Intersex in the Clam Scrobicularia Plana
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Response to Oxygen Deficiency (Depletion): Bivalve Assemblages As an Indicator of Ecosystem Instability in the Northern Adriatic Sea
View metadata, citation and similar papers at core.ac.uk brought to you by CORE Response to oxygen deficiency (depletion): Bivalve assemblages as an indicator of ecosystem instability in the northern Adriatic Sea Vedrana NERLOVIĆ1, Alper DOĞAN2 & Mirjana HRS-BRENKO1 1Ruđer Bošković Institute, Centre for Marine Research, Giordano Paliaga 5, HR-52210 Rovinj, Croatia e-mail: [email protected] 2 Department of Hydrobiology, Faculty of Fisheries, Ege University, 35100 Bornova, Izmir, Turkey e-mail: [email protected] Abstract: Benthic communities represent a powerful tool for the detection of natural and anthropogenic disturbances, as well as for the assessment of marine ecosystem stability. This paper shows that Bivalve assemblages could serve as excellent indicators of disturbance and ecosystem instability. The goal of this study was to compare two sets of data in order to determine the differences between two different periods belonging to Bivalve assemblage in the muddy detritic bottom of the northern Adriatic Sea in the post-anoxic period during December 1989, 1990, 1991 and quite a while later, during 2003, 2004 and 2005. Abundances of some indicator species such as Corbula gibba, Modiolarca subpicta, and Timoclea ovata were detected during the post-anoxic period. Recruitment in the quality of Bivalve assemblages was proved by the ecologic and biotic indexes during 2003, 2004 and 2005, during a period of relatively stable ecological conditions. Fluctuation in Bivalve diversity due to the ecological quality of the marine ecosystem in the eastern part of the northern Adriatic Sea is also discussed. Key words: hypoxia; Bivalve assemblages; indicator species; soft bottoms; northern Adriatic Sea Introduction Recent reviews and summaries have provided good introductions on how hypoxia and anoxia came to be such a large and serious problem in the aquatic ecosystem (Gray et al. -
Reconnaître Les Principaux Bivalves Fouisseurs Ou Foreurs Au Moyen De Leurs Siphons
Reconnaître les principaux bivalves fouisseurs ou foreurs au moyen de leurs siphons. 56 espèces Clé de détermination des 20 taxons les plus gros Yves MÜLLER Yves Müller Mai 2016 Reconnaître les principaux bivalves fouisseurs ou foreurs au moyen de leurs siphons. Dans la quasi-totalité des ouvrages traitant des mollusques lamellibranches (ou mollusques bivalves), ce sont les coquilles qui sont décrites (la conchyologie) avec principalement la description des charnières pour la classification. Pour les parties molles (la malacologie) ce sont les branchies qui sont utilisées. Ce qui n’est pas très accessible au plongeur même photographe ! Selon Martoja (1995) 75 % des espèces de bivalves vivent dans les fonds meubles. Certaines espèces trahissent leur présence par leurs siphons qui affleurent à la surface du sédiment, mais il est difficile, au cours d’une plongée, d’identifier les bivalves enfouis dans le sédiment. D’autres espèces de bivalves vivent dans des substrats durs (bois, roche). Ils forent alors une loge dans ce substrat et en général seuls les siphons sont visibles. Le même problème se pose, à quelle espèce appartiennent les siphons ? Selon Bouchet et al. (1978 :92): « Les siphons constituent un moyen de détermination des bivalves aussi fiable que la coquille et la charnière ». Des auteurs anciens comme Deshayes (1844-1848), Forbes et Hanley (1850-1853), Jeffreys (1863, 1865) et Meyer & Möbius (1872) et quelques autres plus récents comme Owen (1953 ; 1959), Purchon (1955a, b), Holme (1959) et Amouroux (1980) ont décrit les siphons de plusieurs espèces. La plupart des espèces de bivalves mesurent entre un et plusieurs centimètres mais les siphons sont pour la plupart courts ou très fins et rétractiles au moindre danger, donc difficilement observables en plongée. -
