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2017 ANNUAL REPORT 2017 Annual Report Table of Contents the Michael J
Roadmaps for Progress 2017 ANNUAL REPORT 2017 Annual Report Table of Contents The Michael J. Fox Foundation is dedicated to finding a cure for 2 A Note from Michael Parkinson’s disease through an 4 Annual Letter from the CEO and the Co-Founder aggressively funded research agenda 6 Roadmaps for Progress and to ensuring the development of 8 2017 in Photos improved therapies for those living 10 2017 Donor Listing 16 Legacy Circle with Parkinson’s today. 18 Industry Partners 26 Corporate Gifts 32 Tributees 36 Recurring Gifts 39 Team Fox 40 Team Fox Lifetime MVPs 46 The MJFF Signature Series 47 Team Fox in Photos 48 Financial Highlights 54 Credits 55 Boards and Councils Milestone Markers Throughout the book, look for stories of some of the dedicated Michael J. Fox Foundation community members whose generosity and collaboration are moving us forward. 1 The Michael J. Fox Foundation 2017 Annual Report “What matters most isn’t getting diagnosed with Parkinson’s, it’s A Note from what you do next. Michael J. Fox The choices we make after we’re diagnosed Dear Friend, can open doors to One of the great gifts of my life is that I've been in a position to take my experience with Parkinson's and combine it with the perspectives and expertise of others to accelerate possibilities you’d improved treatments and a cure. never imagine.’’ In 2017, thanks to your generosity and fierce belief in our shared mission, we moved closer to this goal than ever before. For helping us put breakthroughs within reach — thank you. -
Lepidoptera of North America 5
Lepidoptera of North America 5. Contributions to the Knowledge of Southern West Virginia Lepidoptera Contributions of the C.P. Gillette Museum of Arthropod Diversity Colorado State University Lepidoptera of North America 5. Contributions to the Knowledge of Southern West Virginia Lepidoptera by Valerio Albu, 1411 E. Sweetbriar Drive Fresno, CA 93720 and Eric Metzler, 1241 Kildale Square North Columbus, OH 43229 April 30, 2004 Contributions of the C.P. Gillette Museum of Arthropod Diversity Colorado State University Cover illustration: Blueberry Sphinx (Paonias astylus (Drury)], an eastern endemic. Photo by Valeriu Albu. ISBN 1084-8819 This publication and others in the series may be ordered from the C.P. Gillette Museum of Arthropod Diversity, Department of Bioagricultural Sciences and Pest Management Colorado State University, Fort Collins, CO 80523 Abstract A list of 1531 species ofLepidoptera is presented, collected over 15 years (1988 to 2002), in eleven southern West Virginia counties. A variety of collecting methods was used, including netting, light attracting, light trapping and pheromone trapping. The specimens were identified by the currently available pictorial sources and determination keys. Many were also sent to specialists for confirmation or identification. The majority of the data was from Kanawha County, reflecting the area of more intensive sampling effort by the senior author. This imbalance of data between Kanawha County and other counties should even out with further sampling of the area. Key Words: Appalachian Mountains, -
Unit-V Evolution of Horse
UNIT-V EVOLUTION OF HORSE Horses (Equus) are odd-toed hooped mammals belong- ing to the order Perissodactyla. Horse evolution is a straight line evolution and is a suitable example for orthogenesis. It started from Eocene period. The entire evolutionary sequence of horse history is recorded in North America. " Place of Origin The place of origin of horse is North America. From here, horses migrated to Europe and Asia. By the end of Pleis- tocene period, horses became extinct in the motherland (N. America). The horses now living in N. America are the de- scendants of migrants from other continents. Time of Origin The horse evolution started some 58 million years ago, m the beginning of Eocene period of Coenozoic era. The modem horse Equus originated in Pleistocene period about 2 million years ago. Evolutionary Trends The fossils of horses that lived in different periods, show that the body parts exhibited progressive changes towards a particular direction. These directional changes are called evo- lutionary trends. The evolutionary trends of horse evolution are summarized below: 1. Increase in size. 2. Increase in the length of limbs. 