Cores, Site 1071

Total Page:16

File Type:pdf, Size:1020Kb

Cores, Site 1071 Site 1071 Hole A Core 1H Cored 0.0-5.1 mbsf 1071A-1H cobble pebble granule sand silt v f mc v clay DESCRIPTION STRUCTURE CORE AND SECTION METERS SAMPLE ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION SILTY SAND DCP Olive gray to dark olive gray (5Y 4/2 to 5Y 3/2), medium to fine 1 SILTY SAND containing abundant silt to sand-sized quartz and DCP mica and sand to granule-sized shell and lithic fragments; large SILTY CLAY clast lies between 58 and 65 cm in Section 2. Shell hash with very coarse fragments occurs in Section 1 between 24 and 29 cm. 2 2 1 3 4 4 HS CC PAL SITE 1071 195 SITE 1071 196 Site 1071 Hole A Core 2H Cored 5.1-7.9 mbsf 1071A-2H 1071A-3H cobble pebble granule sand silt v f mc v clay DESCRIPTION STRUCTURE CORE AND SECTION SAMPLE ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION METERS CLAYEY SILT and SANDY CLAY Very dark gray to dark gray (10YR 4/1 to 5YR 4/1) CLAYEY SILT 1 composed of quartz, mica, and lithic fragments, and SANDY SILT in Section 1 between 0 and 62 cm. SANDY SILT and CLAYEY SILT 2 IW Medium to thickly interbeded very fine-grained SANDY SILT and HS dark brown (10YR 3/3) CLAYEY SILT between 62 cm in Section 1 2 2 and 127 cm in Section 2; localized hydrotroilite staining. DCP CC PAL Site 1071 Hole A Core 3H Cored 7.9-12.0 mbsf cobble pebble granule sand silt v f mc v clay DESCRIPTION STRUCTURE CORE AND SECTION SAMPLE ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION METERS SILTY CLAY and CLAYEY SILT Dark gray (5YR 4/1) SILTY CLAY, interbedded with dark gray 1 (10YR 4/1) very thinly bedded CLAYEY SILT. CLAYEY SILTS are DCP common from 63 cm to 150 cm in Section 1, less common from 18 to 95 cm in Section 2. SILTY CLAY is composed of quartz mica and lithic fragments. 2 3 2 DCP IW HS 3 4 CC PAL Site 1071 Hole A Core 4H Cored 12.0-16.2 mbsf 1071A-4H cobble pebble granule sand silt v f mc v clay DESCRIPTION STRUCTURE CORE AND SECTION SAMPLE ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION METERS SILTY CLAY, SILT, and SAND Dark gray (5YR 4/1) SILTY CLAY thinly to medium interbedded 1 and laminated with SILT and fine SAND. SILTY CLAY contains rare sand-filled burrows; SILT and fine SAND beds have irregular bottoms and tops and locally exhibit grading and/or disruption by bioturbation. 2 4 2 DCP IW 3 HS 4 CC PAL SITE 1071 197 SITE 1071 198 Site 1071 Hole A Core 5H Cored 16.2-25.7 mbsf 1071A-5H cobble pebble granule sand silt v f mc v clay DESCRIPTION STRUCTURE CORE AND SECTION SAMPLE ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION METERS CLAY and SAND Dark gray (10YR 4/1) CLAY thinly to medium interbedded with 1 dark gray (5Y 3/1) fine SAND between 0 and 113 cm in Section 1. DCP Most sand beds have sharp/erosional basal contacts and normal grading. Sand beds contain quartz and micas. SAND and CLAY Dark gray (5Y 3/1) fine SAND medium to thickly interbedded with dark gray (5Y 3/1) CLAY between 113 cm in Section 1 and 119 2 cm in Section 2. 