Clustered Brachiopod Hox Genes Are Not Expressed Collinearly and Are
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Classification
Science Classification Pupil Workbook Year 5 Unit 5 Name: 2 3 Existing Knowledge: Why do we put living things into different groups and what are the groups that we can separate them into? You can think about the animals in the picture and all the others that you know. 4 Session 1: How do we classify animals with a backbone? Key Knowledge Key Vocabulary Animals known as vertebrates have a spinal column. Vertebrates Some vertebrates are warm-blooded meaning that they Species maintain a consistent body temperature. Some are cold- Habitat blooded, meaning they need to move around to warm up or cool down. Spinal column Vertebrates are split into five main groups known as Warm-blooded/Cold- mammals, amphibians, reptiles, birds and fish. blooded Task: Look at the picture here and think about the different groups that each animal is part of. How is each different to the others and which other animals share similar characteristics? Write your ideas here: __________________________ __________________________ __________________________ __________________________ __________________________ __________________________ ____________________________________________________ ____________________________________________________ ____________________________________________________ ____________________________________________________ ____________________________________________________ 5 How do we classify animals with a backbone? Vertebrates are the most advanced organisms on Earth. The traits that make all of the animals in this group special are -
DOGAMI Open-File Report O-86-06, the State of Scientific
"ABLE OF CONTENTS Page INTRODUCTION ..~**********..~...~*~~.~...~~~~1 GORDA RIDGE LEASE AREA ....................... 2 RELATED STUDIES IN THE NORTH PACIFIC .+,...,. 5 BYDROTHERMAL TEXTS ........................... 9 34T.4 GAPS ................................... r6 ACKNOWLEDGEMENT ............................. I8 APPENDIX 1. Species found on the Gorda Ridge or within the lease area . .. .. .. .. .. 36 RPPENDiX 2. Species found outside the lease area that may occur in the Gorda Ridge Lease area, including hydrothermal vent organisms .................................55 BENTHOS THE STATE OF SCIENTIFIC INFORMATION RELATING TO THE BIOLOGY AND ECOLOGY 3F THE GOUDA RIDGE STUDY AREA, NORTZEAST PACIFIC OCEAN: INTRODUCTION Presently, only two published studies discuss the ecology of benthic animals on the Gorda Sidge. Fowler and Kulm (19701, in a predominantly geolgg isal study, used the presence of sublittor31 and planktsnic foraminiferans as an indication of uplift of tfie deep-sea fioor. Their resuits showed tiac sedinenta ana foraminiferans are depositea in the Zscanaba Trough, in the southern part of the Corda Ridge, by turbidity currents with a continental origin. They list 22 species of fararniniferans from the Gorda Rise (See Appendix 13. A more recent study collected geophysical, geological, and biological data from the Gorda Ridge, with particular emphasis on the northern part of the Ridge (Clague et al. 19843. Geological data suggest the presence of widespread low-temperature hydrothermal activity along the axf s of the northern two-thirds of the Corda 3idge. However, the relative age of these vents, their present activity and presence of sulfide deposits are currently unknown. The biological data, again with an emphasis on foraminiferans, indicate relatively high species diversity and high density , perhaps assoc iated with widespread hydrotheraal activity. -
Mechanics Unlocks the Morphogenetic Puzzle of Interlocking Bivalved Shells
