Genomic, Transcriptomic, and Proteomic Insights Into Intracellular
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Vertical, Lateral and Temporal Structure in Larval Distributions at Hydrothermal Vents
MARINE ECOLOGY PROGRESS SERIES Vol. 293: 1–16, 2005 Published June 2 Mar Ecol Prog Ser Vertical, lateral and temporal structure in larval distributions at hydrothermal vents L. S. Mullineaux1,*, S. W. Mills1, A. K. Sweetman2, A. H. Beaudreau3, 4 5 A. Metaxas , H. L. Hunt 1Woods Hole Oceanographic Institution, MS 34, Woods Hole, Massachusetts 02543, USA 2Max-Planck-Institut für marine Mikrobiologie, Celsiusstraße 1, 28359 Bremen, Germany 3University of Washington, Box 355020, Seattle, Washington 98195, USA 4Dalhousie University, Halifax, Nova Scotia B3H 4J1, Canada 5University of New Brunswick, PO Box 5050, Saint John, New Brunswick E2L 4L5, Canada ABSTRACT: We examined larval abundance patterns near deep-sea hydrothermal vents along the East Pacific Rise to investigate how physical transport processes and larval behavior may interact to influence larval dispersal from, and supply to, vent populations. We characterized vertical and lateral distributions and temporal variation of larvae of vent species using high-volume pumps that recov- ered larvae in good condition (some still alive) and in high numbers (up to 450 individuals sample–1). Moorings supported pumps at heights of 1, 20, and 175 m above the seafloor, and were positioned directly above and at 10s to 100s of meters away from vent communities. Sampling was conducted on 4 cruises between November 1998 and May 2000. Larvae of 22 benthic species, including gastropods, a bivalve, polychaetes, and a crab, were identified unequivocally as vent species, and 15 additional species, or species-groups, comprised larvae of probable vent origin. For most taxa, abundances decreased significantly with increasing height above bottom. When vent sites within the confines of the axial valley were considered, larval abundances were significantly higher on-vent than off, sug- gesting that larvae may be retained within the valley. -
New Archaeogastropod Limpets from Hydrothermal Vents New Family Peltospiridae, New Superfamily Peltospiracea
Zoologica Scripta, Vol. 18, No. 1, pp. 49-66,1989 0300-3256/89 $3.00 +.00 Printed in Great Britain Pergamon Press pic 1989 The Norwegian Academy of Science and Letters New archaeogastropod limpets from hydrothermal vents new family Peltospiridae, new superfamily Peltospiracea JAMES H. MCLEAN Accepted 25 February 1988 McLean, J. H. 1989. New archaeogastropod limpets from hydrothermal vents: new family Peltospiridae, new superfamily Peltospiracea.—Zool. Scr. 18:49-66. Seven new species of limpets from hydrothermal vents are described in five new genera in the new family Peltospiridae (new superfamily Peltospiracea). Limpets in this family are known only from the hydrothermal vent community at two sites, near 21°N and 13°N, on the East Pacific Rise. New genera and species are: Peltospira, type species P. operculata from both sites, and P. delicata from 13°N; Nodopelta, type species N. heminoda from both sites, and N. subnoda from 13°N; Rhynchopelta, type species R. concentrica from both sites; Echinopelta, type species E. fistulosa from 21°N; Hirtopelta, type species H. hirta from 13°N. These limpets are associated with the Pompei worm Alvinella, except for Rhynchopelta, which is associated with the vestimentiferan worm Riftia. James H. McLean, Los Angeles County Museum of Natural History, 900 Exposition Blvd, Los Angeles, CA 90007, U.S.A. Introduction and coiled gastropods were illustrated by Turner & Lutz (1984), Turner et al. (1985) and Lutz et al. (1986), who The hydrothermal vent community of the East Pacific has also discussd the potential for larval dispersal in hydro- now been known for a decade, following the first dis thermal vent mollusks. -
The Heart of a Dragon: 3D Anatomical Reconstruction of the 'Scaly-Foot Gastropod'
