Big-Time Insights from a Tiny Bird Fossil Daniel J
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Climatic Shifts Drove Major Contractions in Avian Latitudinal Distributions Throughout the Cenozoic
Climatic shifts drove major contractions in avian latitudinal distributions throughout the Cenozoic Erin E. Saupea,1,2, Alexander Farnsworthb, Daniel J. Luntb, Navjit Sagooc, Karen V. Phamd, and Daniel J. Fielde,1,2 aDepartment of Earth Sciences, University of Oxford, OX1 3AN Oxford, United Kingdom; bSchool of Geographical Sciences, University of Bristol, Clifton, BS8 1SS Bristol, United Kingdom; cDepartment of Meteorology, Stockholm University, 106 91 Stockholm, Sweden; dDivision of Geological and Planetary Sciences, Caltech, Pasadena, CA 91125; and eDepartment of Earth Sciences, University of Cambridge, CB2 3EQ Cambridge, United Kingdom Edited by Nils Chr. Stenseth, University of Oslo, Oslo, Norway, and approved May 7, 2019 (received for review March 8, 2019) Many higher level avian clades are restricted to Earth’s lower lati- order avian historical biogeography invariably recover strong evi- tudes, leading to historical biogeographic reconstructions favoring a dence for an origin of most modern diversity on southern land- Gondwanan origin of crown birds and numerous deep subclades. masses (2, 6, 11). However, several such “tropical-restricted” clades (TRCs) are repre- The crown bird fossil record has unique potential to reveal sented by stem-lineage fossils well outside the ranges of their clos- where different groups of birds were formerly distributed in deep est living relatives, often on northern continents. To assess the time. Fossil evidence, for example, has long indicated that total- drivers of these geographic disjunctions, we combined ecological group representatives of clades restricted to relatively narrow niche modeling, paleoclimate models, and the early Cenozoic fossil geographic regions today were formerly found in different parts of record to examine the influence of climatic change on avian geo- – graphic distributions over the last ∼56 million years. -
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/ 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. -
Reported to Have Been Five Or Six Meters High at the Advent of the Present· Residents of the Region
THE TERTIARY LAKE BASIN AT ~FLORISSANT, COLO., BETWEEN SOUTH AND HAYDEN PAHKS.* I [With a map.] By SAMUEL H. SCUDDER. The following remarks are based upon collections. and notes made during a visit to Florissa:qt, in the summer of 1877, in compap.y ·with Messrs. Arthur Lakes, of Golden, Colo., and F. C. Bowditch, of Boston, . Mass. As five days only were spent in the place, most of the time was . given up to the collection and care of specimens, .so that only a general survey of the locality was·possible. Mr. Lakes ·especially gave himself to the· study of the geol9gy of the district, and as he was previously fttrniliar with the structure of the surrounding country, and placed his notes at my disposal, the first part of this paper should be considered our joint production. GEOLOGY. The tertiary lalw basin at Florissant, already famous for its prolific beds of plants and insects, is situated ina narrow valley high up in the mountains at the soethern extremity of the Front Range of Colorado, at no great distance from "Pike's Peak. The first, and, so fat· as I am aware, the only notice of it which has been published, is that lJy Mr. A. C. Peale, in his account of the geology of Hayden Park and the country lying between it and the upper canon of the South Platte. .t As it is brief, it is given here in full: . ''The latter [Beaver Creek] flows to the northwest, and empties into the South Platte just below the upper canon. -
Supplementary Information
