Ammocrypta Pellucida Putnam Eastern Sand Darter
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The Huron River History Book
THE HURON RIVER Robert Wittersheim Over 15,000 years ago, the Huron River was born as a small stream draining the late Pleistocene landscape. Its original destination was Lake Maumee at present day Ypsilanti where a large delta was formed. As centuries passed, ceding lake levels allowed the Huron to meander over new land eventually settling into its present valley. Its 125 mile journey today begins at Big Lake near Pontiac and ends in Lake Erie. The Huron’s watershed, which includes 367 miles of tributaries, drains over 900 square miles of land. The total drop in elevation from source to mouth is nearly 300 feet. The Huron’s upper third is clear and fast, even supporting a modest trout fishery. The middle third passes through and around many lakes in Livingston and Washtenaw Counties. Eight dams impede much of the Huron’s lower third as it flows through populous areas it helped create. Over 47 miles of this river winds through publicly owned lands, a legacy from visionaries long since passed. White Lake White Lake Mary Johnson The Great Lakes which surround Michigan and the thousands of smaller lakes, hundreds of rivers, streams and ponds were formed as the glacier ice that covered the land nearly 14,000 years ago was melting. The waters filled the depressions in the earth. The glaciers deposited rock, gravel and soil that had been gathered in their movement. This activity sculpted the land creating our landscape. In section 28 of Springfield Township, Oakland County, a body of water names Big Lake by the area pioneers is the source of the Huron River. -
C:\Fish\Eastern Sand Darter Sa.Wpd
EASTERN SAND DARTER STATUS ASSESSMENT Prepared by: David Grandmaison and Joseph Mayasich Natural Resources Research Institute University of Minnesota 5013 Miller Trunk Highway Duluth, MN 55811-1442 and David Etnier Ecology and Evolutionary Biology University of Tennessee 569 Dabney Hall Knoxville, TN 37996-1610 Prepared for: U.S. Fish and Wildlife Service Region 3 1 Federal Drive Fort Snelling, MN 55111 January 2004 NRRI Technical Report No. NRRI/TR-2003/40 DISCLAIMER This document is a compilation of biological data and a description of past, present, and likely future threats to the eastern sand darter, Ammocrypta pellucida (Agassiz). It does not represent a decision by the U.S. Fish and Wildlife Service (Service) on whether this taxon should be designated as a candidate species for listing as threatened or endangered under the Federal Endangered Species Act. That decision will be made by the Service after reviewing this document; other relevant biological and threat data not included herein; and all relevant laws, regulations, and policies. The result of the decision will be posted on the Service's Region 3 Web site (refer to: http://midwest.fws.gov/eco_serv/endangrd/lists/concern.html). If designated as a candidate species, the taxon will subsequently be added to the Service's candidate species list that is periodically published in the Federal Register and posted on the World Wide Web (refer to: http://endangered.fws.gov/wildlife.html). Even if the taxon does not warrant candidate status it should benefit from the conservation recommendations that are contained in this document. ii TABLE OF CONTENTS DISCLAIMER................................................................... -
Huron River Water Trail Trip Description 1 Hudson Mills Metropark
Huron River Water Trail Trip Description Hudson Mills Metropark (Mile 67) to Delhi Metropark (Mile 58.3) - 3.5 hours; 8.7 miles Launch at the Rapids View Picnic Area in Hudson Mills Metropark, near North Territorial Road. This trip provides easy access to both launch and take-out sites. Paddle through parkland and then into Dexter. TRIP DESCRIPTION: Excerpt from “Canoeing Michigan Rivers: A Comprehensive Guide to 45 Rivers” by Jerry Dennis and Craig Date provided with permission from Thunder Bay Press. Put in at Hudson Mills Metropark, where there is good access and parking just below Territorial Road [at the Rapids View Picnic Area]. Upstream, fair access and parking are found a Bell Road. [Note: Launching at Bell Road will take you past the Hudson Mills canoe campground