A Neglected Part of the Mammalian Skull: the Outer Nasal Cartilages As Progressive Remnants of the Chondrocranium
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The Mammary Gland and Its Origin During Synapsid Evolution
P1: GMX Journal of Mammary Gland Biology and Neoplasia (JMGBN) pp749-jmgbn-460568 January 9, 2003 17:51 Style file version Nov. 07, 2000 Journal of Mammary Gland Biology and Neoplasia, Vol. 7, No. 3, July 2002 (C 2002) The Mammary Gland and Its Origin During Synapsid Evolution Olav T. Oftedal1 Lactation appears to be an ancient reproductive trait that predates the origin of mammals. The synapsid branch of the amniote tree that separated from other taxa in the Pennsylva- nian (>310 million years ago) evolved a glandular rather than scaled integument. Repeated radiations of synapsids produced a gradual accrual of mammalian features. The mammary gland apparently derives from an ancestral apocrine-like gland that was associated with hair follicles. This association is retained by monotreme mammary glands and is evident as ves- tigial mammary hair during early ontogenetic development of marsupials. The dense cluster of mammo-pilo-sebaceous units that open onto a nipple-less mammary patch in monotremes may reflect a structure that evolved to provide moisture and other constituents to permeable eggs. Mammary patch secretions were coopted to provide nutrients to hatchlings, but some constituents including lactose may have been secreted by ancestral apocrine-like glands in early synapsids. Advanced Triassic therapsids, such as cynodonts, almost certainly secreted complex, nutrient-rich milk, allowing a progressive decline in egg size and an increasingly altricial state of the young at hatching. This is indicated by the very small body size, presence of epipubic bones, and limited tooth replacement in advanced cynodonts and early mammali- aforms. Nipples that arose from the mammary patch rendered mammary hairs obsolete, while placental structures have allowed lactation to be truncated in living eutherians. -
Molecular Phylogeny of Mobatviruses (Hantaviridae) in Myanmar and Vietnam
viruses Article Molecular Phylogeny of Mobatviruses (Hantaviridae) in Myanmar and Vietnam Satoru Arai 1, Fuka Kikuchi 1,2, Saw Bawm 3 , Nguyễn Trường Sơn 4,5, Kyaw San Lin 6, Vương Tân Tú 4,5, Keita Aoki 1,7, Kimiyuki Tsuchiya 8, Keiko Tanaka-Taya 1, Shigeru Morikawa 9, Kazunori Oishi 1 and Richard Yanagihara 10,* 1 Infectious Disease Surveillance Center, National Institute of Infectious Diseases, Tokyo 162-8640, Japan; [email protected] (S.A.); [email protected] (F.K.); [email protected] (K.A.); [email protected] (K.T.-T.); [email protected] (K.O.) 2 Department of Chemistry, Faculty of Science, Tokyo University of Science, Tokyo 162-8601, Japan 3 Department of Pharmacology and Parasitology, University of Veterinary Science, Yezin, Nay Pyi Taw 15013, Myanmar; [email protected] 4 Institute of Ecology and Biological Resources, Vietnam Academy of Science and Technology, Hanoi, Vietnam; [email protected] (N.T.S.); [email protected] (V.T.T.) 5 Graduate University of Science and Technology, Vietnam Academy of Science and Technology, Hanoi, Vietnam 6 Department of Aquaculture and Aquatic Disease, University of Veterinary Science, Yezin, Nay Pyi Taw 15013, Myanmar; [email protected] 7 Department of Liberal Arts, Faculty of Science, Tokyo University of Science, Tokyo 162-8601, Japan 8 Laboratory of Bioresources, Applied Biology Co., Ltd., Tokyo 107-0062, Japan; [email protected] 9 Department of Veterinary Science, National Institute of Infectious Diseases, Tokyo 162-8640, Japan; [email protected] 10 Pacific Center for Emerging Infectious Diseases Research, John A. -
