The North Pacific Miocene Record of Mytilus (Plicatomytilus), a New Subgenus of Bivalvia

Total Page:16

File Type:pdf, Size:1020Kb

The North Pacific Miocene Record of Mytilus (Plicatomytilus), a New Subgenus of Bivalvia The North Pacific Miocene Record of Mytilus (Plicatomytilus), a New Subgenus of Bivalvia By RICHARD C. ALLISON and WARREN 0. ADDICOTT GEOLOGICAL SURVEY PROFESSIONAL PAPER 962 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Allison, Richard C 1935- The North Pacific Miocene record of Mytilus (Plicatomytilus), a new subgenus of Bivalvia. (Geological Survey professional paper; 962) Bibliography: p. Includes index. Supt. of Doc. no.: 119.16:962 1. Mytilus, Fossil. 2. Paleontology--Miocene. 3. Paleontology--North Pacific region. I. Addicott, Warren O., joint author. 11. Title. 111. Series: United States. Geological Survey. Professional paper; 962. QE812.M94A38 564.11 76-608013 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02764-0 CONTENTS Page Abstract __--________--------------------------------1 Introduction -_________--______----~------------------1 . Family Mytll~dae 2 Subfamily Mytilinae ______--________----_--------___----__2 GenusMytilus Linne', 1758 ____-___________----------------_---- 2 Subgenus Plicatomytilus Allison and Addicott, n. subgen. ____-____-----------2 Mytilus (Plicatomytilus middendorffi Grewingk, 1850 _________----_------ 3 Mytilus (Plicatomytilus) gratacapi n. sp. __~_________~________----------- 9 Mytilus (Plicatomytilus)n. sp. _-_________________---------------------- 13 Locality register _-__-_-----___------____--_-------_-15 References cited ______----____-------_------------19 Index ___-_______~__~____----------------~------_21 ILLUSTRATIONS [Plates follow index] PLATE 1. Mytilus (Plicatomytilus) middendorffi. 2. Mytilus (Plicatomytilus)gratacapi and Mytilus (Plicatomytilus) n. sp. 3. Mytilus (Plicatomytilus) gmtacapi, Mytilus (Plicatomytilus) middendorffi, Mytilus (subgenus?)n. sp., and Mytilus (Mytilus) condoni. Page FIGURE1. Sketch showing comparison of muscle scars of Mytilus (Plicatomytilus) n. subgen. and Mytilus (Mytilusl-_---------------- 3 2. Map showing middle Miocene distribution ofMytilus middendorffi Grewingk _______-_____------------------------6 3. Map showing geographic distribution of Mytilus gratacapi n. sp _--________-________-_---_---------- ------------------ 11 THE NORTH PACIFIC MIOCENE RECORD OF MYTZLUS (PLICATOMYTZL US), A NEW SUBGENUS OF BIVALVIA By RICHARDC. ALLISOS~and ~Z'ARKEN0. ADI)ICOTT' ABSTRACT I Washington,- and the early middle Miocene Kuluven suite of western Kamchatka, U.S.S.R. This previously unrecognized taxon is not, A new subgenus of large plicate fossil mussels of the North however, referable to Plic~tomytilus. Pacific, Mytilus (Plicatomytilus) n. subgen., includes three distinct species, Mytilus (P.) middendorffi Grewingk, 1850, Mytilus (P.) gratacapi n. sp., and Mytilus (P.) n. sp. This extinct subgenus ranged INTRODUCTION from central California to western Kamchatka during the Miocene. The existence of moderately large, heavy-shelled Plicatomytilus is distinguished by strong plications of the shell which deflect the plane of commissure and by the foot retractor muscle plicate mussels in the Tertiary beds of Kodiak and Unga scar which is separated from the posterior byssal retractor and Islands, Alaska, has been recognized since 1850 when posterior adductor muscle scar. I Grewingk described Mytilus middendorffi. Following Mytilus middendorffi occurs in provincial middle Miocene deposits ~rewingk(1850), many authors (Dall and Harris, 1892; of (1) the Narrow Cape Formation, Kodiak Island, Alaska, (2) the Dall, 1896,1904; Gratacap, 1912; Grant and Gale, 1931; upper part of the Astoria Formation, Tillamook County, Oreg., (3) an unnamed