Fossil Evidence of Avian Crops from the Early Cretaceous of China
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Phylogenetic Position of Ambiortus: Comparison with Other Mesozoic Birds from Asia1 J
ISSN 00310301, Paleontological Journal, 2013, Vol. 47, No. 11, pp. 1270–1281. © Pleiades Publishing, Ltd., 2013. The Phylogenetic Position of Ambiortus: Comparison with Other Mesozoic Birds from Asia1 J. K. O’Connora and N. V. Zelenkovb aKey Laboratory of Evolution and Systematics, Institute of Vertebrate Paleontology and Paleoanthropology, 142 Xizhimenwai Dajie, Beijing China 10044 bBorissiak Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia email: [email protected], [email protected] Received August 6, 2012 Abstract—Since the last description of the ornithurine bird Ambiortus dementjevi from Mongolia, a wealth of Early Cretaceous birds have been discovered in China. Here we provide a detailed comparison of the anatomy of Ambiortus relative to other known Early Cretaceous ornithuromorphs from the Chinese Jehol Group and Xiagou Formation. We include new information on Ambiortus from a previously undescribed slab preserving part of the sternum. Ambiortus is superficially similar to Gansus yumenensis from the Aptian Xiagou Forma tion but shares more morphological features with Yixianornis grabaui (Ornithuromorpha: Songlingorni thidae) from the Jiufotang Formation of the Jehol Group. In general, the mosaic pattern of character distri bution among early ornithuromorph taxa does not reveal obvious relationships between taxa. Ambiortus was placed in a large phylogenetic analysis of Mesozoic birds, which confirms morphological observations and places Ambiortus in a polytomy with Yixianornis and Gansus. Keywords: Ornithuromorpha, Ambiortus, osteology, phylogeny, Early Cretaceous, Mongolia DOI: 10.1134/S0031030113110063 1 INTRODUCTION and articulated partial skeleton, preserving several cervi cal and thoracic vertebrae, and parts of the left thoracic Ambiortus dementjevi Kurochkin, 1982 was one of girdle and wing (specimen PIN, nos. -
3H?;Lnbcha Nb? 1?=L?Nm I@
3H?;LNBCHANB?1?=L?NMI@ #>O=;NIL%OC>? 1?=IH>#>CNCIH @C?F>GOM?OGILA13# 'HMC>? ;=EALIOH>'H@ILG;NCIH *?MMIHM@IL%L;>?M] >>CNCIH;F0?MIOL=?M 'HNLI>O=NCIH Unearthing the Secrets of SUE No dinosaur in the world compares to SUE—the largest, most complete, and best preserved Tyrannosaurus rex ever discovered. In May 2000, the unveiling of her 67-million-year-old skeleton at The Field Museum made global headlines. Since then, more than 16 million visitors have marveled over Chicago’s prehistoric giant. Using the story of SUE to captivate students’ imagination, the Unearthing the Secrets of SUE Educator Guide takes pre-k through eighth-grade students on an interactive exploration of SUE at The Field Museum and the scientific insights she’s providing about the world in which she lived. The lessons in this guide will engage students in the science of SUE by: • providing students unique access to SUE, the largest, most complete, and best preserved TYRANNOSAURUS REX ever discovered; • providing students with hands-on activities that enable them to investigate by making observations, developing hypotheses, questioning assumptions, testing ideas, and coming to conclusions; • introducing students to careers in science by highlighting the wide professional expertise involved in the SUE project; and • introducing students to the countless resources available to them through The Field Museum including field trips, and online research and interactive learning opportunities. How to Use this Guide • Detailed Background Information is provided to support educators in sharing the story of SUE with students. Use this information to prepare yourself and your students for learning about SUE. -
Trophic Shift and the Origin of Birds