When Beremendiin Shrews Disappeared in East Asia, Or How We Can Estimate Fossil Redeposition
Historical Biology An International Journal of Paleobiology ISSN: (Print) (Online) Journal homepage: https://www.tandfonline.com/loi/ghbi20 When beremendiin shrews disappeared in East Asia, or how we can estimate fossil redeposition Leonid L. Voyta , Valeriya E. Omelko , Mikhail P. Tiunov & Maria A. Vinokurova To cite this article: Leonid L. Voyta , Valeriya E. Omelko , Mikhail P. Tiunov & Maria A. Vinokurova (2020): When beremendiin shrews disappeared in East Asia, or how we can estimate fossil redeposition, Historical Biology, DOI: 10.1080/08912963.2020.1822354 To link to this article: https://doi.org/10.1080/08912963.2020.1822354 Published online: 22 Sep 2020. Submit your article to this journal View related articles View Crossmark data Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 HISTORICAL BIOLOGY https://doi.org/10.1080/08912963.2020.1822354 ARTICLE When beremendiin shrews disappeared in East Asia, or how we can estimate fossil redeposition Leonid L. Voyta a, Valeriya E. Omelko b, Mikhail P. Tiunovb and Maria A. Vinokurova b aLaboratory of Theriology, Zoological Institute, Russian Academy of Sciences, Saint Petersburg, Russia; bFederal Scientific Center of the East Asia Terrestrial Biodiversity, Far Eastern Branch of Russian Academy of Sciences, Vladivostok, Russia ABSTRACT ARTICLE HISTORY The current paper first time describes a small Beremendia from the late Pleistocene deposits in the Received 24 July 2020 Koridornaya Cave locality (Russian Far East), which associated with the extinct Beremendia minor. The Accepted 8 September 2020 paper is the first attempt to use a comparative analytical method to evaluate a possible case of redeposition KEYWORDS of fossil remains of this shrew. -
The Mesozoic Era Alvarez, W.(1997)
Alles Introductory Biology: Illustrated Lecture Presentations Instructor David L. Alles Western Washington University ----------------------- Part Three: The Integration of Biological Knowledge Vertebrate Evolution in the Late Paleozoic and Mesozoic Eras ----------------------- Vertebrate Evolution in the Late Paleozoic and Mesozoic • Amphibians to Reptiles Internal Fertilization, the Amniotic Egg, and a Water-Tight Skin • The Adaptive Radiation of Reptiles from Scales to Hair and Feathers • Therapsids to Mammals • Dinosaurs to Birds Ectothermy to Endothermy The Evolution of Reptiles The Phanerozoic Eon 444 365 251 Paleozoic Era 542 m.y.a. 488 416 360 299 Camb. Ordov. Sil. Devo. Carbon. Perm. Cambrian Pikaia Fish Fish First First Explosion w/o jaws w/ jaws Amphibians Reptiles 210 65 Mesozoic Era 251 200 180 150 145 Triassic Jurassic Cretaceous First First First T. rex Dinosaurs Mammals Birds Cenozoic Era Last Ice Age 65 56 34 23 5 1.8 0.01 Paleo. Eocene Oligo. Miocene Plio. Ple. Present Early Primate First New First First Modern Cantius World Monkeys Apes Hominins Humans A modern Amphibian—the toad A modern day Reptile—a skink, note the finely outlined scales. A Comparison of Amphibian and Reptile Reproduction The oldest known reptile is Hylonomus lyelli dating to ~ 320 m.y.a.. The earliest or stem reptiles radiated into therapsids leading to mammals, and archosaurs leading to all the other reptile groups including the thecodontians, ancestors of the dinosaurs. Dimetrodon, a Mammal-like Reptile of the Early Permian Dicynodonts were a group of therapsids of the late Permian. Web Reference http://www.museums.org.za/sam/resource/palaeo/cluver/index.html Therapsids experienced an adaptive radiation during the Permian, but suffered heavy extinctions during the end Permian mass extinction. -
