Park Paleontology 8(2)
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PIR/PER) for the State Route 86 / Avenue 50 New Interchange Project, City of Coachella, Riverside County, California E-FIS 0801-000144 (EA 08-0C970
Combined Paleontological Identification Report / Paleontological Evaluation Report (PIR/PER) for the State Route 86 / Avenue 50 New Interchange Project, City of Coachella, Riverside County, California E-FIS 0801-000144 (EA 08-0C970) Submitted to: Kurt Heidelberg, Branch Chief Environmental Studies D California Department of Transportation, District 8 464 West 4th Street, 6th Floor, MS 825 San Bernardino, California 92401-1400 March 2018 EXECUTIVE SUMMARY The City of Coachella (City), in cooperation with the California Department of Transportation (Caltrans) District 8 and Coachella Valley Association of Governments (CVAG), proposes the construction of a new interchange at State Route 86 (SR-86) and Avenue 50 in the City of Coachella, Riverside County, California. The SR-86 /Avenue 50 New Interchange Project (Project) consists of converting a portion of SR-86 from an existing expressway to a freeway with a new overcrossing structure and access ramps. In addition, the proposed Project includes the realignment and widening of Avenue 50 and the realignment of portions of Tyler Street on both the east and west sides of SR-86. Finally, the Project would construct a new bridge over the Coachella Valley Stormwater Channel (CVSC) to replace the existing low water crossing. At the request of TranSystems, Applied EarthWorks, Inc. (Æ) performed a paleontological resource assessment in support of the proposed Project. The study consisted of a search of museum collections records maintained by the Natural History Museum of Los Angeles County, a comprehensive literature and geologic map review, a field reconnaissance survey, and preparation of this combined Paleontological Identification Report (PIR) / Paleontological Evaluation Report (PER). -
Micropaleontological Association from the Middle Miocene Badenian Gypsum Deposits of Paratethys
geosciences Article A New Preparation Method of Microfauna from Gypsum: Micropaleontological Association from the Middle Miocene Badenian Gypsum Deposits of Paratethys Hans-Peter Bojar 1, Claudia Antoniade 2, Victor Barbu 3 and Ana-Voica Bojar 1,4,5,* 1 Studienzentrum Naturkunde—Mineralogie, Universalmuseum Joanneum, Weinzöttlstraße 16, 8045 Graz, Austria; [email protected] 2 OMV Petrom, Research and Design Institute of Technology Petrom Câmpina, Culturii Bldv 29, Câmpina, 15600 Prahova, Romania; [email protected] 3 OMV Petrom, Coralilor str. 22, 013329 Bucharest, Romania; [email protected] 4 Department Geographie und Geologie, Geologie, University of Salzburg, Hellbrunnerstraße 34, 5020 Salzburg, Austria 5 Faculty of Physics, Department of Structure of Matter, Earth and Atmospheric Physics and Astrophysics, University of Bucharest, Bulevardul Regina Elisabeta 4-12, 030018 Bucharest, Romania * Correspondence: [email protected] Received: 23 March 2020; Accepted: 26 April 2020; Published: 28 April 2020 Abstract: Evaporitic gypsum deposits represent an important paleoenvironmental record of the Miocene Badenian of the Carpathian Mountains belt. In this study, we developed a nontoxic method to concentrate calcareous microfossils from gypsum (CaSO 2H O), by treating the sulfate with 4· 2 ammonium acetate. We applied the newly developed method to gypsum collected from the Evaporitic Formation outcropping northward of Slănic-Prahova in the Eastern Carpathians. For the first time for this formation, we describe a calcareous microfossil assemblage characterized by the presence of planktonic foraminifera as well as cysts and fragments of calcareous algae. Keywords: chemical preparation method; gypsum deposits; calcareous microfossil assemblage; Miocene; Eastern Carpathians 1. Introduction In the Earth’s history, sulfate rich marine waters are known for late Precambrian (Vendian), Pennsylvanian-Triassic, Miocene to Quaternary [1]. -
8-2 Kihm 2011