The heart of a dragon: 3D anatomical reconstruction of the 'scaly-foot gastropod' (Mollusca: Gastropoda: Neomphalina) reveals its extraordinary circulatory system Chen, C., Copley, J. T., Linse, K., Rogers, A. D., & Sigwart, J. D. (2015). The heart of a dragon: 3D anatomical reconstruction of the 'scaly-foot gastropod' (Mollusca: Gastropoda: Neomphalina) reveals its extraordinary circulatory system. Frontiers in zoology, 12(13), [13]. https://doi.org/10.1186/s12983-015-0105-1 Published in: Frontiers in zoology Document Version: Publisher's PDF, also known as Version of record Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal Publisher rights © 2015 Chen et al. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated. General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. -
University of Southampton Research Repository Eprints Soton
University of Southampton Research Repository ePrints Soton Copyright © and Moral Rights for this thesis are retained by the author and/or other copyright owners. A copy can be downloaded for personal non-commercial research or study, without prior permission or charge. This thesis cannot be reproduced or quoted extensively from without first obtaining permission in writing from the copyright holder/s. The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the copyright holders. When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given e.g. AUTHOR (year of submission) "Full thesis title", University of Southampton, name of the University School or Department, PhD Thesis, pagination http://eprints.soton.ac.uk UNIVERSITY OF SOUTHAMPTON FACULTY OF NATURAL AND ENVIRONMENTAL SCIENCES Ocean and Earth Science Volume 1 of 1 Life-history biology and biogeography of invertebrates in deep-sea chemosynthetic environments by Verity Nye Thesis for the degree of Doctor of Philosophy December 2013 UNIVERSITY OF SOUTHAMPTON ABSTRACT FACULTY OF NATURAL AND ENVIRONMENTAL SCIENCES Ocean and Earth Science Thesis for the degree of Doctor of Philosophy LIFE-HISTORY BIOLOGY AND BIOGEOGRAPHY OF INVERTEBRATES IN DEEP-SEA CHEMOSYNTHETIC ENVIRONMENTS Verity Nye Globally-distributed, insular and ephemeral deep-sea hydrothermal vents with their endemic faunas provide ‘natural laboratories’ for studying the processes that shape global patterns of marine life. The continuing discovery of hydrothermal vents and their faunal assemblages has yielded hundreds of new species and revealed several biogeographic provinces, distinguished by differences in the taxonomic composition of their assemblages. -
Symmetromphalus Hageni Sp. N., a New Neomphalid Gastropod
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Annalen des Naturhistorischen Museums in Wien Jahr/Year: 1992 Band/Volume: 93B Autor(en)/Author(s): Beck Lothar A. Artikel/Article: Symmetromphalus hageni sp.n., a new neomphalid gastropod (Prosobranchia: Neomphalidae) from hydrothermal vents at the Manus Back- Arc Basin (Bismarck Sea, Papua New Guinea). 243-257 ©Naturhistorisches Museum Wien, download unter www.biologiezentrum.at Ann. Naturhist. Mus. Wien 93 B 243-257 Wien, 30. August 1992 Symmetromphalus hageni sp. n., a new neomphalid gastropod (Prosobranchia: Neomphalidae) from hydrothermal vents at the Manus Back-Arc Basin (Bismarck Sea, Papua New Guinea) By LOTHAR A. BECK1) (With 3 Tables, 6 Figures and 6 Plates) Manuscript submitted November 4th, 1991 Zusammenfassung Eine neue Gastropoden-Art von hydrothermalen Quellen (aktiven Sulfid-Schornsteinen) in der Spreizungszone des Manus Beckens (Bismarck See, Papua Neuguinea) wird beschrieben. Die neue Form hat eine fast symmetrische, napfförmige, flache Schale mit unregelmäßigem Rand. Reste des postembryonalen Gewindes sind adult nur noch selten in Form eines sehr kleinen Schlitzes im Inneren der Schale vorhanden. Die Oberfläche des Protoconchs zeigt eine netzförmige Struktur und einen glatten Bereich an der Mündung. Am Weichkörper fallen der verlängerte, augenlose Kopf- und Nackenbereich, der zu einem komplizierten Penis umgeformte linke Kopftentakel der Männchen, die stark vergrößerte Kieme sowie an der Radula nach distal größer werdende Lateralzähne und der fehlende 5. Lateralzahn auf. Die morphologischen Merkmale sprechen für eine mehr oder weniger festsitzende, filtrierende Lebensweise. Der neue Gastropode wird mit den bisher bekannten Neomphaliden-Arten Symmetrom- phalus regularis MCLEAN, 1990, Neomphalus fretterae MCLEAN, 1981, Cyathermia naticoides WAREN & BOUCHET, 1989 und Lacunoides exquisitus WAREN & BOUCHET, 1989 verglichen. -
