Padatan Terlarut Dan Tss (Total Suspended Solid)/Padatan Terusupensi Di Pesisir Perairan Sungai Kawal Kabupaten Bintan

Total Page:16

File Type:pdf, Size:1020Kb

Padatan Terlarut Dan Tss (Total Suspended Solid)/Padatan Terusupensi Di Pesisir Perairan Sungai Kawal Kabupaten Bintan STRUKTUR KOMUNITAS MOLUSKA BENTIK BERBASIS TDS (TOTAL DISSOLVED SOLID)/PADATAN TERLARUT DAN TSS (TOTAL SUSPENDED SOLID)/PADATAN TERUSUPENSI DI PESISIR PERAIRAN SUNGAI KAWAL KABUPATEN BINTAN Benthic Mollusks Community Strukture Based on TDS (Total Dissolved Solid) and TSS (Total Suspended Solid) at Kawal River Kabupaten Bintan WULAN SUCI 1, WINNY RETNA MELANI DAN TENGKU SAID RAZA’I 2) Study Programme Aquatic Resources Management Faculty of Marine Science and Fisheries, University Maritime Raja Ali Haji Email : [email protected] ABSTRAK Penelitian ini dilakukan di perairan Sungai Kawal Kelurahan Kawal Kabupaten Bintan. Penelitian ini bertujuan untuk mengetahui jumlah kelimpahan moluska bentik dan mengetahui ada atau tidaknya pengaruh dari TSS dan TDS terhadap kelimpahan moluska bentik di perairan Sungai Kawal. Berdasarkan hasil penelitian di lapangan moluska bentik yang ditemukan terdiri dari 2 kelas dari filum Moluska yaitu kelas Gastropoda dan kelas Bivalvia dengan jumlah spesies sebanyak 7 spesies. Setelah di analisis nilai kelimpahan total moluska bentik pada ketiga stasiun penelitian berkisar antara 501 ind/m2 – 1610 ind/m2 .dengan kelimpahan jenis tertinggi berasal dari spesies Pseudovertagus aluco dari Kelas Gastropoda. Nilai indeks Keanekaragaman (H”) moluska bentik berkisar antara 2,18 – 2,57. Nilai indeks Keseragaman (E) moluska bentik berkisar antara 0,88 – 0,91. Sedangkan nilai indeks Dominnasi (C) moluska bentik berkisar antara 0,16 – 0,19. Berdasarkan hasil regresi berganda diperoleh Nilai Koefisien Determinasi (R2) sebesar 76,7 %. Hal ini menunjukkan bahwa persentase sumbangan pengaruh variable bebas (TSS dan TDS) terhadap variable terikat (Kelimpahan) sebesar 76,7 %. Atau variasi variabel bebas yang digunakan dalam model mampu menjelaskan sebesar 76,7 % variasi variabel terikat. ABSTRACT The research was conducted in the waters of the River Kawal, Kawal Village Bintan. This study aims to determine the number and abundance of benthic molluscs determine whether or not the effect of TSS and TDS to the abundance of benthic molluscs in the waters of the waters of the River Guard. Based on the results of research in the field of benthic molluscs are found to be composed of two classes of the phylum molluscs class Gastopod and Bivalve classes with as many as 7 species number of species. Once in the analysis of the value of the total abundance of benthic molluscs in the third research station ranged from 501 ind/m2 – 1610 ind/m2. Comes with the highest species abundance of the species of Class Gastropod a Pseudovertagus alco. Diversity index values (H’) of benthic mollucsc ranged from 2,18 - 2,57. Uniformity index value (E) of benthic ranged from 0,88 – 0,91. While the index value Dominants (C) benthic molluscs ranged from 0,16 – 0,19. Based on the resulots obtained regression coefficient value of determination (R2) of 76,7 %. This suggests that the contribution of the effect variable percentage of free (TSS and TDS) against the dependent variable (abundance) of 76,7% or variations of the independent variables used in the model are