Tiny Fossil Sheds Light on Miniaturization of Birds
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Broad-Tailed Hummingbird Coloration and Sun Orientation 1
1 Broad-tailed hummingbird coloration and sun orientation 1 Two ways to display: male hummingbirds show different 2 color-display tactics based on sun orientation 3 Running header: Broad-tailed hummingbird coloration and sun orientation 4 5 Richard K. Simpson1* and Kevin J. McGraw1 6 1School of Life Sciences, Arizona State University, Tempe, AZ 85287-4501 7 *Corresponding Author. Email: [email protected]; Phone: (480) 965-2593 8 9 ABSTRACT 10 Animals exhibit a diversity of ornaments and courtship behaviors, which often co- 11 occur and are used for communication. The sensory drive hypothesis states that these 12 traits evolved and vary due to interactions with each other, the environment, and signal 13 receiver. However, interactions between colorful ornaments and courtship behaviors, 14 specifically in relation to environmental variation, remain poorly understood. We studied 15 male iridescent plumage (gorgets), display behavior, and sun orientation during courtship 16 flights (shuttle displays) in broad-tailed hummingbirds (Selasphorus platycercus), to 17 understand how these traits interact in both space and time to produce the perceived 18 coloration of males. We also tested how gorget coloration varies among males based on 19 their plumage, behavioral, and morphological characteristics. In contrast with previous 20 work on other animals, we found that displaying males did not directionally face the sun, 21 but instead displayed on a continuum of solar orientation angles. The gorgets of males 22 who tended to face the sun during their displays appeared flashier (i.e. exhibited greater 23 color/brightness changes), brighter, and more colorful, whereas the gorgets of males who 2 Broad-tailed hummingbird coloration and sun orientation 24 tended to not face the sun were more consistently reflective (i.e. -
A New Raptorial Dinosaur with Exceptionally Long Feathering Provides Insights Into Dromaeosaurid flight Performance
ARTICLE Received 11 Apr 2014 | Accepted 11 Jun 2014 | Published 15 Jul 2014 DOI: 10.1038/ncomms5382 A new raptorial dinosaur with exceptionally long feathering provides insights into dromaeosaurid flight performance Gang Han1, Luis M. Chiappe2, Shu-An Ji1,3, Michael Habib4, Alan H. Turner5, Anusuya Chinsamy6, Xueling Liu1 & Lizhuo Han1 Microraptorines are a group of predatory dromaeosaurid theropod dinosaurs with aero- dynamic capacity. These close relatives of birds are essential for testing hypotheses explaining the origin and early evolution of avian flight. Here we describe a new ‘four-winged’ microraptorine, Changyuraptor yangi, from the Early Cretaceous Jehol Biota of China. With tail feathers that are nearly 30 cm long, roughly 30% the length of the skeleton, the new fossil possesses the longest known feathers for any non-avian dinosaur. Furthermore, it is the largest theropod with long, pennaceous feathers attached to the lower hind limbs (that is, ‘hindwings’). The lengthy feathered tail of the new fossil provides insight into the flight performance of microraptorines and how they may have maintained aerial competency at larger body sizes. We demonstrate how the low-aspect-ratio tail of the new fossil would have acted as a pitch control structure reducing descent speed and thus playing a key role in landing. 1 Paleontological Center, Bohai University, 19 Keji Road, New Shongshan District, Jinzhou, Liaoning Province 121013, China. 2 Dinosaur Institute, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA. 3 Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, China. 4 University of Southern California, Health Sciences Campus, BMT 403, Mail Code 9112, Los Angeles, California 90089, USA. -
Ghost of the Forest: the Tangible and Intangible in Natural and Cultural Heritage
Ghost of the Forest: the Tangible and Intangible in Natural and Cultural Heritage Marcel Robischon Ghost of the Forest Ghost of the Forest: the Tangible and Intangible in Natural and Cultural Heritage Marcel Robischon Junior Professor, Department of Life Sciences, Humboldt Universität zu Berlin, Germany ABSTRACT Understanding the close interconnectedness of cultural and natural, tangible and intangible heritage is central to conservation efforts. This point is illustrated by examples in which works of culture have lost their original cultural or natural context – and this includes intangible natural phenomena. Further examples are given in which biological species survived as a genetic continuum but were changed in terms of their intangibles, i.e. their behaviour, in ways that can be perceived by human observers. In this article it is argued that the addition of a fourth category of ‘intangible natural heritage’ to the existing categories of World