920 Z$t Bovb Qgattimote (press BALTIMORE, MD., U. S. A. CAMBRIAN GEOLOGY AND PALEONTOLOGY IV No. 6.—MIDDLE CAMBRIAN SPONGIAE By CHARLES D. WALCOTT (With Plates 60 to 90) CONTENTS PAGE Introduction 263 Habitat = 265 Genera and species 265 Comparison with recent sponges 267 Comparison with Metis shale sponge fauna 267 Description of species 269 Sub-Class Silicispongiae 269 Order Monactinellida Zittel (Monaxonidae Sollas) 269 Sub-Order Halichondrina Vosmaer 269 Halichondrites Dawson 269 Halichondrites elissa, new species 270 Tuponia, new genus 271 Tuponia lineata, new species 272 Tuponia bellilineata, new species 274 Tuponia flexilis, new species 275 Tuponia flexilis var. intermedia, new variety 276 Takakkawia, new genus 277 Takakkawia lineata, new species 277 Wapkia, new genus 279 Wapkia grandis, new species 279 Hazelia, new genus 281 Hazelia palmata, new species 282 Hazelia conf erta, new species 283 Hazelia delicatula, new species 284 Hazelia ? grandis, new species 285. Hazelia mammillata, new species 286' Hazelia nodulifera, new species 287 Hazelia obscura, new species 287 Corralia, new genus 288 Corralia undulata, new species 288 Sentinelia, new genus 289 Sentinelia draco, new species 290 Smithsonian Miscellaneous Collections, Vol. 67, No. 6 261 262 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. 6j Family Suberitidae 291 Choia, new genus 291 Choia carteri, new species 292 Choia ridleyi, new species 294 Choia utahensis, new species 295 Choia hindei (Dawson) 295 Hamptonia, new genus 296 Hamptonia bowerbanki, new species 297 Pirania, new genus 298 Pirania muricata, new species 298 Order Hexactinellida O.
    [Show full text]
  • First Skeletal Microfauna from the Cambrian Series 3 of the Jordan Rift Valley (Middle East)
    First skeletal microfauna from the Cambrian Series 3 of the Jordan Rift Valley (Middle East) OLAF ELICKI ELICKI, O., 2011:12:23. First skeletal microfauna from the Cambrian Series 3 of the Jordan Rift Valley (Middle East). Memoirs of the Association of Australasian Palaeontologists 42, 153-173. ISSN 0810-8889. For the first time, a Cambrian microfauna is reported from the Jordan Rift Valley. The fauna comes from low-latitude carbonates of the Numayri Member (Burj Formation, Jordan) and to a lesser degree the equivalent Nimra Member (Timna Formation, Israel). Co-occuring with trilobite, brachiopod and hyolith macrofossils, the microfauna is represented mostly by disarticulated poriferid (mostly hexactinellids) and echinoderm remains (eocrinoids and edrioasteroids). Among the hexactinellids, Rigbyella sp., many isolated triactins and tetractins, as well as a few pentactins and rare hexactins occur. Additional poriferid spicules come from heteractinids (Eiffelia araniformis [Missarzhevsky, 1981]) and polyactinellids (?Praephobetractinia). Chancelloriids (Archiasterella cf. hirundo Bengtson, 1990, Allonnia sp., Chancelloria sp., ?Ginospina sp.) are a rather rare faunal element. Micromolluscs are represented mainly by an indeterminable helcionellid. The probable octocoral spicule Microcoryne cephalata (Bengtson, 1990), torellellid and hyolithellid hyolithelminths, and a bradoriid arthropod occur as very few or single specimens. The same is the case with a probable siphogonuchitid. The occurrence of a cornulitid related microfossil may extend the stratigraphic range of this fossil group significantly. The rather low-diversity microfauna is overwhelmingly dominated by sessile epibenthic biota. The preferred feeding habit seems to have been suspension feeding and minor deposit feeding. The microfauna from the Jordan Rift Valley is typical for low-latitude carbonate environments of Cambrian Series 3 age that corresponds to the traditional late early to middle Cambrian.