3. Increase in the length of the neck. 4. Increase in the length of preorbital region (face). 5. Increase in the length and size of III digit. 6. Increase in the size and complexity of brain. 7. Molarization of premolars. Olfactory bulb Hyracotherium Mesohippus Equus Fig.: Evolution of brain in horse. 8. Development of high crowns in premolars and molars. 9. Change of plantigrade gait to unguligrade gait. 10. Formation of diastema. 11. Disappearance of lateral digits. -
Hawk Moths of North America Is Richly Illustrated with Larval Images and Contains an Abundance of Life History Information
08 caterpillars EUSA/pp244-273 3/9/05 6:37 PM Page 244 244 TULIP-TREE MOTH CECROPIA MOTH 245 Callosamia angulifera Hyalophora cecropia RECOGNITION Frosted green with shiny yellow, orange, and blue knobs over top and sides of body. RECOGNITION Much like preceding but paler or Dorsal knobs on T2, T3, and A1 somewhat globular and waxier in color with pale stripe running below set with black spinules. Paired knobs on A2–A7 more spiracles on A1–A10 and black dots on abdomen cylindrical, yellow; knob over A8 unpaired and rounded. lacking contrasting pale rings. Yellow abdominal Larva to 10cm. Caterpillars of larch-feeding Columbia tubercle over A8 short, less than twice as high as broad. Silkmoth (Hyalophora columbia) have yellow-white to Larva to 6cm. Sweetbay Silkmoth (Callosamia securifera) yellow-pink instead of bright yellow knobs over dorsum similar in appearance but a specialist on sweet bay. Its of abdomen and knobs along sides tend to be more white than blue (as in Cecropia) and are yellow abdominal tubercle over A8 is nearly three times as set in black bases (see page 246). long as wide and the red knobs over thorax are cylindrical (see page 246). OCCURRENCE Urban and suburban yards and lots, orchards, fencerows, woodlands, OCCURRENCE Woodlands and forests from Michigan, southern Ontario, and and forests from Canada south to Florida and central Texas. One generation with mature Massachusetts to northern Florida and Mississippi. One principal generation northward; caterpillars from late June through August over most of range. two broods in South with mature caterpillars from early June onward. -
Moths Taken in Berrien County, Michigan (With 102 New County Records)
The Great Lakes Entomologist Volume 6 Number 1 -- Spring 1973 Number 1 -- Spring Article 8 1973 May 1973 Moths Taken in Berrien County, Michigan (with 102 New County Records) Russell A. Rahn Follow this and additional works at: https://scholar.valpo.edu/tgle Part of the Entomology Commons Recommended Citation Rahn, Russell A. 1973. "Moths Taken in Berrien County, Michigan (with 102 New County Records)," The Great Lakes Entomologist, vol 6 (1) Available at: https://scholar.valpo.edu/tgle/vol6/iss1/8 This Peer-Review Article is brought to you for free and open access by the Department of Biology at ValpoScholar. It has been accepted for inclusion in The Great Lakes Entomologist by an authorized administrator of ValpoScholar. For more information, please contact a ValpoScholar staff member at [email protected]. Rahn: Moths Taken in Berrien County, Michigan (with 102 New County Reco THE GREAT LAKES ENTOMOLOGIST MOTHS TAKEN IN BERRIEN COLINTY, MICHIGAN (WITH 102 NEW COUNTY RECORDS) Russell A. Rahn 314 North 5th Street, Watertown, Wisconsin 53094 Moore (1955) published a listing of the moths of Michigan, exclusive of the Tineoidea, Other writers (anon., 1968; Voss, 1970) have extended the list of Michigan records. During the fall of 1970, and through the summer of 1971, I lived in Sawyer, Berrien County and collected a number of records new for that area. At the encourage- ment of M.C. Nielsen, a listing of these records is made available. Sawyer is located in the heart of a grape growing region. An ultraviolet light trap was used for the bulk of the collecting, and grape fields were within the area in view of the collecting light. -
