Description and Classification of the Forests of the Upper Illinois River Drainage of Southwestern Oregon
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New Constraints on the Age, Geochemistry
New constraints on the age, geochemistry, and environmental impact of High Arctic Large Igneous Province magmatism: Tracing the extension of the Alpha Ridge onto Ellesmere Island, Canada T.V. Naber1,2, S.E. Grasby1,2, J.P. Cuthbertson2, N. Rayner3, and C. Tegner4,† 1 Geological Survey of Canada–Calgary, Natural Resources Canada, Calgary, Canada 2 Department of Geoscience, University of Calgary, Calgary, Canada 3 Geological Survey of Canada–Northern, Natural Resources Canada, Ottawa, Canada 4 Centre of Earth System Petrology, Department of Geoscience, Aarhus University, Aarhus, Denmark ABSTRACT Island, Nunavut, Canada. In contrast, a new Province (HALIP), is one of the least studied U-Pb age for an alkaline syenite at Audhild of all LIPs due to its remote geographic lo- The High Arctic Large Igneous Province Bay is significantly younger at 79.5 ± 0.5 Ma, cation, and with many exposures underlying (HALIP) represents extensive Cretaceous and correlative to alkaline basalts and rhyo- perennial arctic sea ice. Nevertheless, HALIP magmatism throughout the circum-Arctic lites from other locations of northern Elles- eruptions have been commonly invoked as a borderlands and within the Arctic Ocean mere Island (Audhild Bay, Philips Inlet, and potential driver of major Cretaceous Ocean (e.g., the Alpha-Mendeleev Ridge). Recent Yelverton Bay West; 83–73 Ma). We propose anoxic events (OAEs). Refining the age, geo- aeromagnetic data shows anomalies that ex- these volcanic occurrences be referred to col- chemistry, and nature of these volcanic rocks tend from the Alpha Ridge onto the northern lectively as the Audhild Bay alkaline suite becomes critical then to elucidate how they coast of Ellesmere Island, Nunavut, Canada. -
Site Inspection Report Oriole Mine Colville National Forest
Site Inspection Report Oriole Mine Colville National Forest March 2005 Cascade Earth Sciences 12720 East Nora Avenue, Suite A Spokane, Washington 99216 (509) 921-0290 www.cascade-earth.com SITE INSPECTION REPORT Oriole Mine Colville National Forest Principal Authors and Investigators: Dustin G. Wasley, PE, Managing Engineer II Robert H. Lambeth, PE, PG, Senior Engineer Ryan Tobias, Staff Wildlife Biologist Reviewed By: John D. Martin, RG, Principal Geologist Prepared for: USDA Forest Service Colville National Forest Site Location: Oriole Mine Colville National Forest Pend Oreille County, Washington Prepared by: Cascade Earth Sciences P.O. Box 14725 Spokane, Washington 99214 (509) 921-0290 PN: 2323024/March 2005 Cover Photo: Collapsed Ore Bin (upper left) and Upper Adit (lower right) TABLE OF CONTENTS EXECUTIVE SUMMARY ....................................................................................................................... iii SITE INSPECTION DATA SUMMARY SHEET ................................................................................. iv 1.0 INTRODUCTION AND OBJECTIVES ......................................................................................1 2.0 SITE DESCRIPTION AND OPERATIONAL HISTORY.........................................................1 2.1 Description and Location ................................................................................................... 1 2.1.1 Operational History and Waste Characteristics..................................................... 2 2.1.2 Previous Investigations......................................................................................... -
A-Horizon, 447