2 SAND Dark gray (5Y 3/1) very fine quartz SAND from 119 cm in Section 2 to the bottom of the core with abundant mud clasts in Sections 4 to 7, possibly flow-in. SANDS are very well sorted, angular to subrounded, and contain some glauconite and muscovite. 3 4 Minor disturbed (?) clay bed at ~75 cm in Section 4. 5 4 6 5 8 6 7 CC PAL Site 1071 Hole A Core 6H Cored 25.7-26.8 mbsf 1071A-6H 1071A-7H 1071A-8X cobble pebble granule sand silt clay v f mcv STRUCTURE CORE AND SECTION SAMPLE DESCRIPTION ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION METERS SAND 1 Olive gray (5Y 3/2), fine-grained SAND occurs in Section 1 (0 to 6 29 cm). Sand is most likely disturbed. HS CLAY and SAND CC IW Dark brownish gray (10YR 3/1) CLAY, in Section 1 (29 to 74 cm), PAL is interbedded with thin bedded (0.5 to 4 cm thick), normally graded, fine grained SANDS. Sands have sharp bases and gradational tops. SAND, SILTY CLAY Dark brownish gray (10YR 3/1), fine- to coarse-grained SAND occurs in Section CC. At Interval 0 to 10 cm sand is fine- to medium-grained; at Intervals 10 to 17 cm and 20 to 22 cm sand is medium- to coarse-grained. Sand contains granule-sized lithic clasts. Mica is scattered through Section CC. An interval of SILTY CLAY occurs at 17 to 20 cm. Site 1071 Hole A Core 7H Cored 26.8-36.3 mbsf cobble pebble granule sand silt v f mc v clay DESCRIPTION STRUCTURE SAMPLE CORE AND SECTION ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION METERS CLAY 7 1 Olive gray (5Y 2.5/1) CLAY in Section 1 contains shell fragments PAL up to 2 cm long. Clay is very disturbed due to extrusion. Site 1071 Hole A Core 8X Cored 36.3-39.9 mbsf cobble pebble granule sand silt v f mcv clay DESCRIPTION STRUCTURE SAMPLE CORE AND SECTION ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION METERS 8 CC PAL SAND Medium grayish brown (10YR 4/1) to olive greenish gray (5Y 3/1), very disturbed, fine-grained SAND with shell fragments and lithic granules. SITE 1071 199 SITE 1071 200 1071A-9X NO RECOVERY 1071A-10X 1071B-2X 1071B-3X Site 1071 Hole A Core 10X Cored 49.3-51.9 mbsf cobble pebble granule sand silt v f mcv clay DESCRIPTION STRUCTURE CORE AND SECTION SAMPLE ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION METERS SS SILTY CLAY 1 SS 10 Dark gray (7.5YR 4/1) SILTY CLAY with scattered quartzose HS pebbles and granules and shells fragments (bivalves); very rare CC IW mica-rich (muscovite), fine sand- and silt-filled burrows (1.5 cm in IW diameter) at 24 cm in Section 1. PAL 1071B-1W WASH CORE; undescribed Site 1071 Hole B Core 2X Cored 39.8-49.2 mbsf cobble pebble granule sand silt v f mcv clay DESCRIPTION STRUCTURE CORE AND SECTION METERS SAMPLE ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION DCP CLAY and SAND Dark gray (10YR 4/1) homogeneous CLAY (0-11 cm, Section 1) DCP 1 and fine SAND (9-11 cm, Section 1). SAND contains well-rounded DCP quartz