able to explain 76,7 % of variation in dependent variable. Keywords : Abundance of benthic mollucsc, TSS and TDS 1Student of Aquatic Resource Management Study Programme 2 Lecture of Aquatic Aquatic Resource Management Study Programme sekitar Perairan Sungai Kawal Kelurahan Kawal Kabupaten Bintan. PENDAHULUAN Pesisir adalah daerah pertemuan antara METODE darat dan laut (Soegiarto, dalam Kordi, 2007). Penelitian ini dilaksanakan mulai bulan Sungai Kawal merupakan salah satu daerah Juni sampai Agustus 2012 di lokasi Sungai pesisir yang terdapat di Kabupaten Bintan. Kawal Kabupaten Bintan Provinsi Kepulauan Sungai Kawal terdiri kawasan pesisir sungai Riau. Analisis secara ex situ di lakukan di yang dijadikan oleh masyarakat sebagai Laboratorium Ilmu Kelautan dan Perikanan tempat pemukiman, daerah muara sungai yang Universitas Maritim Raja Ali Haji. dijadikan alur pelayaran kapal nelayan, dimana sungai Kawal ini menjadi tempat Alat dan Bahan aktifitas manusia yang berpengaruh terhadap Alat dan bahan yang digunakan dapat ekosistem di sekitarnya dan daerah hulu sungai dilihat pada Tabel 1. yang jauh dari aktivitas manusia. Peran Sungai Kawal ini sangat penting selain di manfaatkan Tabel 1. Alat dan Bahan yang Digunakan oleh manusia juga dimanfaatkan oleh No Parameter Satua Bahan dan Alat organisme-organisme yang hidup di perairan Lingkungan n sungai baik di permukaan maupun di dasarnya. 1 Moluska Ind/m Eckman Grap, Moluska berperan penting dalam suatu Bentik saringan benthos ekosistem yaitu sebagai bagian dari rantai 2 TDS Mg/l Kertas filter, oven, makanan dan sebagai indikator pencemaran. 3 TSS Mg/l cawan petri, suntik penghisap Perubahan kualitas perairan khususnya 4 Suhu Perairan 0C Thermometer sungai disebabkan oleh buangan dari berbagai 5 Kedalaman M Tali dengan pemberat kegiatan manusia ke lingkungannya, yang 6 Ph Indikator Universal menyebabkan perubahan terhadap kondisi 7 Oksigen Mg/l DO meter fisik, kimia, biologis dan estetis penampakan terlarut (O2) dari luarnya. Menurut EPA (1999) dalam 8 Substrat Saringan bertingkat Hidayat et al. (2004), kekeruhan (TSS dan TDS) secara umum mengganggu biota Prosedur Penelitian dikarenakan akan menghalangi masuknya Sampel moluska bentik di ambil dengan sinar matahari bagi kebutuhan fotosistesis menggunakan eckman grap yang di fitoplankton, menurunkan kesediaan oksigen tenggelamkan ke dasar perairan pada terlarut, memicu sedimentasi penyebab kedalaman 1- 2,5 meter di setiap titik sampling pendangkalan, mengganggu pandangan visual masing-masing stasiun yang di tentukan. hewan, mempengaruhi perilaku dan sistem Sampel moluska yang diperoleh lalu makan (termasuk interaksi biota) dan dimasukkan ke dalam kantong plastik dan pernafasan hewan. Melihat tingginya aktivitas diberi label kemudian di bawa ke Sungai Kawal yang salah satunya di duga Laboratorium Ilmu Kelautan dan Perikanan menyebabkan kekeruhan (TSS dan TDS) yang untuk diamati dan diidentifikasi mulai dari akan berdampak buruk terhadap kehidupan Kelas, Ordo, Famili, dan Genus nya menurut biota mollusca bentik. Adapun tujuan dari buku identifikasi Darma (1988). Sedangkan penelitian ini adalah : pengukuran kualitas air diantaranya: Suhu, 1. Mengetahui kelimpahan dan keragaman Derajat Keasaman (pH), Salinitas, Oksigen jenis mollusca bentik yang dominan di Terlarut, TSS dan TDS. daerah Perairan Sungai Kawal Kelurahan Kawal Padat