(Batillariidae) at a Co-Oceurring Area
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(Gastropoda: Batillariidae) from Elkhorn Slough, California, USA
Mitochondrial DNA Part B Resources ISSN: (Print) 2380-2359 (Online) Journal homepage: https://www.tandfonline.com/loi/tmdn20 The complete mitogenome of the invasive Japanese mud snail Batillaria attramentaria (Gastropoda: Batillariidae) from Elkhorn Slough, California, USA Hartnell College Genomics Group, Paulina Andrade, Lisbeth Arreola, Melissa Belnas, Estefania Bland, Araceli Castillo, Omar Cisneros, Valentin Contreras, Celeste Diaz, Kevin T. Do, Carlos Donate, Estevan Espinoza, Nathan Frater, Garry G. Gabriel, Eric A. Gomez, Gino F. Gonzalez, Myrka Gonzalez, Paola Guido, Dylan Guidotti, Mishell Guzman Espinoza, Ivan Haro, Javier Hernandez Lopez, Caden E. Hernandez, Karina Hernandez, Jazmin A. Hernandez-Salazar, Jeffery R. Hughey, Héctor Jácome-Sáenz, Luis A. Jimenez, Eli R. Kallison, Mylisa S. King, Luis J. Lazaro, Feifei Zhai Lorenzo, Isaac Madrigal, Savannah Madruga, Adrian J. Maldonado, Alexander M. Medina, Marcela Mendez-Molina, Ali Mendez, David Murillo Martinez, David Orozco, Juan Orozco, Ulises Ortiz, Jennifer M. Pantoja, Alejandra N. Ponce, Angel R. Ramirez, Israel Rangel, Eliza Rojas, Adriana Roque, Beatriz Rosas, Colt Rubbo, Justin A. Saldana, Elian Sanchez, Alicia Steinhardt, Maria O. Taveras Dina, Judith Torres, Silvestre Valdez-Mata, Valeria Vargas, Paola Vazquez, Michelle M. Vazquez, Irene Vidales, Frances L. Wong, Christian S. Zagal, Santiago Zamora & Jesus Zepeda Amador To cite this article: Hartnell College Genomics Group, Paulina Andrade, Lisbeth Arreola, Melissa Belnas, Estefania Bland, Araceli Castillo, Omar Cisneros, Valentin Contreras, Celeste Diaz, Kevin T. Do, Carlos Donate, Estevan Espinoza, Nathan Frater, Garry G. Gabriel, Eric A. Gomez, Gino F. Gonzalez, Myrka Gonzalez, Paola Guido, Dylan Guidotti, Mishell Guzman Espinoza, Ivan Haro, Javier Hernandez Lopez, Caden E. Hernandez, Karina Hernandez, Jazmin A. -
Shell Classification – Using Family Plates
Shell Classification USING FAMILY PLATES YEAR SEVEN STUDENTS Introduction In the following activity you and your class can use the same techniques as Queensland Museum The Queensland Museum Network has about scientists to classify organisms. 2.5 million biological specimens, and these items form the Biodiversity collections. Most specimens are from Activity: Identifying Queensland shells by family. Queensland’s terrestrial and marine provinces, but These 20 plates show common Queensland shells some are from adjacent Indo-Pacific regions. A smaller from 38 different families, and can be used for a range number of exotic species have also been acquired for of activities both in and outside the classroom. comparative purposes. The collection steadily grows Possible uses of this resource include: as our inventory of the region’s natural resources becomes more comprehensive. • students finding shells and identifying what family they belong to This collection helps scientists: • students determining what features shells in each • identify and name species family share • understand biodiversity in Australia and around • students comparing families to see how they differ. the world All shells shown on the following plates are from the • study evolution, connectivity and dispersal Queensland Museum Biodiversity Collection. throughout the Indo-Pacific • keep track of invasive and exotic species. Many of the scientists who work at the Museum specialise in taxonomy, the science of describing and naming species. In fact, Queensland Museum scientists -
Bering Sea Marine Invasive Species Assessment Alaska Center for Conservation Science
