An Updated Classification of Animal Behaviour Preserved in Substrates
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Planispiral Burrows from a Recent Lacustrine Beach, Gander Lake, Newfoundland
Planispiral Burrows from a Recent Lacustrine Beach, Gander Lake, Newfoundland ROBERT B. M AC NAUGHTON Geological Survey of Canada, 3303 – 33 Street NW, Calgary, Alberta T2L 2A7 Canada; e-mail: [email protected] MacNaughton, Robert B. 2003. Planispiral burrows from a Recent lacustrine beach, Gander Lake Newfoundland. Canadian Field-Naturalist 117(4): 577-581. Simple horizontal, planispiral burrows occur in Recent beach sediments on the south shore of Gander Lake, Newfoundland. The burrows apparently represent deposit feeding, possibly by an arthropod. This occurrence extends the known environ- mental range of such traces into lacustrine settings and illustrates that such behaviour is not exclusive to marine settings. Key Words: ichnology, lacustrine, Recent, palaeoecology, Newfoundland. Ichnology is the study of the physical records of The beach on which the burrows were observed is behaviour, including, for example, tracks, trails, bur- approximately 90 m east of the mouth of Fifteen Mile rows, and borings (Bromley 1990). Studies are under- Brook (Figure 1). At the time of study, the beach was taken both in fossil and Recent contexts (palichnol- approximately 3 m wide by 24 m long. It passed on ogy and neoichnology, respectively). Fossilised traces the landward side into forest-covered glacio-fluvial are referred to as “trace fossils” or “ichnofossils” and sand and gravel (Figure 1), from which it was prob- are classified using Linnean binominal nomenclature. ably, in part, derived (cf., Batterson and Vatcher 1991). Although much ichnological research is focused on the Small driftwood logs were scattered over the beach. fossil record, neoichnology can provide crucial data The beach surface consisted of damp to wet (but not when interpreting ancient behaviours (e.g., Schäfer water-saturated), muddy to silty, fine- to medium- 1972; Chamberlain 1975; Ratcliffe and Fagerstrom grained sand containing local concentrations of finely 1980; Metz 1987). -
Sensitivity of Wetland Methane Emissions to Model Assumptions: Application and Model Testing Against Site Observations
Biogeosciences, 9, 2793–2819, 2012 www.biogeosciences.net/9/2793/2012/ Biogeosciences doi:10.5194/bg-9-2793-2012 © Author(s) 2012. CC Attribution 3.0 License. Sensitivity of wetland methane emissions to model assumptions: application and model testing against site observations L. Meng1, P. G. M. Hess2, N. M. Mahowald3, J. B. Yavitt4, W. J. Riley5, Z. M. Subin5, D. M. Lawrence6, S. C. Swenson6, J. Jauhiainen7, and D. R. Fuka2 1Department of Geography and Environmental Studies Program, Western Michigan University, Kalamazoo, MI 49008, USA 2Department of Biological and Environmental Engineering, Cornell University, Ithaca, NY 14850, USA 3Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY 14850, USA 4Department of Natural Resources, Cornell University, Ithaca, NY 14850, USA 5Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley CA 94720, USA 6NCAR-CGD, P.O. Box 3000, Boulder, CO 80307, USA 7Department of Forest Sciences, P.O. Box 27, University of Helsinki, Helsinki 00014, Finland Correspondence to: L. Meng ([email protected]) Received: 14 June 2011 – Published in Biogeosciences Discuss.: 30 June 2011 Revised: 13 June 2012 – Accepted: 29 June 2012 – Published: 30 July 2012 −1 Abstract. Methane emissions from natural wetlands and wetlands contributed 201 Tg CH4 yr , or 78 % of the global rice paddies constitute a large proportion of atmospheric wetland flux. Northern latitude (>50 N) systems contributed −1 methane, but the magnitude and year-to-year variation of 12 Tg CH4 yr . However, sensitivity studies show a large −1 these methane sources are still unpredictable. Here we de- range (150–346 Tg CH4 yr ) in predicted global methane scribe and evaluate the integration of a methane biogeochem- emissions (excluding emissions from rice paddies). -
Reef Encounter Reef Encounter