formation at Coos Bay, Oreg., (4) the lower (Miocene) part of Slodkevich [=Slodkewitsch], 1938; Hall, 1958; Burk, Diller's (1903) Empire Formation near Cape Blanco, Oreg., (5) the 1965; Addicott, 1967; and MacNeil, 1967) have repeated Sobrante Sandstone near Castro Valley, Calif., (6) the Oursan Grewingk's original records, or they themselves have Sandstone, Alameda County, Calif., (7) the Temblor Formation of assigned these plicate mytilids from Kodiak and many Crittenden (1951), Santa Clara County, Calif., (8) the Sobrante localities on the Alaska Peninsula and Unga to a single Sandstone, Santa Clara County, Calif., (9) the Temblor Formation of Griswold Hills and the Vallecitos, San Benito County, Calif., and (10) species, M. middendorffi. MacNeil, Wolfe, Miller, and the lower Temblor Formation, Patinopecten zone, Kings County, Hopkins (1961) have indicated the correlation of Calif. Mytilus gratacapi occurs on the Alaska Peninsula and at Unga Miocene strata on Kodiak Island, Unga Island, and the Island, Alaska, in provincial middle(?) arid late Miocene deposits of Alaska Peninsula that they assign to their "Mytilus the upper part of the Unga Conglomerate Member of the Bear Lake middendoffi zone." Formation and upward into the overlying middle part of the Bear Lake Formation. Recently, both of us have realized independently that These two species have been lumped under Mytilus middendorffi the plicate mytilids that occur on the Alaska Peninsula Grewingk, but they do not co-occur. Mytilus middendorffi ranges and Unga Island in the Bear Lake Formation are in fact throughout the "Temblor" Stage and from the upper part of the a distinctly different new species, and that this new Saucesian Stage to the Luisian Stage of the microfaunal sequence. species and Mytilus middendoffi belong to a new Much, if not all, of the range zone of Mytilus gratacapi seems to be of late Miocene age. The standard correlation of the Narrow Cape subgenus of Mytilus Linne. This paper therefore: Formation with the Unga Conglomerate Member ("Mytilus midden- (1) describes the new subgenus Plicatomytilus, (2) de- do@ zone" of MacNeil and others) therefore is probably incorrect. scribes the new species Mytilus (Plicatomytilus) Mytilus (Plicatomytilus) n. sp. occurs in the middle and late Miocene gratacapi from the Bear Lake Formation, (3) reviews Kakert and Etolon suites of the "Kavran Series" in western the stratigraphic and paleozoogeographic distributions Kamchatka, U.S.S.R. Both Mytilus (P.) gratacapi and Mytilus (P.) n. sp. appear to have evolved from Mytilus middendorffi Grewingk. of M. (P.1 middendorffi Grewingk and M. (P.)grataca- The heavy plicate shell of Plicatomytilus was probably well adapted pi n. sp., and (4) reviews the reported occurrences of M. to life in high-energy environments in the shallow part of the inner cf. middendorffi [=Mytilus (Plicatomytilus) n. sp. of this sublittoral zone. Mytilus gratacapi may have been especially well paper] in Kamchatka. adapted to heavy wave surge and surf conditions. Addicott is primarily responsible for the sections on Another distinctive mytilid, Mytilus (subgenus?) n. sp., bearing two folds of the shell along the posterodorsal margin, occurs in the early chronologic and zoogeographic significance, and Allison Miocene Pyramid Hill Sand Member of the Jewett Sand, Kern River is primarily responsible for the systematic sections of area, Calif., as well as in the early Miocene Clallam Formation of the paper. All the fossils, those illustrated and the type -------- specimens, have been placed on deposit in the U.S. ' Department of Geology and Geophysical Institute, University of Alaska, Fairbanks, Alaska 99701. National Museum. The fossils were photographed by U.S. Geological Survey, Menlo Park, Calf 94025. Kenji