Tersuspensi (TSS) 2. Mengetahui hubungan antara kelimpahan Zat padat tersuspensimerupakan residu mollusca bentik dominan dengan TSS dan yang diperoleh apabila zat padat dalam TDS. sampel dipisahkan dengan menggunakan filter Sedangkan manfaat penelitian untuk kertas atau filter fiber glass (serabut kaca) dan memberikan gambaran potensi gangguan kemudian zat padat yang tertahan pada filter kekeruhan (TSS dan TDS) terhadap kehidupan 0 dikeringkan pada suhu ± 105 C. dengan mollusca bentik sebagai akibat aktivitas perhitungan: manusia yang semakin nyata berlanjut di 2 mg/ℓ Zat Tersuspensi =(a-b) x 1000 Analisis Data c Kelimpahan Individu dimana : a = berat filter dan residu sesudah Kelimpahan individu moluska bentik 0 pemanasan 105 C (mg), dihitung dengan menggunakan rumus b = berat filter kering (sudah Shannon-Wener (Odum, 1993). 0 dipanaskan 105 C) (mg) c = mℓ sampel Y = 10.000 x a b Padat Terlarut (TDS) Larutan yang mengandung zat terlarut Dimana : Y = Jumlah organisme moluska adalah residu yang lolos filter ≈ 10 µm yang bentik (ind/m²) kemudian di uapkan dan di keringkan pada a = Jumlah moluska bentik (ind) suhu 1050 C dengan perhitungan : b = Luas alat pengambilan sampel (cm²) mg/ℓ Zat Padat Terlarut = (a-b) x 1000 c Indeks Keanekaragaman Shanon Wiener (H’) dimana : a = berat cawan dan residu sesudah Keanekaragaman suatu biota air dapat pemanasan 1050C ditentukan dengan menggunakan teori b = berat cawan (kosong) (mg) c = mℓ sampel informasi Shanon Wiener (H’). Adapun indeks tersebut adalah sebagai berikut Substrat (Koesoebiono,1987) : Jumlah sample sedimen yang S S diperlukan sekitar 100 gram. Sampel H = ∑Pi ln Pi atau H = ∑ Pi log2 Pi dikeringkan dan dianalisis dengan i=1 i=1 menggunakan ayakan bertingkat (metode ayakan kering) dengan ukuran mata ayakan Dengan : (meshes) 2,36 mm, 2,00 mm, 1,18 mm, 500 Pi = jumlah individu masing-masing µm(0,5 mm), 250µmb (0,25 mm), 125µm jenis (i=1,2,3,...) (0,125mm), dan 106µm (0,106 mm). Analisis S = jumlah jenis substrat berdasarkan bentuk ukuran butir H = penduga keragaman populasi sedimen menurut skala Wenworth, seperti Kategori penilaian tingkat yang tertera dalam tabel 2. keanekaragaman jenis berdasarkan Indeks Tabel 2. Analisis Ukuran Butiran Shannon-Wiener dalam Soegianto (1994) Substrat Wenworth adalah: No Nama Partikel Ukuran (mm) H’ ≤ 1 = Keanekaragaman Sangat 1 Bongkah (Boulder) >256 Rendah 1 ≤ H’ ≤ 1,59 = Keanekaragaman Rendah 2 Krakal (Coble) 64 – 256 1,6 ≤ H’ ≤ 2 = Keanekaragaman Sedang 3 Batu Kerikil (Peble) 4 – 64 (Stone) H’ > 2 = Keanekaragaman Tinggi 4 Butiran (Granule) 2 - 4 Pasir sangat kasar (V. Course Indeks Keseragaman atau Equitabilitas (E) 5 1 - 2 Sand) Bila nilai indeks keseragaman tinggi, 6 Pasir kasar (Course Sand) 0,5 - 1 menandakan kandungan setiap taxon (jenis) Pasir 7 (Sand) Pasir sedang (Medium Sand) 0,25 – 0,5 tidak mengalami perbedaan. Nilai indeks keseragaman berkisar 0-1. Indeks 8 Pasir Halus (Fine Sand) 0,125 – 0,25 keseragaman ini dihitung berdasarkan rumus : Pasir sangat halus (V. fine 9 0,0625 – 0,125 sand) E = H = H’ 10 Lumpur kasar (Coarse Silt) 0,03125 – 0,0625 Hmax log2 (s) Lumpur 11 Lumpur Sedang
Recommended publications
  • Evolution of the Pachychilidae TROSCHEL, 1857 (Chaenogastropoda, Cerithioidea) – from the Tethys to Modern Tropical Rivers 41