A A-Horizon, 447, 452 Aabwas, 522 AAS, 565 Aatis, 523 Abas, 522 Abdomen, 532-533, 540 ABE, 570 Abiotic, 140-141, 170, 172, 176, 187, 189, 193-194 Abiotic Factor, 176 Abnormal Tides, 268 Abrin, 315 Abrus precatorius, 315 Absence of Disease, 575 Abyssal Plain, 49 Abyssal Zone, 204-205 Abyssopelagic, 204 Acacia auriculiformis, 383 Acacia formosa, 384 Acanthaster planci, 252, 261-262 Acanthurus lineatus, 247, 256 Access Routes, 614 Access to US Markets, 553 Accidental Spills, 576 Accumulation of Salts, 457 Accumulation Rate of Soil, 441 Acetone, 578 Acetylene, 663 Achiak, 334 Acid, 73, 78, 87, 164-165, 188-189, 383, 427, 440, 445, 498, 521, 525, 649, 675, 679 ACOE, 5 Acrocephalus luscinia, 374 Acropora, 223, 252 Acrostichum aureum, 363 Actitis, 304 Active Listening, 2 Acute Care, 571 ADA, 563, 565 Adaptation, 160, 180, 182, 184, 223, 250, 310 Addictive Nature, 530 Adding Value to a Product, 545 Administrative Procedure, 623 Adobe-Brick, 705 Adult Basic Education, 570 Adult Supervision, 725 Advanced Life Saving Skills, 567 Adverse Impacts, 598, 654-655 Advocacy, 1 Aerial Bombing, 35 Aerially-sprayed Herbicides, 586 Aerobic Bacteria, 453 Aerodramus vanikorensis, 385 Aerosol Propellants, 650 Aesthetic Design, 711 Africa, 63, 102, 166, 318, 330, 364, 490, 587 Aga, 338, 500 Agatelang, 322 Age of Dinosaurs, 69 Agencies Tasked with Implementing Environmental Laws, 644 Agenda 21, 660 Agfayan Soils, 381 Aggregate Market, 422 Aggregate Supply, 422 Aggrieved Party, 622 Aghurub, Chief, 26 Agingan Point, 418 Agricultural Clearing, 326 Agricultural Crops, -
A Fossil Climbing Perch from the Oligocene of Tibet Helps Solve The
Science Bulletin 64 (2019) 455–463 Contents lists available at ScienceDirect Science Bulletin journal homepage: www.elsevier.com/locate/scib Article Into Africa via docked India: a fossil climbing perch from the Oligocene of Tibet helps solve the anabantid biogeographical puzzle ⇑ ⇑ Feixiang Wu a,b, , Dekui He c, , Gengyu Fang d, Tao Deng a,b,d a Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China b Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Beijing 100101, China c Key Laboratory of Aquatic Biodiversity and Conservation, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China d College of Earth Sciences, University of Chinese Academy of Sciences, Beijing 100049, China article info abstract Article history: The northward drift of the Indian Plate and its collision with Eurasia have profoundly impacted the evo- Received 7 March 2019 lutionary history of the terrestrial organisms, especially the ones along the Indian Ocean rim. Climbing Received in revised form 22 March 2019 perches (Anabantidae) are primary freshwater fishes showing a disjunct south Asian-African distribution, Accepted 22 March 2019 but with an elusive paleobiogeographic history due to the lack of fossil evidence. Here, based on an Available online 28 March 2019 updated time-calibrated anabantiform phylogeny integrating a number of relevant fossils, the divergence between Asian and African climbing perches is estimated to have occurred in the middle Eocene (ca. Keywords: 40 Ma, Ma: million years ago), a time when India had already joined with Eurasia. The key fossil lineage Climbing perches is yEoanabas, the oldest anabantid known so far, from the upper Oligocene of the Tibetan Plateau. -
Ophiolites of Iran: Keys to Understanding the Tectonic Evolution of SW Asia: (II) Mesozoic Ophiolites ⇑ Hadi Shafaii Moghadam A, , Robert J
Journal of Asian Earth Sciences 100 (2015) 31–59 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Review Ophiolites of Iran: Keys to understanding the tectonic evolution of SW Asia: (II) Mesozoic ophiolites ⇑ Hadi Shafaii Moghadam a, , Robert J. Stern b a School of Earth Sciences, Damghan University, Damghan, Iran b Geosciences Dept., University of Texas at Dallas, Richardson, TX 75083-0688, USA article info abstract Article history: Iran is a mosaic of continental terranes of Cadomian (520–600 Ma) age, stitched together along sutures Received 29 May 2014 decorated by Paleozoic and Mesozoic ophiolites. Here we present the current understanding of the Meso- Received in revised form 8 December 2014 zoic (and rare Cenozoic) ophiolites of Iran for the international geoscientific audience. We summarize Accepted 16 December 2014 field, chemical and geochronological data from the literature and our own unpublished data. Mesozoic Available online 13 January 2015 ophiolites of Iran are mostly Cretaceous in age and are related to the Neotethys and associated backarc basins on the S flank of Eurasia. These ophiolites can be subdivided into five belts: 1. Late Cretaceous Keywords: Zagros outer belt ophiolites (ZOB) along the Main Zagros Thrust including Late Cretaceous–Early Paleo- Ophiolite cene Maku–Khoy–Salmas ophiolites in NW Iran as well as Kermanshah–Kurdistan, Neyriz and Esfanda- Neotethys Cimmeria gheh (Haji Abad) ophiolites, also Late Cretaceous–Eocene ophiolites along the Iraq–Iran border; 2. Late Supra-subduction zone Cretaceous Zagros inner belt ophiolites (ZIB) including Nain, Dehshir, Shahr-e-Babak and Balvard–Baft MORB ophiolites along the southern periphery of the Central Iranian block and bending north into it; 3. -