Paludicola 8(2):75-90 March 2011 © by the Rochester Institute of Vertebrate Paleontology RODENTS FROM THE CHADRONIAN (LATEST EOCENE) MEDICINE POLE HILLS LOCAL FAUNA, NORTH DAKOTA. PART 1. EUTYPOMYIDAE, CYLINDRODONTIDAE AND PIPESTONEOMYS Allen J. Kihm Department of Geosciences, Minot State University, 500 University Ave W, Minot, ND 58707 <[email protected]> ABSTRACT The Medicine Pole Hills local fauna is a large Chadronian fauna composed of more than 4600 mammal specimens, mostly isolated teeth, derived from a limited sequence of mudball conglomerates and sandstones. The producing layer probably represents an early stage of deposition of the Chadron Formation in North Dakota, but it may not be related to any of the named members of the formation. The material described includes Eutypomys parvus, Cylindrodon collinus, Pseudocylindrodon neglectus, Ardynomys saskatchewensis and Pipestoneomys sp. The samples of E. parvus and A. saskatchewensis include teeth not previously described for these taxa. The assemblage has the greatest commonality to the middle Chadronian Calf Creek local fauna of southern Saskatchewan. This similarity does not necessarily indicate a middle Chadronian age for the Medicine Pole Hills local fauna. The lack of late early Chadronian localities with large samples of rodents may exaggerate the apparent differences between these faunas and the Medicine Pole Hills sample. The Calf Creek and Medicine Pole Hills local faunas may represent an intermediate stage between the McCarty’s Mountain and Pipestone Springs faunas of Montana. The Medicine Pole Hills fauna may be somewhat older than the Calf Creek local fauna based on the occurrence of Leptomeryx yoderi. INTRODUCTION (Murphy et al., 1993), but continuing studies of the geology, particularly the heavy minerals, suggest this This is the third in a series of papers that describe correlation is poorly supported (Webster and Kihm, the mammals of the Medicine Pole Hills local fauna of 2009). -
Raymond M. Alf Museum of Paleontology EDUCATOR's GUIDE
Raymond M. Alf Museum of Paleontology EDUCATOR’S GUIDE Dear Educator: This guide is recommended for educators of grades K-4 and is designed to help you prepare students for their Alf Museum visit, as well as to provide resources to enhance your classroom curriculum. This packet includes background information about the Alf Museum and the science of paleontology, a summary of our museum guidelines and what to expect, a pre-visit checklist, a series of content standard-aligned activities/exercises for classroom use before and/or after your visit, and a list of relevant terms and additional resources. Please complete and return the enclosed evaluation form to help us improve this guide to better serve your needs. Thank you! Paleontology: The Study of Ancient Life Paleontology is the study of ancient life. The history of past life on Earth is interpreted by scientists through the examination of fossils, the preserved remains of organisms which lived in the geologic past (more than 10,000 years ago). There are two main types of fossils: body fossils, the preserved remains of actual organisms (e.g. shells/hard parts, teeth, bones, leaves, etc.) and trace fossils, the preserved evidence of activity by organisms (e.g. footprints, burrows, fossil dung). Chances for fossil preservation are enhanced by (1) the presence of hard parts (since soft parts generally rot or are eaten, preventing preservation) and (2) rapid burial (preventing disturbance by bio- logical or physical actions). Many body fossils are skeletal remains (e.g. bones, teeth, shells, exoskel- etons). Most form when an animal or plant dies and then is buried by sediment (e.g. -
FOSSIL PREPARATION KIT by Dave Letasi and Terrie Nolinske
p FOSSIL PREPARATION KIT By Dave Letasi and Terrie Nolinske DESCRIPTION This kit includes a real fossil bone from a prehistoric animal and a fossil of a marine animal. A scientific label is also provided with your fossil specimens. The Fossil Preparation Kit instructs you in the cleaning and preparation of invertebrate and vertebrate fossils, following the same process used by paleontologists. By adding several common household items, you can create a fossil preparation lab in your classroom or kitchen. In the first activity, you use basic tools to clean a marine invertebrate fossil. Using a mild household chemical, you will remove the rocky crust found on the fossil and study the