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The Easternmost Occurrence of Mammut Pacificus (Proboscidea: Mammutidae), Based on a Partial Skull from Eastern Montana, USA
The easternmost occurrence of Mammut pacificus (Proboscidea: Mammutidae), based on a partial skull from eastern Montana, USA Andrew T. McDonald1, Amy L. Atwater2, Alton C. Dooley Jr1 and Charlotte J.H. Hohman2,3 1 Western Science Center, Hemet, CA, United States of America 2 Museum of the Rockies, Montana State University, Bozeman, MT, United States of America 3 Department of Earth Sciences, Montana State University, Bozeman, MT, United States of America ABSTRACT Mammut pacificus is a recently described species of mastodon from the Pleistocene of California and Idaho. We report the easternmost occurrence of this taxon based upon the palate with right and left M3 of an adult male from the Irvingtonian of eastern Montana. The undamaged right M3 exhibits the extreme narrowness that characterizes M. pacificus rather than M. americanum. The Montana specimen dates to an interglacial interval between pre-Illinoian and Illinoian glaciation, perhaps indicating that M. pacificus was extirpated in the region due to habitat shifts associated with glacial encroachment. Subjects Biogeography, Evolutionary Studies, Paleontology, Zoology Keywords Mammut pacificus, Mammutidae, Montana, Irvingtonian, Pleistocene INTRODUCTION Submitted 7 May 2020 The recent recognition of the Pacific mastodon (Mammut pacificus (Dooley Jr et al., 2019)) Accepted 3 September 2020 as a new species distinct from and contemporaneous with the American mastodon Published 16 November 2020 (M. americanum) revealed an unrealized complexity in North American mammutid Corresponding author evolution during the Pleistocene. Dooley Jr et al. (2019) distinguished M. pacificus from Andrew T. McDonald, [email protected] M. americanum by a suite of dental and skeletal features: (1) upper third molars (M3) Academic editor and lower third molars (m3) much narrower relative to length in M. -
Inventory and Analysis of Archaeological Site Occurrence on the Atlantic Outer Continental Shelf
OCS Study BOEM 2012-008 Inventory and Analysis of Archaeological Site Occurrence on the Atlantic Outer Continental Shelf U.S. Department of the Interior Bureau of Ocean Energy Management Gulf of Mexico OCS Region OCS Study BOEM 2012-008 Inventory and Analysis of Archaeological Site Occurrence on the Atlantic Outer Continental Shelf Author TRC Environmental Corporation Prepared under BOEM Contract M08PD00024 by TRC Environmental Corporation 4155 Shackleford Road Suite 225 Norcross, Georgia 30093 Published by U.S. Department of the Interior Bureau of Ocean Energy Management New Orleans Gulf of Mexico OCS Region May 2012 DISCLAIMER This report was prepared under contract between the Bureau of Ocean Energy Management (BOEM) and TRC Environmental Corporation. This report has been technically reviewed by BOEM, and it has been approved for publication. Approval does not signify that the contents necessarily reflect the views and policies of BOEM, nor does mention of trade names or commercial products constitute endoresements or recommendation for use. It is, however, exempt from review and compliance with BOEM editorial standards. REPORT AVAILABILITY This report is available only in compact disc format from the Bureau of Ocean Energy Management, Gulf of Mexico OCS Region, at a charge of $15.00, by referencing OCS Study BOEM 2012-008. The report may be downloaded from the BOEM website through the Environmental Studies Program Information System (ESPIS). You will be able to obtain this report also from the National Technical Information Service in the near future. Here are the addresses. You may also inspect copies at selected Federal Depository Libraries. U.S. Department of the Interior U.S. -
Geochemistry, Geophysics, Geosystems Becoming an Open Access Journal: FAQ