bioRxiv preprint doi: https://doi.org/10.1101/2020.08.18.256131; this version posted August 18, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. Title: Trophic shift and the origin of birds Author: Yonghua Wu Affiliations: 1School of Life Sciences, Northeast Normal University, 5268 Renmin Street, Changchun, 130024, China. 2Jilin Provincial Key Laboratory of Animal Resource Conservation and Utilization, Northeast Normal University, 2555 Jingyue Street, Changchun, 130117, China. * Corresponding author: Yonghua Wu, Ph.D Professor, School of Life Sciences Northeast Normal University 5268 Renmin Street, Changchun, 130024, China Tel: +8613756171649 Email: [email protected] 1 bioRxiv preprint doi: https://doi.org/10.1101/2020.08.18.256131; this version posted August 18, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC 4.0 International license. Abstract Birds are characterized by evolutionary specializations of both locomotion (e.g., flapping flight) and digestive system (toothless, crop, and gizzard), while the potential selection pressures responsible for these evolutionary specializations remain unclear. Here we used a recently developed molecular phyloecological method to reconstruct the diets of the ancestral archosaur and of the common ancestor of living birds (CALB). Our results showed that the ancestral archosaur exhibited a predominant Darwinian selection of protein and fat digestion and absorption, whereas the CALB showed a marked enhanced selection of carbohydrate and fat digestion and absorption, suggesting a trophic shift from carnivory to herbivory (fruit, seed, and/or nut-eater) at the archosaur-to-bird transition. -
LETTER Doi:10.1038/Nature14423
LETTER doi:10.1038/nature14423 A bizarre Jurassic maniraptoran theropod with preserved evidence of membranous wings Xing Xu1,2*, Xiaoting Zheng1,3*, Corwin Sullivan2, Xiaoli Wang1, Lida Xing4, Yan Wang1, Xiaomei Zhang3, Jingmai K. O’Connor2, Fucheng Zhang2 & Yanhong Pan5 The wings of birds and their closest theropod relatives share a ratios are 1.16 and 1.08, respectively, compared to 0.96 and 0.78 in uniform fundamental architecture, with pinnate flight feathers Epidendrosaurus and 0.79 and 0.66 in Epidexipteryx), an extremely as the key component1–3. Here we report a new scansoriopterygid short humeral deltopectoral crest, and a long rod-like bone articu- theropod, Yi qi gen. et sp. nov., based on a new specimen from the lating with the wrist. Middle–Upper Jurassic period Tiaojishan Formation of Hebei Key osteological features are as follows. STM 31-2 (Fig. 1) is inferred Province, China4. Yi is nested phylogenetically among winged ther- to be an adult on the basis of the closed neurocentral sutures of the opods but has large stiff filamentous feathers of an unusual type on visible vertebrae, although this is not a universal criterion for maturity both the forelimb and hindlimb. However, the filamentous feath- across archosaurian taxa12. Its body mass is estimated to be approxi- ers of Yi resemble pinnate feathers in bearing morphologically mately 380 g, using an empirical equation13. diverse melanosomes5. Most surprisingly, Yi has a long rod-like The skull and mandible are similar to those of other scansoriopter- bone extending from each wrist, and patches of membranous tissue ygids, and to a lesser degree to those of oviraptorosaurs and some basal preserved between the rod-like bones and the manual digits. -
A Second Cretaceous Ornithuromorph Bird from the Changma Basin, Gansu Province, Northwestern China Author(S): Hai-Lu You , Jessie Atterholt , Jingmai K
A Second Cretaceous Ornithuromorph Bird from the Changma Basin, Gansu Province, Northwestern China Author(s): Hai-Lu You , Jessie Atterholt , Jingmai K. O'Connor , Jerald D. Harris , Matthew C. Lamanna and Da-Qing Li Source: Acta Palaeontologica Polonica, 55(4):617-625. 2010. Published By: Institute of Paleobiology, Polish Academy of Sciences DOI: http://dx.doi.org/10.4202/app.2009.0095 URL: http://www.bioone.org/doi/full/10.4202/app.2009.0095 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. A second Cretaceous ornithuromorph bird from the Changma Basin, Gansu Province, northwestern China HAI−LU YOU, JESSIE ATTERHOLT, JINGMAI K. O’CONNOR, JERALD D. HARRIS, MATTHEW C. LAMANNA, and DA−QING LI You, H.−L., Atterholt, J., O’Connor, J.K., Harris, J.D., Lamanna, M.C., and Li, D.−Q. 2010. A second Cretaceous ornithuromorph bird from the Changma Basin, Gansu Province, northwestern China. -
Review REVIEW 1: 543–559, 2014 Doi: 10.1093/Nsr/Nwu055 Advance Access Publication 5 September 2014
