An Annotated Bibliography of Selected References of Fishes of the North Slope of Alaska, with Emphasis on Research Conducted in National Petroleum Reserve - Alaska
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Abandonment of Unaweep Canyon (1.4–0.8 Ma), Western Colorado: Effects of Stream Capture and Anomalously Rapid Pleistocene River Incision
CRevolution 2: Origin and Evolution of the Colorado River System II themed issue Abandonment of Unaweep Canyon (1.4–0.8 Ma), western Colorado: Effects of stream capture and anomalously rapid Pleistocene river incision Andres Aslan1,*, William C. Hood2,*, Karl E. Karlstrom3,*, Eric Kirby4, Darryl E. Granger5,*, Shari Kelley6, Ryan Crow3,*, Magdalena S. Donahue3,*, Victor Polyak3,*, and Yemane Asmerom3,* 1Department of Physical and Environmental Sciences, Colorado Mesa University, Grand Junction, Colorado 81501, USA 2Grand Junction Geological Society, 515 Dove Court, Grand Junction, Colorado 81501, USA 3Department of Earth and Planetary Sciences, University of New Mexico, Northrop Hall 141, Albuquerque, New Mexico 87131, USA 4College of Earth, Ocean and Atmospheric Sciences, Oregon State University, 202D Wilkinson Hall, Corvallis, Oregon 97330, USA 5Department of Earth and Atmospheric Sciences, Purdue University, 550 Stadium Mall Drive, West Lafayette, Indiana 47907, USA 6New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, New Mexico 87801, USA ABSTRACT opment of signifi cant relief between adjacent through resistant Precambrian bedrock (Fig. 2). stream segments, which led to stream piracy. It has no major river at its base, and is currently Cosmogenic-burial and U-series dating, The response of rivers to the abandonment drained by two underfi t streams, East and West identifi cation of fl uvial terraces and lacus- of Unaweep Canyon illustrates how the Creeks, which drain the northeast and southwest trine deposits, and river profi le reconstruc- mode and tempo of long-term fl uvial incision ends of the canyon, respectively. Starting with tions show that capture of the Gunnison are punctuated by short-term geomorphic the Hayden Survey (Peale, 1877), geologists River by the Colorado River and abandon- events such as stream piracy. -
Topographic Controls on Divide Migration, Stream Capture, and Diversification in Riverine Life
Earth Surf. Dynam., 8, 893–912, 2020 https://doi.org/10.5194/esurf-8-893-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Topographic controls on divide migration, stream capture, and diversification in riverine life Nathan J. Lyons1, Pedro Val2, James S. Albert3, Jane K. Willenbring4, and Nicole M. Gasparini1 1Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA, USA 2Department of Geology, Federal University of Ouro Preto, Ouro Preto, Brazil 3Department of Biology, University of Louisiana at Lafayette, Lafayette, CA, USA 4Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA Correspondence: Nathan J. Lyons ([email protected]) Received: 16 October 2019 – Discussion started: 24 October 2019 Revised: 9 August 2020 – Accepted: 2 September 2020 – Published: 26 October 2020 Abstract. Drainages reorganise in landscapes under diverse conditions and process dynamics that impact biotic distributions and evolution. We first investigated the relative control that Earth surface process parameters have on divide migration and stream capture in scenarios of base-level fall and heterogeneous uplift. A model built with the Landlab toolkit was run 51 200 times in sensitivity analyses that used globally observed values. Large- scale drainage reorganisation occurred only in the model runs within a limited combination of parameters and conditions. Uplift rate, rock erodibility, and the magnitude of perturbation (base-level fall or fault displacement) had the greatest influence on drainage reorganisation. The relative magnitudes of perturbation and topographic relief limited landscape susceptibility to reorganisation. Stream captures occurred more often when the channel head distance to divide was low. -
A Groundwater Sapping in Stream Piracy