Volume 30, No. 2 September 2015 Number 42 REEF ENCOUNTER REEF ENCOUNTER United Nations Climate Change Conference Education about Reefs and Climate Change Climate Change: Reef Fish Ecology, Genetic Diversity and Coral Disease Society Honors and Referendum Digital Underwater Cameras Review The News Journal of the International Society for Reef Studies ISSN 0225-27987 REEF ENCOUNTER The News Journal of the International Society for Reef Studies ISRS Information REEF ENCOUNTER Reef Encounter is the magazine style news journal of the International Society for Reef Studies. It was first published in 1983. Following a short break in production it was re-launched in electronic (pdf) form. Contributions are welcome, especially from members. Please submit items directly to the relevant editor (see the back cover for author’s instructions). Coordinating Editor Rupert Ormond (email: [email protected]) Deputy Editor Caroline Rogers (email: [email protected]) Editor Reef Perspectives (Scientific Opinions) Rupert Ormond (email: [email protected]) Editor Reef Currents (General Articles) Caroline Rogers (email: [email protected]) Editors Reef Edge (Scientific Letters) Dennis Hubbard (email: [email protected]) Alastair Harborne (email: [email protected]) Edwin Hernandez-Delgado (email: [email protected]) Nicolas Pascal (email: [email protected]) Editor News & Announcements Sue Wells (email: [email protected]) Editor Book & Product Reviews Walt Jaap (email: [email protected]) INTERNATIONAL SOCIETY FOR REEF STUDIES The International Society for Reef Studies was founded in 1980 at a meeting in Cambridge, UK. Its aim under the constitution is to promote, for the benefit of the public, the production and dissemination of scientific knowledge and understanding concerning coral reefs, both living and fossil. -
FALL 2017 President’S Reflections
PriscumPriscum NEWSLETTER OF THE VOLUME 24, ISSUE 1 President’s Reflections Paleobiology, the finances of both journals appear secure for INSIDE THIS ISSUE: the foreseeable future, and with a much-improved online presence for both journals. To be sure, more work lies ahead, Report on Student but we are collaborating with Cambridge to expand our au- 3 Diversity and Inclusion thor and reader bases, and, more generally, to monitor the ever-evolving publishing landscape. Our partnership with The Dry Dredgers of 10 Cambridge is providing additional enhancements for our Cincinnati, Ohio members, including the digitization of the Society’s entire archive of special publications; as of this writing, all of the PS Embraces the 13 Hydrologic Cycle Society’s short course volumes are now available through the member’s portal, and all remaining Society publications will be made available soon. We are also exploring an exciting PS Events at 2017 GSA 14 new outlet through Cambridge for all future Special Publica- By Arnie Miller (University of tions. Stay tuned! Book Reviews 15 Cincinnati), President In my first year as President, the Society has continued to These are challenging times for move forward on multiple fronts, as we actively explore and Books Available for 28 scientists and for the profes- pursue new means to carry out our core missions of enhanc- Review Announcement sional societies that represent ing and broadening the reach of our science and of our Socie- them. In the national political ty, and providing expanded developmental opportunities for arena, scientific findings, policies, and funding streams that all of our members. -
Arachnida, Solifugae) with Special Focus on Functional Analyses and Phylogenetic Interpretations
HISTOLOGY AND ULTRASTRUCTURE OF SOLIFUGES Comparative studies of organ systems of solifuges (Arachnida, Solifugae) with special focus on functional analyses and phylogenetic interpretations HISTOLOGIE UND ULTRASTRUKTUR DER SOLIFUGEN Vergleichende Studien an Organsystemen der Solifugen (Arachnida, Solifugae) mit Schwerpunkt auf funktionellen Analysen und phylogenetischen Interpretationen I N A U G U R A L D I S S E R T A T I O N zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) an der Mathematisch-Naturwissenschaftlichen Fakultät der Ernst-Moritz-Arndt-Universität Greifswald vorgelegt von Anja Elisabeth Klann geboren am 28.November 1976 in Bremen Greifswald, den 04.06.2009 Dekan ........................................................................................................Prof. Dr. Klaus Fesser Prof. Dr. Dr. h.c. Gerd Alberti Erster Gutachter .......................................................................................... Zweiter Gutachter ........................................................................................Prof. Dr. Romano Dallai Tag der Promotion ........................................................................................15.09.2009 Content Summary ..........................................................................................1 Zusammenfassung ..........................................................................5 Acknowledgments ..........................................................................9 1. Introduction ............................................................................ -