Sakamoto. We wish to thank Ellen J. Moore and 2 NORTH PACIFIC MIOCENE RECORD OF MYTZLUS (PLZCATOMYTILUS),A NEW SUBGENUS J. Wyatt Durham for their critical reviews of the Grant agd Gale (1931, p. 246) applied the subgeneric manuscript. name Mytiloconcha Conrad, 1862, to several west coast species including Mytilus middendorffi because of their Phylum Mollusca "peculiar heavy terminal hinge." Soot-Ryen (1955, p. Class Bivalvia 29) showed, however, that Mytiloconcha Conrad, 1862, Subclass Pteriomorpha is a junior subjective synonym ofPerna Retzius, 1788. Order Mytiloida Perna Retzius differs from Plicatomytilus in possessing Super f amily Mytilacea a pitted resilial ridge, in lacking an anterior adductor Family Mytilidae muscle, and in having a single elongate anterior byssal Subfamily Mytilinae retractor scar. Perna does, however, have the foot Genus Mytilus Linne, 1758 retractor muscle placed anteriorly, separate from the posterior byssal retractor as in Plicatomytilus. Mytilus Linne, 1758, Systema Naturae, ed. 10, p. 704. Mytilus s.s. (fig. 1B) differs from Plicatomytilus in Type.-By subsequent designation (Gray, 18471, Mytilus edulis Linne, 1758. possessing a pitted resilial ridge, in having an elongate Subgenus Plicatomytilus n. subgen. anterior byssal retractor muscle scar or scars, and in Type.-Mytilus middendorffi Grewingk, 1850. having the posterior retractor muscles coalescent. The Description.-Shell moderate to large, heavy, anterior adductor ofPlicatomytilus is generally similar mytiliform; beaks terminal; lunule grooved and some- to that of the type species of Mytilus, M. edulis LinnB, times incurved, forms two large teeth and several 1758, but may be longer and narrower. smaller ones; margins smooth; shell surface smooth, Crenomytilus Soot-Ryen, 1955, differs from marked only by concentric growth lines and irregular Plicatomytilus in possessing crenulate shell margins, in undulations of growth; shell strongly plicate toward having an obliquely
Recommended publications
  • Download Full Article in PDF Format
    A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans Robert W. BOESSENECKER Department of Geology, University of Otago, 360 Leith Walk, P.O. Box 56, Dunedin, 9054 (New Zealand) and Department of Earth Sciences, Montana State University 200 Traphagen Hall, Bozeman, MT, 59715 (USA) and University of California Museum of Paleontology 1101 Valley Life Sciences Building, Berkeley, CA, 94720 (USA) [email protected] Boessenecker R. W. 2013. — A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans. Geodiversitas 35 (4): 815-940. http://dx.doi.org/g2013n4a5 ABSTRACT e newly discovered Upper Miocene to Upper Pliocene San Gregorio assem- blage of the Purisima Formation in Central California has yielded a diverse collection of 34 marine vertebrate taxa, including eight sharks, two bony fish, three marine birds (described in a previous study), and 21 marine mammals. Pinnipeds include the walrus Dusignathus sp., cf. D. seftoni, the fur seal Cal- lorhinus sp., cf. C. gilmorei, and indeterminate otariid bones. Baleen whales include dwarf mysticetes (Herpetocetus bramblei Whitmore & Barnes, 2008, Herpetocetus sp.), two right whales (cf. Eubalaena sp. 1, cf. Eubalaena sp. 2), at least three balaenopterids (“Balaenoptera” cortesi “var.” portisi Sacco, 1890, cf. Balaenoptera, Balaenopteridae gen. et sp. indet.) and a new species of rorqual (Balaenoptera bertae n. sp.) that exhibits a number of derived features that place it within the genus Balaenoptera. is new species of Balaenoptera is relatively small (estimated 61 cm bizygomatic width) and exhibits a comparatively nar- row vertex, an obliquely (but precipitously) sloping frontal adjacent to vertex, anteriorly directed and short zygomatic processes, and squamosal creases.