Supplementary Information Substitution Rate Variation in a Robust Procellariiform Seabird Phylogeny is not Solely Explained by Body Mass, Flight Efficiency, Population Size or Life History Traits Andrea Estandía, R. Terry Chesser, Helen F. James, Max A. Levy, Joan Ferrer Obiol, Vincent Bretagnolle, Jacob González-Solís, Andreanna J. Welch This pdf file includes: Supplementary Information Text Figures S1-S7 SUPPLEMENTARY INFORMATION TEXT Fossil calibrations The fossil record of Procellariiformes is sparse when compared with other bird orders, especially its sister order Sphenisciformes (Ksepka & Clarke 2010, Olson 1985c). There are, however, some fossil Procellariiformes that are both robustly dated and identified and therefore suitable for fossil calibrations. Our justification of these fossils, below, follows best practices described by Parham et al. (2012) where possible. For all calibration points only a minimum age was set with no upper constraint specified, except for the root of the tree. 1. Node between Sphenisciformes/Procellariiformes Minimum age: 60.5 Ma Maximum age: 61.5 Ma Taxon and specimen: Waimanu manneringi (Slack et al. 2006); CM zfa35 (Canterbury Museum, Christchurch, New Zealand), holotype comprising thoracic vertebrae, caudal vertebrae, pelvis, femur, tibiotarsus, and tarsometatarsus. Locality: Basal Waipara Greensand, Waipara River, New Zealand. Phylogenetic justification: Waimanu has been resolved as the basal penguin taxon using morphological data (Slack et al. 2006), as well as combined morphological and molecular datasets (Ksepka et al. 2006, Clarke et al. 2007). Morphological and molecular phylogenies agree on the monophyly of Sphenisciformes and Procellariiformes (Livezey & Zusi 2007, Prum et al. 2015). Waimanu manneringi was previously used by Prum et al. (2015) to calibrate Sphenisiciformes, and see Ksepka & Clarke (2015) for a review of the utility of this fossil as a robust calibration point. -
A North American Stem Turaco, and the Complex Biogeographic History of Modern Birds Daniel J
Field and Hsiang BMC Evolutionary Biology (2018) 18:102 https://doi.org/10.1186/s12862-018-1212-3 RESEARCHARTICLE Open Access A North American stem turaco, and the complex biogeographic history of modern birds Daniel J. Field1,2* and Allison Y. Hsiang2,3 Abstract Background: Earth’s lower latitudes boast the majority of extant avian species-level and higher-order diversity, with many deeply diverging clades restricted to vestiges of Gondwana. However, palaeontological analyses reveal that many avian crown clades with restricted extant distributions had stem group relatives in very different parts of the world. Results: Our phylogenetic analyses support the enigmatic fossil bird Foro panarium Olson 1992 from the early Eocene (Wasatchian) of Wyoming as a stem turaco (Neornithes: Pan-Musophagidae), a clade that is presently endemic to sub-Saharan Africa. Our analyses offer the first well-supported evidence for a stem musophagid (and therefore a useful fossil calibration for avian molecular divergence analyses), and reveal surprising new information on the early morphology and biogeography of this clade. Total-clade Musophagidae is identified as a potential participant in dispersal via the recently proposed ‘North American Gateway’ during the Palaeogene, and new biogeographic analyses illustrate the importance of the fossil record in revealing the complex historical biogeography of crown birds across geological timescales. Conclusions: In the Palaeogene, total-clade Musophagidae was distributed well outside the range of crown Musophagidae in the present day. This observation is consistent with similar biogeographic observations for numerous other modern bird clades, illustrating shortcomings of historical biogeographic analyses that do not incorporate information from the avian fossil record. -
Ancient Seabird Discovery Suggests Paleogene Bird Diversification 31 January 2014
Ancient seabird discovery suggests Paleogene bird diversification 31 January 2014 Bones of a previously unknown species prove to Provided by Taylor & Francis be one of the oldest seabirds. Fossils discovered in Canterbury, New Zealand reveal the nature of one of the world's oldest flying seabirds. Thought to have lived between 60.5 and 61.6 million years ago, the fossil is suggested to have formed shortly after the extinction of dinosaurs and many marine organisms. Bones of the bird were discovered in 2009 by Leigh Love, an amateur fossil collector. The new species, Australornis lovei has been named as such in honour of Love's discovery. The bird lacks key morphological