Bulletin 90 Tfiakhir PALEONTOLOGY •! 4
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Plant Rarity Under Federal and State Laws and Regulations
Plant Rarity Under Federal and State Laws and Regulations Various government laws, regulations and policies protect rare plants. Probably the most surprising aspect of rare plant protection is that, unlike animals, plants are the property of the landowner whether that might be an individual, corporation, or government agency. This means that the protection of rare plants is under control of the landowner unless, in some cases, a government-regulated action is affecting them. Then the government entity regulating the action may require that protection efforts take place to preserve the rare plants and their habitat. Federal Law One of the results of the environmental movement of the 1960s and 70s was the enactment of the Endangered Species Act of 1973 (https://www.fws.gov/endangered/laws-policies/index.html). The Act was designed to prevent the extinction of plants and animals, addressing problems of both exploitation and habitat destruction. The Act defines an endangered species as any species of animal or plant that is in danger of extinction over all or a significant portion of its range. A threatened species is defined as one that is likely to become endangered. The Act regulates the "taking" of endangered and threatened plants on federal land or when they are affected by federal actions or the use of federal funds. Specific protection is outlined in the Endangered Species Act of 1973 and states: It is unlawful for any person subject to the jurisdiction of the United States to: import any such species into, or export any such species -
Nautiloid Shell Morphology
MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOWER STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO MEMOIR 13 Nautiloid Shell Morphology By ROUSSEAU H. FLOIVER 1964 STATEBUREAUOFMINESANDMINERALRESOURCES NEWMEXICOINSTITUTEOFMININGANDTECHNOLOGY CAMPUSSTATION SOCORRO, NEWMEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS EXOFFICIO THEHONORABLEJACKM.CAMPBELL ................................ Governor of New Mexico LEONARDDELAY() ................................................... Superintendent of Public Instruction APPOINTEDMEMBERS WILLIAM G. ABBOTT ................................ ................................ ............................... Hobbs EUGENE L. COULSON, M.D ................................................................. Socorro THOMASM.CRAMER ................................ ................................ ................... Carlsbad EVA M. LARRAZOLO (Mrs. Paul F.) ................................................. Albuquerque RICHARDM.ZIMMERLY ................................ ................................ ....... Socorro Published February 1 o, 1964 For Sale by the New Mexico Bureau of Mines & Mineral Resources Campus Station, Socorro, N. Mex.—Price $2.50 Contents Page ABSTRACT ....................................................................................................................................................... 1 INTRODUCTION -
New Fossil Finds from the Cambro-Silurian Meta-Sediments on Hardangervidda
New Fossil Finds from the Cambro-Silurian Meta-sediments on Hardangervidda ARILD ANDRESEN Andresen, A. 1974: New fossil finds from the Cambro-Silurian meta-sedi ments on Hardangervidda. Norges geol. Unders. 304, 55-60. The occurrence of Actinoceroid cephalopods {Ormoceras (?) sp.), brachiopods {Orthis ss.), and trilobites {Ptycbopyge sp.) in a crystalline limestone over lying bluish quartzite on Hardangervidda indicates that Orthoceras Limestone of the Lower Ordovician Asaphus Series (Etage 3c) is present. The underlying quartzites are correlated with stage 3a-3b in the Oslo Region. A. Andresen, Mineralogisk-Geologisk Museum, Sarsgt. 1, Oslo 5, Norway Introduction Hardangervidda (Fig. 1) is, outside the Oslo Region, one of the largest areas in Norway where Cambro-Silurian sediments of eastern facies (foreland fac ies) are exposed. The stratigraphy and structure of these rocks are not very well known, partly because of the inaccessibility of the area, and partly due to the intense deformation and lack of fossiliferous beds. Even though the fossils described in this paper are badly preserved, making identification of species in some cases uncertain and in other cases impossible, they give some information about the Cambro-Silurian stratigraphy. The earliest contribution to the geology of Hardangervidda was made by Dahll (1861), who reported fossiliferous beds with Dictyonema flabelliforme (2e in the stratigraphic sequence of the Oslo Region) from Holberget (Fig. 1). Later, Brøgger (1893), after more detailed mapping, established a strati graphic sequence for the rocks overlying the Precambrian basement. In this sequence all the rocks above the Precambrian basement were assumed to be in a normal succession. The subdivision he established was, from the base upwards: 1, Alum shale; 2, Quartizite; 3, Crystalline limestone (marble); 4, Phyllites; 5, Various crystalline rocks. -