    [Show full text]
  • A Review of Ethnographic and Historically Recorded Dentaliurn Source Locations
    FISHINGFOR IVORYWORMS: A REVIEWOF ETHNOGRAPHICAND HISTORICALLY RECORDEDDENTALIUM SOURCE LOCATIONS Andrew John Barton B.A., Simon Fraser University, 1979 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS IN THE DEPARTMENT OF ARCHAEOLOGY Q Andrew John Barton 1994 SIMON FRASER UNIVERSITY Burnaby October, 1994 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means without permission of the author. Name: Andrew John Barton Degree: Master of Arts (Archaeology) Title of Thesis: Fishing for Ivory Worms: A Review of Ethnographic and Historically Recorded Dentaliurn Source Locations Examining Committee: Chairperson: Jack D. Nance - -, David V. Burley Senior Supervisor Associate Professor Richard Inglis External Examiner Department of Aboriginal Affairs Government of British Columbia PARTIAL COPYRIGHT LICENSE I hereby grant to Simon Fraser University the right to lend my thesis or dissertation (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for multiple copying of this thesis for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Title of ThesisIDissertation: Fishing for Ivory Worms: A Review of Ethnographic and Historically Recorded Dentalium Source Locations Author: Andrew John Barton Name October 14, 1994 Date This study reviews and examines historic and ethnographic written documents that identify locations where Dentaliurn shells were procured by west coast Native North Americans.
    [Show full text]
  • Mio-Oligocene (Aquitanian) Foraminifera from the Goajira Peninsula, Colombia
    CUSHMAN FOUNDATION FOil FOHAMINIFEHAL HESEAHCH SPECIAL PUBLICATION NO.4 MIO-OLIGOCENE (AQUITANIAN) FORAMINIFERA FROM THE GOAJIRA PENINSULA, COLOMBIA BY LEHOY E. BECKEH and A. N. DUSENBURY, Jr. FEBIWAH\ 15. 19;)3 Prke $2.00 postpaid CONTENTS ABSTRACT Il\TRODlJCTION 5 List of Samples 5 Identification. 5 Ackn"wlcdgments 5 ECOLOGY 6 AGE 6 CORREIXfION 6 SYSTEMATIC DESCRIPTIONS OF SPECIES 8 BIBLIOGRAPHY 46 ·Pi/uranu '\ ft If (, \\ "\\ J ;/ •~... ~ CA$TILLETES ,," t/'" /J i'f~ MAP SHOWING COLLECTING LOCALITIES GOA.JIRA PENINSULA COLOMBIA o 2 4 8 10 12 I I I , I I ! " Ki Iometers ( 4- 1 MIO-OLIGOCENE (AQUITANIAK) FORAMINIFERA FROM THE GOAJIRA PENINSULA, COLOMBIAI LEROY E. BECKER ANlJ A. N. DUSENBURY, JR. Maracaibo, Venezuela 1 dentiiicatioll Tlw fonuninir"ntl rauna:-; at t'itlHl an;] ~illtlmaHa. Several comprehensive papers on the Tertiarv Fo­ ColomlJi::., have heen tliyidl'd illlo ;I~ genera Hnd 1:-17 I aminif"ra of northern South America and the Carib­ HIH:·cif"~. ~f'\'l'n IH'''W i->lWch-;o arE' (\ps(:ribed. The fon.t1lli­ njft:ral a~sell\llJagE's indicaip a ),llo-ulig"o('E'lH::' (Aquitanian) bean islands have been published recently. The writers ag'e and a Jnat'inp, Ol/f'H-:'W<I f-nvil'onnlPl1t IlptWPPH li)i) and have compared their Goajiran Foraminifera with those :JOt) talholllH in tlf1-pth, CnITt'latioll};, ha~H'(l on FOl'aminif­ appearing in the published literamre dealing primarily era, are :SUgg('sif>(l ht'l\vf'f'1l thf' '\iio-Oli).w('('nf' l,ed:-; or the with the Miocene and Oligocene of the Caribhean area.