Trace Fossils from Silurian and Devonian Turbidites of the Chauvay Area, Southern Tien Shan, Kyrgyzstan
Annales Societatis Geologorum Poloniae (2009), vol. 79: 1-11. TRACE FOSSILS FROM SILURIAN AND DEVONIAN TURBIDITES OF THE CHAUVAY AREA, SOUTHERN TIEN SHAN, KYRGYZSTAN Michał WARCHO£1 & Stanisław LESZCZYŃSKI2 1 Institute o f Geological Sciences, Polish Academy of Sciences, ul. Senacka 1, 31-002 Kraków, Poland, e-mail: [email protected] Institute o f Geological Sciences, Jagiellonian University, ul. Oleandry 2a, 30-063 Kraków, Poland, e-mail: [email protected] Warchoł, M. & Leszczyński, S., 2009. Trace fossils from Silurian and Devonian turbidites of the Chauvay area, southern Tien Shan, Kyrgyzstan. Annales Societatis Geologorum Poloniae, 79: 1-11. Abstract: The siliciclastic turbidite successions (Pul’gon and Dzhidala Formations) that crop out in the eastern part of the Chauvay River valley, are marked on geological maps as a belt of terrigenous deposits of Silurian- Devonian age. They resemble deposits of overbank areas and deposilional lobes of deep sea fans, and display common trace fos sils particularly on lower surfaces of sandstone beds. Sixleen ichnolaxa representing four morphological groups have been dislinguished. The trace fos sil as semblages suggest their affiliation to the Nereites ichnolacies. Various branched, prelurbidlte forms predominate in both examlned units, although the assemblages of individual units differ slightly in composition. In the Pulg’on Formation, small, densely distributed burrows commonly occur on lower surfaces of sandstone beds. Shallow burrowing depth together with relatively low diversity trace fossil assemblages indicate lowered oxygenation of the sea floor. Key words: Tien Shan; Kyrgyzstan; Silurian-Devonian; turbidites; trace fossils. Manuscript received 12 August 2008, accepted 26 February 2009 INTRODUCTION described from these deposits. -
O ANNALS of CARNEGIE MUSEUM VOL
o ANNALS OF CARNEGIE MUSEUM VOL. 74, NUMBER 3, PP. 151^188 30 SEPTEMBER 2005 MIOCENE FOSSIL DECAPODA (CRUSTACEA: BRACHYURA) FROM PATAGONIA, ARGENTINA, AND THEIR PALEOECOLOGICAL SETTING SILVIO CASADIO Universidad Nacional de La Pampa, Uruguay 151, 6300 Santa Rosa, La Pampa, Argentina ([email protected]) RODNEY M. FELDMANN Research Associate, Section of Invertebrate Paleontology; Department of Geology, Kent State University, Kent, Ohio, 44242 ([email protected]) ANA PARRAS Universidad Nacional de La Pampa, Uruguay 151, 6300 Santa Rosa, La Pampa, Argentina ([email protected]) CARRIE E. SCHWEITZER Research Associate, Section of Invertebrate Paleontology; Department of Geology, Kent State University Stark Campus, Canton, OH 44720 ([email protected]) ABSTRACT Five previously undescribed decapod taxa have been collected from lower upper Miocene rocks of the Puerto Madryn Formation, Peninsula Valdes region, Chubut Province, Patagonia, Argentina. New species include Osachila valdesensis, Rochinia boschii, Romaleon parspinosus, Panopeus piramidensis, and Ocypode vericoncava. Chaceon peruvianus and Proterocarcinus latus are also reported from the unit, in addition to two indeterminate xanthoid species. Assignment of fossil taxa to genera within the Panopeidae Ortmann, 1893, is difficult due to the marked similarity in dorsal carapace characters among several genera. Panopeus whittenensis Glaessner, 1980, is herein referred to Pakicarcinus Schweitzer et al., 2004. The Puerto Madryn Formation exposed near Puerto Piramide contains three distinct Facies Associations (1-3), each associated with specific paleoecological and paleoenvironmental conditions, and which recur throughout the section and represent trangressive systems tract (TST) deposits and highstand systems tract (HST) deposits. Within Facies Association 1, near the base of the section at Puerto Piramide, three paleosurfaces containing invertebrate fossils in life position are exposed and have been carefully mapped in plan view. -
Lecture 16. Endocrine System II
