Method for Coating Mineral Granules to Improve Bonding to Hydrocarbon-Based Substrate and Coloring of Same
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Microplastics in Beaches of the Baja California Peninsula
UNIVERSIDAD AUTÓNOMA DE BAJA CALIFORNIA Chemical Sciences and Engineering Department MICROPLASTICS IN BEACHES OF THE BAJA CALIFORNIA PENINSULA TERESITA DE JESUS PIÑON COLIN FERNANDO WAKIDA KUSUNOKI Sixth International Marine Debris Conference SAN DIEGO, CALIFORNIA, UNITED STATES 7 DE MARZO DEL 2018 OUTLINE OF THE PRESENTATION INTRODUCTION METHODOLOGY RESULTS CONCLUSIONS OBJECTIVE. The aim of this study was to investigate the occurrence and distribution of microplastics in sandy beaches located in the Baja California peninsula. STUDY AREA 1200 km long and around 3000 km of seashore METHODOLOGY SAMPLED BEACHES IN THE BAJA CALIFORNIA PENINSULA • . • 21 sampling sites. • 12 sites located in the Pacific ocean coast. • 9 sites located the Gulf of California coast. • 9 sites classified as urban beaches (U). • 12 sites classified as rural beaches (R). SAMPLING EXTRACTION METHOD BY DENSITY. RESULTS Bahía de los Angeles. MICROPLASTICS ABUNDANCE (R) rural. (U) urban. COMPARISON WITH OTHER PUBLISHED STUDIES Area CONCENTRATIÓN UNIT REFERENCE West coast USA 39-140 (85) Partícles kg-1 Whitmire et al. (2017) (National Parks) United Kigdom 86 Partícles kg-1 Thompson et al. (2004) Mediterranean Sea 76 – 1512 (291) Partícles kg-1 Lots et al. (2017) North Sea 88-164 (190) Particles Kg-1 Lots et al. (2017) Baja California Ocean Pacific 37-312 (179) Particles kg-1 This study Gulf of 16-230 (76) Particles kg-1 This study California MORPHOLOGY OF MICROPLASTICS FOUND 2% 3% 4% 91% Fibres Granules spheres films Fiber color percentages blue Purple black Red green 7% 2% 25% 7% 59% Examples of shapes and colors of the microplastics found PINK FILM CABO SAN LUCAS BEACH POSIBLE POLYAMIDE NYLON TYPE Polyamide nylon type reference (Browne et al., 2011). -
Natural Communities of Michigan: Classification and Description
Natural Communities of Michigan: Classification and Description Prepared by: Michael A. Kost, Dennis A. Albert, Joshua G. Cohen, Bradford S. Slaughter, Rebecca K. Schillo, Christopher R. Weber, and Kim A. Chapman Michigan Natural Features Inventory P.O. Box 13036 Lansing, MI 48901-3036 For: Michigan Department of Natural Resources Wildlife Division and Forest, Mineral and Fire Management Division September 30, 2007 Report Number 2007-21 Version 1.2 Last Updated: July 9, 2010 Suggested Citation: Kost, M.A., D.A. Albert, J.G. Cohen, B.S. Slaughter, R.K. Schillo, C.R. Weber, and K.A. Chapman. 2007. Natural Communities of Michigan: Classification and Description. Michigan Natural Features Inventory, Report Number 2007-21, Lansing, MI. 314 pp. Copyright 2007 Michigan State University Board of Trustees. Michigan State University Extension programs and materials are open to all without regard to race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, marital status or family status. Cover photos: Top left, Dry Sand Prairie at Indian Lake, Newaygo County (M. Kost); top right, Limestone Bedrock Lakeshore, Summer Island, Delta County (J. Cohen); lower left, Muskeg, Luce County (J. Cohen); and lower right, Mesic Northern Forest as a matrix natural community, Porcupine Mountains Wilderness State Park, Ontonagon County (M. Kost). Acknowledgements We thank the Michigan Department of Natural Resources Wildlife Division and Forest, Mineral, and Fire Management Division for funding this effort to classify and describe the natural communities of Michigan. This work relied heavily on data collected by many present and former Michigan Natural Features Inventory (MNFI) field scientists and collaborators, including members of the Michigan Natural Areas Council. -
Flood Basalts and Glacier Floods—Roadside Geology