Geochemistry, Geophysics, Geosystems becoming an open access journal: FAQ Why is Geochemistry, Geophysics, Geosystems becoming an open access journal? AGU remains committed to open science and open data. As a part of our mission, we are focused on making science available to the widest possible audience. Since many researchers around the world have open access requirements by funders, this move to an open access model will make compliance easier. Authors will pay an open access article processing charge (APC) and retain copyright of their article which they can publish under a Creative Commons license (choose from CC-BY or CC-BY-NC-ND). There will be no excess page fees or any other additional fees for publication. In addition, there will be no subscription paywall, which means that more people will have access to your research so they can actively cite, read and share data for free. When will Geochemistry, Geophysics, Geosystems become open access? All articles in the journal will be open access as of 1 January 2022. After 8 September 2021, submissions received/accepted must agree to pay the open access article processing charge (APC), but there will be no excess page fees or any other additional fees for publication. What if I already have a paper under consideration to Geochemistry, Geophysics, Geosystems? If your paper: • is under consideration before 8 September 2021 and • publishes after 1 January 2021, then your paper will publish with copyright to the authors under a Creative Commons license for free (the fee will be waived). If your paper publishes in 2021, then the paper will publish as a subscription article (copyright AGU). -
Developing Protocols for Reconstructing Submerged Paleocultural Landscapes and Identifying Ancient Native American Archaeological Sites in Submerged Environments
OCS Study BOEM 2020-024 Developing Protocols for Reconstructing Submerged Paleocultural Landscapes and Identifying Ancient Native American Archaeological Sites in Submerged Environments: Geoarchaeological Modeling US Department of the Interior Bureau of Ocean Energy Management Office of Renewable Energy Programs OCS Study BOEM 2020-024 Developing Protocols for Reconstructing Submerged Paleocultural Landscapes and Identifying Ancient Native American Archaeological Sites in Submerged Environments: Geoarchaeological Modeling March 2020 Authors: David S. Robinson, Carol L. Gibson, Brian J. Caccioppoli, and John W. King Prepared under BOEM Award M12AC00016 by The Coastal Mapping Laboratory Graduate School of Oceanography, University of Rhode Island 215 South Ferry Road Narragansett, RI 02882 US Department of the Interior Bureau of Ocean Energy Management Office of Renewable Energy Programs DISCLAIMER Study collaboration and funding were provided by the US Department of the Interior, Bureau of Ocean Energy Management, Environmental Studies Program, Washington, DC, under Agreement Number M12AC00016 between BOEM and the University of Rhode Island. This report has been technically reviewed by BOEM and it has been approved for publication. The views and conclusions contained in this document are those of the authors and should not be interpreted as representing the opinions or policies of the US Government, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. REPORT AVAILABILITY To download a PDF file of this report, go to the US Department of the Interior, Bureau of Ocean Energy Management Data and Information Systems webpage (http://www.boem.gov/Environmental-Studies- EnvData/), click on the link for the Environmental Studies Program Information System (ESPIS), and search on 2020-024. -
Distribution and Sedimentary Characteristics of Tsunami Deposits
Sedimentary Geology 200 (2007) 372–386 www.elsevier.com/locate/sedgeo Distribution and sedimentary characteristics of tsunami deposits along the Cascadia margin of western North America ⁎ Robert Peters a, , Bruce Jaffe a, Guy Gelfenbaum b a USGS Pacific Science Center, 400 Natural Bridges Drive, Santa Cruz, CA 95060, United States b USGS 345 Middlefield Road, Menlo Park, CA 94025, United States Abstract Tsunami deposits have been found at more than 60 sites along the Cascadia margin of Western North America, and here we review and synthesize their distribution and sedimentary characteristics based on the published record. Cascadia tsunami deposits are best preserved, and most easily identified, in low-energy coastal environments such as tidal marshes, back-barrier marshes and coastal lakes where they occur as anomalous layers of sand within peat and mud. They extend up to a kilometer inland in open coastal settings and several kilometers up river valleys. They are distinguished from other sediments by a combination of sedimentary