and rapids where a portage is recommended.] The river here is 60-90 feet wide and alternates sections of slow water one to four feet deep with sections of very shallow riffles. Low water in summer will produce some bottom-bumping. Hudson Mills has been the site of a saw mill, grist mill, cider mill and plaster mill, the earliest dating back to 1827. Today, only the ruins of foundations and a short stretch of light rapids mark the spot just below Territorial Road Bridge where the mills were located. The rapids can be run down the chute at left center. Pumpkin- to bushel-size rocks create standing waves that could become fairly high during high water. If in doubt, portage on the left just beyond the bridge. Light riffles extend well into Hudson Mills Metropark, where there are several access sites and two overnight canoe campgrounds. -
Eastern Sand Darter (Ammocrypta Pellucida) in Canada (Ontario Populations) for the Period 2012 - 2017
Species at Risk Act Recovery Strategy Report Series Report on the Progress of Recovery Strategy Implementation for the Eastern Sand Darter (Ammocrypta pellucida) in Canada (Ontario Populations) for the Period 2012 - 2017 Eastern Sand Darter 2018 c Report on the Progress of Recovery Strategy Implementation for the Eastern Sand Darter 2018 Recommended Citation: Fisheries and Oceans Canada. 2018. Report on the Progress of Recovery Strategy Implementation for the Eastern Sand Darter (Ammocrypta pellucida) in Canada (Ontario Populations) for the Period 2012 – 2017. Species at Risk Act Recovery Strategy Report Series. Fisheries and Oceans Canada, Ottawa. v + 33 p. For copies of the progress report, or for additional information on species at risk, including COSEWIC Status Reports, recovery strategies, residence descriptions, action plans, and other related recovery documents, please visit the Species at Risk Public Registry. Cover illustration: Alan Dextrase, Ontario Ministry of Natural Resources and Forestry Également disponible en français sous le titre « Rapport sur les progrès de la mise en œuvre du programme de rétablissement du dard de sable (Ammocrypta pellucida) au Canada, populations de l’Ontario pour la période 2012-2017» © Her Majesty the Queen in Right of Canada, represented by the Minister of Fisheries and Oceans Canada, 2018. All rights reserved. ISBN 978-0-660-24756-4 Catalogue no. En3-4/122-1-2018E-PDF Content (excluding the cover illustration) may be used without permission, with appropriate credit to the source. i Report on the Progress of Recovery Strategy Implementation for the Eastern Sand Darter 2018 Preface The federal, provincial, and territorial government signatories under the 3Accord for the Protection of Species at Risk (1996) agreed to establish complementary legislation and programs that provide for effective protection of species at risk throughout Canada. -
Ruffe (Gymnocephalus Cernua) Ecological Risk Screening Summary
U.S. Fish and Wildlife Service Ruffe (Gymnocephalus cernua) Ecological Risk Screening Summary US Fish and Wildlife Service, February 2011 Revised, July 2014 Revised, June 2015 Photo: USFWS 1 Native Range, and Status in the United States Native Range From Fuller et al. (2014): “Northern Europe and Asia (Berg 1949; Holcik and Hensel 1974; Wheeler 1978; Page and Burr 1991).” Status in the United States From Fuller et al. (2014): “The ruffe was first identified by Wisconsin DNR in specimens collected from the St. Louis River at the border of Minnesota and Wisconsin in 1987 (Pratt 1988; Pratt et al. 1992; Czypinski et al. 1999, 2000, 2001, 2003). Following that report, reexamination of archived samples revealed misidentified larval specimens of ruffe had been collected from the same area in 1986 (Pratt 1988). The ruffe subsequently spread into Duluth Harbor in Lake Superior and several tributaries of the lake (Underhill 1989; Czypinski et al. 1999, 2000, 2004; Scheidegger, pers. comm.; J. Slade, pers. comm.). It is found in the Amnicon, Flag, Iron, Middle, Raspberry, and Bad rivers, Chequamegon Bay, and Apostle Islands National Lakeshore in Wisconsin (Czypinski et al. 1999, 2000, 2001, 2003, 2004; Tilmant 1999). In August 1994, it was found in Saxon Harbor, Wisconsin, and in the upper peninsula of Michigan at the mouths of the Black and Ontonagon rivers (K. Kindt, pers. comm.). In the lower Peninsula of Michigan along Lake Huron, the first three specimens were caught at the mouth of the Thunder Bay River in August 1995 (K. Kindt, pers. comm.). This species has also been collected in Michigan in Lake Michigan, Lake Superior, Torch Lake, Little Bay de Noc in Escanaba, Big Bay de Noc, Misery River, Ontonagon River, Thunder Bay, and Sturgeon River Sloughs (Czypinski et al. -
