Bayesian Phylogenetic Estimation of Fossil Ages
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Bayesian Total-Evidence Dating Reveals the Recent Crown Radiation of Penguins Alexandra Gavryushkina University of Auckland
Ecology, Evolution and Organismal Biology Ecology, Evolution and Organismal Biology Publications 2017 Bayesian Total-Evidence Dating Reveals the Recent Crown Radiation of Penguins Alexandra Gavryushkina University of Auckland Tracy A. Heath Iowa State University, [email protected] Daniel T. Ksepka Bruce Museum David Welch University of Auckland Alexei J. Drummond University of Auckland Follow this and additional works at: http://lib.dr.iastate.edu/eeob_ag_pubs Part of the Ecology and Evolutionary Biology Commons The ompc lete bibliographic information for this item can be found at http://lib.dr.iastate.edu/ eeob_ag_pubs/207. For information on how to cite this item, please visit http://lib.dr.iastate.edu/ howtocite.html. This Article is brought to you for free and open access by the Ecology, Evolution and Organismal Biology at Iowa State University Digital Repository. It has been accepted for inclusion in Ecology, Evolution and Organismal Biology Publications by an authorized administrator of Iowa State University Digital Repository. For more information, please contact [email protected]. Syst. Biol. 66(1):57–73, 2017 © The Author(s) 2016. Published by Oxford University Press, on behalf of the Society of Systematic Biologists. This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/by-nc/4.0/), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the original work is properly cited. For commercial re-use, please contact [email protected] DOI:10.1093/sysbio/syw060 Advance Access publication August 24, 2016 Bayesian Total-Evidence Dating Reveals the Recent Crown Radiation of Penguins , ,∗ , ALEXANDRA GAVRYUSHKINA1 2 ,TRACY A. -
A Rhinopristiform Sawfish (Genus Pristis) from the Middle Eocene (Lutetian) of Southern Peru and Its Regional Implications
Carnets Geol. 20 (5) E-ISSN 1634-0744 DOI 10.4267/2042/70759 A rhinopristiform sawfish (genus Pristis) from the middle Eocene (Lutetian) of southern Peru and its regional implications Alberto COLLARETA 1, 2 Luz TEJADA-MEDINA 3, 4 César CHACALTANA-BUDIEL 3, 5 Walter LANDINI 1, 6 Alí ALTAMIRANO-SIERRA 7, 8 Mario URBINA-SCHMITT 7, 9 Giovanni BIANUCCI 1, 10 Abstract: Modern sawfishes (Rhinopristiformes: Pristidae) are circumglobally distributed in warm wa- ters and are common in proximal marine and even freshwater habitats. The fossil record of modern pristid genera (i.e., Pristis and Anoxypristis) dates back to the early Eocene and is mostly represented by isolated rostral spines and oral teeth, with phosphatised rostra representing exceptional occurren- ces. Here, we report on a partial pristid rostrum, exhibiting several articulated rostral spines, from middle Eocene strata of the Paracas Formation (Yumaque Member) exposed in the southern Peruvian East Pisco Basin. This finely preserved specimen shows anatomical structures that are unlikely to leave a fossil record, e.g., the paracentral grooves that extend along the ventral surface of the rostrum. Ba- sed on the morphology of the rostral spines, this fossil sawfish is here identified as belonging to Pristis. To our knowledge, this discovery represents the geologically oldest known occurrence of Pristidae from the Pacific Coast of South America. Although the fossil record of pristids from the East Pisco Basin spans from the middle Eocene to the late Miocene, sawfishes are no longer present in the modern cool, upwelling-influenced coastal waters of southern Peru. Given the ecological preferences of the extant members of Pristis, the occurrence of this genus in the Paracas deposits suggests that middle Eocene nearshore waters in southern Peru were warmer than today. -
Acosta Hospitaleche.Vp
