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BIBLIOGRAPHICAL SKETCH Kevin J. Eckelbarger Professor of Marine
BIBLIOGRAPHICAL SKETCH Kevin J. Eckelbarger Professor of Marine Biology School of Marine Sciences University of Maine (Orono) and Director, Darling Marine Center Walpole, ME 04573 Education: B.Sc. Marine Science, California State University, Long Beach, 1967 M.S. Marine Science, California State University, Long Beach, 1969 Ph.D. Marine Zoology, Northeastern University, 1974 Professional Experience: Director, Darling Marine Center, The University of Maine, 1991- Prof. of Marine Biology, School of Marine Sciences, Univ. of Maine, Orono 1991- Director, Division of Marine Sciences, Harbor Branch Oceanographic Inst. (HBOI), Ft. Pierce, Florida, 1985-1987; 1990-91 Senior Scientist (1981-90), Associate Scientist (1979-81), Assistant Scientist (1973- 79), Harbor Branch Oceanographic Inst. Director, Postdoctoral Fellowship Program, Harbor Branch Oceanographic Inst., 1982-89 Currently Member of Editorial Boards of: Invertebrate Biology Journal of Experimental Marine Biology & Ecology Invertebrate Reproduction & Development For the past 30 years, much of his research has concentrated on the reproductive ecology of deep-sea invertebrates inhabiting Pacific hydrothermal vents, the Bahamas Islands, and methane seeps in the Gulf of Mexico. The research has been funded largely by NSF (Biological Oceanography Program) and NOAA and involved the use of research vessels, manned submersibles, and ROV’s. Some Recent Publications: Eckelbarger, K.J & N. W. Riser. 2013. Derived sperm morphology in the interstitial sea cucumber Rhabdomolgus ruber with observations on oogenesis and spawning behavior. Invertebrate Biology. 132: 270-281. Hodgson, A.N., K.J. Eckelbarger, V. Hodgson, and C.M. Young. 2013. Spermatozoon structure of Acesta oophaga (Limidae), a cold-seep bivalve. Invertertebrate Reproduction & Development. 57: 70-73. Hodgson, A.N., V. -
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. -
MOLECULAR PHYLOGENY of the NERITIDAE (GASTROPODA: NERITIMORPHA) BASED on the MITOCHONDRIAL GENES CYTOCHROME OXIDASE I (COI) and 16S Rrna
ACTA BIOLÓGICA COLOMBIANA Artículo de investigación MOLECULAR PHYLOGENY OF THE NERITIDAE (GASTROPODA: NERITIMORPHA) BASED ON THE MITOCHONDRIAL GENES CYTOCHROME OXIDASE I (COI) AND 16S rRNA Filogenia molecular de la familia Neritidae (Gastropoda: Neritimorpha) con base en los genes mitocondriales citocromo oxidasa I (COI) y 16S rRNA JULIAN QUINTERO-GALVIS 1, Biólogo; LYDA RAQUEL CASTRO 1,2 , Ph. D. 1 Grupo de Investigación en Evolución, Sistemática y Ecología Molecular. INTROPIC. Universidad del Magdalena. Carrera 32# 22 - 08. Santa Marta, Colombia. [email protected]. 2 Programa Biología. Universidad del Magdalena. Laboratorio 2. Carrera 32 # 22 - 08. Sector San Pedro Alejandrino. Santa Marta, Colombia. Tel.: (57 5) 430 12 92, ext. 273. [email protected]. Corresponding author: [email protected]. Presentado el 15 de abril de 2013, aceptado el 18 de junio de 2013, correcciones el 26 de junio de 2013. ABSTRACT The family Neritidae has representatives in tropical and subtropical regions that occur in a variety of environments, and its known fossil record dates back to the late Cretaceous. However there have been few studies of molecular phylogeny in this family. We performed a phylogenetic reconstruction of the family Neritidae using the COI (722 bp) and the 16S rRNA (559 bp) regions of the mitochondrial genome. Neighbor-joining, maximum parsimony and Bayesian inference were performed. The best phylogenetic reconstruction was obtained using the COI region, and we consider it an appropriate marker for phylogenetic studies within the group. Consensus analysis (COI +16S rRNA) generally obtained the same tree topologies and confirmed that the genus Nerita is monophyletic. The consensus analysis using parsimony recovered a monophyletic group consisting of the genera Neritina , Septaria , Theodoxus , Puperita , and Clithon , while in the Bayesian analyses Theodoxus is separated from the other genera. -
Gałęzice Syncline, Holy Cross Mts)
