Paleontological Resources Assessment Technical Report
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Notes on the Mountain Limestone and Lower Carboniferous Rocks of the Fifeshire Coast from Burntisland to St Andrews
( 385 ) XVI.—Notes on the Mountain Limestone and Lower Carboniferous Rocks of the Fifeshire Coast from Burntisland to St Andrews. By the Rev. THOMAS BROWN, Edinburgh. (Read 17th April 1860.) Introduction. Mountain Limestone—continued. I. General Course of Strata. 2. Estuarine Strata, F to L. II. Trap Rocks. 3. Limestone L. III. Mountain Limestone. IV. Lower Carboniferous. 1. Six Upper Limestones, A to F. Myalina Beds. Corals. Petrified Trees. Shells. Marine Beds. Crustacea. Fossils. Fish. V. Results—The Two Groups defined. Tuberculated Fish. Introduction. In this paper I shall first refer to the circumstances under which the follow- ing observations were made. I had gone in the autumn of 1856 for a few weeks to Elie on the Fife coast, and was induced, as a means of relaxation and exercise in the open air, to pay some attention to the geology of the neighbourhood, resuming for a brief interval what was once a favourite pursuit. About a mile to the east of the village, I found a stratum well deserving attention—a thin bed of limestone—dipping in- land a little beyond the cliff on which stands the ruined Castle of Ardross. The fossil shells which it contained were of unusual form, and beautifully preserved ; there were fish remains of two or three species, and a small group of crustaceans still more remarkable. Among the fish I thought I could detect the large scales of an Irish species—the Holoirtijchius Fortlockii—and among the crustaceans there were the valves of Dithyrocaris, a genus particularly characteristic of the Irish beds. At once the question arose whether these fossils might not serve as links connecting this Ardross bed with the Irish series. -
Discussion. Brachiopod Zonation and Age of the Permian Kapp Starostin Formation (Central Spitsbergen)
Discussion. Brachiopod zonation and age of the Permian Kapp Starostin Formation (Central Spitsbergen) LARS STEMMERIK Stemmerik, L. 1988: Discussion. Brachiopod zonation and age of the Permian Kapp Starostin Formation (Central Spitsbergen). Polar Research 6, 179-180. Lars Stemmerik, Grgnlands Geologiske Unders~geke,0ster Voldgade 10, 0-1350KQbenhaun K, Denmark; May 1988. The following discussion will concentrate on the rhynchus kempei, and Muirwoodia greenlandica stratigraphical implications of the brachiopod for the Megousia weyprechti Zone and Ptero- zonation proposed by Nakamura et al. (1987). No spirifer alatus, Pleurohorridonia scoresbyensis, such brachiopod zonation can be recognised in Choristites s#derberghi, and Odontospirifer mir- Greenland where in contrast diagnostic species abilis for the Pterospirifer alatus Zone (Nakamura of the upper zones in the Kapp Starostin For- et al. 1987, p. 213). Furthermore, Liosotella spitz- mation co-occur throughout the entire section. bergiana, Paeckelmannia toulai and Kochi- It is therefore concluded that the correlations productus plexicostatus confined to the uppermost proposed by Nakamura et al. (1987) are not valid. zones in the Kapp Starostin Formation are found At best the overall similarities of the East Green- in East Greenland. land and Svalbard faunas may indicate a Kaz- The work of Dunbar (1955) does not imply a anian-early Tatarian age for the upper part of the two-fold zonation of the brachiopods in the Fold- Kapp Starostin Formation. vik Creek Group in East Greenland. As discussed The paper of Nakamura et al. (1987) has wide below the different collections described by Dun- stratigraphic implications both for local cor- bar (1955) include a mixture of species diagnostic relation of the Foldvik Creek Group (sensu for the Megousia weyprechti Zone, Pterospirifer Surlyk et al. -
Meg-Bitten Bone
