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Tiny Fossil Sheds Light on Miniaturization of Birds
Retraction Tiny fossil sheds light on miniaturization of birds Roger B. J. Benson Nature 579, 199–200 (2020) In view of the fact that the authors of ‘Hummingbird-sized dinosaur from the Cretaceous period of Myanmar‘ (L. Xing et al. Nature 579, 245–249; 2020) are retracting their report, I wish to retract this News & Views article, which dealt with this study and was based on the accuracy and reproducibility of their data. Nature | 22 July 2020 ©2020 Spri nger Nature Li mited. All rights reserved. drives the assembly of DNA-PK and stimulates regulation of protein synthesis. And, although 3. Dragon, F. et al. Nature 417, 967–970 (2002). its catalytic activity in vitro, although does so further studies are required, we might have 4. Adelmant, G. et al. Mol. Cell. Proteom. 11, 411–421 (2012). much less efficiently than can DNA. taken a step closer to deciphering the 5. Britton, S., Coates, J. & Jackson, S. P. J. Cell Biol. 202, Taken together, these observations suggest mysterious ribosomopathies. 579–595 (2013). a model in which KU recruits DNA-PKcs to the 6. Barandun, J. et al. Nature Struct. Mol. Biol. 24, 944–953 (2017). small-subunit processome. In the case of Alan J. Warren is at the Cambridge Institute 7. Ma, Y. et al. Cell 108, 781–794 (2002). kinase-defective DNA-PK, the mutant enzyme’s for Medical Research, Hills Road, Cambridge 8. Yin, X. et al. Cell Res. 27, 1341–1350 (2017). inability to regulate its own activity gives the CB2 OXY, UK. 9. Sharif, H. et al. -
Spraberry of the Midland Basin
Stratigraphic Framework of the Wolfcamp – Spraberry of the Midland Basin Roswell Geologic Society October 8, 2019 Lowell Waite Department of Geosciences Permian Basin Research Lab University of Texas at Dallas Permian Basin Research Lab at UT Dallas Dr. Robert J. Stern and Mr. Lowell Waite, Co-Directors -- established January, 2019 -- Goals: • Advance understanding of all geologic aspects of the Permian Basin through open applied research, linking academia and industry • Educate and better prepare students for professional careers in the oil and gas industry • Graduate courses offered: • Geology of the Permian Basin • Petroleum Geoscience • Paleo Earth Systems: Global Themes https://labs.utdallas.edu/permianbasinresearch/ Stratigraphic framework of Wolfcamp – Spraberry: Objectives • Review the tectono-stratigraphic framework of the Wolfcamp and Spraberry deep-water units of the Midland Basin, west Texas • Briefly discuss the facies/characteristics of these rocks • Highlight the differences between the Wolfcamp shale (A – D) and Spraberry depositional systems Note: although not specifically addressed, the framework outlined here is applicable to the Delaware Basin Greater Permian Basin Region • Confluence of Marathon- Ouachita fold and thrust belt and Ancestral Rockies basement-involved uplifts (Penn. – early Permian) Study Area Precursor Tobosa Basin (Ord. to Miss.) Fold and thrust belt Basement uplift Shallow marine shelf Reef / shoal complex Deep marine basin Permian Basin Stratigraphy and Tectonic History Ma System Series Delaware Basin -
Ocean Drilling Program Scientific Results Volume
Wise, S. W., Jr., Schlich, R., et al., 1992 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 120 44. ISOTOPE AND TRACE ELEMENT GEOCHEMISTRY OF EOCENE AND OLIGOCENE FORAMINIFERS FROM SITE 748, KERGUELEN PLATEAU1 James C. Zachos,2 William A. Berggren,3 Marie-Pierre Aubry,3,4 and Andreas Mackensen5 ABSTRACT Stable carbon and oxygen isotope analyses were conducted on well-preserved planktonic and benthic foraminifers from a continuous middle Eocene to Oligocene sequence at Ocean Drilling Program (ODP) Site 748 on the Kerguelen Plateau. Benthic foraminifer δ18θ values show a 1.0‰ increase through the middle and upper Eocene, followed by a rapid 1.2%c increase in the lowermost Oligocene (35.5 Ma). Surface-dwelling planktonic foraminifer δ18θ values increase in the lowermost Oligocene, but only by 0.6%e whereas intermediate-depth planktonic foraminifers show an increase of about l.O‰. Benthic