features of penguins, though it was found near the fossils of the Waimanu manneringi, the oldest penguin, of which it is also estimated to be the same age. The research is published in Journal of the Royal Society of New Zealand by Dr Gerald Mayr and Dr Paul Scofield. The authors claim the discovery 'represents one of the most significant records of a marine Paleocene bird from the Southern Hemisphere' and supports the 'emerging view that most modern birds were already diversified in the earliest Paleogene'. Despite the distinctness of this new species, its derived features are not limited to a single bird group. It does resemble an extinct species from Antarctica, however, highlighting the links between Antarctica and New Zealand in the late Cretaceous period. More information: G Mayr & RP Scofield, "First diagnosable non-sphenisciform bird from the early Paleocene of New Zealand." Journal of the Royal Society of New Zealand, DOI: 10.1080/03036758.2013.863788 1 / 2 APA citation: Ancient seabird discovery suggests Paleogene bird diversification (2014, January 31) retrieved 27 September 2021 from https://phys.org/news/2014-01-ancient-seabird-discovery-paleogene- bird.html This document is subject to copyright. -
Bird Fossils from the Takatika Grit, Chatham Island
BIRD FOSSILS FROM THE TAKATIKA GRIT, CHATHAM ISLAND, NEW ZEALAND A thesis submitted in partial fulfilment of the requirements for the Degree of Master of Science in Geology At the University of Canterbury By Jacob Christopher Blokland University of Canterbury 2017 Figure I: An interpretation of Archaeodyptes stilwelli. Original artwork by Jacob Blokland. i ACKNOWLEDGEMENTS The last couple years have been exciting and challenging. It has been a pleasure to work with great people, and be involved with new research that will hopefully be of contribution to science. First of all, I would like to thank my two supervisors, Dr Catherine Reid and Dr Paul Scofield, for tirelessly reviewing my work and providing feedback. I literally could not have done it without you, and your time, patience and efforts are very much appreciated. Thank you for providing me with the opportunity to do a vertebrate palaeontology based thesis. I would like to extend my deepest gratitude to Catherine for encouragement regarding my interest in palaeontology since before I was an undergraduate, and providing great information regarding thesis and scientific format. I am also extremely grateful to Paul for welcoming me to use specimens from Canterbury Museum, and providing useful information and recommendations for this project through your expertise in this particular discipline. I would also like to thank Associate Professor Jeffrey Stilwell for collecting the fossil specimens used in this thesis, and for the information you passed on regarding the details of the fossils. Thank you to Geoffrey Guinard for allowing me to use your data from your published research in this study. -
A Record of a Landbird (Telluraves) from the Eocene Ikovo Locality (East Ukraine)
Acta zoologica cracoviensia, 59(1) 2016 ISSN 2299-6060, e-ISSN 2300-0163 Kraków, 28 October, 2016 doi:10.3409/azc.59_1.37 Ó Institute of Systematics and Evolution of Animals, PAS A record of a landbird (Telluraves) from the Eocene Ikovo locality (East Ukraine) Evgeniy ZVONOK and Leonid GOROBETS Received: 06 June 2016. Accepted: 30 August 2016. Available online: 14 September 2016. ZVONOK E., GOROBETS L. 2016. A record of a landbird (Telluraves) from the Eocene Ikovo locality (East Ukraine). Acta zool. cracov., 59(1): 37-45. Abstract. First remains of a landbird from the Eocene (Lutetian) marine deposits of the Ikovo locality in Ukraine are described here. These include a single coracoid bone of an imma- ture individual. The coracoid exhibits a combination of traits that is unknown in other spe- cies of birds. However, a more complete individual is required to decide if there is a new species of extinct bird. The described specimen exhibits traits comparable to those of the Telluraves clade and is most similar to the Eocene leptosomid Plesiocathartes. Key words: Lutetian, Ukraine, Telluraves, coracoid, Plesiocathartes. * Evgeniy ZVONOK, Taras Shevchenko University, Department of Geography, Oboronnaya st. 2, Luhansk 91011, Ukraine. E-mail: [email protected] Leonid GOROBETS, National Museum of Natural History at the National Academy of Sci- ences of Ukraine, Department of Paleontology, Bohdan Khmelnitsky st. 15, Kyiv 199034, Ukraine; Taras Shevchenko National University of Kyiv, Department of Ecology and En- vironmental Protection, Volodymyrska st. 64/13, Kyiv 01601, Ukraine. E-mail: [email protected] I. INTRODUCTION The assemblage of birds from the Ikovo locality, Luhansk Region, Ukraine (49°31¢42¢¢ N, 39°3¢59.5¢¢ E; lower Lutetian; Fig. -
