The Renaissance of Avian Paleontology and Its Bearing on the Higher-Level Phylogeny of Birds
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Flamingo ABOUT the GROUP
Flamingo ABOUT THE GROUP Bulletin of the IUCN-SSC/Wetlands International The Flamingo Specialist Group (FSG) was established in 1978 at Tour du Valat in France, under the leadership of Dr. Alan Johnson, who coordinated the group until 2004 (see profile at www.wetlands.org/networks/Profiles/January.htm). Currently, the group is FLAMINGO SPECIALIST GROUP coordinated from the Wildfowl & Wetlands Trust at Slimbridge, UK, as part of the IUCN- SSC/Wetlands International Waterbird Network. The FSG is a global network of flamingo specialists (both scientists and non- scientists) concerned with the study, monitoring, management and conservation of the world’s six flamingo species populations. Its role is to actively promote flamingo research and conservation worldwide by encouraging information exchange and cooperation amongst these specialists, and with other relevant organisations, particularly IUCN - SSC, Ramsar, WWF International and BirdLife International. FSG members include experts in both in-situ (wild) and ex-situ (captive) flamingo conservation, as well as in fields ranging from field surveys to breeding biology, diseases, tracking movements and data management. There are currently 165 members around the world, from India to Chile, and from France to South Africa. Further information about the FSG, its membership, the membership list serve, or this bulletin can be obtained from Brooks Childress at the address below. Chair Assistant Chair Dr. Brooks Childress Mr. Nigel Jarrett Wildfowl & Wetlands Trust Wildfowl & Wetlands Trust Slimbridge Slimbridge Glos. GL2 7BT, UK Glos. GL2 7BT, UK Tel: +44 (0)1453 860437 Tel: +44 (0)1453 891177 Fax: +44 (0)1453 860437 Fax: +44 (0)1453 890827 [email protected] [email protected] Eastern Hemisphere Chair Western Hemisphere Chair Dr. -
Uropygial Gland in Birds
UROPYGIAL GLAND IN BIRDS Prepared by Dr. Subhadeep Sarker Associate Professor, Department of Zoology, Serampore College Occurrence and Location: • The uropygial gland, often referred to as the oil or preen gland, is a bilobed gland and is found at the dorsal base of the tail of most psittacine birds. • The uropygial gland is a median dorsal gland, one per bird, in the synsacro-caudal region. A half moon-shaped row of feather follicles of the upper median and major tail coverts externally outline its position. • The uropygial area is located dorsally over the pygostyle on the midline at the base of the tail. • This gland is most developed in waterfowl but very reduced or even absent in many parrots (e.g. Amazon parrots), ostriches and many pigeons and doves. Anatomy: • The uropygial gland is an epidermal bilobed holocrine gland localized on the uropygium of most birds. • It is composed of two lobes separated by an interlobular septum and covered by an external capsule. • Uropygial secretory tissue is housed within the lobes of the gland (Lobus glandulae uropygialis), which are nearly always two in number. Exceptions occur in Hoopoe (Upupa epops) with three lobes, and owls with one. Duct and cavity systems are also contained within the lobes. • The architectural patterns formed by the secretory tubules, the cavities and ducts, differ markedly among species. The primary cavity can comprise over 90% of lobe volume in the Oilbird (Steatornis caripensis) and some woodpeckers and pigeons. • The gland is covered by a circlet or tuft of down feathers called the uropygial wick in many birds. -
Onetouch 4.0 Scanned Documents
/ Chapter 2 THE FOSSIL RECORD OF BIRDS Storrs L. Olson Department of Vertebrate Zoology National Museum of Natural History Smithsonian Institution Washington, DC. I. Introduction 80 II. Archaeopteryx 85 III. Early Cretaceous Birds 87 IV. Hesperornithiformes 89 V. Ichthyornithiformes 91 VI. Other Mesozojc Birds 92 VII. Paleognathous Birds 96 A. The Problem of the Origins of Paleognathous Birds 96 B. The Fossil Record of Paleognathous Birds 104 VIII. The "Basal" Land Bird Assemblage 107 A. Opisthocomidae 109 B. Musophagidae 109 C. Cuculidae HO D. Falconidae HI E. Sagittariidae 112 F. Accipitridae 112 G. Pandionidae 114 H. Galliformes 114 1. Family Incertae Sedis Turnicidae 119 J. Columbiformes 119 