    44 44 he A Rei Series A/ Zitteliana An International Journal of Palaeontology and Geobiology Series A /Reihe A Mitteilungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie 44 An International Journal of Palaeontology and Geobiology München 2004 Zitteliana Umschlag 44 1 18.01.2005, 10:04 Uhr Zitteliana An International Journal of Palaeontology and Geobiology Series A/Reihe A Mitteilungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie 44 CONTENTS/INHALT REINHOLD R. LEINFELDER & MICHAEL KRINGS Editorial 3 DIETRICH HERM Herbert HAGN † 5 KAMIL ZÁGORŠEK & ROBERT DARGA Eocene Bryozoa from the Eisenrichterstein beds, Hallthurm, Bavaria 17 THORSTEN KOWALKE Evolution of the Pachychilidae TROSCHEL, 1857 (Chaenogastropoda, Cerithioidea) – from the Tethys to modern tropical rivers 41 HERBERT W. SCHICK The stratigraphical signifi cance of Cymaceras guembeli for the boundary between Platynota Zone and Hypselocyclum Zone, and the correlation of the Swabian and Franconian Alb 51 GÜNTER SCHWEIGERT, RODNEY M. FELDMANN & MATTHIAS WULF Macroacaena franconica n. sp. (Crustaceae: Brachyura: Raninidae) from the Turonian of S Germany 61 JÜRGEN KRIWET & STEFANIE KLUG Late Jurassic selachians (Chondrichthyes, Elasmobranchii) from southern Germany: Re-evaluation on taxonomy and diversity 67 FELIX SCHLAGINTWEIT Calcareous green algae from the Santonian Hochmoos Formation of Gosau (Northern Calcareous Alps, Austria, Lower Gosau Group) 97 MICHAEL KRINGS & HELMUT MAYR Bassonia hakelensis (BASSON) nov. comb., a rare non-calcareous
    [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]
  • (Gastropoda, Cerithiidae) from Western Australia
    Rec. West. Aust. Mus., 1975, 3 '(4) A NEW LARGE SPECIES OF PSEUDOVERTAGUS (GASTROPODA, CERITHIIDAE) FROM WESTERN AUSTRALIA B. R. WILSON* [Received 1 September 1974. Accepted 4 September 1974. Published 31 December 1975.] INTRODUCTION Cerithiids are generally gregarious and abundant within their habitat. It is a surprise therefore to discover a large and hitherto unknown species from the Western Australian coast near Perth. In February 1964 Mrs Gladys Hansen of Perth found a shell near Point Peron, Cockburn Sound, which she brought to me for identification. Provisionally I identified it as Pseudovertagus clava (Gmelin, 1791), but since then I have seen specimens of that species and I am now satisfied that Mrs Hansen's shell is new. I have seen only two other specimens, both shells occupied by hermit crabs taken from lobster pots in the Fremantle area and now in the collection of the late Mr Harry Baker of Fremantle. Although there is so little material and no live-taken specimen, the species is so distinctive that I have no hesitation in describing and naming it as follows. Pseudovertagus peroni sp. novo (Pi. I, figs. 1-4) Holotype WAM 324-73, a shell without operculum collected by Mrs G. Hansen, February, 1964. Type locality: Point Peron, Western Australia, 32° 16'S, 115°42'E. Description of the holotype Large, solid, attenuate with almost straight sides. Protoconch broken off, teleoconch comprising 13 whorls, sutures sharply incised grooves, thin and shallow, with a prominent broad pre-sutural band comprising posterior 1/4 - 1/3 of spire whorls. On badly worn early spire whorls (1 to 6) pre-sutural band flat and smooth, on whorls 7 to 10 pre-sutural band cast into irregular low axial folds becoming broad, low but prominent axial ribs on the pre­ sutural band of 3 remaining whorls.