Cambrian Cephalopods
BULLETIN 40 Cambrian Cephalopods BY ROUSSEAU H. FLOWER 1954 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Eugene Callaghan, Director THE REGENTS MEMBERS Ex OFFICIO The Honorable Edwin L. Mechem ...................... Governor of New Mexico Tom Wiley ......................................... Superintendent of Public Instruction APPOINTED MEMBERS Robert W. Botts ...................................................................... Albuquerque Holm 0. Bursum, Jr. ....................................................................... Socorro Thomas M. Cramer ........................................................................ Carlsbad Frank C. DiLuzio ..................................................................... Los Alamos A. A. Kemnitz ................................................................................... Hobbs Contents Page ABSTRACT ...................................................................................................... 1 FOREWORD ................................................................................................... 2 ACKNOWLEDGMENTS ............................................................................. 3 PREVIOUS REPORTS OF CAMBRIAN CEPHALOPODS ................ 4 ADEQUATELY KNOWN CAMBRIAN CEPHALOPODS, with a revision of the Plectronoceratidae ..........................................................7 -
Topography Section References
Section 8 References 8. REFERENCES 1. Purpose and Need for the proposed Action Bureau of Indian Affairs (2006). Website. Retrieved May 24, 2006 from http://www.doi.gov/bureau-indian-affairs.html. 3.2.1 Topography Fenneman, N.M., & Johnson, D.W. (1946). Physical Divisions of the United States: Washington, DC. US Geological Survey Special Map Series. NASA Visible Earth Image catalog (1991, October 18). SRTM, Landsat. Retreived February 13, 2000, from http://visibleearth.nasa.gov USGS (2006). Seamless Data Distribution System. Earth Resources Observation and Science (EROS). United States Geological Survey. Retrieved March 22, 2006, from http://seamless.usgs.gov 3.2.2 Soils USDA– SCS (1987). Hydric Soils of the United States. United States Department of Agriculture– Soil Conservation Service. USDA. Natural Resource Conservation Service Soil Data Mart. United States Department of Agriculture. Retrieved from http://soildatamart.nrcs.usda.gov/. United States Department of Agriculture. Natural Resources Conservation Service. (1993, October). Soil Survey Manual. Retrieved April 8, 2006 from http://soils.usda.gov/technical/manual/print_version/chapter6.html U.S. Department of Agriculture, Natural Resources Conservation Service, (2005). National Soil Survey Handbook, title 430-VI. Retrieved from http://soils.usda.gov/technical/handbook/ 3.2.3 Geological Setting and Mineral Resources Cadwell, D.H., Connally, G.G., Dineen, R.J., Fleisher, P.J., & Rich, J.L. (1987) Surficial Geologic Map of New York – Hudson-Mohawk Sheet. New York State Museum Geological Survey. Bureau of Indian Affairs Draft EIS 8-1 Oneida Nation of New York Conveyance of Lands Into Trust Section 8 References Fisher, D.W., Isachsen, Y.W., & Rickard, L.V. -
Part I. Revision of Buttsoceras. Part II. Notes on the Michelinoceratida
MEMOIR 10 PART I Revision of Buttsoceras PART II Notes on the Michelinoceratida By ROUSSEAU H. FLOWER 1 9 6 2 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING AND TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Alvin J. Thompson, Director THE REGENTS MEMBERS Ex OFFICIO The Honorable Edwin L. Mechem ........................................ Governor of New Mexico Tom Wiley .......................................................... Superintendent of Public Instruction APPOINTED MEMBERS William G. Abbott ............................................................................................... Hobbs Holm 0. Bursum, Jr. ......................................................................................... Socorro Thomas M. Cramer ......................................................................................... Carlsbad Frank C. DiLuzio ...................................................................................... Albuquerque Eva M. Larrazolo (Mrs. Paul F.) ............................................................... Albuquerque Published October I2, 1962 For Sale by the New Mexico Bureau of Mines & Mineral Resources Campus Station, Socorro, N. Mex.—Price $2.00 Contents PART I REVISION OF BUTTSOCERAS Page ABSTRACT ....................................................................................................................... INTRODUCTION ............................................................................................................................. -