    [Show full text]
  • Sedimentology and Palaeontology of the Withycombe Farm Borehole, Oxfordshire, UK
    Sedimentology and Palaeontology of the Withycombe Farm Borehole, Oxfordshire, England By © Kendra Morgan Power, B.Sc. (Hons.) A thesis submitted to the School of Graduate Studies in partial fulfillment of the requirements for the degree of Master of Science Department of Earth Sciences Memorial University of Newfoundland May 2020 St. John’s Newfoundland Abstract The pre-trilobitic lower Cambrian of the Withycombe Formation is a 194 m thick siliciclastic succession dominated by interbedded offshore red to purple and green pyritic mudstone with minor sandstone. The mudstone contains a hyolith-dominated small shelly fauna including: orthothecid hyoliths, hyolithid hyoliths, the rostroconch Watsonella crosbyi, early brachiopods, the foraminiferan Platysolenites antiquissimus, the coiled gastropod-like Aldanella attleborensis, halkieriids, gastropods and a low diversity ichnofauna including evidence of predation by a vagile infaunal predator. The assemblage contains a number of important index fossils (Watsonella, Platysolenites, Aldanella and the trace fossil Teichichnus) that enable correlation of strata around the base of Cambrian Stage 2 from Avalonia to Baltica, as well as the assessment of the stratigraphy within the context of the lower Cambrian stratigraphic standards of southeastern Newfoundland. The pyritized nature of the assemblage has enabled the study of some of the biota using micro-CT, augmented with petrographic studies, revealing pyritized microbial filaments of probable giant sulfur bacteria. We aim to produce the first complete description of the core and the abundant small pyritized fossils preserved in it, and develop a taphonomic model for the pyritization of the “small” shelly fossils. i Acknowledgements It is important to acknowledge and thank the many people who supported me and contributed to the successful completion of this thesis.
    [Show full text]
  • The Early History of the Metazoa—A Paleontologist's Viewpoint
    ISSN 20790864, Biology Bulletin Reviews, 2015, Vol. 5, No. 5, pp. 415–461. © Pleiades Publishing, Ltd., 2015. Original Russian Text © A.Yu. Zhuravlev, 2014, published in Zhurnal Obshchei Biologii, 2014, Vol. 75, No. 6, pp. 411–465. The Early History of the Metazoa—a Paleontologist’s Viewpoint A. Yu. Zhuravlev Geological Institute, Russian Academy of Sciences, per. Pyzhevsky 7, Moscow, 7119017 Russia email: [email protected] Received January 21, 2014 Abstract—Successful molecular biology, which led to the revision of fundamental views on the relationships and evolutionary pathways of major groups (“phyla”) of multicellular animals, has been much more appre ciated by paleontologists than by zoologists. This is not surprising, because it is the fossil record that provides evidence for the hypotheses of molecular biology. The fossil record suggests that the different “phyla” now united in the Ecdysozoa, which comprises arthropods, onychophorans, tardigrades, priapulids, and nemato morphs, include a number of transitional forms that became extinct in the early Palaeozoic. The morphology of these organisms agrees entirely with that of the hypothetical ancestral forms reconstructed based on onto genetic studies. No intermediates, even tentative ones, between arthropods and annelids are found in the fos sil record. The study of the earliest Deuterostomia, the only branch of the Bilateria agreed on by all biological disciplines, gives insight into their early evolutionary history, suggesting the existence of motile bilaterally symmetrical forms at the dawn of chordates, hemichordates, and echinoderms. Interpretation of the early history of the Lophotrochozoa is even more difficult because, in contrast to other bilaterians, their oldest fos sils are preserved only as mineralized skeletons.