Darryll T. Pederson, Department of energy to the system as increased logic settings, such as in a delta, stream Geosciences, University of Nebraska, recharge causes groundwater levels to piracy is a cyclic event. The final act of Lincoln, NE 68588-0340, USA rise, accelerating stream piracy. stream piracy is likely a rapid event that should be reflected as such in the geo- INTRODUCTION logic record. Understanding the mecha- The term stream piracy brings to mind nisms for stream piracy can lead to bet- ABSTRACT an action of forcible taking, leaving the ter understanding of the geologic record. Stream piracy describes a water-diver- helpless and plundered river poorer for Recognition that stream piracy has sion event during which water from one the experience—a takeoff on stories of occurred in the past is commonly based stream is captured by another stream the pirates of old. In an ironic sense, on observations such as barbed tribu- with a lower base level. Its past occur- two schools of thought are claiming vil- taries, dry valleys, beheaded streams, rence is recognized by unusual patterns lain status. Lane (1899) thought the term and elbows of capture. A marked of drainage, changes in accumulating too violent and sudden, and he used change of composition of accumulating sediment, and cyclic patterns of sediment “stream capture” to describe a ground- sediment in deltas, sedimentary basins, deposition. Stream piracy has been re- water-sapping–driven event, which he terraces, and/or biotic distributions also ported on all time and size scales, but its envisioned to be less dramatic and to be may signify upstream piracy (Bishop, mechanisms are controversial. -
Formation Mechanism for Upland Low-Relief Surface Landscapes in the Three Gorges Region, China
remote sensing Article Formation Mechanism for Upland Low-Relief Surface Landscapes in the Three Gorges Region, China Lingyun Lv 1,2, Lunche Wang 1,2,* , Chang’an Li 1,2, Hui Li 1,2 , Xinsheng Wang 3 and Shaoqiang Wang 1,2,4 1 Key Laboratory of Regional Ecology and Environmental Change, School of Geography and Information Engineering, China University of Geosciences, Wuhan 430074, China; [email protected] (L.L.); [email protected] (C.L.); [email protected] (H.L.); [email protected] (S.W.) 2 Hubei Key Laboratory of Critical Zone Evolution, School of Geography and Information Engineering, China University of Geosciences, Wuhan 430074, China 3 Hubei Key Laboratory of Regional Development and Environmental Response, Hubei University, Wuhan 430062, China; [email protected] 4 Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China * Correspondence: [email protected] Received: 9 November 2020; Accepted: 26 November 2020; Published: 27 November 2020 Abstract: Extensive areas with low-relief surfaces that are almost flat surfaces high in the mountain ranges constitute the dominant geomorphic feature of the Three Gorges area. However, their origin remains a matter of debate, and has been interpreted previously as the result of fluvial erosion after peneplain uplift. Here, a new formation mechanism for these low-relief surface landscapes has been proposed, based on the analyses of low-relief surface distribution, swath profiles, χ mapping, river capture landform characteristics, and a numerical analytical model. The results showed that the low-relief surfaces in the Three Gorges area could be divided into higher elevation and lower elevation surfaces, distributed mainly in the highlands between the Yangtze River and Qingjiang River. -
Alaska Fisheries Data Series Number 2013-3
U.S. Fish & Wildlife Service Seasonal Migrations and Essential Habitats of Broad Whitefish, Humpback Whitefish, and Least Cisco in the Selawik River Delta, as Inferred from Radiotelemetry Data, 2004–2006 Alaska Fisheries Data Series Number 2013-3 Fairbanks Fish and Wildlife Field Office Fairbanks, Alaska April 2013 The Alaska Region Fisheries Program of the U.S. Fish and Wildlife Service conducts fisheries monitoring and population assessment studies throughout many areas of Alaska. Dedicated professional staff located in Anchorage, Fairbanks, and Kenai Fish and Wildlife Offices and the Anchorage Conservation Genetics Laboratory serve as the core of the Program’s fisheries management study efforts. Administrative and technical support is provided by staff in the Anchorage Regional Office. Our program works closely with the Alaska Department of Fish and Game and other partners to conserve and restore Alaska’s fish populations