u 0 by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor FLOOD BASALTS AND GLACIER FLOODS: Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 Kaleen Cottingham - Supervisor Division of Geology and Earth Resources WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher-Commissio11er of Public Lands Kaleeo Cottingham-Supervisor DMSION OF GEOLOGY AND EARTH RESOURCES Raymond Lasmanis-State Geologist J. Eric Schuster-Assistant State Geologist William S. Lingley, Jr.-Assistant State Geologist This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 3.24 Tax (WA residents only) ~ Total $ 3.50 Mail orders must be prepaid: please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. Front Cover: Palouse Falls (56 m high) in the canyon of the Palouse River. Printed oo recycled paper Printed io the United States of America Contents 1 General geology of southeastern Washington 1 Magnetic polarity 2 Geologic time 2 Columbia River Basalt Group 2 Tectonic features 5 Quaternary sedimentation 6 Road log 7 Further reading 7 Acknowledgments 8 Part 1 - Walla Walla to Palouse Falls (69.0 miles) 21 Part 2 - Palouse Falls to Lower Monumental Dam (27.0 miles) 26 Part 3 - Lower Monumental Dam to Ice Harbor Dam (38.7 miles) 33 Part 4 - Ice Harbor Dam to Wallula Gap (26.7 mi les) 38 Part 5 - Wallula Gap to Walla Walla (42.0 miles) 44 References cited ILLUSTRATIONS I Figure 1. -
Coastal and Marine Ecological Classification Standard (2012)
FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ...................................................... -
The Rate of Granule Ripple Movement on Earth and Mars
Icarus 203 (2009) 71–76 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus The rate of granule ripple movement on Earth and Mars James R. Zimbelman a,*, Rossman P. Irwin III a, Steven H. Williams b, Fred Bunch c, Andrew Valdez c, Scott Stevens d a Center for Earth and Planetary Studies, National Air and Space Museum MRC 315, Smithsonian Institution, Washington, DC 20013-7012, USA b Education Division, National Air and Space Museum MRC 305, Smithsonian Institution, Washington, DC 20013-7012, USA c Great Sand Dunes National Park and Preserve, 11500 Highway 150, Mosca, CO 81146-9798, USA d National Climatic Data Center, Federal Building, 151 Patton Ave., Asheville, NC 28801-5001, USA article info abstract Article history: The rate of movement for 3- and 10-cm-high granule ripples was documented in September of 2006 at Received 25 July 2008 Great Sand Dunes National Park and Preserve during a particularly strong wind event. Impact creep Revised 13 March 2009 induced by saltating sand caused 24 granules minÀ1 to cross each cm of crest length during wind that Accepted 13 March 2009 averaged 9msÀ1 (at a height well above 1 m), which is substantially larger than the threshold for sal- Available online 17 April 2009 tation of sand. Extension of this documented granule movement rate to Mars suggests that a 25-cm-high granule ripple should require from hundreds to thousands of Earth-years to move 1 cm under present Keywords: atmospheric conditions. Earth Published by Elsevier Inc. Geological processes Mars surface 1. Introduction ples. -
Marine Plankton Diatoms of the West Coast of North America
MARINE PLANKTON DIATOMS OF THE WEST COAST OF NORTH AMERICA BY EASTER E. CUPP UNIVERSITY OF CALIFORNIA PRESS BERKELEY AND LOS ANGELES 1943 BULLETIN OF THE SCRIPPS INSTITUTION OF OCEANOGRAPHY OF THE UNIVERSITY OF CALIFORNIA LA JOLLA, CALIFORNIA EDITORS: H. U. SVERDRUP, R. H. FLEMING, L. H. MILLER, C. E. ZoBELL Volume 5, No.1, pp. 1-238, plates 1-5, 168 text figures Submitted by editors December 26,1940 Issued March 13, 1943 Price, $2.50 UNIVERSITY OF CALIFORNIA PRESS BERKELEY, CALIFORNIA _____________ CAMBRIDGE UNIVERSITY PRESS LONDON, ENGLAND [CONTRIBUTION FROM THE SCRIPPS INSTITUTION OF OCEANOGRAPHY, NEW SERIES, No. 190] PRINTED IN THE UNITED STATES OF AMERICA Taxonomy and taxonomic names change over time. The names and taxonomic scheme used in this work have not been updated from the original date of publication. The published literature on marine diatoms should be consulted to ensure the use of current and correct taxonomic names of diatoms. CONTENTS PAGE Introduction 1 General Discussion 2 Characteristics of Diatoms and Their Relationship to Other Classes of Algae 2 Structure of Diatoms 3 Frustule 3 Protoplast 13 Biology of Diatoms 16 Reproduction 16 Colony Formation and the Secretion of Mucus 20 Movement of Diatoms 20 Adaptations for Flotation 22 Occurrence and Distribution of Diatoms in the Ocean 22 Associations of Diatoms with Other Organisms 24 Physiology of Diatoms 26 Nutrition 26 Environmental Factors Limiting Phytoplankton Production and Populations 27 Importance of Diatoms as a Source of food in the Sea 29 Collection and Preparation of Diatoms for Examination 29 Preparation for Examination 30 Methods of Illustration 33 Classification 33 Key 34 Centricae 39 Pennatae 172 Literature Cited 209 Plates 223 Index to Genera and Species 235 MARINE PLANKTON DIATOMS OF THE WEST COAST OF NORTH AMERICA BY EASTER E. -