details of its anatomical structures. In the second activity, you will preserve fossil vertebrate bone fragments before fitting the fragments back together to create the original structure. GOALS You will be able to… demonstrate procedures used by scientists to reconstruct fossil fragments and turn them into specimens for study or display; learn and implement scientific procedures used in the safe handling of chemicals used for cleaning fossils; and identify at least three ways in which fossils allow scientists to study life forms from the prehistoric past. ARE YOU A TEACHER? The subject matter in this kit is aligned with the following Sunshine State Standards: Grades 3-5: SC. D.1.2.1, SC. D. 2.2.1 SC. H.! 2.1, SC.H.1.2.2, SC.H.2.2.1 Grades 6-8: SC.D.1.3.1, SC.h.1.3.1, SC.H.1.3.2, SC.G.2.3.1 Grades 9-12: SC.D.1.4.2, SC.D.1.4.4, SC.D.2.4.1, SC.G.2.4.1 2 HELPFUL TIPS To complement activities in this kit, you might want to read about prehistory and fossils before you start. -
Novitatesamerican MUSEUM PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET NEW YORK, N.Y
NovitatesAMERICAN MUSEUM PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET NEW YORK, N.Y. 10024 U.S.A. NUMBER 2626 JUNE 30, 1977 JOHN H. WAHLERT Cranial Foramina and Relationships of Eutypomys (Rodentia, Eutypomyidae) AMERICAN MUSEUM Novitates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2626, pp. 1-8, figs. 1-3, table 1 June 30, 1977 Cranial Foramina and Relationships of Eutypomys (Rodentia, Eutypomyidae) JOHN H. WAHLERT1 ABSTRACT Derived characters of the sphenopalatine, lies had common ancestry in a stem species from interorbital, and dorsal palatine foramina are which no other rodent groups are descended. The shared by the Eutypomyidae and Castoridae. two families may be included in a monophyletic These support the hypothesis that the two fami- superfamily, Castoroidea. INTRODUCTION Eutypomys is an extinct sciuromorphous gave more characters shared with castorids; he, rodent known in North America from strata that too, found many features in common with the range in age from latest Eocene to early Miocene. ischyromyoids. Wood noted the similarity of The genus was named by Matthew (1905) based molar crown pattern to that of Paramys and ex- on the species Eutypomys thomsoni. "Progres- plained it as a parallelism that possibly indicates sive" characters of the teeth and hind feet led relationship. Wilson (1949b) pointed out that the Matthew to ally it with the beaver family, Cas- dental pattern of Eutypomys is more like that of toridae. He pointed out that it retains many sciuravids than that of paramyids. -
INSIGHTS INTO RELATIONSHIPS AMONG RODENT LINEAGES BASED on MITOCHONDRIAL GENOME SEQUENCE DATA a Dissertation by LAURENCE JOHN FR
INSIGHTS INTO RELATIONSHIPS AMONG RODENT LINEAGES BASED ON MITOCHONDRIAL GENOME SEQUENCE DATA A Dissertation by LAURENCE JOHN FRABOTTA Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY December 2005 Major Subject: Zoology INSIGHTS INTO RELATIONSHIPS AMONG RODENT LINEAGES BASED ON MITOCHONDRIAL GENOME SEQUENCE DATA A Dissertation by LAURENCE JOHN FRABOTTA Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Approved by: Chair of Committee, Rodney L. Honeycutt Committee Members, James B. Woolley John W. Bickham James R. Manhart Head of Department, Vincent M. Cassone December 2005 Major Subject: Zoology iii ABSTRACT Insights into Relationships among Rodent Lineages Based on Mitochondrial Genome Sequence Data. (December 2005) Laurence John Frabotta, B.S.; M.S., California State University, Long Beach Chair of Advisory Committee: Dr. Rodney L. Honeycutt This dissertation has two major sections. In Chapter II, complete mitochondrial (mt DNA) genome sequences were used to construct a hypothesis for affinities of most major lineages of rodents that arose quickly in the Eocene and were well established by the end of the Oligocene. Determining the relationships among extant members of such old lineages can be difficult. Two traditional schemes on subordinal classification of rodents have persisted for over a century, dividing rodents into either two or three suborders, with relationships among families or superfamilies remaining problematic. The mtDNA sequences for four new rodent taxa (Aplodontia, Cratogeomys, Erethizon, and Hystrix), along with previously published Euarchontoglires taxa, were analyzed under parsimony, likelihood, and Bayesian criteria. -
