Co-Option of the Cardiac Transcription Factor Nkx2.5 During Development of the Emu Wing
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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. -
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. -
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. -
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. -
Megaphylls, Microphylls and the Evolution of Leaf Development
Opinion Megaphylls, microphylls and the evolution of leaf development Alexandru M.F. Tomescu Department of Biological Sciences, Humboldt State University, Arcata, CA 95521, USA Originally coined to emphasize morphological differ- However, the microphyll–megaphyll divide is not as ences, ‘microphyll’ and ‘megaphyll’ became synon- clear cut, and morphological definitions that contrast ymous with the idea that vascular plant leaves are not microphylls and megaphylls as mutually exclusive con- homologous. Although it is now accepted that leaves cepts of leaves are inconsistent. Moreover, current under- evolved independently in several euphyllophyte standing of plant phylogeny and leaf development fails to lineages, ‘megaphyll’ has grown to reflect another type shed light on the origin of microphylls, and supports of homology, that of euphyllophyte leaf precursor struc- several independent origins of megaphylls. Here, I review tures. However, evidence from the fossil record and plant phylogeny and developmental data from fossil and developmental pathways fails to indicate homology extant trachephytes, as well as the current understanding and suggests homoplasy of precursor structures. Thus, of genetic pathways controlling leaf development, to argue as I discuss here, ‘megaphyll’ should be abandoned that the megaphyll concept should be abandoned because because it perpetuates an unsupported idea of it perpetuates misconceptions and confusion based on homology, leading to misconceptions that pervade plant unsupported homology. biology thinking and can bias hypothesis and inference in developmental and phylogenetic studies. Alternative Morphological inconsistencies and overlap in the definitions are needed that are based on development microphyll–megaphyll dichotomy and phylogeny for different independently evolved leaf Microphylls are defined as leaves of small size, with simple types. -
The Formal Social World of British Egg-Collecting
n Cole, Edward (2016) Handle with care: historical geographies and difficult cultural legacies of egg-collecting. PhD thesis. http://theses.gla.ac.uk/7800/ Copyright and moral rights for this work are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This work cannot be reproduced or quoted extensively from without first obtaining permission in writing from the author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Glasgow Theses Service http://theses.gla.ac.uk/ [email protected] Handle With Care: Historical Geographies and Difficult Cultural Legacies of Egg-Collecting Edward Cole Submitted for the requirements for the Degree of Doctor of Philosophy (PhD) School of Geographical and Earth Sciences College of Science and Engineering University of Glasgow Abstract This thesis offers an examination of egg-collecting, which was a very popular pastime in Britain from the Victorian era well into the twentieth century. Collectors, both young and old, would often spend whole days and sometimes longer trips in a wide variety of different habitats, from sea shores to moorlands, wetlands to craggy mountainsides, searching for birds’ nests and the bounty to be found within them. Once collectors had found and taken eggs, they emptied out the contents; hence, they were really egg shell collectors. Some egg collectors claimed that egg-collecting was not just a hobby but a science, going by the name of oology, and seeking to establish oology as a recognised sub- discipline of ornithology, these collectors or oologists established formal institutions such as associations and societies, attended meetings where they exhibited unusual finds, and also contributed to specialist publications dedicated to oology. -
Thick-Billed Parrot (Rhynchopsitta Pachyrhyncha) Recovery Plan Addendum