    [Show full text]
  • Systema Naturae. the Classification of Living Organisms
    Systema Naturae. The classification of living organisms. c Alexey B. Shipunov v. 5.601 (June 26, 2007) Preface Most of researches agree that kingdom-level classification of living things needs the special rules and principles. Two approaches are possible: (a) tree- based, Hennigian approach will look for main dichotomies inside so-called “Tree of Life”; and (b) space-based, Linnaean approach will look for the key differences inside “Natural System” multidimensional “cloud”. Despite of clear advantages of tree-like approach (easy to develop rules and algorithms; trees are self-explaining), in many cases the space-based approach is still prefer- able, because it let us to summarize any kinds of taxonomically related da- ta and to compare different classifications quite easily. This approach also lead us to four-kingdom classification, but with different groups: Monera, Protista, Vegetabilia and Animalia, which represent different steps of in- creased complexity of living things, from simple prokaryotic cell to compound Nature Precedings : doi:10.1038/npre.2007.241.2 Posted 16 Aug 2007 eukaryotic cell and further to tissue/organ cell systems. The classification Only recent taxa. Viruses are not included. Abbreviations: incertae sedis (i.s.); pro parte (p.p.); sensu lato (s.l.); sedis mutabilis (sed.m.); sedis possi- bilis (sed.poss.); sensu stricto (s.str.); status mutabilis (stat.m.); quotes for “environmental” groups; asterisk for paraphyletic* taxa. 1 Regnum Monera Superphylum Archebacteria Phylum 1. Archebacteria Classis 1(1). Euryarcheota 1 2(2). Nanoarchaeota 3(3). Crenarchaeota 2 Superphylum Bacteria 3 Phylum 2. Firmicutes 4 Classis 1(4). Thermotogae sed.m. 2(5).
    [Show full text]
  • Shell Microstructures in Early Mollusks
    Vol. XLII(4): 2010 THE FESTIVUS Page 43 SHELL MICROSTRUCTURES IN EARLY MOLLUSKS MICHAEL J. VENDRASCO1*, SUSANNAH M. PORTER1, ARTEM V. KOUCHINSKY2, GUOXIANG LI3, and CHRISTINE Z. FERNANDEZ4 1Institute for Crustal Studies, University of California, Santa Barbara, CA, 93106, USA 2Department of Palaeozoology, Swedish Museum of Natural History, Box 50007, SE-104 05 Stockholm, Sweden 3LPS, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, P.R. China, 414601 Madris Ave., Norwalk, CA 90650, USA Abstract: Shell microstructures in some of the oldest known mollusk fossils (from the early to middle Cambrian Period; 542 to 510 million years ago) are diverse, strong, and in some cases unusual. We herein review our recent work focused on different aspects of shell microstructures in Cambrian mollusks, briefly summarizing some of the major conclusions from a few of our recent publications and adding some new analysis. Overall, the data suggest that: (1) mollusks rapidly evolved disparate shell microstructures; (2) early mollusks had a complex shell with a different type of shell microstructure in the outer layer than in the inner one; (3) the modern molluscan biomineralization system, with precise control over crystal shapes and arrangements in a mantle cavity bounded by periostracum, was already in place during the Cambrian; (4) shell microstructure data provide a suite of characters useful in phylogenetic analyses of mollusks and mollusk-like Problematica, allowing better determination
    [Show full text]
  • Terreneuvian Stratigraphy and Faunas from the Anabar Uplift, Siberia
    Terreneuvian stratigraphy and faunas from the Anabar Uplift, Siberia ARTEM KOUCHINSKY, STEFAN BENGTSON, ED LANDING, MICHAEL STEINER, MICHAEL VENDRASCO, and KAREN ZIEGLER Kouchinsky, A., Bengtson, S., Landing, E., Steiner, M., Vendrasco, M., and Ziegler, K. 2017. Terreneuvian stratigraphy and faunas from the Anabar Uplift, Siberia. Acta Palaeontologica Polonica 62 (2): 311‒440. Assemblages of mineralized skeletal fossils are described from limestone rocks of the lower Cambrian Nemakit-Daldyn, Medvezhya, Kugda-Yuryakh, Manykay, and lower Emyaksin formations exposed on the western and eastern flanks of the Anabar Uplift of the northern Siberian Platform. The skeletal fossil assemblages