Quantification of the Position and Depth of the Flexor Hallucis Longus Groove in Euarchontans, with Implications for the Evolution of Primate Positional Behavior
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Iliopsoas Tendonitis/Bursitis Exercises
ILIOPSOAS TENDONITIS / BURSITIS What is the Iliopsoas and Bursa? The iliopsoas is a muscle that runs from your lower back through the pelvis to attach to a small bump (the lesser trochanter) on the top portion of the thighbone near your groin. This muscle has the important job of helping to bend the hip—it helps you to lift your leg when going up and down stairs or to start getting out of a car. A fluid-filled sac (bursa) helps to protect and allow the tendon to glide during these movements. The iliopsoas tendon can become inflamed or overworked during repetitive activities. The tendon can also become irritated after hip replacement surgery. Signs and Symptoms Iliopsoas issues may feel like “a pulled groin muscle”. The main symptom is usually a catch during certain movements such as when trying to put on socks or rising from a seated position. You may find yourself leading with your other leg when going up the stairs to avoid lifting the painful leg. The pain may extend from the groin to the inside of the thigh area. Snapping or clicking within the front of the hip can also be experienced. Do not worry this is not your hip trying to pop out of socket but it is usually the iliopsoas tendon rubbing over the hip joint or pelvis. Treatment Conservative treatment in the form of stretching and strengthening usually helps with the majority of patients with iliopsoas bursitis. This issue is the result of soft tissue inflammation, therefore rest, ice, anti- inflammatory medications, physical therapy exercises, and/or injections are effective treatment options. -
The World at the Time of Messel: Conference Volume
T. Lehmann & S.F.K. Schaal (eds) The World at the Time of Messel - Conference Volume Time at the The World The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment and the History of Early Primates 22nd International Senckenberg Conference 2011 Frankfurt am Main, 15th - 19th November 2011 ISBN 978-3-929907-86-5 Conference Volume SENCKENBERG Gesellschaft für Naturforschung THOMAS LEHMANN & STEPHAN F.K. SCHAAL (eds) The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference Frankfurt am Main, 15th – 19th November 2011 Conference Volume Senckenberg Gesellschaft für Naturforschung IMPRINT The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates 22nd International Senckenberg Conference 15th – 19th November 2011, Frankfurt am Main, Germany Conference Volume Publisher PROF. DR. DR. H.C. VOLKER MOSBRUGGER Senckenberg Gesellschaft für Naturforschung Senckenberganlage 25, 60325 Frankfurt am Main, Germany Editors DR. THOMAS LEHMANN & DR. STEPHAN F.K. SCHAAL Senckenberg Research Institute and Natural History Museum Frankfurt Senckenberganlage 25, 60325 Frankfurt am Main, Germany [email protected]; [email protected] Language editors JOSEPH E.B. HOGAN & DR. KRISTER T. SMITH Layout JULIANE EBERHARDT & ANIKA VOGEL Cover Illustration EVELINE JUNQUEIRA Print Rhein-Main-Geschäftsdrucke, Hofheim-Wallau, Germany Citation LEHMANN, T. & SCHAAL, S.F.K. (eds) (2011). The World at the Time of Messel: Puzzles in Palaeobiology, Palaeoenvironment, and the History of Early Primates. 22nd International Senckenberg Conference. 15th – 19th November 2011, Frankfurt am Main. Conference Volume. Senckenberg Gesellschaft für Naturforschung, Frankfurt am Main. pp. 203. -
Strain Assessment of Deep Fascia of the Thigh During Leg Movement
Strain Assessment of Deep Fascia of the Thigh During Leg Movement: An in situ Study Yulila Sednieva, Anthony Viste, Alexandre Naaim, Karine Bruyere-Garnier, Laure-Lise Gras To cite this version: Yulila Sednieva, Anthony Viste, Alexandre Naaim, Karine Bruyere-Garnier, Laure-Lise Gras. Strain Assessment of Deep Fascia of the Thigh During Leg Movement: An in situ Study. Frontiers in Bioengineering and Biotechnology, Frontiers, 2020, 8, 15p. 10.3389/fbioe.2020.00750. hal-02912992 HAL Id: hal-02912992 https://hal.archives-ouvertes.fr/hal-02912992 Submitted on 7 Aug 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. fbioe-08-00750 July 27, 2020 Time: 18:28 # 1 ORIGINAL RESEARCH published: 29 July 2020 doi: 10.3389/fbioe.2020.00750 Strain Assessment of Deep Fascia of the Thigh During Leg Movement: An in situ Study Yuliia Sednieva1, Anthony Viste1,2, Alexandre Naaim1, Karine Bruyère-Garnier1 and Laure-Lise Gras1* 1 Univ Lyon, Université Claude Bernard Lyon 1, Univ Gustave Eiffel, IFSTTAR, LBMC UMR_T9406, Lyon, France, 2 Hospices Civils de Lyon, Hôpital Lyon Sud, Chirurgie Orthopédique, 165, Chemin du Grand-Revoyet, Pierre-Bénite, France Fascia is a fibrous connective tissue present all over the body. -