The Classic Upper Ordovician Stratigraphy and Paleontology of the Eastern Cincinnati Arch
International Geoscience Programme Project 653 Third Annual Meeting - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett – Kyle R. Hartshorn – Allison L. Young – Cameron E. Schwalbach – Alycia L. Stigall International Geoscience Programme (IGCP) Project 653 Third Annual Meeting - 2018 - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Kyle R. Hartshorn Dry Dredgers, 6473 Jayfield Drive, Hamilton, Ohio 45011, USA ([email protected]) Allison L. Young Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Cameron E. Schwalbach 1099 Clough Pike, Batavia, OH 45103, USA ([email protected]) Alycia L. Stigall Department of Geological Sciences and OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Lab, Athens, Ohio 45701, USA ([email protected]) ACKNOWLEDGMENTS We extend our thanks to the many colleagues and students who have aided us in our field work, discussions, and publications, including Chris Aucoin, Ben Dattilo, Brad Deline, Rebecca Freeman, Steve Holland, T.J. Malgieri, Pat McLaughlin, Charles Mitchell, Tim Paton, Alex Ries, Tom Schramm, and James Thomka. No less gratitude goes to the many local collectors, amateurs in name only: Jack Kallmeyer, Tom Bantel, Don Bissett, Dan Cooper, Stephen Felton, Ron Fine, Rich Fuchs, Bill Heimbrock, Jerry Rush, and dozens of other Dry Dredgers. We are also grateful to David Meyer and Arnie Miller for insightful discussions of the Cincinnatian, and to Richard A. -
Before Albany
Before Albany THE UNIVERSITY OF THE STATE OF NEW YORK Regents of the University ROBERT M. BENNETT, Chancellor, B.A., M.S. ...................................................... Tonawanda MERRYL H. TISCH, Vice Chancellor, B.A., M.A. Ed.D. ........................................ New York SAUL B. COHEN, B.A., M.A., Ph.D. ................................................................... New Rochelle JAMES C. DAWSON, A.A., B.A., M.S., Ph.D. ....................................................... Peru ANTHONY S. BOTTAR, B.A., J.D. ......................................................................... Syracuse GERALDINE D. CHAPEY, B.A., M.A., Ed.D. ......................................................... Belle Harbor ARNOLD B. GARDNER, B.A., LL.B. ...................................................................... Buffalo HARRY PHILLIPS, 3rd, B.A., M.S.F.S. ................................................................... Hartsdale JOSEPH E. BOWMAN,JR., B.A., M.L.S., M.A., M.Ed., Ed.D. ................................ Albany JAMES R. TALLON,JR., B.A., M.A. ...................................................................... Binghamton MILTON L. COFIELD, B.S., M.B.A., Ph.D. ........................................................... Rochester ROGER B. TILLES, B.A., J.D. ............................................................................... Great Neck KAREN BROOKS HOPKINS, B.A., M.F.A. ............................................................... Brooklyn NATALIE M. GOMEZ-VELEZ, B.A., J.D. ............................................................... -
Holochoanites Are Endoceroids Rousseau H
HOLOCHOANITES ARE ENDOCEROIDS ROUSSEAU H. FLOWER, New York State Museum Albany 1, N. Y. INTRODUCTION The Holochoanites may be defined as those cephalopods in which the septal necks are so elongated that they extend from the septum of which they are a part and a prolongation, apicad to the next septum, or even farther. Hyatt (1884) first regarded the Holochoanoidea as one of two major divisions of the Nautiloidea. Later (1900) he replaced his other division, the Ellipochoanoidea, by four divisions the Orthochaonites, Cyrtochoanites, Schistochoanites and Mixochoanites, and changed the name Holochoanoidea to Holochoanites for uniformity. In the mean- time, further study caused him to modify the contents of the holochoanitic division materially. Some genera originally placed in this group, such as Trocholites, proved upon further study to possess