National Science Review REVIEW 1: 543–559, 2014 doi: 10.1093/nsr/nwu055 Advance access publication 5 September 2014 GEOSCIENCES Special Topic: Paleontology in China The Jehol Biota, an Early Cretaceous terrestrial Lagerstatte:¨ new discoveries and implications Zhonghe Zhou ABSTRACT The study of the Early Cretaceous terrestrial Jehol Biota, which provides a rare window for reconstruction of a Lower Cretaceous terrestrial ecosystem, is reviewed with a focus on some of the latest progress. A newly proposed definition of the biota based on paleoecology and taphonomy is accepted. Although theJehol fossils are mainly preserved in two types of sedimentary rocks, there are various types of preservation with a complex mechanism that remains to be understood. New discoveries of significant taxa from the Jehol Biota, with an updated introduction of its diversity, confirm that the Jehol Biota represents one of themost diversified biotas of the Mesozoic. The evolutionary significance of major biological groups (e.g. dinosaurs, birds, mammals, pterosaurs, insects, and plants) is discussed mainly in the light of recent discoveries, and some of the most remarkable aspects of the biota are highlighted. The global and local geological, paleogeographic, and paleoenvironmental background of the Jehol Biota have contributed to the unique composition, evolution, and preservation of the biota, demonstrating widespread faunal exchanges between Asia and other continents caused by the presence of the Eurasia–North American continental mass and its link to South America, and confirming northeastern China as the origin and diversification center fora variety of Cretaceous biological groups. Although some progress has been made on the reconstruction of the paleotemperature at the time of the Jehol Biota, much more work is needed to confirm a possible link between the remarkable diversity of the biota and the cold intervals during the Early Cretaceous. -
The Molecular Evolution of Feathers with Direct Evidence from Fossils
The molecular evolution of feathers with direct evidence from fossils Yanhong Pana,1, Wenxia Zhengb, Roger H. Sawyerc, Michael W. Penningtond, Xiaoting Zhenge,f, Xiaoli Wange,f, Min Wangg,h, Liang Hua,i, Jingmai O’Connorg,h, Tao Zhaoa, Zhiheng Lig,h, Elena R. Schroeterb, Feixiang Wug,h, Xing Xug,h, Zhonghe Zhoug,h,i,1, and Mary H. Schweitzerb,j,1 aChinese Academy of Sciences Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China; bDepartment of Biological Sciences, North Carolina State University, Raleigh, NC 27695; cDepartment of Biological Sciences, University of South Carolina, Columbia, SC 29205; dAmbioPharm Incorporated, North Augusta, SC 29842; eInstitute of Geology and Paleontology, Lingyi University, Lingyi City, 27605 Shandong, China; fShandong Tianyu Museum of Nature, Pingyi, 273300 Shandong, China; gCAS Key Laboratory of Vertebrate Evolution and Human Origins of the Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, 100044 Beijing, China; hCenter for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, 100044 Beijing, China; iCollege of Earth and Planetary Sciences, University of Chinese Academy of Sciences, 100049 Beijing, China; and jNorth Carolina Museum of Natural Sciences, Raleigh, NC 27601 Contributed by Zhonghe Zhou, December 15, 2018 (sent for review September 12, 2018; reviewed by Dominique G. Homberger and Chenxi Jia) Dinosaur fossils possessing integumentary appendages of various feathers in Anchiornis, barbules that interlock to form feather morphologies, interpreted as feathers, have greatly enhanced our vanes critical for flight have not been identified yet (12). -
Appendix A. Supplementary Material