Bering Sea Marine Invasive Species Assessment Alaska Center for Conservation Science Scientific Name: Batillaria attramentaria Phylum Mollusca Common Name Japanese false cerith Class Gastropoda Order Neotaenioglossa Family Batillariidae Z:\GAP\NPRB Marine Invasives\NPRB_DB\SppMaps\BATATT.png 153 Final Rank 46.00 Data Deficiency: 12.50 Category Scores and Data Deficiencies Total Data Deficient Category Score Possible Points Distribution and Habitat: 12.25 23 7.50 Anthropogenic Influence: 6 10 0 Biological Characteristics: 17 25 5.00 Impacts: 5 30 0 Figure 1. Occurrence records for non-native species, and their geographic proximity to the Bering Sea. Ecoregions are based on the classification system by Spalding et al. (2007). Totals: 40.25 87.50 12.50 Occurrence record data source(s): NEMESIS and NAS databases. General Biological Information Tolerances and Thresholds Minimum Temperature (°C) -2 Minimum Salinity (ppt) 7 Maximum Temperature (°C) 40 Maximum Salinity (ppt) 33 Minimum Reproductive Temperature (°C) Minimum Reproductive Salinity (ppt) Maximum Reproductive Temperature (°C) Maximum Reproductive Salinity (ppt) Additional Notes Size of adult shells ranges from 10 to 34 mm. The shell is usually gray-brown, often with a white band below the suture, but can range from light brown to dirty-black. Historically introduced with the Pacific oyster, Crassostrea gigas, but in recent years, it has been found in areas where oysters are not cultivated. Nevertheless, its spread has been attributed to anthropogenic vectors rather than natural dispersal. Report updated on Wednesday, December 06, 2017 Page 1 of 13 1. Distribution and Habitat 1.1 Survival requirements - Water temperature Choice: Considerable overlap – A large area (>75%) of the Bering Sea has temperatures suitable for year-round survival Score: A 3.75 of High uncertainty? 3.75 Ranking Rationale: Background Information: Temperatures required for year-round survival occur over a large Based on its geographic distribution, B. -
Estuary Monitoring Toolkit Turning the Tide 2006
An estuaries toolkit for New Zealand communities Gretchen Robertson & Monica Peters Published by the TAIERI Trust, 2006 Cover Artwork by Theresa Reihana - www.maoriart.com Illustrations by Monica Peters Graphic Design by Mark Jackson - www.ecoimage.co.nz This work is copyright. The copying, adaptation, or issuing of this work to the public on a non-profit basis is welcomed. No other use of this work is permitted without the prior consent of the copyright holder(s). The TAIERI Trust acknowledges the Minister for the Environment’s Sustainable Management Fund, which is administered by the Ministry for the Environment. The Ministry for the Environment does not support or endorse the content of this publication in any way. I Acknowledgements Thank you to the Waikouaiti-Karitane River and Estuary Care Group for your patience in trialing early drafts of the monitoring section. To Dr Barry Robertson and Leigh Stevens of Wriggle Coastal Management, your willingness to work with us to develop user-friendly tools for estuarine monitoring and assessment have transformed this kit from an idea to a reality. To Mark Jackson for his wonderful graphic design skills. To the Cawthron Institute for providing images and advice, especially Rod Asher for his species identification knowledge. To employees of the New Zealand Landcare Trust for providing information about community estuary groups around New Zealand. To the Manawatu Estuary Trust for providing us with inspiration and a copy of your wonderful CD. To the Auckland Regional Council and Christchurch City Council for information about your estuarine programmes. To NIWA for providing inspiration through your mangrove based ‘Estuary Monitoring by Communities’ document. -
Molecular Phylogenetic Relationship of Thiaridean Genus Tarebia Lineate