FM), 3-9 July, 3-10 September and 10-13 December 1990
BULLETIN OF THE ALLYN MUSEUM 3621 Bayshore Rd. Sarasota, Florida 34234 Published By Florida Museum of Natural History University of Florida Gainesville, Florida 32611 Number 133 14 June 1991 ISSN-0097-3211 THE BUTTERFLIES OF ANEGADA, BRITISH VIRGIN ISLANDS, WITH DESCRIPTIONS OF A NEW CALISTO (SATYRIDAE) AND A NEW COPAEODES (HESPERIIDAE) ENDEMIC TO THE ISLAND David Spencer Smith Hope Entomological Collections, The University Museum, Parks Road, Oxford, OX! 3PW, England. Lee D. Miller Allyn Museum of Entomology of the Florida Museum of Natural History, 3621 Bay Shore Road, Sarasota, Florida 34234, U.S.A. Faustino KcKenzie Institute of Neurobiology, University of Puerto Rico, Boulevard del Valle 201, Old San Juan, Puerto Rico 00901, U.S.A. This paper is dedicated to the memory of John Griffith of Jesus College, Oxford. INTRODUCTION Anegada island is the northernmost member of the Lesser Antillean arc, situated at 18" 43'N and 64" 19'W. Its nearest neighbors are Anguilla, about 80 statute miles (127 km} across the Anegada Passage to the east-southeast and Virgin Gorda, about 13 miles (21 km} due south. Whereas the Virgin Islands are generally mountainous, Anegada reaches perhaps 18 ' above mean sea level and much of the island is considerably lower (D 'Arcy, 1975}. It is about 10 miles (16 km} in length, about 15 square miles (39 km'} in area, oriented along the east-west axis and is just over 2 miles (3.5 km} across the widest point (Fig. 16}. From the south coast and into the Anegada Passage to the southeast extends the Horseshoe Reef, long a hazard to navigation. -
Geologic Map of the Victoria Quadrangle (H02), Mercury
H01 - Borealis Geologic Map of the Victoria Quadrangle (H02), Mercury 60° Geologic Units Borea 65° Smooth plains material 1 1 2 3 4 1,5 sp H05 - Hokusai H04 - Raditladi H03 - Shakespeare H02 - Victoria Smooth and sparsely cratered planar surfaces confined to pools found within crater materials. Galluzzi V. , Guzzetta L. , Ferranti L. , Di Achille G. , Rothery D. A. , Palumbo P. 30° Apollonia Liguria Caduceata Aurora Smooth plains material–northern spn Smooth and sparsely cratered planar surfaces confined to the high-northern latitudes. 1 INAF, Istituto di Astrofisica e Planetologia Spaziali, Rome, Italy; 22.5° Intermediate plains material 2 H10 - Derain H09 - Eminescu H08 - Tolstoj H07 - Beethoven H06 - Kuiper imp DiSTAR, Università degli Studi di Napoli "Federico II", Naples, Italy; 0° Pieria Solitudo Criophori Phoethontas Solitudo Lycaonis Tricrena Smooth undulating to planar surfaces, more densely cratered than the smooth plains. 3 INAF, Osservatorio Astronomico di Teramo, Teramo, Italy; -22.5° Intercrater plains material 4 72° 144° 216° 288° icp 2 Department of Physical Sciences, The Open University, Milton Keynes, UK; ° Rough or gently rolling, densely cratered surfaces, encompassing also distal crater materials. 70 60 H14 - Debussy H13 - Neruda H12 - Michelangelo H11 - Discovery ° 5 3 270° 300° 330° 0° 30° spn Dipartimento di Scienze e Tecnologie, Università degli Studi di Napoli "Parthenope", Naples, Italy. Cyllene Solitudo Persephones Solitudo Promethei Solitudo Hermae -30° Trismegisti -65° 90° 270° Crater Materials icp H15 - Bach Australia Crater material–well preserved cfs -60° c3 180° Fresh craters with a sharp rim, textured ejecta blanket and pristine or sparsely cratered floor. 2 1:3,000,000 ° c2 80° 350 Crater material–degraded c2 spn M c3 Degraded craters with a subdued rim and a moderately cratered smooth to hummocky floor. -