ROCZNIK POLSKIEGO TOWARZYSTWA GEOLOGICZNEGO A N N A L E S DE LA SOCIÉTÉ G É O L O G IQ U E DE P O L O G N E Tom (Volume) XLIV — 1974 Zeszyt (Fascicule) 1 Kraków 1974 HALINA ŻAKOWA GONIATITINA FROM THE UPPER YISEAN (GAŁĘZICE SYNCLINE, HOLY CROSS MTS) (Pl. I— IV and 10 Figs.) Goniatitina z serii wapiennej i wapienno-iłowcowej górnego wizenu synkliny gałęzickiej (Góry Świętokrzyskie) (Tabl. I—IV i 10 fig.) Abstract: The organodetritic and organogenic limestones under study have been assigned to Goa Zone and Goßmu Subzone. In the systematic part the follow ing species have been described: Goniatites crenistria Phill., G. ex gr. crenistria Phill., G. sphaericostriatus Bisat, G. robustus Moore et Hod., G. cf. m ucro- natus (K n о p p), Goniatites sp., Muensteroceras truncatum (Phil 1.), M. sp. cf. jo u r- nieri (Del épine), Nomismoceras vittiger (P hill.), Glyphiolobus pseudodiscrepans (Moor e). Correlation of discussed profiles is based on both paleontological and geological investigations. INTRODUCTION Notwithstanding a considerable advance in the studies on the Gałęziee syncline (e.g. Ż а к o w a 1970 a, b, 1971 a; Jachowicz, Żakowa, 1969; Jurkiewicz, Żak o w a, 1972), not all the problems concerning the stratigraphy of the Carboniferous rocks have been- satisfactorily elucidated. The present paper deals with the stratigraphy of the Upper Visean calcareous rocks (visible in outcrops) and their lateral equivalents* i.e. calcareous-clayey rocks (known from boreholes). According to Czarnocki (1965) and Kwiatkowski (1959), the calcareous rocks represent the whole Visean, whereas Czarniec ki, Kostecka and Kwiatkowski (1965) are of the opinion that they belong to D3_2zones only. -
Limitations of Cytochrome Oxidase I for the Barcoding of Neritidae (Mollusca: Gastropoda) As Revealed by Bayesian Analysis
Limitations of cytochrome oxidase I for the barcoding of Neritidae (Mollusca: Gastropoda) as revealed by Bayesian analysis S.Y. Chee Center for Marine and Coastal Studies, Universiti Sains Malaysia, Penang, Malaysia Corresponding author: S.Y. Chee E-mail: [email protected] Genet. Mol. Res. 14 (2): 5677-5684 (2015) Received September 5, 2014 Accepted February 26, 2015 Published May 25, 2015 DOI http://dx.doi.org/10.4238/2015.May.25.20 ABSTRACT. The mitochondrial DNA (mtDNA) cytochrome oxidase I (COI) gene has been universally and successfully utilized as a barcoding gene, mainly because it can be amplified easily, applied across a wide range of taxa, and results can be obtained cheaply and quickly. However, in rare cases, the gene can fail to distinguish between species, particularly when exposed to highly sensitive methods of data analysis, such as the Bayesian method, or when taxa have undergone introgressive hybridization, over-splitting, or incomplete lineage sorting. Such cases require the use of alternative markers, and nuclear DNA markers are commonly used. In this study, a dendrogram produced by Bayesian analysis of an mtDNA COI dataset was compared with that of a nuclear DNA ATPS-α dataset, in order to evaluate the efficiency of COI in barcoding Malaysian nerites (Neritidae). In the COI dendrogram, most of the species were in individual clusters, except for two species: Nerita chamaeleon and N. histrio. These two species were placed in the same subcluster, whereas in the ATPS-α dendrogram they were in their own subclusters. Analysis of the ATPS-α gene also placed the two genera of nerites (Nerita and Neritina) in separate clusters, whereas COI gene Genetics and Molecular Research 14 (4): 5677-5684 (2014) ©FUNPEC-RP www.funpecrp.com.br S.Y. -
Type Kinderhook Ammonoids