foraminifer δ13C values increase by 0.9‰ in the lowermost Oligocene at precisely the same time as the large δ18θ increase, whereas planktonic foraminifer δ13C values show little or no change. Site 748 oxygen isotope and paleontological records suggest that southern Indian Ocean surface and intermediate waters underwent significant cooling from the early to late Eocene. The rapid 1.2%o oxygen isotope increase recorded by benthic foraminifers just above the Eocene/Oligocene boundary represents the ubiquitous early Oligocene δ18θ event. The shift here is unique, however, as it coincided with the sudden appearance of ice-rafted debris (IRD), providing the first direct link between Antarctic glacial activity and the earliest Oligocene δ18θ increase. -
AOU Classification Committee – North and Middle America
AOU Classification Committee – North and Middle America Proposal Set 2016-C No. Page Title 01 02 Change the English name of Alauda arvensis to Eurasian Skylark 02 06 Recognize Lilian’s Meadowlark Sturnella lilianae as a separate species from S. magna 03 20 Change the English name of Euplectes franciscanus to Northern Red Bishop 04 25 Transfer Sandhill Crane Grus canadensis to Antigone 05 29 Add Rufous-necked Wood-Rail Aramides axillaris to the U.S. list 06 31 Revise our higher-level linear sequence as follows: (a) Move Strigiformes to precede Trogoniformes; (b) Move Accipitriformes to precede Strigiformes; (c) Move Gaviiformes to precede Procellariiformes; (d) Move Eurypygiformes and Phaethontiformes to precede Gaviiformes; (e) Reverse the linear sequence of Podicipediformes and Phoenicopteriformes; (f) Move Pterocliformes and Columbiformes to follow Podicipediformes; (g) Move Cuculiformes, Caprimulgiformes, and Apodiformes to follow Columbiformes; and (h) Move Charadriiformes and Gruiformes to precede Eurypygiformes 07 45 Transfer Neocrex to Mustelirallus 08 48 (a) Split Ardenna from Puffinus, and (b) Revise the linear sequence of species of Ardenna 09 51 Separate Cathartiformes from Accipitriformes 10 58 Recognize Colibri cyanotus as a separate species from C. thalassinus 11 61 Change the English name “Brush-Finch” to “Brushfinch” 12 62 Change the English name of Ramphastos ambiguus 13 63 Split Plain Wren Cantorchilus modestus into three species 14 71 Recognize the genus Cercomacroides (Thamnophilidae) 15 74 Split Oceanodroma cheimomnestes and O. socorroensis from Leach’s Storm- Petrel O. leucorhoa 2016-C-1 N&MA Classification Committee p. 453 Change the English name of Alauda arvensis to Eurasian Skylark There are a dizzying number of larks (Alaudidae) worldwide and a first-time visitor to Africa or Mongolia might confront 10 or more species across several genera. -
Geology of London, UK
Geology of London, UK Katherine R. Royse1, Mike de Freitas2,3, William G. Burgess4, John Cosgrove5, Richard C. Ghail3, Phil Gibbard6, Chris King7, Ursula Lawrence8, Rory N. Mortimore9, Hugh Owen10, Jackie Skipper 11, 1. British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK. [email protected] 2. Imperial College London SW72AZ, UK & First Steps Ltd, Unit 17 Hurlingham Studios, London SW6 3PA, UK. 3. Department of Civil and Environmental Engineering, Imperial College London, London, SW7 2AZ, UK. 4. Department of Geological Sciences, University College London, WC1E 6BT, UK. 5. Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, UK. 6. Cambridge Quaternary, Department of Geography, University of Cambridge CB2 3EN, UK. 7. 16A Park Road, Bridport, Dorset 8. Crossrail Ltd. 25 Canada Square, Canary Wharf, London, E14 5LQ, UK. 9. University of Brighton & ChalkRock Ltd, 32 Prince Edwards Road, Lewes, BN7 1BE, UK. 10. Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK. 11. Geotechnical Consulting Group (GCG), 52A Cromwell Road, London SW7 5BE, UK. Abstract The population of London is around 7 million. The infrastructure to support this makes London one of the most intensively investigated areas of upper crust. however construction work in London continues to reveal the presence of unexpected ground conditions. These have been discovered in isolation and often recorded with no further work to explain them. There is a scientific, industrial and commercial need to refine the geological framework for London and its surrounding area. This paper reviews the geological setting of London as it is understood at present, and outlines the issues that current research is attempting to resolve. -
