(Echinoderms). National Museum of Natural History, Smithsonian Institution, Washington D.C
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Grazing by the Sea Urchins Arbacia Lixula L. and Paracentrotus Lividus Lam. in the Northwest Mediterranean
Journal of Experimental Marine Biology and Ecology, L 241 (1999) 81±95 Grazing by the sea urchins Arbacia lixula L. and Paracentrotus lividus Lam. in the Northwest Mediterranean Fabio Bulleri, Lisandro Benedetti-Cecchi* , Francesco Cinelli Dipartimento di Scienze dell'Uomo e dell'Ambiente via A. Volta 6, 56126 Pisa, Italy Received 2 October 1998; received in revised form 12 April 1999; accepted 5 May 1999 Abstract The sea urchins Arbacia lixula and Paracentrotus lividus are common on shallow subtidal reefs in the Mediterranean. Previous studies on the ecology of these species reported that P. lividus is generally more abundant on horizontal or gently sloping substrata, where it forages mainly on erect algae. In contrast, A. lixula is more common on vertical substrata and it is considered a main grazer of encrusting coralline algae. Observations on some rocky shores in the Ligurian sea indicated that P. lividus occurs mainly in crevices at the bottom of the vertical walls, and that neither species is present on horizontal or sub-horizontal substrata. In this study we investigated the distribution and abundance of the two species of sea urchins on vertical substrata at different spatial scales and through time. A ®eld experiment was used to test whether A. lixula constrained the distribution of P. lividus on vertical substrata, and to test for the predicted differences in the effects of the 2 species on assemblages of algae and invertebrates. Four treatments were used: (1) control (sea urchins left untouched); (2) A. lixula removed, P. lividus present; (3) A. lixula present, P. lividus removed, and (4) both species removed. -
Biscuit Clypeaster Subdepressus (Echinodermata: Clypeasteroida)
Embryonic, Larval, and Juvenile Development of the Sea Biscuit Clypeaster subdepressus (Echinodermata: Clypeasteroida) Bruno C. Vellutini1,2*, Alvaro E. Migotto1,2 1 Centro de Biologia Marinha, Universidade de Sa˜o Paulo, Sa˜o Sebastia˜o, Sa˜o Paulo, Brazil, 2 Departamento de Zoologia, Instituto de Biocieˆncias, Universidade de Sa˜o Paulo, Sa˜o Paulo, Sa˜o Paulo, Brazil Abstract Sea biscuits and sand dollars diverged from other irregular echinoids approximately 55 million years ago and rapidly dispersed to oceans worldwide. A series of morphological changes were associated with the occupation of sand beds such as flattening of the body, shortening of primary spines, multiplication of podia, and retention of the lantern of Aristotle into adulthood. To investigate the developmental basis of such morphological changes we documented the ontogeny of Clypeaster subdepressus. We obtained gametes from adult specimens by KCl injection and raised the embryos at 260C. Ciliated blastulae hatched 7.5 h after sperm entry. During gastrulation the archenteron elongated continuously while ectodermal red-pigmented cells migrated synchronously to the apical plate. Pluteus larvae began to feed in 3 d and were *20 d old at metamorphosis; starved larvae died 17 d after fertilization. Postlarval juveniles had neither mouth nor anus nor plates on the aboral side, except for the remnants of larval spicules, but their bilateral symmetry became evident after the resorption of larval tissues. Ossicles of the lantern were present and organized in 5 groups. Each group had 1 tooth, 2 demipyramids, and 2 epiphyses with a rotula in between. Early appendages consisted of 15 spines, 15 podia (2 types), and 5 sphaeridia. -
Geological-Geomorphological and Paleontological Heritage in the Algarve (Portugal) Applied to Geotourism and Geoeducation
land Article Geological-Geomorphological and Paleontological Heritage in the Algarve (Portugal) Applied to Geotourism and Geoeducation Antonio Martínez-Graña 1,* , Paulo Legoinha 2 , José Luis Goy 1, José Angel González-Delgado 1, Ildefonso Armenteros 1, Cristino Dabrio 3 and Caridad Zazo 4 1 Department of Geology, Faculty of Sciences, University of Salamanca, 37008 Salamanca, Spain; [email protected] (J.L.G.); [email protected] (J.A.G.