Solenodon Genome Reveals Convergent Evolution of Venom in Eulipotyphlan Mammals
Solenodon genome reveals convergent evolution of venom in eulipotyphlan mammals Nicholas R. Casewella,1, Daniel Petrasb,c, Daren C. Cardd,e,f, Vivek Suranseg, Alexis M. Mychajliwh,i,j, David Richardsk,l, Ivan Koludarovm, Laura-Oana Albulescua, Julien Slagboomn, Benjamin-Florian Hempelb, Neville M. Ngumk, Rosalind J. Kennerleyo, Jorge L. Broccap, Gareth Whiteleya, Robert A. Harrisona, Fiona M. S. Boltona, Jordan Debonoq, Freek J. Vonkr, Jessica Alföldis, Jeremy Johnsons, Elinor K. Karlssons,t, Kerstin Lindblad-Tohs,u, Ian R. Mellork, Roderich D. Süssmuthb, Bryan G. Fryq, Sanjaya Kuruppuv,w, Wayne C. Hodgsonv, Jeroen Kooln, Todd A. Castoed, Ian Barnesx, Kartik Sunagarg, Eivind A. B. Undheimy,z,aa, and Samuel T. Turveybb aCentre for Snakebite Research & Interventions, Liverpool School of Tropical Medicine, Pembroke Place, L3 5QA Liverpool, United Kingdom; bInstitut für Chemie, Technische Universität Berlin, 10623 Berlin, Germany; cCollaborative Mass Spectrometry Innovation Center, University of California, San Diego, La Jolla, CA 92093; dDepartment of Biology, University of Texas at Arlington, Arlington, TX 76010; eDepartment of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA 02138; fMuseum of Comparative Zoology, Harvard University, Cambridge, MA 02138; gEvolutionary Venomics Lab, Centre for Ecological Sciences, Indian Institute of Science, 560012 Bangalore, India; hDepartment of Biology, Stanford University, Stanford, CA 94305; iDepartment of Rancho La Brea, Natural History Museum of Los Angeles County, Los Angeles, -
Mammal Evolution
Mammal Evolution Geology 331 Paleontology Triassic synapsid reptiles: Therapsids or mammal-like reptiles. Note the sprawling posture. Mammal with Upright Posture From Synapsids to Mammals, a well documented transition series Carl Buell Prothero, 2007 Synapsid Teeth, less specialized Mammal Teeth, more specialized Prothero, 2007 Yanoconodon, Lower Cretaceous of China Yanoconodon, Lower Cretaceous of China, retains ear bones attached to the inside lower jaw Morganucodon Yanoconodon = articular of = quadrate of Human Ear Bones, or lower reptile upper reptile Auditory Ossicles jaw jaw Cochlea Mammals have a bony secondary palate Primary Palate Reptiles have a soft Secondary Palate secondary palate Reduction of digit bones from Hand and Foot of Permian Synapsid 2-3-4-5-3 in synapsid Seymouria ancestors to 2-3-3-3-3 in mammals Human Hand and Foot Class Mammalia - Late Triassic to Recent Superorder Tricodonta - Late Triassic to Late Cretaceous Superorder Multituberculata - Late Jurassic to Early Oligocene Superorder Monotremata - Early Cretaceous to Recent Superorder Metatheria (Marsupials) - Late Cretaceous to Recent Superorder Eutheria (Placentals) - Late Cretaceous to Recent Evolution of Mammalian Superorders Multituberculates Metatheria Eutheria (Marsupials) (Placentals) Tricodonts Monotremes . Live Birth Extinct: . .. Mammary Glands? Mammals in the Age of Dinosaurs – a nocturnal life style Hadrocodium, a lower Jurassic mammal with a “large” brain (6 mm brain case in an 8 mm skull) Were larger brains adaptive for a greater sense of smell? Big Brains and Early Mammals July 14, 2011 The Academic Minute http://www.insidehighered.com/audio/academic_pulse/big_brains_and_early_mammals Lower Cretaceous mammal from China Jawbones of a Cretaceous marsupial from Mongolia Mammal fossil from the Cretaceous of Mongolia Reconstructed Cretaceous Mammal Early Cretaceous mammal ate small dinosaurs Repenomamus robustus fed on psittacosaurs. -
A New Mammaliaform from the Early Jurassic and Evolution Of