Omnibus Essential Fish Habitat (Efh) Amendment 2 Draft Environmental Impact Statement
New England Fishery Management Council 50 WATER STREET | NEWBURYPORT, MASSACHUSETTS 01950 | PHONE 978 465 0492 | FAX 978 465 3116 E.F. “Terry” Stockwell III, Chairman | Thomas A. Nies, Executive Director OMNIBUS ESSENTIAL FISH HABITAT (EFH) AMENDMENT 2 DRAFT ENVIRONMENTAL IMPACT STATEMENT Appendix D: The Swept Area Seabed Impact (SASI) approach: a tool for analyzing the effects of fishing on Essential Fish Habitat Appendix D: The Swept Area Seabed Impact Approach This document was prepared by the following members of the NEFMC Habitat Plan Development team, with feedback from the NEFMC Habitat Oversight Committee, NEFMC Habitat Advisory Panel, and interested members of the public. Michelle Bachman, NEFMC staff Peter Auster, University of Connecticut Chad Demarest, NOAA/Northeast Fisheries Science Center Steve Eayrs, Gulf of Maine Research Institute Kathyrn Ford, Massachusetts Division of Marine Fisheries Jon Grabowski, Gulf of Maine Research Institute Brad Harris, University of Massachusetts School of Marine Science and Technology Tom Hoff, Mid-Atlantic Fishery Management Council Mark Lazzari, Maine Department of Marine Resources Vincent Malkoski, Massachusetts Division of Marine Fisheries Dave Packer, NOAA/ Northeast Fisheries Science Center David Stevenson, NOAA/Northeast Regional Office Page Valentine, U.S. Geological Survey January 2011 Page 2 of 257 Appendix D: The Swept Area Seabed Impact Approach Table of Contents 1.0 OVERVIEW OF THE SWEPT AREA SEABED IMPACT MODEL ........... 13 2.0 DEFINING HABITAT ...................................................................................... -
Redalyc.Sedimentology and Stratigraphy of the Upper Miocene
Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Ochoa Landín, Lucas; Ruiz, Joaquín; Calmus, Thierry; Pérez Segura, Efrén; Escandón, Francisco Sedimentology and Stratigraphy of the Upper Miocene El Boleo Formation, Santa Rosalía, Baja California, Mexico Revista Mexicana de Ciencias Geológicas, vol. 17, núm. 2, 2000, pp. 83-96 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57217201 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas, volumen 17, número 2, 83 2000, p. 83-96 Universidad Nacional Autónoma de México, Instituto de Geología, México, D.F SEDIMENTOLOGY AND STRATIGRAPHY OF THE UPPER MIOCENE EL BOLEO FORMATION, SANTA ROSALÍA, BAJA CALIFORNIA, MEXICO Lucas Ochoa-Landín,1 Joaquín Ruiz,2 Thierry Calmus,3 Efrén Pérez-Segura1, and Francisco Escandón4 ABSTRACT The transtensional Upper Miocene Santa Rosalía basin, located in the east-central part of the Baja California Peninsula, consists of almost 500 m of non-marine to marine sedimentary deposits, and interbedded tuffaceous beds. The Santa Rosalía basin is a NW-SE elongated fault-bounded depocenter that records the sedimentation from Upper Miocene to Pleistocene time. The sequence is divided in El Boleo, La Gloria, Infierno and Santa Rosalía Formations. The lower most stratigraphic unit is the El Boleo Formation, a 200 to 300 m thick section composed in its lower part by a 1 to 5 m thick basal limestone and gypsum bodies followed by 170 to 300 m of clastic coarsening upward fan-delta, marine and nonmarine deposits. -
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. -
Tamarack Area Facilities Task 3
TAMARACK AREA FACILITIES TASK 3 - PHASE 2 REPORT Historical Archive Research and Mapping From Hubbell Beach through Tamarack City C&H Historic Properties of Torch Lake Prepared for: MICHIGAN DEPARTMENT OF ENVIRONMENTAL QUALITY Reclamation and Redevelopment Division 55195 US Highway 41 Calumet, Michigan 49913 Prepared by: MICHIGAN TECHNOLOGICAL UNIVERSITY Carol MacLennan, Principal Investigator With John Baeten, Emma Schwaiger, Dan Schneider, Brendan Pelto Industrial Archaeology and Heritage Program Department of Social Sciences October 2014 Contract No. Y4110 1 TABLE OF CONTENTS Section 1: Introduction …………………………………………………………………………………….5 Section 2: Narratives and Timelines ……………….