Redalyc.Quitones (Mollusca: Polyplacophora) Del Mar Caribe
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Enrico SCHWABE Zoologische Staatssammlung Muenchen
. , E. SCHWABE NOVAPEX 6 (4): 89-105, 10 décembre 2005 A catalogue of Récent and fossil chitons (MoUusca: Polyplacophora) Addenda Enrico SCHWABE Zoologische Staatssammlung Muenchen, Muenchhausenstrasse 2 1 D-81247 Muenchen, Germany [email protected] KEYWORDS. MoUusca, Polyplacophora, taxon list, bibliography ABSTRACT. This paper lists species-group names of Récent and fossil Polyplacophora (MoUusca) that were published after 1998 (for the Récent species) and 1987 (for the fossil species). A total of 171 species were since then introduced, of which 123 are attributed to valid fossil taxa and 48 to valid Récent taxa. The authorship and complète références are provided for each species-group name. INTRODUCTION Considerazioni suUa famiglia Leptochitonidae Dali, 1889 (MoUusca: Polyplacophora). III. Le species Taxonomic work is impossible without an overview of terziarie e quatemarie Europee, con note sistematiche the scientific names existing in the particular taxon e filogenetiche. - Atti délia prima Giornata di Studi group. Catalogues generally are a great tool to obtain Malacologici Centra lîaliano di Studi Malacologici such overviews, as they often summarize information (1989): 19-140 (: 79; pi. 26). otherwise hard to gather and master. Type locality: Pezzo, near Villa S. Giovanni (Reggio Of the nearly 2600 taxa introduced on species level Calabria prov.); in material of upper Pleistocene, but within the Polyplacophora, 368 fossils and 914 Récent presumably originated from adjacent deposits of lower species are considered as valid (closing date: Pleistocene of bathyal faciès [Pezzo, presso Villa S. 31/10/2005). Giovanni (RC); in materiale del Pleistocene superiore, In the past, excellent catalogues of species-group ma presumibilmente originato da contigui depositi del names in Polyplacophora were compiled by Kaas & Pleistocene inferiore di faciès batiale]. -
JEFFERSONIANA Contributions from the Virginia Museum of Natural History
JEFFERSONIANA Contributions from the Virginia Museum of Natural History Number 19 10 January 2009 Unusual Cambrian Thrombolites from the Boxley Blue Ridge Quarry, Bedford County, Virginia Alton C. Dooley, Jr. ISSN 1061-1878 Virginia Museum of Natural History Jeffersoniana, Number 19, pp. 1-14 Scientific Publications Series Virginia Museum of Natural History The Virginia Museum of Natural History produces five scientific Unusual Cambrian Thrombolites from the Boxley Blue publication series, with each issue published as suitable material becomes Ridge Quarry, Bedford County, Virginia available and each numbered consecutively within its series. Topics consist of original research conducted by museum staff or affiliated ALTON C. DOOLEY , JR. investigators based on the museum’s collections or on subjects relevant to Virginia Museum of Natural History the museum’s areas of interest. All are distributed to other museums and 21 Starling Avenue libraries through our exchange program and are available for purchase by Martinsville, Virginia 24112, USA individual consumers. [email protected] Memoirs are typically larger productions: individual monographs on ABSTRACT a single subject such as a regional survey or comprehensive treatment of an entire group. The standardized format is an 8.5 x 11 inch page with two Three unusual thrombolites were collected in June 2008 from the Late columns. Cambrian Conococheague Formation at the Boxley Materials Blue Ridge Quarry in Bedford County, Virginia. These specimens are isolated low domes Jeffersoniana is an outlet for relatively short studies treating a single with a thrombolitic core and a pustulate, stromatolitic outer layer. The two subject, allowing for expeditious publication. The standardized format is largest domes have a distinctive thickened rim around their margins. -
(Polyplacophora: Leptochitonidae) and Its Phylogenetic Affinities
