Molecular Evidence for the Existence of Five Cryptic Species Within The
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Life History and Stable Regeneration of the Endangered Saltmarsh
Plankton Benthos Res 9(2): 114–121, 2014 Plankton & Benthos Research © The Japanese Association of Benthology Life history and stable regeneration of the endangered saltmarsh sesarmid crab Clistocoeloma sinense in small populations of the isolated metapopulation of Tokyo Bay, Japan 1, 2 TAKESHI YUHARA * & TOSHIO FUROTA 1 Department of Environmental Science, Graduate School of Science, Toho University, Funabashi, Chiba 274–8510, Japan 2 Faculty of Sciences, Tokyo Bay Ecosystem Research Center, Toho University, Funabashi, Chiba 274–8510, Japan Received 2 October 2013; Accepted 17 March 2014 Abstract: The saltmarsh sesarmid crab, Clistocoeloma sinense, inhabits the muddy substrata in upper intertidal saltmarshes, and is designated as endangered in Japan. Seasonal changes were investigated in population characters, including abundance, time to sexual maturity, reproductive season, and recruitment of juveniles in a regional meta- population in Tokyo Bay. Crab samples were collected monthly at five small isolated habitats along the coast of the bay from July, 2011, to March, 2013. Ovigerous females were found during summer in a single peak, and a peak of ju- venile recruitment occurred in autumn. Size distribution analysis indicates that growth is slower than for other salt- marsh crab species and life span is at least 4 years. Females reach maturity when they enter the second breeding sea- son following recruitment. The slow growth and reclusive behavior of C. sinense may be closely related to the charac- teristics of its habitat which is under buried stones or wood in the uppermost part of intertidal muddy substrata. Re- cruitment of juveniles and the presence of breeding females were observed at all five study sites located along the Tokyo Bay coastline, suggesting that each population stably regenerates by larval settlement following larval disper- sal and growth in the water column in Tokyo Bay. -
A Phylogenetic Analysis of the Genus Eunice (Eunicidae, Polychaete, Annelida)
Blackwell Publishing LtdOxford, UKZOJZoological Journal of the Linnean Society0024-4082© 2007 The Linnean Society of London? 2007 1502 413434 Original Article PHYLOGENY OF EUNICEJ. ZANOL ET AL. Zoological Journal of the Linnean Society, 2007, 150, 413–434. With 12 figures A phylogenetic analysis of the genus Eunice (Eunicidae, polychaete, Annelida) JOANA ZANOL1*, KRISTIAN FAUCHALD2 and PAULO C. PAIVA3 1Pós-Graduação em Zoologia, Museu Nacional/UFRJ, Quinta da Boa Vista s/n°, São Cristovão, Rio de Janeiro, RJ 20940–040, Brazil 2Department of Invertebrate Zoology, NMNH, Smithsonian Institution, PO Box 37012, NHB MRC 0163, Washington, DC 20013–7012, USA 3Departamento de Zoologia, Insituto de Biologia, Universidade Federal do Rio de Janeiro, CCS, Bloco A, Sala A0-104, Ilha do Fundão, Rio de Janeiro, RJ 2240–590, Brazil Received April 2006; accepted for publication December 2006 Species of Eunice are distributed worldwide, inhabiting soft and hard marine bottoms. Some of these species play sig- nificant roles in coral reef communities and others are commercially important. Eunice is the largest and most poorly defined genus in Eunicidae. It has traditionally been subdivided in taxonomically informal groups based on the colour and dentition of subacicular hooks, and branchial distribution. The monophyly of Eunice and of its informal subgroups is tested here using cladistic analyses of 24 ingroup species based on morphological data. In the phylo- genetic hypothesis resulting from the present analyses Eunice and its subgroups are paraphyletic; the genus may be divided in at least two monophyletic groups, Eunice s.s. and Leodice, but several species do not fall inside these two groups. -
And Biofacies of Mudstone in the Pliocene-Pleistocene Title Kazusa Group, Boso Peninsula, Central Japan
