Devonian Carrier Shells (Euomphalidae) from North America and Germany

Total Page:16

File Type:pdf, Size:1020Kb

Devonian Carrier Shells (Euomphalidae) from North America and Germany Devonian Carrier Shells (Euomphalidae) from North America and Germany GEOLOGICAL SURVEY PROFESSIONAL PAPER 824 Devonian Carrier Shells (Euomphalidae) from North America and Germany By ROBERT M. LINSLEY and ELLIS L. YOCHELSON GEOLOGICAL SURVEY PROFESSIONAL PAPER 824 A study of a behavior pattern in which foreign matter is attached to the shell of living and Devonian gastropods UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600142 For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington, D.C. 20402 Price $1.15 (paper cover) Stock Number 2401-02370 CONTENTS Page Page Abstract------------------------------------------------------------------------------------- 1 Systematic paleontology- Continued Introduction and acknowledgments-------------------------------------- 1 Superfamily Euomphalacea- Continued Implantation among the recent fauna _________________________________ _ 2 Family Euomphalidae- Continued . The Xenophoridae ___________________________________________________________________ _ 3 Genus Straparollus Montfort- Continued Habits of Xenophora conchyl·iophora ___________________________ , 3 Subgenus Euomphalus J. Sowerby______ 12 Habits of Xenophora neozelanica_________________________________ _ 4 Stratigraphic distribution______________________________________________________ 14 Functional significance of implanted material in Positioning of shell during implantation_____________________________ 15 the Xenop horidae .. __________________________________________ . ___________ _ 6 Distribution and nature of implanted materiaL________________ 17 Implantation in fossil gastropod shells _______________________________ _ 6 Functional significance of implanted materiaL_________________ 18 Systematic paleontology-------------------------------·------------------------- 7 Presence and absence of implanted materials_____________________ 19 Superfamily Euomphalacea __________________________________________ _ 7 The status of Philoxene___________________________________________________________ 19 Family Euomphalidae ____________________________________________ _ 7 Evolutionary groups of Devonian carrier shells________________ 19 Genus Straparollus Montfort ________________________ _ 7 Conclusions-------------------------------------------------------------------------------- 21 Subgenus Serpulospira Cossman __________ _ 7 Selected references------------------------------------------------------------------- 22 Subgenus Straparollus Montfort __________ _ 8 IndeX------------------------------------------------------------------------------------------- 25 ILLUSTRATIONS [Plates follow index] PLATE 1. Xenophora pallidula Reeve. 2. Xenophora neozelanica Suter. 3. Straparollus (Strapm·ollus) and S. (Serpulospira). 4. Straparollus (Strapat·ollus). 5, 6. Straparollus (Euomphalus) and S. (Straparollus). Page FIGURE 1. Chart showing stratigraphic occurrence of incrusting euomphalids_______________________________________ 15 2. Drawings showing reconstruction of euomphalids as mobile animals__________________________________ 16 3. Drawings showing reconstruction of euomphalids as sessile animals__________________________________ 17 III DEVONIAN CARRIER SHELLS (EUOMPHALIDAE) FROM NORTH AMERICA AND GERMANY By RoBERT M. LINSLEYl and ELLIS L. YocHELSON ABSTRACT p. 241) noted in his comprehensive study of Paleo­ The modern carrier shell Xenophm·a has an elaborate be­ zoic gastropod type species, the holotype of E. laevis havior pattern in which the gastropod attaches foreign mat­ does not have any foreign material attached to its ter to its shell. The process is a long and deliberate one that has selective significance in terms of visual and olfactory shell. Other specimens, which are presumably con­ camouflage. Besides the Xenophoridae, first certainly known specific, to some degree do cement shell material to from the Cretaceous, one turritellid in the Miocene-Pliocene their shells. and one Miocene modulid mastered this peculiar art. Various Examination of topotypic material of the type members of the Euomphalacea from the Ordovician, Silurian, species of Philoxene and of all the available Devo­ and Devonian implanted shell