Journal of Systematic Palaeontology 5 (2): 123–132 Issued 25 May 2007 doi:10.1017/S1477201906001982 Printed in the United Kingdom C The Natural History Museum First record of a chiton from the Palaeocene of Denmark (Polyplacophora: Leptochitonidae) and its phylogenetic affinities Julia D. Sigwart National Museum of Ireland, Natural History Division, Merrion Street, Dublin 2, Ireland & School of Biology and Biochemistry, Queens University Belfast, BT7 1NN, UK Søren Bo Andersen Department of Earth Sciences, Aarhus University, DK – 8000 Aarhus C, Denmark Kai Ingemann Schnetler Fuglebakken 14, Stevnstrup, DK – 8870 Lang˚a, Denmark SYNOPSIS A new species of fossil polyplacophoran from the Danian (Lower Palaeocene) of Denmark is described from over 450 individual disarticulated plates. The polyplacophorans originate from the ‘nose-chalk’ in the classical Danish locality of Fakse Quarry, an unconsolidated coral limestone in whicharagoniticmolluscshellsarepreserved throughtransformation intocalcite.In platearchitecture and sculpture, the new Danish material is similar to Recent Leptochiton spp., but differs in its underdeveloped apophyses and high dorsal elevation (height/width ca. 0.54). Cladistic analysis of 55 original shell characters coded for more than 100 Recent and fossil species in the order Lepidopleurida shows very high resolution of interspecific relationships, but does not consistently recover traditional genera or subgenera. Inter-relationships within the suborder Lepidopleurina are of particular interest as it is often considered the most ‘basal’ neoloricate lineage. In a local context, the presence of chitons in the faunal assemblage of Fakse contributes evidence of shallow depositional depth for at least some elements of this Palaeocene seabed, a well-studied formation of azooxanthellic coral limestones. -
Shell Microstructures in Early Cambrian Molluscs
Shell microstructures in Early Cambrian molluscs ARTEM KOUCHINSKY Kouchinsky, A. 2000. Shell microstructures in Early Cambrian molluscs. - Acta Palaeontologica Polonica 45,2, 119-150. The affinities of a considerable part of the earliest skeletal fossils are problematical, but investigation of their microstructures may be useful for understanding biomineralization mechanisms in early metazoans and helpful for their taxonomy. The skeletons of Early Cambrian mollusc-like organisms increased by marginal secretion of new growth lamel- lae or sclerites, the recognized basal elements of which were fibers of apparently aragon- ite. The juvenile part of some composite shells consisted of needle-like sclerites; the adult part was built of hollow leaf-like sclerites. A layer of mineralized prism-like units (low aragonitic prisms or flattened spherulites) surrounded by an organic matrix possibly existed in most of the shells with continuous walls. The distribution of initial points of the prism-like units on a periostracurn-like sheet and their growth rate were mostly regular. The units may be replicated on the surface of internal molds as shallow concave poly- gons, which may contain a more or less well-expressed tubercle in their center. Tubercles are often not enclosed in concave polygons and may co-occur with other types of tex- tures. Convex polygons seem to have resulted from decalcification of prism-like units. They do not co-occur with tubercles. The latter are interpreted as casts of pore channels in the wall possibly playing a role in biomineralization or pits serving as attachment sites of groups of mantle cells. Casts of fibers and/or lamellar units may overlap a polygonal tex- ture or occur without it. -
Chitons (Mollusca: Polyplacophora) Known from Benthic Monitoring Programs in the Southern California Bight
ISSN 0738-9388 THE FESTIVUS A publication of the San Diego Shell Club Volume XLI Special Issue June 11, 2009 Chitons (Mollusca: Polyplacophora) Known from Benthic Monitoring Programs in the Southern California Bight Timothy D. Stebbins and Douglas J. Eernisse COVER PHOTO Live specimen of Lepidozona sp. C occurring on a piece of metal debris collected off San Diego, southern California at a depth of 90 m. Photo provided courtesy of R. Rowe. Vol. XLI(6): 2009 THE FESTIVUS Page 53 CHITONS (MOLLUSCA: POLYPLACOPHORA) KNOWN FROM BENTHIC MONITORING PROGRAMS IN THE SOUTHERN CALIFORNIA BIGHT TIMOTHY D. STEBBINS 1,* and DOUGLAS J. EERNISSE 2 1 City of San Diego Marine Biology Laboratory, Metropolitan Wastewater Department, San Diego, CA, USA 2 Department of Biological Science, California State University, Fullerton, CA, USA Abstract: About 36 species of chitons possibly occur at depths greater than 30 m along the continental shelf and slope of the Southern California Bight (SCB), although little is known about their distribution or ecology. Nineteen species are reported here based on chitons collected as part of long-term, local benthic monitoring programs or less frequent region-wide surveys of the entire SCB, and these show little overlap with species that occur at depths typically encountered by scuba divers. Most chitons were collected between 30-305 m depths, although records are included for a few from slightly shallower waters. Of the two extant chiton lineages, Lepidopleurida is represented by Leptochitonidae (2 genera, 3 species), while Chitonida is represented by Ischnochitonidae (2 genera, 6-9 species) and Mopaliidae (4 genera, 7 species). -