Heritage would strengthen conservation efforts and bring forward the discussion with an integrated understanding of natural and cultural heritage. Keywords Intangible Natural Heritage, co-extinction of cultural and biological phenomena, conservation, artistic inspiration, bio- diversity, bio-cultural interaction, ephemerality, World Heritage. The interdependence and the fragility of phrased by Singer (2006), Tangible heritage is expressed tangible and intangible heritage in objects, concrete matter, enduring years and Ultimately, buildings, human-made structures and sometimes centuries, carrying with it some of the artwork would be merely near-surface biogenic substance of human life, feeling, and thought. sediments resulting from highly complex processes of bio-turbation if it were not for the cultural motivation The cultural significance of ancient tangible heritage behind their creation and the meanings attached to them. -
Dinosaur Footprints
DINOSAUR FOOTPRINTS ACTIVITY SHEET YOU WILL NEED: Measuring tape and chalk DINOSAUR BODY SIZE Playground Calculator/paper for calculations Dinosaur footprint length: measure in a straight line from the back of the foot to the tip of the longest toe. Dinosaur leg length = footprint length × 4 Dinosaur stride length: Distance between footprints Dinosaur body length = from the same foot footprint length × 10 1. Use a measuring tape, chalk and the information below to draw out your dinosaur footprints in the playground. Tip - measure the footprint length first and then draw your footprint shape. If students are working in groups, each group could choose a different footprint. Footprint length - from back Dinosaur Footprint shape of foot to tip of longest toe Stride length (cm) (cm) Allosaurus 85 340 Triceratops 90 360 Compsognathus 7.5 90 Brachiosaurus 260 1040 DINOSAUR FOOTPRINTS ACTIVITY SHEET Stride length 2. Use your measuring tape to measure the dinosaur’s stride length. Use chalk to mark where the second dinosaur footprint would go. Footprint 2 Footprint 1 3. Using the calculations on page 1 work out the leg lengths and body lengths of each dinosaur. If you have space use a measuring tape and chalk to measure out the dinosaur body lengths in the playground (some of them will be very long!). Dinosaur Footprint length (cm) Leg length (cm) Body length (cm) Allosaurus 85 Triceratops 90 Compsognathus 7.5 Brachiosaurus 260 DINOSAUR SPEED We can now work out the relative speed of the dinosaur – whether it was walking, trotting or running, by looking at its leg length and stride length. -
Wildlife Ecology Provincial Resources
MANITOBA ENVIROTHON WILDLIFE ECOLOGY PROVINCIAL RESOURCES !1 ACKNOWLEDGEMENTS We would like to thank: Olwyn Friesen (PhD Ecology) for compiling, writing, and editing this document. Subject Experts and Editors: Barbara Fuller (Project Editor, Chair of Test Writing and Education Committee) Lindsey Andronak (Soils, Research Technician, Agriculture and Agri-Food Canada) Jennifer Corvino (Wildlife Ecology, Senior Park Interpreter, Spruce Woods Provincial Park) Cary Hamel (Plant Ecology, Director of Conservation, Nature Conservancy Canada) Lee Hrenchuk (Aquatic Ecology, Biologist, IISD Experimental Lakes Area) Justin Reid (Integrated Watershed Management, Manager, La Salle Redboine Conservation District) Jacqueline Monteith (Climate Change in the North, Science Consultant, Frontier School Division) SPONSORS !2 Introduction to wildlife ...................................................................................7 Ecology ....................................................................................................................7 Habitat ...................................................................................................................................8 Carrying capacity.................................................................................................................... 9 Population dynamics ..............................................................................................................10 Basic groups of wildlife ................................................................................11 -
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. -
A Fast-Growing Basal Troodontid (Dinosauria: Theropoda) from The