……………...………………………………11 Ahmeek Mill Facilities1 - Narrative & Timeline ...……………...………………………………….12 Tamarack Reclamation Plant2 – Narrative & Timeline ………….……………………………..23 Lake Chemical Co. – Narrative & Timeline …………………………………………………………..46 Building Narratives ………………………………………………………………………………………..…55 Ahmeek Stamp Mill ………………………………………………..……………………………….58 Ahmeek Pump House ...……………………………………………………………………………60 Ahmeek Power House ……………………………………………………………………………..62 Ahmeek Transformer House ……………………………………………………………………64 Ahmeek Boiler House …...…………………………………………………………………………65 Tamarack Regrinding Plant ……………………………………………………………………..67 Tamarack Electric Sub-Station ...………………………………………………………………69 Tamarack Classifying Plant ..……………………………………………………………………70 Tamarack Flotation Plant ………………………………………………………………………..72 Tamarack Leaching Plant ...……………………………………………………………………...74 Tamarack Stamp -
Florida Keys Species List
FKNMS Species List A B C D E F G H I J K L M N O P Q R S T 1 Marine and Terrestrial Species of the Florida Keys 2 Phylum Subphylum Class Subclass Order Suborder Infraorder Superfamily Family Scientific Name Common Name Notes 3 1 Porifera (Sponges) Demospongia Dictyoceratida Spongiidae Euryspongia rosea species from G.P. Schmahl, BNP survey 4 2 Fasciospongia cerebriformis species from G.P. Schmahl, BNP survey 5 3 Hippospongia gossypina Velvet sponge 6 4 Hippospongia lachne Sheepswool sponge 7 5 Oligoceras violacea Tortugas survey, Wheaton list 8 6 Spongia barbara Yellow sponge 9 7 Spongia graminea Glove sponge 10 8 Spongia obscura Grass sponge 11 9 Spongia sterea Wire sponge 12 10 Irciniidae Ircinia campana Vase sponge 13 11 Ircinia felix Stinker sponge 14 12 Ircinia cf. Ramosa species from G.P. Schmahl, BNP survey 15 13 Ircinia strobilina Black-ball sponge 16 14 Smenospongia aurea species from G.P. Schmahl, BNP survey, Tortugas survey, Wheaton list 17 15 Thorecta horridus recorded from Keys by Wiedenmayer 18 16 Dendroceratida Dysideidae Dysidea etheria species from G.P. Schmahl, BNP survey; Tortugas survey, Wheaton list 19 17 Dysidea fragilis species from G.P. Schmahl, BNP survey; Tortugas survey, Wheaton list 20 18 Dysidea janiae species from G.P. Schmahl, BNP survey; Tortugas survey, Wheaton list 21 19 Dysidea variabilis species from G.P. Schmahl, BNP survey 22 20 Verongida Druinellidae Pseudoceratina crassa Branching tube sponge 23 21 Aplysinidae Aplysina archeri species from G.P. Schmahl, BNP survey 24 22 Aplysina cauliformis Row pore rope sponge 25 23 Aplysina fistularis Yellow tube sponge 26 24 Aplysina lacunosa 27 25 Verongula rigida Pitted sponge 28 26 Darwinellidae Aplysilla sulfurea species from G.P. -
An Integrated Assessment of Torch Lake Area of Concern Noel R. Urban, Carol A. Maclennan, Judith A. Perlinger
An Integrated Assessment of Torch Lake Area of Concern Noel R. Urban, Carol A. MacLennan, Judith A. Perlinger Michigan Technological University Funding provided by Michigan Sea Grant This is Contribution No. 53 of the Great Lakes Research Center at Michigan Technological University Calumet & Hecla operations in Lake Linden ca 1940. In the foreground are the Calumet and Hecla stamp mills with the stacks of the power house. Photo courtesy of Michigan Tech Archives. Acknowledgments The authors thank Michigan Sea Grant for funding to enable this integrated assessment. Without the support, insights, historical knowledge and perspectives offered by Sharon Baker, MDEQ site coordinator for many years, this project would not have been possible. We also owe tremendous thanks to the two students, Ankita Mandelia and Emma Schwaiger-Zawisza, whose thesis research contributed major parts of this report. Other people who have contributed to our understanding of the site and its history are too numerous to mention individually, but include state and federal agency personnel, colleagues at MTU and the Keweenaw National Historic Park, TLPAC members, and community members. Administration and staff members at Sea Grant were very helpful in administering the grant, creating and maintaining a web site for the project (http://www.miseagrant.umich.edu/torchlake/), and facilitating compilation of the final report. The assessment was greatly improved thanks to the contributions of eight anonymous reviewers representing agency, scientist, and local citizen viewpoints.