Liolophura Species Discrimination with Geographical Distribution Patterns and Their Divergence and Expansion History on the Nort
www.nature.com/scientificreports OPEN Liolophura species discrimination with geographical distribution patterns and their divergence and expansion history on the northwestern Pacifc coast Eun Hwa Choi1,2,5, Mi Yeong Yeo1,5, Gyeongmin Kim1,3,5, Bia Park1,2,5, Cho Rong Shin1, Su Youn Baek1,2 & Ui Wook Hwang1,2,3,4* The chiton Liolophura japonica (Lischke 1873) is distributed in intertidal areas of the northwestern Pacifc. Using COI and 16S rRNA, we found three genetic lineages, suggesting separation into three diferent species. Population genetic analyses, the two distinct COI barcoding gaps albeit one barcoding gap in the 16S rRNA, and phylogenetic relationships with a congeneric species supported this fnding. We described L. koreana, sp. nov. over ca. 33°24′ N (JJ), and L. sinensis, sp. nov. around ca. 27°02′–28°00′ N (ZJ). We confrmed that these can be morphologically distinguished by lateral and dorsal black spots on the tegmentum and the shape of spicules on the perinotum. We also discuss species divergence during the Plio-Pleistocene, demographic expansions following the last interglacial age in the Pleistocene, and augmentation of COI haplotype diversity during the Pleistocene. Our study sheds light on the potential for COI in examining marine invertebrate species discrimination and distribution in the northwestern Pacifc. Chitons (Polyplacophora, Neoloricata, and Chitonida) are marine mollusks of the class Polyplacophora that possess a dorsal shell, which is composed of eight separate calcium carbonate plates1. Nearly a thousand extant chiton species are distributed worldwide, and over 430 fossil species have been reported, stretching back ca. 300 million years, from the late Ordovician to the Early Periman age 1,2; some have been dated as early as 500 million years old3,4. -
Cambrian Substrate Revolution
Vol. 10, No. 9 September 2000 INSIDE • Research Grants, p. 12 • Section Meetings Northeastern, p. 16 GSA TODAY Southeastern, p. 18 A Publication of the Geological Society of America • Happy Birthday, NSF, p. 22 The Cambrian Substrate Revolution David J. Bottjer, Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, [email protected] James W. Hagadorn, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, [email protected] Stephen Q. Dornbos, Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, [email protected] ABSTRACT The broad marine ecological settings prevalent during the late Neo- proterozoic–early Phanerozoic (600–500 Ma) interval of early metazoan body plan origination strongly impacted the subsequent evolution and development of benthic metazoans. Recent work demonstrates that late Neoproterozoic seafloor sediment had well-developed microbial mats and poorly developed, vertically oriented bioturbation, thus producing fairly stable, relatively low water content substrates and a sharp water-sediment interface. Later in the Cambrian, seafloors with microbial mats became increasingly scarce in shallow-marine environments, largely due to the evolution of burrowing organisms with an increasing vertically oriented component to their bioturba- tion. The evolutionary and ecological effects of these substrate changes on Figure 1. Looping and meandering trace fossil Taphrhelminthopsis, made by a large Early Cambrian benthic metazoans, referred to as the bioturbator, on a bedding plane from Lower Cambrian Poleta Formation, White-Inyo Mountains, California. Such traces, consisting of a central trough between lateral ridges, occur in sandstones Cambrian substrate revolution, are deposited in shallow-marine environments. -