K. Psittaciforines 120 L. Family Incertae Sedis Zygodactylidae 121 IX. The "Higher" Land Bird Assemblage 122 A. Coliiformes 124 B. Coraciiformes (Including Trogonidae and Galbulae) 124 C. Strigiformes 129 D. Caprimulgiformes 132 E. Apodiformes 134 F. Family Incertae Sedis Trochilidae 135 G. Order Incertae Sedis Bucerotiformes (Including Upupae) 136 H. Piciformes 138 I. Passeriformes 139 X. The Water Bird Assemblage 141 A. Gruiformes 142 B. Family Incertae Sedis Ardeidae 165 79 Avian Biology, Vol. Vlll ISBN 0-12-249408-3 80 STORES L. OLSON C. Family Incertae Sedis Podicipedidae 168 D. Charadriiformes 169 E. Anseriformes 186 F. Ciconiiformes 188 G. Pelecaniformes 192 H. Procellariiformes 208 I. Gaviiformes 212 J. Sphenisciformes 217 XI. Conclusion 217 References 218 I. Introduction Avian paleontology has long been a poor stepsister to its mammalian counterpart, a fact that may be attributed in some measure to an insufRcien- cy of qualified workers and to the absence in birds of heterodont teeth, on which the greater proportion of the fossil record of mammals is founded. -
A Skull of a Very Large Crane from the Late Miocene of Southern Germany, with Notes on the Phylogenetic Interrelationships of Extant Gruinae
Journal of Ornithology https://doi.org/10.1007/s10336-020-01799-0 ORIGINAL ARTICLE A skull of a very large crane from the late Miocene of Southern Germany, with notes on the phylogenetic interrelationships of extant Gruinae Gerald Mayr1 · Thomas Lechner2 · Madelaine Böhme2 Received: 3 June 2020 / Revised: 1 July 2020 / Accepted: 2 July 2020 © The Author(s) 2020 Abstract We describe a partial skull of a very large crane from the early late Miocene (Tortonian) hominid locality Hammerschmiede in southern Germany, which is the oldest fossil record of the Gruinae (true cranes). The fossil exhibits an unusual preservation in that only the dorsal portions of the neurocranium and beak are preserved. Even though it is, therefore, very fragmentary, two morphological characteristics are striking and of paleobiological signifcance: its large size and the very long beak. The fossil is from a species the size of the largest extant cranes and represents the earliest record of a large-sized crane in Europe. Overall, the specimen resembles the skull of the extant, very long-beaked Siberian Crane, Leucogeranus leucogeranus, but its afnities within Gruinae cannot be determined owing to the incomplete preservation. Judging from its size, the fossil may possibly belong to the very large “Grus” pentelici, which stems from temporally and geographically proximate sites. The long beak of the Hammerschmiede crane conforms to an open freshwater paleohabitat, which prevailed at the locality. Keywords Aves · Evolution · Gruidae · Systematics · Tortonian Zusammenfassung Ein Schädel eines sehr großen Kranichs aus dem Obermiozän Süddeutschlands, mit Bemerkungen zu den Verwandtschaftsbeziehungen heutiger Gruinae Wir beschreiben einen partiell erhaltenen Schädel eines sehr großen Kranichs aus dem frühen Obermiozän (Tortonium) der Hominiden-Fundstelle Hammerschmiede in Süddeutschland, welcher den ältesten Fossilnachweis der Gruinae (echte Kraniche) repräsentiert. -
Ichnotaxonomy of the Eocene Green River Formation
Ichnotaxonomy of the Eocene Green River Formation, Soldier Summit and Spanish Fork Canyon, Uinta Basin, Utah: Interpreting behaviors, lifestyles, and erecting the Cochlichnus Ichnofacies By © 2018 Joshua D. Hogue B.S. Old Dominion University, 2013 Submitted to the graduate degree program in Geology and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements for the degree of Master of Science. Chair: Dr. Stephen T. Hasiotis Dr. Paul Selden Dr. Georgios Tsoflias Date Defended: May 1, 2018 ii The thesis committee for Joshua D. Hogue certifies that this is the approved version of the following thesis: Ichnotaxonomy of the Eocene Green River Formation, Soldier Summit and Spanish Fork Canyon, Uinta Basin, Utah: Interpreting behaviors, lifestyles, and erecting the Cochlichnus Ichnofacies Chair: Dr. Stephen T. Hasiotis Date Approved: May 1, 2018 iii ABSTRACT The Eocene Green River Formation in the Uinta Basin, Utah, has a diverse ichnofauna. Nineteen ichnogenera and 26 ichnospecies were identified: Acanthichnus cursorius, Alaripeda lofgreni, c.f. Aquatilavipes isp., Aulichnites (A. parkerensis