R EPORTS tary trough with a shelflike dorsal medial ridge, and all other nonmammalian mamma- A New Mammaliaform from the liaforms have a medial concavity on the man- dibular angle (8–14, 23), as in nonmamma- Early Jurassic and Evolution of liaform cynodonts (9, 14, 24–27). The post- dentary trough and the medial concavity on Mammalian Characteristics the mandibular angle respectively accommo- dated the prearticular/surangular and the re- Zhe-Xi Luo,1* Alfred W. Crompton,2 Ai-Lin Sun3 flected lamina of the angular (9, 25–27) that are the homologs to the mammalian middle A fossil from the Early Jurassic (Sinemurian, ϳ195 million years ago) represents ear bones (9, 14, 16–21, 23, 26). The absence a new lineage of mammaliaforms, the extinct groups more closely related to of these structures indicates that the postden- the living mammals than to nonmammaliaform cynodonts. It has an enlarged tary bones (“middle ear ossicles”) must have cranial cavity, but no postdentary trough on the mandible, indicating separation been separated from the mandible (Fig. 3). of the middle ear bones from the mandible. This extends the earliest record of Hadrocodium lacks the primitive meckelian these crucial mammalian features by some 45 million years and suggests that sulcus of the mandible typical of all nonmam- separation of the middle ear bones from the mandible and the expanded brain maliaform cynodonts (24–27), stem groups vault could be correlated. It shows that several key mammalian evolutionary of mammaliaforms (8, 9, 14, 23, 26, 27), innovations in the ear region, the temporomandibular joint, and the brain vault triconodontids (28, 29), and nontribosphenic evolved incrementally through mammaliaform evolution and long before the therian mammals (30). -
Mesozoic: the Dark Age for Mammals!
Ed’s Simplified History of the Mammals Note progression from Pelycosaurs (1) to Therapsids and Cynodonts (2) in Triassic. Stem mammals appeared in Late Triassic and Early Jurassic (3). Relationships among the Middle Jurassic forms (4) are controversial (see handout). Therian clade, identified by the tribosphenic molar (5), emerged at the end of the Jurassic, Early Cretaceous. A slightly more detailed version… in case you like something that looks more slick From Pough et al. 2009. Vertebrate Life, 8th ed. Pelycosaurs Dominated the late Permian, gave rise to therapsids Therapsids Rapid radiation in late Permian, around 270 MYA Still “mammal-like reptiles” The mass extinction at the end of the Permian was the greatest loss of diversity ever with >80% of all known genera and about 90% of all species going extinct, both terrestrial and marine. Cynodonts Late Permian to mid Triassic Last remaining group of therapsids, survived mass extinction at the end of the Permian. Persisted well Only 1 lineage of into Triassic and developed cynodonts survived many features associated through the late Triassic, with mammals. and this group became ancestors of mammals. Mesozoic: the Dark Age for Mammals! multituberculate Morganucodon, one of the earliest mammals (What else was happening in the Late Triassic and Jurassic Hadrocodium that may have contributed to mammals becoming small and Most were very small with nocturnal?) conservative morphology ...but new fossil finds indicate more diversity than we thought Repenomanus Still, largest known mammal during Mesozic Most were shrew to is no larger than a mouse sized, for 125 woodchuck million years! Some Mesozoic events and mammals you should know 1. -
Molecular Phylogenetics of Shrews (Mammalia: Soricidae) Reveal Timing of Transcontinental Colonizations