    [Show full text]
  • Caenogastropoda
    13 Caenogastropoda Winston F. Ponder, Donald J. Colgan, John M. Healy, Alexander Nützel, Luiz R. L. Simone, and Ellen E. Strong Caenogastropods comprise about 60% of living Many caenogastropods are well-known gastropod species and include a large number marine snails and include the Littorinidae (peri- of ecologically and commercially important winkles), Cypraeidae (cowries), Cerithiidae (creep- marine families. They have undergone an ers), Calyptraeidae (slipper limpets), Tonnidae extraordinary adaptive radiation, resulting in (tuns), Cassidae (helmet shells), Ranellidae (tri- considerable morphological, ecological, physi- tons), Strombidae (strombs), Naticidae (moon ological, and behavioral diversity. There is a snails), Muricidae (rock shells, oyster drills, etc.), wide array of often convergent shell morpholo- Volutidae (balers, etc.), Mitridae (miters), Buccin- gies (Figure 13.1), with the typically coiled shell idae (whelks), Terebridae (augers), and Conidae being tall-spired to globose or fl attened, with (cones). There are also well-known freshwater some uncoiled or limpet-like and others with families such as the Viviparidae, Thiaridae, and the shells reduced or, rarely, lost. There are Hydrobiidae and a few terrestrial groups, nota- also considerable modifi cations to the head- bly the Cyclophoroidea. foot and mantle through the group (Figure 13.2) Although there are no reliable estimates and major dietary specializations. It is our aim of named species, living caenogastropods are in this chapter to review the phylogeny of this one of the most diverse metazoan clades. Most group, with emphasis on the areas of expertise families are marine, and many (e.g., Strombidae, of the authors. Cypraeidae, Ovulidae, Cerithiopsidae, Triphori- The fi rst records of undisputed caenogastro- dae, Olividae, Mitridae, Costellariidae, Tereb- pods are from the middle and upper Paleozoic, ridae, Turridae, Conidae) have large numbers and there were signifi cant radiations during the of tropical taxa.
    [Show full text]
  • Systematic Revision of Palaeocene Brackish Water Gastropoda from Mons, Belgium, Based on Their Early Ontogenetic Shells
    BULLETIN DE L’INSTITUT ROYAL DES SCIENCES NATURELLES DE BELGIQUE SCIENCES DE LA TERRE. 72: 111-134, 2002 BULLETIN VAN HET KONINKLIJK BELGISCH INSTITUUT VOOR NATUURWETENSCHAPPEN AARDWETENSCHAPPEN, 72: 111-134, 2002 Systematic revision of Palaeocene brackish water Gastropoda from Mons, Belgium, based on their early ontogenetic shells by Thorsten KOWALKE Kowalke, T.. 2002. - Systematic revision of Palaeocene brackish Introduction water Gastropoda from Mons, Belgium, based on their early ontoge­ netic shells. Bulletin de l'Institut royal des Sciences naturelles de Belgique, Sciences de la Terre, 72: 111-134, 4 pis., Bruxelles-Brussel, The Early Mid-Palaeocene sediments of Mons, Southeast March 31, 2002. - ISSN 0374-6291 Belgium, were brought to the attention of geologists, when the mining engineers F.L. Cornet and A. Briart recognised a section within a domestic well on the Gof- fint property in 1865. In 1874, the Geological Society of Abstract France initiated a second pit a few metres to the west on The systematic position of Early Mid-Palaeocene brackish water Gas­ the Coppée estate. These original sinkings were termi­ tropoda from the Dano-Montian of Mons, South-east Belgium, is nated at a depth of about 20 m, when the ground water revised. Representatives of the subclasses Neritimorpha (with the floor was reached. In 1969 another boring was initiated new genus Monsneritina- Neritoidea, Neritidae), Caenogastropoda (with the new genus Monspotamides - Cerithioidea, Potamididae) by the Belgian Geological Survey, located 10 m south of and Heterostropha are characterised with regard to their paleoecology. the Gofflnt pit. The sections - detailed descriptions of the Three different modes of early ontogenetic development are recognised stratigraphy and sketches of the locality were given by and paleoecological inferences are discussed.