Petrography, Geochemistry and Provenance of Saudi Arabian Palaeozoic Sandstones
Petrography, geochemistry and provenance of Saudi Arabian Palaeozoic sandstones vom Fachbereich Material- und Geowissenschaften der Technische Universität Darmstadt zur Erlangung des Grades Doktor rerum naturalium (Dr. rer. nat.) genehmigte Dissertation von Diplom-Geologe Alexander Bassis aus Malsch Referenten: Prof. Dr. Matthias Hinderer Prof. Dr. Christoph Schüth Tag der Einreichung: 05.12.2016 Tag der mündlichen Prüfung: 18.04.2017 Darmstadt 2017 D17 Declaration of Authorship I hereby certify that the complete work to this PhD thesis 'Petrography, geochemistry and provenance of Saudi Arabian Palaeozoic sandstones.' was done by me and only with the use of the referenced literature and the described methods. …………………………….. ……………………………… Place, date Signature 'There is no real ending. It’s just the place where you stop the story.' Frank Herbert Index Abstract Zusammenfassung 1. Introduction ....................................................................................................................................... 1 1.1. Aims ............................................................................................................................................ 1 1.2. Concept....................................................................................................................................... 2 1.3. Study areas ................................................................................................................................. 3 2. Geological background .................................................................................................................... -
Lower Palaeozoic Sedimentology and Stratigraphy of the Kerman Region, East-Central Iran Mir Alireza Hamedi University of Wollongong
University of Wollongong Thesis Collections University of Wollongong Thesis Collection University of Wollongong Year Lower Palaeozoic sedimentology and stratigraphy of the Kerman region, East-Central Iran Mir Alireza Hamedi University of Wollongong Hamedi, Mir A, Lower Palaeozoic sedimentology and stratigraphy of the Kerman region, East-Central Iran, PhD thesis, Department of Geology, University of Wollongong, 1995. http://ro.uow.edu.au/theses/542 This paper is posted at Research Online. http://ro.uow.edu.au/theses/542 NORTHIRAN CENTR.- EAST IRAN ~ Padeha Formation c"oo ci 0 ...J ---------------- E~ :;)-0 ::.Go ::> Niur Formation ... ..... "...J ~ <, -= e C/.l- ------------------- en E C",....u c ~ :::::.G ~ Shirgesht Formation 0,- 0 ,......=;- ~'~'Member 5 '5 ~ E "E 0 " l:: :u u 0 C. ...J ..J..>o:tJ., ::J ~ .9 0 eu Member 4 .--- l- - ;.C ei. E 0 :u Member 3 Z ::J '""0 ~ Derenjal Formation E... t.L. u < - Member 2 ~ ~ !!! '- -c:: -ci 0 :::; Member I Kalshaneh Fm. .c",'c c "~ ~ ::Ic .;: ~'" '" ~ ~ ~ < "Top Quartzite" E U ~ - :u .3 Lalun Sandstone (Dahu Series) U --------------------------- ------- -- Zaigun Formation Z < Barut Formation .gc '"u eu - Colle nia Limestone .t: E c:: I I u ... "~ U) 0 t.L. < Soltanieh .~.~ .s '. ::J U Dolomite § E t.g '"u eu... ,::.9 U)~ ;> -e c eu ~ o 8 := 0 ~ Chapoghlu Shale U) N '" LI.. .- \0 Z I <; - IBayandor Formation Gharadash Form., Granites Doran G ranite III. IIII IIIII 11111 Z Kahar Fonn.,Tashk Form., < Kahar Form., Morad Series, ~ Taknar Form. -c:: Metamorphic rocks: Metamorphic rocks' ~ Shorm Beds, Barir Formation, U< Golpaygan Met., Anarak UJ Alamkuh Metamorphics, Schists, Boneh Shurou c.. Gorgan Schists, Complex, " etc, etc. -
The Diatoms: a Primer
