(Batillariidae) at a Co-Oceurring Area

Total Page:16

File Type:pdf, Size:1020Kb

(Batillariidae) at a Co-Oceurring Area The malacologicalsocietymalacological society of Japan VENUS Jour. Malac.)n# (Jup, - VoL 57, No. 2C]99R): 115 120 Distribution of Two Intertidal Gastropods, Batielaria 7n2LltofoTmis at a Co-oceurring Area and B. c2emingi (Batillariidae) Naoko ADAcHI and Keiji WADA (Department of Biological Science, fucutty of Science. IVitra Plk)men's University. Kitauaya-nishimachi, IVbra 630-8506, Jtapan) Abstract: Distributions of two intertidal gastropods, Batillaria multijbrmis (Lischke) and B. cumingi (Crosse), were studied in relation to intertidal height and vegetation on a tidal in the intertidalhigher flat where they co-occuTred. B. multijbrmis occurred abundantly lower tevel around tide shore line. In areas with level, while B, cumingi did in the low two species tended to segregate to each other with regard to plant halophilous plants, the in water to species. Laboratery experiment indicated that B. cumingi preferred to stay in interti- more extent than B. muttijbrmis, corresponding with the distributional difference dal height between the two species. Keywords: Distributien, Batillaria multijbrmis, BatiUaria cumingi, tidal flat Introduction to the family Batil- Batiltaria multijbrmis and B. cumingi are intertidal snails belonging lariidae. Their shel! morphology and anatomica! features are similar to each other, which has caused taxonomical confusion (Kurozumi, 1995). But phyletic analysis using mitochon- drial DNA has confirmed that they are distinct species (Ozawa, 1996). The form of egg capsule and the developmental mede has been also known to differ between them (Furota, personal communication). Whilst the two species occur in intertidal zone of various substrata such as rock, boulder and sand or mud in wave-protected bays and estuaries (Abe, 1934; Wells 1983; Adachi & Wada, 1997>, there has been no published work analyzing the distributional difference quantitatively between the two species. This study was under- taken to elucidate distributional diffeTence between B. muttijbrmis and B, cumingi at a co-occurring area. In addition, laboratory experiment was made to compare the preference for air-exposed/submerged condition between thern. Materials and Methods m2) 135055'E), Field study was conducted at a tidal flat(1750 in Yukashigata (33e36'N, middle Japan, located on O.5 km up the mouth of Yukawa Bay in Wakayama Prefecture, half of the during the daytime low tide of spring on 8 and 9 April, 1997. More than tetragonum, Artemisia flat area had halophilous plants such as Zqysia sinica, Limonium the surface water jukudo, and Phragmites communis (Fig. 1). Salinity and temperature of salinometer Toa measured at 3 points around the study area by portable (CM-14P: NII-Electronic Library Service The malacologicalsocietymalacological society of Japan 116 VENUS: Vol, 57, No.2(1998) Electronics Ltd.) at low tide of the study period, ranged from 11.6 to 29.0CVbo and from 16.0 to 34.90C, respectively. Distributions of B. multijbrmis and B. eumingi were investigat- ed by establishing 7 transects crossing the flat. Along each transeet, sampling points were selected at intervals of 2m. Additional 4 sampling points were established