SMC 136 Gazin 1958 1 1-112.Pdf
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 136, NUMBER 1 Cftarlesi 3B, anb JKarp "^aux OTalcott 3^es(earcf) Jf unb A REVIEW OF THE MIDDLE AND UPPER EOCENE PRIMATES OF NORTH AMERICA (With 14 Plates) By C. LEWIS GAZIN Curator, Division of Vertebrate Paleontology United States National Museum Smithsonian Institution (Publication 4340) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JULY 7, 1958 THE LORD BALTIMORE PRESS, INC. BALTIMORE, MD., U. S. A. CONTENTS Page Introduction i Acknowledgments 2 History of investigation 4 Geographic and geologic occurrence 14 Environment I7 Revision of certain lower Eocene primates and description of three new upper Wasatchian genera 24 Classification of middle and upper Eocene forms 30 Systematic revision of middle and upper Eocene primates 31 Notharctidae 31 Comparison of the skulls of Notharctus and Smilodectcs z:^ Omomyidae 47 Anaptomorphidae 7Z Apatemyidae 86 Summary of relationships of North American fossil primates 91 Discussion of platyrrhine relationships 98 References 100 Explanation of plates 108 ILLUSTRATIONS Plates (All plates follow page 112) 1. Notharctus and Smilodectes from the Bridger middle Eocene. 2. Notharctus and Smilodectes from the Bridger middle Eocene. 3. Notharctus and Smilodectcs from the Bridger middle Eocene. 4. Notharctus and Hemiacodon from the Bridger middle Eocene. 5. Notharctus and Smilodectcs from the Bridger middle Eocene. 6. Omomys from the middle and lower Eocene. 7. Omomys from the middle and lower Eocene. 8. Hemiacodon from the Bridger middle Eocene. 9. Washakius from the Bridger middle Eocene. 10. Anaptomorphus and Uintanius from the Bridger middle Eocene. 11. Trogolemur, Uintasorex, and Apatcmys from the Bridger middle Eocene. 12. Apatemys from the Bridger middle Eocene. -
8. Primate Evolution
8. Primate Evolution Jonathan M. G. Perry, Ph.D., The Johns Hopkins University School of Medicine Stephanie L. Canington, B.A., The Johns Hopkins University School of Medicine Learning Objectives • Understand the major trends in primate evolution from the origin of primates to the origin of our own species • Learn about primate adaptations and how they characterize major primate groups • Discuss the kinds of evidence that anthropologists use to find out how extinct primates are related to each other and to living primates • Recognize how the changing geography and climate of Earth have influenced where and when primates have thrived or gone extinct The first fifty million years of primate evolution was a series of adaptive radiations leading to the diversification of the earliest lemurs, monkeys, and apes. The primate story begins in the canopy and understory of conifer-dominated forests, with our small, furtive ancestors subsisting at night, beneath the notice of day-active dinosaurs. From the archaic plesiadapiforms (archaic primates) to the earliest groups of true primates (euprimates), the origin of our own order is characterized by the struggle for new food sources and microhabitats in the arboreal setting. Climate change forced major extinctions as the northern continents became increasingly dry, cold, and seasonal and as tropical rainforests gave way to deciduous forests, woodlands, and eventually grasslands. Lemurs, lorises, and tarsiers—once diverse groups containing many species—became rare, except for lemurs in Madagascar where there were no anthropoid competitors and perhaps few predators. Meanwhile, anthropoids (monkeys and apes) emerged in the Old World, then dispersed across parts of the northern hemisphere, Africa, and ultimately South America. -
Fossil Primates