fragments. The systematic part of this report consists primarily of de­ nian species in North America that attach foreign scriptions of the known Middle and Late Devonian carrier material suggests that this peculiar habit may be shells of North America; it includes a discussion of eight indulged in by individuals within a population but species, five of which are new. The new species are Strapa­ is not necessarily followed by all members. Our study rollus (Straparollus) mortoni, S. (Straparollus) cottrelli, S. has also demonstrated that the implantation of for­ (Euomphalus) hoffmani, S. (Euomphalus) winnipegosis, and S. ( ?Euomphalus) incrustatus. Specimens of the type species eign matter on the shell is not restricted to a par­ of Philoxene and two related forms were also studied. ticular shell form but cuts across the lines of three The Devonian carrier shells are of two or more separate currently recognized subgenera. These observations evolutionary stocks having different stratigraphic ranges. raise questions concerning the taxonomic, functional, One group implants foreign matter regularly; in the other, and stratigraphic significance of this particular trait this feature is quite irregular. Both groups include species having individuals that do not implant material. as well as the biologic validity of Philoxene. In an In both living and fossil carrier shells, the animals show attempt to understand the problems presented by little preference in materials selected except on the basis of these Devonian forms, we have examined the modern size. The implanted material probably served primarily as carrier shell X enophora and the closely related Tu­ tactile camouflage as well as visual camouflage. gurium. Philoxene Kayser is based on implantation and is here re­ The present study is a fusion of interests origi­ garded as based on a spurious concept. The type species should be placed in the Straparollus senso stricto and other nally derived from two separate geographic areas. species distributed under various subgenera of Straparollus; More than a decade ago, M. H. Staatz, U.S. Geologi­ implantation alone seems a poor criterion for discriminating cal Survey, submitted for examination a collection a species. The species studied in this paper are treated under from Nevada which was later identified asPhiloxene. three subgenera: Straparollus (Straparollus), S. (Serpulo­ The effort required to transport a large block of spira), and S. (Euomphalus). Species of S. (Euomphalus) in which implantation occurs seem to indicate that the angu­ limestone for acid treatment from an area difficult lated whorl profile characteristic of this taxon evolved more of access is cordially acknowledged. than once in time. For the past 10 years, Linsley has been engaged INTRODUCTION AND ACKNOWLEDGMENTS in a study of the gastropod fauna of the Rogers City Limestone. Access to the Calcite quarry, Michigan Kayser (1889, p. 292) established the genus Phil­ Limestone Operations, U.S. Steel Corp., at Rogers oxene and designated Euomphalus laevis Archiac City, Mich., and to the Presque Isle Corporation and Verneuil (1842) as type species. The genus was quarry (formerly Lake of the Woods quarry) north judged distinct from other euomphalid gastropods of Alpena, Mich., managed by Mr. Roy Hutchison because individuals attached foreign matter, usually for a consortium of steel companies, has always been shell fragments, to their shells. As Knight (1941, graciously granted. Field investigations in 1966-69 1Department of Geology, Colgate University, Hamilton, N.Y. were supported by the ~esearch Council of Colgate 1 2 DEVONIAN CARRIER SHELLS (EUOMPHALIDAE) FROM NORTH AMERICA AND GERMANY University. In addition, during 1965, the National IMPLANTATION AMONG THE RECENT FAUNA Science Foundation provided a grant to support a The incorporation of foreign bodies into the hard collecting trip by 10 high school students under Lins­ parts of an organism is not a common trait, but it ley's supervision. Further, the Research Council of is widespread in a systematic sense. Some Forami­ Colgate University provided an Undergraduate Re­ nifera have apparently been building an agglutinated search Participation Grant which permitted John test (Towe, 1967) since the Cambrian; other Fo­ Cottrell and John Hoffman to assist with fieldwork. raminifera may imbed