Contributions to Zoology, 68 (4) 245-260 (2000)
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1 Crustaceans in Cold Seep Ecosystems: Fossil Record, Geographic Distribution, Taxonomic Composition, 2 and Biology 3 4 Adiël A
1 Crustaceans in cold seep ecosystems: fossil record, geographic distribution, taxonomic composition, 2 and biology 3 4 Adiël A. Klompmaker1, Torrey Nyborg2, Jamie Brezina3 & Yusuke Ando4 5 6 1Department of Integrative Biology & Museum of Paleontology, University of California, Berkeley, 1005 7 Valley Life Sciences Building #3140, Berkeley, CA 94720, USA. Email: [email protected] 8 9 2Department of Earth and Biological Sciences, Loma Linda University, Loma Linda, CA 92354, USA. 10 Email: [email protected] 11 12 3South Dakota School of Mines and Technology, Rapid City, SD 57701, USA. Email: 13 [email protected] 14 15 4Mizunami Fossil Museum, 1-47, Yamanouchi, Akeyo-cho, Mizunami, Gifu, 509-6132, Japan. 16 Email: [email protected] 17 18 This preprint has been submitted for publication in the Topics in Geobiology volume “Ancient Methane 19 Seeps and Cognate Communities”. Specimen figures are excluded in this preprint because permissions 20 were only received for the peer-reviewed publication. 21 22 Introduction 23 24 Crustaceans are abundant inhabitants of today’s cold seep environments (Chevaldonné and Olu 1996; 25 Martin and Haney 2005; Karanovic and Brandão 2015), and could play an important role in structuring 26 seep ecosystems. Cold seeps fluids provide an additional source of energy for various sulfide- and 27 hydrocarbon-harvesting bacteria, often in symbiosis with invertebrates, attracting a variety of other 28 organisms including crustaceans (e.g., Levin 2005; Vanreusel et al. 2009; Vrijenhoek 2013). The 29 percentage of crustaceans of all macrofaunal specimens is highly variable locally in modern seeps, from 30 0–>50% (Dando et al. 1991; Levin et al. -
Balanus Glandula Class: Multicrustacea, Hexanauplia, Thecostraca, Cirripedia
Phylum: Arthropoda, Crustacea Balanus glandula Class: Multicrustacea, Hexanauplia, Thecostraca, Cirripedia Order: Thoracica, Sessilia, Balanomorpha Acorn barnacle Family: Balanoidea, Balanidae, Balaninae Description (the plate overlapping plate edges) and radii Size: Up to 3 cm in diameter, but usually (the plate edge marked off from the parietes less than 1.5 cm (Ricketts and Calvin 1971; by a definite change in direction of growth Kozloff 1993). lines) (Fig. 3b) (Newman 2007). The plates Color: Shell usually white, often irregular themselves include the carina, the carinola- and color varies with state of erosion. Cirri teral plates and the compound rostrum (Fig. are black and white (see Plate 11, Kozloff 3). 1993). Opercular Valves: Valves consist of General Morphology: Members of the Cirri- two pairs of movable plates inside the wall, pedia, or barnacles, can be recognized by which close the aperture: the tergum and the their feathery thoracic limbs (called cirri) that scutum (Figs. 3a, 4, 5). are used for feeding. There are six pairs of Scuta: The scuta have pits on cirri in B. glandula (Fig. 1). Sessile barna- either side of a short adductor ridge (Fig. 5), cles are surrounded by a shell that is com- fine growth ridges, and a prominent articular posed of a flat basis attached to the sub- ridge. stratum, a wall formed by several articulated Terga: The terga are the upper, plates (six in Balanus species, Fig. 3) and smaller plate pair and each tergum has a movable opercular valves including terga short spur at its base (Fig. 4), deep crests for and scuta (Newman 2007) (Figs. -
Thoracia, Balanomorpha, Tetraclitidae
Rei'. West. Aust. Mus. 1990, 14(4): 665-668 Occurrence of the barnacle Tesseropora rosea (Krauss) (Thoracica, Balanomorpha, Tetraclitidae) in western Australian waters. Diana S. Jones* Tesseropora rosea was originally described from one specimen collected at Algoa Bay, South Africa (Krauss 1848). Darwin (1854) recorded material from eastern Australia and, after examining the unique South African specimen commented (p. 335) 'There can be no doubt of the identify of the African and Australian specimens. It is a singular circumstance that the same species should occur in these two distant places, and, as far as at present known, not in the intermediate, more tropical coasts'. The species has not been