Discovery and Evolution of Novel Hemerythrin Genes in Annelid Worms Elisa M
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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. -
OREGON ESTUARINE INVERTEBRATES an Illustrated Guide to the Common and Important Invertebrate Animals
OREGON ESTUARINE INVERTEBRATES An Illustrated Guide to the Common and Important Invertebrate Animals By Paul Rudy, Jr. Lynn Hay Rudy Oregon Institute of Marine Biology University of Oregon Charleston, Oregon 97420 Contract No. 79-111 Project Officer Jay F. Watson U.S. Fish and Wildlife Service 500 N.E. Multnomah Street Portland, Oregon 97232 Performed for National Coastal Ecosystems Team Office of Biological Services Fish and Wildlife Service U.S. Department of Interior Washington, D.C. 20240 Table of Contents Introduction CNIDARIA Hydrozoa Aequorea aequorea ................................................................ 6 Obelia longissima .................................................................. 8 Polyorchis penicillatus 10 Tubularia crocea ................................................................. 12 Anthozoa Anthopleura artemisia ................................. 14 Anthopleura elegantissima .................................................. 16 Haliplanella luciae .................................................................. 18 Nematostella vectensis ......................................................... 20 Metridium senile .................................................................... 22 NEMERTEA Amphiporus imparispinosus ................................................ 24 Carinoma mutabilis ................................................................ 26 Cerebratulus californiensis .................................................. 28 Lineus ruber ......................................................................... -
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). -
Clustered Brachiopod Hox Genes Are Not Expressed Collinearly and Are
Clustered brachiopod Hox genes are not expressed PNAS PLUS collinearly and are associated with lophotrochozoan novelties Sabrina M. Schiemanna,1, José M. Martín-Durána,1, Aina Børvea, Bruno C. Vellutinia, Yale J. Passamaneckb, and Andreas Hejnol1,a,2 aSars International Centre for Marine Molecular Biology, University of Bergen, Bergen 5006, Norway and bKewalo Marine Laboratory, Pacific Biosciences Research Center, University of Hawaii, Honolulu, HI 96822 Edited by Sean B. Carroll, Howard Hughes Medical Institute and University of Wisconsin–Madison, Madison, WI, and approved January 19, 2017 (received for review August 30, 2016) Temporal collinearity is often considered the main force preserving viding spatial information (29). They also are involved in Hox gene clusters in animal genomes. Studies that combine patterning different tissues (30), and often have been recruited genomic and gene expression data are scarce, however, particularly for the evolution and development of novel morphological traits, in invertebrates like the Lophotrochozoa. As a result, the temporal such as vertebrate limbs (31, 32), cephalopod funnels and arms collinearity hypothesis is currently built on poorly supported foun- (28), and beetle horns (33). dations. Here we characterize the complement, cluster, and expres- Thus, it is not surprising that Hox genes show diverse ar- sion of Hox genes in two brachiopod species, Terebratalia transversa rangements regarding their genomic organization and expression and Novocrania anomala. T. transversa has a split cluster with 10 profiles in the Spiralia (34), a major animal clade that includes lab pb Hox3 Dfd Scr Lox5 Antp Lox4 Post2 Post1 genes ( , , , , , , , , ,and ), highly disparate developmental strategies and body organizations N. anomala Post1 whereas has 9 genes (apparently missing ). -
Polychaete Worms Definitions and Keys to the Orders, Families and Genera