Mechanics unlocks the morphogenetic puzzle of interlocking bivalved shells Derek E. Moultona,1 , Alain Gorielya , and Regis´ Chiratb aMathematical Institute, University of Oxford, Oxford, OX2 6GG, United Kingdom; and bCNRS 5276, LGL-TPE (Le Laboratoire de Geologie´ de Lyon: Terre, Planetes,` Environnement), Universite´ Lyon 1, 69622 Villeurbanne Cedex, France Edited by Sean H. Rice, Texas Tech University, Lubbock, TX, and accepted by Editorial Board Member David Jablonski November 11, 2019 (received for review September 24, 2019) Brachiopods and mollusks are 2 shell-bearing phyla that diverged tal events causing shell injuries. Yet, in all cases the interlocking from a common shell-less ancestor more than 540 million years ago. of the 2 shell edges is tightly maintained. These observations Brachiopods and bivalve mollusks have also convergently evolved imply that the interlocking pattern emerges as the result of epi- a bivalved shell that displays an apparently mundane, yet strik- genetic interactions modulating the behavior of the secreting ing feature from a developmental point of view: When the shell mantle during shell development. is closed, the 2 valve edges meet each other in a commissure that Here, we provide a geometric and mechanical explanation forms a continuum with no gaps or overlaps despite the fact that for this morphological trait based on a detailed analysis of the each valve, secreted by 2 mantle lobes, may present antisymmet- shell geometry during growth and the physical interaction of the ric ornamental patterns of varying regularity and size. Interlock- shell-secreting soft mantle with both the rigid shell edge and ing is maintained throughout the entirety of development, even the opposing mantle lobe. -
Six3 Demarcates the Anterior-Most Developing Brain Region In
Steinmetz et al. EvoDevo 2010, 1:14 http://www.evodevojournal.com/content/1/1/14 RESEARCH Open Access Six3 demarcates the anterior-most developing brain region in bilaterian animals Patrick RH Steinmetz1,6†, Rolf Urbach2†, Nico Posnien3,7, Joakim Eriksson4,8, Roman P Kostyuchenko5, Carlo Brena4, Keren Guy1, Michael Akam4*, Gregor Bucher3*, Detlev Arendt1* Abstract Background: The heads of annelids (earthworms, polychaetes, and others) and arthropods (insects, myriapods, spiders, and others) and the arthropod-related onychophorans (velvet worms) show similar brain architecture and for this reason have long been considered homologous. However, this view is challenged by the ‘new phylogeny’ placing arthropods and annelids into distinct superphyla, Ecdysozoa and Lophotrochozoa, together with many other phyla lacking elaborate heads or brains. To compare the organisation of annelid and arthropod heads and brains at the molecular level, we investigated head regionalisation genes in various groups. Regionalisation genes subdivide developing animals into molecular regions and can be used to align head regions between remote animal phyla. Results: We find that in the marine annelid Platynereis dumerilii, expression of the homeobox gene six3 defines the apical region of the larval body, peripherally overlapping the equatorial otx+ expression. The six3+ and otx+ regions thus define the developing head in anterior-to-posterior sequence. In another annelid, the earthworm Pristina, as well as in the onychophoran Euperipatoides, the centipede Strigamia and the insects Tribolium and Drosophila,asix3/optix+ region likewise demarcates the tip of the developing animal, followed by a more posterior otx/otd+ region. Identification of six3+ head neuroectoderm in Drosophila reveals that this region gives rise to median neurosecretory brain parts, as is also the case in annelids. -
Analysis of the Complete Mitochondrial DNA Sequence of the Brachiopod Terebratulina Retusa Places Brachiopoda Within the Protostomes
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/12415870 Analysis of the complete mitochondrial DNA sequence of the brachiopod Terebratulina retusa places Brachiopoda within the protostomes Article in Proceedings of the Royal Society B: Biological Sciences · November 1999 DOI: 10.1098/rspb.1999.0885 · Source: PubMed CITATIONS READS 83 50 2 authors, including: Martin Schlegel University of Leipzig 151 PUBLICATIONS 2,931 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Rare for a reason? Scale-dependence of factors influencing rarity and diversity of xylobiont beetles View project Bat diversity and vertical niche activity in the fluvial flood forest Leipzig View project All content following this page was uploaded by Martin Schlegel on 22 May 2014. The user has requested enhancement of the downloaded file. Analysis of the complete mitochondrial DNA sequence of the brachiopod Terebratulina retusa places Brachiopoda within the protostomes Alexandra Stechmann* and Martin Schlegel UniversitÌt Leipzig, Institut fÏr Zoologie/Spezielle Zoologie,Talstr. 