and aquatic habitats. Our fisheries studies occur throughout the 16 National Wildlife Refuges in Alaska as well as off- Refuges to address issues of interjurisdictional fisheries and aquatic habitat conservation. Additional information about the Fisheries Program and work conducted by our field offices can be obtained at: http://alaska.fws.gov/fisheries/index.htm The Alaska Region Fisheries Program reports its study findings through the Alaska Fisheries Data Series (AFDS) or in recognized peer-reviewed journals. The AFDS was established to provide timely dissemination of data to fishery managers and other technically oriented professionals, for inclusion in agency databases, and to archive detailed study designs and results for the benefit of future investigations. Publication in the AFDS does not preclude further reporting of study results through recognized peer-reviewed journals. -
Fort:Ton of the Eastern.Most Ventura Basin Eu Gene M. Shoemaker
Geomorphology o f a :F o r t:ton of the East e rn.most Ventura Basin by Eu gene M. Shoemaker 1 948 Relief model of the HtUJi.phreys ( uadr&.ngl e, view lool\:ing northe <~ st (model and photograph by John Lnnce}. Abstract The hl..UYiphreys ;{uadrangl e is a p o rtion of the eastern ; most Ventura Basin underlain by a thic k series of Tertiary sedime ntary rocks . On t~eso rocks a gr eat variety of geomorphic forms have bee n molded by t he p rocess es of r unninc water t y:o ical of· a semi-arid climate ancl. b y several ty:qe s of :rw.ss movement . Among t he dii'ferent c a t ar;o:r> i e s of n1s.ss mo v ement -o:i:' e sent, t:t n evr t ype, the sil t f'l..£:2: ,,._ras obs r-i rvc d . 'T'b.e r::eomor::;hj_c f orm.s o:f s:oecia1 int er•e s t :ore ,s-":'nt i .n thG c:~ ·n ·'.' C\ r !.1.:r~ :) .0 :;. r e rock .;ones, open can:y-onh e ads, as~!rmne tri c cs.nyons , e.nd s tre8In terraces and stra.ths . 'l'he author urges t h e a doption of the definition of strath as thRt :p ai~t o f a n old dissectec~. v alley floor, i ncluding the floors of tributary valleys, which was not part of t h e floodp l a i n of t he main v.all ey strearn. -
Annual Management Report for Sport Fisheries in the Arctic-Yukon-Kuskokwim Region, 1987
Fishery Management Report No. 91-1 Annual Management Report for Sport Fisheries in the Arctic-Yukon-Kuskokwim Region, 1987 William D. Arvey, Michael J. Kramer, Jerome E. Hallberg, James F. Parker, and Alfred L. DeCicco April 1991 Alaska Department of Fish and Game Division of Sport Fish FISHERY MANAGEMENT REPORT NO. 91-1 ANNUAL MANAGEMENT REPORT FOR SPORT FISHERIES IN THE ARCTIC-YUKON-KUSKOKWIM REGION, 1987l William D. Arvey, Michael J. Kramer, Jerome E. Hallberg, James F. Parker, and Alfred L. DeCicco Alaska Department of Fish and Game Division of Sport Fish Anchorage, Alaska April 1991 Some of the data included in this report were collected under various jobs of project F-10-3 of the Federal Aid in Fish Restoration Act (16 U.S.C. 777-777K). TABLE OF CONTENTS LIST OF TABLES............................................... iv LIST OF FIGURES.............................................. V LIST OF APPENDICES ........................................... vii ABSTRACT ..................................................... 1 PREFACE...................................................... 2 INTRODUCTION................................................. 3 TANANA AREA DESCRIPTION ...................................... 3 Geographic and Geologic Setting ......................... 3 Lake and Stream Development ............................. 10 Climate................................................. 13 Primary Species for Sport Fishing ....................... 13 Status and Harvest Trends of Wild Stocks ................ 13 Chinook Salmon .................................... -
Guided Notes on Stream Development, Section 9.2