character and stratigraphic context. Recurrence intervals range from 300–1000 years with an average of 500–600 years. The tsunami deposits have been used to help evaluate and mitigate tsunami hazards in Cascadia. They show that the Cascadia subduction zone is prone to great earthquakes that generate large tsunamis. The inclusion of tsunami deposits on inundation maps, used in conjunction with results from inundation models, allows a more accurate assessment of areas subject to tsunami inundation. The application of sediment transport models can help estimate tsunami flow velocity and wave height, parameters which are necessary to help establish evacuation routes and plan development in tsunami prone areas. -
The Geologic Implications of the Factors That Affected Relative Sea
University of South Carolina Scholar Commons Theses and Dissertations 12-15-2014 The Geologic Implications of the Factors that Affected Relative Sea-level Positions in South Carolina During the Pleistocene and the Associated Preserved High-stand Deposits William Richardson Doar III University of South Carolina - Columbia Follow this and additional works at: https://scholarcommons.sc.edu/etd Part of the Geology Commons Recommended Citation Doar, W. R.(2014). The Geologic Implications of the Factors that Affected Relative Sea-level Positions in South Carolina During the Pleistocene and the Associated Preserved High-stand Deposits. (Doctoral dissertation). Retrieved from https://scholarcommons.sc.edu/ etd/2969 This Open Access Dissertation is brought to you by Scholar Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. The Geologic Implications of the Factors that Affected Relative Sea-level Positions in South Carolina During the Pleistocene and the Associated Preserved High-stand Deposits by William Richardson Doar, III Bachelor of Science East Carolina University, 1993 Master of Science East Carolina University, 1998 Submitted in Partial Fulfillment of the Requirements For the Degree of Doctor of Philosophy in Geological Sciences College of Arts and Sciences University of South Carolina 2014 Accepted by: George Voulgaris, Major Professor Christopher G. St. C. Kendall, Major Professor David L. Barbeau, Jr., Committee Member Robert E. Weems, Committee Member Lacy Ford, Vice Provost and Dean of Graduate Studies ©Copyright by William Richardson Doar, III, 2014 All rights reserved ii DEDICATION This project is dedicated to my family and friends who supported this endeavor and to Emily Ann Louder, my daughter, who at this time has no understanding of why her father is still in school, but is so excited that I am. -
Latex Submission Guidelines
Latex submission guidelines The current version of the zip archive containing all components is marked April 30, 2019 The current version of the main CLS file is April 16, 2019 You are not required to use the newest template, but it is strongly recommended. Zip Contents: April‐30‐2019‐latex‐templates.zip contains these files: agujournaltemplate.tex o This is a “sample” manuscript. It contains commented out instructions and pre‐defined sections to add your work. agujournal2019.cls o This is the primary class file. It corresponds to agujournaltemplate.tex si_template_2019.tex o A “sample” supporting information readme. Like agujournaltemplate.tex, it contains a framework to fill with information about your supplemental files. agutexSI2019.cls o The class file for the supporting information readme file, si_template_2019.tex trackchanges.sty o a third‐party package that facilitates manuscript annotation, usually for tracking changes. Set package options to “inline” to show annotations, “finalnew” to compile an unmarked paper. Complete documentation is here. a directory, trackchanges‐0.7.0 o contains python scripts for automated removal of change tracking commands, if needed o also includes documentation and authorship info for the package above 1 Using agujournaltemplate.tex 1. enter the journal’s name in plain text \journalname{here} 2. enter your paper’s title \title{here} 3. List all authors \authors{here} List authors by first name or initial followed by last name and separated by commas. Use \affil{} to number affiliations, and \thanks{} for author notes. Additional author notes should be indicated with \thanks{} (current addresses, for example). Example: \authors{A. B. -