Appendix A. Supplementary material Comprehensive taxon sampling and vetted fossils help clarify the time tree of shorebirds (Aves, Charadriiformes) David Cernˇ y´ 1,* & Rossy Natale2 1Department of the Geophysical Sciences, University of Chicago, Chicago 60637, USA 2Department of Organismal Biology & Anatomy, University of Chicago, Chicago 60637, USA *Corresponding Author. Email: [email protected] Contents 1 Fossil Calibrations 2 1.1 Calibrations used . .2 1.2 Rejected calibrations . 22 2 Outgroup sequences 30 2.1 Neornithine outgroups . 33 2.2 Non-neornithine outgroups . 39 3 Supplementary Methods 72 4 Supplementary Figures and Tables 74 5 Image Credits 91 References 99 1 1 Fossil Calibrations 1.1 Calibrations used Calibration 1 Node calibrated. MRCA of Uria aalge and Uria lomvia. Fossil taxon. Uria lomvia (Linnaeus, 1758). Specimen. CASG 71892 (referred specimen; Olson, 2013), California Academy of Sciences, San Francisco, CA, USA. Lower bound. 2.58 Ma. Phylogenetic justification. As in Smith (2015). Age justification. The status of CASG 71892 as the oldest known record of either of the two spp. of Uria was recently confirmed by the review of Watanabe et al. (2016). The younger of the two marine transgressions at the Tolstoi Point corresponds to the Bigbendian transgression (Olson, 2013), which contains the Gauss-Matuyama magnetostratigraphic boundary (Kaufman and Brigham-Grette, 1993). Attempts to date this reversal have been recently reviewed by Ohno et al. (2012); Singer (2014), and Head (2019). In particular, Deino et al. (2006) were able to tightly bracket the age of the reversal using high-precision 40Ar/39Ar dating of two tuffs in normally and reversely magnetized lacustrine sediments from Kenya, obtaining a value of 2.589 ± 0.003 Ma. -
Insight Into the Evolution of Avian Flight from a New Clade of Early
J. Anat. (2006) 208, pp287–308 IBlackwnell Publishing sLtd ight into the evolution of avian flight from a new clade of Early Cretaceous ornithurines from China and the morphology of Yixianornis grabaui Julia A. Clarke,1 Zhonghe Zhou2 and Fucheng Zhang2 1Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC, USA 2Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, China Abstract In studies of the evolution of avian flight there has been a singular preoccupation with unravelling its origin. By con- trast, the complex changes in morphology that occurred between the earliest form of avian flapping flight and the emergence of the flight capabilities of extant birds remain comparatively little explored. Any such work has been limited by a comparative paucity of fossils illuminating bird evolution near the origin of the clade of extant (i.e. ‘modern’) birds (Aves). Here we recognize three species from the Early Cretaceous of China as comprising a new lineage of basal ornithurine birds. Ornithurae is a clade that includes, approximately, comparatively close relatives of crown clade Aves (extant birds) and that crown clade. The morphology of the best-preserved specimen from this newly recognized Asian diversity, the holotype specimen of Yixianornis grabaui Zhou and Zhang 2001, complete with finely preserved wing and tail feather impressions, is used to illustrate the new insights offered by recognition of this lineage. Hypotheses of avian morphological evolution and specifically proposed patterns of change in different avian locomotor modules after the origin of flight are impacted by recognition of the new lineage. -
Late Pleistocene Birds from Kingston Saltpeter Cave, Southern Appalachian Mountains, Georgia
Bull. Fla. Mus. Nat. Hist. (2005) 45(4):231-248 231 LATE PLEISTOCENE BIRDS FROM KINGSTON SALTPETER CAVE, SOUTHERN APPALACHIAN MOUNTAINS, GEORGIA David W. Steadman1 Kingston Saltpeter Cave, Bartow County, Georgia, has produced late Quaternary fossils of 38 taxa of birds. The presence of extinct species of mammals, and three radiocarbon dates on mammalian bone collagen ranging from approximately 15,000 to 12,000 Cal B.P., indicate a late Pleistocene age for this fauna, although a small portion of the fossils may be Holocene in age. The birds are dominated by forest or woodland species, especially the Ruffed Grouse (Bonasa umbellus) and Passenger Pigeon (Ectopistes migratorius). Species indicative of brushy or edge habitats, wetlands, and grasslands also are present. They include the Greater Prairie Chicken (Tympanuchus cupido, a grassland indicator) and Black-billed Magpie (Pica pica, characteristic of woody edges bordering grasslands). Both of these species reside today no closer than 1000+ km to the west (mainly northwest) of Georgia. An enigmatic owl, perhaps extinct and