Thick-billed Parrot (Rhynchopsitta pachyrhyncha) Recovery Plan Addendum Adenda al PACE: “Programa de Acción para la Conservación de las Especies: Cotorras Serranas (Rhynchopsitta spp.)” Photo by Jim Rorabaugh Including the English translation of the PACE, published by Mexico’s National Commission of Protected Areas (CONANP) 2009 U.S. Fish and Wildlife Service Southwest Region, Albuquerque, New Mexico June 2013 Approved: _________________________ Date: ____________________ Regional Director, Region 2, U.S. Fish and Wildlife Service Concurred: _________________________ Date: ____________________ Director, Arizona Game And Fish Department i DISCLAIMER The Endangered Species Act of 1973 (ESA), as amended (16 U.S.C. 1531 et seq.), requires the development of recovery plans for listed species, unless such a plan would not promote the conservation of a particular species. Recovery plans delineate such reasonable actions as may be necessary, based upon the best scientific and commercial data available, for the conservation and survival of listed species. Plans are published by the U.S. Fish and Wildlife Service (USFWS), sometimes prepared with the assistance of recovery teams, contractors, State agencies and others. Recovery plans do not necessarily represent the views, official positions, or approval of any individuals or agencies involved in the plan formulation, other than USFWS. They represent the official position of the USFWS only after they have been signed by the Regional Director. Recovery plans are guidance and planning documents only; identification of an action to be implemented by any public or private party does not create a legal obligation beyond existing legal requirements. Nothing in this plan should be construed as a commitment or requirement that any Federal agency obligate or pay funds in any one fiscal year in excess of appropriations made by Congress for that fiscal year in contravention of the Anti-Deficiency Act, 31 U.S.C. -
Evidence for Sea-Level Falls in the Permian-Triassic Transition in the Ziyun Area, South China
GEOLOGICAL JOURNAL Geol. J. 45: 170–185 (2010) Published online 21 July 2009 in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/gj.1168 Evidence for sea-level falls in the Permian-Triassic transition in the Ziyun area, South China WU YA-SHENG*, JIANG HONG-XIA and FAN JIA-SONG Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China The sedimentology of three sections showing the Permian–Triassic (P–T) transition on an Upper Permian reef in Ziyun, Guizhou Province, southwest China provides evidence of sea-level fall in this area. The P–T transition in the Gendan section, which covers a reef-front sequence, contains a subaerial exposure surface and various desiccation cracks (including rolled-up chips, in-chip cracks, pyramid cracks, vertical cracks and sheet cracks), indicating sea-level falls. The P–T transition in the Shitouzhai section, which covers a reef-core sequence, contains three micritic beds with abundant pseudomorphs of tabular gypsum crystals replaced by calcite. The underlying centimetres of deposits are composed of fine-crystalline dolostone, and have a sharp contact with the underlying reef-core facies. The association of gypsum pseudomorphs and fine-crystalline dolostone suggests an origin related to a supratidal evaporative environment. The P–T transition in the Tanluzhai section, which covers a back-reef sequence, is fine-crystalline dolostone, and shows a laminated algal structure indicating tidal- flat environments. The middle part of the dolostone interval has become a collapse breccia composed of dolostone fragments and a matrix of micrites or crustose multi-generation calcite cements. The formation of the collapse breccia is interpreted to be related to the dissolution of the evaporite interbeds originally present between the thin dolostone beds. -
An Antarctic Stratigraphic Record of Stepwise Ice Growth Through the Eocene-Oligocene Transition
Montclair State University Montclair State University Digital Commons Department of Earth and Environmental Studies Faculty Scholarship and Creative Works Department of Earth and Environmental Studies 3-1-2017 An Antarctic stratigraphic record of stepwise ice growth through the Eocene-Oligocene transition Sandra Passchier Montclair State University, [email protected] Daniel J. Ciarletta Montclair State University Triantafilo E. Miriagos Montclair State University Peter K. Bijl Utrecht University Steven M. Bohaty University of Southampton Follow this and additional works at: https://digitalcommons.montclair.edu/earth-environ-studies-facpubs Part of the Geology Commons MSU Digital Commons Citation Passchier, Sandra; Ciarletta, Daniel J.; Miriagos, Triantafilo E.; Bijl, eterP K.; and Bohaty, Steven M., "An Antarctic stratigraphic record of stepwise ice growth through the Eocene-Oligocene transition" (2017). Department of Earth and Environmental Studies Faculty Scholarship and Creative Works. 27. https://digitalcommons.montclair.edu/earth-environ-studies-facpubs/27 This Article is brought to you for free and open access by the Department of Earth and Environmental Studies at Montclair State University Digital Commons. It has been accepted for inclusion in Department of Earth and Environmental Studies Faculty Scholarship and Creative Works by an authorized administrator of Montclair State University Digital Commons. For more information, please contact [email protected]. An Antarctic stratigraphic record of stepwise ice growth