33, 04103 Leipzig, Germany Brachiopod phylogeny is still a controversial subject. Analyses using nuclear 18SrRNA and mitochondrial 12SrDNA sequences place them within the protostomes but some recent interpretations of morphological data support a relationship with deuterostomes. In order to investigate brachiopod a¤nities within the metazoa further,we compared the gene arrangement on the brachiopod mitochondrial genome with several metazoan taxa. The complete (15 451bp) mitochondrial DNA (mtDNA) sequence of the articulate brachiopod Terebratulina retusa was determined from two overlapping long polymerase chain reaction products. All the genes are encoded on the same strand and gene order comparisons showed that only one major rearrangement is required to interconvert the T.retusa and Katharina tunicata (Mollusca: Polyplaco- phora) mitochondrial genomes. -
Coincidence of Photic Zone Euxinia and Impoverishment of Arthropods
www.nature.com/scientificreports OPEN Coincidence of photic zone euxinia and impoverishment of arthropods in the aftermath of the Frasnian- Famennian biotic crisis Krzysztof Broda1*, Leszek Marynowski2, Michał Rakociński1 & Michał Zatoń1 The lowermost Famennian deposits of the Kowala quarry (Holy Cross Mountains, Poland) are becoming famous for their rich fossil content such as their abundant phosphatized arthropod remains (mostly thylacocephalans). Here, for the frst time, palaeontological and geochemical data were integrated to document abundance and diversity patterns in the context of palaeoenvironmental changes. During deposition, the generally oxic to suboxic conditions were interrupted at least twice by the onset of photic zone euxinia (PZE). Previously, PZE was considered as essential in preserving phosphatised fossils from, e.g., the famous Gogo Formation, Australia. Here, we show, however, that during PZE, the abundance of arthropods drastically dropped. The phosphorous content during PZE was also very low in comparison to that from oxic-suboxic intervals where arthropods are the most abundant. As phosphorous is essential for phosphatisation but also tends to fux of the sediment during bottom water anoxia, we propose that the PZE in such a case does not promote the fossilisation of the arthropods but instead leads to their impoverishment and non-preservation. Thus, the PZE conditions with anoxic bottom waters cannot be presumed as universal for exceptional fossil preservation by phosphatisation, and caution must be paid when interpreting the fossil abundance on the background of redox conditions. 1 Euxinic conditions in aquatic environments are defned as the presence of H2S and absence of oxygen . If such conditions occur at the chemocline in the water column, where light is available, they are defned as photic zone euxinia (PZE). -
GY 112L: Earth History Lab
UNIVERSITY OF SOUTH ALABAMA GY 112L: Earth History Lab Week 9: Paleozoic Part 3 Instructor: Dr. Douglas W. Haywick Today’s Agenda The Paleozoic Part 3 (Week 9 exercises) 1) Brachiopods 2) Molluscs 3) Alabama Stratigraphy Brachiopoda Brachiopod Facts: Taxonomy: (under review) Phylum: Brachiopoda Class: Inarticulata Class: Articulata Brachiopoda Brachiopod Facts: Taxonomy: Phylum: Brachiopoda Class: Inarticulata Class: Articulata Range: Cambrian-Recent (Inarticulates were first) Brachiopoda Brachiopod Facts: Taxonomy: Phylum: Brachiopoda Class: Inarticulata Class: Articulata Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder Brachiopoda Brachiopod Facts: Taxonomy: Phylum: Brachiopoda Class: Inarticulata Class: Articulata Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder Mineral composition: calcite, phosphate Brachiopoda Brachiopod Facts: Taxonomy: Phylum: Brachiopoda Class: Inarticulata Class: Articulata Range: Cambrian-Recent Mode of Life: Marine, benthic, filter feeder Mineral composition: calcite, phosphate Fossil Pres.: pristine (sometimes external molds) The Brachiopod Animal Inarticulates The Brachiopod Animal Inarticulates Brachiopod Symmetry Symmetrical across the valves (down the medial line) Brachiopod Symmetry Symmetrical across the valves (down the medial line) Brachiopod Symmetry Symmetrical across the valves (down the medial line) Articulate Brachiopods Brachiopod Symmetry Symmetrical across the valves (down the medial line) Articulate Brachiopods Brachiopod Symmetry Not symmetrical between -