vol. 34, no. 4, pp. 397–412, 2013 doi: 10.2478/popore−2013−0018 New crania from Seymour Island (Antarctica) shed light on anatomy of Eocene penguins Carolina ACOSTA HOSPITALECHE CONICET. División Paleontología de Vertebrados, Museo de La Plata, Paseo del Bosque s/n, B1900FWA La Plata, Argentina <[email protected]> Abstract: Antarctic skulls attributable to fossil penguins are rare. Three new penguin crania from Antarctica are here described providing an insight into their feeding function. One of the specimens studied is largely a natural endocast, slightly damaged, and lacking preserved osteological details. Two other specimens are the best preserved fossil penguin crania from Antarctica, enabling the study of characters not observed so far. All of them come from the uppermost Submeseta Allomember of the La Meseta Formation (Eocene–?Oligocene), Seymour (Marambio) Island, Antarctic Peninsula. The results of the comparative studies suggest that Paleogene penguins were long−skulled birds, with strong nuchal crests and deep temporal fossae. The configuration of the nuchal crests, the temporal fossae, and the parasphenoidal processes, appears to indicate the presence of powerful muscles. The nasal gland sulcus devoid of a supraorbital edge is typical of piscivorous species. Key words: Antarctica, Sphenisciformes, crania, La Meseta Formation, late Eocene. Introduction Penguins (Aves, Sphenisciformes) are the best represented Paleogene Antarc− tic seabirds. This is probably so because of the intrinsic features of their skeletons, dense and heavy bones increase the chance of fossilization, and the presumably gregarious habit, typical of extant species. The oldest penguin record is known from the Paleocene of New Zealand (Slack et al. -
At the Root of the Early Penguin Neck: a Study of the Only Two Cervicodorsal Spines Recovered from the Eocene of Antarctica Piotr Jadwiszczak
RESEARCH/REVIEW ARTICLE At the root of the early penguin neck: a study of the only two cervicodorsal spines recovered from the Eocene of Antarctica Piotr Jadwiszczak Institute of Biology, University of Bialystok, Swierkowa 20B, PL-15-950, Bialystok, Poland Keywords Abstract Antarctic Peninsula; La Meseta Formation; Palaeogene; early Sphenisciformes; The spinal column of early Antarctic penguins is poorly known, mainly due to cervicodorsal vertebrae. the scarcity of articulated vertebrae in the fossil record. One of the most interesting segments of this part of the skeleton is the transitional series located Correspondence at the root of the neck. Here, two such cervicodorsal series, comprising rein- Piotr Jadwiszczak, Institute of Biology, terpreted known material and a new specimen from the Eocene of Seymour University of Bialystok, Swierkowa 20B, Island (Antarctic Peninsula), were investigated and contrasted with those PL-15-950 Bialystok, Poland. of modern penguins and some fossil bones. The new specimen is smaller E-mail: [email protected] than the counterpart elements in recent king penguins, whereas the second series belonged to a large-bodied penguin from the genus Palaeeudyptes. It had been assigned by earlier researchers to P. gunnari (a species of ‘‘giant’’ penguins) and a Bayesian analysis*a Bayes factor approach based on size of an associated tarsometatarsus*strongly supported such an assignment. Morphological and functional studies revealed that mobility within the aforementioned segment probably did not differ substantially between extant and studied fossil penguins. There were, however, intriguing morphological differences between the smaller fossil specimen and the comparative material related to the condition of the lateral excavation in the first cervicodorsal vertebra and the extremely small size of the intervertebral foramen located just prior to the first ‘‘true’’ thoracic vertebra. -
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. -
Antarctic Peninsula Paleontology Project Matt Lamanna
