Aerodynamics from Cursorial Running to Aerial Gliding for Avian Flight Evolution
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First Turtle Remains from the Middle-Late Jurassic Yanliao Biota, NE China
Vol.7, No.1 pages 1-11 Science Technology and Engineering Journal (STEJ) Research Article First Turtle Remains from the Middle-Late Jurassic Yanliao Biota, NE China Lu Li1,2,3, Jialiang Zhang4, Xiaolin Wang1,2,3, Yuan Wang1,2,3 and Haiyan Tong1,5* 1 Laboratory of Vertebrate Evolution and Human Origins of the Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China 2 CAS Center for Excellence in Life and Paleoenvironment, Beijing 100044, China 3 College of Earth and Planetary Sciences, University of China Academy of Sciences, Beijing 100044, China 4 State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China 5 Palaeontological Research and Education Centre, Mahasarakham University, Kantarawichai, Maha Sarakham 44150, Thailand * Corresponding author: [email protected] (Received: 14th August 2020, Revised: 11th January 2021, Accepted: 9th March 2021) Abstract - The Middle-Late Jurassic Yanliao Biota, preceding the Early Cretaceous Jehol Biota in NE China has yielded a rich collection of plant, invertebrate and vertebrate fossils. But contrary to the Jehol Biota which is rich in freshwater vertebrates, in the Yanliao Biota the aquatic reptiles are absent, and turtles have not been reported so far. In this paper, we report on the first turtle remains from the Yanliao Biota. The material consists of a partial skeleton from the Upper Jurassic Tiaojishan Formation of Bawanggou site (Qinglong, Hebei Province, China). Characterized by a broad skull with a pair of sulci carotici and a remnant of an interpterygoid vacuity, a well-developed anterior lobe of the plastron with mesiolaterally elongated epiplastra and a relatively large oval entoplastron; it is assigned to Annemys sp. -
Middle Jurassic Plant Diversity and Climate in the Ordos Basin, China Yun-Feng Lia, B, *, Hongshan Wangc, David L
ISSN 0031-0301, Paleontological Journal, 2019, Vol. 53, No. 11, pp. 1216–1235. © Pleiades Publishing, Ltd., 2019. Middle Jurassic Plant Diversity and Climate in the Ordos Basin, China Yun-Feng Lia, b, *, Hongshan Wangc, David L. Dilchera, b, d, E. Bugdaevae, Xiao Tana, b, d, Tao Lia, b, Yu-Ling Naa, b, and Chun-Lin Suna, b, ** aKey Laboratory for Evolution of Past Life and Environment in Northeast Asia, Jilin University, Changchun, Jilin, 130026 China bResearch Center of Palaeontology and Stratigraphy, Jilin University, Changchun, Jilin, 130026 China cFlorida Museum of Natural History, University of Florida, Gainesville, Florida, 32611 USA dDepartment of Earth and Atmospheric Sciences, Indiana University, Bloomington, Indiana, 47405 USA eFederal Scientific Center of the East Asia Terrestrial Biodiversity, Far Eastern Branch of Russian Academy of Sciences, Vladivostok, 690022 Russia *e-mail: [email protected] **e-mail: [email protected] Received April 3, 2018; revised November 29, 2018; accepted December 28, 2018 Abstract—The Ordos Basin is one of the largest continental sedimentary basins and it represents one major and famous production area of coal, oil and gas resources in China. The Jurassic non-marine deposits are well developed and cropped out in the basin. The Middle Jurassic Yan’an Formation is rich in coal and con- tains diverse plant remains. We recognize 40 species in 25 genera belonging to mosses, horsetails, ferns, cycadophytes, ginkgoaleans, czekanowskialeans and conifers. This flora is attributed to the early Middle Jurassic Epoch, possibly the Aalenian-Bajocian. The climate of the Ordos Basin during the Middle Jurassic was warm and humid with seasonal temperature and precipitation fluctuations. -
The Jurassic Fossil Wood Diversity from Western Liaoning, NE China