Proceedings of the Iowa Academy of Science Volume 80 Number Article 6 1973 Type Kinderhook Ammonoids W. M. Furnish University of Iowa Walter L. Manger University of Iowa Let us know how access to this document benefits ouy Copyright ©1973 Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/pias Recommended Citation Furnish, W. M. and Manger, Walter L. (1973) "Type Kinderhook Ammonoids," Proceedings of the Iowa Academy of Science, 80(1), 15-24. Available at: https://scholarworks.uni.edu/pias/vol80/iss1/6 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Proceedings of the Iowa Academy of Science by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. Furnish and Manger: Type Kinderhook Ammonoids 15 Type Kinderhook Ammonoids W. M. FURNISH1 and WALTER L. MANGER FURNISH, W. M. and WALTER L. MANGER. Type Kinderhook Am and the associated conodont faunal data. The Kinderhookian monoids. Proc. Iowa Acad. Sci., 80( 1): 15-24, 1973. Wassonville Member of the Hampton Formation in southeastern SYNOPSIS: Lower Mississippian rocks in the type area of North Iowa and the Chouteau Limestone of Missouri fall within the America have produced only a few scattered ammonoid cephalo lower "Pericyclus-Stufe" of the upper Tournaisian Stage as these pods. Those specimens from southeastern Iowa and northwestern units are designated for the early Lower Carboniferous of Western Missouri lie within the general vicinity of the designated type Europe. -
Neevia Docconverter 5.1
UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO FACULTAD DE CIENCIAS CEFALÓPODOS DE LA FORMACIÓN SANTIAGO, MISISÍPICO DE LA REGIÓN DE NOCHIXTLÁN, OAXACA. T E S I S QUE PARA OBTENER EL TÍTULO DE: BIÓLOGA P R E S E N T A: KARLA MARÍA CASTILLO ESPINOZA TUTOR: DR. FRANCISCO SOUR TOVAR 2008 FACULTAD DE CIENCIAS UNAM Neevia docConverter 5.1 UNAM – Dirección General de Bibliotecas Tesis Digitales Restricciones de uso DERECHOS RESERVADOS © PROHIBIDA SU REPRODUCCIÓN TOTAL O PARCIAL Todo el material contenido en esta tesis esta protegido por la Ley Federal del Derecho de Autor (LFDA) de los Estados Unidos Mexicanos (México). El uso de imágenes, fragmentos de videos, y demás material que sea objeto de protección de los derechos de autor, será exclusivamente para fines educativos e informativos y deberá citar la fuente donde la obtuvo mencionando el autor o autores. Cualquier uso distinto como el lucro, reproducción, edición o modificación, será perseguido y sancionado por el respectivo titular de los Derechos de Autor. Formato Ejemplo 1.Datos del alumno 1. Datos del alumno Apellido paterno Castillo Apellido materno Espinoza Nombre(s) Karla María Teléfono 56 44 99 69 Universidad Nacional Autónoma de México Universidad Nacional Autónoma de México Facultad de Ciencias Facultad de Ciencias Carrera Biología Número de cuenta 300003323 2. Datos del tutor 2. Datos del tutor Grado Dr. Nombre(s) Francisco Apellido paterno Sour Apellido materno Tovar 3. Datos del sinodal 1 3. Datos del sinodal 1 Grado Dra. Nombre(s) Sara Alicia Apellido paterno Quiroz Apellido materno Barroso 4. Datos del sinodal 2 4. Datos del sinodal 2 Grado Dra. -
Evolution of the Goniatitaceae and Vis6an-Namurian Biogeography
Evolution of the Goniatitaceae and Vis6an-Namurian biogeography DIETERKORN Korn, D. 1997. Evolution of the Goniatitaceaeand Vis6an-Namurian biogeography.- Acta Pal eontologica P olonica 42, 2, 177 -199. Evolutionary lineages within the Carboniferous ammonoid superfamily Goniatitaceae can be recognized using cladistic and stratopheneticanalyses, showing that both ap- proaches lead to coinciding results. In the late Vis6an and Namurian A, ammonoid provinces can be defined by the distribution of lineages within the goniatite superfamily Goniatitaceae. The first province corresponds to the Subvariscan Realm (where the superfamily became extinct near the Vis6an-Namurian boundary), and the second em- braces the majority of the occurrences,e.g. the south urals, central Asia, and North America (where the superfamily with different independent lieages continued up into the late Namurian A). In the Vis6an, the superfamily was, in two short epochs, globally distributed with major transgressions,which probably led to migration events. The first is at the end of the late Vis6an A(G. fi.mbrians and G. spirifer Zones, when the genus Goniatites had a world-wide distribution with various species),and the second at the beginning of the late Vis6an C (L. poststriatumZone, when Lusitanoceras is globally distributed). K e y w o r d s : Ammonoidea, Goniatitaceae, Early Carboniferous, phylogeny, palaeo- biogeography. Dieter Korn [dieter.korn@uni+uebingen.de], Institut und Museum fiir Geologie und Palciontologieder Eberhard-Karls-(Jniversitrit, SigwartstraJJe10, 72076 Tiibingen, Ger- many. Introduction Late Vis6an and early Namurian goniatite faunashave been reported fiom numerous localities in the northernhemisphere, from Alaska andCanada, the Westernand Central United States,various regions in Europeand North Africa, Novaya Zemlya and the South Urals, Central Asia, as well as from China. -