    [Show full text]
  • SURVEY of the LITERATURE on RECENT SHELLS from the RED SEA (Second Enlarged and Revised Edition)
    TRITON 24 SEPTEMBER 2011 SUPPLEMENT 1 SURVEY OF THE LITERATURE ON RECENT SHELLS FROM THE RED SEA (second enlarged and revised edition) L.J. van Gemert *) Abstract: About 2,100 references are listed in the survey. Shells are being considered here as shell-bearing mollusks of the Gastropoda, Bivalvia and Scaphopoda. And the region covered is not only the Red Sea, but also the Gulf of Aden, including Somalia, and the Suez Canal, including Lessepsian species. Literature on fossils finds, especially from the Pliocene, Pleistocene and Holocene, is listed too. Introduction My interest in recent shells from the Red Sea dates from about 1996. Since then, I have been, now and then, trying to obtain information on this subject. Recently I decide to stop gathering information in a haphazard way and to do it more properly. This resulted in a survey of approximately 1,420 references (Van Gemert, 2010). Since then, this survey has been enlarged considerably and contains now approximately 2,100 references. They are presented here. Scope In principle every publication in which mollusks are reported to live or have lived in the Red Sea should be listed in the survey. This means that besides primary literature, i.e. articles in which researchers are reporting their finds for the first time, secondary and tertiary literature, i.e. reviews, monographs, books, etc are to be included too. These publications were written not only by a wide range of authors ranging from amateur shell collectors to profesional malacologists but also by people interested in other fields. This implies that not only malacological journals and books should be considered, but also publications from other fields or disciplines, such as environmental pollution, toxicology, parasitology, aquaculture, fisheries, biochemistry, biogeography, geology, sedimentology, ecology, archaeology, Egyptology and palaeontology, in which Red Sea shells are mentioned.
    [Show full text]
  • Mollusca of New Caledonia
    Plate 12 Mollusca of New Caledonia Philippe BOUCHET, Virginie HEROS, Philippe MAESTRATI, Pierre LOZOUET, Rudo von COSEL, Delphine BRABANT Museum National d'Histoire Naturelle, Paris malaco@mnhnJr The first record of a land mollusc (Placostylus fibratus (Martyn, 1784» from New Caledonia can unequivocally be traced to the voyage of Cook that discovered the island in 1774. By contrast, the marine molluscs of New Caledonia ironically remained out of reach to European natural history cab­ inets until well into the 19th century. New Caledonia remained untouched by the circumnavigating expeditions of the 1830-1840s onboard, e.g., the "Astrolabe", the "Zelee" or the "Uranie". Seashells may have been collected in New Caledonia by whalers and other merchants in search of sandalwood or beche-de-mer, and then traded, but by the time they reached European conchologists, all indica­ tion of their geographical origin had faded away. It is impossible to tell whether Indo-West Pacific species originally described from localities such as "Mers du Sud" or "Southern Seas" were original­ ly collected in, e.g., Fiji, Tahiti, Australia or New Caledonia. However, even ifNew Caledonian shells may have arrived on the European market or in cabinets, it must have been in very small amount, as such an emblematic species of the New Caledonia molluscan fauna as Nautilus macromphalus was not named until 1859. In fact, it was not until Xavier Montrouzier set foot in New Caledonia that the island was placed on the map of marine conchology. From there on, three major periods can be rec­ ognized in the history of New Caledonia marine malacology.