THE POLYCHAETE WORMS DEFINITIONS AND KEYS TO THE ORDERS, FAMILIES AND GENERA THE POLYCHAETE WORMS Definitions and Keys to the Orders, Families and Genera By Kristian Fauchald NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY In Conjunction With THE ALLAN HANCOCK FOUNDATION UNIVERSITY OF SOUTHERN CALIFORNIA Science Series 28 February 3, 1977 TABLE OF CONTENTS PREFACE vii ACKNOWLEDGMENTS ix INTRODUCTION 1 CHARACTERS USED TO DEFINE HIGHER TAXA 2 CLASSIFICATION OF POLYCHAETES 7 ORDERS OF POLYCHAETES 9 KEY TO FAMILIES 9 ORDER ORBINIIDA 14 ORDER CTENODRILIDA 19 ORDER PSAMMODRILIDA 20 ORDER COSSURIDA 21 ORDER SPIONIDA 21 ORDER CAPITELLIDA 31 ORDER OPHELIIDA 41 ORDER PHYLLODOCIDA 45 ORDER AMPHINOMIDA 100 ORDER SPINTHERIDA 103 ORDER EUNICIDA 104 ORDER STERNASPIDA 114 ORDER OWENIIDA 114 ORDER FLABELLIGERIDA 115 ORDER FAUVELIOPSIDA 117 ORDER TEREBELLIDA 118 ORDER SABELLIDA 135 FIVE "ARCHIANNELIDAN" FAMILIES 152 GLOSSARY 156 LITERATURE CITED 161 INDEX 180 Preface THE STUDY of polychaetes used to be a leisurely I apologize to my fellow polychaete workers for occupation, practised calmly and slowly, and introducing a complex superstructure in a group which the presence of these worms hardly ever pene- so far has been remarkably innocent of such frills. A trated the consciousness of any but the small group great number of very sound partial schemes have been of invertebrate zoologists and phylogenetlcists inter- suggested from time to time. These have been only ested in annulated creatures. This is hardly the case partially considered. The discussion is complex enough any longer. without the inclusion of speculations as to how each Studies of marine benthos have demonstrated that author would have completed his or her scheme, pro- these animals may be wholly dominant both in num- vided that he or she had had the evidence and inclina- bers of species and in numbers of specimens. -
Oxygen, Ecology, and the Cambrian Radiation of Animals
Oxygen, Ecology, and the Cambrian Radiation of Animals The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Sperling, Erik A., Christina A. Frieder, Akkur V. Raman, Peter R. Girguis, Lisa A. Levin, and Andrew H. Knoll. 2013. Oxygen, Ecology, and the Cambrian Radiation of Animals. Proceedings of the National Academy of Sciences 110, no. 33: 13446–13451. Published Version doi:10.1073/pnas.1312778110 Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:12336338 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA Oxygen, ecology, and the Cambrian radiation of animals Erik A. Sperlinga,1, Christina A. Friederb, Akkur V. Ramanc, Peter R. Girguisd, Lisa A. Levinb, a,d, 2 Andrew H. Knoll Affiliations: a Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, 02138 b Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, 92093- 0218 c Marine Biological Laboratory, Department of Zoology, Andhra University, Waltair, Visakhapatnam – 530003 d Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA, 02138 1 Correspondence to: [email protected] 2 Correspondence to: [email protected] PHYSICAL SCIENCES: Earth, Atmospheric and Planetary Sciences BIOLOGICAL SCIENCES: Evolution Abstract: 154 words Main Text: 2,746 words Number of Figures: 2 Number of Tables: 1 Running Title: Oxygen, ecology, and the Cambrian radiation Keywords: oxygen, ecology, predation, Cambrian radiation The Proterozoic-Cambrian transition records the appearance of essentially all animal body plans (phyla), yet to date no single hypothesis adequately explains both the timing of the event and the evident increase in diversity and disparity. -
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 -
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. -
Nephtyidae: Polychaeta) Described from the Eastern Pacific
l.OVELL: REVIEW OF NI:PIITYS FROM EASTERN PACIFIC 353 Figure 2. A. Ventral view, dissected specimen of Nephfys caecoides Hartman, 1938, showing pro- boscidial features. Paratype (LACM-AHF 0794). pdp = paired distal papillae, mup = median un- paired papilla. sp = subdistal papillae. B. Frontal view, proboscis of Nephfys caecoides Hartman, 1938, showing paired distal papillae. Paratype (LACM-AHF 0794). pdp = paired distal papillae. Bars I mm. 354 BULLETIN OF MARINE SCIENCE, VOL. 60. NO.2. 1997 118°02.53'W,Aug. 1985,Sta. 13, Rep. 4, 59 m., 1 specimen (CSDOC-P475), Rep. 3, 59 m" 1 speci- men (CSDOC-P476),Oct. 1991,Sta. 13, Rep. 4, 60 m., I specimen (LLL), Jan. 1995,Sta. 13, Rep. 2, 60 m" 2 specimens (LLL), 33°35.59'N, 118°00.05'W,luI. 1994, Sta, 11,30 m., 1 specimen (LLL), 33°35.50'N, 117°58.15'W,luI. 1994, Sta. IS, 30 m., 3 specimens (LLL), 33°34.29'N, 118°00.12'W, luI. 1994,Sta. ZB, Rep. 2, 56 m., 3 specimens (LLL); Santa Barbara Co., GOLETA, 4 Oct. 1994, Sta. B2, Rep. 1, 90 ft., 1 specimen (MBC), Sta. B4, Rep. 2, 1 specimen (MBC), Sta. B6, Rep, 3, 2 speci- mens (MBC); San Luis Obispo Co., just north of Morro Bay, 2\ May 1993,Sta. B1, Rep. 1, 2 speci- mens (MBC), Rep. 4, 1 specimen (MBC), Sta. B2, Rep. 2, 2 specimens(MBC); San Diego Co., Fisher, col., 33°\5.17'N, 117°28.09'W,17 m., 2 specimens (LLL). Corrections and Additions to the Description.-Proboscis with 20 paired distal papillae (Fig. -
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.