    [Show full text]
  • Qt53v080hx.Pdf
    UC Berkeley PaleoBios Title A new Early Pliocene record of the toothless walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California Permalink https://escholarship.org/uc/item/53v080hx Journal PaleoBios, 34(0) ISSN 0031-0298 Author Boessenecker, Robert W. Publication Date 2017-06-15 DOI 10.5070/P9341035289 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PaleoBios 34:1-6, June 15, 2017 PaleoBios OFFICIAL PUBLICATION OF THE UNIVERSITY OF CALIFORNIA MUSEUM OF PALEONTOLOGY Boessenecker, Robert W. (2017). A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California. Cover photo: Life restoration of the extinct Pliocene walrus Valenictus and flightless auks (Mancalla) hauled out on the rocky shore of the uplifted Coast Ranges of California (top right); cliff exposures of the Purisima Formation near Santa Cruz, from where Valenictus was collected by Wayne Thompson (left); bivalves, chiefly Clinocardium meekianum, exposed in the Purisima Formation near the locality (bottom). Photo credit and original artwork: Robert W. Boessenecker. Citation: Boessenecker, Robert W. 2017. A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Puri- sima Formation of Northern California. PaleoBios, 34. ucmp_paleobios_35289 A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California ROBERT W. BOESSENECKER1,2 1Department of Geology and Environmental Geosciences, College of Charleston, Charleston, SC 29424; [email protected] 2University of California Museum of Paleontology, University of California, Berkeley, CA 94720 The walrus (Odobenus rosmarus) is a large tusked molluskivore that inhabits the Arctic and is the sole living member of the family Odobenidae.
    [Show full text]
  • Microanatomical Studies of Dentalium Pilsbryi Rehder, 1942 and D. Texasianum Philippi, 1848 Kenneth R
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Open-Access* Master's Theses from the University Libraries at University of Nebraska-Lincoln of Nebraska-Lincoln 7-1974 Microanatomical Studies of Dentalium pilsbryi Rehder, 1942 and D. texasianum Philippi, 1848 Kenneth R. Bazata University of Nebraska-Lincoln Follow this and additional works at: http://digitalcommons.unl.edu/opentheses Part of the Zoology Commons Bazata, Kenneth R., "Microanatomical Studies of Dentalium pilsbryi Rehder, 1942 and D. texasianum Philippi, 1848" (1974). Open- Access* Master's Theses from the University of Nebraska-Lincoln. 31. http://digitalcommons.unl.edu/opentheses/31 This Thesis is brought to you for free and open access by the Libraries at University of Nebraska-Lincoln at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Open-Access* Master's Theses from the University of Nebraska-Lincoln by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. MICROANAT0t1ICAL STUDIES OF DENTALIUM PILSBRYI REHDER, 1942 AND D. TEXASIANUM PHILIPPI, 1848 by Kenneth R. Bazata A THESIS Presented to the Faculty of The Graduate College in the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Department of Zoology Under the Supervision of Dr. Carl W. Gugler Lincoln, Nebraska July, 1974 ACKNm~LEDGEt1ENTS The author wishes to express sincere thanks to Dr. Carl W. Gugler for his encouragement and guidance during the research and writing of this thesis. Sincere thanks are also given to my parents, Mr. and Mrs. Rudolph Bazata. The author hopes one day to achieve the knowledge of life my parents and Dr.
    [Show full text]
  • Bulletin 111
    SMITHSONIAN INSTITUTION UNITED STATES NATIONAL MUSEUM Bulletin 111 A MONOGRAPH OF THE EAST AMERICAN SCAPHOPOD MOLLUSKS BY JOHN B. HENDERSON Of Washington, District of Columbia WASHINGTON GOVERNMENT PRINTING OFFICE 1920 ADVERTISEMENT. States National Museum The scientific publications of the United the Bulletins. consist of two series, the Proceedings and issued m 1878, are The Proceedings, the first volume of which was publication of original, and intended primarily as a medium for the of the National Museum, usually brief, papers based on the collections geology, and anthro- presentincr newly acquired facts in zoology, animals, and revisions pology, including descriptions of new forms of are issued annually and dis- of limited groups. One or two volumes organizations. A limited number tributed to libraries and scientific form, is distributed to specialists of copies of each paper, in pamphlet as soon as printed. and others interested in the different subjects, the tables of contents of the The dates of publication are recorded in . volumes. „ issued m 1875, consist ot a The Bulletins, the first of which was comprising chiefly monographs ot series of separate publications general systematic treatises (occa- laro-e zoological groups and other works, reports of expeditions, and sionally in several volumes), faunal collections, etc. ihe majority catalogues of type-specimens, special quarto size has been adopted m a of the volumes^re octavos, but a regarded as indispensable. few instances in which large plates were containing papers relating to Since 1902 a series of octavo volumes and known as the Contribu- the botanical collections of the Museum, has been published as bulletins.