Highlights from Pesticides Lecture Prior to World War II pesticides were _______________, while post-WW II they were ______________. What is meant by the biomagnification of pesticides and what are its consequences? Differentiate between acute and chronic pesticide toxicity. Define the term LD50. Provide two major consequences of the wide-spread use of Mirex (chlorinated hydrocarbon) to control fire ants. Characterize chlorinated hydrocarbon insecticides (DDT and its relatives). What is meant when it is said that the use of pesticides is contextual? Define the term naturally-occurring inorganic pesticide and provide an example. Highlights from Biological Control Lecture Define the three types of biological control and provide an example of each. Contrast predators and parasitoids. What is a density-dependent mortality factor? How has the introduction of the soybean aphids affected pest management in the Midwest? Name one untoward effect related to controlling tamarisk trees on the Colorado River. What is meant by an inoculative release of a biological control agent? How do pesticide economic thresholds affect biological control programs? Lecture 19. Endocrine system II Physiological functions of hormones • Anatomy • Hormones: 14 • Functions Functions of insect hormones: diversity Hormonal functions: Molting as a paradigm egg Eat and grow Bridge Disperse and passage reproduce embryo Postembryonic sequential polymorphism • Nature of molting, growth or metamorphosis? • When and how to molt? The molting process Ecdysis phase Pre-ecdysis phase Post-ecdysis phase Overview • About 90 years’ study (1917-2000): 7 hormones are involved in regulating molting / metamorphosis • 3 in Pre-ecdysis preparatory phase: the initiation and determination of new cuticle formation and old cuticle digestion, regulated by PTTH, MH (Ecdysteroids), and JH • 3 in Ecdysis phase: Ecdysis, i.e. -
Continental Invertebrate and Plant Trace Fossils in Space and Time: State of the Art and Prospects
48 3RD INTERNATIONAL CONFERENCE OF CONTINENTAL ICHNOLOGY, ABSTRACT VOLUME & FIELD TRIP GUIDE Continental invertebrate and plant trace fossils in space and time: State of the art and prospects M. GABRIELA MANGANO1 *, LUIS A. BUATOIS1 1 Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon SK S7N 5E2, Canada * presenting author, [email protected] Continental invertebrate ichnology has experienced a substantial development during the last quarter of century. From being a field marginal to mainstream marine ichnology, represented by a handful of case studies, continental ichnology has grown to occupy a central position within the field of ani- mal-substrate interactions. This evolution is illustrated not only through the accumulation of ichnolog- ic information nurtured by neoichnologic observations and a detailed scrutiny of ancient continental successions, but also through the establishment of new concepts and methodologies. From an ichnofacies perspective, various recurrent associations were defined B( UATOIS & MÁNGANO 1995; GENISE et al. 2000, 2010, 2016; HUNT & LUCAS 2007; EKDALE et al. 2007; KRAPOVICKAS et al. 2016), a situation sharply contrasting with the sole recognition of the Scoyenia ichnofacies as the only valid one during the seventies and eighties (Table 1; Fig. 1). The ichnofacies model now includes not only freshwater ich- nofacies, but also terrestrial ones, most notably those reflecting the complex nature of paleosol trace fossils (GENISE 2017). Trace fossils are now being increasingly used to establish a chronology of the colonization of the land and to unravel the patterns and processes involved in the occupation of ecospace in continental set- tings (e.g. BUATOIS & MÁNGANO 1993; BUATOIS et al. -
Hierarchical Random Walks in Trace Fossils and the Origin of Optimal Search Behavior
Hierarchical random walks in trace fossils and the origin of optimal search behavior David W. Simsa,b,c,1, Andrew M. Reynoldsd, Nicolas E. Humphriesa, Emily J. Southalla, Victoria J. Wearmoutha, Brett Metcalfee, and Richard J. Twitchettf aMarine Biological Association of the United Kingdom, Plymouth PL1 2PB, United Kingdom; bOcean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, Southampton SO14 3ZH, United Kingdom; cCentre for Biological Sciences, University of Southampton, Highfield Campus, Southampton SO17 1BJ, United Kingdom; dRothamsted Research, Harpenden, Hertfordshire AL5 2JQ, United Kingdom; eEarth and Climate Cluster, Faculty of Earth and Life Sciences, VU University Amsterdam, 1081 HV, Amsterdam, The Netherlands; and fDepartment of Earth Sciences, The Natural History Museum, London SW7 5BD, United Kingdom Edited by H. Eugene Stanley, Boston University, Boston, MA, and approved June 19, 2014 (received for review April 1, 2014) −μ Efficient searching is crucial for timely location of food and other “walk clusters” with no characteristic scale, such that P(l) ∼ l , resources. Recent studies show that diverse living animals use a with 1 < μ ≤ 3, where l is the move step length between