P1: SJT Trim: 276mm × 219mm Top: 10mm Gutter: 21.089mm CUUK1067-02 cuuk1067/Smol ISBN: 978 0 521 50996 1 May 20, 2010 11:46 2 The diatoms: A primer MATTHEW L. JULIUS AND EDWARD C. THERIOT Texas Natural Science Center, The University of Texas at Austin, Austin, TX 78705, USA 2.1 Introduction than the specialized teeth found in mammals, including those Diatoms have long been lauded for their use as powerful in the reader’s mouth (Shubin, 2008). Dates for the origin and reliable environmental indicators (Cholnoky, 1968; Lowe, of the diatom common ancestor are bracketed by molecular 1974). This utility can be attributed to their high abundance clock estimates (Sorhannus, 2007) and the oldest stratigraphic and species diversity, which is distributed among most aquatic observation (Rothpletz, 1896, 1900). Both of these estimates environments. Additionally, their remains are highly durable are inherently biased. The temporal proximity of each esti- and well preserved in accumulated sediments. Often, scientists mate to one another does, however, suggest a certain degree of exploiting the group simply as environmental proxies give little accuracy, given the complimentary nature of the biases. Molec- thought as to how and why the species diversity exists in these ular estimates represent an attempt to identify the absolute environments. This may be a by-product of how diatoms are moment two populations diverged from one another. The old- collected and identified. Diatoms are most often recognized by est stratigraphic observation represents a period where fossil the presence of a siliceous cell wall, the frustule. This structure remains were sufficiently abundant to allow discovery. -
Rapid Fluctuations in Mid-Latitude Siliceous Plankton Production
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln ANDRILL Research and Publications Antarctic Drilling Program 1-2014 Rapid Fluctuations in Mid-Latitude Siliceous Plankton Production during the Middle Eocene Climatic Optimum (ODP Site 1051, Western North Atlantic) Jakub Witkowski University of Szczecin, [email protected] Steven M. Bohaty University of Southampton, [email protected] Kirsty M. Edgar Cardiff nU iversity David M. Harwood University of Nebraska-Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/andrillrespub Part of the Climate Commons, Marine Biology Commons, Other Plant Sciences Commons, and the Paleobiology Commons Witkowski, Jakub; Bohaty, Steven M.; Edgar, Kirsty M.; and Harwood, David M., "Rapid Fluctuations in Mid-Latitude Siliceous Plankton Production during the Middle Eocene Climatic Optimum (ODP Site 1051, Western North Atlantic)" (2014). ANDRILL Research and Publications. 58. https://digitalcommons.unl.edu/andrillrespub/58 This Article is brought to you for free and open access by the Antarctic Drilling Program at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in ANDRILL Research and Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Published in Marine Micropaleontology 106, January (2014), pp. 110–129; doi: 10.1016/j.marmicro.2014.01.001 Copyright © 2014 Elsevier. Used by permission. Submitted September 22, 2013; revised December 5, 2013; accepted January 3, 2014; published online January 11, 2014. Rapid fluctuations in mid-latitude siliceous plankton production during the Middle Eocene Climatic Optimum (ODP Site 1051, western North Atlantic) Jakub Witkowski,1 Steven M. Bohaty,2 Kirsty M. -
Closure of the Proterozoic Mozambique Ocean Was Instigated by a Late Tonian Plate Reorganization Event ✉ Alan S
ARTICLE https://doi.org/10.1038/s43247-021-00149-z OPEN Closure of the Proterozoic Mozambique Ocean was instigated by a late Tonian plate reorganization event ✉ Alan S. Collins 1 , Morgan L. Blades1, Andrew S. Merdith2 & John D. Foden 1 Plate reorganization events involve fundamental changes in lithospheric plate-motions and can influence the lithosphere-mantle system as well as both ocean and atmospheric circu- lation through bathymetric and topographic changes. Here, we compile published data to interpret the geological record of the Neoproterozoic Arabian-Nubian Shield and integrate this with a full-plate tectonic reconstruction. Our model reveals a plate reorganization event 1234567890():,; in the late Tonian period about 720 million years ago that changed plate-movement directions in the Mozambique Ocean. After the reorganization, Neoproterozoic India moved towards both the African cratons and Australia-Mawson and instigated the future amalgamation of central Gondwana about 200 million years later. This plate kinematic change is coeval with the breakup of the core of Rodinia between Australia-Mawson and Laurentia and Kalahari and Congo. We suggest the plate reorganization event caused the long-term shift of continents to the southern hemisphere and created a pan-northern hemisphere ocean in the Ediacaran. 