undescribed, is represented by two juvenile tarsometatarsi. The avifauna of Kingston Saltpeter Cave suggests that deciduous or mixed deciduous/coniferous forests and woodlands were the dominant habitats in the late Pleistocene of southernmost Appalachia, with wetlands and grasslands present as well. Key Words: Georgia; late Pleistocene; southern Appalachians; Aves; extralocal species; faunal change INTRODUCTION dates have been determined from mammal bones at Numerous late Pleistocene vertebrate faunas have been KSC. The first (10,300 ± 130 yr B.P.; Beta-12771, un- recovered from caves and other karst features of the corrected for 13C/12C; = 12,850 – 11,350 Cal B.P.) is Appalachian region (listed in Lundelius et al. -
Additional Specimen of Microraptor Provides Unique Evidence of Dinosaurs Preying on Birds
Additional specimen of Microraptor provides unique evidence of dinosaurs preying on birds Jingmai O’Connor1, Zhonghe Zhou1, and Xing Xu Key Laboratory of Evolutionary Systematics of Vertebrates, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China Contributed by Zhonghe Zhou, October 28, 2011 (sent for review September 13, 2011) Preserved indicators of diet are extremely rare in the fossil record; The vertebral column of this specimen is complete except for even more so is unequivocal direct evidence for predator–prey its proximal and distal ends; pleurocoels are absent from the relationships. Here, we report on a unique specimen of the small thoracic vertebrae, as in dromaeosaurids and basal birds. Poor nonavian theropod Microraptor gui from the Early Cretaceous preservation prevents clear observation of sutures; however, Jehol biota, China, which has the remains of an adult enantiorni- there does not appear to be any separation between the neural thine bird preserved in its abdomen, most likely not scavenged, arches and vertebral centra, or any other indicators that the but captured and consumed by the dinosaur. We provide direct specimen is a juvenile. The number of caudal vertebrae cannot evidence for the dietary preferences of Microraptor and a nonavian be estimated, but the elongate distal caudals are tightly bounded dinosaur feeding on a bird. Further, because Jehol enantiorni- by elongated zygapophyses, as in other dromaeosaurids. The rib thines were distinctly arboreal, in contrast to their cursorial orni- cage is nearly completely preserved; both right and left sides are thurine counterparts, this fossil suggests that Microraptor hunted visible ventrally closed by the articulated gastral basket. -
Sind Vögel Dinosaurier? Eine Kritische Analyse Fossiler Befunde
W+W Special Paper B-19-4 SIND VÖGEL DINOSAURIER? EINE KRITISCHE ANALYSE FOSSILER BEFUNDE Reinhard Junker August 2019 https://www.wort-und-wissen.de/artikel/sp/b-19-4_dinos-voegel.pdf Bild: Ein rekonstruiertes und künstlerisch dargestelltes Paar von Microraptor gui (Dromaeosauridae , Micro raptorinae). (durbed.deviantart.com, CC BY-SA 3.0) Sind Vögel Dinosaurier? Inhalt 1. Einleitung ...................................................................................... 3. kompakt ..................................................................................................... 4 Methodische Vorbemerkungen ............................................................................... 5 Zitate zu schrittweisem Erwerb von Vogelmerkmalen ...................................................... 6 2. Vogelmerkmale bei Theropoden: Vorläufer oder Konvergenzen ............................................................................... 9 2.1 Federtypen und Flugfähigkeit ..................................................................... 9 2.2 Zähne und Schnabel ................................................................................ 14 Zitate zu Konvergenzen bei Zahnverlust und Ausbildung eines Schnabels ................15 2.3 Gehirn und EQ ........................................................................................ 17 2.4 Furkula ..................................................................................................... 18 2.5 Gastralia, Rippenkorb, Brustbein ..............................................................