Guided Notes on Stream Development, Section 9.2 1. As a stream develops, it changes in shape, width, and size, as well as the landscapes over which it flows. 2. The first and foremost condition necessary for stream formation is an adequate supply of water. 3. The region where water first accumulates to supply a stream is called the headwaters. 4. Moving water carves a narrow pathway into the sediment or rock called a stream channel. 5. Stream banks are the ground bordering the stream on each side. 6. The process by which small streams erode away the rock or soil at the head of a stream is known as headward erosion. 7. Sometimes, a stream erodes its way through the high area separating two drainage basins, joins another stream, and then draws away its water. This process is called stream capture or stream piracy. 8. As a stream actively erodes its path through the sediment or rock, a V-shaped channel develops. V-shaped channels have steep sides and sometimes form canyons or gorges. 9. The lowest base level possible for any stream is sea level, the point at which the stream enters the ocean. 10. As stream channels develop into U-shaped valleys, the volume of water and sediment that they are able to carry increases. 11. A bend or curve in a stream channel caused by moving water is called a meander. 12. The blocked-off meander becomes an oxbow lake, which eventually dries up. 13. The differences in the rate of water flow within meanders cause the meanders to become more accentuated over time. -
Deficiencies in Our Understanding of the Hydro-Ecology of Several Native Australian Fish: a Rapid Evidence Synthesis
Marine and Freshwater Research, 2018, 69, 1208–1221 © CSIRO 2018 https://doi.org/10.1071/MF17241 Supplementary material Deficiencies in our understanding of the hydro-ecology of several native Australian fish: a rapid evidence synthesis Kimberly A. MillerA,D, Roser Casas-MuletB,A, Siobhan C. de LittleA, Michael J. StewardsonA, Wayne M. KosterC and J. Angus WebbA,E ADepartment of Infrastructure Engineering, The University of Melbourne, Parkville, Vic. 3010, Australia. BWater Research Institute, Cardiff University, The Sir Martin Evans Building, Museum Avenue, Cardiff, CF10 3AX, UK. CArthur Rylah Institute for Environmental Research, Department of Environment, Land, Water and Planning, Heidelberg, Vic. 3084, Australia. DPresent address: Healesville Sanctuary, Badger Creek Road, Healesville, Vic. 3777, Australia. ECorresponding author. Email address: [email protected] Page 1 of 30 Marine and Freshwater Research © CSIRO 2018 https://doi.org/10.1071/MF17241 Table S1. All papers located by standardised searches and following citation trails for the two rapid evidence assessments All papers are marked as Relevant or Irrelevant based on a reading of the title and abstract. Those deemed relevant on the first screen are marked as Relevant or Irrelevant based on a full assessment of the reference.The table contains incomplete citation details for a number of irrelevant papers. The information provided is as returned from the different evidence databases. Given that these references were not relevant to our review, we have not sought out the full citation details. Source Reference Relevance Relevance (based on title (after reading and abstract) full text) Pygmy perch & carp gudgeons Search hit Anon (1998) Soy protein-based formulas: recommendations for use in infant feeding. -
Niukluk River Salmon Counting Tower Project Summary Report, 1999
Niukluk River Salmon Counting Tower Project Summary Report, 1999 by Tom Kohler Alaska DepaIlment of Fish & Game Commercial Fisheries Division, AYK Region 333 RaspbelTY Road Anchorage, Alaska 99518-l599 Regional InFormational Report 1 No. 3AOO-09 January 2000 'The Regional Information Report Series was establi hed in 1987 to provide an information access systcm for all unpublished divisional reports. 1l1ese reports frequently scrve diverse ad hoc informational purposes or archive basic uninterpreted data. To accommodate timely rcporting of rccently collected information. reports in this series undergo only limited internal review and may contain preliminary data: this infonnation may be subsequently finalized and published in thc formal literature. Cons quently. tl1ese reports should not be cited without prior approval of tl1e author or the Commercial Fisheries Division. TABLE OF CONTENTS List of Tables II List of Figures III Introduction 1 Objecti ves......................................................................................................... 1 Methods . Results 3 Discussion 4 Acknowledgments 6 Literature Cited........................................................................................................ 