NEWS and NOTES by Paul Hess
NEWS AND NOTES by Paul Hess First-year Migrants sumably innate southwesterly bearing, and many ended up May Need Experience in Iberia far south of the usual winter range. His report in 1958 suggests that adults improve their inherent naviga - Inheritance or experience? Genetic programming or practi - tional map based on experience, but that first-year birds’ di - cal learning? Various studies show that both inherited and rectional behavior has not progressed beyond an inherited learned information helps birds to migrate to the right rudimentary compass ( Ardea 46:1–37). place in fall and to return to the right place in spring. Im - Fifty years later, Kasper Thorup and six coauthors have mature birds apparently use an innate compass that may added a radio-tracking dimension to similar research using not always allow them to deviate from “hard-wired” direc - White-crowned Sparrows. Results they report in 2007 are a near-perfect analogy to Perdeck’s findings, except that long- distance, non-social, nocturnal migrants are studied rather than short-distance, social, diurnal migrants ( Proceedings of the National Academy of Sciences 104:18115–18119). Fif - teen adult and 15 first-year southbound migrants of the gambelii subspecies were captured at a fall stopover site in Washington state and transported to New Jersey, where each was fitted with a tiny radio transmitter. The birds’ ini - tial movements near the release site were monitored by ground crews, but after flying away from the immediate area (usually at night) they were tracked individually by aircraft for distances as far as 122 kilometers. Adults and immatures rapidly demonstrated a conspicu - ous behavioral difference. -
Co-Option of the Cardiac Transcription Factor Nkx2.5 During Development of the Emu Wing
ARTICLE DOI: 10.1038/s41467-017-00112-7 OPEN Co-option of the cardiac transcription factor Nkx2.5 during development of the emu wing Peter G. Farlie 1,2, Nadia M. Davidson1, Naomi L. Baker1,2, Mai Raabus1, Kelly N. Roeszler1, Claire Hirst3, Andrew Major 3, Mylene M. Mariette4, David M. Lambert 5, Alicia Oshlack 1 & Craig A. Smith1,3 The ratites are a distinctive clade of flightless birds, typified by the emu and ostrich that have acquired a range of unique anatomical characteristics since diverging from basal Aves at least 100 million years ago. The emu possesses a vestigial wing with a single digit and greatly reduced forelimb musculature. However, the embryological basis of wing reduction and other anatomical changes associated with loss of flight are unclear. Here we report a previously unknown co-option of the cardiac transcription factor Nkx2.5 to the forelimb in the emu embryo, but not in ostrich, or chicken and zebra finch, which have fully developed wings. Nkx2.5 is expressed in emu limb bud mesenchyme and maturing wing muscle, and mis- expression of Nkx2.5 throughout the limb bud in chick results in wing reductions. We propose that Nkx2.5 functions to inhibit early limb bud expansion and later muscle growth during development of the vestigial emu wing. 1 Murdoch Children’s Research Institute, Royal Children’s Hospital, Parkville, VIC 3052, Australia. 2 Department of Paediatrics, University of Melbourne, Parkville, VIC 3052, Australia. 3 Biomedicine Discovery Institute, Department of Anatomy and Developmental Biology, Monash University, Clayton, VIC 3800, Australia. 4 Centre for Integrative Ecology, School of Life and Environmental Sciences, Deakin University, Waurn Ponds, VIC 3216, Australia. -
Columbiformes ~ Pterocliformes ~ Mesitornithiformes