Jiang et al. Journal of Palaeogeography (2019) 8:1 https://doi.org/10.1186/s42501-018-0018-y Journal of Palaeogeography RESEARCH Open Access The Jurassic fossil wood diversity from western Liaoning, NE China Zi-Kun Jiang1,2, Yong-Dong Wang2,3*, Ning Tian4,5, Ao-Wei Xie2,6, Wu Zhang7, Li-Qin Li2 and Min Huang1 Abstract Western Liaoning is a unique region in China that bears diverse types of Jurassic plants, including leaves, fern rhizomes, and wood, providing significant proxy for vegetation and palaeoenvironment reconstruction of the well-known Yanliao Flora in East Asia. In particular, the silicified wood is very abundant in the fossil Lagerstätte of the Jurassic Tiaojishan Formation in Beipiao, western Liaoning. Previous and recent systematic investigations documented a high diversity of the Jurassic wood assemblages. These assemblages are dominated by conifers, followed by cycads and ginkgoaleans. In total, about 30 species belonging to 21 genera of fossil wood have been recorded so far, which are represented by Cycadopsida, Ginkgopsida, Coniferopsida, and Gymnospermae incertae sedis. The evolutionary implications of several distinctive fossil wood taxa as well as palaeoclimate implications are summarized based on their anatomical structures and growth ring patterns. This work approaches the vegetation development and evolutionary significances of the wood taxa and their relatives, and provides clues for the further understanding of the diversity of the Jurassic Yanliao Flora in East Asia. Keywords: Fossil wood, Diversity, Evolution, Tiaojishan Formation, Jurassic 1 Introduction 2004;Wangetal.,2009). Among these localities, western Fossil floras are a significant record for the vegetation Liaoning is a well-known fossil Lagerstätte with diverse and for the palaeoenvironment reconstructions of the and well-preserved fossil plant foliages and wood (Zhang Mesozoic. -
Acoustic Monitoring of Night-Migrating Birds: a Progress Report
Acoustic Monitoring of Night-Migrating Birds: A Progress Report William R. Evans Kenneth V. Rosenberg Abstract—This paper discusses an emerging methodology that to give regular vocalizations in night migration are the vireos uses electronic technology to monitor vocalizations of night-migrat- (Vireonidae), flycatchers (Tyrannidae), and orioles (Icterinae). ing birds. On a good migration night in eastern North America, If a monitoring protocol is consistently maintained, an array thousands of call notes may be recorded from a single ground-based, of microphone stations can provide information on how the audio-recording station, and an array of recording stations across a species composition and number of vocal migrants vary across region may serve as a “recording net” to monitor a broad front of time and space. Such data have application for monitoring migration. Data from pilot studies in Florida, Texas, New York, and avian populations and identifying their migration routes. In British Columbia illustrate the potential of this technique to gather addition, detection and classification of distinctive call-types information that cannot be gathered by more conventional methods, is possible with computers (Mills 1995; Taylor 1995), thus such as mist-netting or diurnal counts. For example, the Texas information on bird populations might be gained automati- station detected a major migration of grassland sparrows, and a cally. In this paper, we summarize the current state of station in British Columbia detected hundreds of Swainson’s knowledge for identifying night-flight calls to species; present Thrushes; both phenomena were not detected with ground monitor- selected results from four ongoing studies that are monitoring ing efforts. -
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. -
The Dinosaurs Are Back!