foreign grains in a calcium Naming of two species after these assistants is a carbonate test. A few tunicates and sponges aggluti­ partial acknowledgment of the calibre of help they nate sand grains in their flesh, in part, perhaps, provided throughout the various stages of this inves­ accidentally. Worm burrows may be formed of tigation. grains of sand bound by mucus, and many worms Specimens were generously loaned by Dr. Roger that live on the bottom construct tubes of clastic Batten, American Museum of Natural History grains. Fresh-water caddis fly larvae and terrestrial (AMNH). Large collections were lent for study by bagworms are well-known examples of makers of the Museum of Paleontology, University of Michi­ agglutinated tubes. Several animals, such as the gan (UMMP). Dr. G. M. Ehlers, University of "decorator crab," which
Recommended publications
  • XENOPHORIDAE Een Overzicht Van Alle Recent Voorkomende Soorten
    XENOPHORIDAE Een overzicht van alle recent voorkomende soorten. J.Goud en G.Kronenberg TROQUE (Trochus) Troque agglutinant INLEIDING Dit artikel is bedoeld om het determineren van de videerd (Ponder, 1983), waarmee nu een duide­ diverse soorten behorende tot de familie Xenop­ li jk overzicht van de familie voorhanden is. De horidae Ph il ippi, 1853 te vergemakkelijken. Tot indeling die Ponder geeft zal hier grotendeels voor kort was dit een schier ondoenlijk werk, gevolgd worden. mede door de verschillende namen die aan één Tevens betreft dit artikel de inlossing van een soort gegeven werden (synoniemen) , maar ook oude belofte om een dergelijk overzicht in Vi ta vaak dezelfde naam aan verschillende soorten Marina te publiceren (Faber, 1978). In dat artikel (homoniemen), waardoor de nomenclatuur van wordt beschreven hoe de aanhechting van ma­ deze groep een grote chaos was. teriaal in zi jn werk gaat en wordt ingegaan op de Enkele jaren geleden is deze groep echter gere- diverse theorieën die bestaan over het waarom vita marina zeebiologische dokumentatie juli-dec. 1988 bu ikpotigen 457 van dit opvallende gedrag. Verder worden er familie: enkele opmerkingen gemaakt over de levenswij­ Xenophoridae Troschel, 1852 ze en de manier van voortbeweging. Hierop zal (op lijst ICNZ opninie 715 als Philippi, 1853) verder niet worden ingegaan, wij verwijzen daar­ geslacht: voor naar bedoeld artikel. Xenophora Fischer von Waldheim, 1807 Uitgestorven soorten zijn in onderstaand over­ ondergeslacht: zicht niet opgenomen. Xenophora s.S. O. soorten : conchyliophora (Born, 1780) 0.000 OORSPRONG EN VERSPRE IDING cerea (Reeve, 1845) 0.010 flindersi flindersi (eotton & Godfrey, 1938) De Xenophoridae kennen een rijke fossiele histo­ 0.020 e rie.
    [Show full text]
  • Bull. Geol. Soc. Am. Vol. 46, 1935, Pl. 33
    BULL. GEOL. SOC. AM. VOL. 46, 1935, PL. 33 F ig u r e 2. E a stern F a ce o f t h e Q uarry DUNDEE-ANDERDON CONTACT IN SIBLEY QUARRY Downloaded from http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/46/3/425/3415212/BUL46_3-0425.pdf by guest on 01 October 2021 BULLETIN OF THE GEOLOGICAL SOCIETY CfF A M E R IC A VOL. 46, PP. 428-462, PLS. 33-39, 1 FIG. MARCH 31. 1935 PROCEEDINGS OF THE PALEONTOLOGICAL SOCIETY STRATIGRAPHY AND PALEONTOLOGY OF THE DUNDEE LIMESTONE OF SOUTHEASTERN MICHIGAN* BY CHARLES FERNANDO BASSETT (Presented before the Paleontological Society, December SO, 193S) CONTENTS Page Introduction............................................................................................................. 425 Statement of the problem................................................................................ 425 Acknowledgments............................................................................................. 427 Stratigraphy of the Dundee limestone................................................................... 427 Distribution....................................................................................................... 427 Previous classification...................................................................................... 427 Description of sections..................................................................................... 428 Sibley quarry............................................................................................. 428 Christiancy or Macon quarry.................................................................