and A. tsouloufeidos isp. nov.), Aviadactyla (c.f. Av. isp. and Av. vialovi), Avipeda phoenix, Cochlichnus (C. anguineus and C. plegmaeidos isp. nov.), Conichnus conichnus, Fuscinapeda texana, Glaciichnium liebegastensis, Glaroseidosichnus ign. nov. gierlowskii isp. nov., Gruipeda (G. fuenzalidae and G. gryponyx), Midorikawapeda ign. nov. semipalmatus isp. nov., Planolites montanus, Presbyorniformipes feduccii, Protovirgularia dichotoma, Sagittichnus linki, Treptichnus (T. bifurcus, T. pedum, and T. vagans), and Tsalavoutichnus ign. nov. (Ts. ericksonii isp. nov. and Ts. leptomonopati isp. nov.). Four ichnocoenoses are represented by the ichnofossils—Cochlichnus, Conichnus, Presbyorniformipes, and Treptichnus—representing dwelling, feeding, grazing, locomotion, predation, pupation, and resting behaviors of organisms in environments at and around the sediment-water-air interface. -
Sex Recognition by Odour and Variation in the Uropygial Gland Secretion In
1 Sex recognition by odour and variation in the uropygial gland secretion in 2 starlings 3 4 Luisa Amo1, Jesús Miguel Avilés1, Deseada Parejo1, Aránzazu Peña2, Juan Rodríguez1, 5 Gustavo Tomás1 6 7 1 Departamento de Ecología Funcional y Evolutiva, Estación Experimental de Zonas 8 Áridas (CSIC), Carretera de Sacramento s/n, E-04120, La Cañada de San Urbano, 9 Almería, Spain. 10 2 Instituto Andaluz de Ciencias de la Tierra (IACT, CSIC-UGR), Avda de las Palmeras, 11 4, 18100, Armilla, Granada, Spain. 12 13 *corresponding author: Luisa Amo. Departamento de Ecología Funcional y Evolutiva, 14 Estación Experimental de Zonas Áridas (CSIC), Carretera de Sacramento s/n, E-04120, 15 La Cañada de San Urbano, Almería, Spain. E-mail: [email protected] 16 17 18 Running headline: Odour-based sex recognition in a bird 19 20 2 21 1. Although a growing body of evidence supports that olfaction based on chemical 22 compounds emitted by birds may play a role in individual recognition, the possible role 23 of chemical cues in sexual selection of birds has been only preliminarily studied. 24 2. We investigated for the first time whether a passerine bird, the spotless starling 25 Sturnus unicolor, was able to discriminate the sex of conspecifics by using olfactory 26 cues and whether the size and secretion composition of the uropygial gland convey 27 information on sex, age and reproductive status in this species. 28 3. We performed a blind choice experiment during mating and we found that starlings 29 were able to discriminate the sex of conspecifics by using chemical cues alone. -
Fossil Birds of the Nebraska Region
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Transactions of the Nebraska Academy of Sciences and Affiliated Societies Nebraska Academy of Sciences 1992 Fossil Birds of the Nebraska Region James E. Ducey [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/tnas Part of the Life Sciences Commons Ducey, James E., "Fossil Birds of the Nebraska Region" (1992). Transactions of the Nebraska Academy of Sciences and Affiliated Societies. 130. https://digitalcommons.unl.edu/tnas/130 This Article is brought to you for free and open access by the Nebraska Academy of Sciences at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Transactions of the Nebraska Academy of Sciences and Affiliated Societiesy b an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. 1992. Transactions of the Nebraska Academy of Sciences, XIX: 83-96 FOSSIL BIRDS OF THE NEBRASKA REGION James Ducey 235 Nebraska Hall Lincoln, Nebraska 68588-0521 ABSTRACT Crane (Grus haydeni = Grus canadensis) (Marsh, 1870) and a species of hawk (Buteo dananus) from along the This review compiles published and a few unpublished Loup Fork (Marsh, 1871). records offossil and prehistoric birds for the Nebraska region (Nebraska and parts of adjacent states) from the Cretaceous Many ofthe species first described were from mate Period to the late Pleistocene, about 12,000 years before present. Species recorded during the various epochs include: rial collected in the Great Plains region, including Kan Oligocene and Early Miocene (13 families; 29 species), Middle sas and Wyoming (Marsh, 1872b). The work of scien Miocene (six families; 12 species), Late Miocene (14 families; tists associated with the University of Nebraska in 21 species), Pliocene (six families; 15 species), Early-Middle cluded studies made around the turn-of-the-century. -