pebbles (up to 2 cm in diameter) and shell fragments; 2 discrete burrows are filled with very fine quartz SAND. These DCP sediments may have been washed in from above. IW Dark greenish gray (5GY 4/1) CLAY (11-47 cm, Section 1), containing discrete burrows filled with fine mica-bearing quartz 2 HS DCP SAND, shell hash, and pebbles. Gradational lower contact with 2 PAL dark greenish gray (5GY 4/1) fine angular quartz SAND (47-72 CC cm, Section 1) with minor glauconite, pyrite, and sharp-based thin interbeds of CLAY. Reddish gray (10R 5/1) CLAY (72-140 cm, Section 1) with minor glauconite and pyrite (at 72-84 cm and107-113 cm, Section 1) and medium dark gray (N4/4) CLAY and fine SAND (83-84 cm, Section 1); contains discrete burrows filled with fine quartz SAND. All sharp contacts are burrowed. Site 1071 Hole B Core 3X Cored 49.2-52.9 mbsf cobble pebble granule sand silt v f mc v clay DESCRIPTION STRUCTURE CORE AND SECTION METERS SAMPLE ACCESSORIES DISTURBANCE ICHNOFOSSILS BIOTURBATION 1 HS CLAY and SILT 3 CC IW Brownish gray (5YR 4/1) CLAY (0-24 cm, Section 1); contains rare PAL burrows filled with quartz SILT; lower contact is sharp and pinched, suggesting possible biscuiting. Alternating laminae of brownish gray (5YR 4/1) and weak red (10R 5/2) fissile CLAY (24-38 cm, Section 1) contains a few quartz SILT laminae and rare burrows filled with SILT. Gas void occurs between 38 and 44 cm (Section 1). Site 1071 Hole B Core 4X Cored 52.9-58.4 mbsf 1071B-4X 1071B-5X cobble pebble granule sand silt clay v f mcv ACCESSORIES ICHNOFOSSILS DESCRIPTION STRUCTURE BIOTURBATION CORE AND SECTION METERS SAMPLE DISTURBANCE HS SILTY CLAY and CLAY 1 4 SS Very dark gray (5YR 3/1) fissile SILTY CLAY (0-47 cm, Section 1) CC DCP PAL contains scattered muscovite; very dark gray (5YR 3/1) homogenous CLAY (47-52.5 cm, Section 1) with bioturbated lower contact; and weak red (10R 4/2) homogeneous CLAY (52.5-56 cm, Section 1). Site 1071 Hole B Core 5X Cored 58.4-67.8 mbsf cobble pebble granule sand silt clay v f mcv CORE AND SECTION SAMPLE DESCRIPTION ACCESSORIES ICHNOFOSSILS STRUCTURE BIOTURBATION METERS DISTURBANCE SILTY CLAY Dark gray (5YR 4/1) micaceous SILTY CLAY (Section 1 and 0-17 1 cm, Section 2); contains rare burrows filled with fine SAND. SILTY CLAY and SAND DCP 2 Brownish gray (5YR 4/1) medium bedded SILTY CLAY 2 interbedded with brownish gray (5YR 5/1) fine to medium SAND with glauconite and mica (17-140 cm, Section 2). IW SILTY CLAY and SAND SS Medium gray (10YR 5/1) SAND (0-2 cm, Section 3) with 5 glauconite and biotite; sharp lower contact. Dusky yellow green 3 (5GY 5/2) homogeneous SILTY CLAY (from 2 cm, Section 3 4 through 62 cm, Section 5) with scattered small lithic pebbles and granules; granule-sized bone fragment (50 cm, Section 5).
Recommended publications
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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 ......................................................