Phylogenetically Vetted and Stratigraphically Constrained Fossil Calibrations Within Aves
Palaeontologia Electronica palaeo-electronica.org Phylogenetically vetted and stratigraphically constrained fossil calibrations within Aves Daniel Ksepka and Julia Clarke ABSTRACT Understanding the timing of the crown radiation of birds is a major goal of avian molecular systematists and paleontologists. Despite the availability of ever-larger molecular datasets and increasingly sophisticated methods for phylogeny reconstruc- tion and divergence time estimation, relatively little attention has been paid to outlining and applying fossil calibrations. As the avian fossil record has become better sampled, and more extinct taxa have been incorporated into a phylogenetic framework, the potential for this record to serve as a powerful source of temporal data for divergence dating analyses has increased. Nonetheless, the desire for abundant calibrations must be balanced by careful vetting of candidate fossils, especially given the prevalence of inaccurate fossil calibrations in the recent past. In this contribution, we provide seven phylogenetically vetted fossil calibrations for major divergences within crown Aves rep- resenting the splits between (1) Anatoidea, (2) Sphenisciformes, (3) Coracioidea, (4) Apodidae, (5) Coliiformes, (6) Psittaciformes, and (7) Upupiformes, and the respective extant sister taxon for each of these clades. Each calibration is based an individual specimen, which maintains the clearest possible chain of inference for converting the relevant stratigraphic horizon to a numerical date. Minimum ages for each fossil are tightly constrained and incorporate associated dating errors, and the distributions of younger fossils from the clades of interest are summarized to provide a starting point for workers interested in estimating confidence intervals or outlining prior age distribu- tion curves. Daniel Ksepka. National Evolutionary Synthesis Center, Durham, North Carolina, 27706, USA. -
Phylogenetic Characters in the Humerus and Tarsometatarsus of Penguins
vol. 35, no. 3, pp. 469–496, 2014 doi: 10.2478/popore−2014−0025 Phylogenetic characters in the humerus and tarsometatarsus of penguins Martín CHÁVEZ HOFFMEISTER School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, BS8 1RJ, Bristol, United Kingdom and Laboratorio de Paleoecología, Instituto de Ciencias Ambientales y Evolutivas, Universidad Austral de Chile, Valdivia, Chile <[email protected]> Abstract: The present review aims to improve the scope and coverage of the phylogenetic matrices currently in use, as well as explore some aspects of the relationships among Paleogene penguins, using two key skeletal elements, the humerus and tarsometatarsus. These bones are extremely important for phylogenetic analyses based on fossils because they are commonly found solid specimens, often selected as holo− and paratypes of fossil taxa. The resulting dataset includes 25 new characters, making a total of 75 characters, along with eight previously uncoded taxa for a total of 48. The incorporation and analysis of this corrected subset of morphological characters raise some interesting questions consider− ing the relationships among Paleogene penguins, particularly regarding the possible exis− tence of two separate clades including Palaeeudyptes and Paraptenodytes, the monophyly of Platydyptes and Paraptenodytes, and the position of Anthropornis. Additionally, Noto− dyptes wimani is here recovered in the same collapsed node as Archaeospheniscus and not within Delphinornis, as in former analyses. Key words: Sphenisciformes, limb bones, phylogenetic analysis, parsimony method, revised dataset. Introduction Since the work of O’Hara (1986), the phylogeny of penguins has been a sub− ject of great interest. During the last decade, several authors have explored the use of molecular (e.g., Subramanian et al. -