Low-Head Dams Facilitate Round Goby Neogobius Melanostomus Invasion
Biol Invasions (2018) 20:757–776 https://doi.org/10.1007/s10530-017-1573-3 ORIGINAL PAPER Low-head dams facilitate Round Goby Neogobius melanostomus invasion Dustin Raab . Nicholas E. Mandrak . Anthony Ricciardi Received: 9 July 2017 / Accepted: 23 September 2017 / Published online: 3 October 2017 Ó Springer International Publishing AG 2017 Abstract Round Goby Neogobius melanostomus inclusion of both reservoir-associated abiotic variables invasion of the Grand River (Ontario, Canada) and Round Goby abundance as model terms. To presents an opportunity to assess the role of abiotic determine establishment potential of the uninvaded gradients in mediating the establishment and impact of reach immediately upstream, four environmental nonnative benthic fishes in rivers. In this system, habitat characteristics were used in discriminant sequential low-head dams delineate uninvaded and function analysis (DFA) to predict three potential invaded river reaches and create upstream gradients of outcomes of introduction: non-invaded and either increasing water velocity. We hypothesized that flow lower or higher Round Goby abundance (low and high refugia created by impounded reservoirs above low- invasion status, respectively) than the median number head dams enhance local Round Goby abundance. of Round Goby at invaded sites. Our DFA function Round Goby influence on the native fish community correctly classified non-invaded and high-abundance was determined by variance partitioning, and we used invasion status sites [ 85% of the time, with lower generalized additive models to identify small-bodied (73%) success in classifying low-abundance invasion benthic fish species most likely to be impacted by status sites, and the spatial pattern of our results Round Goby invasion. -
Delhi Metropark
PARK MAP Park Entrance H udso GPS: 42º23’18.52”N 83º54’12.17”W n Mills M etropa te rk i s S s West HUR e c c River ON RIVER DR Trail to g A n Dexter i CHAMBERLIN RD h s Fi Hur HUR o r n R e Group iv D ON RIVER DR e r elh Camp i n Riv Me o tr r op u ar H Labyrinth k 1 3 2 NOR PARK ENTRANCE TH TERRIT GPS: 42º23’11.88”N 83º54’31.13”W ORIAL RD DEXTER-HURON METROPARK 6535 Huron River Drive, Dexter, MI 48130 (Administered through Hudson Mills Metropark) Rapids View 734-426-8211 • www.metroparks.com Service 23 Area MAP KEY PICNIC SHELTERS Outdoor Sports Small Boat Launch 1 West HUR Restroom Toll Booth 2 Central River Grove ON RIVER DR Oak ROADS AND TRAILS 3 East 2 Meadows Paved Road Paved Hike-Bike Trail Dirt Road Railroad Track Nature Trail FEET 0 250 500 750 1000 MILES 0 ¼ lls Met Y RD Y Mi ropa son rks ud H & on ur H r- W HUR te Activity Center ex E TER PINCKN TER D ON RIVER DR Hur X DE on Riv r 4 ive West er ron R Delhi HUR u H DELHI CT ON RIVER DR DELHI METROPARK 1 3902 East Delhi Road Ann Arbor, MI 48103 HUDSON MILLS (Administered through E DELHI RD Hudson Mills Metropark) East METROPARK 5 734-426-8211 Park Entrance Delhi 8801 North Territorial Road www.metroparks.com GPS: 42º19’55.99”N 83º48’37.65”W Pineview A Dexter, MI 48130 n GREGORY RD MAP KEY n 734-426-8211 A r www.metroparks.com Restrooms b RAILR o H OAD ST r u Small Boat Launch ro MAP KEY n R iv Camping er Boat Rental D Toll Booth Disc Golf e x t e r - Playground Outdoor Sports H u r o n Outdoor Sports & D e Paved Road Playground lh i FLEMMING RD M e Dirt Road Golf t r o p a r Railroad Track Restroom k s Small Boat Launch PICNIC SHELTERS FEET 0 250 500 750 1000 1 North Shelter Toll Booth MILES 0 ¼ Trail-head Waterslide WHITMORE Paved Roads LAKE 23 Dirt Roads N. -
A Synopsis of the Biology and Life History of Ruffe