Journal of Entomology and Zoology Studies 2017; 5(3): 1489-1492 E-ISSN: 2320-7078 P-ISSN: 2349-6800 Molecular phylogenetic relationship of Thiaridean JEZS 2017; 5(3): 1489-1492 © 2017 JEZS genus Tarebia lineate (Gastropoda: Cerithioidea) Received: 23-03-2017 Accepted: 24-04-2017 as determined by partial COI sequences Chittaranjan Jena Department of Biotechnology, Vignan’s University (VFSTRU), Chittaranjan Jena and Krupanidhi Srirama Vadlamudi, Andhra Pradesh, India Abstract An attempt was made to investigate phylogenetic affinities of the genus Tarebia lineata sampled from Krupanidhi Srirama the Indian subcontinent using partial mitochondrial COI gene sequence. The amplified partial mt-COI Department of Biotechnology, gene sequence using universal primers, LCO1490 and HCO2198 resulted into ~700 base pair DNA Vignan’s University (VFSTRU), Vadlamudi, Andhra Pradesh, fragment. The obtained nucleotide sequence of partial COI gene of T. lineata was submitted to BLAST India analysis and 36 close relative sequences of the chosen genera, Cerithioidea were derived. Maximum likelihood (ML) algorithm in-biuilt in RAxML software tool was used to estimate phylogenetic their affinities. The present analysis revealed that a single assemblage of the family Thiaridae supported by a bootstrap value of 96% is earmarked at the base of the derived cladogram as a cluster and emerged as a sister group with another four Cerithioideans. Our dataset brought add-on value to the current taxonomy of Thiaridae of the clade Sorbeconcha by clustering them as sister and non-sister groups indicating the virtual relations. Out of seven genera, Tarebia and Melanoides formed as primary and secondary clusters within the Thiaridae. The monophyly of Thiaridae and its conspecifics were depicted in the cladogram. -
8. the Mollusk Fauna of the Monte Postale
Rendiconti della Società Paleontologica Italiana, 4, 2014, pp. 89-94 Excursion guidebook CBEP 2014-EPPC 2014-EAVP 2014-Taphos 2014 Conferences The Bolca Fossil-Lagerstätten: A window into the Eocene World (editors C.A. Papazzoni, L. Giusberti, G. Carnevale, G. Roghi, D. Bassi & R. Zorzin) 8. The mollusk fauna of the Monte Postale Stefano DOMINICI S. Dominici, Museo di Storia Naturale, Università di Firenze, Via La Pira 4, I-50121 Firenze, Italy; !$`"$ Fossil marine mollusks from Monte Postale, about one mile NE of Bolca (Verona and Vicenza Provinces) and 300 m N of the “Pesciara” (see the map in Papazzoni & Trevisani, 2006), were collected and catalogued at least since the 18th`[ seen, in the second decade of the 19th century, as means to date the rocks, and the already O"~P`[` geologists. In 1823, on the footsteps of Alberto Fortis (1778), Alexandre Brongniart drew stratigraphic sections and collected fossils in the Vicenza province, assigning the Bolca and Roncà invertebrates to one and the same geological interval. In the newly introduced 5~`[` Paris Basin. This meant to Brongniart that they belonged to the older Tertiary, and were distinct from the fossil shells described by Giambattista Brocchi in 1814, typifying the younger Tertiary (Rudwick, 2005). “I can relate the calcareous-trappic terrains of Northern Italy to the lower formation, the most ancient of the upper sediment [i.e., the Tertiary]. I’m struck by the analogy between these two terrains, their utter similarity under almost any aspect. Nothing of the lower terrains of the Parisian limestone is missing in Bolca, Roncà, etc. -
Gastropod Fauna of the Cameroonian Coasts