    [Show full text]
  • The Taxonomic and Evolutionary History of Fossil and Modern Balaenopteroid Mysticetes
    Journal of Mammalian Evolution, Vol. 12, Nos. 1/2, June 2005 (C 2005) DOI: 10.1007/s10914-005-6944-3 The Taxonomic and Evolutionary History of Fossil and Modern Balaenopteroid Mysticetes Thomas A. Demer´ e,´ 1,4 Annalisa Berta,2 and Michael R. McGowen2,3 Balaenopteroids (Balaenopteridae + Eschrichtiidae) are a diverse lineage of living mysticetes, with seven to ten species divided between three genera (Megaptera, Balaenoptera and Eschrichtius). Extant members of the Balaenopteridae (Balaenoptera and Megaptera) are characterized by their engulfment feeding behavior, which is associated with a number of unique cranial, mandibular, and soft anatomical characters. The Eschrichtiidae employ suction feeding, which is associated with arched rostra and short, coarse baleen. The recognition of these and other characters in fossil balaenopteroids, when viewed in a phylogenetic framework, provides a means for assessing the evolutionary history of this clade, including its origin and diversification. The earliest fossil balaenopterids include incomplete crania from the early late Miocene (7–10 Ma) of the North Pacific Ocean Basin. Our preliminary phylogenetic results indicate that the basal taxon, “Megaptera” miocaena should be reassigned to a new genus based on its possession of primitive and derived characters. The late late Miocene (5–7 Ma) balaenopterid record, except for Parabalaenoptera baulinensis and Balaenoptera siberi, is largely undescribed and consists of fossil specimens from the North and South Pacific and North Atlantic Ocean basins. The Pliocene record (2–5 Ma) is very diverse and consists of numerous named, but problematic, taxa from Italy and Belgium, as well as unnamed taxa from the North and South Pacific and eastern North Atlantic Ocean basins.
    [Show full text]
  • 692 Association Round Table
    692 Association Round Table Chrons C19r and C20n, based on a 40Ar/39Ar date of 42.8J ± 0.24 Ma in rocks tracers, particularly when taking into account hydrothermal alteration and of normal polarity (contrary to Bottjer et 31., 1991, who correlated it with Chror. mantle metasomatism. Furthermore, Neogene arc systems show reorgan­ C18n based on questionable P13 Zone planktonic foraminifera). These ization in magmatic loci and microplates at time scales comparable to correlations contradict several sequence stratigraphic correlations of these typical uncertainties in absolute age determinations. strata May et al. (1984), May (1985) and May and Warme (1987) correlated the Friars/Stadium contact with nan no zone CP1 5b and foram zone P1 5 (about 36 Ma), but this clearly clearly conflicts with the date on the overlying Mission Critical stratigraphic, structural, and timing relations within the Valley Formation by at least 6 million years. western Sierra Nevada, California, and their bearing on models for origin of the Foothills terrane and the Great Valley basin Magnetic Stratigraphy of the Type Zemorrian Stage (Oligocene), Lower Temblor Formation, Temblor Range, Kern County, California SCHWEICKERT, RICHARD A., Department of Geological Sciences, University of Nevada, Reno, NV RESSEGUIE, JENNIFER L., and DONALD R. PROTHERO, Department of Geology, Occidental College, Los Angeles, CA Several models exist for Jurassic-Cretaceous evolution of the western Sierra Nevada, the adjacent Great Valley basin, and the Coast Range ophiolite, Kleinpell (1938) erected the Zemorrian stage based on benthic foraminifera as recently clarified by Dickinson and others (1996). To evaluate the models from the lower Temblor Formation in Zemorra Creek, southern Temblor Range, requires both an examination of critical stratigraphic and structural relations Kern County, California.