J. Great Lakes Res. 24(2): 170-1 85 Internat. Assoc. Great Lakes Res., 1998 A Synopsis of the Biology and Life History of Ruffe Derek H. Ogle* Northland College Mathematics Department Ashland, Wisconsin 54806 ABSTRACT. The ruffe (Gymnocephalus cernuus), a Percid native to Europe and Asia, has recently been introduced in North America and new areas of Europe. A synopsis of the biology and life history of ruffe suggests a great deal of variability exists in these traits. Morphological characters vary across large geographical scales, within certain water bodies, and between sexes. Ruffe can tolerate a wide variety of conditions including fresh and brackish waters, lacustrine and lotic systems, depths of 0.25 to 85 m, montane and submontane areas, and oligotrophic to eutrophic waters. Age and size at maturity dif- fer according to temperature and levels of mortality. Ruffe spawn on a variety ofsubstrates, for extended periods of time. In some populations, individual ruffe may spawn more than once per year. Growth of ruffe is affected by sex, morphotype, water type, intraspecific density, and food supply. Ruffe feed on a wide variety of foods, although adult ruffe feed predominantly on chironomid larvae. Interactions (i.e., competition and predation) with other species appear to vary considerably between system. INDEX WORDS: Ruffe, review, taxonomy, reproduction, diet, parasite, predation. INTRODUCTION DISTRIBUTION This is a review of the existing literature on Ruffe are native to all of Europe except for along ruffe, providing a synopsis of its biology and life the Mediterranean Sea, western France, Spain, Por- history. A review of the existing literature is tugal, Norway, northern Finland, Ireland, and Scot- needed at this time because the ruffe, which is na- land (Collette and Banarescu 1977, Lelek 1987). -
Eurasian Ruffe (Gymnocephalus Cernua), Native to Northern Europe and Asia, Have Threatened the Great Lakes and Surrounding States Since the Late 1980S
State of Michigan’s Status and Strategy for Eurasian Ruffe Management Scope Invasive Eurasian ruffe (Gymnocephalus cernua), native to northern Europe and Asia, have threatened the Great Lakes and surrounding states since the late 1980s. The goals of this document are to: • Summarize the current understanding level of the biology and ecology of Eurasian ruffe. • Summarize the current management options for Eurasian ruffe in Michigan. • Identify possible future directions of Eurasian ruffe management in Michigan. Biology and Ecology I. Identification Eurasian ruffe, also known as blacktail Gary Cholwek – National Biological Service or river ruffe, is a member of genus Gymnocephalus within Percidae. Eurasian ruffe is a small, aggressive, benthic fish native to Europe and Asia. The species resemble yellow perch with distinct walleye markings (McLean 1997). The Eurasian ruffe can be distinguished from other perch by their large, jointed dorsal fin composed of 11 to 16 spines with rows of dark spots between each spine. Adult ruffe are typically five to six inches long with large individuals rarely exceeding 10 inches. They have a small, downturned mouth, lack scales on their head, and are slimy when handled (McLean 1997). Eurasian ruffe have two dorsal fins, one spiny (anterior) and one soft (posterior), and are commonly mistaken for troutperch, which have only a single dorsal fin. Their coloration consists of an olive-brown dorsal surface, pale sides, and a yellow underside (Fuller 2014, Hajjar 2002). Eurasian ruffe have two ventral fins with sharp spines on the leading edges; the anterior fin has only one spine where the posterior fin has two spines. -
Zootaxa,Three New Percid Fishes (Percidae: Percina)
Zootaxa 1549: 1–28 (2007) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2007 · Magnolia Press ISSN 1175-5334 (online edition) Three new percid fishes (Percidae: Percina) from the Mobile Basin drainage of Alabama, Georgia, and Tennessee JAMES D. WILLIAMS¹, DAVID A. NEELY², STEPHEN J. WALSH³ & NOEL M. BURKHEAD³ ¹Florida Museum of Natural History, University of Florida, Gainesville, Florida 32611, USA. E-mail: [email protected] ²Department of Ichthyology, California Academy of Sciences, San Francisco, California 904103, USA. E-mail: [email protected] ³U.S. Geological Survey, 7920 NW 71st Street, Gainesville, Florida 32653, USA. E-mail: [email protected]; [email protected] Abstract Three new species of Percina are described from upland drainages of the Mobile Basin. Two of the