Philadelphia College of Osteopathic Medicine DigitalCommons@PCOM PCOM Scholarly Papers 2-11-2016 Science AMA Series: Antarctic Peninsula Paleontology Project Matt Lamanna Julia Clarke Pat O'Connor Ross MacPhee Erik Gorscak See next page for additional authors Follow this and additional works at: http://digitalcommons.pcom.edu/scholarly_papers Part of the Paleontology Commons Recommended Citation Lamanna, Matt; Clarke, Julia; O'Connor, Pat; MacPhee, Ross; Gorscak, Erik; West, Abby; Torres, Chris; Claeson, Kerin M.; Jin, Meng; Salisbury, Steve; Roberts, Eric; and Jinnah, Zubair, "Science AMA Series: Antarctic Peninsula Paleontology Project" (2016). PCOM Scholarly Papers. Paper 1677. http://digitalcommons.pcom.edu/scholarly_papers/1677 This Article is brought to you for free and open access by DigitalCommons@PCOM. It has been accepted for inclusion in PCOM Scholarly Papers by an authorized administrator of DigitalCommons@PCOM. For more information, please contact [email protected]. Authors Matt Lamanna, Julia Clarke, Pat O'Connor, Ross MacPhee, Erik Gorscak, Abby West, Chris Torres, Kerin M. Claeson, Meng Jin, Steve Salisbury, Eric Roberts, and Zubair Jinnah This article is available at DigitalCommons@PCOM: http://digitalcommons.pcom.edu/scholarly_papers/1677 REDDIT Science AMA Series: We’re a group of paleontologists and geologists on our way to Antarctica to look for fossils of non-avian dinosaurs, ancient birds, and more. AUA! ANTARCTICPALEO R/SCIENCE Hi Reddit! Our research team—collectively working as part of the Antarctic Peninsula Paleontology Project, or AP3—is on a National Science Foundation-supported research vessel on its way to Antarctica. This will be our third expedition to explore the Antarctic Peninsula for fossils spanning the end of the Age of Dinosaurs (the Late Cretaceous) to the dawn of the Age of Mammals (the early Paleogene). -
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. -
Paleogene Equatorial Penguins Challenge the Proposed Relationship Between Biogeography, Diversity, and Cenozoic Climate Change
Paleogene equatorial penguins challenge the proposed relationship between biogeography, diversity, and Cenozoic climate change Julia A. Clarkea,b,c,d, Daniel T. Ksepkac, Marcelo Stucchie, Mario Urbinaf, Norberto Gianninig,h, Sara Bertellii,g, Yanina Narva´ ezj, and Clint A. Boyda aDepartment of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Campus Box 8208, Raleigh, NC 27695; bDepartment of Paleontology, North Carolina Museum of Natural Sciences, 11 West Jones Street, Raleigh, NC 27601-1029; Divisions of cPaleontology and gVertebrate Zoology, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024; eAsociacio´n para la Investigacio´n y Conservacio´n de la Biodiversidad, Los Agro´logos 220, Lima 12, Peru´; fDepartment of Vertebrate Paleontology, Museo de Historia Natural, Universidad Nacional Mayor de San Marcos, Avenida Arenales 1256, Lima 14, Peru´; hProgram de Investigaciones de Biodiversidad Argentina (Consejo Nacional de Investigaciones Cientı´ficas y Te´cnicas), Facultad de Ciencias Naturales, Instituto Miguel Lillo de la Universidad Nacional de Tucuma´n, Miguel Lillo 205, CP 4000, Tucuma´n, Argentina; iThe Dinosaur Institute, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007; and jDepartment of Geology, Centro de Investigacio´n Cientı´ficay de Educacio´n Superior de Ensenada, Kilometer 107 Carretera Tijuana–Ensenada, 22860 Ensenada, Baja California, Me´xico Edited by R. Ewan Fordyce, University of Otago, Dunedin, New Zealand, and accepted by the Editorial Board May 21, 2007 (received for review December 14, 2006) New penguin fossils from the Eocene of Peru force a reevaluation of presence of at least five penguin taxa (ref. -
Feeding Habits of Antarctic Eocene Penguins from a Morpho- Functional Perspective
N. Jb. Geol. Paläont. Abh. 263/2, 125–131 Article Stuttgart, February 2012 Feeding habits of Antarctic Eocene penguins from a morpho- functional perspective Nadia Haidr and Carolina Acosta Hospitaleche With 6 figures Haidr, N. & acosta HospitalecHe, C. (2012): Feeding habits of Antarctic Eocene penguins from a morpho-functional perspective. – N. Jb. Geol. Paläont. Abh., 263: 125–131; Stuttgart. Abstract: Cranial and mandibular penguin remains from the Eocene of Antarctica were studied in order to determine their feeding habits and food item preferences. Their osteology and musculature were compared with those of modern taxa. Different morphotypes were recognized based on their skull, configuration of the articular region of the mandible and bill shape. The results point to a vari- ety of trophic habits and food preferences consistent with the known taxonomic diversity for this unit. For the middle Eocene, large sized penguins were interpreted as fish and crustacean eaters, whereas for the late Eocene, taxonomic diversity and number of individuals in the colonies during the late Eocene seems to increase. This colony could be reconstructed as being composed of medium-sized generalist penguins, piscivorous large- and medium-sized species, and also large penguins with a diet based on crustaceans and squids. Key words: Fossil Spheniscidae, Antarctica, anatomy, osteology, musculature. 