EXHIBITION FOR HIRE THE DINOSAURS ARE BACK! THE DINOSAURS ARE BACK! In partnership with Emilio’s Creations, Universeum proudly presents the unique dinosaur exhibition “The dinosaurs are back”. The latest scientific discoveries are summarised in a spectacular visitor experience with 16 life-size dinosaurs that move and make noises. Ten of them are feathered in accordance with recent research. The exhibition for hire comprises eight different species set in a prehistoric forest landscape with trees and plants from that specific era. Included is the world’s largest known land predator, theSpinosaurus , at 14 metres long and five metres tall. Also on display are the four-metre tall and fully feathered Therizinosaurus and the legendary Tyrannosaurus rex, together with a feathered juvenile. Feathers The dinosaurs in the exhibition for hire The dinosaurs never really died out. They live The dinosaurs in the exhibition have been carefully on and we see and hear them every day. After selected to show a diverse range of species and all, birds are directly descended from some of highlight scientifically interesting points. the most ferocious and predatory dinosaurs, Sinosauropteryx (x2). The first genus of dinosaur discovered with recent research confirming the close outside of Avialae(birds) that is known to have been links between dinosaurs and birds. This feathered. point is clearly illustrated when visitors see the Tyrannosaurus rex (x2). As well as being famous, it is of great feathered dinosaurs in the exhibition. scientific interest. Researchers are speculating as to whether the adult lost the coat of feathers it had when young or Environment whether it retained all or part of it throughout its life. -
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. -
The Princeton Field Guide to Dinosaurs, Second Edition
MASS ESTIMATES - DINOSAURS ETC (largely based on models) taxon k model femur length* model volume ml x specific gravity = model mass g specimen (modeled 1st):kilograms:femur(or other long bone length)usually in decameters kg = femur(or other long bone)length(usually in decameters)3 x k k = model volume in ml x specific gravity(usually for whole model) then divided/model femur(or other long bone)length3 (in most models femur in decameters is 0.5253 = 0.145) In sauropods the neck is assigned a distinct specific gravity; in dinosaurs with large feathers their mass is added separately; in dinosaurs with flight ablity the mass of the fight muscles is calculated separately as a range of possiblities SAUROPODS k femur trunk neck tail total neck x 0.6 rest x0.9 & legs & head super titanosaur femur:~55000-60000:~25:00 Argentinosaurus ~4 PVPH-1:~55000:~24.00 Futalognkosaurus ~3.5-4 MUCPv-323:~25000:19.80 (note:downsize correction since 2nd edition) Dreadnoughtus ~3.8 “ ~520 ~75 50 ~645 0.45+.513=.558 MPM-PV 1156:~26000:19.10 Giraffatitan 3.45 .525 480 75 25 580 .045+.455=.500 HMN MB.R.2181:31500(neck 2800):~20.90 “XV2”:~45000:~23.50 Brachiosaurus ~4.15 " ~590 ~75 ~25 ~700 " +.554=~.600 FMNH P25107:~35000:20.30 Europasaurus ~3.2 “ ~465 ~39 ~23 ~527 .023+.440=~.463 composite:~760:~6.20 Camarasaurus 4.0 " 542 51 55 648 .041+.537=.578 CMNH 11393:14200(neck 1000):15.25 AMNH 5761:~23000:18.00 juv 3.5 " 486 40 55 581 .024+.487=.511 CMNH 11338:640:5.67 Chuanjiesaurus ~4.1 “ ~550 ~105 ~38 ~693 .063+.530=.593 Lfch 1001:~10700:13.75 2 M. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Therizinosaurus Cheloniformis
3-EURO-SUPERSAURS THERIZINOSAURUS CHELONIFORMIS Series Supersaurs Appearances can be deceptive. Weighing five tons, up to ten metres tall and boas- ting sharp claws that were longer than those of any other land animal that has ever Face value ¤ 3 existed, the Therizinosaurus was not as dangerous as it looked. The subject of the Date of Issue 17 February 2021 sixth coin in the superlative Supersaurs series was actually a vegetarian and its claws Design K. Kuntner/ H. Andexlinger more suited to detaching vegetation than attacking the other animals that roamed Diameter 34 mm the planet some 70 million years ago. Quality Uncirculated Mintage 65,000 As a theropod, Therizinosaurus cheloniformis was not only distantly related to pre- Alloy Coloured metal dators such as Tyrannosaurus rex but also to present-day birds. Originally carnivor- Total Weight 16.00 g ous, over time the Therizinosaurus changed its diet and became a pure herbivore. Edge Plain During the late