Alvinella Pompejana (Annelida)
MARINE ECOLOGY - PROGRESS SERIES Vol. 34: 267-274, 1986 Published December 19 Mar. Ecol. Prog. Ser. Tubes of deep sea hydrothermal vent worms Riftia pachyptila (Vestimentif era) and Alvinella pompejana (Annelida) ' CNRS Centre de Biologie Cellulaire, 67 Rue Maurice Gunsbourg, 94200 Ivry sur Seine, France Department of Biological Sciences, University of Lancaster, Bailrigg. Lancaster LA1 4YQ. England ABSTRACT: The aim of this study was to compare the structure and chemistry of the dwelling tubes of 2 invertebrate species living close to deep sea hydrothermal vents at 12"48'N, 103'56'W and 2600 m depth and collected during April 1984. The Riftia pachyptila tube is formed of a chitin proteoglycan/ protein complex whereas the Alvinella pompejana tube is made from an unusually stable glycoprotein matrix containing a high level of elemental sulfur. The A. pompejana tube is physically and chemically more stable and encloses bacteria within the tube wall material. INTRODUCTION the submersible Cyana in April 1984 during the Biocy- arise cruise (12"48'N, 103O56'W). Tubes were pre- The Pompeii worm Alvinella pompejana, a poly- served in alcohol, or fixed in formol-saline, or simply chaetous annelid, and Riftia pachyptila, previously rinsed and air-dried. considered as pogonophoran but now placed in the Some pieces of tubes were post-fixed with osmium putative phylum Vestimentifera (Jones 1985), are tetroxide (1 O/O final concentration) and embedded in found at a depth of 2600 m around deep sea hydrother- Durcupan. Thin sections were stained with aqueous mal vents. R. pachyptila lives where the vent water uranyl acetate and lead citrate and examined using a (anoxic, rich in hydrogen sulphide, temperatures up to Phillips EM 201 TEM at the Centre de Biologie 15°C) mixes with surrounding seawater (oxygenated, Cellulaire, CNRS, Ivry (France). -
Fossils of Indiana of Indiana of Indiana
Fossils of Indiana Lesson Plan Grades 4 ––– 666 INFORMATION FOR EDUCATORS TABLE OF CONTENTS Background Text for Educators……pps. 3 – 9 Vocabulary…………………………pps. 10 – 12 Discussion Questions…………........pps. 13 – 17 Activities…………………………...pps. 18 – 32 Additional Activities……………….pps. 33 – 37 Activity Handouts………………….pps. 38 – 45 Activity Answers..…………………pps. 46 – 49 Resources……………………………p. 50 Evaluation……………………………p. 51 INTRODUCTION The study of fossils is a key element to understanding our past. Fossils give us clues about how humans and different animals lived and evolved. This lesson plan incorporates oral and written language, reading, vocabulary development, science, social studies and critical thinking. The lessons contained in this packet are intended for grades 4 to 6. The activities are designed to be innovative and meet Indiana Academic Standards. The text and worksheets are reproducible. SETTING THE STAGE To begin the lesson plan, you might want the environment of your entire classroom to reflect the ideas of science, geology and discovery. This can be achieved by incorporating this theme into bulletin boards, learning centers, art projects and whatever else you are doing in your classroom. Educators looking for good picture resources for their classroom can contact the Indiana State Museum Store and ask about our The Carr Poster Series, which depicts animals throughout Indiana’s geologic history and includes a geologic timeline. When you set the tone of your classroom in this manner, learning becomes an all- encompassing experience for your students. We encourage you to use this lesson plan as a springboard to further knowledge about fossils and their importance in understanding history. This lesson plan is comprised of four general areas: Geologic Time, Fossil Formation, Discovering Fossils and Paleozoic Fossils. -
Tropical Marine Invertebrates CAS BI 569 Phylum ANNELIDA by J