1 Tectonics and Earth Systems (TES), Department of Earth Sciences, The University of Adelaide, Adelaide, SA, Australia. 2 UnivLyon, UniversitéLyon 1, Ens de Lyon, CNRS, UMR 5276 LGL-TPE, Villeurbanne, France. ✉email: [email protected] COMMUNICATIONS EARTH & ENVIRONMENT | (2021) 2:75 | https://doi.org/10.1038/s43247-021-00149-z | www.nature.com/commsenv 1 ARTICLE COMMUNICATIONS EARTH & ENVIRONMENT | https://doi.org/10.1038/s43247-021-00149-z late tectonics is characterized by periods of gradual, broadly Event17,18, to the biosphere tumult that included the ecological continuous, plate movement that are punctuated by rela- takeover of eukaryote cells19,20 and, ultimately, to the evolution of P 1,2 21,22 tively short times of plate reorganization . -
The Occurrence and Preservation of Diatoms in the Palaeogene of the North Sea Basin
The Occurrence and Preservation of Diatoms in the Palaeogene of The North Sea Basin Alexander Gideon Mitlehner Thesis submitted for the degree of Doctor of Philosophy University of London Postgraduate Unit of Micropalaeontology Department of Geological Sciences University College London September 1994 ProQuest Number: 10044326 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest. ProQuest 10044326 Published by ProQuest LLC(2016). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States Code. Microform Edition © ProQuest LLC. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 ABSTRACT The often widespread occurrence of diatoms in the marine sediments of the North Sea Palaeogene has long been recognised. They occur in abundance through a number of intervals where calcareous microfossils are absent (due to palaeoenvironmental conditions and subsequent dissolution). However, poor preservation has previously impeded the taxonomic identification of these diatom assemblages, with most specimens occurring as pyritised inner moulds (steinkems). This study has involved the first detailed description of these assemblages, which was achieved through the use of electron microscopy combined with comparisons with well-preserved specimens, and a survey of original species descriptions held in the Natural History Museum. These techniques have enabled the identification of a total of 79 species, 40 of which have not previously been formally described in pyritised form. -
Madbi Amran / Qishn Total Petroleum System of the Ma′Rib–Al Jawf / Shabwah, and Masila-Jeza Basins, Yemen
Madbi Amran / Qishn Total Petroleum System of the Ma′Rib–Al Jawf / Shabwah, and Masila-Jeza Basins, Yemen 2001 Rub' Al Khali Basin Yemen Volcanic 2019 Ghudun-Khasfeh Flank Province Basin (North) 2010 2101 SAUDI ARABIA Ma'Rib-Al Jabal Ras 1 Al-Saidah As'ad al-Kamil Jawf Basin Saif Bin Yazen Sunah Sunah Northeast Dostour Al-Wahdah Qarn Qaymah 1 Kamaran Raydan Meem Wadi Taribah 2004 Azal Balquis Al-Shura Hemiar North Jabal Samadan Kharir Suqatrah Masila-Jeza Basin Hemiar Al-Raja - Jannah Hemiar South Al-Tahreer Husn El Kradis 1 Hemiar West Shaharah Al Kharwah 1 Haru Sanaa Al-Wihdah Atuf Northwest Yah 1 Camaal North Camaal Nazaih Wadi Bana Tawila Ayad West Heijah Hays Structural Belt Lam 1 Mukalla Ma'een 1 Amal Ayad East 2009 Alif Mawza 1 Aser 1 High Jabal Nuqum Al Khair 1 Nakaa 1 Magraf 1 Y Jabal Habah Dhahab 1 emen V Jabal Barat 1 Al Nasr 1 Mintaq 1 Rajwan 1 Halewah-Sabatayn Mukalla Sharmah Rift Basin olcanic Basin (South) Arabian Shield 2007 Red Sea Basin 2101 Taiz Shabwah YEMEN Basin 2002 2006 Mukalla Rift Basin Gulf of Aden 2005 0 100 KILOMETERS 2003 Aden 2071 EXPLANATION Geologic province and code Madbi Amran/Qishn Total Petroleum System outline Gas field Assessment unit outline Oil field Source rock outline Country boundary Location of thermal modeling (fig. 14) INDEX MAP City U.S. Geological Survey Bulletin 2202-G U.S. Department of the Interior U.S. Geological Survey Madbi Amran / Qishn Total Petroleum System of the Ma′Rib–Al Jawf / Shabwah, and Masila-Jeza Basins, Yemen By Thomas S.