collected either in South Africa, or on the 'intermediate more tropical coasts' since that time. However, as well as eastern Australia, the species is also known from Lord Howe Island and the Kermadec Islands (Endean et al. 1956a, 1956b; Foster 1978; Anderson & Anderson 1985). In eastern Australia T. rosea occurs between lat. 1905 and 380, and has never been recorded from western areas ofthe continent. The species occurs abundantly in exposed coastal areas and on flat rock platforms which are subjected to strong wave action, extending from betweenjust above mean low water neap to mean high water neap tidal levels (Pope 1945; Dakin et al. 1948, 1953; Denley & Underwood 1979; Anderson & Buckle 1983; Anderson & Anderson 1985). In 1986 three live specimens of T. rosea were collected on intertidal granitic rocks at Cottesloe, Western Australia, by Ms L. M. Marsh (WAM crustacean registration number WAM 2347-86). Since 1986 four isolated large individuals of T. -
Macro-To-Nanoscale Investigation of Wall-Plate Joints in the Acorn Barnacle Semibalanus Balanoides
This is a repository copy of Macro-to-nanoscale investigation of wall-plate joints in the acorn barnacle Semibalanus balanoides : correlative imaging, biological form and function, and bioinspiration. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/161302/ Version: Published Version Article: Mitchell, R.L. orcid.org/0000-0002-6328-3998, Coleman, M., Davies, P. et al. (5 more authors) (2019) Macro-to-nanoscale investigation of wall-plate joints in the acorn barnacle Semibalanus balanoides : correlative imaging, biological form and function, and bioinspiration. Journal of The Royal Society Interface, 16 (157). 20190218. ISSN 1742-5689 https://doi.org/10.1098/rsif.2019.0218 Reuse This article is distributed under the terms of the Creative Commons Attribution (CC BY) licence. This licence allows you to distribute, remix, tweak, and build upon the work, even commercially, as long as you credit the authors for the original work. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Macro-to-nanoscale investigation of wall-plate joints in the acorn barnacle royalsocietypublishing.org/journal/rsif Semibalanus balanoides: correlative imaging, biological form and function, Research and bioinspiration Cite this article: Mitchell RL, Coleman M, R. L. Mitchell1, M. Coleman1, P. Davies1, L. North1, E. C. Pope2, Davies P, North L, Pope EC, Pleydell-Pearce C, C. -
Cirripedia: Balanomorpha
Contributions to Zoology, 68 (4) 245-260 (2000) SPB Academic Publishing bv, The Hague Pyrgoma kuri Hoek, 1913: a case study in morphology and systematics of a symbiotic coral barnacle (Cirripedia: Balanomorpha) Arnold Ross & William+A. Newman Scripps Institution of Oceanography, La Jolla, California 92093-0202, U.S.A atrial Keywords: Pyrgomatidae, passageways, chemical mediation, parasitic dinoflagellates “Whoever attempts to make outfrom external characters alone, Systematics 247 without the valves will almost Chemical mediation between barnacle and host 254 disarticulating ... certainly fall into errors 259 many ...” Acknowledgements Charles Darwin, 1854 References 259 Abstract Introduction The of from the systematics pyrgomatids, stemming early 1800’s, During 1899 and 1900 H.M.S. “Siboga” explored has been based the number of traditionally on plates making up the waters of the Netherlands East Indies, or what the wall (six, four or one) and specializations in the opercular Indonesia. is now largely known as The “Siboga”, plates. A recent study ofthe related bryozobiines focused attention some 50 m in length, takes its name from a town on detailed structural modifications ofthe basis, which we now on the west coast of Sumatra. find also applies to some highly derived pyrgomatids and an Although originally archaeobalanine. Reexamination of the Indonesian coral barnacle designed to be a gun-boat it was retrofitted as a Pyrgoma kuri Hoek, 1913 has revealed previously unknown research vessel prior to completion. Under the lead- morphological features, including separable opercular plates, a ership of Max Weber (Pieters & De Visser, 1993), and basis lined with ladder arch-like true tergal spur, a to the shipboard party collected samples at 323 sta- calcareous structures covering “atrial passageways”. -
Fossil Calibrations for the Arthropod Tree of Life