-D.); [email protected] (I.A.) 2 GeoBioTec, Department of Earth Sciences, NOVA School of Science and Technology, Universidade NOVA de Lisboa, Caparica, 2829-516 Almada, Portugal; [email protected] 3 Department of Stratigraphy, Faculty of Geology, Complutense University of Madrid, 28040 Madrid, Spain; [email protected] 4 Department of Geology, Museo Nacional de Ciencias Naturales, 28006 Madrid, Spain; [email protected] * Correspondence: [email protected]; Tel.: +34-923294496 Abstract: A 3D virtual geological route on Digital Earth of the geological-geomorphological and paleontological heritage in the Algarve (Portugal) is presented, assessing the geological heritage of nine representative geosites. Eighteen quantitative parameters are used, weighing the scientific, didactic and cultural tourist interest of each site. A virtual route has been created in Google Earth, with overlaid georeferenced cartographies, as a field guide for students to participate and improve their learning. This free application allows loading thematic georeferenced information that has Citation: Martínez-Graña, A.; previously been evaluated by means of a series of parameters for identifying the importance and Legoinha, P.; Goy, J.L.; interest of a geosite (scientific, educational and/or tourist). The virtual route allows travelling from González-Delgado, J.A.; Armenteros, one geosite to another, interacting in real time from portable devices (e.g., smartphone and tablets), I.; Dabrio, C.; Zazo, C. -
State of the Environment Rocky Shore Monitoring Report 2015-2017
State of the Environment Rocky Shore Monitoring Report 2015-2017 Technical Report 2017-79 Taranaki Regional Council Private Bag 713 ISSN: 1178-1467 (Online) STRATFORD Document: 1845984 (Word) Document: 1918743 (Pdf) October 2017 Executive summary Section 35 of the Resource Management Act 1991 requires local authorities to undertake monitoring of the region’s environment, including land, air, marine and freshwater. The rocky shore component of the State of the Environment Monitoring (SEM) programme for Taranaki was initiated by the Taranaki Regional Council in the 1994-1995 monitoring year and has subsequently continued each year. This report covers the state and trends of intertidal hard shore communities in Taranaki. As part of the SEM programme, six representative reef sites were monitored twice a year (spring and summer surveys) using a fixed transect, random quadrat survey design. For each survey, a 50 m transect was laid parallel to the shore and substrate cover, algal cover and animal cover/abundance in 25 x 0.25 m2 random quadrats were quantified. Changes in the number of species per quadrat (species richness) and Shannon-Wiener index per quadrat (diversity) were assessed at the six reef sites over the 23 years of the SEM programme (spring 1994 to summer 2017). Of the six sites surveyed, the intertidal communities at Manihi (west Taranaki) were the most species rich (median = 19.4 species per quadrat) and diverse (median Shannon Wiener index = 1.05 per quadrat) due to the low supply of sand and the presence of pools that provided a stable environment with many ecological niches. The intertidal communities at Waihi (south Taranaki) were the least species rich (median = 11.5 species per quadrat) and diverse (median Shannon Wiener index = 0.84 per quadrat) due to the high energy wave environment, lack of stable habitat and periodic sand inundation. -
Diversity and Phylogeography of Southern Ocean Sea Stars (Asteroidea)
Diversity and phylogeography of Southern Ocean sea stars (Asteroidea) Thesis submitted by Camille MOREAU in fulfilment of the requirements of the PhD Degree in science (ULB - “Docteur en Science”) and in life science (UBFC – “Docteur en Science de la vie”) Academic year 2018-2019 Supervisors: Professor Bruno Danis (Université Libre de Bruxelles) Laboratoire de Biologie Marine And Dr. Thomas Saucède (Université Bourgogne Franche-Comté) Biogéosciences 1 Diversity and phylogeography of Southern Ocean sea stars (Asteroidea) Camille MOREAU Thesis committee: Mr. Mardulyn Patrick Professeur, ULB Président Mr. Van De Putte Anton Professeur Associé, IRSNB Rapporteur Mr. Poulin Elie Professeur, Université du Chili Rapporteur Mr. Rigaud Thierry Directeur de Recherche, UBFC Examinateur Mr. Saucède Thomas Maître de Conférences, UBFC Directeur de thèse Mr. Danis Bruno Professeur, ULB Co-directeur de thèse 2 Avant-propos Ce doctorat s’inscrit dans le cadre d’une cotutelle entre les universités de Dijon et Bruxelles et m’aura ainsi permis d’élargir mon réseau au sein de la communauté scientifique tout en étendant mes horizons scientifiques. C’est tout d’abord grâce au programme vERSO (Ecosystem Responses to global change : a multiscale approach in the Southern Ocean) que ce travail a été possible, mais aussi grâce aux collaborations construites avant et pendant ce travail. Cette thèse a aussi été l’occasion de continuer à aller travailler sur le terrain des hautes latitudes à plusieurs reprises pour collecter les échantillons et rencontrer de nouveaux collègues. Par le biais de ces trois missions de recherches et des nombreuses conférences auxquelles j’ai activement participé à travers le monde, j’ai beaucoup appris, tant scientifiquement qu’humainement. -