Birds of the World part 2 Galloanseres, Neoaves: Columbea NEOGNATHAE (the rest of the birds!): Galloanseres • ORDER ANSERIFORMES – waterfowl • Family Anhimidae – screamers (3 species) • Family Anseranatidae – magpie goose (1 species) • Family Anatidae – ducks, geese, and swans (173 species) • ORDER GALLIFORMES – landfowl • Family Megapodiidae – megapodes (21 species) • Family Cracidae – chachalacas, curassows, and guans (55 species) • Family Numididae – guineafowl (6 species) • Family Odontophoridae – New World quail (34 species) • Family Phasianidae – pheasants and allies (183 species) NEOGNATHAE : Neoaves (the rest of the birds!): COLUMBEA • ORDER PODICIPEDIFORMES – Family Podicipedidae – grebes (23 species) • ORDER PHOENICOPTERIFORMES – Family Phoenicopteridae – flamingos (6 species) • ORDER COLUMBIFORMES – Family Columbidae – pigeons and doves (334 species) • ORDER PTEROCLIDIFORMES – Family Pteroclididae – sandgrouse (16 species) • ORDER MESITORNITHIFORMES – Family Mesitornithidae – mesites (3 species) NEOGNATHAE : Galloanseres • ORDER ANSERIFORMES – waterfowl • Family Anhimidae – screamers (3 species) • Family Anseranatidae – magpie goose (1 species) • Family Anatidae – ducks, geese, and swans (173 species) • ORDER GALLIFORMES – landfowl • Family Megapodiidae – megapodes (21 species) • Family Cracidae – chachalacas, curassows, and guans (55 species) • Family Numididae – guineafowl (6 species) • Family Odontophoridae – New World quail (34 species) • Family Phasianidae – pheasants and allies (183 species) southern or crested screamer -
Geology of London, UK
Proceedings of the Geologists’ Association 123 (2012) 22–45 Contents lists available at ScienceDirect Proceedings of the Geologists’ Association jo urnal homepage: www.elsevier.com/locate/pgeola Review paper Geology of London, UK a, b,c d e c Katherine R. Royse *, Mike de Freitas , William G. Burgess , John Cosgrove , Richard C. Ghail , f g h i j k Phil Gibbard , Chris King , Ursula Lawrence , Rory N. Mortimore , Hugh Owen , Jackie Skipper a British Geological Survey, Keyworth, Nottingham NG12 5GG, UK b First Steps Ltd, Unit 17 Hurlingham Studios, London SW6 3PA, UK c Department of Civil and Environmental Engineering, Imperial College London, London SW7 2AZ, UK d Department of Earth Sciences, University College London, WC1E 6BT, UK e Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, UK f Cambridge Quaternary, Department of Geography, University of Cambridge, CB2 3EN, UK g 16A Park Road, Bridport, Dorset, UK h Crossrail Ltd. 25 Canada Square, Canary Wharf, London E14 5LQ, UK i University of Brighton & ChalkRock Ltd, 32 Prince Edwards Road, Lewes BN7 1BE, UK j Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK k Geotechnical Consulting Group (GCG), 52A Cromwell Road, London SW7 5BE, UK A R T I C L E I N F O A B S T R A C T Article history: The population of London is around 7 million. The infrastructure to support this makes London one of the Received 25 February 2011 most intensively investigated areas of upper crust. However construction work in London continues to Received in revised form 5 July 2011 reveal the presence of unexpected ground conditions. -
The Evolutionary Relationship Between Beak Shape, Mechanical Advantage
1 The evolutionary relationship between beak shape, mechanical advantage, 2 and feeding ecology in modern birds 3 4 5 Guillermo Navalón1,2,*, Jen A. Bright3,4, Jesús Marugán-Lobón2,5 & Emily J. Rayfield1 6 1. School of Earth Sciences, University of Bristol, Life Sciences Building, Bristol, UK 7 2. Unidad de Paleontología, Departamento de Biología, Universidad Autónoma de Madrid, Madrid, Spain. 8 3. School of Geosciences, University of South Florida, Tampa, FL 33620, USA. 9 4. Centre for Virtualization and Applied Spatial Technologies, University of South Florida, Tampa, FL 33620, USA 10 5. Dinosaur Institute, Natural History Museum of Los Angeles County, Los Angeles, CA, USA. 11 *Corresponding author. Email: [email protected]. 12 13 14 Author’s contributions: GN, JAB, JML and EJR designed the project. GN conducted the analyses. 15 GN, JAB, JML and EJR co-wrote the manuscript. 16 17 Acknowledgements 18 The authors are grateful to Melissa Tallman for important insights on shape analysis. We are 19 grateful to Gavin H. Thomas and Mark N. Puttick for advice on phylogenetic comparative 20 methods. We want to thank Luis Porras, Matteo Fabbri and Francisco J. Serrano for 21 enlightening discussion on the implications of our results. We are grateful to Miriam L. 22 Zelditch and three anonymous reviewers for their valuable comments that further improved the 23 quality of this research. GN is supported by a PG Scholarship/Studentship from The Alumni 24 Foundation, University of Bristol, UK. JML is supported by the Spanish MINECO, Project 25 CGL-2013-42643. EJR and JAB were supported by BBSRC grant BB/I011668/1. -