consist mainly of anabaritids, molluscs, and hyoliths, and also contain other taxa such as Blastulospongia, Chancelloria, Fomitchella, Hyolithellus, Platysolenites, Protohertzina, and Tianzhushanella. The first tianzhushanellids from Siberia, including Tianzhushanella tolli sp. nov., are described. The morphological variation of Protohertzina anabarica and Anabarites trisulcatus from their type locality is documented. Prominent longitudinal keels in the anabaritid Selindeochrea tripartita are demon- strated. Among the earliest molluscs from the Nemakit-Daldyn Formation, Purella and Yunnanopleura are interpreted as shelly parts of the same species. Fibrous microstructure of the outer layer and a wrinkled inner layer of mineralised cuticle in the organophosphatic sclerites of Fomitchella are reported. A siliceous composition of the globular fossil Blastulospongia
    [Show full text]
  • 325015 1 En Bookbackmatter 357..405
    Appendix © Springer India 2017 357 S. Jain, Fundamentals of Invertebrate Palaeontology, Springer Geology, DOI 10.1007/978-81-322-3658-0 358 Ch. no. Species name Age Locality Chapter Fig. no. Fig. no. 2 Otavia antiqua Brian et al. Cryogenian-Ediacaran Namibia, South Africa Sponges 1 1 2 Sycetta sagittifera Haeckel Recent South India Sponges 3 6 2 Archaeocyaths atlanticus Billings Early Cambrian West coast, USA Sponges 7 3–4 2 Ajacicyathus nevadensis Oklulitch Early Cambrian West coast, USA Sponges 7 5 2 Ethmophyllum whitneyi Meek Cambrian British Columbia, Canada Sponges 7 6–7 2 Pycnoidocyathus occidentalis (Raymond) Early Cambrian British Columbia, Canada Sponges 7 8 2 Protospongia fenestrate Salter Middle Cambrian (Burgess) British Columbia, Canada Sponges 8 1 2 Chancelloria eros Walcott Middle Cambrian (Burgess) British Columbia, Canada Sponges 8 2 2 Eiffelia globosa Walcott Middle Cambrian (Burgess) British Columbia, Canada Sponges 8 3 2 Choia carteri Walcott Middle Cambrian (Burgess) British Columbia, Canada Sponges 8 4 2 Brachiospongia digitata (Owen) Middle Ordovician Kentucky, USA Sponges 9 1 2 Hindia parva Ulrich Middle Ordovician Minnesota, USA Sponges 9 2–3 2 Ischadites iowensis (Owen) Middle Ordovician Kentucky, USA Sponges 9 4 2 Receptaculites oweni Hall Middle Ordovician Kentucky, USA Sponges 9 5 2 Astaeospongia meniscus (Roemer) Middle Silurian (Niagaran) Tennessee, USA Sponges 10 1–2 2 Prismodictya prismatica (Hall) Late Devonian New York, USA Sponges 10 3 2 Prismodictya telum (Hall) Late Devonian New York, USA Sponges 10
    [Show full text]
  • Anomalocaris
    Life of the Paleozoic Tuesday, November 22, 11 Life of the Paleozoic • Overview: • Cambrian, Vast expansion of shelly marine life forms and jawless fish • Ordovician - most modern phyla established • Late Paleozoic- land plants and vertebrates (tetrapods and amniotes) Tuesday, November 22, 11 Invertebrates • Marine environments • Nektic, planktic, benthic • Adaptions: • Epifaunal- animals living on the sea floor • Infaunal – animals that burrow into the sea floor Tuesday, November 22, 11 Early cambrian • Small Shelly fossils • Rarely more than a few millimeters long • A- Anabarella • B- Camanella • C- Aldanella • D- Sponge Spicule • E- Formitchella • F- Lapworthella Tuesday, November 22, 11 Early Soft-body fossils • The Burgess shale: • Most fossils reduced to shiny black impressions What type of fossilization is this? • Viewed as one of the most important finds of the fossil record • Altogether, over 60,000 species have been collected Tuesday, November 22, 11 The Burgess shale • Four Groups of Arthropods • Trilobites • Crustaceans • Scorpions • Insects • Sponges • Onycophorans • Crinoids • Sea Cucumbers • Chordates Tuesday, November 22, 11 Chordates • Shows evolution of early notochord • Notochord- dorsally situated nerve cord Why is this important? • Pikaia- small animal that has notochord and also shows evidence of v-shaped muscle bands (this indicated sinosoidal swimming motion THESE ANIMALS ARE ANCESTORS TO ALL MODERN VERTEBRATES Tuesday, November 22, 11 Other Notable Fossils • Anomalocaris- fierce predator over 50cm long (~2ft) • Opabinia-
    [Show full text]