    [Show full text]
  • Supplementary Information
    Supplementary Information Substitution Rate Variation in a Robust Procellariiform Seabird Phylogeny is not Solely Explained by Body Mass, Flight Efficiency, Population Size or Life History Traits Andrea Estandía, R. Terry Chesser, Helen F. James, Max A. Levy, Joan Ferrer Obiol, Vincent Bretagnolle, Jacob González-Solís, Andreanna J. Welch This pdf file includes: Supplementary Information Text Figures S1-S7 SUPPLEMENTARY INFORMATION TEXT Fossil calibrations The fossil record of Procellariiformes is sparse when compared with other bird orders, especially its sister order Sphenisciformes (Ksepka & Clarke 2010, Olson 1985c). There are, however, some fossil Procellariiformes that are both robustly dated and identified and therefore suitable for fossil calibrations. Our justification of these fossils, below, follows best practices described by Parham et al. (2012) where possible. For all calibration points only a minimum age was set with no upper constraint specified, except for the root of the tree. 1. Node between Sphenisciformes/Procellariiformes Minimum age: 60.5 Ma Maximum age: 61.5 Ma Taxon and specimen: Waimanu manneringi (Slack et al. 2006); CM zfa35 (Canterbury Museum, Christchurch, New Zealand), holotype comprising thoracic vertebrae, caudal vertebrae, pelvis, femur, tibiotarsus, and tarsometatarsus. Locality: Basal Waipara Greensand, Waipara River, New Zealand. Phylogenetic justification: Waimanu has been resolved as the basal penguin taxon using morphological data (Slack et al. 2006), as well as combined morphological and molecular datasets (Ksepka et al. 2006, Clarke et al. 2007). Morphological and molecular phylogenies agree on the monophyly of Sphenisciformes and Procellariiformes (Livezey & Zusi 2007, Prum et al. 2015). Waimanu manneringi was previously used by Prum et al. (2015) to calibrate Sphenisiciformes, and see Ksepka & Clarke (2015) for a review of the utility of this fossil as a robust calibration point.
    [Show full text]
  • Marine Shell Hoard from the Late Neolithic Site of :Epin-Ov;Ara (Slavonia, Croatia)
    Documenta Praehistorica XLIII (2016) Marine shell hoard from the Late Neolithic site of :epin-Ov;ara (Slavonia, Croatia) Boban Tripkovic´ 1, Vesna Dimitrijevic´ 2 and Dragana Rajkovic´ 3 1 Department of Archaeology, Faculty of Philosophy, University of Belgrade, RS [email protected] 2 Laboratory for Bioarchaeology, Department of Archaeology, Faculty of Philosophy, University of Belgrade, RS [email protected] 3 Museum of Slavonia in Osijek, HR [email protected] ABSTRACT – The focus of this paper is the ornament hoard from the Sopot culture site of ∞epin-Ov- ≠ara in eastern Slavonia (the Republic of Croatia). The hoard contained pendants and beads made of shells of marine clam Spondylus gaederopus and scaphopod Antalis vulgaris. The paper analyses the context and use wear of the objects in the hoard. The results form a basis for: the reconstruction of the role of some of the items and the ways in which they were worn; the premise that the dynam- ics and mechanisms of acquisition of ornaments made of the two Mediterranean mollusc species could have differed; and the identification of a cross-cultural pattern of deposition of ornament hoards. IZVLE∞EK – V ≠lanku se osredoto≠amo na zakladno najdbo z nakitom iz ≠asa sopotske kulture na najdi∏≠u ∞epin-Ov≠ara v vzhodni Slavoniji (Republika Hrva∏ka). Depo vsebuje obeske in jagode, iz- delane iz lupin morskih ∏koljk vrste Spondylus gaederopus in pol∫kov vrste Antalis vulgaris. V ≠lanku analiziramo kontekste in sledove uporabe teh izdelkov. Rezultati nam nudijo osnovo za: rekonstruk- cijo vloge nekaterih izdelkov in na≠inov no∏enja nakita; premiso o razli≠nih dinamikah in mehaniz- mih pridobivanja okrasov iz dveh sredozemskih vrst mehku∫cev; in za prepoznavanje medkulturnih vzorcev odlaganja zakladnih najdb z nakitom.