A Palaeobiologist's Guide to 'Virtual' Micro-CT Preparation
Palaeontologia Electronica palaeo-electronica.org A palaeobiologist’s guide to ‘virtual’ micro-CT preparation Richard Leslie Abel, Carolina Rettondini Laurini, and Martha Richter ABSTRACT This paper provides a brief but comprehensive guide to creating, preparing and dissecting a ‘virtual’ fossil, using a worked example to demonstrate some standard data processing techniques. Computed tomography (CT) is a 3D imaging modality for producing ‘virtual’ models of an object on a computer. In the last decade, CT technol- ogy has greatly improved, allowing bigger and denser objects to be scanned increas- ingly rapidly. The technique has now reached a stage where systems can facilitate large-scale, non-destructive comparative studies of extinct fossils and their living rela- tives. Consequently the main limiting factor in CT-based analyses is no longer scan- ning, but the hurdles of data processing (see disclaimer). The latter comprises the techniques required to convert a 3D CT volume (stack of digital slices) into a virtual image of the fossil that can be prepared (separated) from the matrix and ‘dissected’ into its anatomical parts. This technique can be applied to specimens or part of speci- mens embedded in the rock matrix that until now have been otherwise impossible to visualise. This paper presents a suggested workflow explaining the steps required, using as example a fossil tooth of Sphenacanthus hybodoides (Egerton), a shark from the Late Carboniferous of England. The original NHMUK copyrighted CT slice stack can be downloaded for practice of the described techniques, which include segmenta- tion, rendering, movie animation, stereo-anaglyphy, data storage and dissemination. Fragile, rare specimens and type materials in university and museum collections can therefore be virtually processed for a variety of purposes, including virtual loans, web- site illustrations, publications and digital collections. -
Dosdall and Lehmkuhl 1979 Qev15n1 3 116 CC Released.Pdf
This work is licensed under the Creative Commons Attribution-Noncommercial-Share Alike 3.0 United States License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/3.0/us/ or send a letter to Creative Commons, 171 Second Street, Suite 300, San Francisco, California, 94105, USA. STONEFLIES (PLECOPTERA) OF SASKATCHEWAN LLOYD M. DOSDALL1 Biology Department University of Saskatchewan Saskatoon, Saskatchewan S7N0W0 D.M. LEHMKUHL Biology Department University of Saskatchewan Saskatoon, Saskatchewan Quaestiones Entomologicae S7N0W0 15:3-116 1979 Forty-one species, twenty-nine genera and eight families of Plecoptera are recorded from Saskatche wan. Distinguishing characters are given and keys are provided. Species recorded are: Pteronarcys dorsata (Say), Pteronarcella badia (Hagen), Taeniopteryx nivalis (Fitch), Oemopteryx fosketti (Packer), Capnia coloradensis Claassen, Capnia confusa Claassen, Capnia gracilaria Claassen, Capnia vernalis Newport, Paracapnia angulata Hanson, Isocapnia crinita (Needham and Claassen), Isocapnia missourii Ricker, Utacapnia trava (Nebeker and Gaufin), Nemoura rickeri Jewett, Shipsa rotunda (Claassen), Amphinemura linda (Ricker), Zapada cinctipes (Banks), Malenka californica (Claassenj, Podmosta delicatula (Claassen, Paraleuctra vershina Gaufin and Ricker, Leuctra ferruginea (Walker), Acroneuria abnormis (Newman), Acroneuria lycorias (Newman), Hesperoperla pacifica (Banks), C'laassenia sabulosa (Banks), Paragnetina media (Walker), Perlesta placida (Hagen), Isoperla bilineata (Say), -
NPS Museum Handbook, Part I Appendix U: Curatorial Care Of