Molecular Phylogeny of Basal Gastropods (Vetigastropoda) Shows Stochastic Colonization of Chemosynthetic Habitats at Least from the Mid Triassic
Cah. Biol. Mar. (2006) 47 : 343-346 Molecular phylogeny of basal gastropods (Vetigastropoda) shows stochastic colonization of chemosynthetic habitats at least from the mid Triassic Daniel L. GEIGER1 and Christine E. THACKER2 (1) Santa Barbara Museum of Natural History, Invertebrate Zoology, 2559 Puesta del Sol Road, Santa Barbara, CA 93105, USA. phone: (805) 683 4711 x152, fax: (805) 563 0574. E-mail: [email protected] (2) Natural History Museum of Los Angeles County, Ichthyology Section, 900 Exposition Blvd., Los Angeles, CA 90007, USA. E-mail: [email protected] Abstract: A molecular phylogeny of 40 basal gastropod species representing 14 families (including eight species in four families from chemosynthetic habitats) was constructed, based on 3038 characters (Histone 3, COI, 18S). Unambiguous fossils indicated minimum ages of four major lineages. It suggests that chemosynthetic habitats were colonized several times independently and date back to at least the mid Triassic. Keywords: Gastropods l Hydrothermal vent l Molecular phylogeny l Colonization l Triassic Introduction thetic lineages. We can analyze their relationships despite the fact that the membership of Vetigastropoda is not yet Determining the age of taxa living at chemosynthetic fully agreed upon. There is a broad consensus that habitats (hydrothermal vents, cold seeps, whale and wood Haliotidae (abalone), Scissurellidae (little slit shells), falls) is an interesting question. Several groups of Fissurellidae (key hole limpets), Pleurotomariidae (slit organisms are found in more than one chemosynthetic shells) and Trochoidea (top snails, turban snails) belong in habitat type, but are not know from either shallow water or Vetigastropoda. Some of the chemosynthetic groups the general deep sea. -
1 SUPPORTING INFORMATION APPENDIX 1: Data Sources The
SUPPORTING INFORMATION APPENDIX 1: Data Sources The next 64 pages comprise a reference list for all literary sources given as references for trait scores and/or comments in the sFDvent raw (marked with an asterisk (*) if not then included in recommended) and/or recommended datasets (Tables S4.3 and S4.2, respectively). These references are not in alphabetical order, as the database is a ‘living’ record, so new references will be added and a new number assigned. In the recommended dataset (Table S4.2), the references are recorded according to the numbers listed below (and in Table S1.1), to ensure that citations are relatively easy for users to carry through when conducting analyses using subsets of the data, for example. If a score in the recommended dataset is supported by more than one reference, multiple reference identifiers are provided and separated by a semi-colon (;). The references are not provided as numbers / identifiers in the other versions of the dataset, as information is lost during this processing step (e.g., ‘expert opinion’, or 66, replaces comments made by experts in each reference column regarding additional observations, rationale for certainty scores, etc.), which may prove useful for some users. Other versions of the dataset thus maintain raw reference entries for transparency and as potentially useful metadata. We provide a copy of the recommended dataset without the references as numbers (Table S4.2A), in case it is easier for users to cross-reference between the two sheets to seek additional comments for a given data subset of interest. 1. Aguado, M. -
Supplementary Information
Title Ecology and biogeography of megafauna and macrofauna at the first known deep-sea hydrothermal vents on the ultraslow- spreading Southwest Indian Ridge Authors Copley, JT; Marsh, L; Glover, AG; Hühnerbach, V; Nye, VE; Reid, WDK; Sweeting, CJ; Wigham, BD; Wiklund, H Description 0000-0002-9489-074X Date Submitted 2017-05-02 SUPPLEMENTARY INFORMATION Ecology and biogeography of megafauna and macrofauna at the first known deep-sea hydrothermal vents on the ultraslow-spreading Southwest Indian Ridge Copley JT 1,* , Marsh L 1, Glover AG 2, Hühnerbach V 3, Nye VE 1, Reid WDK 4, Sweeting CJ 5, Wigham BD 5, Wiklund H 2 1Ocean & Earth Science, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK 2Life Sciences Department, Natural History Museum, Cromwell Road, London SW7 5BD, UK 3formerly at National Oceanography Centre, European Way, Southampton SO14 3ZH, UK 4School of Biology, Newcastle University, Newcastle Upon Tyne NE1 7RU, UK 5Dove Marine Laboratory, School of Marine Science & Technology, Newcastle University, Cullercoats NE30 4PZ, UK *email [email protected] (corresponding author) SUPPLEMENTARY FIGURE: Images of faunal assemblages observed at Longqi vent field, Southwest Indian Ridge, during the first remotely operated vehicle (ROV) dives in November 2011: (a) active “black smoker” chimneys occupied by Rimicaris kairei ; (b) assemblage of Chrysomallon squamiferum , Hesiolyra cf. bergi , Kiwa n. sp. “SWIR”, Mirocaris fortunata in close proximity to vent fluid source; (c) abundant Chrysomallon squamiferum and Gigantopelta aegis , with Kiwa n. sp. “SWIR”, Bathymodiolus marisindicus , and Mirocaris fortunata on platform of “Tiamat” vent chimney (d) zonation of Chysomallon squamiferum , Gigantopelta aegis , Bathymodiolus marisindicus , and Neolepas sp. -
A New Species of Depressigyra! (Gastropoda: Peltospiridae) from Cold- Seep Carbonates in Eocene and Oligocene Rocks of Western Washington JAMES L
(SioQcWi, si L f b<?v\miM, THE VELIGER © CMS, Inc., 1999 The Veliger 42(2): 112-116 (April 1, 1999) A New Species of Depressigyra! (Gastropoda: Peltospiridae) from Cold- Seep Carbonates in Eocene and Oligocene Rocks of Western Washington JAMES L. GOEDERT 15207 84th Avenue Court NW, Gig Harbor, Washington 98329, USA AND STEVEN R. BENHAM Department of Geosciences, Pacific Lutheran University, Tacoma, Washington 98447, USA Abstract. Continued study of chemosynthetic marine-invertebrate faunas preserved in carbonates formed by the oxidation of methane at ancient cold-seeps reveals, tentatively, the first fossil record of the gastropod family Peltospiridae and the genus Depressigyra. Depressigyral statura sp. nov., was found in three cold-seep carbonates within bathyal marine strata in western Washington: the middle Eocene Humptulips Formation; the early Oligocene part of the Makah Formation; and the late Oligocene part of the Lincoln Creek Formation. INTRODUCTION chthonous (Goedert & Campbell, 1995), but they are methane-derived and contain chemosynthetic taxa. This Taxonomic work on minute (< 5 mm height) gastropods carbonate was precipitated at cold-seeps in a shelf or from modern chemosynthetic communities such as those slope environment, and then broke into blocks up to 2.5 found near hydrothermal vents and cold seeps is resulting m across when it slid or slumped into deeper parts of a in the recognition of many new families, genera, and spe- basin (Goedert & Campbell, 1995). A cold-seep carbon- cies (e.g., McLean, 1989; War6n & Bouchet, 1989, 1993). One recently described gastropod, Depressigyra globulus ate (LACMIP loc. 16504) from the late Oligocene part of Waren & Bouchet, 1989, is the only known living species the Lincoln Creek Formation was first reported by of the genus (War6n & Bouchet, 1993). -
A Phylogeny of Vetigastropoda and Other Archaeogastropods
Invertebrate Biology 129(3): 220–240. r 2010, The Authors Journal compilation r 2010, The American Microscopical Society, Inc. DOI: 10.1111/j.1744-7410.2010.00198.x A phylogeny of Vetigastropoda and other ‘‘archaeogastropods’’: re-organizing old gastropod clades Stephanie W. Aktipisa and Gonzalo Giribet Department of Organismic and Evolutionary Biology and Museum of Comparative Zoology, Harvard University, Cambridge, Massachusetts 02138, USA Abstract. The phylogenetic relationships among the ‘‘archaeogastropod’’ clades Patellogastro- poda, Vetigastropoda, Neritimorpha, and Neomphalina are uncertain; the phylogenetic place- ment of these clades varies across different analyses, and particularly among those using morphological characteristics and those relying on molecular data. This study explores the re- lationships among these groups using a combined analysis with seven molecular loci (18S rRNA, 28S rRNA, histone H3, 16S rRNA, cytochrome c oxidase subunit I [COI], myosin heavy-chain type II, and elongation factor-1a [EF-1a]) sequenced for 31 ingroup taxa and eight outgroup taxa. The deep evolutionary splits among these