Feather Mite Abundance Increases with Uropygial
Ibis (2006), 148, 687–697 FeatherBlackwell Publishing Ltd mite abundance increases with uropygial gland size and plumage yellowness in Great Tits Parus major ISMAEL GALVÁN* & JUAN J. SANZ Departamento de Ecología Evolutiva, Museo Nacional de Ciencias Naturales (CSIC), José Gutiérrez Abascal 2, E-28006 Madrid, Spain Plumicolous feather mites are ectosymbiotic organisms that live on bird feathers. Despite their abundance and prevalence among birds, the ecology of the interaction between these organisms and their hosts is poorly known. As feather mites feed on oil that birds spread from their uropygial gland, it has been hypothesized, but never tested, that the number of feather mites increases with the size of the uropygial gland of their hosts. In this study the number of feather mites is considered with respect to uropygial gland size in a breeding popu- lation of Great Tits Parus major in order to test this hypothesis. As predicted, the number of feather mites correlated positively with the uropygial gland size of their hosts, showing for the first time that uropygial gland size can explain the variance in feather mite load among conspecifics. Previous studies relating feather mite load to plumage colour have suggested that feather mites may be parasitic or neutral. To confirm this, the yellowness of breast feath- ers was also assessed. However, the results ran in the opposite direction to that expected, showing a positive correlation between mite load and plumage yellowness, which suggests that further work is needed to give clear evidence for a specific nature of feather mites. How- ever, Great Tits with higher mite loads had lower hatching and breeding success, which may support the idea that feather mites are parasites, although this effect must be taken with caution because it was only found in males. -
X Congreso Argentino De Paleontología Y Bioestratigrafía VII Congreso Latinoamericano De Paleontología La Plata, Argentina - Septiembre De 2010
X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 Financian Auspician 1 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 2 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 3 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 X Congreso Argentino de Paleontología y Bioestratigrafía y VII Congreso Latinoamericano de Paleontología Resúmenes/coordinado por Sara Ballent ; Analia Artabe ; Franco Tortello. 1a ed. - La Plata: Museo de la Plata; Museo de la Plata, 2010. 238 p. + CD-ROM; 28x20 cm. ISBN 978-987-95849-7-2 1. Paleontología. 2. Bioestratigrafía. I. Ballent, Sara , coord. II. Artabe, Analia, coord. III. Tortello, Franco, coord. CDD 560 Fecha de catalogación: 27/08/2010 4 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología Declarado de Interés Municipal, La Plata (Decreto N° 1158) 5 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 6 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología Prólogo Una vez más el Congreso Argentino de Paleontología y Bioestratigrafía y el Congreso Latino- americano de Paleontología se realizan de manera conjunta. -
Fused Thoracic Vertebrae in Birds: Their Occurrence and Possible Significance
J. Yamashina Inst. Ornith., 14: 86-95, 1982 Fused Thoracic Vertebrae in Birds: Their Occurrence and Possible Significance Robert W. Storer* Abstract The notarium, a group of fused thoracic vertebrae, is characteristic of birds of five orders and is found in one or more families of five more orders of non-passerine birds . Sixteen patterns of variation in the number of vertebrae in the notarium and of unfused vertebrae between it and the synsacrum were found. The occurrence of these patterns in the groups having a notarium is tabulated. Selective factors favoring the evolution of fusion of these vertebrae may have included the shock induced by landing on hard substrates or of striking prey and the prevention of downward bending of the ends of the thoracic portion of vertebral column while the birds are in flight. Phylogenetic implications of the presence of a notarium in several groups are discussed. The notarium of Os dorsale of birds is a group of fused thoracic vertebrae usually separated by one or more unfused vertebrae from the anteriormost vertebra of the synsacrum (Baumel 1979: 93, 112). Although it was described and figured as early as 1856 (Barkow 1856: pl. II), I have found little more than casual mention of it in the literature. It therefore seems worthwhile to survey the distribution of this structure among the orders and families of birds, to describe the variation in the numbers of vertebrae in the notarium and between it and the synsacrum, to speculate on its possible adaptive significance, and to discuss phylogenetic implications of its presence. -