Mollusca, Polyplacophora) Movement Behaviour, with Comparison Between Habitats Differing in Complexity
The first observations of Ischnochiton (Mollusca, Polyplacophora) movement behaviour, with comparison between habitats differing in complexity Kiran Liversage1 and Kirsten Benkendorff2 1 Estonian Marine Institute, University of Tartu, Tallinn, Estonia 2 Marine Ecology Research Centre, Southern Cross University, Lismore, NSW, Australia ABSTRACT Most species of Ischnochiton are habitat specialists and are almost always found underneath unstable marine hard-substrata such as boulders. The difficulty of experimenting on these chitons without causing disturbance means little is known about their ecology despite their importance as a group that often contributes greatly to coastal species diversity. In the present study we measured among-boulder distributional patterns of Ischnochiton smaragdinus, and used time-lapse photography to quantify movement behaviours within different habitat types (pebble substrata and rock-platform). In intertidal rock-pools in South Australia, I. smaragdinus were significantly overdispersed among boulders, as most boulders had few individuals but a small proportion harboured large populations. I. smaragdinus individuals emerge from underneath boulders during nocturnal low-tides and move amongst the inter-boulder matrix (pebbles or rock-platform). Seventy-two percent of chitons in the pebble matrix did not move from one pebble to another within the periods of observation (55–130 min) but a small proportion moved across as many as five pebbles per hour, indicating a capacity for adults to migrate among disconnected habitat -
Polyplacophora : Mollusca) in Port Phillip
Patullo, B. (2012) List of chitons (Polyplacophora : Mollusca) in Port Phillip. Museum Victoria, Melbourne. This list is based on Museum Victoria collection records and knowledge of local experts. It includes all species in Port Phillip and nearby waters that are known to these sources. Number of species listed: 32. Species (Author) Higher Classification Acanthochitona bednalli (Pilsbry, 1894) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Acanthochitona gatliffi (Ashby, 1919) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Acanthochitona granostriata (Pilsbry, 1894) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Acanthochitona kimberi (Torr, 1912) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Acanthochitona pilsbryi (Sykes, 1896) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Acanthochitona retrojecta (Pilsbry, 1894) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Bassethullia glypta (Sykes, 1896) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Bassethullia matthewsi (Bednall & Pilsbry, 1894) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Callistochiton antiquus (Reeve, 1847) Ischnochitonidae : Neoloricata : Polyplacophora : Mollusca Craspedochiton variabilis (Adams & Angas, 1864) Acanthochitonidae : Neoloricata : Polyplacophora : Mollusca Cryptoplax iredalei Ashby, 1923 Cryptoplacidae : Neoloricata : Polyplacophora : Mollusca Cryptoplax striata (Lamarck, 1819) Cryptoplacidae : Neoloricata : Polyplacophora : Mollusca Ischnochiton australis -
Mollusca: Polyplacophora
Revista de Biología Marina y Oceanografía Vol. 53, N°1: 19-26, abril 2018 http://dx.doi.org/10.4067/S0718-19572018000100019 ARTÍCULO Variaciones estacionales de la comunidad de quitones (Mollusca: Polyplacophora) en una zona intermareal rocosa del sur del Golfo de México Seasonal variations of the chiton community structure (Mollusca: Polyplacophora) in a rocky intertidal shore from the southern Gulf of Mexico Laura Sanvicente-Añorve1*, Rodrigo Rodríguez-Vázquez2, Elia Lemus-Santana2, Miguel Alatorre-Mendieta1 y Martha Reguero1 1Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Circuito Exterior S/N, Ciudad Universitaria, Delegación Coyoacán, 04510 Ciudad de México, México. *Autor para correspondencia: [email protected] 2Facultad de Ciencias, Universidad Nacional Autónoma de México, Circuito Exterior S/N, Ciudad Universitaria, Delegación Coyoacán, 04510 Ciudad de México, México Abstract.- The southern Gulf of Mexico is typically a coastal plain where rocky shores are scattered distributed. The goal of this study was to compare the chiton community structure of the rocky shore of Montepío during the dry and ‘nortes’ (stormy) weather periods, and to gather data on the relative growth of the dominant species. Sampling was carried out along a transect of 100 x 2 m in the intertidal zone and 83 individuals were collected. Six species were identified: Lepidochitona rosea, Chaetopleura apiculata, Ischnochiton kaasi, Lepidochitona pseudoliozonis, Lepidochitona liozonis and Acanthochitona andersoni. Species richness (S= 4) and Shannon diversity (1.36 and 1.29 bits ind-1 in dry and stormy seasons) were very similar between the 2 seasons; however, only 2 species occurred in both periods, suggesting a strong seasonal exchange of species (50%). -