Litho- and Biofacies of Mudstone in the Pliocene-Pleistocene Title Kazusa Group, Boso Peninsula, Central Japan Author(s) Sato, Mika Memoirs of the Faculty of Science, Kyoto University. Series of Citation geology and mineralogy (1992), 57(1): 1-31 Issue Date 1992-08-31 URL http://hdl.handle.net/2433/186673 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University MEMolRs oF THE FAcuLTy oF SclENcE, KyoTO UNIvERslTy,SERIEs oF GEoL. & MINERAL, , VoL LVII, No. 1, pp. 1-31, August 31, l992 Litho- and Biofacies of Mudstone in the Pliocene-Pleistocene Kazusa Group, Boso Peninsu la, Central Japan By Mika SATo" (Manuscript received March 30, 1992) Contents Abstract ."...",".,,".,..H,,",,.,....",,,",H.H..,,".,,,...H.,.-H,,,",...,"..,,,,",,",.. 1 Introduction.,,.",,...,.".,,,.,.H,,.-,,,,-H.,.,,,,"......,.,,,,"...,.H.H.....,,,,,",....H 2 Geological setting ",,,"........,,,",,..H...,,.,...H...,-,,.,.H".......,.,,,,.,,............, 3 Stratigraphy ...-,,...,,H",,-,",.H...,",,,..."...",,,,...H...-,,,,,-....H,.,,,m,,".... 3 Geological age of the Kazusa Group .,..,,,........J•••-••-••••--•••-••••J,,••••-••••••J• 10 Sedimentological features ofmudstone and benthic faunas ,,..,.......,..,,.,, 10 Sedjmentary environment ofmudstones in the Kazusa Group ...,.,,,....... 25 A. Stratigraphic change ofmudstone facies ..,..........,,..,,,............,, 25 B. Reconstruction ofsedimentary environemtns ofthe laminated fine-grained mudstone (Facies E) ,..........,,...............,...,,.......... 27 Conclusion ,,"..H.,,,.,,,,H..H..-,,,..,..H,,.,,",....H.,",,",..-"....,,..,,,,H......,H,,. -
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 ......................................................................... -
Symposium Full Program
11.4 Center for Condensed Matter Sciences, NTU 11.5-6 Howard Civil Service International House 2019 Organizer Ecological Engineering Research Center, National Taiwan University Co-Organizers College of Bioresources and Agriculture, National Taiwan University Wisdom Informatics Solutions for Environment Co., Ltd Symposium Program Sponsors Biodiversity Research Center, Academia Sinica The Japanese Association of Benthology Marine National Park Headquartrers, Taiwan Ministry of Science and Technology, Taiwan The Plankton Society of Japan Ocean Conversation Administration, Ocean Affairs Council, Taiwan Contents Welcome Messages .........................................................................2 More Welcomes and Greetings from Previous AMBS Chairmans .................................................3 Symposium Schedule ......................................................................7 Conference Information ................................................................8 Symposium Venue Map ..................................................................9 Information for the Presenters .................................................11 Student Presentation Contest Rules .......................................12 Presentation Schedule .................................................................13 Poster Presentation Schedule ...................................................20 Keynote Speaker Abstracts & Biographies ............................25 Organizers and Sponsors.............................................................32 -
Mie Prefecture, Japan
Vol.3, No.2, 205-213 (2013) Open Journal of Ecology http://dx.doi.org/10.4236/oje.2013.32024 Vegetation communities in estuarine tidal flats in the different river and basin environments of the four major rivers of Ise Bay (Suzuka, Tanaka, Kushida and Miya), Mie Prefecture, Japan Korehisa Kaneko1*, Seiich Nohara2 1Ecosystem Conservation Society-Japan, Tokyo, Japan; *Corresponding Author: [email protected] 2Center for Environmental Biology and Ecosystem Studies, National Institute for Environmental Studies, Ibaraki, Japan Received 10 January 2013; revised 13 February 2013; accepted 10 March 2013 Copyright © 2013 Korehisa Kaneko, Seiich Nohara. This is an open access article distributed under