Relevance of Aquatic Environments for Hominins: a Case Study from Trinil (Java, Indonesia)
Journal of Human Evolution 57 (2009) 656–671 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Relevance of aquatic environments for hominins: a case study from Trinil (Java, Indonesia) J.C.A. Joordens a,*, F.P. Wesselingh b, J. de Vos b, H.B. Vonhof a, D. Kroon c a Institute of Earth Sciences, VU University Amsterdam, De Boelelaan 1056, 1051 HV Amsterdam, The Netherlands b Naturalis National Museum of Natural History , P.O. Box 9517, 2300 RA Leiden, The Netherlands c School of Geosciences, The University of Edinburgh, West Mains Road, Edinburgh EH9 3JW, UK article info abstract Article history: Knowledge about dietary niche is key to understanding hominin evolution, since diet influences body Received 31 December 2008 proportions, brain size, cognition, and habitat preference. In this study we provide ecological context for Accepted 9 April 2009 the current debate on modernity (or not) of aquatic resource exploitation by hominins. We use the Homo erectus site of Trinil as a case study to investigate how research questions on possible dietary relevance of Keywords: aquatic environments can be addressed. Faunal and geochemical analysis of aquatic fossils from Trinil Hominin evolution Hauptknochenschicht (HK) fauna demonstrate that Trinil at w1.5 Ma contained near-coastal rivers, lakes, Strontium isotopes swamp forests, lagoons, and marshes with minor marine influence, laterally grading into grasslands. Freshwater wetland Marine influence Trinil HK environments yielded at least eleven edible mollusc species and four edible fish species that Stingray could be procured with no or minimal technology. We demonstrate that, from an ecological point of Fish view, the default assumption should be that omnivorous hominins in coastal habitats with catchable Molluscs aquatic fauna could have consumed aquatic resources. -
OREGON ESTUARINE INVERTEBRATES an Illustrated Guide to the Common and Important Invertebrate Animals
OREGON ESTUARINE INVERTEBRATES An Illustrated Guide to the Common and Important Invertebrate Animals By Paul Rudy, Jr. Lynn Hay Rudy Oregon Institute of Marine Biology University of Oregon Charleston, Oregon 97420 Contract No. 79-111 Project Officer Jay F. Watson U.S. Fish and Wildlife Service 500 N.E. Multnomah Street Portland, Oregon 97232 Performed for National Coastal Ecosystems Team Office of Biological Services Fish and Wildlife Service U.S. Department of Interior Washington, D.C. 20240 Table of Contents Introduction CNIDARIA Hydrozoa Aequorea aequorea ................................................................ 6 Obelia longissima .................................................................. 8 Polyorchis penicillatus 10 Tubularia crocea ................................................................. 12 Anthozoa Anthopleura artemisia ................................. 14 Anthopleura elegantissima .................................................. 16 Haliplanella luciae .................................................................. 18 Nematostella vectensis ......................................................... 20 Metridium senile .................................................................... 22 NEMERTEA Amphiporus imparispinosus ................................................ 24 Carinoma mutabilis ................................................................ 26 Cerebratulus californiensis .................................................. 28 Lineus ruber ......................................................................... -
The Earliest Bioturbators As Ecosystem Engineers