Tropical Marine Invertebrates CAS BI 569 Phylum ANNELIDA by J. R. Finnerty Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA “BILATERIA” (=TRIPLOBLASTICA) Bilateral symmetry (?) Mesoderm (triploblasty) Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA “COELOMATA” True coelom Coelomata gut cavity endoderm mesoderm coelom ectoderm [note: dorso-ventral inversion] Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA PROTOSTOMIA “first mouth” blastopore contributes to mouth ventral nerve cord The Blastopore ! Forms during gastrulation ectoderm blastocoel blastocoel endoderm gut blastoderm BLASTULA blastopore The Gut “internal, epithelium-lined cavity for the digestion and absorption of food sponges lack a gut simplest gut = blind sac (Cnidaria) blastopore gives rise to dual- function mouth/anus through-guts evolve later Protostome = blastopore contributes to the mouth Deuterostome = blastopore becomes the anus; mouth is a second opening Protostomy blastopore mouth anus Deuterostomy blastopore -
Two Episodes of Environmental Change at the Permian–Triassic Boundary of the GSSP Section Meishan
Earth-Science Reviews 115 (2012) 163–172 Contents lists available at SciVerse ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Two episodes of environmental change at the Permian–Triassic boundary of the GSSP section Meishan Hongfu Yin a,⁎, Shucheng Xie a, Genming Luo a, Thomas J. Algeo b, Kexin Zhang a a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China b Department of Geology, University of Cincinnati, Cincinnati, OH 45221, USA article info abstract Article history: High-resolution stratigraphic records through the Permian–Triassic boundary (PTB) interval of the global Received 4 May 2012 stratotype section and point (GSSP) at Meishan, Zhejiang Province, China reveal that the PTB crisis was not a sin- Accepted 10 August 2012 gle, abrupt catastrophe. A bed-by-bed analysis of environmental and biotic changes makes clear that the crisis Available online 29 August 2012 can be resolved into two discrete episodes, each consisting of three stages: A) unstably oscillating conditions, B) peak crisis conditions, and C) ameliorating conditions. The first crisis episode commenced in Bed 23, peaked Keywords: in Beds 24e–26, and ameliorated in Beds 27 and 28, while the second crisis episode commenced in Bed 29, Mass extinction – Conodont biostratigraphy peaked in Beds 34 38, and ameliorated in Beds 39 and higher. The macroscopic mass extinctions happened Carbon isotopes not at the beginning, nor the end of each cycle, but at times when the crisis or perturbation of environments Volcanic event beds began. These extinction events do not show detectable feedbacks to concurrent environmental changes. -
Discovery and Evolution of Novel Hemerythrin Genes in Annelid Worms Elisa M
Costa-Paiva et al. BMC Evolutionary Biology (2017) 17:85 DOI 10.1186/s12862-017-0933-z RESEARCHARTICLE Open Access Discovery and evolution of novel hemerythrin genes in annelid worms Elisa M. Costa-Paiva1,2, Nathan V. Whelan2,3, Damien S. Waits2, Scott R. Santos2, Carlos G. Schrago1 and Kenneth M. Halanych2* Abstract Background: Despite extensive study on hemoglobins and hemocyanins, little is known about hemerythrin (Hr) evolutionary history. Four subgroups of Hrs have been documented, including: circulating Hr (cHr), myohemerythrin (myoHr), ovohemerythrin (ovoHr), and neurohemerythrin (nHr). Annelids have the greatest diversity of oxygen carrying proteins among animals and are the only phylum in which all Hr subgroups have been documented. To examine Hr diversity in annelids and to further understand evolution of Hrs, we employed approaches to survey annelid transcriptomes in silico. Results: Sequences of 214 putative Hr genes were identified from 44 annelid species in 40 different families and Bayesian inference revealed two major clades with strong statistical support. Notably, the topology of the Hr gene tree did not mirror the phylogeny of Annelida as presently understood, and we found evidence of extensive Hr gene duplication and loss in annelids. Gene tree topology supported monophyly of cHrs and a myoHr clade that included nHrs sequences, indicating these designations are functional rather than evolutionary. Conclusions: The presence of several cHrs in early branching taxa suggests that a variety of Hrs were present in the common ancestor of extant annelids. Although our analysis was limited to expressed-coding regions, our findings demonstrate a greater diversity of Hrs among annelids than previously reported.