Helgol Mar Res (1999) 53:129–140 © Springer-Verlag and AWI 1999 ORIGINAL ARTICLE Klaus Bandel · Thorsten Kowalke Gastropod fauna of the Cameroonian coasts Received: 15 January 1999 / Accepted: 26 July 1999 Abstract Eighteen species of gastropods were encoun- flats become exposed. During high tide, most of the tered living near and within the large coastal swamps, mangrove is flooded up to the point where the influence mangrove forests, intertidal flats and the rocky shore of of salty water ends, and the flora is that of a freshwater the Cameroonian coast of the Atlantic Ocean. These re- regime. present members of the subclasses Neritimorpha, With the influence of brackish water, the number of Caenogastropoda, and Heterostropha. Within the Neriti- individuals of gastropod fauna increases as well as the morpha, representatives of the genera Nerita, Neritina, number of species, and changes in composition occur. and Neritilia could be distinguished by their radula Upstream of Douala harbour and on the flats that lead anatomy and ecology. Within the Caenogastropoda, rep- to the mangrove forest next to Douala airport the beach resentatives of the families Potamididae with Tympano- is covered with much driftwood and rubbish that lies on tonos and Planaxidae with Angiola are characterized by the landward side of the mangrove forest. Here, Me- their early ontogeny and ecology. The Pachymelaniidae lampus liberianus and Neritina rubricata are found as are recognized as an independent group and are intro- well as the Pachymelania fusca variety with granulated duced as a new family within the Cerithioidea. Littorini- sculpture that closely resembles Melanoides tubercu- morpha with Littorina, Assiminea and Potamopyrgus lata in shell shape. -
Constructional Morphology of Cerithiform Gastropods
Paleontological Research, vol. 10, no. 3, pp. 233–259, September 30, 2006 6 by the Palaeontological Society of Japan Constructional morphology of cerithiform gastropods JENNY SA¨ LGEBACK1 AND ENRICO SAVAZZI2 1Department of Earth Sciences, Uppsala University, Norbyva¨gen 22, 75236 Uppsala, Sweden 2Department of Palaeozoology, Swedish Museum of Natural History, Box 50007, 10405 Stockholm, Sweden. Present address: The Kyoto University Museum, Yoshida Honmachi, Sakyo-ku, Kyoto 606-8501, Japan (email: [email protected]) Received December 19, 2005; Revised manuscript accepted May 26, 2006 Abstract. Cerithiform gastropods possess high-spired shells with small apertures, anterior canals or si- nuses, and usually one or more spiral rows of tubercles, spines or nodes. This shell morphology occurs mostly within the superfamily Cerithioidea. Several morphologic characters of cerithiform shells are adap- tive within five broad functional areas: (1) defence from shell-peeling predators (external sculpture, pre- adult internal barriers, preadult varices, adult aperture) (2) burrowing and infaunal life (burrowing sculp- tures, bent and elongated inhalant adult siphon, plough-like adult outer lip, flattened dorsal region of last whorl), (3) clamping of the aperture onto a solid substrate (broad tangential adult aperture), (4) stabilisa- tion of the shell when epifaunal (broad adult outer lip and at least three types of swellings located on the left ventrolateral side of the last whorl in the adult stage), and (5) righting after accidental overturning (pro- jecting dorsal tubercles or varix on the last or penultimate whorl, in one instance accompanied by hollow ventral tubercles that are removed by abrasion against the substrate in the adult stage). Most of these char- acters are made feasible by determinate growth and a countdown ontogenetic programme. -
Quantifying Geographic Variation in Physiological Performance to Address the Absence of Invading Species1