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 Engineering the Cambrian explosion: the earliest bioturbators as ecosystem engineers LIAM G. HERRINGSHAW1,2*, RICHARD H. T. CALLOW1,3 & DUNCAN MCILROY1 1Department of Earth Sciences, Memorial University of Newfoundland, Prince Philip Drive, St John’s, NL, A1B 3X5, Canada 2Geology, School of Environmental Sciences, University of Hull, Cottingham Road, Hull HU6 7RX, UK 3Statoil ASA, Stavanger 4035, Norway *Correspondence: [email protected] Abstract: By applying modern biological criteria to trace fossil types and assessing burrow mor- phology, complexity, depth, potential burrow function and the likelihood of bioirrigation, we assign ecosystem engineering impact (EEI) values to the key ichnotaxa in the lowermost Cambrian (Fortunian). Surface traces such as Monomorphichnus have minimal impact on sediment properties and have very low EEI values; quasi-infaunal traces of organisms that were surficial modifiers or biodiffusors, such as Planolites, have moderate EEI values; and deeper infaunal, gallery biodiffu- sive or upward-conveying/downward-conveying traces, such as Teichichnus and Gyrolithes, have the highest EEI values. The key Cambrian ichnotaxon Treptichnus pedum has a moderate to high EEI value, depending on its functional interpretation. Most of the major functional groups of mod- ern bioturbators are found to have evolved during the earliest Cambrian, including burrow types that are highly likely to have been bioirrigated. In fine-grained (or microbially bound) sedimentary environments, trace-makers of bioirrigated burrows would have had a particularly significant impact, generating advective fluid flow within the sediment for the first time, in marked contrast with the otherwise diffusive porewater systems of the Proterozoic. -
Campus Field Trip Guidebook Department of Earth and Atmospheric Sciences University of Houston
Campus Field Trip Guidebook Department of Earth and Atmospheric Sciences University of Houston Art on the UH campus uses rocks! Download the UH ARTour app for Apple and Android Laurentian Pink Granite in sculpture – Benches by Scott Burton at the south entrance of the Gerald D. Hines College of Architecture, sculpted in 1985 Town Mountain Granite in the sculpture – Lotus by Jesus Bautista Moroles in the courtyard of the Graduate School of Social Work, sculpted in 1982 Black Cambrian Granite in the untitled sculpture by Matt Mullican at the plaza of the Science Center Building, sculpted in 1991 1 UH Campus Map showing locations of various stops in your Guide Book Most of the figures and images used in this guide are from GEOL 1330 textbook – Earth by Tarbuck, Lutgens and Tasa, 12th edition, 2017 Figure on the front page is Figure 1.22, see https://goo.gl/dYWRsL 2 STOP 1 Location: first floor lobby S&R 1 (building 550). All three types of rocks are used for various facing stones within the lobby. Sedimentary Rock: travertine wall panels on lobby walls. Description: Travertine is a chemical sedimentary rock formed by precipitation of carbonate minerals often influenced by microbial activity. Travertine is composed of aragonite and calcite, although iron and organic impurities can alter its color to yellow, grey, brown and even red. Travertine deposits are located either in hot or cold springs in karst areas. Water dissolves limestone at depth and become saturated with CO2. The CO2 makes the water acidic. As the groundwater resurfaces, a sudden drop in pressure causes the release of CO2 and crystallization of calcium carbonate. -
TREATISE ONLINE Number 48
TREATISE ONLINE Number 48 Part N, Revised, Volume 1, Chapter 31: Illustrated Glossary of the Bivalvia Joseph G. Carter, Peter J. Harries, Nikolaus Malchus, André F. Sartori, Laurie C. Anderson, Rüdiger Bieler, Arthur E. Bogan, Eugene V. Coan, John C. W. Cope, Simon M. Cragg, José R. García-March, Jørgen Hylleberg, Patricia Kelley, Karl Kleemann, Jiří Kříž, Christopher McRoberts, Paula M. Mikkelsen, John Pojeta, Jr., Peter W. Skelton, Ilya Tëmkin, Thomas Yancey, and Alexandra Zieritz 2012 Lawrence, Kansas, USA ISSN 2153-4012 (online) paleo.ku.edu/treatiseonline PART N, REVISED, VOLUME 1, CHAPTER 31: ILLUSTRATED GLOSSARY OF THE BIVALVIA JOSEPH G. CARTER,1 PETER J. HARRIES,2 NIKOLAUS MALCHUS,3 ANDRÉ F. SARTORI,4 LAURIE C. ANDERSON,5 RÜDIGER BIELER,6 ARTHUR E. BOGAN,7 EUGENE V. COAN,8 