www.nature.com/scientificreports OPEN A fast‑growing basal troodontid (Dinosauria: Theropoda) from the latest Cretaceous of Europe Albert G. Sellés1,2*, Bernat Vila1,2, Stephen L. Brusatte3, Philip J. Currie4 & Àngel Galobart1,2 A characteristic fauna of dinosaurs and other vertebrates inhabited the end‑Cretaceous European archipelago, some of which were dwarves or had other unusual features likely related to their insular habitats. Little is known, however, about the contemporary theropod dinosaurs, as they are represented mostly by teeth or other fragmentary fossils. A new isolated theropod metatarsal II, from the latest Maastrichtian of Spain (within 200,000 years of the mass extinction) may represent a jinfengopterygine troodontid, the frst reported from Europe. Comparisons with other theropods and phylogenetic analyses reveal an autapomorphic foramen that distinguishes it from all other troodontids, supporting its identifcation as a new genus and species, Tamarro insperatus. Bone histology shows that it was an actively growing subadult when it died but may have had a growth pattern in which it grew rapidly in early ontogeny and attained a subadult size quickly. We hypothesize that it could have migrated from Asia to reach the Ibero‑Armorican island no later than Cenomanian or during the Maastrichtian dispersal events. During the latest Cretaceous (ca. 77–66 million years ago) in the run-up to the end-Cretaceous mass extinc- tion, Europe was a series of islands populated by diverse and distinctive communities of dinosaurs and other vertebrates. Many of these animals exhibited peculiar features that may have been generated by lack of space and resources in their insular habitats. -
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. -
Alpha Codes for 2168 Bird Species (And 113 Non-Species Taxa) in Accordance with the 62Nd AOU Supplement (2021), Sorted Taxonomically
Four-letter (English Name) and Six-letter (Scientific Name) Alpha Codes for 2168 Bird Species (and 113 Non-Species Taxa) in accordance with the 62nd AOU Supplement (2021), sorted taxonomically Prepared by Peter Pyle and David F. DeSante The Institute for Bird Populations www.birdpop.org ENGLISH NAME 4-LETTER CODE SCIENTIFIC NAME 6-LETTER CODE Highland Tinamou HITI Nothocercus bonapartei NOTBON Great Tinamou GRTI Tinamus major TINMAJ Little Tinamou LITI Crypturellus soui CRYSOU Thicket Tinamou THTI Crypturellus cinnamomeus CRYCIN Slaty-breasted Tinamou SBTI Crypturellus boucardi CRYBOU Choco Tinamou CHTI Crypturellus kerriae CRYKER White-faced Whistling-Duck WFWD Dendrocygna viduata DENVID Black-bellied Whistling-Duck BBWD Dendrocygna autumnalis DENAUT West Indian Whistling-Duck WIWD Dendrocygna arborea DENARB Fulvous Whistling-Duck FUWD Dendrocygna bicolor DENBIC Emperor Goose EMGO Anser canagicus ANSCAN Snow Goose SNGO Anser caerulescens ANSCAE + Lesser Snow Goose White-morph LSGW Anser caerulescens caerulescens ANSCCA + Lesser Snow Goose Intermediate-morph LSGI Anser caerulescens caerulescens ANSCCA + Lesser Snow Goose Blue-morph LSGB Anser caerulescens caerulescens ANSCCA + Greater Snow Goose White-morph GSGW Anser caerulescens atlantica ANSCAT + Greater Snow Goose Intermediate-morph GSGI Anser caerulescens atlantica ANSCAT + Greater Snow Goose Blue-morph GSGB Anser caerulescens atlantica ANSCAT + Snow X Ross's Goose Hybrid SRGH Anser caerulescens x rossii ANSCAR + Snow/Ross's Goose SRGO Anser caerulescens/rossii ANSCRO Ross's Goose -
Anatomy of the Early Cretaceous Enantiornithine Bird Rapaxavis Pani
Anatomy of the Early Cretaceous enantiornithine bird Rapaxavis pani JINGMAI K. O’CONNOR, LUIS M. CHIAPPE, CHUNLING GAO, and BO ZHAO O’Connor, J.K., Chiappe, L.M., Gao, C., and Zhao, B. 2011. Anatomy of the Early Cretaceous enantiornithine bird Rapaxavis pani. Acta Palaeontologica Polonica 56 (3): 463–475. The exquisitely preserved longipterygid enantiornithine Rapaxavis pani is redescribed here after more extensive prepara− tion. A complete review of its morphology is presented based on information gathered before and after preparation. Among other features, Rapaxavis pani is characterized by having an elongate rostrum (close to 60% of the skull length), rostrally restricted dentition, and schizorhinal external nares. Yet, the most puzzling feature of this bird is the presence of a pair of pectoral bones (here termed paracoracoidal ossifications) that, with the exception of the enantiornithine Concornis lacustris, are unknown within Aves. Particularly notable is the presence of a distal tarsal cap, formed by the fu− sion of distal tarsal elements, a feature that is controversial in non−ornithuromorph birds. The holotype and only known specimen of Rapaxavis pani thus reveals important information for better understanding the anatomy and phylogenetic relationships of longipterygids, in particular, as well as basal birds as a whole. Key words: Aves, Enantiornithes, Longipterygidae, Rapaxavis, Jiufotang Formation, Early Cretaceous, China. Jingmai K. O’Connor [[email protected]], Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, 142 Xizhimenwaidajie, Beijing, China, 100044; The Dinosaur Institute, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007 USA; Luis M. Chiappe [[email protected]], The Dinosaur Institute, Natural History Museum of Los Angeles County, 900 Ex− position Boulevard, Los Angeles, CA 90007 USA; Chunling Gao [[email protected]] and Bo Zhao [[email protected]], Dalian Natural History Museum, No.