    [Show full text]
  • OGS 1962 RI-42.Pdf
    ·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·i i STATE CE OHIO • MICHAEL V. DISALLI, eo-- DD'AU'MEHT CE NATIJl\AL llES<XmCES Ilo IElllEl\T a, EAGON, Dlncllor In'ISION OF GEOLOGICAL SURVEY l\AJ.PH J. KIUIHACEN, Chief Ii I• lo I REPORT OF INVESTIGATIONS NO. 42 LOWER AND MIDDLE DEVONIAN LIMESTONES IN NORTHEASTERN OHIO • I • AND ADJACENT AREAS I i• I ~ ~ By i John W. Dow i II • I • I • I I • i I . • I I COLUMBUS ~ . 1962 I I • • I• I I • • I I ~-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-· STATE OF OHIO Michael V. DiSalle Governor DEPARTMENT OF NATURAL RESOURCES Herbert B. Eagon Director NATURAL RESOURCES COMMISSION Herbert B. Eagon Lawrence Kimble Byron Frederick Roy M. Kottman Forrest G. Hall Demas L. Sears William Hoyne Myron T.· Sturgeon Joseph E. Hurst DIVISION OF GEOLOGICAL SURVEY Ralph J. Bernhagen Chief The F . J . Heer Printing Company Columbus 16, Ohio 1962 Bound by the State of Ohio ;-·-·-·-·-·-·-·-·-·-~-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·i i• i I ~Of~ I• 0 MICHAEL V. DI SALLE, Governor lo DEPAR1MENT Of NATURAL RESOURCES I HERBERT II. EAGON, Director I DIVISION OF GEOLOGICAL SURVEY RALPH J. BERNHAGEN, Chief • I • I.. I REPORT OF INVESTIGATIONS NO. 42 i i;. ! .I .I I LOWER AND MIDDLE DEVONIAN LIMESTONES . IN NORTHEASTERN OHIO I • AND ADJACENT AREAS .I I• I.. I By i• John W. Dow I ! ! ! I • I • I • .I .I .I I I COLUMBUS • . 1962 I I • . I.. I For sale l::ry Ohio Division of Geological Survey, Columbus, Ohio I • Price 97 cents plus 3 cents tax in Ohio • I ~ ...... _...... ··-.- .- ·-.- .- .- .- .- .- .- .- .- .- .- ._,,. -.- .- .- .- .- .- . BLANK PAGE CONTENTS Page Introduction. 1 Purpose of study 1 Previous studies 1 Methods of investigation.
    [Show full text]
  • Cambrian Ordovician
    Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation.
    [Show full text]
  • THE GEOMETRY of COILING in GASTROPODS Thompson.6
    602 ZO6LOGY: D. M. RA UP PROC. N. A. S. 3 Cole, L. J., W. E. Davis, R. M. Garver, and V. J. Rosen, Jr., Transpl. Bull., 26, 142 (1960). 4 Santos, G. W., R. M. Garver, and L. J. Cole, J. Nat. Cancer Inst., 24, 1367 (1960). I Barnes, D. W. H., and J. F. Loutit, Proc. Roy. Soc. B., 150, 131 (1959). 6 Koller, P. C., and S. M. A. Doak, in "Immediate and Low Level Effects of Ionizing Radia- tions," Conference held in Venice, June, 1959, Special Supplement, Int. J. Rad. Biol. (1960). 7 Congdon, C. C., and I. S. Urso, Amer. J. Pathol., 33, 749 (1957). 8 Biological Problems of Grafting, ed. F. Albert and P. B. Medawar (Oxford University Press, 1959). 9 Lederberg, J., Science, 129, 1649 (1959). 10Burnet, F. M., The Clonal Selection Theory of Acquired Immunity (Cambridge University Press, 1959). 11 Billingham, R. E., L. Brent, and P. B. Medawar, Phil. Trans. Roy. Soc. (London), B239, 357 (1956). 12 Rubin, B., Natyre, 184, 205 (1959). 13 Martinez, C., F. Shapiro, and R. A. Good, Proc. Soc. Exper. Biol. Med., 104, 256 (1960). 14 Cole, L. J., Amer. J. Physiol., 196, 441 (1959). 18 Cole, L. J., in Proceedings of the IXth International Congress of Radiology, Munich 1959 (Georg Thieme Verlag, in press). 16 Cole, L. J., R. M. Garver, and M. E. Ellis, Amer. J. Physiol., 196, 100 (1959). 17 Cole, L. J., and R. M. Garver, Nature, 184, 1815 (1959). 18 Cole, L. J., and W. E. Davis, Radiation Res., 12, 429 (1960).