Bulletin 182 Contributions to Canadian Paleontology
BULLETIN 182 CONTRIBUTIONS TO CANADIAN PALEONTOLOGY (eleven papers) B. S. Norford, D. E. Jaclcson and A. C. Lenz, D. H. Collins, W. T. Dean, D. C. McGregor, E. W. Bomber, W. W. Nassichuk, Charles A. Ross, R. T. D. Wiclcenden, L. V. Hills and Sandra Wallace Ottawa, Canada Price, $ 6.00 1969 CONTRIBUTIONS TO CANADIAN PALEONTOLOGY J ,450-1968-573 I -6 Technical Editors, B. S. NORFORD AND E. J . W. IRISH Editor MARGUERITE RAFUSE Text printed on No. I enamel Set in Times Roman with 20th Century captions by CANADIAN GOVERNMENT PRINTING BUREAU Artwork by CARTOGRAPHIC UNlT, GSC Collotype by COTSWOLD GEOLOGICAL SURVEY OF CANADA BULLETIN 182 CONTRIBUTIONS TO CANADIAN PALEONTOLOGY (eleven papers) By B. S. Norford, D. E Jackson and A. C. Lenz, D. H. Collins, W. T. Dean, D. C. McGregor, E. W. Bamber, W. W. Nassichuk, Charles A. Ross, R. T. D. Wickenden, L. V. Hills and Sandra Wallace DEPARTMENT OF ENERGY, MINES AND RESOURCES. CANADA © Crown Copyrights reserved Available by mail from the Queen's Printer, Ottawa, from Geological Survey of Canada, 601 Booth St., Ottawa, and at the following Canadian Government bookshops : HALIFAX 1735 Barrington Street MONTREAL tEterna-Vie Building, 11 82 St. Catherine Street West OTTAWA Daly Building, corner Mackenzie and Rideau TORONTO 221 Yonge Street WINNIPEG Mall Centcr Building, 499 Portage Avenue VANCOUVER 657 Granville Street or through your bookseller A deposit copy of this publication is also available for reference in public libraries across Canada Price $6.00 Catalogue No. M42-182 Price subject to change without notice The Queen's Printer Ottawa, Canada 1969 PREFACE From time to time it has been appropriate to issue several short papers on related paleontological topics in a single Bulletin under the general title of Contri butions to Canadian Paleontology. -
Ammonoid Intraspecific Variability
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2015 Ammonoid Intraspecific Variability De Baets, Kenneth ; Bert, Didier ; Hoffmann, René ; Monnet, Claude ; Yacobucci, Margaret M;Klug, Christian Abstract: Because ammonoids have never been observed swimming, there is no alternative to seeking indirect indications of the locomotory abilities of ammonoids. This approach is based on actualistic com- parisons with the closest relatives of ammonoids, the Coleoidea and the Nautilida, and on the geometrical and physical properties of the shell. Anatomical comparison yields information on the locomotor muscu- lar systems and organs as well as possible modes of propulsion while the shape and physics of ammonoid shells provide information on buoyancy, shell orientation, drag, added mass, cost of transportation and thus on limits of acceleration and swimming speed. On these grounds, we conclude that ammonoid swim- ming is comparable to that of Recent nautilids and sepiids in terms of speed and energy consumption, although some ammonoids might have been slower swimmers than nautilids. DOI: https://doi.org/10.1007/978-94-017-9630-9_9 Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-121836 Book Section Accepted Version Originally published at: De Baets, Kenneth; Bert, Didier; Hoffmann, René; Monnet, Claude; Yacobucci, Margaret M; Klug, Christian (2015). Ammonoid Intraspecific Variability. In: Klug, C; Korn, D; De Baets, K; Kruta, I; Mapes, R H. Ammonoid Paleobiology: From anatomy to ecology. Dordrecht: Springer, 359-426. DOI: https://doi.org/10.1007/978-94-017-9630-9_9 Chapter 9 Ammonoid Intraspecific Variability Kenneth De Baets, Didier Bert, René Hoffmann, Claude Monnet, Margaret M. -