Thirty-Six Dramatic Situations
G o zzi m a int a ine d th a t th ere ca n b e but thirty- six tra gic s a o s . e oo ea a s t o find o e h e was itu ti n Schill r t k gr t p in " m r , but e e . un abl e t o find eve n so m any as G ozzi . G o th Th e Thirty - Six Dram atic Situ ations GE ORGES POLTI Transl a ted by Lucil e R ay a o Fr nklin , Ohi J A M ES K NAPP H E R V E 1 9 2 4 PY H 1 9 1 6 1 9 1 7 CO RI G T , , T H E E D ITO R CO M PAN Y P H 1 92 1 CO YRI G T , JAM E S KN APP R E E VE 2 839 6 T H E T H I R TY - SI X D R AMAT I C SITUAT I ONS I NTR OD U CTI ON G o zzi m a int a in ed th a t th ere can b e but thirty - six tra gic s a o s . e o o ea a s t o fin o e h e itu ti n Schill r t k gr t p in d m r , but was a e s s un bl t o find even o m a ny a G o zzi . - Th irty six situations only ! There is , to me , some a thing t ntalizing about the assertion , unaccompanied as it is by any explanation either from Gozzi , or from Goethe or Schiller , and presenting a problem which it does not solve . -
Lista Taxonómica Actualizada De Los Esfíngidos De Cuba (Lepidoptera)
Lista taxonómica actualizada de los esfíngidos de Cuba (Lepidoptera) Alfonso Iorio [email protected] La última y más reciente clasificacion taxonómica (la misma que adopté en mi libro sobre los esfíngidos de Ecuador: “Mariposas del Ecuador. Sphingidae”) es de Kitching & Cadiou (2000). Así, la familia contiene las siguentes agrupaciones: Familia: Sphingidae Latreille, [1802] Subfamilia: Smerinthinae Grote & Robinson, 1865 Tribu: Smerinthini Grote & Robinson, 1865 Sphingulini Rothschild & Jordan, 1903 Ambulycini Butler, 1876 Subfamilia: Sphinginae Latreille, [1802] Tribu: Sphingini Latreille, [1802] Acherontiini Boisduval, [1875] Subfamilia: Macroglossinae Harris, 1839 Tribu: Dilophonotini Burmeister, 1878 Subtribu: Dilophonotina Burmeister, 1878 Hemarina Tutt, 1902 Tribu : Philampelini Burmeister, 1878 Macroglossini Harris, 1839 Subtribu: Macroglossina Harris, 1839 Choerocampina Grote & Robinson, 1865 Subfamilias, tribus y subtribus que se encuentran en Cuba: Familia: Sphingidae Latreille, [1802] Subfamilia: Smerinthinae Grote & Robinson, 1865 Tribu: Ambulycini Butler, 1876 Protambulyx strigilis (L., 1771) Adhemarius gannascus cubanus (Rothschild & Jordan, 1908) Subfamilia: Sphinginae Latreille, [1802] Tribu: Sphingini Latreille, [1802] Nannoparce poeyi (Grote, 1865) Manduca afflicta (Grote, 1865) Manduca brontes cubensis (Grote, 1865) Manduca quinquemaculatus (Haworth, 1803) Manduca rustica cubana (Wood, 1915) Manduca sexta jamaicensis (Butler, 1875) Neococytius cluentius (Cramer, 1775) Cocytius antaeus (Drury, 1773) Cocytius duponchel -
CHECKLIST of WISCONSIN MOTHS (Superfamilies Mimallonoidea, Drepanoidea, Lasiocampoidea, Bombycoidea, Geometroidea, and Noctuoidea)
WISCONSIN ENTOMOLOGICAL SOCIETY SPECIAL PUBLICATION No. 6 JUNE 2018 CHECKLIST OF WISCONSIN MOTHS (Superfamilies Mimallonoidea, Drepanoidea, Lasiocampoidea, Bombycoidea, Geometroidea, and Noctuoidea) Leslie A. Ferge,1 George J. Balogh2 and Kyle E. Johnson3 ABSTRACT A total of 1284 species representing the thirteen families comprising the present checklist have been documented in Wisconsin, including 293 species of Geometridae, 252 species of Erebidae and 584 species of Noctuidae. Distributions are summarized using the six major natural divisions of Wisconsin; adult flight periods and statuses within the state are also reported. Examples of Wisconsin’s diverse native habitat types in each of the natural divisions have been systematically inventoried, and species associated with specialized habitats such as peatland, prairie, barrens and dunes are listed. INTRODUCTION This list is an updated version of the Wisconsin moth checklist by Ferge & Balogh (2000). A considerable amount of new information from has been accumulated in the 18 years since that initial publication. Over sixty species have been added, bringing the total to 1284 in the thirteen families comprising this checklist. These