    [Show full text]
  • Middle Devonian Formations in the Subsurface of Northwestern Ohio
    STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 SCIENTIFIC AND TECHNICAL STAFF OF THE OHIO DIVISION OF GEOLOGICAL SURVEY ADMINISTRATIVE SECTION Horace R. Collins, State Geologist and Di v ision Chief David K. Webb, Jr., Geologist and Assistant Chief Eleanor J. Hyle, Secretary Jean S. Brown, Geologist and Editor Pauline Smyth, Geologist Betty B. Baber, Geologist REGIONAL GEOLOGY SECTION SUBSURFACE GEOLOGY SECTION Richard A. Struble, Geologist and Section Head William J. Buschman, Jr., Geologist and Section Head Richard M. Delong, Geologist Michael J. Clifford, Geologist G. William Kalb, Geochemist Adriaan J anssens, Geologist Douglas L. Kohout, Geologis t Frederick B. Safford, Geologist David A. Stith, Geologist Jam es Wooten, Geologist Aide Joel D. Vormelker, Geologist Aide Barbara J. Adams, Clerk· Typist B. Margalene Crammer, Clerk PUBLICATIONS SECTION LAKE ERIE SECTION Harold J. Fl inc, Cartographer and Section Head Charles E. Herdendorf, Geologist and Sectwn Head James A. Brown, Cartographer Lawrence L. Braidech, Geologist Donald R. Camburn, Cartovapher Walter R. Lemke, Boat Captain Philip J. Celnar, Cartographer David B. Gruet, Geologist Aide Jean J. Miller, Photocopy Composer Jean R. Ludwig, Clerk- Typist STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 GEOLOGY SERVES OHIO CONTENTS Page Introduction . 1 Previous investigations .. .. .. .. .. .. .. .. .. 1 Study methods . 4 Detroit River Group . .. .. .. ... .. ... .. .. .. .. .. .. .. ... .. 6 Sylvania Sandstone ..........................
    [Show full text]
  • Homeomorphic Gastropods from the Silurian of Norway, Estonia and Bohemia
    Homeomorphic gastropods from the Silurian of Norway, Estonia and Bohemia MARE ISAKAR, JAN OVE R. EBBESTAD & JOHN S. PEEL Isakar, M,. Ebbestad, J. O. R. & Peel, J. S.: Homeomorphic gastropods from the Silurian of Norway, Estonia and Bohemia. Norsk Geologisk Tidsskrift, Vol. 79, pp. 281-288. Oslo 1999. ISSN 0029-196X. Redescription of the gastropodEuomphalus undiferus Schmidt, 1858 fromthe Upper Llandovery Rumba Formation of Estonia requires reinvestigation of the hitherto monotypic genus Kiaeromphalus Peel & Y ochelson, 1976, originally described from the Rytteråker Formation of the Oslo Region. The Estonian K. undiferus and the Norwegian type species occur in similar depositional facies of Early Silurian age within the sedgwickii Graptolite Zone. The redescribed type specimen of Horologium kokeni Perner, 1907 from the late Silurian (Ludlow) of Bohemia shows strong morphological convergence with the two Baltic species, but Kiaeromphalus is distinguished by its lower rate of whorl expansion and less oblique aperture. Both genera were adapted to a sessile life, possibly on a soft substratum. Mare lsakar, Museum ofGeology, University ofTartu, Vanemuise 46, 51014 Tartu, Estonia. E-mail: [email protected]; Jan OveR. Ebbestad & JohnS. Peel, Department of Earth Sciences (Historical Geology and Palaeontology), Uppsala University, Norbyviigen 22, S-752 36 Uppsala, Sweden. E-mail: [email protected]; [email protected]. Introduction morphic, genera; Schmidt's (1858) species from Estonia is ascribed to the latter genus. Thus, Kiaeromphalus occurs In 1976, Peel & Yochelson reviewed Early Silurian from southem Norway to Estonia in the Lower Silurian (Llandovery) gastropods from the Oslo Region and rocks, although it remains unreported from the Silurian of proposed two new genera, Kiaeromphalus and Kjerulfo­ Sweden.
    [Show full text]
  • Givetian Brachiopods from the Trois-Fontaines Formation (Belgium, Dinant Synclinorium)
    bulletin de l'institut royal des sciences naturelles de belgique sciences de la terre, 75: 5-23, 2005 bulletin van het koninklijk belgisch instituut voor natuurwetenschappen aardwetenschappen, 75: 5-23, 2005 Givetian brachiopods from the Trois-Fontaines Formation at Marenne (Belgium, Dinant Synclinorium) by Jacques GODEFROID & Bernard MOTTEQUIN Godefroid, J. & Mottequin. B„ 2005. — Givetian brachiopods from sisting of five units (thickness of these units from the base the Trois-Fontaines Formation at Marenne (Belgium, Dinant Syncli¬ to the norium). Bulletin de l'Institut royal des Sciences naturelles de Belgi¬ top: 26 m, 11 m, 23 m, 3.2 m, 23 m) (Fig. 3). The que, Sciences de la Terre, 75: 5-23, 2 pis., 9 figs., 4 tables, Bruxelles- brachiopods described herein have been collected Brussel, March 31, 2005 - ISSN 0374-6291. in the dark, well-bedded and bioclastic limestones with silty and crinoidal levels (unit 1), in the fine, dark co- loured, well-bedded limestones (unit 3) and in the crinoi¬ Abstract dal limestones rich in Scoliopora (unit 4). In units 1 and 3, although some beds are very rich in The brachiopods sampled from the Trois-Fontaines Formation in the brachiopods (some of them very large), it is difficult to Marenne quarry are mainly represented by two species: Spinatrypina sample well-preserved material and present the complete (Spinatrypina) fontis n. sp. and Eifyris socia n. sp. Orthid, rhyncho- inventory of the fauna. On the other hand, in unit 4, nellid, spiriferid and terebratulid brachiopods are also present but much rarer. Among them a new species, Bornhardtina equitis n.