three species are nar- rowly distributed: P. kusha, the Bridled Darter, is currently known only from the Conasauga River drainage in Georgia and Tennessee and Etowah River drainage in Georgia, both tributaries of the Coosa River, and P. s ip si, the Bankhead Darter, which is restricted to tributaries of Sipsey Fork of the Black Warrior River in northwestern Alabama. The third species, P. smithvanizi, the Muscadine Darter, occurs above the Fall Line in the Tallapoosa River drainage in eastern Ala- bama and western Georgia. In a molecular analysis using mitochondrial cytochrome b sequence data, P. kusha and P. smithvanizi were recovered as sister species, while Percina sipsi was recovered in a clade consisting of P. aurolineata (P. sciera + P. sipsi). Two of the three species, P. kusha and P. sipsi, are considered to be imperiled species and are in need of conservation actions to prevent their extinction. -
History of the Lake St. Clair Fisheries Research Station, 1966 - 2003
DEPARTMENT OF NATURAL RESOURCES History of the Lake St. Clair Fisheries Research Station, 1966 - 2003 Mike Thomas, Research Biologist (retired) and Todd Wills, Area Station Manager Email: [email protected] Email: [email protected] The Lake St. Clair Great Lakes Station was constructed on a confined dredge disposal site at the mouth of the Clinton River and opened for business in 1974. In this photo, the Great Lakes Station (red roof) is visible in the background behind the lighter colored Macomb County Sheriff Marine Division Office. Lake St. Clair Fisheries Research Station Website: http://www.michigan.gov/dnr/0,4570,7-153-10364_52259_10951_11304---,00.html FISHERIES DIVISION LSCFRS History - 1 History of the Lake St. Clair Fisheries Research Station, 1966-2003 Preface: the other “old” guys at the station. It is my From 1992 to 2016, it was my privilege to hope that this “report” will be updated serve as a fisheries research biologist at the periodically by Station crew members who Lake St. Clair Fisheries Research Station have an interest in making sure that the (LSCFRS). During my time at the station, I past isn’t forgotten. – Mike Thomas learned that there was a rich history of fisheries research and assessment work The Beginning - 1966-1971: that was largely undocumented by the By 1960, Great Lakes fish populations and standard reports or scientific journal the fisheries they supported had been publications. This history, often referred to decimated by degraded habitat, invasive as “institutional memory”, existed mainly in species, and commercial overfishing. The the memories of station employees, in invasive alewife was overabundant and vessel logs, in old 35mm slides and prints, massive die-offs ruined Michigan beaches. -
Detroit River Group in the Michigan Basin
GEOLOGICAL SURVEY CIRCULAR 133 September 1951 DETROIT RIVER GROUP IN THE MICHIGAN BASIN By Kenneth K. Landes UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Washington, D. C. Free on application to the Geological Survey, Washington 25, D. C. CONTENTS Page Page Introduction............................ ^ Amherstburg formation................. 7 Nomenclature of the Detroit River Structural geology...................... 14 group................................ i Geologic history ....................... ^4 Detroit River group..................... 3 Economic geology...................... 19 Lucas formation....................... 3 Reference cited........................ 21 ILLUSTRATIONS Figure 1. Location of wells and cross sections used in the study .......................... ii 2. Correlation chart . ..................................... 2 3. Cross sections A-«kf to 3-G1 inclusive . ......................;.............. 4 4. Facies map of basal part of Dundee formation. ................................. 5 5. Aggregate thickness of salt beds in the Lucas formation. ........................ 8 6. Thickness map of Lucas formation. ........................................... 10 7. Thickness map of Amherstburg formation (including Sylvania sandstone member. 11 8. Lime stone/dolomite facies map of Amherstburg formation ...................... 13 9. Thickness of Sylvania sandstone member of Amherstburg formation.............. 15 10. Boundary of the Bois Blanc formation in southwestern Michigan.