groups have made resolution of stable relationships difficult, and so EF-1a and myosin are used in an attempt to re-examine these ancient radiation events. Three phylogenetic analyses were performed utilizing all seven genes: a single-step direct optimization analysis using parsimony, and two-step approaches using par- simony and maximum likelihood. A single-step direct optimization parsimony analysis was also performed using only five molecular loci (18S rRNA, 28S rRNA, histone H3, 16S rRNA, and COI) in order to determine the utility of EF-1a and myosin in resolving deep relationships. In the likelihood and POY optimal phylogenetic analyses, Gastropoda, Caenogastropoda, Neritimorpha, Neomphalina, and Patellogastropoda were monophyletic. -
SOB Hereafter) 133 and the Rarer One Being Methane-Oxidising Bacteria (MOB Hereafter) in the Family 134 Methylococcaceae
bioRxiv preprint doi: https://doi.org/10.1101/2020.09.23.308304; this version posted September 23, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Dual symbiosis in the deep-sea hydrothermal vent snail 2 Gigantopelta aegis revealed by its hologenome 3 1 1 2 1 3 1 4 4 Yi Lan , Jin Sun , Chong Chen , Yanan Sun , Yadong Zhou , Yi Yang , Weipeng Zhang , 5 Runsheng Li5, Kun Zhou1, Wai Chuen Wong1, Yick Hang Kwan1, Aifang Cheng1, Salim 6 Bougouffa6,7, Cindy Lee Van Dover8, Jian-Wen Qiu5, Pei-Yuan Qian1* 7 8 1 Department of Ocean Science, Division of Life Science and Hong Kong Branch of the 9 Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), The Hong 10 Kong University of Science and Technology, Hong Kong, China 11 2 X-STAR, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 2-15 12 Natsushima-cho, Yokosuka, Kanagawa Prefecture 237-0061, Japan 13 3 Key Laboratory of Marine Ecosystem Dynamics, Second Institute of Oceanography, Ministry 14 of Natural Resources, Hangzhou, China 15 4 College of Marine Life Science, Ocean University of China, 5 Yushan Road, Qingdao, 16 266003, China 17 5 Department of Biology, Hong Kong Baptist University, Kowloon Tong, Hong Kong 18 6 Computational Bioscience Research Centre, King Abdullah University of Science and 19 Technology, Thuwal, 23955-6900, Saudi Arabia 20 7 King Abdullah University of Science and Technology (KAUST), Core Labs, Thuwal, 23955- 21 6900, Saudi Arabia 22 8 Division of Marine Science and Conservation, Nicholas School of the Environment, Duke 23 University, Beaufort, NC, United States 24 25 * Corresponding author 26 Prof. -
The Limpet Form in Gastropods: Evolution, Distribution, and Implications for the Comparative Study of History
Biological Journal of the Linnean Society, 2016, , – . With 1 figure. Biological Journal of the Linnean Society, 2017, 120 , 22–37. With 1 figures 2 G. J. VERMEIJ A B The limpet form in gastropods: evolution, distribution, and implications for the comparative study of history GEERAT J. VERMEIJ* Department of Earth and Planetary Science, University of California, Davis, Davis, CA,USA C D Received 19 April 2015; revised 30 June 2016; accepted for publication 30 June 2016 The limpet form – a cap-shaped or slipper-shaped univalved shell – convergently evolved in many gastropod lineages, but questions remain about when, how often, and under which circumstances it originated. Except for some predation-resistant limpets in shallow-water marine environments, limpets are not well adapted to intense competition and predation, leading to the prediction that they originated in refugial habitats where exposure to predators and competitors is low. A survey of fossil and living limpets indicates that the limpet form evolved independently in at least 54 lineages, with particularly frequent origins in early-diverging gastropod clades, as well as in Neritimorpha and Heterobranchia. There are at least 14 origins in freshwater and 10 in the deep sea, E F with known times ranging from the Cambrian to the Neogene. Shallow-water limpets are most diverse at mid- latitudes; predation-resistant taxa are rare in cold water and absent in freshwater. These patterns contrast with the mainly Late Cretaceous and Caenozoic warm-water origins of features such as the labral tooth, enveloped shell, varices, and burrowing-enhancing sculpture that confer defensive and competitive benefits on molluscs.