bioRxiv preprint doi: https://doi.org/10.1101/044859; this version posted June 10, 2016. 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 4.0 International license. FOSSIL CALIBRATIONS FOR THE ARTHROPOD TREE OF LIFE AUTHORS Joanna M. Wolfe1*, Allison C. Daley2,3, David A. Legg3, Gregory D. Edgecombe4 1 Department of Earth, Atmospheric & Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA 2 Department of Zoology, University of Oxford, South Parks Road, Oxford OX1 3PS, UK 3 Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PZ, UK 4 Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK *Corresponding author: [email protected] ABSTRACT Fossil age data and molecular sequences are increasingly combined to establish a timescale for the Tree of Life. Arthropods, as the most species-rich and morphologically disparate animal phylum, have received substantial attention, particularly with regard to questions such as the timing of habitat shifts (e.g. terrestrialisation), genome evolution (e.g. gene family duplication and functional evolution), origins of novel characters and behaviours (e.g. wings and flight, venom, silk), biogeography, rate of diversification (e.g. Cambrian explosion, insect coevolution with angiosperms, evolution of crab body plans), and the evolution of arthropod microbiomes. We present herein a series of rigorously vetted calibration fossils for arthropod evolutionary history, taking into account recently published guidelines for best practice in fossil calibration. -
Hydrothermal Vents in the Lau Basin
Bull. Mus. natl. Hist. nat., Paris, 4e sér., 17, 1995 section A, n" 3-4 : 221-243. A new sessile barnade (Cirripedia, Brachylepadomorpha) from the Lau Back-Arc Basin, Tonga; fïrst record of a living représentative since the Miocène by William A. NEWMAN & Toshiyuki YAMAGUCHI Abstract. — An extant représentative of the Brachylepadomorpha, Neobrachylepas relica gen. et sp. nov., has been discovered associated with hydrothermal vents in the Lau Basin. The suborder, comprising the earliest sessile barnacles, appeared in the Jurassic. It underwent a modest diversification before the close of the Cretaceous, when it began to décline concomitant with the origin and diversification of the modem sessile barnacles (Ver- rucomorpha and Balanomorpha) as well as certain shell-crushing predators, and it has been absent from the fossil record since the Miocène. Thus Neobrachylepas is unique among previously known hydrothermal vent barnacles, Neolepas (Scalpellomorpha), Neoverruca (Verrucomorpha) and Eochionelasmus (Balanomorpha), in being the only known living member rather than simply the most primitive living member of its respective suborder. The Lau Basin fauna includes représentatives of ail four of thèse suborders and therefore represents the most diverse cirriped fauna of any known hydrothermal vent community. Keywords. — Mesozoic relies, hydrothermal vents, center of diversity. Un nouveau cirripède sessile (Cirripedia, Brachylepadomorpha) de l'arc postérieur du bassin de Lau, Tonga; première observation d'un représentant vivant de ce groupe non signalé depuis le Miocène Résumé. — Un représentant actuel des Brachylepadomorpha, Neobrachylepas relica, n. gen., n. sp., a été découvert dans les sources hydrothermales du bassin de Lau. Le sous-ordre, comprenant les cirripèdes les plus anciens, est apparu au Jurassique. -
The Recent Species of Megabalanus (Cirripedia: Balanomorpha) with Special Emphasis on Balanus Tintinnabulum (Linnaeus) Sensu Lato
THE RECENT SPECIES OF MEGABALANUS (CIRRIPEDIA: BALANOMORPHA) WITH SPECIAL EMPHASIS ON BALANUS TINTINNABULUM (LINNAEUS) SENSU LATO by DORA P. HENRY and PATSY A. MCLAUGHLIN Henry, Dora P. & Patsy A. McLaughlin: The Recent species of Megabalanus (Cirripedia: Balanomorpha) with special emphasis on Balanus tintinnabulum (Linnaeus) sensu lato. Zool. Verh. Leiden 235, 25-viii-1986: 1-69, figs. 1-14, appendix. — ISSN 0024-1652. Key words: Crustacea; Cirripedia; Balanomorpha; Megabalanus; key, species. Since Darwin's (1854) description of 11 varieties of Megabalanus tintinnabulum (Linnaeus) [as Balanus tintinnabulum], 26 Recent taxa have been assigned to the genus. In this review, two taxa confounded by Darwin are reestablished [i.e., M. crispatus (Schroter) and M. dorbignii (Chenu)]. M. antillensis (Pilsbry) and