Males and Females Gonad Fatty Acids of the Sea Urchins and (Echinodermata) Inés Martínez-Pita, Francisco J
Males and females gonad fatty acids of the sea urchins and (Echinodermata) Inés Martínez-Pita, Francisco J. García, María-Luisa Pita To cite this version: Inés Martínez-Pita, Francisco J. García, María-Luisa Pita. Males and females gonad fatty acids of the sea urchins and (Echinodermata). Helgoland Marine Research, Springer Verlag, 2009, 64 (2), pp.135-142. 10.1007/s10152-009-0174-7. hal-00535207 HAL Id: hal-00535207 https://hal.archives-ouvertes.fr/hal-00535207 Submitted on 11 Nov 2010 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Helgol Mar Res (2010) 64:135–142 DOI 10.1007/s10152-009-0174-7 ORIGINAL ARTICLE Males and females gonad fatty acids of the sea urchins Paracentrotus lividus and Arbacia lixula (Echinodermata) Inés Martínez-Pita · Francisco J. García · María-Luisa Pita Received: 25 May 2009 / Revised: 18 September 2009 / Accepted: 24 September 2009 / Published online: 15 October 2009 © Springer-Verlag and AWI 2009 Abstract The aim of this study was to analyze male and 20:5n-3 and 22:6n-3 found in males and females of the female gonad fatty acids of two sea urchin species, Para- Mediterranean specimens compared to those of the Atlantic centrotus lividus and Arbacia lixula, from the south coast coast. -
SI Appendix for Hopkins, Melanie J, and Smith, Andrew B
Hopkins and Smith, SI Appendix SI Appendix for Hopkins, Melanie J, and Smith, Andrew B. Dynamic evolutionary change in post-Paleozoic echinoids and the importance of scale when interpreting changes in rates of evolution. Corrections to character matrix Before running any analyses, we corrected a few errors in the published character matrix of Kroh and Smith (1). Specifically, we removed the three duplicate records of Oligopygus, Haimea, and Conoclypus, and removed characters C51 and C59, which had been excluded from the phylogenetic analysis but mistakenly remain in the matrix that was published in Appendix 2 of (1). We also excluded Anisocidaris, Paurocidaris, Pseudocidaris, Glyphopneustes, Enichaster, and Tiarechinus from the character matrix because these taxa were excluded from the strict consensus tree (1). This left 164 taxa and 303 characters for calculations of rates of evolution and for the principal coordinates analysis. Other tree scaling methods The most basic method for scaling a tree using first appearances of taxa is to make each internal node the age of its oldest descendent ("stand") (2), but this often results in many zero-length branches which are both theoretically questionable and in some cases methodologically problematic (3). Several methods exist for modifying zero-length branches. In the case of the results shown in Figure 1, we assigned a positive length to each zero-length branch by having it share time equally with a preceding, non-zero-length branch (“equal”) (4). However, we compared the results from this method of scaling to several other methods. First, we compared this with rates estimated from trees scaled such that zero-length branches share time proportionally to the amount of character change along the branches (“prop”) (5), a variation which gave almost identical results as the method used for the “equal” method (Fig. -
PUBLICATIONS by JAMES SPRINKLE 1965 -- Sprinkle, James