AccessScience from McGraw-Hill Education Page 1 of 16 www.accessscience.com Fossil primates Contributed by: Eric Delson Publication year: 2014 Extinct members of the order of mammals to which humans belong. All current classifications divide the living primates into two major groups (suborders): the Strepsirhini or “lower” primates (lemurs, lorises, and bushbabies) and the Haplorhini or “higher” primates [tarsiers and anthropoids (New and Old World monkeys, greater and lesser apes, and humans)]. Some fossil groups (omomyiforms and adapiforms) can be placed with or near these two extant groupings; however, there is contention whether the Plesiadapiformes represent the earliest relatives of primates and are best placed within the order (as here) or outside it. See also: FOSSIL; MAMMALIA; PHYLOGENY; PHYSICAL ANTHROPOLOGY; PRIMATES. Vast evidence suggests that the order Primates is a monophyletic group, that is, the primates have a common genetic origin. Although several peculiarities of the primate bauplan (body plan) appear to be inherited from an inferred common ancestor, it seems that the order as a whole is characterized by showing a variety of parallel adaptations in different groups to a predominantly arboreal lifestyle, including anatomical and behavioral complexes related to improved grasping and manipulative capacities, a variety of locomotor styles, and enlargement of the higher centers of the brain. Among the extant primates, the lower primates more closely resemble forms that evolved relatively early in the history of the order, whereas the higher primates represent a group that evolved more recently (Fig. 1). A classification of the primates, as accepted here, appears above. Early primates The earliest primates are placed in their own semiorder, Plesiadapiformes (as contrasted with the semiorder Euprimates for all living forms), because they have no direct evolutionary links with, and bear few adaptive resemblances to, any group of living primates. -
Hamstring Muscle Injuries
DISEASES & CONDITIONS Hamstring Muscle Injuries Hamstring muscle injuries — such as a "pulled hamstring" — occur frequently in athletes. They are especially common in athletes who participate in sports that require sprinting, such as track, soccer, and basketball. A pulled hamstring or strain is an injury to one or more of the muscles at the back of the thigh. Most hamstring injuries respond well to simple, nonsurgical treatments. Anatomy The hamstring muscles run down the back of the thigh. There are three hamstring muscles: Semitendinosus Semimembranosus Biceps femoris They start at the bottom of the pelvis at a place called the ischial tuberosity. They cross the knee joint and end at the lower leg. Hamstring muscle fibers join with the tough, connective tissue of the hamstring tendons near the points where the tendons attach to bones. The hamstring muscle group helps you extend your leg straight back and bend your knee. Normal hamstring anatomy. The three hamstring muscles start at the bottom of the pelvis and end near the top of the lower leg. Description A hamstring strain can be a pull, a partial tear, or a complete tear. Muscle strains are graded according to their severity. A grade 1 strain is mild and usually heals readily; a grade 3 strain is a complete tear of the muscle that may take months to heal. Most hamstring injuries occur in the thick, central part of the muscle or where the muscle fibers join tendon fibers. In the most severe hamstring injuries, the tendon tears completely away from the bone. It may even pull a piece of bone away with it. -
Stem Members of Platyrrhini Are Distinct from Catarrhines in at Least One Derived Cranial Feature