turns and theoretically optimal scale-free random search for sparse resources μ the power-law exponent. Over many iterations, a Lévy walk will known as a Lévy walk, but little is known of the origins and evo- be distributed much further from its starting position than a lution of foraging behavior and the search strategies of extinct Brownian walk of the same length [hence is termed super- organisms. Here, using simulations of self-avoiding trace fossil trails, diffusive (8)], because small-step walk clusters are interspersed we show that randomly introduced strophotaxis (U-turns)—initiated by long “steps” to new locations, with this pattern repeating by obstructions such as self-trail avoidance or innate cueing—leads across all scales. -
Trace Fossils from Lower Palaeozoic Ocean-Floor Sediments of the Southern Uplands of Scotland M
Transactions of the Royal Society of Edinburgh: Earth Sciences, 73, 67-87, 1982 Trace fossils from Lower Palaeozoic ocean-floor sediments of the Southern Uplands of Scotland M. J. Benton ABSTRACT: The Ordovician and Silurian rocks of the Southern Uplands of Scotland have been interpreted as sediments deposited on the northern margin of the Iapetus Ocean. Trace fossils are abundant at many localities in ocean-floor turbidites and mudstones that usually lack all other evidence of life. Twelve ichnogenera are present, and they are mainly meandering locomotion and feeding trails and burrow networks: Dictyodora, Caridolites, Helminthoida, Neonereites, Nereites, Protovirgularia, Gordia, Megagrapton, Paleodictyon, Chondrites, Plano- lites and Skolithos. The trace fossils occur in at least five distinct assemblages and the composition of these was probably controlled by the frequency and nature of the turbidity currents, and possibly by the oxygen content of the mudstones. Where turbidity currents were weak, abundant Dictyodora, together with Caridolites, Neonereites, Nereites, Protovirgularia and Gordia occur in various combinations. Where currents were stronger, traces such as Gordia, Paleodictyon and Megagrapton may be exhumed and cast on turbidite soles, and the sand may contain Skolithos. The 'deep-sea' Nereites trace fossil facies is divisible into several assemblages, presumably environmentally controlled. KEY WORDS: Iapetus Ocean, ichnology, mudstone, Nereites Facies, Ordovician, shale, Silurian, turbidite. Deep-sea trace fossil assemblages of the Ordovician and 1. Geological setting Silurian are poorly known. The Lower Palaeozoic turbidites and associated mudstones of the Southern Uplands of Scot- 1.1. Structure and history of deposition land preserve at least 12 ichnogenera and there are several The Ordovician and Silurian rocks of the Southern Uplands distinct assemblages that are associated with particular (basalts, cherts, graptolitic shales, greywackes and red or sedimentary conditions. -
Physics of Structural Colors
HOME | SEARCH | PACS & MSC | JOURNALS | ABOUT | CONTACT US Physics of structural colors This article has been downloaded from IOPscience. Please scroll down to see the full text article. 2008 Rep. Prog. Phys. 71 076401 (http://iopscience.iop.org/0034-4885/71/7/076401) The Table of Contents and more related content is available Download details: IP Address: 132.72.138.1 The article was downloaded on 02/07/2008 at 16:04 Please note that terms and conditions apply. IOP PUBLISHING REPORTS ON PROGRESS IN PHYSICS Rep. Prog. Phys. 71 (2008) 076401 (30pp) doi:10.1088/0034-4885/71/7/076401 Physics of structural colors S Kinoshita, S Yoshioka and J Miyazaki Graduate School of Frontier Biosciences, Osaka University, Suita, Osaka 565-0871, Japan E-mail: [email protected] Received 3 September 2007, in final form 16 January 2008 Published 6 June 2008 Online at stacks.iop.org/RoPP/71/076401 Abstract In recent years, structural colors have attracted great attention in a wide variety of research fields. This is because they are originated from complex interaction between light and sophisticated nanostructures generated in the natural world. In addition, their inherent regular structures are one of the most conspicuous examples of non-equilibrium order formation. Structural colors are deeply connected with recent rapidly growing fields of photonics and have been extensively studied to clarify their peculiar optical phenomena. Their mechanisms are, in principle, of a purely physical origin, which differs considerably from the ordinary coloration mechanisms such as in pigments, dyes and metals, where the colors are produced by virtue of the energy consumption of light.