M. intermedius (Darwin) are placed in synonymy with M. tintin- nabulum sensu stricto. M. galapaganus (Pilsbry) is synonymized with M. peninsularis (Pilsbry) and M. xishaensis Xianqui & Liu is considered a synonym of M. occator. Diagnoses and an il- lustrated key to the species are presented. Lectotypes are designated for M. tintinnabulum, M. crispatus, M. dorbignii, M. coccopoma (Darwin), M. spinosus (Chenu), M. validus (Darwin), and M. ajax (Darwin). Dora P. Henry, School of Oceanography, University of Washington, Seattle, Washington 98195, U.S.A. Patsy A. McLaughlin, Department of Biological Sciences, Florida International University, Miami, Florida 33199, U.S.A. TABLE OF CONTENTS Introduction 3 Historical Account 5 Taxonomic Account 9 Megabalaninae 9 Megabalanus 9 Key to the recent species of Megabalanus 10 M. tintinnabulum (Linnaeus) 17 M. azoricus (Pilsbry) 21 M. californicus (Pilsbry) 22 M. clippertonensis (Zullo) 23 M. coccopoma (Darwin) 25 M. -
Balanidae, Balanomorpha, Cirripedia) Research Cite This Article: Checa AG, Salas C, Rodríguez- Antonio G
Articulation and growth of skeletal elements in royalsocietypublishing.org/journal/rsos balanid barnacles (Balanidae, Balanomorpha, Cirripedia) Research Cite this article: Checa AG, Salas C, Rodríguez- Antonio G. Checa1,2, Carmen Salas3, Alejandro Navarro AB, Grenier C, Lagos NA. 2019 4 1 Articulation and growth of skeletal elements in B. Rodríguez-Navarro , Christian Grenier balanid barnacles (Balanidae, Balanomorpha, and Nelson A. Lagos5 Cirripedia). R. Soc. open sci. 6: 190458. http://dx.doi.org/10.1098/rsos.190458 1Departamento de Estratigrafía y Paleontología, Universidad de Granada, 18071 Granada, Spain 2Instituto Andaluz de Ciencias de la Tierra, CSIC-Universidad de Granada, 18100 Armilla, Spain 3Departamento de Biología Animal, Facultad de Ciencias, Universidad de Málaga, Received: 12 March 2019 29071 Málaga, Spain Accepted: 8 August 2019 4Departamento de Mineralogía y Petrología, Universidad de Granada, 18071 Granada, Spain 5Centro de Investigación e Innovación para el Cambio Climático, Universidad Santo Tomás, Santiago, Chile AGC, 0000-0001-7873-7545 Subject Category: Biology (whole organism) The morphology and ultrastructure of the shells of two balanid species have been examined, paying special attention to the three types of boundaries between plates: (i) radii-parietes, (ii) Subject Areas: alae-sheaths, and (iii) parietes-basal plate. At the carinal biophysics/biomaterials surfaces of the radii and at the rostral surfaces of the alae, there are series of crenulations with dendritic edges. The crenulations Keywords: of the radius margins interlock with less prominent features biomineralization, barnacle, plate, growth, of the opposing paries margins, whereas the surfaces of the structure, morphology longitudinal abutments opposing the ala margins are particularly smooth. The primary septa of the parietes also develop dendritic edges, which abut the internal surfaces of the primary tubes of the base plates. -
Arthropoda, Cirripedia: the Barnacles Andrew J
Arthropoda, Cirripedia: The Barnacles Andrew J. Arnsberg The Cirripedia are the familiar stalked and acorn barnacles found on hard surfaces in the marine environment. Adults of these specialized crustaceans are sessile. They are usually found in dense aggregations among conspecifics and other fouling organisms. For the most part, sexually mature Cirripedia are hermaphroditic. Cross-fertilization is the dominant method of reproduction. Embryos are held in ovisacs within the mantle cavity (Strathmann, 1987).Breeding season varies with species as well as with local conditions (e.g., water temperature or food availability). The completion of embryonic development culminates in the hatching of hundreds to tens of thousands of nauplii. There are approximately 29 species of intertidal and shallow subtidal barnacles found in the Pacific Northwest, of which 12 have descriptions of the larval stages (Table 1). Most of the species without larval descriptions (11 species) are parasitic barnacles, order Rhizocephala; a brief general review of this group is provided at the end of the chapter. Development and Morphology The pelagic phase of the barnacle life cycle consists of two larval forms. The first form, the nauplius, undergoes a series of molts producing four to six planktotrophic or lecithotrophic naupliar stages (Strathmann, 1987). Each naupliar stage is successively larger in size and its appendages more setose than the previous. The final nauplius stage molts into the non-feeding cyprid a-frontal filament LI - \ horn Fig. I .Ventral view of a stageV nauplius larva. posterior shield spine ! (From Miller and - furcal ramus Roughgarden, 1994, Fig. -dorsal thoracic spine 1) 155 156 Identification Guide to Larval Marine Invertebrates of the Pacific Northwest I Table 1. -