under water depth) below the lowest level (1-32cm of low tide. Total number of sampling points was 99 (-40 cm to +58.5 cm relative to mean tide level). At each point, snails were collected by hands to the depth of 2cm, using two 25 x 25 cm quadrats. For quadrats where vegetation occurred, the species plant were recorded. Substratum of all the quadrats was muddy sand with pebbles. The following diagnostic characters were used to identify BatiUaria snails, based on their shell morphology, except small snails for the (<10 mm in shell length) lacking charac- teristic features of respective species. B. multijbrmis; 1) varix turned to siphonal canal well developed, 2) outer lip and shell shape smoothly projecting curved from shell apex to siphonal canal, 3) callus between outer lip and inner white and well developed, B. lip cumingi; 1) no varix turned to siphonal canal, no 2) projecting outer lip,and shell shape not smoothly curved from shell apex siphonal canal, callus to 3) between outer lip and inner lip translucent and not developed. Snail species was identified in case when the speci- men had all the three or the two characters of each species, When the specimen showed beth characters of B. muUijbrmis B. and cumingi or intermediate character between B. muttijbrmis and B. cumingi, its species was not determined. Among 2362 BatiUaria snails collected through the survey, specimens identified as B. multijbrmis accounted for 18.80glb and those as B. cumingi for 64.44{7b. Data of species-undetermined specimens were omitted from analysis. Laboratory experiment was carried out to compare preference for air-exposed!submerged condition between B. muttijbrmis and B. cumingi, using two plastic tanks (19 x 12 x 12 cm high) under constant temperature (250C). Each tank, with seawater (2 cm deep), was tilted in order to make one fourth area of the bottom exposed to air and the remaining area submerged. Ten snails of each species, after being kept under seawater for 12 hours, were placed at the center of each tank, where submerged. The numbers of snails staying under water and those above water were counted at 10 minute intervals during an hour. The experiment was carried out sirnultaneousty between the two tanks (two species) and triplicat- ed, using different individuals. Results Densities of Batillaria multijbrmis and B. cttmingi at sampling points are shown in Fig. 1. B. muttijbrmis was found above low-tide shore-line of the southern half of the study area, whereas B. c"mingi occurred in high density around low-tide shore-line of the northern half of the study area. B. multijbrmis occurred from -16.5 cm to +48.5 cm relative to mean tide level (MTL), while B. cumingi did widely from - 40 cm to + 51.5 cm relative to MTL. The mean (± SD) density per O,125 m2 were 4.67 ± 13.03 in B. mutti- formis and 15.25 ± 26.02 in B. cumingi. The highest density was recorded at 39.5 cm above MTL (73 snails per O,125 m2) in B. miltijbrmis and at 25.5 cm below MTL (133 snails per O.125 m2) in B. cumingi. NII-Electronic Library Service The malaoologloalmalacological societysoolety of Japan Adach1 & Wada Distnbution of Bati〃arla ll7 Seaward B .cumln I ● 一 ● 、 ● ’/ 紅 孝 数 ’一一,,一● P ● 、 、 ● , ■ ; ● 、 ノμ 響 、 ’, ■ , 」 鮮 ● 、、 , ● 、 ’ 緊 、、一 !” o 雲 修 二 ● 、、、 ● 嫡 穿 丶 ’/ ● 丶 ● 窺 莚 圭 ・ : 、 (、 喝4 霊 靠 、、噛眇噛 6 ≒ ; . } 9 、 ● ・ 1 ’ で 豊 : \ _一 ・ ノ 。 