Appendix U: Curatorial Care of Paleontological and Geological Collections Page Section I: Paleontological Collections.....................................................................................................U:1 A. Overview............................................................................................................................................U:1 What information concerning paleontological collections will I find in this appendix? .......................U:1 Why is it important to practice preventive conservation with paleontological specimens?................U:1 How do I learn about preventive conservation?.................................................................................U:1 Where can I find the latest information on care of paleontological specimens? ................................U:2 B. Paleontological Collections and Fossils ......................................................................................U:2 What are paleontological collections?................................................................................................U:2 What is a fossil? .................................................................................................................................U:2 Are there other types of fossils?.........................................................................................................U:2 How can I identify the fossils in my collection? ..................................................................................U:3 C. Body Fossils ....................................................................................................................................U:3 -
Fossil Footnotes
Fossil Footnotes Central Texas Paleontological Society March 2005 President’s Report FOSSIL of the MONTH Many of you have seen this before but it is worth Hi to all. Mercy this weather has been cold and showing again. It is a spectacular, perfectly nasty. I have been suffering with a bad cold as a preserved Cidarid sea urchin found by Mike result and am just now getting over it. I hope Smith a couple of years ago on a field trip to everyone else has made it through unscathed. Lake Travis hosted by Hal Hopkins. These are The one good thing, with all this rain, hopefully extremely rare and a once in a lifetime find. a lot of fossils will weather out for us to collect. Lower Cretaceous - Lower Glen Rose Formation We had a great February meeting with excellent attendance. A lot of new faces and new members attended which we were all very happy to see. Welcome to all of the new members. On a cool wet Saturday February the 19th four club members volunteered their time to man a table at the Austin Children’s Museum grand opening of there Dinosaur Expo. The four were Marcelle Spilker, David Lindberg, Mike Smith and Danny Harlow. There was excellent attendance and we all had a lot of fun showing the kids and parents Fossils of Texas. It will be open every Saturday on into the summer so go by a see it if you get a chance. See you at the March meeting! Danny March Meeting to be held on CTPS Minutes February 8, 2005 Tuesday, March 8, 2005 The meeting had a great turn out with several The March meeting will be at the LCRA new members. -
Aplodontid, Sciurid, Castorid, Zapodid and Geomyoid Rodents of the Rodent Hill Locality, Cypress Hills Formation, Southwest Saskatchewan
APLODONTID, SCIURID, CASTORID, ZAPODID AND GEOMYOID RODENTS OF THE RODENT HILL LOCALITY, CYPRESS HILLS FORMATION, SOUTHWEST SASKATCHEWAN A Thesis Submitted to the College of Graduate Studies and Research in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geological Sciences University of Saskatchewan Saskatoon By Sean D. Bell © Copyright Sean D. Bell, December 2004. All rights reserved. PERMISSION TO USE In presenting this thesis in partial fulfilment of the requirements for a Master’s degree from the University of Saskatchewan, I agree that the libraries of the University of Saskatchewan may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professors who supervised my thesis work or, in their absence, by the Head of the Department of Geological Sciences or the Dean of the College of Graduate Studies and Research. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other use of material in this thesis in whole or part should be addressed to: Head of the Department of Geological Sciences 114 Science Place University of Saskatchewan Saskatoon, Saskatchewan S7N 5E2 i ABSTRACT The Rodent Hill Locality is a fossil-bearing site that is part of the Cypress Hills Formation, and is located roughly 15 km northwest of the town of Eastend, Saskatchewan.