AGU Electronics Editions Package, AGU
SCHEDULE 3 Addition(s), Deletion(s) to Agreement, Licensed Materials, Subscription Period and Access Method A schedule dated 11'/11./UlfJ to the License dated 1/;-t./u;ot{ between American Geophysical Union and The California Digital Library. ADDITION(s) DELETION(s) TO THE LICENSED MATERIALS AND SUBSCRIPTION PERIOD AND ACCESS METHOD: Addition(s), Deletion(s) made by the Licensee must be approved by Publisher, agreed to, and signed by both parties. Titles(s) Period • • •• Fee AGU Electronics Editions Package* Jan 1 - Dec 31, 2011 AGU Digital Library Jan 1 - Dec 31, 2011 Purchase starting Jan 1, 2011 *Includes the journals titled: Journal of Geophysical Research - All sections Journal of Geophysical Research - Space Physics Section Journal of Geophysical Research - Solid Earth Section Journal of Geophysical Research - Oceans Section Journal of Geophysical Research - Atmospheres Section Journal of Geophysical Research - Planets Section Journal of Geophysical Research - Earth Surface Section Journal of Geophysical Research - Biogeosciences Section Water Resources Research Reviews of Geophysics Geophysical Research Letters Radio Science Tectonics Paleoceanography Global Biogeochemical Cycles Geochemistry Geophysics Geosystems Space Weather Earth Interactions (copublished with AMS and AAG) Chinese Journal of Geophysics (distributed by AGU) Nonlinear Processes in Geophysics (copublished with EGU) **Each year thereafter, a ccess fee would be charged to the Licensee. SUBSCRIBING LOCATION IP ADDRESSES UC Berkeley [Including Lawrence Berkeley Lab] -
UNIVERSITY of CALIFORNIA, SAN DIEGO Stress in the Lithosphere
UNIVERSITY OF CALIFORNIA, SAN DIEGO Stress in the Lithosphere from Non-Tectonic Loads with Implications for Plate Boundary Processes A dissertation submitted in partial satisfaction of the requirements for the degree Doctor of Philosophy in Earth Sciences by Karen Marie Luttrell Committee in charge: David Sandwell, Chair Bruce Bills Donna Blackman Steve Cande Yuri Fialko Xanthippi Markenscoff 2010 © 2010 Karen Marie Luttrell All rights reserved The Dissertation of Karen Marie Luttrell is approved, and it is acceptable in quality and form for publication on microfilm and electronically: Chair University of California, San Diego 2010 iii DEDICATION To Chad and Oliver, with all my love iv EPIGRAPH Before the hills in order stood or earth received her frame from everlasting, thou art God to endless years the same Isaac Watts, 1719 v TABLE OF CONTENTS Signature Page iii Dedication iv Epigraph v Table of Contents vi List of Figures ix List of Tables xi Acknowledgements xii Vita xv Abstract of the Dissertation xvii Chapter 1 Introduction 1 1.1 Preface 1 1.2 Plate tectonics 2 1.3 Non-Tectonic sources of stress 4 1.3.1 Time varying surface loads 4 1.3.2 Topography loads 7 1.4 Conclusions 11 1.4.1 Summary of results 11 1.4.2 Future research 12 Chapter 2 Ocean loading effects on stress at near shore plate boundary fault 15 systems 2.1 Introduction 16 2.2 Methods 21 2.2.1 Plate bending stress from ocean loading 21 2.2.2 Ocean loading stress on plate boundary faults 27 2.3 Results 30 2.3.1 Eustatic ocean loading at the San Andreas system 30 2.3.2 -
Geology of Florida Local Abundance of Quartz Sand
28390_00_cover.qxd 1/16/09 4:03 PM Page 1 Summary of Content The geologic past of Florida is mostly out of sight with its maximum elevation at only ~105 m (in the panhandle) and much of south Florida is virtually flat. The surface of Florida is dominated by subtle shorelines from previous sea-level high-stands, karst-generated lakes, and small river drainage basins What we see are modern geologic (and biologic) environments, some that are world famous such as the Everglades, the coral reefs, and the beaches. But, where did all of this come from? Does Florida have a geologic history other than the usual mantra about having been “derived from the sea”? If so, what events of the geologic past converged to produce the Florida we see today? Toanswer these questions, this module has two objectives: (1) to provide a rapid transit through geologic time to describe the key events of Florida’s past emphasizing processes, and (2) to present the high-profile modern geologic features in Florida that have made the State a world-class destination for visitors. About the Author Albert C. Hine is the Associate Dean and Professor in the College of Marine Science at the University of South Florida. He earned his A.B. from Dartmouth College; M.S. from the University of Massachusetts, Amherst; and Ph.D. from the University of South Carolina, Columbia—all in the geological sciences. Dr. Hine is a broadly-trained geological oceanographer who has addressed sedimentary geology and stratigraphy problems from the estuarine system out to the base of slope. -