Molecular Phylogenetics and Evolution 44 (2007) 126–137 www.elsevier.com/locate/ympev Molecular phylogenetics of shrews (Mammalia: Soricidae) reveal timing of transcontinental colonizations Sylvain Dubey a,*, Nicolas Salamin a, Satoshi D. Ohdachi b, Patrick Barrie`re c, Peter Vogel a a Department of Ecology and Evolution, University of Lausanne, CH-1015 Lausanne, Switzerland b Institute of Low Temperature Science, Hokkaido University, Sapporo 060-0819, Japan c Laboratoire Ecobio UMR 6553, CNRS, Universite´ de Rennes 1, Station Biologique, F-35380, Paimpont, France Received 4 July 2006; revised 8 November 2006; accepted 7 December 2006 Available online 19 December 2006 Abstract We sequenced 2167 base pairs (bp) of mitochondrial DNA cytochrome b and 16S, and 1390 bp of nuclear genes BRCA1 and ApoB in shrews taxa (Eulipotyphla, family Soricidae). The aim was to study the relationships at higher taxonomic levels within this family, and in particular the position of difficult clades such as Anourosorex and Myosorex. The data confirmed two monophyletic subfamilies, Soric- inae and Crocidurinae. In the former, the tribes Anourosoricini, Blarinini, Nectogalini, Notiosoricini, and Soricini were supported. The latter was formed by the tribes Myosoricini and Crocidurini. The genus Suncus appeared to be paraphyletic and included Sylvisorex.We further suggest a biogeographical hypothesis, which shows that North America was colonized by three independent lineages of Soricinae during middle Miocene. Our hypothesis is congruent with the first fossil records for these taxa. Using molecular dating, the first exchang- es between Africa and Eurasia occurred during the middle Miocene. The last one took place in the Late Miocene, with the dispersion of the genus Crocidura through the old world. -
Alexis Museum Loan NM
STANFORD UNIVERSITY STANFORD, CALIFORNIA 94305-5020 DEPARTMENT OF BIOLOGY PH. 650.725.2655 371 Serrra Mall FAX 650.723.0589 http://www.stanford.edu/group/hadlylab/ [email protected] 4/26/13 Joseph A. Cook Division of Mammals The Museum of Southwestern Biology at the University of New Mexico Dear Joe: I am writing on behalf of my graduate student, Alexis Mychajliw and her collaborator, Nat Clarke, to request the sampling of museum specimens (tissue, skins, skeletons) for DNA extraction for use in our study on the evolution of venom genes within Eulipotyphlan mammals. Please find included in this request the catalogue numbers of the desired specimens, as well as a summary of the project in which they will be used. We have prioritized the use of frozen or ethanol preserved tissues to avoid the destruction of museum skins, and seek tissue samples from other museums if only skins are available for a species at MSB. The Hadly lab has extensive experience in the non-destructive sampling of specimens for genetic analyses. Thank you for your consideration and assistance with our research. Please contact Alexis ([email protected]) with any questions or concerns regarding our project or sampling protocols, or for any additional information necessary for your decision and the processing of this request. Alexis is a first-year student in my laboratory at Stanford and her project outline is attached. As we are located at Stanford University, we are unable to personally pick up loan materials from the MSB. We request that you ship materials to us in ethanol or buffer. -
Cryptic Diversity in Forest Shrews of the Genus Myosorex from Southern Africa, with the Description of a New Species and Comments on Myosorex Tenuis