    [Show full text]
  • Oup Mollus Eyx001 153..160 ++
    UC Davis UC Davis Previously Published Works Title Shell features associated with the sand-burying habit in gastropods Permalink https://escholarship.org/uc/item/4mg4w2vk Journal Journal of Molluscan Studies, 83(2) ISSN 0260-1230 Author Vermeij, GJ Publication Date 2017-05-01 DOI 10.1093/mollus/eyx001 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Journal of The Malacological Society of London Molluscan Studies Journal of Molluscan Studies (2017) 83: 153–160. doi:10.1093/mollus/eyx001 Advance Access publication date: 14 February 2017 Shell features associated with the sand-burying habit in gastropods Geerat J. Vermeij Department of Earth and Planetary Sciences, University of California, One Shields Avenue, Davis, CA 95616, USA Correspondence: G.J. Vermeij; e-mail: [email protected] (Received 22 July 2016; editorial decision 29 November 2016) ABSTRACT The relationship between shell form and mode of life in gastropods is important to the interpretation of fossils, but has been little explored owing, in part, to the great diversity of gastropod shells. Infaunal gas- tropods that actively bury in sand must conform to the demands of moving efficiently and noiselessly through a dense granular medium, but which shell characters reflect these demands and how infaunal gastropods differ from surface-dwelling (epifaunal) species remain incompletely answered questions. Here, I survey infaunal and epifaunal Indo-West Pacific members of four families (Cerithiidae, Mitridae, Costellariidae and Conidae) and consider more broadly the distribution of shell traits that confer stream- lining and other potential benefits to infaunal species. Sand-burying cerithiids, mitrids and costellariids (but not conids) have on average slenderer shells than their epifaunal counterparts.
    [Show full text]
  • Cerithiidae: Prosobranchia)
    ^? THE NAUTILUS 101(3):101-110, 1987 Page 101 Anatomy and Systematic Position of Fastigiella carinata Reeve (Cerithiidae: Prosobranchia) Richard S. Houbrick Robert Robertson R. Tucker Abbott National Museum of Natural History The Academy of Natural Sciences American Malacologists, Inc. Smithsonian Institution 19th and the Parkway PO Box 2255 Washington. DC 20560, USA Philadelphia, PA 19103, USA Melbourne, FL 32902, USA ABSTRACT broad. Opinions on the relationships of Fastigiella within the superfamily Cerithiacea and related superfamilies Fastigiella carinata is placed in the family Cerithiidae, close (as presently conceived) have also been varied. For ex- to the genus Pseiidooertagus Vignal on the basis of conchologi- cal, radular, and anatomical characters. Fastigiella has a shell ample, Mörch (1877:209), although placing Fastigiella sculptured with three strong spiral cords, an aperture with a near Cerithium {sensu lato), stated that Fastigiella is distinct anterior canal, a pseudumbilicus, missing in juveniles, closest to a Recent "Triphoris" (= Triphora Blainville; and a siphonal fasciole. The operculum is ovate, corneous, and Triphoridae) and to a Pliocene "Cerithium" (assigned paucispiral with an eccentric nucleus, and the radula is tae- by Wenz, 1940, to the Potamididae). More orthodox dis- nioglossate. The animal has an unusual hypobranchial gland cussions and placements of Fastigiella are those of Fisch- comprised of many transverse leaflets, a ridge dividing the er (1884:679), Tryon (1887:115,149), Thiele (1929:214), anterior oviductal groove, and an open pallia! oviduct with the Pérez Farfante (1940:71), Wenz (1943:770), and Sarasúa seminal receptacle in the medial lamina of the posterior ovi- and Espinosa (1977:2). Ford (1944:8) considered Ceri- duct.
    [Show full text]
  • Prosobranch Gastropods of Guam
    Micronesica 35-36:244-270. 2003 Prosobranch gastropods of Guam BARRY D. SMITH Marine Laboratory University of Guam Mangilao, Guam 96923 U.S.A. email: [email protected] Abstract—Based on records from invertebrate collections at the University of Guam, specimens cataloged at other institutions, and the published literature, there are 895 species of prosobranch gastropods from Guam. The vast majority of the species are marine, but terrestrial and aquatic prosobranchs are included. Most the species recorded to date are conspicuous, epibenthic species from shallow reef habitats, but some species have been taken from depths up to 400 m. Microgastropods less than 7 mm in size have been poorly investigated to date. Comparison of prosobranch gastropods from Guam and Enewetak reveal that some 56% of the species occurring at Enewetak are found in Guam. Introduction Molluscs have been collected in Guam since the arrival of the earliest inhabitants (Thompson, 1945). Despite the long history of European contact with the island, scant attention was given to systematic investigation of the fauna until the collections of Quoy and Gaimard (1824–1826; 1830–1834). Hidalgo (1904– 1905) was the first to produce a catalog that included molluscs from Guam, but his emphasis was mostly on the Philippine Islands fauna. This catalog was followed by a series of unpublished lists produced by shell collectors and shell club members during the last several decades. Synoptic collections of molluscs from Guam and Micronesia were started by faculty of the University of Guam in the mid-1960s. These collections are housed in the Richard E. Dickinson Memorial Mollusc Collection at the University of Guam Marine Laboratory.