ellipochoanitic septal necks. The genus Aturia, while properly holochoanitic, was removed, because it was recognized that it represented a development of elongated septal necks in Tertiary time, which was obviously quite unrelated to that of other holochoanitic cephalopods, few of which survived the close of the Ordovician. Miller and Thompson (1937) showed that the elongation of the septal necks in Aturia was a secondary feature and the ellipochoanitic ancestry was indicated by the retention of connecting rings. It was believed that the Holochaonites proper contain cephalopods in which the long necks were primitive, and no connecting rings were developed. Unfortunately Hyatt does not seem to have committed himself on his ideas concerning the relationship of the Holochoanites with other cephalopods. It is not clear whether this was because of his preoccupation with the phyletic sig- nificance of early stages and the controversy that developed about the origin of the Ammonoidea and their relationship to the Nautiloidea, or whether he was as much perplexed by the problem as have been those of us who have come after him in the study of cephalopods. -
Checklist of Amphibians, Reptiles, Birds and Mammals of New York
CHECKLIST OF AMPHIBIANS, REPTILES, BIRDS AND MAMMALS OF NEW YORK STATE Including Their Legal Status Eastern Milk Snake Moose Blue-spotted Salamander Common Loon New York State Artwork by Jean Gawalt Department of Environmental Conservation Division of Fish and Wildlife Page 1 of 30 February 2019 New York State Department of Environmental Conservation Division of Fish and Wildlife Wildlife Diversity Group 625 Broadway Albany, New York 12233-4754 This web version is based upon an original hard copy version of Checklist of the Amphibians, Reptiles, Birds and Mammals of New York, Including Their Protective Status which was first published in 1985 and revised and reprinted in 1987. This version has had substantial revision in content and form. First printing - 1985 Second printing (rev.) - 1987 Third revision - 2001 Fourth revision - 2003 Fifth revision - 2005 Sixth revision - December 2005 Seventh revision - November 2006 Eighth revision - September 2007 Ninth revision - April 2010 Tenth revision – February 2019 Page 2 of 30 Introduction The following list of amphibians (34 species), reptiles (38), birds (474) and mammals (93) indicates those vertebrate species believed to be part of the fauna of New York and the present legal status of these species in New York State. Common and scientific nomenclature is as according to: Crother (2008) for amphibians and reptiles; the American Ornithologists' Union (1983 and 2009) for birds; and Wilson and Reeder (2005) for mammals. Expected occurrence in New York State is based on: Conant and Collins (1991) for amphibians and reptiles; Levine (1998) and the New York State Ornithological Association (2009) for birds; and New York State Museum records for terrestrial mammals. -
Geology and Fossils Craigleith Area Ontario
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
Upper Peninsula
GEOLOGICAL SURVEY OF MICHIGAN. For this object I have zealously worked. How far I have succeeded in the effort the reader may judge; and I shall feel well satisfied if he finds the picture I give worth UPPER PENINSULA attentive study, without having it surrounded by a 1869-1873 borrowed glistening frame, composed of a collection of ACCOMPANIED BY AN items from almost every branch of human knowledge. ATLAS OF MAPS. Very respectfully yours, C. ROMINGER. VOL. I. PART III. PALÆOZOIC ROCKS. INTRODUCTION. BY DR. C. ROMINGER BY the Legislative Assembly of 1871, the continuation of a geological survey of the State of Michigan was determined upon, in such a manner as to divide the work PUBLISHED BY AUTHORITY OF THE LEGISLATURE OF into three districts, each of which was to be investigated MICHIGAN. independently by different parties. UNDER THE DIRECTION OF THE BOARD OF GEOLOGICAL SURVEY. The third district, intrusted to me, comprises the Lower Peninsula, and the eastern half of the Upper Peninsula, NEW YORK or that portion which Is not included in the iron and JULIUS BIEN copper regions. Its surface rock is exclusively 1873 composed of members of the palæozoic series; while In Entered according to Act of Congress, in the year 1873, by the other two, older crystalline and metamorphic rocks GOVERNOR J. J. BAGLEY, prevail. for the State of Michigan, in the Office of the Librarian of Congress, at Washington. On the Lower Peninsula only a partial reconnoissance TO THE HONORABLE BOARD OF GEOLOGICAL SURVEY OF tour has been made through Little Traverse Bay region.