bs_bs_banner Zoological Journal of the Linnean Society, 2013, 169, 881–902. With 7 figures Cryptic diversity in forest shrews of the genus Myosorex from southern Africa, with the description of a new species and comments on Myosorex tenuis PETER JOHN TAYLOR1,2*, TERESA CATHERINE KEARNEY3, JULIAN C. KERBIS PETERHANS4,5, RODERICK M. BAXTER6 and SANDI WILLOWS-MUNRO2 1SARChI Chair on Biodiversity Value & Change in the Vhembe Biosphere Reserve & Core Member of Centre for Invasion Biology, School of Mathematical & Natural Sciences, University of Venda, P. Bag X5050, Thohoyandou, 0950, South Africa 2School of Life Science, University of KwaZulu-Natal, Durban and Pietermaritzburg, South Africa 3Department of Vertebrates, Small Mammals Section, Ditsong National Museum of Natural History (formerly Transvaal Museum), P.O. Box 413, Pretoria, 0001 South Africa 4University College, Roosevelt University, 430 South Michigan Avenue, Chicago, IL 60605, USA 5Department of Zoology, Field Museum of Natural History, 1400 Lake Shore Drive, Chicago, IL 60605, USA 6Department of Ecology & Resource Management, School of Environmental Sciences, University of Venda, P. Bag X5050, Thohoyandou 0950, South Africa Received 31 March 2013; revised 19 August 2013; accepted for publication 19 August 2013 Forest or mouse shrews (Myosorex) represent a small but important radiation of African shrews generally adapted to montane and/or temperate conditions. The status of populations from Zimbabwe, Mozambique, and the north of South Africa has long been unclear because of the variability of traits that have traditionally been ‘diagnostic’ for the currently recognized South African taxa. We report molecular (mitochondrial DNA and nuclear DNA), craniometric, and morphological data from newly collected series of Myosorex from Zimbabwe (East Highlands), Mozambique (Mount Gorogonsa, Gorongosa National Park), and the Limpopo Province of South Africa (Soutpansberg Range) in the context of the available museum collections from southern and eastern Africa and published DNA sequences. -
The Mesozoic Mesozoic Things to Think About
The Mesozoic Mesozoic Things to think about • Breakup of Pangea and its relationship to sealevel and climate • Dominance of reptiles • Origin of birds • Origin of mammals • Origin of flowers (angiosperms) • Expansion of insects • Life in the seas assumes an (almost) modern form 1 2 3 4 5 Triassic Period 248 to 206 Million Years Ago 6 The Connecticut River Valley 7 Dinosaur Footprints of the Connecticut Valley Edward Hitchcock Fossil Fish of the Connecticut Valley 8 Jurassic Period 206 to 144 Million Years Ago 9 Cretaceous Period 144 to 65 Million Years Ago 10 11 Mesozoic Ammonites 12 Cretaceous Heteromorph Ammonites Nipponites mirabilis Kamchatka, Russia Macroscaphites sp. Baculites sp. Didymoceras stevensoni Rudistid Bivalves: Jurassic- Cretaceous 13 Durania cornupastoris at Abu Roash, Western Desert near Gizah, Egypt Fringing Upper Cretaceous rudist reef reservoirs flanking basement highs, Augila oil field, eastern Libya Reef-forming rudist (Radiolites) from Sarvak Formation, Cenomanian, south Iran. 14 Biostrome of hippuritid rudists at Montagne des Cornes; Santonian, Pyrenees, France Rudistid Buildups 15 Biostrome of Vaccinites vesiculosus (Woodward, 1855); Campanian of Saiwan, Oman Monopleura marcida Albian, Viotía, Greece 16 Chalk 17 Pterosaurs Mosasaurs 18 Plesiosaurs Ichthyosaurs 19 A Dinosaur Family Tree (aka Phylogeny) 20 Sauropods Theropods 21 Dilong paradoxus Early Cretaceous, China A feathered tyrannosaurid? 22 A Dinosaur Family Tree (aka Phylogeny) Ornithopods (aka Hadrosaurs) 23 Thyreophorans (aka Ankylosaurs, etc) Margincephalians (aka Ceratopsians) 24 A Dinosaur Family Tree (aka Phylogeny) The Liaoning Fauna: An early Cretaceous Lagerstatten Some highlights: -- feathered dinosaurs -- preserved internal organs -- oldest placental mammal 25 The Liaoning Fauna The Liaoning Fauna Caudipteryx. Microraptor gui MICRORAPTOR zhaoianus.