Rapid Laurasian Diversification of a Pantropical Bird Family During The
Ibis (2020), 162, 137–152 doi: 10.1111/ibi.12707 Rapid Laurasian diversification of a pantropical bird family during the Oligocene–Miocene transition CARL H. OLIVEROS,1,2* MICHAEL J. ANDERSEN,3 PETER A. HOSNER,4,7 WILLIAM M. MAUCK III,5,6 FREDERICK H. SHELDON,2 JOEL CRACRAFT5 & ROBERT G. MOYLE1 1Department of Ecology and Evolutionary Biology and Biodiversity Institute, University of Kansas, Lawrence, KS, USA 2Museum of Natural Science and Department of Biological Sciences, Louisiana State University, Baton Rouge, LA, USA 3Department of Biology and Museum of Southwestern Biology, University of New Mexico, Albuquerque, NM, USA 4Division of Birds, Department of Vertebrate Zoology, National Museum of Natural History, Washington, DC, USA 5Department of Ornithology, American Museum of Natural History, New York, NY, USA 6New York Genome Center, New York, NY, USA 7Natural History Museum of Denmark and Center for Macroecology, Evolution, and Climate; University of Copenhagen, Copenhagen, Denmark Disjunct, pantropical distributions are a common pattern among avian lineages, but dis- entangling multiple scenarios that can produce them requires accurate estimates of his- torical relationships and timescales. Here, we clarify the biogeographical history of the pantropical avian family of trogons (Trogonidae) by re-examining their phylogenetic rela- tionships and divergence times with genome-scale data. We estimated trogon phylogeny by analysing thousands of ultraconserved element (UCE) loci from all extant trogon gen- era with concatenation and coalescent approaches. We then estimated a time frame for trogon diversification using MCMCTree and fossil calibrations, after which we performed ancestral area estimation using BioGeoBEARS. We recovered the first well-resolved hypothesis of relationships among trogon genera. -
Climatic Shifts Drove Major Contractions in Avian Latitudinal Distributions Throughout the Cenozoic
Climatic shifts drove major contractions in avian latitudinal distributions throughout the Cenozoic Erin E. Saupea,1,2, Alexander Farnsworthb, Daniel J. Luntb, Navjit Sagooc, Karen V. Phamd, and Daniel J. Fielde,1,2 aDepartment of Earth Sciences, University of Oxford, OX1 3AN Oxford, United Kingdom; bSchool of Geographical Sciences, University of Bristol, Clifton, BS8 1SS Bristol, United Kingdom; cDepartment of Meteorology, Stockholm University, 106 91 Stockholm, Sweden; dDivision of Geological and Planetary Sciences, Caltech, Pasadena, CA 91125; and eDepartment of Earth Sciences, University of Cambridge, CB2 3EQ Cambridge, United Kingdom Edited by Nils Chr. Stenseth, University of Oslo, Oslo, Norway, and approved May 7, 2019 (received for review March 8, 2019) Many higher level avian clades are restricted to Earth’s lower lati- order avian historical biogeography invariably recover strong evi- tudes, leading to historical biogeographic reconstructions favoring a dence for an origin of most modern diversity on southern land- Gondwanan origin of crown birds and numerous deep subclades. masses (2, 6, 11). However, several such “tropical-restricted” clades (TRCs) are repre- The crown bird fossil record has unique potential to reveal sented by stem-lineage fossils well outside the ranges of their clos- where different groups of birds were formerly distributed in deep est living relatives, often on northern continents. To assess the time. Fossil evidence, for example, has long indicated that total- drivers of these geographic disjunctions, we combined ecological group representatives of clades restricted to relatively narrow niche modeling, paleoclimate models, and the early Cenozoic fossil geographic regions today were formerly found in different parts of record to examine the influence of climatic change on avian geo- – graphic distributions over the last ∼56 million years.