    [Show full text]
  • ABSTRACT Title of Dissertation: PATTERNS IN
    ABSTRACT Title of Dissertation: PATTERNS IN DIVERSITY AND DISTRIBUTION OF BENTHIC MOLLUSCS ALONG A DEPTH GRADIENT IN THE BAHAMAS Michael Joseph Dowgiallo, Doctor of Philosophy, 2004 Dissertation directed by: Professor Marjorie L. Reaka-Kudla Department of Biology, UMCP Species richness and abundance of benthic bivalve and gastropod molluscs was determined over a depth gradient of 5 - 244 m at Lee Stocking Island, Bahamas by deploying replicate benthic collectors at five sites at 5 m, 14 m, 46 m, 153 m, and 244 m for six months beginning in December 1993. A total of 773 individual molluscs comprising at least 72 taxa were retrieved from the collectors. Analysis of the molluscan fauna that colonized the collectors showed overwhelmingly higher abundance and diversity at the 5 m, 14 m, and 46 m sites as compared to the deeper sites at 153 m and 244 m. Irradiance, temperature, and habitat heterogeneity all declined with depth, coincident with declines in the abundance and diversity of the molluscs. Herbivorous modes of feeding predominated (52%) and carnivorous modes of feeding were common (44%) over the range of depths studied at Lee Stocking Island, but mode of feeding did not change significantly over depth. One bivalve and one gastropod species showed a significant decline in body size with increasing depth. Analysis of data for 960 species of gastropod molluscs from the Western Atlantic Gastropod Database of the Academy of Natural Sciences (ANS) that have ranges including the Bahamas showed a positive correlation between body size of species of gastropods and their geographic ranges. There was also a positive correlation between depth range and the size of the geographic range.
    [Show full text]
  • Biodiversity, Distribution and Patterns of Extinction of the Last Odontopleuroid Trilobites During the Devonian (Givetian, Frasnian)
    Geol. Mag. 144 (5), 2007, pp. 777–796. c 2007 Cambridge University Press 777 doi:10.1017/S0016756807003779 First published online 13 August 2007 Printed in the United Kingdom Biodiversity, distribution and patterns of extinction of the last odontopleuroid trilobites during the Devonian (Givetian, Frasnian) ∗ RAIMUND FEIST & KENNETH J. MCNAMARA† ∗Laboratoire de Paleontologie,´ Institut des Sciences de l’Evolution, Universite´ Montpellier II, Cc 062, Place E. Bataillon, 34095 Montpellier, France †Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK (Received 18 September 2006; accepted 22 February 2007) Abstract – Biostratigraphical ranges and palaeogeographical distribution of mid-Givetian to end- Frasnian odontopleurids are investigated. The discovery of Leonaspis rhenohercynica sp. nov. in mid-Givetian strata extends this genus unexpectedly up to the late Middle Devonian. New material of Radiaspis radiata (Goldfuss, 1843) and the first koneprusiine in Britain, Koneprusia? sp., are described from the famous Lummaton shell-bed, Torquay, Devon. New taxa of Koneprusia, K. serrensis, K. aboussalamae, K. brevispina,andK. sp. A and K. sp. B are defined. Ceratocephala (Leonaspis) harborti Richter & Richter, 1926, is revised and reassigned to Gondwanaspis Feist, 2002. Two new species of Gondwanaspis, G. dracula and G. spinosa, plus three others left in open nomenclature, are described from the late Frasnian of Western Australia. A further species of Gondwanaspis, G. prisca, is described from the early Frasnian of Montagne Noire. Species of Gondwanaspis are shown to possess a number of paedomorphic features. A functional analysis suggests that, unlike other odontopleurids, Gondwanaspis actively fed and rested with the same cephalic orientation. The sole odontopleurid survivors of the severe terminal mid-Givetian biocrisis (‘Taghanic Event’) belong to the koneprusiine Koneprusia in the late Givetian and Frasnian, and, of cryptogenic origin, the acidaspidine Gondwanaspis in the Frasnian.