JOHN C. W. COPE,9 SIMON M. CRAgg,10 JOSÉ R. GARCÍA-MARCH,11 JØRGEN HYLLEBERG,12 PATRICIA KELLEY,13 KARL KLEEMAnn,14 JIřÍ KřÍž,15 CHRISTOPHER MCROBERTS,16 PAULA M. MIKKELSEN,17 JOHN POJETA, JR.,18 PETER W. SKELTON,19 ILYA TËMKIN,20 THOMAS YAncEY,21 and ALEXANDRA ZIERITZ22 [1University of North Carolina, Chapel Hill, USA, [email protected]; 2University of South Florida, Tampa, USA, [email protected], [email protected]; 3Institut Català de Paleontologia (ICP), Catalunya, Spain, [email protected], [email protected]; 4Field Museum of Natural History, Chicago, USA, [email protected]; 5South Dakota School of Mines and Technology, Rapid City, [email protected]; 6Field Museum of Natural History, Chicago, USA, [email protected]; 7North -
Catalog of Recent and Fossil Molluscan Types in the Santa Barbara Museum of Natural History. I. Caudofoveata
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/256082238 Catalog of Recent and Fossil Molluscan Types in the Santa Barbara Museum of Natural History. I. Caudofoveata... Article in Veliger -Berkeley- · January 1990 CITATIONS READS 4 108 3 authors: Paul Valentich-Scott F.G. Hochberg Santa Barbara Museum of Natural History Santa Barbara Museum of Natural History 66 PUBLICATIONS 537 CITATIONS 48 PUBLICATIONS 755 CITATIONS SEE PROFILE SEE PROFILE Barry Roth 176 PUBLICATIONS 1,113 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Marine Bivalve Mollusks of Western South America View project Description of new polygyrid land snails from Oregon and California View project Available from: Paul Valentich-Scott Retrieved on: 21 November 2016 THE VELIGER © CMS, Inc., 1990 The Veliger 33(Suppl. 1):1-27 (January 2, 1990) Catalog of Recent and Fossil Molluscan Types in the Santa Barbara Museum of Natural History. I. Caudofoveata, Polyplacophora, Bivalvia, Scaphopoda, and Cephalopoda by PAUL H. SCOTT, F. G. HOCHBERG, AND BARRY ROTH Department of Invertebrate Zoology, Santa Barbara Museum of Natural History, 2559 Puesta del Sol, Santa Barbara, California 93105, USA Abstract. The non-gastropod molluscan types currently housed in the Department of Invertebrate Zoology at the Santa Barbara Museum are listed. Three hundred seventeen type lots are reported, representing 211 recent species and 9 species originally described as fossils. Each type lot recorded includes a complete citation, type locality, and the current type status of the specimens. An author index and alphabetic index are provided. -
Tayside, Central and Fife Tayside, Central and Fife
Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland. -
Intersex in the Clam Scrobicularia Plana (Da Costa): Widespread Occurrence In
Intersex in the clam Scrobicularia plana (Da Costa): Widespread occurrence in English Channel estuaries and surrounding areas. N D Pope1*, K Childs1, C. Dang2, M S Davey1, S C M O’Hara1, K Langston1, C Minier2, P L Pascoe1, E Shortridge and W J Langston1 1 Marine Biological Association, The Laboratory, Citadel Hill, Plymouth PL1 2PB, UK 2 Laboratory of Ecotoxicology, Universite du Havre, BP540, 76058, Le Havre, France * Corresponding author. Tel.: +44 1752 633272; fax: +44 1752 633102 E-mail address: [email protected] Abstract Estuarine clams Scrobicularia plana were sampled from 108 intertidal locations around the English Channel and adjacent areas. Although S. plana is believed to be a strict gonochorist, 58% of the populations sampled included intersexed individuals (described as male clams exhibiting ovotestis). Over the entire region, on average, 8.6% of male clams exhibited intersex, although proportions of affected males ranged from 0% to 53% depending on location. The severity of intersex was assessed using a simple classification scale, with the majority of individuals showing low levels of impact. Sex ratios were significantly skewed at some sites. There were no significant relationships between the incidence and severity of intersex; or of associations with size or parasitism of individual clams. Intersex in S. plana is a useful tool to assess endocrine disruptive effects in estuaries, although mechanisms of impact and causative agents remain uncertain. Keywords: Intersex, endocrine disruption, Scrobicularia plana, sex ratio, English Channel 1. Introduction Intersex In gonochoristic (dioecious) organisms, intersex is defined as the abnormal condition of being intermediate between male and female sexes, a hermaphrodite. -