    [Show full text]
  • Download the Full Paper
    Int. J. Biosci. 2020 International Journal of Biosciences | IJB | ISSN: 2220-6655 (Print), 2222-5234 (Online) http://www.innspub.net Vol. 16, No. 3, p. 157-166, 2020 RESEARCH PAPER OPEN ACCESS Intertidal Microhabitat Preferences of Cerithiidae in Selected Areas of Zamboanga del Norte and Misamis Occidental, Philippines Saliha P. Mamaroba, Carlo Stephen O. Moneva* Department of Biological Sciences, College of Science and Mathematics, Mindanao State University – Iligan Institute of Technology, Iligan City, Philippines Key words: Intertidal microhabitats, Cerithium, Clypeomorus, Pseudovertagus. http://dx.doi.org/10.12692/ijb/16.3.157-166 Article published on March 18, 2020 Abstract Various studies have been concerned with intertidal zones in determining the ecological interaction that produce the diverse groupings of plants and animals. This study was conducted to ascertain microhabitat preferences of Cerithiid species in intertidal areas of Bucana Sicayab and Aliguay Island in Dapitan City, Zamboanga del Norte and in Punta Sulong, Baliangao, Misamis Occidental. Microhabitats and abundance of Cerithiid snails were surveyed using the belt-transect method. Specimens encountered in different microhabitats were collected through hand-picking or hand-digging the substratum. Eight microhabitat types were observed and classified as bedrocks, macroalgae (brown, green and red), muddy sand, reef flats, seagrass beds and tidepools. A total of 14 species of Cerithiids under three genera (Cerithium, Clypeomorus and Psuedovertagus) were identified. Kruskal Wallis test revealed that there is a significant difference in the abundance of Cerithiid species among microhabitat types (p<0.05). Using Cramer’s contingency coefficient test, the microhabitat preference of Cerithiids was determined. Cerithium columna had high preference on flatreefs and tidepool, while Cerithium coralium on muddy sand and Cerithium nodulosum on red algae.
    [Show full text]
  • Atoll Research Bulletin No. 326
    ATOLL RESEARCH BULLETIN NO. 326 ISSUED BY NATIONAL MUSEUM OF NATURAL HISTORY SMITHSONIAN INSTITUTION WASHINGTON, D.C., U.S.A. October 1989 MARINE INVERTE S: SPECIES COMPOSITION D BIOGEOGW LS, MOLLUSCS, D ECWINODE GUSTAV PAU ABSTRACT The marine invertebrate fauna of the Pitcairn Islands consists of a depauparate assemblage of Indo-West Pacific species; 54 corals, 198 molluscs, and 58 echinoderms are recorded. I discuss the physiography and marine communities of each island and the origin and characteristics of the fauna. There is considerably variation in species composition among islands as well as through time, indicating that these peripheral islands have an unstable, dynamic fauna, The marine fauna of the of particular biogeographic interest because of the group's isolati ation, and unusu ated at the southeastern edge o acific province, east of their nearest neighbor, Temcse the Tuamotu-6 1570 km west of Easter Island. They are the easternmost islands on the Pacific plate and indeed within the Indo-West Pacific province, with the exception of faunistically depauperate and unusual Easter Island and Sala y Gomez. Situated between 24-25OS, the Pitcairns are also more austral than most other tropical Pacific islands. Two of the Pitcairn Islands have a physiography that is uncommon for the Central Pacific: Henderson is an uplifted atoll, whereas Pitcairn is a precipitous Pleistocene volcano evelopment. The remaining islands, Ducie d Beno, are small ept for Pitcairn, the islan in the group are a rare glimpse of Studies on the marine fauna of the Pitcairn Group have been infrequent. Curring made the first collections in the archipelago, visiting Ducie, Menderso Pitcairn in 1827, and Pitcairn again in 1828 (Dance 1980).
    [Show full text]