1999 EOS Reference Handbook
1999 EOS Reference Handbook A Guide to NASA’s Earth Science Enterprise and the Earth Observing System http://eos.nasa.gov/ 1999 EOS Reference Handbook A Guide to NASA’s Earth Science Enterprise and the Earth Observing System Editors Michael D. King Reynold Greenstone Acknowledgements Special thanks are extended to the EOS Prin- Design and Production cipal Investigators and Team Leaders for providing detailed information about their Sterling Spangler respective instruments, and to the Principal Investigators of the various Interdisciplinary Science Investigations for descriptions of their studies. In addition, members of the EOS Project at the Goddard Space Flight Center are recognized for their assistance in verifying and enhancing the technical con- tent of the document. Finally, appreciation is extended to the international partners for For Additional Copies: providing up-to-date specifications of the instruments and platforms that are key ele- EOS Project Science Office ments of the International Earth Observing Mission. Code 900 NASA/Goddard Space Flight Center Support for production of this document, Greenbelt, MD 20771 provided by Winnie Humberson, William Bandeen, Carl Gray, Hannelore Parrish and Phone: (301) 441-4259 Charlotte Griner, is gratefully acknowl- Internet: [email protected] edged. Table of Contents Preface 5 Earth Science Enterprise 7 The Earth Observing System 15 EOS Data and Information System (EOSDIS) 27 Data and Information Policy 37 Pathfinder Data Sets 45 Earth Science Information Partners and the Working Prototype-Federation 47 EOS Data Quality: Calibration and Validation 51 Education Programs 53 International Cooperation 57 Interagency Coordination 65 Mission Elements 71 EOS Instruments 89 EOS Interdisciplinary Science Investigations 157 Points-of-Contact 340 Acronyms and Abbreviations 354 Appendix 361 List of Figures 1. -
The Last Interglacial Sea-Level Record of Aotearoa New Zealand (Aotearoa)
The last interglacial sea-level record of Aotearoa New Zealand (Aotearoa) Deirdre D. Ryan1*, Alastair J.H. Clement2, Nathan R. Jankowski3,4, Paolo Stocchi5 1MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany 5 2School of Agriculture and Environment, Massey University, Palmerston North, New Zealand 3 Centre for Archeological Science, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, Australia 4Australian Research Council (ARC) Centre of Excellence for Australian Biodiversity and Heritage, University of Wollongong, Wollongong, Australia 10 5NIOZ, Royal Netherlands Institute for Sea Research, Coastal Systems Department, and Utrecht University, PO Box 59 1790 AB Den Burg (Texel), The Netherlands Correspondence to: Deirdre D. Ryan ([email protected]) Abstract: This paper presents the current state-of-knowledge of the Aotearoa New Zealand (Aotearoa) last interglacial (MIS 5 sensu lato) sea-level record compiled within the framework of the World Atlas of Last Interglacial Shorelines (WALIS) 15 database. Seventy-seven total relative sea-level (RSL) indicators (direct, marine-, and terrestrial-limiting points), commonly in association with marine terraces, were identified from over 120 studies reviewed. Extensive coastal deformation around New Zealand has prompted research focused on active tectonics, which requires less precision than sea-level reconstruction. The range of last interglacial paleo-shoreline elevations are resulted in a significant range of elevation measurements on both the North Island (276.8 ± 10.0 to -94.2 ± 10.6 m amsl) and South Island (173.1165.8 ± 2.0 to -70.0 ± 10.3 m amsl) and 20 prompted the use of RSL indicators tohave been used to estimate rates of vertical land movement; however, indicators in many instances lackk adequate description and age constraint for high-quality RSL indicators.