12 (3): 358-365 (2005) Quantifying geographic variation in physiological performance to address the absence of invading species1 James E. BYERS, Department of Zoology, University of New Hampshire, 46 College Road, Durham, New Hampshire 03824, USA, e-mail: [email protected] Abstract: An estuarine snail (Batillaria attramentaria), introduced to northern California marshes, is displacing a native confamilial mudsnail (Cerithidea californica) through superior competition for shared, limiting food resources. Batillaria, however, is absent from similar marsh habitats in southern California. I tested whether regional-scale variation in relative performance (growth) of the snails may have influenced Batillaria’s invasion pattern. I quantified growth using RNA:DNA ratios (a growth index that I ground-truthed with direct growth measurements) for snails collected throughout their entire collective North American distribution. Batillaria exhibited a high growth rate that was more than double Cerithidea’s growth rate in sympatric populations. A broad-scale relationship of species’ growth rates against latitude projected an amply adequate growth rate for Batillaria in southern California where it is presently absent. Furthermore, growth rates of Cerithidea did not increase in southern California, suggesting that Batillaria would maintain its dramatic relative performance advantage. Thus, even if resources are limiting at southern latitudes, biotic resistance through competition with Cerithidea does not explain Batillaria’s absence. Among alternative, untested hypotheses for Batillaria’s absence, insufficient propagule inoculation has strongest support. Because transplant experiments with nonindigenous species are unethical, examination of species’ performance over geographic scales provides a powerful alternative approach for invasion studies. Keywords: estuaries, exotic species, exploitative competition, invasibility, latitudinal gradients, macroecology, nonindigenous species, RNA:DNA ratios. -
Paleocene Freshwater, Brackish-Water and Marine Molluscs from Al-Khodh, Oman
Late Cretaceous to ?Paleocene freshwater, brackish-water and marine molluscs from Al-Khodh, Oman Simon Schneider, heinz A. KollmAnn & mArtin PicKford Bivalvia and Gastropoda from the late Campanian to Maastrichtian deltaic Al-Khodh Formation and from the overlying ?Paleocene shallow marine Jafnayn Limestone Formation of northeastern Oman are described. Freshwater bivalves include three species of Unionidae, left in open nomenclature, due to limited preservation. These are the first pre-Pleistocene unionids recorded from the Arabian Peninsula, where large freshwater bivalves are absent today. Brackish-water bivalves are represented by two species of Cyrenidae. Geloina amithoscutana sp. nov. extends the range of Geloina to the Mesozoic and to ancient Africa. Muscatella biszczukae gen. et sp. nov. has a unique combination of characters not shared with other genera in the Cyrenidae. Brackish-water gastropods comprise Stephaniphera coronata gen. et sp. nov. in the Hemisinidae; Subtemenia morgani in the new genus Subtemenia (Pseudomelaniidae); Cosinia sp. (Thiaridae); Pyrazus sp. (Batillariidae); and Ringiculidae sp. indet. From the Jafnayn Limestone Formation, several marginal marine mollusc taxa are also reported. The fossils are assigned to four mollusc communities and associations, which are indicative of different salinity regimes. • Key words: Unionidae, Cyrenidae, Pseudomelaniidae, Hemisinidae, taxonomy, palaeobiogeography. SCHNEIDER, S., KOLLMANN, H.A. & PICKFORD, M. 2020. Late Cretaceous to ?Paleocene freshwater, brackish-water and marine molluscs from Al-Khodh, Oman. Bulletin of Geosciences 95(2), 179–204 (10 figures, 5 tables). Czech Geo- l ogical Survey, Prague. ISSN 1214-1119. Manuscript received August 12, 2019; accepted in revised form March 30, 2020; published online May 30, 2020; issued May 30, 2020. -
Marine Ecology Progress Series 228:153