the Creative Commons Attribu- tion License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. ABSTRACT tion of a gravelly sandy surface where an annual salt marsh plant community of Suaeda maritime In this study, we compared and analysed vege- and Artemisia fukudo has been established and tation communities in the estuarine tidal flats of grown as the annual precipitation and catch- the four major rivers of Ise Bay (Suzuka River, ment volume of the basin have increased. Tanaka River, Kushida River and Miya River) in Mie Prefecture, Japan. Along the Suzuka River, Keywords: Annual Salt Marsh Plant; Perennial Salt Eragrostis curvula of the exotic plant accounted Marsh Plant; Flood Volume; Water Level; for 60.0% or more of the entire surface area, and Disturbance the plant volume was high. Along the Tanaka River, Suaeda maritima community occupied the sand-mud zone in the vicinity of the shoreline on 1. -
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Kameo et al. Progress in Earth and Planetary Science (2020) 7:36 Progress in Earth and https://doi.org/10.1186/s40645-020-00355-x Planetary Science RESEARCH ARTICLE Open Access Calcareous nannofossil biostratigraphy of the Lower–Middle Pleistocene boundary of the GSSP, Chiba composite section in the Kokumoto Formation, Kazusa Group, central Japan, and implications for sea- surface environmental changes Koji Kameo1*, Yoshimi Kubota2, Yuki Haneda3, Yusuke Suganuma4,5 and Makoto Okada6 Abstract The Chiba composite section (CbCS), in the middle of the Boso Peninsula in central Japan, was ratified as the Global Boundary Stratotype Section and Point (GSSP) for the Lower–Middle Pleistocene boundary, accompanied by the Matuyama–Brunhes (M–B) paleomagnetic polarity boundary in January 2020. This study examined the calcareous nannofossil biostratigraphy of the CbCS to describe potential nannofossil events and discuss sea-surface environments around the M–B paleomagnetic polarity boundary. There are no clear biohorizons at the M–B paleomagnetic polarity boundary, although a temporary disappearance of Gephyrocapsa specimens (≥ 5 μmin diameter), an important calcareous nannofossil genus in the Pleistocene, occurs just above the Lower–Middle Pleistocene boundary. Although this is a characteristic event around the M–B paleomagnetic polarity boundary, it is unclear whether the event is globally traceable. Changes in the environmental proxy taxa of calcareous nannofossils in the CbCS revealed that sea-surface environments were driven by glacial-interglacial and millennial-scale climate forces. The time-transgressive change of the Tn value, a calcareous nannofossil temperature index, is mostly concordant with the planktonic foraminiferal oxygen isotope fluctuation. Abundant occurrences of a warm-water species, Umbilicosphaera spp., indicate that the Kuroshio Current was strong after ~ 783 ka. -
An Annotated Checklist of the Marine Macroinvertebrates of Alaska David T
NOAA Professional Paper NMFS 19 An annotated checklist of the marine macroinvertebrates of Alaska David T. Drumm • Katherine P. Maslenikov Robert Van Syoc • James W. Orr • Robert R. Lauth Duane E. Stevenson • Theodore W. Pietsch November 2016 U.S. Department of Commerce NOAA Professional Penny Pritzker Secretary of Commerce National Oceanic Papers NMFS and Atmospheric Administration Kathryn D. Sullivan Scientific Editor* Administrator Richard Langton National Marine National Marine Fisheries Service Fisheries Service Northeast Fisheries Science Center Maine Field Station Eileen Sobeck 17 Godfrey Drive, Suite 1 Assistant Administrator Orono, Maine 04473 for Fisheries Associate Editor Kathryn Dennis National Marine Fisheries Service Office of Science and Technology Economics and Social Analysis Division 1845 Wasp Blvd., Bldg. 178 Honolulu, Hawaii 96818 Managing Editor Shelley Arenas National Marine Fisheries Service Scientific Publications Office 7600 Sand Point Way NE Seattle, Washington 98115 Editorial Committee Ann C. Matarese National Marine Fisheries