families are estimated to comprise approximately one-half of the state’s total moth fauna. Historical records of Wisconsin moths are relatively meager. Checklists including Wisconsin moths were compiled by Hoy (1883), Rauterberg (1900), Fernekes (1906) and Muttkowski (1907). Hoy's list was restricted to Racine County, the others to Milwaukee County. Records from these publications are of historical interest, but unfortunately few verifiable voucher specimens exist. Unverifiable identifications and minimal label data associated with older museum specimens limit the usefulness of this information. Covell (1970) compiled records of 222 Geometridae species, based on his examination of specimens representing at least 30 counties. -
Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals Willow H
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences 7-2017 Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals Willow H. Nguy University of Nebraska-Lincoln, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Paleobiology Commons, and the Paleontology Commons Nguy, Willow H., "Middle Miocene Paleoenvironmental Reconstruction of the Central Great Plains from Stable Carbon Isotopes in Large Mammals" (2017). Dissertations & Theses in Earth and Atmospheric Sciences. 91. http://digitalcommons.unl.edu/geoscidiss/91 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. MIDDLE MIOCENE PALEOENVIRONMENTAL RECONSTRUCTION OF THE CENTRAL GREAT PLAINS FROM STABLE CARBON ISOTOPES IN LARGE MAMMALS by Willow H. Nguy A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Ross Secord Lincoln, Nebraska July, 2017 MIDDLE MIOCENE PALEOENVIRONMENTAL RECONSTRUCTION OF THE CENTRAL GREAT PLAINS FROM STABLE CARBON ISOTOPES IN LARGE MAMMALS Willow H. Nguy, M.S. University of Nebraska, 2017 Advisor: Ross Secord Middle Miocene (18-12 Mya) mammalian faunas of the North American Great Plains contained a much higher diversity of apparent browsers than any modern biome. -
Large Impact Basins on Mercury: Global Distribution, Characteristics, and Modification History from MESSENGER Orbital Data Caleb I
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117, E00L08, doi:10.1029/2012JE004154, 2012 Large impact basins on Mercury: Global distribution, characteristics, and modification history from MESSENGER orbital data Caleb I. Fassett,1 James W. Head,2 David M. H. Baker,2 Maria T. Zuber,3 David E. Smith,3,4 Gregory A. Neumann,4 Sean C. Solomon,5,6 Christian Klimczak,5 Robert G. Strom,7 Clark R. Chapman,8 Louise M. Prockter,9 Roger J. Phillips,8 Jürgen Oberst,10 and Frank Preusker10 Received 6 June 2012; revised 31 August 2012; accepted 5 September 2012; published 27 October 2012. [1] The formation of large impact basins (diameter D ≥ 300 km) was an important process in the early geological evolution of Mercury and influenced the planet’s topography, stratigraphy, and crustal structure. We catalog and characterize this basin population on Mercury from global observations by the MESSENGER spacecraft, and we use the new data to evaluate basins suggested on the basis of the Mariner 10 flybys. Forty-six certain or probable impact basins are recognized; a few additional basins that may have been degraded to the point of ambiguity are plausible on the basis of new data but are classified as uncertain. The spatial density of large basins (D ≥ 500 km) on Mercury is lower than that on the Moon. Morphological characteristics of basins on Mercury suggest that on average they are more degraded than lunar basins. These observations are consistent with more efficient modification, degradation, and obliteration of the largest basins on Mercury than on the Moon. This distinction may be a result of differences in the basin formation process (producing fewer rings), relaxation of topography after basin formation (subduing relief), or rates of volcanism (burying basin rings and interiors) during the period of heavy bombardment on Mercury from those on the Moon.