Young, FJ, & Vinther, J. (2017)
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Supplement of Reconstructing Late Holocene North Atlantic Atmospheric Circulation Changes Using Functional Paleoclimate Networks
Supplement of Clim. Past, 13, 1593–1608, 2017 https://doi.org/10.5194/cp-13-1593-2017-supplement © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Supplement of Reconstructing Late Holocene North Atlantic atmospheric circulation changes using functional paleoclimate networks Jasper G. Franke et al. Correspondence to: Jasper G. Franke ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 3.0 License. J. G. Franke et al.: Supplementary Material 1 S1 Possible impacts on human societies As mentioned in Sec. 5.3 of the main paper, it can be expected that at longer time scales, the alternation between different phases of the NAO has had a considerable impact on human societies via modifications of temperature and precipitation patterns and their resulting consequences for natural and agricultural ecosystems (Hurrell et al., 2003; Hurrell and Deser, 2010, and references therein). In the following, we discuss possible implications of our qualitative reconstruction of the NAO phase 5 in the context of European history during the Common Era. Since the climatic influence of the NAO differs among different parts of Europe, we restrict this discussion to two key regions, the Western Roman Empire and Norse colonies in the North Atlantic. Prior to presenting some further thoughts on corresponding relationships, we emphasize that one has to keep in mind, that climatic conditions have almost never been the sole reason for societal changes. However, they can be either beneficial or disadvantageous, also depending on how vulnerable a society is to environmental disruptions (Diaz and Trouet, 2014; Weiss 10 and Bradley, 2001; Diamond, 2005). -
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. -
Fossils from South China Redefine the Ancestral Euarthropod Body Plan Cédric Aria1 , Fangchen Zhao1, Han Zeng1, Jin Guo2 and Maoyan Zhu1,3*
Aria et al. BMC Evolutionary Biology (2020) 20:4 https://doi.org/10.1186/s12862-019-1560-7 RESEARCH ARTICLE Open Access Fossils from South China redefine the ancestral euarthropod body plan Cédric Aria1 , Fangchen Zhao1, Han Zeng1, Jin Guo2 and Maoyan Zhu1,3* Abstract Background: Early Cambrian Lagerstätten from China have greatly enriched our perspective on the early evolution of animals, particularly arthropods. However, recent studies have shown that many of these early fossil arthropods were more derived than previously thought, casting uncertainty on the ancestral euarthropod body plan. In addition, evidence from fossilized neural tissues conflicts with external morphology, in particular regarding the homology of the frontalmost appendage. Results: Here we redescribe the multisegmented megacheirans Fortiforceps and Jianfengia and describe Sklerolibyon maomima gen. et sp. nov., which we place in Jianfengiidae, fam. nov. (in Megacheira, emended). We find that jianfengiids show high morphological diversity among megacheirans, both in trunk ornamentation and head anatomy, which encompasses from 2 to 4 post-frontal appendage pairs. These taxa are also characterized by elongate podomeres likely forming seven-segmented endopods, which were misinterpreted in their original descriptions. Plesiomorphic traits also clarify their connection with more ancestral taxa. The structure and position of the “great appendages” relative to likely sensory antero-medial protrusions, as well as the presence of optic peduncles and sclerites, point to an overall -
The Extent of the Sirius Passet Lagerstätte (Early Cambrian) of North Greenland
The extent of the Sirius Passet Lagerstätte (early Cambrian) of North Greenland JOHN S. PEEL & JON R. INESON Ancillary localities for the Sirius Passet biota (early Cambrian; Cambrian Series 2, Stage 3) are described from the im- mediate vicinity of the main locality on the southern side of Sirius Passet, north-western Peary Land, central North Greenland, where slope mudstones of the Transitional Buen Formation abut against the margin of the Portfjeld Forma- tion carbonate platform. Whilst this geological relationship may extend over more than 500 km east–west across North Greenland, known exposures of the sediments yielding the lagerstätte are restricted to a 1 km long window at the south-western end of Sirius Passet. • Keywords: Early Cambrian, Greenland, lagerstätte. PEEL, J.S. & INESON, J.R. The extent of the Sirius Passet Lagerstätte (early Cambrian) of North Greenland. Bulletin of Geosciences 86(3), 535–543 (4 figures). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript received March 24, 2011; accepted in revised form July 8, 2011; published online July 28, 2011; issued September 30, 2011. John S. Peel, Department of Earth Sciences (Palaeobiology), Uppsala University, Villavägen 16, SE-75 236 Uppsala, Sweden; [email protected] • Jon R. Ineson, Geological Survey of Denmark and Greenland, Øster Voldgade 10, DK-1350 Copenhagen K, Denmark; [email protected] Almost all of the fossils described from the early Cambrian The first fragmentary fossils from the Sirius Passet Sirius Passet Lagerstätte of northern Peary Land, North Lagerstätte (GGU collection 313035) were collected by Greenland, were collected from a single, west-facing talus A.K. -