    [Show full text]
  • Xenophoridae, Cypraeoidea, Mitriforms and Terebridae (Caenogastropoda)
    Taxonomic study on the molluscs collected in Marion-Dufresne expedition (MD55) to SE Brazil: Xenophoridae, Cypraeoidea, mitriforms and Terebridae (Caenogastropoda) Luiz Ricardo L. SIMONE Carlo M. CUNHA Museu de Zoologia da Universidade de São Paulo, caixa postal 42494, 04218-970 São Paulo, SP (Brazil) [email protected] [email protected] Simone L. R. L. & Cunha C. M. 2012. — Taxonomic study on the molluscs collected in Marion-Dufresne expedition (MD55) to SE Brazil: Xenophoridae, Cypraeoidea, mitriforms and Terebridae (Caenogastropoda). Zoosystema 34 (4): 745-781. http://dx.doi.org/10.5252/z2012n4a6 ABSTRACT The deep-water molluscs collected during the expedition MD55 off SE Brazil have been gradually studied in some previous papers. The present one is focused on samples belonging to caenogastropod taxa Xenophoridae Troschel, 1852, Cypraeoidea Rafinesque, 1815, mitriforms and Terebridae Mörch, 1852. Regarding the Xenophoridae, Onustus aquitanus n. sp. is a new species, collected off the littoral of Espírito Santo and Rio de Janeiro, Brazil, 430-637 m depth (continental slope). The main characters of the species include the small size (c. 20 mm), the proportionally wide shell, the white colour, the short peripheral flange, the oblique riblets weakly developed and a brown multispiral protoconch. This appears to be the smallest living species of the family, resembling in this aspect fossil species. In respect to the Cypraeoidea, the following results were obtained: family Cypraeidae Rafinesque, 1815: Erosaria acicularis (Gmelin, 1791) and Luria cinerea (Gmelin, 1791) had the deepest record, respectively 607-620 m and 295-940 m, although the samples were all dead, eroded shells. Family Lamellariidae d’Orbigny, 1841: a total of three lots were collected, provisionally identified as Lamellaria spp.
    [Show full text]
  • Solaropsis Brasiliana, Anatomy, Range Extension and Its Phylogenetic Position Within Pleurodontidae (Mollusca, Gastropoda, Stylommatophora)
    Anais da Academia Brasileira de Ciências (2018) (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201820170261 www.scielo.br/aabc | www.fb.com/aabcjournal Solaropsis brasiliana, anatomy, range extension and its phylogenetic position within Pleurodontidae (Mollusca, Gastropoda, Stylommatophora) MARÍA GABRIELA CUEZZO1, AUGUSTO P. DE LIMA2 and SONIA B. DOS SANTOS2 1Instituto de Biodiversidad Neotropical/CONICET-UNT, Crisóstomo Álvarez, 722, 4000 Tucumán, Argentina 2Instituto de Biologia Roberto Alcantara Gomes, Universidade do Estado do Rio de Janeiro, Rua São Francisco Xavier, 524, PHLC, Sala 525-2, 20550-900 Rio de Janeiro, RJ, Brazil Manuscript received on April 7, 2017; accepted for publication on October 13, 2017 ABSTRACT A detailed anatomical revision on Solaropsis brasiliana (Deshayes 1832) has been carried out. New characters on shell, anatomy of soft parts, and a review of the genus distribution in South America, as well as clarification on S. brasiliana distributional area are provided in the present study. Solaropsis brasiliana is diagnosed by its globose, solid, and hirsute shell, with periphery obsoletely angular, bursa copulatrix with a thick, long diverticulum, a thick, long flagellum and a penis retractor muscle forked, with the vas deferens passing through it. This compiled information was used to test the phylogenetic position of S. brasiliana within South American Pleurodontidae through a cladistics analysis. In the phylogenetic hypothesis obtained, S. brasiliana is sister group of S. gibboni (Pfeiffer 1846) and the monophyly of the genus Solaropsis Beck is also supported. Here, we sustain that the distribution of S.
    [Show full text]