Journal of Human Evolution 100 (2016) 16e24 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Stem members of Platyrrhini are distinct from catarrhines in at least one derived cranial feature * Ethan L. Fulwood a, , Doug M. Boyer a, Richard F. Kay a, b a Department of Evolutionary Anthropology, Duke University, Box 90383, Durham, NC 27708, USA b Division of Earth and Ocean Sciences, Nicholas School of the Environment, Duke University, Durham, NC 27708, USA article info abstract Article history: The pterion, on the lateral aspect of the cranium, is where the zygomatic, frontal, sphenoid, squamosal, Received 3 August 2015 and parietal bones approach and contact. The configuration of these bones distinguishes New and Old Accepted 2 August 2016 World anthropoids: most extant platyrrhines exhibit contact between the parietal and zygomatic bones, while all known catarrhines exhibit frontal-alisphenoid contact. However, it is thought that early stem- platyrrhines retained the apparently primitive catarrhine condition. Here we re-evaluate the condition of Keywords: key fossil taxa using mCT (micro-computed tomography) imaging. The single known specimen of New World monkeys Tremacebus and an adult cranium of Antillothrix exhibit the typical platyrrhine condition of parietal- Pterion Homunculus zygomatic contact. The same is true of one specimen of Homunculus, while a second specimen has the ‘ ’ Tremacebus catarrhine condition. When these new data are incorporated into an ancestral state reconstruction, they MicroCT support the conclusion that pterion frontal-alisphenoid contact characterized the last common ancestor of crown anthropoids and that contact between the parietal and zygomatic is a synapomorphy of Platyrrhini. -
Early Eocene Primates from Gujarat, India
ARTICLE IN PRESS Journal of Human Evolution xxx (2009) 1–39 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Early Eocene Primates from Gujarat, India Kenneth D. Rose a,*, Rajendra S. Rana b, Ashok Sahni c, Kishor Kumar d, Pieter Missiaen e, Lachham Singh b, Thierry Smith f a Johns Hopkins University School of Medicine, Baltimore, Maryland 21205, USA b H.N.B. Garhwal University, Srinagar 246175, Uttarakhand, India c Panjab University, Chandigarh 160014, India d Wadia Institute of Himalayan Geology, Dehradun 248001, Uttarakhand, India e University of Ghent, B-9000 Ghent, Belgium f Royal Belgian Institute of Natural Sciences, B-1000 Brussels, Belgium article info abstract Article history: The oldest euprimates known from India come from the Early Eocene Cambay Formation at Vastan Mine Received 24 June 2008 in Gujarat. An Ypresian (early Cuisian) age of w53 Ma (based on foraminifera) indicates that these Accepted 8 January 2009 primates were roughly contemporary with, or perhaps predated, the India-Asia collision. Here we present new euprimate fossils from Vastan Mine, including teeth, jaws, and referred postcrania of the Keywords: adapoids Marcgodinotius indicus and Asiadapis cambayensis. They are placed in the new subfamily Eocene Asiadapinae (family Notharctidae), which is most similar to primitive European Cercamoniinae such as India Donrussellia and Protoadapis. Asiadapines were small primates in the size range of extant smaller Notharctidae Adapoidea bushbabies. Despite their generally very plesiomorphic morphology, asiadapines also share a few derived Omomyidae dental traits with sivaladapids, suggesting a possible relationship to these endemic Asian adapoids. In Eosimiidae addition to the adapoids, a new species of the omomyid Vastanomys is described. -
Back of Thigh
Back of thigh Dr Garima Sehgal Associate Professor King George’s Medical University UP, Lucknow DISCLAIMER: • The presentation includes images which have been taken from google images or books. • The author of the presentation claims no personal ownership over these images taken from books or google images. • They are being used in the presentation only for educational purpose. Learning Objectives By the end of this teaching session on back of thigh – I all the MBBS 1st year students must be able to: • Enumerate the contents of posterior compartment of thigh • Describe the cutaneous innervation of skin of back of thigh • Enumerate the hamstring muscles • List the criteria for inclusion of muscles as hamstring muscles • Describe the origin, insertion, nerve supply & actions of hamstring muscles • Describe origin, course and branches of sciatic nerve • Write a short note on posterior cutaneous nerve of thigh • Write a note on arteries and arterial anastomosis at the back of thigh • Discuss applied anatomy of back of thigh Compartments of the thigh Cutaneous innervation of back of thigh 1 4 2 3 Contents of Back of thigh Muscles: Hamstring muscles & short head of biceps femoris Nerves: Sciatic nerve & posterior cutaneous nerve of thigh Arterial Anastomosis: The Posterior Femoral Cutaneous Nerve (n. cutaneus femoralis posterior) Dorsal divisions of – S1, S2 & Ventral divisions of S2, S3 Exits from pelvis through the greater sciatic foramen below the Piriformis. Descends beneath the Gluteus maximus with the inferior gluteal artery Runs down the back of the thigh beneath the fascia lata, to the back of the knee and leg Posterior Femoral Cutaneous Nerve contd…. -