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Method for Coating Mineral Granules to Improve Bonding to Hydrocarbon-Based Substrate and Coloring of Same
    Michigan Technological University Digital Commons @ Michigan Tech Michigan Tech Patents Vice President for Research Office 10-29-2013 Method for coating mineral granules to improve bonding to hydrocarbon-based substrate and coloring of same Bowen Li [email protected] Ralph Hodek [email protected] Domenic Popko Jiann-Yang Hwang [email protected] Follow this and additional works at: https://digitalcommons.mtu.edu/patents Part of the Mining Engineering Commons Recommended Citation Li, Bowen; Hodek, Ralph; Popko, Domenic; and Hwang, Jiann-Yang, "Method for coating mineral granules to improve bonding to hydrocarbon-based substrate and coloring of same" (2013). Michigan Tech Patents. 125. https://digitalcommons.mtu.edu/patents/125 Follow this and additional works at: https://digitalcommons.mtu.edu/patents Part of the Mining Engineering Commons US008568524B2 (12) United States Patent (io) Patent No.: US 8,568,524 B2 Li et al. (45) Date of Patent: Oct. 29,2013 (54) METHOD FOR COATING MINERAL 106/472, 474, 475, 481, 482, 483, 486, 490, GRANULES TO IMPROVE BONDING TO 106/502, 284.04; 427/186; 588/256 HYDROCARBON-BASED SUBSTRATE AND See application file for complete search history. COLORING OF SAME (56) References Cited (75) Inventors: Bowen Li, Chassell, MI (US); Ralph Hodek, Chassell, MI (US); Domenic U.S. PATENT DOCUMENTS Popko, Lake Linden, MI (US); 2,118,898 A * 5/1938 Price ............. 428/145 Jiann-Yang Hwang, Chassell, MI (US) 3,397,073 A * 8/1968 Fehner .......... 428/405 4,378,403 A 3/1983 Kotcharian (73) Assignee: Michigan Technology University, 5,240,760 A 8/1993 George et al. Houghton, MI (US) 5,380,552 A 1/1995 George et al.
    [Show full text]
  • 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 ......................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Particle-Size Analysis
    Particle-Size Analysis Geologic Lab Methods – Dr. C.E. Heinzel University of Northern Iowa Dept. of Earth and Environmental Science Learning objectives 2 • Review sedimentary particle textures • Know Udden-Wentworth grain size scale and Phi (f) scale, and the relationships between the two • Know how to plot grain size data: histograms; frequency curves; cumulative frequency curves • Know how to obtain grain size data • Understand grain size descriptive statistics • Mode • Median • Graphic estimation of mean • Phi standard deviation (graphic estimation of sorting) • Graphic skewness Sedimentary textures 3 Textural properties of siliciclastic sediments and rocks include: 1. Grain size 2. Sorting 3. Grain shape 1. Rounding 2. Sphericity 4. Particle surface textures 5. Grain fabric Grain size scales 4 Udden-Wentworth scale • Geometric scale in which each step is twice as large as the previous one • Range is from 1/256 mm to >256 mm • Four major size classes are • Gravel (> 2.00 mm) • Sand (1/16 mm to 2.00 mm) • Silt (1/256 mm to 1/16 mm) • Clay (< 1/256 mm) } mud Grain size scales (continued) 5 • Phi scale (Krumbein) • Logarithmic scale useful for plotting and statistical calculations = -log2d (where d = grain diameter, in mm) Note that 1.00 mm = 0f increases with smaller grain size, decreases with larger grain size Handout Wentworth grain size chart from United States Geological Survey Open-File Report 2006-1195 Measuring grain size 7 • Technique for measuring grain size depends on: • Purpose of study • Size range of material being measured
    [Show full text]
  • Late Cretaceous and Paleocene Decapod Crustaceans from James Ross Basin, Antarctic Peninsula Author(S): Rodney M
    Paleontological Society Late Cretaceous and Paleocene Decapod Crustaceans from James Ross Basin, Antarctic Peninsula Author(s): Rodney M. Feldmann, Dale M. Tshudy, Michael R. A. Thomson Source: Memoir (The Paleontological Society), Vol. 28, Supplement to Vol. 67, no. 1 of the Journal of Paleontology (Jan., 1993), pp. 1-41 Published by: Paleontological Society Stable URL: http://www.jstor.org/stable/1315582 Accessed: 16/01/2009 20:00 Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/page/info/about/policies/terms.jsp. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/action/showPublisher?publisherCode=paleo. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. JSTOR is a not-for-profit organization founded in 1995 to build trusted digital archives for scholarship. We work with the scholarly community to preserve their work and the materials they rely upon, and to build a common research platform that promotes the discovery and use of these resources. For more information about JSTOR, please contact [email protected]. Paleontological Society is collaborating with JSTOR to digitize, preserve and extend access to Memoir (The Paleontological Society).
    [Show full text]