1. Introduction HospitalecHe & Haidr 2011). As in modern penguins, these small differences in bill shape can reflect not Eocene Antarctic penguins are characterized by a only the feeding habits, but minor divergences in the high specific and morphological diversity. While four- adaptiveness of closely related forms (Bock 1966). teen species (but see Jadwiszczak 2006a) have been Cranial and mandibular remains from the Eocene described for La Meseta Formation, little is known of Antarctica were here studied in order to determine about their feeding habits and food preferences. -
Quantifying Historical Trends in the Completeness of the Fossil Record and the Contributing Factors: an Example Using Aves Author(S) :Daniel T
Quantifying historical trends in the completeness of the fossil record and the contributing factors: an example using Aves Author(s) :Daniel T. Ksepka and Clint A. Boyd Source: Paleobiology, 38(1):112-125. 2012. Published By: The Paleontological Society DOI: URL: http://www.bioone.org/doi/full/10.1666/10059.1 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. PersonIdentityServiceImpl Paleobiology, 38(1), 2012, pp. 112–125 Quantifying historical trends in the completeness of the fossil record and the contributing factors: an example using Aves Daniel T. Ksepka and Clint A. Boyd Abstract.—Improvements in the perceived completeness of the fossil record may be driven both by new discoveries and by reinterpretation of known fossils, but disentangling the relative effects of these processes can be difficult. Here, we propose a new methodology for evaluating historical trends in the perceived completeness of the fossil record, demonstrate its implementation using the freely available software ASCC (version 4.0.0), and present an example using crown-group birds (Aves). -
The Fossil Record of Birds from the James Ross Basin, West Antarctica
• Review • Advances in Polar Science doi: 10.13679/j.advps.2019.0014 September 2019 Vol. 30 No. 3: 251-273 The fossil record of birds from the James Ross Basin, West Antarctica Carolina ACOSTA HOSPITALECHE1,2*, Piotr JADWISZCZAK3, Julia A. CLARKE4 & Marcos CENIZO5,6 1 Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Godoy Cruz, Argentina; 2 División Paleontología Vertebrados, Museo de La Plata, Facultad de Ciencias Naturales y Museo, Argentina; 3 Institute of Biology, University of Bialystok, Bialystok, Poland; 4 Jackson School of Geosciences, The University of Texas, Austin, Texas, USA; 5 División Paleontología, Museo de Historia Natural de La Pampa, Santa Rosa, La Pampa, Argentina; 6 Fundación de Historia Natural Félix de Azara, Departamento de Ciencias Naturales y Antropología, CEBBAD– Universidad Maimónides, Buenos Aires, Argentina Received 10 March 2019; accepted 12 June 2019; published online 22 July 2019 Abstract The fossil record of birds from Antarctica is concentrated in the James Ross Basin, located in north-east of the Antarctic Peninsula. Birds are here represented by an extensive Paleogene record of penguins (Sphenisciformes) and Cretaceous–Paleogene record of Anseriformes, followed by other groups with a minor representation (Procellariiformes, Falconiformes, and Pelagornithidae), and others previously assigned controversially to “Ratites”, Threskiornithidae, Charadriiformes, Gruiformes, Phoenicopteriformes, and Gaviiformes. We provide a complete update of these records, commenting on the importance of some of these remains for the evolution of the major clades. Keywords fossil, avifauna, Cretaceous, Paleogene, Seymour Island, Vega Island Citation: Acosta Hospitaleche C, Jadwiszczak P, Clarke J A, et al. The fossil record of birds from the James Ross Basin, West Antarctica.