J32 the Importance of the Burgess Shale < Soft Bodied Fauna >
580 Chapter j PALEOCONTINENTS The Present is the Key to the Past: HUGH RANCE j32 The importance of the Burgess shale < soft bodied fauna > Only about 33 animal body plans are presently [sic] being used on this planet (Margulis and Schwartz, 1988). —Scott F. Gilbert, Developmental Biology, 1991.1 Almost all animal phyla known today were already present by 505 million years ago— the age of the Burgess shale, Middle Cambrian marine sediments, discovered at the Kicking Horse rim, British Columbia, in 1909 by Charles Doolittle Walcott, that provide a unique window on life without hard parts that had continued to exist shortly after the time of the Cambrian explosion (see Topic j34).2 Legend has it that Walcott, then secretary of the Smithsonian Institution, vacationing near Field, British Columbia, was thrown from a horse carrying him, when it tripped on, and split open a stray fallen slab of shale. Walcott, with his face literally rubbed in it, saw strange, but not hallucinational, forms crisply etched in black against the blue-black bedding surface of the shale: a bonanza of fossils of sea creatures without mineralized shells or backbones. Many are preserved whole; including those with articulated organic (biodegradable) exoskeletons. Details of even their soft body parts can be seen (best using PTM)3 as silvery films (formed of phyllosilicates on a coating of kerogenized carbon) that commonly outline even the most delicate structures on the fossilized animal.4 The Burgess shale is part of the Stephen Formation of greenish shales and thin-bedded limestones, which is a marine-offlap deposit between the thick, massive, carbonates of the overlying Eldon formation, and the underlying Cathedral formation.6 As referenced in the Geological Atlas of the Western Canada Sedimentary Basin - Chapter 8, the Stephen Formation has been “informally divided into a normal, ‘thin Stephen’ on the platform areas and a ‘thick Stephen’ west of the Cathedral Escarpment. -
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Journal of Language Contact 6 (2013) 134–159 brill.com/jlc Ukrainian in the Language Map of Central Europe: Questions of Areal-Typological Profiling Andrii Danylenko Department of Modern Languages and Cultures Pace University, New York [email protected] Abstract The paper deals with the areal-typological profiling of Ukrainian among languages of Europe, constituting Standard Average European (SAE) and especially Central European (CE). Placed recently in the context of the ‘areal typology’ and the ‘dynamic taxonomy’, Ukrainian together with Russian and Belarusian appear to be mere replica languages. Such languages are capable of only borrowing surface structures migrating all over the Europe unie or imitating deep structures on the model of SAE or CE. In order to elaborate on an alternative profiling of Ukrainian among languages of (Central) Europe, the author concentrates on both phonological and morphosyntactic features treated commonly as CE Sprachbund-forming (the spirantization of *g, the dispalatalization of the pala- talized consonants, the existence of medial l, the umlauting, the three-tense system, including a simple preterit from the perfect, and the periphrastic ‘ingressive’ future). As a result, the author advances another vector of areal classification, thus positioning Russian in the core of ‘Standard Average Indo-European’ and (Southwest) Ukrainian as an intermediate language between Russian and the rest of (Central) European languages. Keywords Ukrainian; North Slavic; Central European Sprachbund; ‘Standard Average Indo-European’; areal-typological profiling 1. Introduction In comparative and typological studies, Ukrainian has been routinely treated as a transitional language from East Slavic (cf. Jakobson, 1929; Stadnik, 2001:94) to North Slavic (Mrázek, 1990:28-30; Besters-Dilger, 2000), West Slavic (Lehfeldt, 1972:333-336) or even South Slavic (Smal-Stockyj and Gartner, 1913). -
Appendix 1*) for Essential Information Very Well Illustrated in Google and Wikipedia
Appendix 1*) For Essential Information Very Well Illustrated in Google and Wikipedia *) in Support of the Text with Literature Citations. Referrals to illustrations in Appendix 2. Cancer in the Plant. The insertion of the Agrobacterium tumefaciens circular plasmid T (transferred) DNA into the genome of its new host, the plant (Gelvin BS. Microbiol Molecular Biol Rev 2003;67:16–37). The plant cancer “crown gall” (agrocallus; Agrobacterial crown gall) consists of malignantly transformed cells replicating the agrobacterial T DNA plasmid (reviewed in postscript Table XXXV). For reference: Koncz C Mayerhofer R Koncz-Kálmán Zs et al EMBO J 1990;9:1337–1346. Transfer of potentially oncogenic bacterial genes and proteins to patients: Septicemic Bacteroides enterotoxigenic (Sinkovics J G & Smith JP Cancer 1970;25:663–671; Viljoen KS et al PLoS One 2015;10(3):e0119462); Bartonella bacilliformis etc (Guy L et al PLoS Genet 2013;9(3):e1003393; Harms A & Dehio C Clin Microbiol Rev 2012;25:42–78; Llosa M et al Trends Microbiol 2012;20:355–9; Minnick MF et al PLoS Negl Trop Dis 2014;6(7):e2919); Helicobacter pylori (Bonsor DA et al J Biol Chem 2015;pii:jbc.M115.641829; Su YL et al J Immunol 2015;194:3997–4007; Vaziri F et al Pathog Dis 2015;73(3). pii.ftu021); Porphyromonas gingivalis (Katz J et al Int J Oral Sci 2011;3:209–215); Tuberculous infections with A. tumefaciens in patients (Ramirez FC et al Clin Infect Dis 1992;15:938–940). DNA-binding Antibodies. DNA- (or RNA-) binding proteins use zink finger motifs, leucine zippers and winged (beta-sheet loops) helix-turn helix motifs (HTH, two helices separated by the loop, RNA/DNA-binding domains) in recognition of RNA/DNA receptors for attachment. -
An Ordovician Lobopodian from the Soom Shale Lagerstätte, South Africa
[Palaeontology, Vol. 52, Part 3, 2009, pp. 561–567] AN ORDOVICIAN LOBOPODIAN FROM THE SOOM SHALE LAGERSTA¨ TTE, SOUTH AFRICA by ROWAN J. WHITTLE*,à, SARAH E. GABBOTT*, RICHARD J. ALDRIDGE* and JOHANNES THERON *Department of Geology, University of Leicester, Leicester LE1 7RH, UK; e-mails: [email protected]; [email protected] Department of Geology, University of Stellenbosch, Private Bag XI, Stellenbosch 7602, South Africa; e-mail: [email protected] àPresent address: British Antarctic Survey, Madingley Road, Cambridge, CB3 0ET, UK; e-mail: [email protected] Typescript received 18 July 2008; accepted in revised form 27 January 2009 Abstract: The first lobopodian known from the Ordovician and Carboniferous. The new fossil preserves an annulated is described from the Soom Shale Lagersta¨tte, South Africa. trunk, lobopods with clear annulations, and curved claws. It The organism shows features homologous to Palaeozoic mar- represents a rare record of a benthic organism from the ine lobopodians described from the Middle Cambrian Bur- Soom Shale, and demonstrates intermittent water oxygena- gess Shale, the Lower Cambrian Chengjiang biota, the Lower tion during the deposition of the unit. Cambrian Sirius Passet Lagersta¨tte and the Lower Cambrian of the Baltic. The discovery provides a link between marine Key words: Lagersta¨tte, lobopodian, Ordovician, Soom Cambrian lobopodians and younger forms from the Silurian Shale. Cambrian lobopodians are a diverse group showing a in an intracratonic basin with water depths of approxi- great variety of body shape, size and ornamentation. mately 100 m (Gabbott 1999). Dominantly quiet water However, they share a segmented onychophoran-like conditions are indicated by a lack of flow-induced sedi- body, paired soft-skinned annulated lobopods, and in mentary structures and the taphonomy of the fossils. -
Corporate Taxation in the Global Offshore Shipping Industry
Transportation & Logistics International Tax Corporate taxation in the global offshore shipping industry www.pwc.com/transport Contents Introduction 4 Executive Summary 6 Vessel types related to the oil & gas offshore industry 8 Vessel types related to the offshore wind farm and offshore construction industry 10 Vessel types related to other services provided offshore 12 Other tax incentives for shipping entities 14 Final remark 15 Territory contacts 16 your priorities, our professionalism… …doing great work together Corporate taxation in the global offshore shipping industry 3 Introduction Shipping companies that are part of the offshore value chain need to understand how differences in tax treatments can affect their business in key territories. This paper, Corporate taxation in the global offshore industry, takes a detailed look at how relevant vessels are handled. It is a supplement to our longer report, “Choosing your course - Corporate taxation of the shipping industry around the globe” , which focuses more broadly on how the shipping industry is taxed. Both papers focus on the countries around the world that are most important for the 1 shipping industry. In this paper, we focus specifically on The offshore industry is a good shipping companies that are part of example. Traditional fossil energy the value chain within the offshore extraction, green energy and offshore industry (wind farms, oil rigs etc.). construction have all made significant While offshore activities may be more advances to keep pace with growing commonly seen as part of the energy demand. That’s led to an increased businesses, the shipping industry demand for specialised offshore vessels actually performs a number of critical and for the development of offshore services using highly specialised vessels. -
Lobopodian Phylogeny Reanalysed