The ECPHORA The Newsletter of the Calvert Marine Museum Fossil Club Volume 32 Number 2 June 2017 Meg-Bitten Bone Features Meg-Bitten Whale Bone The Bruce Museum The State Museum of New Jersey Inside Micro-Teeth Donated Fecal Pellets in Ironstone Starfish Eocene Bird Tracks Bear and Shark Tooth Over-Achieving Shark Turtle Myth Horse Foot Bones Meg 7 Months Apart Capacious Coprolite Small Dolphin Radius Otter Cam Pen Shell Miocene Volute Peccary Scapula Found Club Events Pegmatite from C. Cliffs This small piece of fossil whale bone was found along the Potomac Crayfish on the Potomac River by Paul Murdoch. It is noteworthy because two of its sides are Hadrodelphis Caudals strongly marked by parallel grooves cut into the bone, prior to it Fractured Caudal becoming fossilized, by the serrations on the cutting edge of the teeth What is nice about large bite of Carcharocles megalodon. The thickness of the bone suggests baleen marks on whale bone from this whale in origin, but which bone remains unknown. Below, serrated locality is that there is no other edge of C. megalodon tooth. Photos by S. Godfrey. ☼ shark with serrated teeth large enough (right) to mark fossil bone thusly; confirming a meg/cetacean encounter. It is not known from this piece of bone if this was a predatory or scavenging event. Metric scale. CALVERT MARINE MUSEUM www.calvertmarinemuseum.com 2 The Ecphora June 2017 Micros Donated to CMM Adrien Malick found and donated this piece of limonite that preserves impressions of fecal? pellets (upper left of image; enlarged below). (Limonite is a sedimentary rock made of iron oxyhydroxides.) Enlarged view of what appear to be impressions of millimeter-scale fecal pellets in limonite. -
A New Insight on the Symbiotic Association Between the Fan Mussel Pinna Rudis and the Shrimp Pontonia Pinnophylax in the Azores (NE Atlantic)
Global Journal of Zoology Joao P Barreiros1, Ricardo JS Pacheco2 Short Communication and Sílvia C Gonçalves2,3 1CE3C /ABG, Centre for Ecology, Evolution and Environmental Changes, Azorean Biodiversity A New Insight on the Symbiotic Group. University of the Azores, 9700-042 Angra do Heroísmo, Portugal Association between the Fan 2MARE, Marine and Environmental Sciences Centre, ESTM, Polytechnic Institute of Leiria, 2520-641 Peniche, Portugal Mussel Pinna Rudis and the Shrimp 3MARE, Marine and Environmental Sciences Centre, Department of Life Sciences, Faculty of Sciences Pontonia Pinnophylax in the Azores and Technology, University of Coimbra, 3004-517 Coimbra, Portugal (NE Atlantic) Dates: Received: 05 July, 2016; Accepted: 13 July, 2016; Published: 14 July, 2016 collect fan mussels which implied that the presence of the shrimps was *Corresponding author: João P. Barreiros, evaluated through underwater observation of the shell (when slightly CE3C /ABG, Centre for Ecology, Evolution and Environmental Changes, Azorean Biodiversity opened) or through counter light (by means of pointing a lamp). A Group. University of the Azores, 9700-042 Angra do previous note on this work was reported by the authors [4]. Presently, Heroísmo, Portugal, E-mail; [email protected] the authors are indeed collecting specimens of P. rudis in the same www.peertechz.com areas referred here for a more comprehensive project on symbiotic mutualistic/ relationships in several subtidal Azorean animals (work Communication in progress). Bivalves Pinnidae are typical hosts of Pontoniinae shrimps. Pinna rudis is widely distributed along Atlantic and Several species of this family were documented to harbor these Mediterranean waters but previous records of the association decapods inside their shells, especially shrimps from the genus between this bivalve and P. -
A New Insight on the Symbiotic Association Between the Fan Mussel Pinna Rudis and the Shrimp Pontonia Pinnophylax in the Azores (NE Atlantic)
Global Journal of Zoology Joao P Barreiros1, Ricardo JS Pacheco2 Short Communication and Sílvia C Gonçalves2,3 1CE3C /ABG, Centre for Ecology, Evolution and Environmental Changes, Azorean Biodiversity A New Insight on the Symbiotic Group. University of the Azores, 9700-042 Angra do Heroísmo, Portugal Association between the Fan 2MARE, Marine and Environmental Sciences Centre, ESTM, Polytechnic Institute of Leiria, 2520-641 Peniche, Portugal Mussel Pinna Rudis and the Shrimp 3MARE, Marine and Environmental Sciences Centre, Department of Life Sciences, Faculty of Sciences Pontonia Pinnophylax in the Azores and Technology, University of Coimbra, 3004-517 Coimbra, Portugal (NE Atlantic) Dates: Received: 05 July, 2016; Accepted: 13 July, 2016; Published: 14 July, 2016 collect fan mussels which implied that the presence of the shrimps was *Corresponding author: João P. Barreiros, evaluated through underwater observation of the shell (when slightly CE3C /ABG, Centre for Ecology, Evolution and