A Synopsis of the Literature on the Turtle Barnacles (Cirripedia: Balanomorpha: Coronuloidea) 1758-2007
EPIBIONT RESEARCH COOPERATIVE SPECIAL PUBLICATION NO. 1 (ERC-SP1) A SYNOPSIS OF THE LITERATURE ON THE TURTLE BARNACLES (CIRRIPEDIA: BALANOMORPHA: CORONULOIDEA) 1758-2007 COMPILED BY: THE EPIBIONT RESEARCH COOPERATIVE ©2007 CURRENT MEMBERS OF THE EPIBIONT RESEARCH COOPERATIVE ARNOLD ROSS (founder)† GEORGE H. BALAZS Scripps Institution of Oceanography NOAA, NMFS Marine Biology Research Division Pacific Islands Fisheries Science Center LaJolla, California 92093-0202 USA 2570 Dole Street †deceased Honolulu, Hawaii 96822 USA [email protected] MICHAEL G. FRICK Assistant Director/Research Coordinator THEODORA PINOU Caretta Research Project Assistant Professor 9 Sandy Creek Court Secondary Science Education Savannah, Georgia 31406 USA Coordinator [email protected] Department of Biological & 912 308-8072 Environmental Sciences Western Connecticut State University JOHN D. ZARDUS 181 White Street Assistant Professor Danbury, Connecticut 06810 USA The Citadel [email protected] Department of Biology 203 837-8793 171 Moultrie Street Charleston, South Carolina 29407 USA ERIC A. LAZO-WASEM [email protected] Division of Invertebrate Zoology 843 953-7511 Peabody Museum of Natural History Yale University JOSEPH B. PFALLER P.O. Box 208118 Florida State University New Haven, Connecticut 06520 USA Department of Biological Sciences [email protected] Conradi Building Tallahassee, Florida 32306 USA CHRIS LENER [email protected] Lower School Science Specialist 850 644-6214 Wooster School 91 Miry Brook Road LUCIANA ALONSO Danbury, Connecticut 06810 USA Universidad de Buenos Aires/Karumbé [email protected] H. Quintana 3502 203 830-3996 Olivos, Buenos Aires 1636 Argentina [email protected] KRISTINA L. WILLIAMS 0054-11-4790-1113 Director Caretta Research Project P.O. -
Phylogeny of Coral-Inhabiting Barnacles (Cirripedia; Thoracica; Pyrgomatidae) Based on 12S, 16S and 18S Rdna Analysis
Molecular Phylogenetics and Evolution 44 (2007) 1333–1341 www.elsevier.com/locate/ympev Phylogeny of coral-inhabiting barnacles (Cirripedia; Thoracica; Pyrgomatidae) based on 12S, 16S and 18S rDNA analysis N. Simon-Blecher a, D. Huchon b, Y. Achituv a,* a The Mina and Everard Goodman Faculty of Life Sciences, Bar-Ilan University, Ramat Gan 52900, Israel b Department of Zoology, The George S. Wise Faculty of Life Sciences, Tel Aviv University, Tel Aviv 69978, Israel Received 2 November 2006; revised 8 March 2007; accepted 29 March 2007 Available online 6 May 2007 Abstract The traditional phylogeny of the coral-inhabiting barnacles, the Pyrgomatidae, is based on morphological characteristics, mainly of the hard parts. It has been difficult to establish the phylogenetic relationships among Pyrgomatidae because of the apparent convergence of morphological characteristics, and due to the use of non-cladistic systematics, which emphasize ancestor-descendant relationships rather than sister-clade relationships. We used partial sequences of two mithochondrial genes, 12S rDNA and 16S rDNA, and a nuclear gene, 18S rDNA, to infer the molecular phylogeny of the pyrgomatids. Our phylogenetic results allowed us to reject previous classifica- tions of Pyrgomatidae based on morphological characteristics. Our results also suggested the possibility of paraphyly of the Pyrgomat- idae. The hydrocoral barnacle Wanella is not found on the same clade as the other pyrgomatids, but rather, with the free-living balanids. The basal position of Megatrema and Ceratoconcha is supported. The archeaobalanid Armatobalanus is grouped with Cantellius at the base of the Indo-Pacific pyrgomatines. Fusion of the shell plate and modification of the opercular valves are homoplasious features that occurred more than three times on different clades.