6 Tables 7 Figures 21 LIST OF TABLES I. Expanded daily and cumulative migration of all salmonid species past the 7 Niukluk River counting tower, orton Sound 1999 . 2. Expanded daily hourly chum salmon migration past the Niukluk River counting tower, Norton Sound, 1999 . 8 3. Expanded daily hourly pink salmon migration past the iukluk River counting tower, Norton Sound, 1999 . 9 4. Expanded daily hourly king salmon migration past the Niukluk River counting tower, NOlton Sound, 1999 .. 10 5. Expanded daily hourly coho salmon migration past the Niukluk River counting tower, Ol1on Sound, 1999 .. II 6. Expanded daily hourly Dolly Varden migration past the Niukluk River counting tower, NOIton Sound, 1999 . -
Norton Sound Golovin and Moses Point Subdistricts Chum Salmon Stock Status and Action Plan
NORTON SOUND GOLOVIN AND MOSES POINT SUBDISTRICTS CHUM SALMON STOCK STATUS AND ACTION PLAN A Report to the Alaska Board of Fisheries By: Jim Menard Daniel 1. Bergstrom Regional Information Report No. 3A03-36 Alaska Department of Fish and Game Division of Commercial Fisheries 333 Raspberry Road Anchorage, Alaska 99518 December 2003 I The Rcgioo31lnforrnatioo Rl,.-port Series was cslablished in 1987 (0 provide an infonnatioo access system for aU wlpublished divisional reports. Th(.'SC reports frequelllly SCI"'tC diverse ad hoc infonnationa.l purpooes or archive basic uninlcrprcted data. To accommodmc needs for up-t(}{laIC infonn.1tion, rt.-p<>rts in this !.(..";es may contain preliminary d'lta; this information may be subsequently finalized and published in the fannal literature. onscqucntly, theM: reports should nOl be ciled without prior approval oCthe aulllor of tile Division ofCommercial Fisheries. AUTHORS Jim Menard is the Area Management Biologist for the Norton Sound -P rt Clarence Area and the Kotzebue Area, Alaska Department of Fish and Game, DiVIsion of Commercial Fisheries, P.O. Box 1148, Nome, AK 99762. Daniel 1. Bergstrom is the AYK Regional Management Biologist for the Alaska Department of Fish and Game, Division of Commercial Fisheries, 333 RaspbelTY Road, Anchorage, AK 99518. OFFICE OF EQUAL OPPORTUNITY (OEO) STATEMENT The Alaska Department of Fish and Game administers all programs an activities free from discrimination based on race, color, national origin, age, sex, reli ion, marital status, pregnancy, parenthood, or disability. The department administers all pr grams and activities in compliance with Title VI of the Civil Rights Act of 1964, Section 504 of the Rehabilitation Act of 1973, Title II of the Americans with Disabilities Act of 1990, the Age Discrimination Act of 1975, and Title [)( of the Education Amendments of 1972. -
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i 1 , . .... "~ sa:J!AldS ldp-eqJ pu~ lOtU.NO~ l.N3V\IO::lOG . ) ~OScJ}I/ifufqS~tJ~JJOc!S OJ.. u.ml.aH asea1d l . '~~ ~ ·---*-"to!'< • • '1~}'~1';:>'·-.~-z::_-'", V)ISVI]V JaqwnN +uawnooo ;:un+Ua 1\ lU!Of BUl!SnS @@®W@ID o W~MW{}{l .. Alaska Department of Fish and Game Sport Fish Division Jay S. Hammond, Governor t r-- " •' .! STATE OF AJ,.4SIU\ \) .. ·J:.y s, Hammond, Govf}Cnor t l } ,r ~ " ,.r -t'' L :.~ DJ:PARTMENT: OF 'FISH:.ANO .. GAME:.· 1, f f . ·.Ronald O._Skoog, Commlaaloner ) I( ·~~ ! . ~~ ~ .. t ·'' -~. :-""'.' ~ ~ ·.• ... ~~. SPORT FISH [IIVISION ... ·... ,.;"!. .. ... ,. .- 'Rup.,-t E. An~r•v~a, Director .· · d ·' ',' . ~ · Thls.bQOkJ~t ls_tritended, a{a~!~~tory of. sport ff~hlng r~sorts and charter.. services in -Alaska and ~~es rrQ~ co~stltute endprsem~nt; py th~ "'- dO, ~ ' " ~ " l .. Stat$ of· ·Afaska. Additional Information and prices may be'obtalried b¥ writ!ng diF~cJiyto the operators listed. · ·· ' ,. I ~ • ,, .~ } ••• spoit':flshln~ license Is req~JI;ed'al1c.t'must~ b~ hi the posseslon ~f. all 'persons 16 y.ears of age an~·oider while flshrn~.Jn tM State. r· ' ..... ·. ~ ' .. · '., .. ,.,. t .. -Licehs$~ .maY. be purcHased~ by· maillrorn "the b'epartment of.Fif}venue, 'Ffsh- and. Gam& Llcens~ Olvislon, 240 South franklin. Stre~t: . ::4u~e.au •. Aias~~998Q1. T11.ey ~re ~rso ~Sold by Ucense..v~~~ors In cUtes-throughout th~ ,State. The yew.ly ~oqreslder;Jt sport fisliing. Hcerist:. · ·~}, ... : ,· ··: ' ". " .. ,. ~ fee Is $30: .how~ver., ~ speQ.Ial1-:day vll?itor'$ollcensemaybe .pur'chased tot ~5 or a 1O.:day vlsitor~s .lfc;e.nse fqr·$15.