Environmental Changes, Azorean Biodiversity opened) or through counter light (by means of pointing a lamp). A Group. University of the Azores, 9700-042 Angra do previous note on this work was reported by the authors [4]. Presently, Heroísmo, Portugal, E-mail; [email protected] the authors are indeed collecting specimens of P. rudis in the same ISSN: 2640-7930 areas referred here for a more comprehensive project on symbiotic www.peertechz.com mutualistic/ relationships in several subtidal Azorean animals (work in progress). Communication Pinna rudis is widely distributed along Atlantic and Mediterranean waters but previous records of the association Bivalves Pinnidae are typical hosts of Pontoniinae shrimps. between this bivalve and P. pinnophylax were unknown, despite the Several species of this family were documented to harbor these existence of association records with Pinna nobilis [1,3,5]. -
The Carboniferous Evolution of Nova Scotia
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The Carboniferous evolution of Nova Scotia J. H. CALDER Nova Scotia Department of Natural Resources, PO Box 698, Halifax, Nova Scotia, Canada B3J 2T9 Abstract: Nova Scotia during the Carboniferous lay at the heart of palaeoequatorial Euramerica in a broadly intermontane palaeoequatorial setting, the Maritimes-West-European province; to the west rose the orographic barrier imposed by the Appalachian Mountains, and to the south and east the Mauritanide-Hercynide belt. The geological affinity of Nova Scotia to Europe, reflected in elements of the Carboniferous flora and fauna, was mirrored in the evolution of geological thought even before the epochal visits of Sir Charles Lyell. The Maritimes Basin of eastern Canada, born of the Acadian-Caledonian orogeny that witnessed the suture of Iapetus in the Devonian, and shaped thereafter by the inexorable closing of Gondwana and Laurasia, comprises a near complete stratal sequence as great as 12 km thick which spans the Middle Devonian to the Lower Permian. Across the southern Maritimes Basin, in northern Nova Scotia, deep depocentres developed en echelon adjacent to a transform platelet boundary between terranes of Avalon and Gondwanan affinity. The subsequent history of the basins can be summarized as distension and rifting attended by bimodal volcanism waning through the Dinantian, with marked transpression in the Namurian and subsequent persistence of transcurrent movement linking Variscan deformation with Mauritainide-Appalachian convergence and Alleghenian thrusting. This Mid- Carboniferous event is pivotal in the Carboniferous evolution of Nova Scotia. Rapid subsidence adjacent to transcurrent faults in the early Westphalian was succeeded by thermal sag in the later Westphalian and ultimately by basin inversion and unroofing after the early Permian as equatorial Pangaea finally assembled and subsequently rifted again in the Triassic. -
TREATISE ONLINE Number 48
TREATISE ONLINE Number 48 Part N, Revised, Volume 1, Chapter 31: Illustrated Glossary of the Bivalvia Joseph G. Carter, Peter J. Harries, Nikolaus Malchus, André F. Sartori, Laurie C. Anderson, Rüdiger Bieler, Arthur E. Bogan, Eugene V. Coan, John C. W. Cope, Simon M. Cragg, José R. García-March, Jørgen Hylleberg, Patricia Kelley, Karl Kleemann, Jiří Kříž, Christopher McRoberts, Paula M. Mikkelsen, John Pojeta, Jr., Peter W. Skelton, Ilya Tëmkin, Thomas Yancey, and Alexandra Zieritz 2012 Lawrence, Kansas, USA ISSN 2153-4012 (online) paleo.ku.edu/treatiseonline PART N, REVISED, VOLUME 1, CHAPTER 31: ILLUSTRATED GLOSSARY OF THE BIVALVIA JOSEPH G. CARTER,1 PETER J. HARRIES,2 NIKOLAUS MALCHUS,3 ANDRÉ F. SARTORI,4 LAURIE C. ANDERSON,5 RÜDIGER BIELER,6 ARTHUR E. BOGAN,7 EUGENE V. COAN,8 JOHN C. W. COPE,9 SIMON M. CRAgg,10 JOSÉ R. GARCÍA-MARCH,11 JØRGEN HYLLEBERG,12 PATRICIA KELLEY,13 KARL KLEEMAnn,14 JIřÍ KřÍž,15 CHRISTOPHER MCROBERTS,16 PAULA M. MIKKELSEN,17 JOHN POJETA, JR.,18 PETER W. SKELTON,19 ILYA TËMKIN,20 THOMAS YAncEY,21 and ALEXANDRA ZIERITZ22 [1University of North Carolina, Chapel Hill, USA, [email protected]; 2University of South Florida, Tampa, USA, [email protected], [email protected]; 3Institut Català de Paleontologia (ICP), Catalunya, Spain, [email protected], [email protected]; 4Field Museum of Natural History, Chicago, USA, [email protected]; 5South Dakota School of Mines and Technology, Rapid City, [email protected]; 6Field Museum of Natural History, Chicago, USA, [email protected]; 7North -