MARINE ECOLOGY PROGRESS SERIES Vol. 228: 153–163, 2002 Published March 6 Mar Ecol Prog Ser Carnivore/non-carnivore ratios in northeastern Pacific marine gastropods James W. Valentine1,*, Kaustuv Roy2, David Jablonski3 1Department of Integrative Biology and Museum of Paleontology, University of California, Berkeley, California 94720, USA 2Ecology, Behavior and Evolution Section, Division of Biology, University of California at San Diego, 9500 Gilman Drive, La Jolla, California 92093-0116, USA 3Department of Geophysical Sciences, University of Chicago, 5734 Ellis Avenue, Chicago, Illinois 60637, USA ABSTRACT: For 2321 species of shelled gastropods of the northeastern Pacific, the ratio of carnivo- rous to non-carnivorous species (C/NC ratio), computed for each degree of latitude, reveals striking spatial changes, with tropical and arctic areas characterized by high values and with the mid- latitudes having the lowest ratios. This latitudinal trend is markedly different from trends for terres- trial clades. The zonal variation in C/NC ratios within bins is largely due to differences in geographic ranges of the groups; for example, tropical carnivorous species range farther than non-carnivorous ones, thus overlapping them in more latitudinal bins. Differences in the distribution and diversity of carnivorous and non-carnivorous species may arise from a number of sources, including variability of primary production in the tropical eastern Pacific, patchiness of substrates to which non-carnivores are adapted, narrow dietary specializations of tropical carnivores, and higher provinciality found in extratropical regions. KEY WORDS: Trophic ratios · Latitudinal diversity trends · Provinciality · Variable productivity Resale or republication not permitted without written consent of the publisher INTRODUCTION diversities (Faaborg 1985, Jeffries & Lawton 1985, Karr et al. -
Terra Australis 24
Appendix 5: Shellfish reference collection* FAMILY SPECIES COMMON NAME/S PREFERRED ENVIRONMENT/SIZE MARINE BIVALVIA Anomiidae Anomia trigonopsis (Hutton, 1877) To 10m among shell debris; to 75mm jingle shell Arcidae Anadara trapezia (Deshayes, 1840) Intertidal mangroves; estuarine tidal flats; seagrass beds; Sydney cockle; blood to 70mm cockle; mud ark Cardiidae Acrosterigma vertebratum In muddy sand of intertidal flats Carditidae Venericardia sp. In sand in shallow water Chamidae Chama fibula (Reeve, 1846) Attached to shell or coral debris to 10m; to 30mm spiny oyster Corbulidae Corbula (Serracorbula) crassa (Reeve, 1843) Sandy/muddy substrates; to 18mm Donacidae Donax (Plebidonax) deltoides (Lamarck, 1818) pipi; Littoral sand; to 60mm eugarie; wong Mactridae Mactrid sp. Littoral sand Mytilidae Trichomya hirsutus (Lamarck, 1819) Tidal estuary; attached to rocks from low tide level to 16m; hairy mussel to 65mm Noetiidae Arcopsis deliciosa (Iredale, 1939) Rocky substrates to 81m; to 10mm Noetiidae Arcopsis symmetrica (Reeve, 1844) Rocky substrates; shallow water; to 16mm Ostreidae Saccostrea glomerata (Gould, 1850) Sheltered rocky shores and mangroves; mid-intertidal; syn. S. cuccullata Sydney rock oyster; to 100mm syn. S. commercialis rock oyster; commercial oyster Pteriidae Pinctada albina sugillata (Reeve, 1857) Attached to rocks and corals to 22m; to 110mm pearl oyster Tellinidae Tellina sp. Littoral sand Tellinidae Tellina (Cyclotellina) remies (Linnaeus, 1758) Littoral sand; to 70mm Trapeziidae Trapezium (Neotrapezium) (Lamarck, 1819) Littoral shell debris, coral crevices or in oyster clumps; sublaevigatum 3–10m; to 65mm Ungulinidae Felaniella (Zemysia) subglobosa (E.A. Smith, 1885) Coral/mud to 13m; to 4.5mm syn. F. subglobosa Veneridae Antigona chemnitzii (Hanley, 1844) Littoral sand; to 100mm Veneridae Dosinia tumida (Gray, 1838) Littoral sand; to 58mm Veneridae Gafrarium australe (Sowerby, 1850) Intertidal, muddy sand; to 25mm Veneridae Irus sp.