First Findings of the Rare Chiton Acanthochitona Leopoldi (Mollusca
ZOOSYSTEMATICA ROSSICA ISSN 2410-0226 Zoological Institute, Russian Academy of Sciences, St Petersburg ▪ https://www.zin.ru/journals/zsr/ [ onl ine] 0320-9180 Vol. 29(1): 93–100 ▪ Published online 12 June 2020 ▪ DOI 10.31610/zsr/2020.29.1.93 [ print] RESEARCH ARTICLE First findings of the rare chiton Acanthochitona leopoldi (Mollusca: Polyplacophora) in the South China Sea Первые находки редкого хитона Acanthochitona leopoldi (Mollusca: Polyplacophora) в Южно-Китайском море B.I. Sirenko & T. Nguyen Tai Б.И. Сиренко, Т. Нгуен Тай Boris I. Sirenko, Zoological Institute, Russian Academy of Sciences, 1 Universitetskaya Emb., St Petersburg, 199034, Russia. E-mail: [email protected] Tu Nguyen Tai, Joint Russian–Vietnamese Tropical Research and Technological Center, 63 Nguyen Van Huyen Road, Nghia Do, Cau Giay, Hanoi, Vietnam. E-mail: [email protected] Abstract. The rare chiton Acanthochitona leopoldi (Leloup, 1933) is recorded for the first time from the Spratly Islands (Truong Sa), Vietnam. The species is redescribed based on the scanning electron micro- scope examination of the recently collected specimens. Age variability of the shell, radula and perinotum of this species is also given. Резюме. Редкий вид хитонов Acanthochitona leopoldi (Leloup, 1933) впервые зарегистрирован у островов Спратли (Чыонг Ша), Вьетнам. Дано переописание этого вида на основе электронно- микроскопического изучения собранных экземпляров. Представлена также возрастная изменчивость раковины, радулы и перинотума этого вида. Key words: chitons, redescription, age variability, South China Sea, Spratly Islands, Acanthochitonidae, Acanthochitona Ключевые слова: хитоны, переописание, возрастная изменчивость, Южно-Китайское море, острова Спратли, Acanthochitonidae, Acanthochitona Zoobank Article LSID: urn:lsid:zoobank.org:pub:7723201B-6228-41FD-8C8C-F5454A275670 Introduction ogy Centre organised two marine expeditions to the southern part of the South China Sea. -
Molluscan Studies
Journal of The Malacological Society of London Molluscan Studies Journal of Molluscan Studies (2013) 79: 372–377. doi:10.1093/mollus/eyt029 Advance Access publication date: 23 August 2013 RESEARCH NOTE EGG-HULL ULTRASTRUCTURE OF ISCHNOCHITON STRAMINEUS (SOWERBY, 1832), A SOUTH AMERICAN BROODING CHITON (CHITONINA: ISCHNOCHITONIDAE) Marı´a G. Liuzzi1 and Diego G. Zelaya2 1Divisio´n Invertebrados, Museo Argentino de Ciencias Naturales, CONICET, A´ngel Gallardo 470, Buenos Aires (C1405DJR), Argentina; and 2Departamento Biodiversidad, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, CONICET, Argentina Correspondence: M.G. Liuzzi; e-mail: [email protected] Reproductive aspects of the life history of chitons have been rela- Celebron˜a(¼Kidney) Island, Malvinas/Falkland Islands tively little studied in comparison with some morphological (518370S–578450W). Thirty-eight eggs were removed from the characters, such as valve morphology, girdle scales and radulae, pallial groove, dehydrated in an ascending ethanol series (from which have historically been considered of taxonomic value. In 70 to 100%), dried in an EMS 850 critical-point dryer using recent times, however, some authors have pointed out that char- liquid CO2, coated with gold-palladium (40–60%) and photo- acters related to reproduction, such as egg-hull morphology, are graphed with a Phillips XL-30 scanning electron microscope. also valuable for taxonomic purposes (Eernisse, 1988; Hodgson One juvenile was dehydrated and photographed in the same et al., 1988; Sirenko, 1993; Pashchenko & Drozdov, 1998; Okusu way as the eggs, but treated with hexamethyldisilazane and air et al., 2003; Buckland-Nicks, 2006, 2008; Sirenko, 2006a; dried instead of critical-point dried.