University of Texas Bulletin No
; univ. OF ECON. >GY CATION ?) 2433 . University of Texas Bulletin No. 2433: September 1, 1924. Species of the Genus Schwagerina and Their Stratigraphic Significance By J. W. Beede AND Hedwig T. Kniker PUBLISHED BY THE UNIVERSITY OF TEXAS AUSTIN Publications of the University of Texas Publications Committee : Frederic Duncalf J. L. Henderson Killis Campbell E. J. Mathews F. W. Graff H. J. Muller C. G. Haines Hal C. Weaver The University publishes bulletins four times a month, so numbered, that the first two digits of the number show the year of issue, the last two the position in the;yearly series. (Fcb example, No. 2201 is the first bulletin of the year 1922.) These comprise the official publications of the University, publications on humanistic and scientific sub- jects, bulletins prepared by the Division of Extension, by the Bureau of Economic Geology, and other bulletins of general educational interest. With the exception offspecial num- bers, any bulletin willbe sent to a citizen of 'pTexas free on request. Allcommunications about University publications should be addressed to University Publications, University of Texas, Austin. University of Texas Bulletin No. 24331,1924 Species of the Genus Schwagerina and Their Stratigraphic Significance By J. W. Beede AND Hedwig T. Kniker PUBLISHED BY THE UNIVERSITYFOUR TIMESA MONTH. ANDENTERED AS SECOND-CLASS MATTER AT THE POSTOFFICE AT AUSTIN. TEXAS, UNDER THE ACT OF AUGUST 24. 1912 1 ¦ill00025560 The benefits of education and of useful knowledge, generally diffused through a community, are essential to the preservation of a free govern- ment. Sam Houston Cultivated mind is the guardian genius of democracy. -
Silver Creek Hydraulic Limestone Southeastern Indiana
, \ " THE Silver Creek Hydraulic Limestone OF Southeastern Indiana. By C. E. SIEBENTHAL. 1900. / ! LETTER OF TRANSMITTAL. Bloomington, Ind., January 10, 1901. Dear Sir-I have the honor to transmit herewith my report upon the "Silver Creek Hydraulic Limestone," written in 1899 and em bodying the results of field work done in that year, but recently gone over and brought down to date. I take pleasure in acknowledging the services of Messrs. H. M. Adkinson and F. H. H.Calhoun, gradu ate students at the University of Chicago, who generously gave their assistance in the gathering of the data for the paper. The thanks of the Survey are also due to Prof. Stuart Weller, of the University of Chicago, for valuable assistance in the paleontological part of this report. Respectfully submitted, C. E. SIEBENTHAL. Prof. W. S. Blatchley, State Geologist. (332) ,\ THE SILVER CREEK. HYDRAULIC LIMESTONE OF SOUTHEASTERN INDIANA. By U. E. SIEBENTHAL. OUTLINK 1. STRATIGRAPHY. Historical Resume. 1827. 1. A. Lapham. 1841. Jas.Hall. 1843. Dr. A. Clapp. 1843. D. D. Owen. 1843. H. D. Rogers. 1847. Yandell & Bhumal'lI. 1857. Maj. S. S. Lyon. 1859. Lyon and CassedllY· 1860. Maj. S. S. Lyon, 1874. W. W. Borden. 1875. W. W. Borden. 1879. Jas. Hall. 1897. Aug. F. Foerste. 1899. E. M. Kindle. Stratigraphy and Paleontology. Knobstone. Rockford limestone. New Albany black shale. Sellersburg limestone. Silver Creek hydraulic IimestOlIP. Jefl'ersonville limestone. Pendleton sandstone. Upper Silurian. Lower Silurian. Local Details of Distribution and Structure. Clark County. River region. Silver Creek region. Charlestown region. Scott County. Lexington region. Woods Fork region. -
Appendices (3.601Mb)
University of Plymouth PEARL https://pearl.plymouth.ac.uk 04 University of Plymouth Research Theses 01 Research Theses Main Collection 2015 Palaeoecology of the late Permian mass extinction and subsequent recovery Foster, William J. http://hdl.handle.net/10026.1/5467 Plymouth University 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. Appendix 2.1: Balaton Highlands and Bükk Mountains Investigated sites. The Permian-Triassic succession of Balaton Highlands comprises part of the ALCAPA megaunit (Kóvacs and Haas, 2010) and is represented by Permian fluvial red sandstones and Triassic shallow marine rocks. The Lower Triassic succession in the Balaton Highlands is divided into four formations: the Kóveskál Dolomite Formation, Arács Marl Formation, Hidegkút Formation and Csopak Marl Formation (Figure A2.1). These formations paraconformably overlay the Permian Baltonfelvidék Formation and are capped by the Middle Triassic Aszòfo Dolomite Formation (Haas et al., 2012). Field visits (June 2012) to the Balaton Highlands (Figure A2.2) recorded 5m of the Kóveskál Formation at Balatonfüred; 15m at Balataonálmadi; and 1m of the Csopak Marl Formation at the Sóly section. Broglio Loriga et al. (1990) studied the biostratigraphy of the entire succession, but their data, were acquired from a trench that is no longer exposed (János Haas, pers. comm.) and their collections were not available for study (Renato Posenato, pers. -