Anthroquest the Newsletter of the Leakey Foundation
no. 35 Spring/Summer 2017 AnthroQuest The Newsletter of The Leakey Foundation Leakey Grantee Finds Oldest Primates of India THIERRY SMITH, LEAKEY FOUNDATION GRANTEE, ROYAL BELGIAN INSTITUTE OF NATURAL SCIENCES n 2004, Professor Kenneth D. Rose from John Hopkins I University invited me to lead a small team of paleontologists planning to explore lignite (brown coal) mines in India. The goal was to prospect for Paleocene-Eocene deposits (66-34 million years ago), which could yield ancient terrestrial mammals. Ken thought the screen-washing technique we used to find small fossil mammals in Wyoming would work well in India. I went to Mumbai with a student, Pieter Missiaen, and we travelled about 250 mile north to the Vastan mine in Thierry Smith screenwashing sediments for small remains of earliest Indian primates Gujarat to meet our Indian colleagues Photo: Annelise Folie for the first time. I remember well that on the second day in the mine, it was a mammal incisor the size of a human million years old). We published this hot, and I was nervous because we were incisor. It was the beginning of our jaw with four teeth under the new name six persons sharing only two hammers Indian adventure! Asiadapis cambayensis, and today this to look for fossils in a sticky clay layer. specimen is the reference of the family This deposit was so rich that we Asiadapidae. I suggested to my colleague, Professor collected all the matrix and screen- Rajendra Singh Rana, that he ask a washed it completely. Each sieve The Vastan mine was a paradise for miner to remove the lignite layer above contained small mammal teeth or paleontologists. -
Primates, Adapiformes) Skull from the Uintan (Middle Eocene) of San Diego County, California
AMERICAN JOURNAL OF PHYSICAL ANTHROPOLOGY 98:447-470 (1995 New Notharctine (Primates, Adapiformes) Skull From the Uintan (Middle Eocene) of San Diego County, California GREGG F. GUNNELL Museum of Paleontology, University of Michigan, Ann Arbor, Michigan 481 09-1079 KEY WORDS Californian primates, Cranial morphology, Haplorhine-strepsirhine dichotomy ABSTRACT A new genus and species of notharctine primate, Hespero- lemur actius, is described from Uintan (middle Eocene) aged rocks of San Diego County, California. Hesperolemur differs from all previously described adapiforms in having the anterior third of the ectotympanic anulus fused to the internal lateral wall of the auditory bulla. In this feature Hesperolemur superficially resembles extant cheirogaleids. Hesperolemur also differs from previously known adapiforms in lacking bony canals that transmit the inter- nal carotid artery through the tympanic cavity. Hesperolemur, like the later occurring North American cercamoniine Mahgarita steuensi, appears to have lacked a stapedial artery. Evidence from newly discovered skulls ofNotharctus and Smilodectes, along with Hesperolemur, Mahgarita, and Adapis, indicates that the tympanic arterial circulatory pattern of these adapiforms is charac- terized by stapedial arteries that are smaller than promontory arteries, a feature shared with extant tarsiers and anthropoids and one of the character- istics often used to support the existence of a haplorhine-strepsirhine dichot- omy among extant primates. The existence of such a dichotomy among Eocene primates is not supported by any compelling evidence. Hesperolemur is the latest occurring notharctine primate known from North America and is the only notharctine represented among a relatively diverse primate fauna from southern California. The coastal lowlands of southern California presumably served as a refuge area for primates during the middle and later Eocene as climates deteriorated in the continental interior.