Marine Ecology Progress Series 373:25–35 (2008)
The following appendices accompany the article Distributional overlap rather than habitat differentiation characterizes co-occurrence of bivalves in intertidal soft sediment systems Tanya J. Compton1, 2, 3,*, Tineke A. Troost1, Jaap van der Meer1, Casper Kraan1, 2, Pieter J. C. Honkoop1, Danny I. Rogers4, Grant B. Pearson3, Petra de Goeij1, Pierrick Bocher5, Marc S. S. Lavaleye1, Jutta Leyrer1, 2, Mick G. Yates6, Anne Dekinga1, Theunis Piersma1, 2 1Department of Marine Ecology, Royal Netherlands Institute for Sea Research (NIOZ), PO Box 59, 1790 AB Den Burg, Texel, The Netherlands 2Centre for Ecological and Evolutionary Studies, University of Groningen, PO Box 14, 9750 AA Haren, The Netherlands 3Western Australian Department of Environment and Conservation (DEC), WA Wildlife Research Centre, PO Box 51, Wanneroo, Western Australia 6065, Australia 4Institute of Land, Water and Society, Charles Sturt University, PO Box 789, Albury, New South Wales 2640, Australia 5Centre de Recherche sur les Ecosystèmes Littoraux Anthropisés (CRELA), UMR 6217, Pôle science, CNRS-IFREMER-Université de la Rochelle, La Rochelle 17042, France 6Centre for Ecology and Hydrology — Monks Wood, Abbots Ripton, Huntingdon, Cambridgeshire PE28 2LS, UK *Email: [email protected] Marine Ecology Progress Series 373:25–35 (2008) Appendix 1. Maps showing the gridding programme in each system. Benthic sampling points are shown as small dots; sediment sample points are indicated as larger dots. Median grain size values are shown in categories (Wentworth scale). Darker colours are muddy sample points, whereas lighter colours are sandier. The map of the German Wadden Sea has been divided to show the grid sampling at each location (A: 54° 32’ N, 8° 34’ E; B: 53° 59’ N, 8° 51’ E) 2 Appendix 1 (continued) Appendix 1 (continued) 3 4 Appendix 1 (continued) 5 Appendix 2. -
The Evolution of Extreme Longevity in Modern and Fossil Bivalves
Syracuse University SURFACE Dissertations - ALL SURFACE August 2016 The evolution of extreme longevity in modern and fossil bivalves David Kelton Moss Syracuse University Follow this and additional works at: https://surface.syr.edu/etd Part of the Physical Sciences and Mathematics Commons Recommended Citation Moss, David Kelton, "The evolution of extreme longevity in modern and fossil bivalves" (2016). Dissertations - ALL. 662. https://surface.syr.edu/etd/662 This Dissertation is brought to you for free and open access by the SURFACE at SURFACE. It has been accepted for inclusion in Dissertations - ALL by an authorized administrator of SURFACE. For more information, please contact [email protected]. Abstract: The factors involved in promoting long life are extremely intriguing from a human perspective. In part by confronting our own mortality, we have a desire to understand why some organisms live for centuries and others only a matter of days or weeks. What are the factors involved in promoting long life? Not only are questions of lifespan significant from a human perspective, but they are also important from a paleontological one. Most studies of evolution in the fossil record examine changes in the size and the shape of organisms through time. Size and shape are in part a function of life history parameters like lifespan and growth rate, but so far little work has been done on either in the fossil record. The shells of bivavled mollusks may provide an avenue to do just that. Bivalves, much like trees, record their size at each year of life in their shells. In other words, bivalve shells record not only lifespan, but also growth rate.