Basic Avian Anatomy
Basic Avian Anatomy Peter S. Sakas DVM, MS Niles Animal Hospital and Bird Medical Center 7278 N. Milwaukee Ave. Niles, IL 60714 (847)-647-9325 FAX (847)-647-8498 Introduction Everyone is familiar with the anatomy of mammals and may also have some knowledge of a few avian anatomical characteristics. The purpose of this discussion is to provide a deeper insight into avian anatomy and provide some comparisons to mammalian features. An understanding of avian anatomy is essential for avian practitioners. Sources of information for this discussion include the fine work of Dr. Howard Evans and Dr. Robert Clipsham. Feathers Feathers are unique to birds. Birds grow feathers in and around eight well- defined feather tracts or pterylae; they are not haphazardly arranged. Feathers compromise from 10-20% of a bird’s body weight. Each feather can be raised by a separate skin muscle (‘raising their hackles’ or fanning tail).Feathers are outgrowths of the feather follicles of the skin and are the counterpart to hairs and hair follicles in mammals. Feathers provide many functions for birds, attracts mate or deceives predator, heat control, flight, aerodynamic streamlining and water buoyancy. Feathers are not really “bird hairs” but are probably modified scales passed down from their reptilian ancestors. Feathers can be grouped into three categories: 1) Contour feathers or penna – These feathers cover the body, wings and tail, and are the feathers most obviously visible on the bird. 2) Down feathers or plumules – These tiny, soft down feathers are found associated with contour feathers and/or the spaces between them. 3) Tufted bristle feathers or filoplumes- Feathers which are modified and appear as ‘eyelashes and nose hairs.’ Contour Feathers The contour feather consists of a shaft with a vane. -
Fish Remains, Mostly Otoliths, from the Non−Marine Early Miocene of Otago, New Zealand
Fish remains, mostly otoliths, from the non−marine early Miocene of Otago, New Zealand WERNER SCHWARZHANS, R. PAUL SCOFIELD, ALAN J.D. TENNYSON, JENNIFER P. WORTHY, and TREVOR H. WORTHY Schwarzhans, W., Scofield, R.P., Tennyson, A.J.D., Worthy, J.P., and Worthy, T.H. 2012. Fish remains, mostly otoliths, from the non−marine early Miocene of Otago, New Zealand. Acta Palaeontologica Polonica 57 (2): 319–350. Fish remains described from the early Miocene lacustrine Bannockburn Formation of Central Otago, New Zealand, con− sist of several thousand otoliths and one skeleton plus another disintegrated skull. One species, Mataichthys bictenatus Schwarzhans, Scofield, Tennyson, and T. Worthy gen. et sp. nov., an eleotrid, is established on a skeleton with otoliths in situ. The soft embedding rock and delicate, three−dimensionally preserved fish bones were studied by CT−scanning tech− nology rather than physical preparation, except where needed to extract the otolith. Fourteen species of fishes are de− scribed, 12 new to science and two in open nomenclature, representing the families Galaxiidae (Galaxias angustiventris, G. bobmcdowalli, G. brevicauda, G. papilionis, G. parvirostris, G. tabidus), Retropinnidae (Prototroctes modestus, P. vertex), and Eleotridae (Mataichthys bictenatus, M. procerus, M. rhinoceros, M. taurinus). These findings prove that most of the current endemic New Zealand/southern Australia freshwater fish fauna was firmly established in New Zea− land as early as 19–16 Ma ago. Most fish species indicate the presence of large fishes, in some cases larger than Recent species of related taxa, for instance in the eleotrid genus Mataichthys when compared to the extant Gobiomorphus. The finding of a few otoliths from marine fishes corroborates the age determination of the Bannockburn Formation as the Altonian stage of the New Zealand marine Tertiary stratigraphy.