Phylogeny, Historical Biogeography and the Evolution of Migration in Accipitrid Birds of Prey (Aves: Accipitriformes)
Ornis Hungarica 2014. 22(1): 15–35. DOI: 10.2478/orhu-2014-0008 Phylogeny, historical biogeography and the evolution of migration in accipitrid birds of prey (Aves: Accipitriformes) Jenő nagy1 & Jácint tökölyi2* Jenő Nagy & Jácint Tökölyi 2014. Phylogeny, historical biogeography and the evolution of mig ration in accipitrid birds of prey (Aves: Accipitriformes). – Ornis Hungarica 22(1): 15–35. Abstract Migration plays a fundamental part in the life of most temperate bird species. The re gu lar, largescale seasonal movements that characterize temperate migration systems appear to have originated in parallel with the postglacial northern expansion of tropical species. Migratoriness is also in- fluenced by a number of ecological factors, such as the ability to survive harsh winters. Hence, understanding the origins and evolution of migration requires integration of the biogeographic history and ecology of birds in a phylogenetic context. We used molecular dating and ancestral state reconstruction to infer the origins and evolu- tionary changes in migratory behavior and ancestral area reconstruction to investigate historical patterns of range evolution in accipitrid birds of prey (Accipitriformes). Migration evolved multiple times in birds of prey, the ear- liest of which occurred in true hawks (Accipitrinae), during the middle Miocene period, according to our analy- ses. In most cases, a tropical ancestral distribution was inferred for the nonmigratory ancestors of migratory line- ages. Results from directional evolutionary tests indicate that migration evolved in the tropics and then increased the rate of colonization of temperate habitats, suggesting that temperate species might be descendants of tropi- cal ones that dispersed into these seasonal habitats. -
2.0 the Natural Landscape of London
2.0 The Natural Landscape of London London: A Green City? Contrary to perceptions, London is an unusually green city as of how they contribute to the city as a whole. This disconnection ‘natural’ environment. This may be the case for those architectures compared to other major world centres such as New York and Tokyo. between our daily experience of London and its relatively ‘green’ which reject the vernacular – notably modernism, which aimed at Nevertheless, for many, the impression of London is that of a highly character is exacerbated by the prevalence of travel by Underground, an international style − but vernacular architecture has by definition built up urban area, surrounded by less dense residential suburbs, whilst the topography of London, albeit gentle, has largely been an intimate relationship with its locale, whether as a form, such and whilst the Royal Parks are much-loved for their serenity and their disguised by London’s built environment. as the pitched roof, a direct response to frequent rainfall, or in the amenity value, how far we integrate them into our wider perception use of local building materials. Yet it is difficult to think of London’s of London is questionable. Likewise, whilst Londoners may regularly Underlying such perceptions is not only the disparity between architecture as vernacular, even though, to a large extent, London’s use local green spaces such as parks and commons, they are not daily living and travelling and a city-wide perspective but, perhaps built environment is derived from, rather than in opposition to, its necessarily perceived as integral parts of London’s character; private deeper, a fundamental assumption that architecture and urban underlying natural condition.