Cretaceous period, it lived in areas of the northern continent of Colour application, glow in the dark, Laurasia that now correspond to North America, China and Mongolia. Up to one no packaging. metre in length, flat, curved and pointed at the end, the dinosaur’s claws are re- sponsible for its nickname, ‘scythe lizard’. They were used primarily to reach high Recommended branches in trees as well as perhaps for self-defence. Well preserved remains of one initial issue price: ¤ 12.60 (incl. 20% VAT) of its close relatives have suggested that, rather surprisingly, the Therizinosaurus was also partially feathered. WITH COIN MOTIF COLOURED GLOW-IN-THE-DARK Therizinosaurus features all 12 of the extreme prehistoric animals in the Supersaurs EFFECT series in silhouette on its obverse, while a colour-printed Therizinosaurus is shown in its native prehistoric habitat next to a nest full of eggs on the coin’s glow-in-the- dark reverse. -
A Bird's Eye View of the Evolution of Avialan Flight
Chapter 12 Navigating Functional Landscapes: A Bird’s Eye View of the Evolution of Avialan Flight HANS C.E. LARSSON,1 T. ALEXANDER DECECCHI,2 MICHAEL B. HABIB3 ABSTRACT One of the major challenges in attempting to parse the ecological setting for the origin of flight in Pennaraptora is determining the minimal fluid and solid biomechanical limits of gliding and powered flight present in extant forms and how these minima can be inferred from the fossil record. This is most evident when we consider the fact that the flight apparatus in extant birds is a highly integrated system with redundancies and safety factors to permit robust performance even if one or more components of their flight system are outside their optimal range. These subsystem outliers may be due to other adaptive roles, ontogenetic trajectories, or injuries that are accommodated by a robust flight system. This means that many metrics commonly used to evaluate flight ability in extant birds are likely not going to be precise in delineating flight style, ability, and usage when applied to transitional taxa. Here we build upon existing work to create a functional landscape for flight behavior based on extant observations. The functional landscape is like an evolutionary adap- tive landscape in predicting where estimated biomechanically relevant values produce functional repertoires on the landscape. The landscape provides a quantitative evaluation of biomechanical optima, thus facilitating the testing of hypotheses for the origins of complex biomechanical func- tions. Here we develop this model to explore the functional capabilities of the earliest known avialans and their sister taxa. -
A Comparison of Flight Potential Among Small-Bodied Paravians
Chapter 11 High Flyer or High Fashion? A Comparison of Flight Potential among Small-Bodied Paravians T. ALEXANDER DECECCHI,1 HANS C.E. LARSSON,2 MICHAEL PITTMAN,3 AND MICHAEL B. HABIB4 ABSTRACT The origin of flight in birds and its relationship to bird origins itself has achieved something of a renaissance in recent years, driven by the discovery of a suite of small-bodied taxa with large pen- naceous feathers. As some of these specimens date back to the Middle Jurassic and predate the earli- est known birds, understanding how these potential aerofoil surfaces were used is of great importance to answering the question: which came first, the bird or the wing? Here we seek to address this question by directly comparing key members of three of the major clades of paravians: anchiorni- thines, Microraptor and Archaeopteryx across their known size classes to see how they differ in terms of major flight-related parameters (wing loading; disc loading; specific lift; glide speed; takeoff poten- tial). Using specimens with snout to vent length (SVL) ranging from around 150 mm to 400 mm and mass ranging from approximately 130 g to 2 kg, we investigated patterns of inter- and intraspe- cific changes in flight potential. We find that anchiornithines show much higher wing- and disc- loading values and correspondingly high required minimum glide and takeoff speeds, along with lower specific lift and flapping running outputs suggesting little to no flight capability in this clade. In contrast, we see good support for flight potential, either gliding or powered flight, for all size classes of both Microraptor and Archaeopteryx, though there are differing patterns of how this shifts ontogenetically.