Service James W. Orr National Marine Fisheries Service The NOAA Professional Paper NMFS (ISSN 1931-4590) series is pub- lished by the Scientific Publications Of- *Bruce Mundy (PIFSC) was Scientific Editor during the fice, National Marine Fisheries Service, scientific editing and preparation of this report. NOAA, 7600 Sand Point Way NE, Seattle, WA 98115. The Secretary of Commerce has The NOAA Professional Paper NMFS series carries peer-reviewed, lengthy original determined that the publication of research reports, taxonomic keys, species synopses, flora and fauna studies, and data- this series is necessary in the transac- intensive reports on investigations in fishery science, engineering, and economics. tion of the public business required by law of this Department. -
The Techniques and Tools of the Kazusabori Well-Boring
地球環境研究,Vol.6(2004) The Techniques and Tools of the Kazusabori Well-boring Hiroki TAKAMURA* Keyword: boring technology, lower Pleistocene system, traditional, a thin strip of bamboo Making much of that opportunity, Hisahiro . Introduction Ishiwatari (Risshop University) and the author car- Kazusabori, a well-boring technology developed in the ried out studies on the details of the technical aspect, area now called Kimitsu-gun, Chiba Prefecture, has tools and history of Kazusabori. contributed to construction of numerous flowing (ar- tesian) wells for non-commercial and farming water . Geological considerations on the history of supply, since its birth during the Bunka period (1804- Kazusabori 1818) in the Edo era. In 1892, this method was em- ployed even in oil well development in Niigataand The Kazusa district occupies the central part of Chiba Akita Prefectures. It was also introduced to the inter- Prefecture, bordering on the Shimousa district on the national community, to India, in particular, as the north, on Awa on the south, facing Tokyo Bay on the Kazusa System. It was Japan's most advanced well- west and facing the Pacific Ocean on theeast. In the boring technology of the time. southern area, a mountain range forms a border be- tween Kazusaand Awa, from Mt. Kiyosumi (383m) However, in the wake of the introduction of the ro- to Mt. Nokogiri (228m). Having their headwaters in tary boring technology and the spread of water- this area, the Yoro, Obitsu, Koito andMinato Rivers works, the Kazusabori methodbegan losing its pour into the Bay of Tokyo while the Ichinomiyaand prevalence since the mid-1950s, and today, it is no Isumi Rivers flow into the Pacific Ocean. -
Formation in Chiba Prefecture, Japan
ll Lateral change of foraminiferal fauna at the horizon ● just below the tuffaceous key bed, O7, of the Otadai Formation in Chiba Prefecture, Japan Akio Hatta (Received October 8, 1985) Department of Science Education, Faculty of Education, Kagoshima University. K喝oshima 890, Japan Abstract Lateral change of foraminiferal fauna in a siltstone just below a tu打key bed O7 0f the Otadai Format- ion of Chiba Prefecture was investigated traversing the whole breadth of the Boso Peninsula. ● Faunal composition of planktonic Foraminifera of this horizon shows insignificant lateral change (Text-figure 4). This hirizon may belong to N.22 of the Blow (1969)'s zonation scheme, judging from the ranges of Globorotalia tosaensis Takayanagi & Saito, G. hirtuta d'Orbigny and Globigerina parabulloides Blow. The planktonic ratios of this horizon indicate the values between 70.3 and 84.1 %, and this suggests a typical off-shore environment. Faunal composition of benthonic Foraminifera shows significant lateral change (Text-figure 5). The siltstone beneath the O7 bed contains many specimens of deep sea species, such as Bulimina aculeata d'Orbigny, B. nipponica Asano, Bolivina robusta Brady and Uvigerina akitaensis Asano at every locality. Elphidium group and Quinqueloculina group, which are characteristic of shallow water, are very rare m the central part, but increase westward. ● Faunal change of benthonic Foraminifera is scrutinized by using the factor aualysis. The results are interpreted by referring to the distribution of Foraminifera in the adjacent seas of Japan. From the result, it can be thought that the second factor in the g-mode factor analysis is a parameter of abundance of shallow water elements (Table 2 and Text一五gure 6). -