BRIEF COMMUNICATIONS ARISING Phylogenetic position of Diania challenged ARISING FROM J. Liu et al. Nature 470, 526–530 (2011) Liu et al.1 describe a new and remarkable fossil, Diania cactiformis. absent. For example, character 6 (position of frontal appendage) can This animal apparently combined the soft trunk of lobopodians (a only be coded in taxa that possess a frontal appendage (character 5) in group including the extant velvet worms in addition to many the first instance (such that a ‘‘0’’ for character 5 necessitates a ‘‘-’’ for Palaeozoic genera) with the jointed limbs that typify arthropods. character 6). In morphological analyses such as this, inapplicable They go on to promote Diania as the immediate sister group to the states are usually assumed to have no bearing on the analysis, being arthropods, and conjecture that sclerotized and jointed limbs may reconstructed passively in the light of known states. In analyses of therefore have evolved before articulated trunk tergites in the imme- nucleotide data, by contrast, gaps may alternatively be construed as a diate arthropod stem. The data published by Liu et al.1 do not un- fifth and novel state, because shared deletions from some ancestral ambiguously support these conclusions; rather, we believe that Diania sequence may actually be informative. If this assumption is made with probably belongs within an unresolved clade or paraphyletic grade of morphological data, however, all the logically uncodable states in a lobopodians. character are initially assumed to be homologous, and a legitimate Without taking issue with the interpretation of Diania offered by basis for recognizing clades. -
Hallucigenia's Onychophoran-Like Claws
LETTER doi:10.1038/nature13576 Hallucigenia’s onychophoran-like claws and the case for Tactopoda Martin R. Smith1 & Javier Ortega-Herna´ndez1 The Palaeozoic form-taxon Lobopodia encompasses a diverse range of Onychophorans lack armature sclerites, but possess two types of ap- soft-bodied‘leggedworms’ known from exceptionalfossil deposits1–9. pendicular sclerite: paired terminal claws in the walking legs, and den- Although lobopodians occupy a deep phylogenetic position within ticulate jaws within the mouth cavity9,23.AsinH. sparsa, claws in E. Panarthropoda, a shortage of derived characters obscures their evo- kanangrensis exhibit a broad base that narrows to a smooth conical point lutionary relationships with extant phyla (Onychophora, Tardigrada (Fig. 1e–h). Each terminal clawsubtends anangle of130u and comprises and Euarthropoda)2,3,5,10–15. Here we describe a complex feature in two to three constituent elements (Fig. 1e–h). Each smaller element pre- the terminal claws of the mid-Cambrian lobopodian Hallucigenia cisely fills the basal fossa of its container, from which it can be extracted sparsa—their construction from a stack of constituent elements— with careful manipulation (Fig. 1e, g, h and Extended Data Fig. 3a–g). and demonstrate that equivalent elements make up the jaws and claws Each constituent element has a similar morphology and surface orna- of extant Onychophora. A cladistic analysis, informed by develop- ment (Extended Data Fig. 3a–d), even in an abnormal claw where mental data on panarthropod head segmentation, indicates that the element tips are flat instead of pointed (Extended Data Fig. 3h). The stacked sclerite components in these two taxa are homologous— proximal bases of the innermost constituent elements are associated with resolving hallucigeniid lobopodians as stem-group onychophorans. -
The Cambrian ''Explosion'
Perspective The Cambrian ‘‘explosion’’: Slow-fuse or megatonnage? Simon Conway Morris* Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom Clearly, the fossil record from the Cambrian period is an invaluable tool for deciphering animal evolution. Less clear, however, is how to integrate the paleontological information with molecular phylogeny and developmental biology data. Equally challenging is answering why the Cambrian period provided such a rich interval for the redeployment of genes that led to more complex bodyplans. illiam Buckland knew about it, The First Metazoans. Ediacaran assem- 1). The overall framework of early meta- WCharles Darwin characteristically blages (2, 5) are presumably integral to zoan evolution comes from molecular agonized over it, and still we do not fully understanding the roots of the Cambrian data, but they cannot provide insights into understand it. ‘‘It,’’ of course, is the seem- ‘‘explosion,’’ and this approach assumes the anatomical changes and associated ingly abrupt appearance of animals in the that the fossil record is historically valid. It changes in ecology that accompanied the Cambrian ‘‘explosion.’’ The crux of this is markedly at odds, however, with an emergence of bodyplans during the Cam- evolutionary problem can be posed as a alternative view, based on molecular data. brian explosion. The fossil record series of interrelated questions. Is it a real These posit metazoan divergences hun- provides, therefore, a unique historical event or simply an artifact of changing dreds of millions of years earlier (6, 7). As perspective. fossilization potential? If the former, how such, the origination of animals would be Only those aspects of the Ediacaran rapidly did it happen and what are its more or less coincident with the postu- record relevant to the Cambrian diversi- consequences for understanding evolu- lated ‘‘Big Bang’’ of eukaryote diversifi- fication are noted here.