Smithsonian Miscellaneous Collections
VOL. 52, PL. IX SMITHSONIAN MISCELLANEOUS COLLECTIONS HENRY NETTELROTH Vol. 52 1908 Smithsonian Miscellaneous Collections Vol. V Quarterly issue Part 2 THE XETTELROTH COLLECTION OF INVERTEBRATE FOSSILS By R. S. BASSLER (With 3 Plates) One of the most important accessions in the division of strati- graphic paleontology during the year 1907 was the collection of the late Henry Nettelroth, acquired jointly by the Smithsonian Institu- tion and the U. S. National Museum from his sons, H. H. Nettel- roth and Dr. Alexander Nettelroth, of Louisville, Kentucky. The registration and installation of these specimens was recently com- pleted, and it seemed in order, as well as very desirable on account of Mr. Nettelroth's work in science and of the valuable nature of his collection, to publish an article upon the subject. The collection is composed entirely of invertebrate fossils, mainly from the Silurian and Devonian strata of Indiana and Kentucky, although many other American as well as foreign localities are represented. The total number of specimens is rather small compared with the number of species represented, the collection comprising about 8,000 specimens, registered under nearly 1,000 entries; but all of the material is the best that could be had. Mr. Nettelroth prided himself upon the fact that his cabinet contained only choice specimens, representing years of careful selection. Imperfect material was retained only when it showed something of scientific interest. In exchanging. Air. Nettelroth also insisted upon a few good specimens rather than numerous poor representatives of a species. Likewise he paid par- ticular attention to a class of fossils, the mollusca, which is seldom well represented in the cabinets of even the best collectors. -
Early Triassic (Late Griesbachian) Gastropods from South China (Shanggan, Guangxi)
Swiss J Geosci (2010) 103:121–128 DOI 10.1007/s00015-010-0005-5 Early Triassic (Late Griesbachian) gastropods from South China (Shanggan, Guangxi) Andrzej Kaim • Alexander Nu¨tzel • Hugo Bucher • Thomas Bru¨hwiler • Nicolas Goudemand Received: 17 December 2009 / Accepted: 2 February 2010 / Published online: 9 June 2010 Ó Swiss Geological Society 2010 Abstract An Early Triassic (Griesbachian) gastropod about gastropods from the aftermath of the end-Permian fauna is reported from South China (Shanggan, Guangxi) mass extinction event. The gastropod association from and consists of four species: Bellerophon abrekensis, Shanggan shares one species with Primorye, Far East Wannerispira shangganensis Kaim & Nu¨tzel sp. nov., Russia (B. abrekensis). Two species, W. shangganensis and Naticopsis sp., and Palaeonarica guangxinensis Kaim & P. guangxinensis, closely resemble specimens reported Nu¨tzel sp. nov. The taxon Wannerispira Kaim & Nu¨tzel from the Griesbachian of Oman. This could suggest that nom. nov. replaces Pagodina Wanner non Van Beneden. Griesbachian gastropod faunas of the Tethys were rather This is the first report of Bellerophon abrekensis from homogenous although the data are still scarce. China. Previously, it was only known from its type locality in Far East Russia. Wannerispira shangganensis sp. is the Keywords Gastropoda Á China Á Early Triassic Á first certain Triassic report of the Permian subfamily Extinction Á Recovery Á Taxonomy Neilsoniinae and represents a holdover taxon. The neritimorph Palaeonarica is reported for the first time from the Early Triassic and this is the oldest occurrence of this genus. Introduction Compared with other Griesbachian gastropods, the present material is relatively well preserved so that the taxonomy The fauna in the immediate aftermath of the end-Permian rests on rather firm ground.