、、■ : 《 o ’ 、 、 一 ’ 丶 ・ 0< < 20 丶ご ! 、臓 二 毒 ● ! 、、 ノ r 、 書 ’ ● 20 ≦ < 50 、、 ● , 一 , \ ● 50 ≦ 丶 ↓ 一..− r (denslty per O 125m2 ) : F 且91Densttie 、 of Bantlana mutttformls and B cutntngt at each sampling pomt Sohd hne, broken】lne dnd 、hddcd area lndlcaIe nverbank (at low tide}, low t置de shore lme of tidal fldt dnd 、 dlt marsh arca respectively 各採集 地 声 て の ウ ミ ニ ナ と ホ ソ ウ ミ ニ ナ の 密 度 実線 は 川 岸 (十 潮 時 〕 を , uH 線 及 ひ そ の 内 側 は 人 潮 低 潮線 と i 出域 を,灰 色 の 部 分 は 植 生 σ)範 囲 を 示 す Table l shows the denslty of the two specles ln re 且anon to vegetatlon In areas wlthout vegetatlon the mean of multtformts was at the mld −nde whlle , denslty B hlghest level, of β cu 〃 llngl was at the −tlde areas wlth vegetatlon that hlghest low level In , the hlghest denslty of both specles was observed ln hlgh−tlde level η 〃 , and the denslty of B . 7〃 妙 br lts was hlgher ln sampllng domlnated by Zoysla slnlca and Limonium ごetragonum whlle polnts , the denslty of 、B cumlngl was hlgher m sampllng polnts domlnated by Phragmites communIS − Laboratory experlment showed that the number of snalls found above water was slgnlfl cantly ln muttOformls larger B than ln 8 cumln81 ln one of trlpllcates,and the mean va 匡ue was hlgher ln B 〃 zulhfor 〃 lls than ln B .α 〃 ltngl ln an the trlpllcates(Table 2) 一 NII-ElectronicN 工 工 Eleotronlo LibraryLlbrary Service ・The malaoologioalmalacological societysooiety of Japan ll8 VENUS : Vol .57 , No .2 (1998 ) Tabie 1Mean and range of densities(per O .0625 m2 )of βα ∫1〃aria mutt ヴformis(1eft values )and B . − cumingi (right values )at sampling points with vegctutkon und without vegetation (bare), sepa − and rately for three tide leve且s of high(35−60 cm above MTL )。 mid (0 35 cm above MTL ) low (40−O cm below MTI .), 植 生 の あ る 調 査 点 と 植 生 の な い 調 査 点 に お け る ウ ミ ニ ナ (左 側 の 値 ) と ホ ソ ウ ミ ニ ナ (右 ・ 側 の 値) の ,密 度 の 乎均 値 と 最 大 最 小 値 .調 査 点 を 潮 位 に よ り,高潮 位 (平均 海 水 面 に − − 対 す る 高 さ : 35−60cm ),中 潮 位 (O 35 cm ),低 潮位 ← 40 O・cm > に 分 け て 示 し た . Vegetation dominated by Level Bare ZoysiasinicaLimonium ノ 4厂 ’emis ’c〜 厂σ 8〃1’1θ∫ 1・’〃lonium tet厂agonu 〃 1 fukudoPh comm 初 n ’5 & 14 厂ごe 〃 2 ’∫’α HighMeanRangeN 0/0 .80 3.5/30 9 .2/1.5 0 .3/00 0/18 0.4/0.5 /O−711 −46 /0 −42 0−42 /0− 10 −1/0 0〆14−22 0−3/0−4 39 12 4 2 8 MidMeanRangeN 4 .9/10.3 0 .5f1 .50 1/00 0/0 .50 − 0−34/0 −56 − 1/0−3 _2/0 /O 1 68 2 2 2 LowMeanRangcN 0 .5/12レ9 0−8/0− 104 48 Tab 且e 2 The number of snails recorded as staying above water at 6 counts during l hour in each of replicate : 10 and itsstatistical comparison three replicates (number of snails used in each ) between Batillaria muttiformis and B . cumingi , n .s .: not significant . ウ ミ ニ ナ と ホ ソ ウ ミ ニ ナ の 水 に 対 す る 選 好性 の 室 内実 験 の 結果 .水 槽 内 に お い て ,水 中 に 放 逐 後 ,水 の な い 場 所 に い た 個体 数 を ,10分 お き に 1 時 間 ま で 記録 し,そ の 平均 値 と 標 準 偏 差 お よ び そ れ の 2 種 間 で の 違 い の 検 定 結 果 を 示 し た . Replicate B . mutttformis B . cumingi Wilcoxon signed −ranks test No . Mean ± SDRange Mean ± SDRange 1 1.50 ± 1.12 0 −30 0 00 n .s . (p =0.0679 ) 自う 1.33 ± 1.ll −31 00 n ,s . (p =0.0679 ) 3 l.33 ± 0 .75 −3 ,17 ± 0.37 〇一1 p く 0.05 (p =0 .043D Discussion
Recommended publications
  • (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.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]