Ammonite Fauna of Subfamily Harpoceratinae Neumayr, 1875 from Jurassic Janovky and Adnet Formations in the Veľká Fatra Mts. (Central Slovakia)
Mineralia Slovaca, 44 (2012), 285 – 294 Web ISSN 1338-3523, ISSN 0369-2086 Ammonite fauna of subfamily Harpoceratinae NEUMAYR, 1875 from Jurassic Janovky and Adnet formations in the Veľká Fatra Mts. (Central Slovakia) ANDREJ BENDÍK Slovak National Museum in Martin – Andrej Kmeť Museum, A. Kmeťa 20, SK-036 01 Martin, Slovak Republic; [email protected] Abstract The abundant ammonite fauna from the collection of Slovak National Museum in Martin – the Andrej Kmeť Museum, from the Veľká Fatra Mts., especially of the Harpoceratinae subfamily is discussed. The stone core of ammonites comes from the Janovky and Adnet formations of Liassic sequence of the Krížna nappe. Due to the poor preservation, only limited number of individuals was distinguished: Fuciniceras compressum, Fuciniceras cornacaldense, Fuciniceras lavinianum, Fuciniceras sp., Harpoceras cf. elegans, Harpoceras sp. cf. eseri, Harpoceras falcifer, Harpoceras pseudoserpentinum, Harpoceras exaratum, Harpoceras cf. falcifer, Harpoceras sp., Micropolyplectus sp., Polyplectus discoides, Protogrammoceras incertum and Protogrammoceras normanianum. This ammonite fauna indicates the Late Pliensbachian – Late Toarcian time span. Key words: Harpoceratinae, ammonite fauna, Lower Jurassic, the Veľká Fatra Mts. Introduction Rovné and Skladaná skala), but mainly in situ position. Faunistic composition of the subfamily Harpoceratinae The occurrence of the Ammonitico Rosso facies in the encompasses the species Protogrammoceras incertum Veľká Fatra Mts. is associated with the Adnet Formation (M ONESTIER ), Protogrammoceras normanianum of Liassic age. Rich ammonite fauna from the Adnet (D´ORBIGNY), Fuciniceras compressum (MONESTIER), Fm. in this mountain range was found around the 1850s Fuciniceras cornacaldense (TAUSCH), Fuciniceras (Hauer, 1855; Štúr, 1859, 1868) and sporadically also in lavinianum (FUCINI), Harpoceras cf. elegans (SOWERBY), 20th century (Andrusov, 1931; Rakús, 1964; Peržel, 1967). -
JMS 68/4 Pps. 337-344 Final
AN ULTRASTRUCTURAL STUDY OF OOGENESIS IN A PLANKTONIC AND A DIRECT-DEVELOPING SPECIES OF SIPHONARIA (GASTROPODA: PULMONATA) PURBA PAL AND ALAN N. HODGSON Department of Zoology and Entomology, Rhodes University, Grahamstown, 6140, South Africa (Received 7 January 2002; accepted 27 March 2002) ABSTRACT Oogenesis and vitellogenesis were compared at an ultrastructural level in Siphonaria capensis (a plank- Downloaded from https://academic.oup.com/mollus/article-abstract/68/4/337/1004678 by guest on 07 September 2019 tonic developer) and S. serrata (a direct developer). Except for some months in winter, most stages of oogenesis were observed during the year within a gonad, although oogenesis was asynchronous between the gonad acini. Previtellogenic oocytes, which contained few organelles, were surrounded by follicle cells. During vitellogenesis three types of storage products were accumulated in the ooplasm: yolk, lipid and glycogen. In S. capensis yolk formation begun before lipid synthesis and the yolk was produced autosynthetically. By contrast in S. serrata lipid was deposited before yolk synthesis. Morpho- logical evidence (production of yolk by Golgi bodies and rough endoplasmic reticulum; endocytotic pits along the oolemma) was found for yolk formation by both auto and heterosynthesis. In both species as the oocytes grew the follicle cells became hypertrophic and then gradually withdrew from the oocytes. Results from this study add further support to the suggestion that siphonariid limpets had a marine ancestry. INTRODUCTION Siphonaria, there have been no descriptions of egg formation (oogenesis and vitellogenesis; Hodgson, 1999). While the life Siphonariid limpets are very common pulmonates in the inter- history strategy or developmental mode is constrained by ances- tidal regions of warm temperate to tropical rocky shores, try (as has been shown in littorinids, Reid, 1990) some studies especially in the southern hemisphere (Hodgson, 1999).