    [Show full text]
  • Appendix G Paleontological Resources Assessment
    Appendix G Paleontological Resources Assessment Paleontological Resource Assessment for the California Flats Solar Project, Monterey and San Luis Obispo Counties, California Jessica L. DeBusk Prepared By Applied EarthWorks, Inc. 743 Pacific Street, Suite A San Luis Obispo, CA 93401 Prepared For Element Power US, LLC 421 SW Sixth Avenue, Suite 1000 Portland, OR 97204 April 2013 draft SUMMARY OF FINDINGS At the request of Element Power US, LLC, parent company of California Flats Solar, LLC (the Applicant), Applied EarthWorks Inc. (Æ) performed a paleontological resource assessment for the California Flats Solar Project (Project) located southeast of Parkfield in Monterey and San Luis Obispo counties, California. The study consisted of a museum records search, a comprehensive literature and geologic map review, and a field survey. This report summarizes the methods and results of the paleontological resource assessment and provides Project-specific management recommendations. This assessment included a comprehensive review of published and unpublished literature and museum collections records maintained by the Natural History Museum of Los Angeles County (LACM) and the University of California Museum of Paleontology (UCMP). The purpose of the literature review and museum records search was to identify the geologic units underlying the Project area and to determine whether or not previously recorded paleontological localities occur either within the Project boundaries or within the same geologic units elsewhere. The museum records search was followed by a field survey. The purpose of the field survey was to visually inspect the ground surface for exposed fossils and to evaluate geologic exposures for their potential to contain preserved fossil material at the subsurface.
    [Show full text]
  • Formation, Central Chile, South America
    Cainozoic Research, 3-18, 2006 4(1-2), pp. February An Early Miocene elasmobranch fauna from the Navidad Formation, Central Chile, South America ³* Mario+E. Suarez Alfonso Encinas² & David Ward ¹, 'Museo Paleontoldgico de Caldera, Cousino, 695, Caldera, Atacama, Chile, [email protected] 2 Departamento de Geologia. Universidad de Chile, Plaza Ercilla 803, Santiago Chile. [email protected] J David J. Kent ME4 4AW UK. Ward, School of Earth Sciences, University of Greenwich, Chatham Maritime, Address for correspon- dence: Crofton Court, 81 Crofton Lane, Orpington, Kent BR5 1HB, UK. E-mail: [email protected]. [* corresponding author] Received 5 March 2003; revised version accepted 12 January 2005 A rich elasmobranch assemblage is reported from the Early Neogenemarine sediments ofthe lower member of the NavidadFormation, Central Chile. The fauna comprise Squalus sp., Pristiophorus sp., Heterodontus sp., Megascyliorhinus trelewensis. Carcharias cuspi- data, Isurus hastalis, Carcharoides and Cal- Odontaspisferox, oxyirinchus,Isurus hastalis, Cosmopolitodus totuserratus, Myliobatis sp. for the the Miocene The of lorhinchus sp., all ofwhich are reported first time in Early ofChile. presence Carcharoides totuserratus sup- the Miocene for the lower ofthe basal Navidad Formation. The Chilean fossil elasmobranch fauna is ports Early age part representedby deep water and shallow water taxa, which probably were mixed in a submarine fan. Certain taxa suggest warm-temperate waters. The Early Miocene fauna from the Navidad Formation show affinities with other faunas previously reported from the Late Paleogene and Neogene of Argentina and New Zealand. Se describe rica asociacion de fosiles veniente de los sedimentos marines del Inferior de la Formación una elasmobranquios pro Neogeno central.
    [Show full text]