Giant Eunicid Polychaetes (Annelida) in Shallow Tropical and Temperate Seas
FORUM Giant Eunicid Polychaetes (Annelida) in shallow tropical and temperate seas Sergio I. Salazar-Vallejo1, Luis F. Carrera-Parra1 & J. Angel de León-González2 1. El Colegio de la Frontera Sur, Chetumal, México; [email protected] 2. Fac. Ciencias Biológicas, Universidad Autónoma Nuevo León, Monterrey Received 04-XI-2010. Corrected 10-IV-2011. Accepted 19-V-2011. Abstract: Some species of Eunice might reach giant size, often being longer than 2m, and they are known from tropical and temperate seas. Despite their large size and recent internet notoriety, there remain some taxonomic problems in large-sized eunicids, especially since original descriptions were brief and type materials are often missing. As a mean to encourage the solution of this situation, we review the historical progress in the taxonomy of the group, including some comments on generic and specific delineation, and recommend some critical steps to solve the current confusion. These ideally would include collecting in type localities, evaluate ontogenetic morphological changes, and generate some molecular analysis to complement the morphological approach. Rev. Biol. Trop. 59 (4): 1463-1474. Epub 2011 December 01. Key words: Eunicidae, Eunice, Leodice, Indian Ocean, Red Sea, Pacific Ocean, Caribbean Sea, Mediterranean Sea, opinion article. Some species of Eunice can be over 3m very large, but in this note we will only refer to long (Pruvot & Racovitza 1895, Uchida et al. members of Eunice. 2009), making them the largest polychaete These “Giant Eunicids” were called “Bob- species and placing them among the longest bit-worms” by an underwater photographer benthic invertebrates. The genus is very rich in alluring to the regretful incident of the USA species, having about 300 available names, and Bobbit family, where the wife cut off her making it the largest genus among polychaetes. -
RÍAS and TIDAL-SEA ESTUARIES F. Vilas, Departamento De
Rías and tidal-sea estuaries in: Knowledge for Sustainable Development, an insight into the Encyclopedia of Life Support Systems. UNESCO- EOLSS (ed.) vol 2, theme 11.6.3, 799-829. 2002 RÍAS AND TIDAL-SEA ESTUARIES F. Vilas, Departamento de Geociencias Marinas, Universidad de Vigo, Spain Keywords: Rías, tidal-sea estuaries, sedimentology, morphology, sedimentary infilling Summary Coastal inlets such as estuaries, rías and bays occupy areas which are partially exposed to wave action and the hydrodynamic processes generated by tidal currents and fluvial discharges. These processes are often quite complex, and regulate many of the morphological and sedimentological characteristics occurring in this type of environment. In aerial view, rías and estuaries are characterised by a funnel-shaped geometry and deep entrances, with a considerable reduction on both dimensions upstream. From a physiographical viewpoint, both types are classified as drowned river valleys as they were formed by sea flooding of Pleistocene-Holocene river valleys during the last transgression. This chapter is a review of the main processes and attributes in rías and tidal-sea estuaries, initially focusing on the basic physical processes, morphology and sedimentology, with some examples highlighting the differences between both types which, historically, were considered as one. To document the Late Quaternary history of the Rías Baixas on the north-west Atlantic coast of Spain, a brief description of the sedimentary infilling is presented. It is also intended to form a discussion of individual cases, and to the more specific characteristics given in other works in this volume, that were only briefly mentioned in the present article. 1.