PUBLICATIONS BY JAMES SPRINKLE 1965 -- Sprinkle, James. 1965. Stratigraphy and sedimentary petrology of the lower Lodgepole Formation of southwestern Montana. M.I.T. Department of Geology and Geophysics, unpublished Senior Thesis, 29 p. (see #56 and 66 below) 1966 1. Sprinkle, James and Gutschick, R. C. 1966. Blastoids from the Sappington Formation of southwest Montana (Abst.). Geological Society of America Special Paper 87:163-164. 1967 2. Sprinkle, James and Gutschick, R. C. 1967. Costatoblastus, a channel fill blastoid from the Sappington Formation of Montana. Journal of Paleon- tology, 41(2):385-402. 1968 3. Sprinkle, James. 1968. The "arms" of Caryocrinites, a Silurian rhombiferan cystoid (Abst.). Geological Society of America Special Paper 115:210. 1969 4. Sprinkle, James. 1969. The early evolution of crinozoan and blastozoan echinoderms (Abst.). Geological Society of America Special Paper 121:287-288. 5. Robison, R. A. and Sprinkle, James. 1969. A new echinoderm from the Middle Cambrian of Utah (Abst.). Geological Society of America Abstracts with Programs, 1(5):69. 6. Robison, R. A. and Sprinkle, James. 1969. Ctenocystoidea: new class of primitive echinoderms. Science, 166(3912):1512-1514. 1970 -- Sprinkle, James. 1970. Morphology and Evolution of Blastozoan Echino- derms. Harvard University Department of Geological Sciences, unpublished Ph.D. Thesis, 433 p. (see #8 below) 1971 7. Sprinkle, James. 1971. Stratigraphic distribution of echinoderm plates in the Antelope Valley Limestone of Nevada and California. U.S. Geological Survey Professional Paper 750-D (Geological Survey Research 1971):D89-D98. 1973 8. Sprinkle, James. 1973. Morphology and Evolution of Blastozoan Echino- derms. Harvard University, Museum of Comparative Zoology Special Publication, 283 p. -
Wilson's Creek National Battlefield Geologic Resources Inventory
Geologic Resources Inventory Scoping Summary Wilson’s Creek National Battlefield, Missouri Geologic Resources Division Prepared by John Graham National Park Service June 8, 2011 US Department of the Interior The Geologic Resources Inventory (GRI) provides each of 270 identified natural area National Park System units with a geologic scoping meeting and summary (this document), a digital geologic map, and a Geologic Resources Inventory report. The purpose of scoping is to identify geologic mapping coverage and needs, distinctive geologic processes and features, resource management issues, and monitoring and research needs. Geologic scoping meetings generate an evaluation of the adequacy of existing geologic maps for resource management, provide an opportunity to discuss park-specific geologic management issues, and if possible include a site visit with local experts. The National Park Service held a GRI scoping meeting for Wilson’s Creek National Battlefield on April 5, 2011 at park headquarters. Jason Kenworthy (NPS Geologic Resources Division) presented an overview of the Geologic Resources Inventory and led the discussion regarding geologic issues, features, and processes at Wilson’s Creek National Battlefield. After Bill Duley (Missouri Department of Natural Resources) presented an overview of Missouri’s geology, Tim Connors (NPS Geologic Resources Division) facilitated the discussion of map coverage at the park. In addition to Bill Duley, other geologists who were familiar with the local geology included Jerry Prewett (Missouri Department of Natural Resources) and Doug Gouzie (Missouri State University). Participants at the meeting also included Superintendent Ted Hillmer and Resource Manager Gary Sullivan. In the afternoon, Gary Sullivan led the participants on a field trip throughout the park. -
Distribution of the Middle Ordovician Copenhagen Formation and Its Trilobites in Nevada
Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada By REUBEN JAMES ROSS, JR., and FREDERICK C. SHAW GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Descriptions of Middle Ordovician trilobites belonging to 21 genera contribute to correlations between similar strata in Nevada) California) and 0 klahoma UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. lVIOR TON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 78-190301 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 70 cents (paper cover) Stock Number 2401-2109 CONTENTS Page Page Abstract ______________________________ -------------------------------------------------- 1 Descriptions of trilobites __________________________________________________ _ 14 Introduction ________________________________________________________________________ _ 1 Genus T1·iarth1·us Green, 1832 .... ------------------------------ 14 Previous investigations _____________________________________________ _ 1 Genus Carrickia Tripp, 1965 ____________________________________ _ 14 Acknowledgments-------------------------------------------------------· 1 Genus Hypodicranotus Whittington, 1952 _____________ _ 15 Geographic occurrences of the Copenhagen Genus Robergia Wiman, 1905·---------------------------------- -
For Peer Review
Page 1 of 40 Geological Journal Page 1 of 32 1 2 3 Neogene echinoids from the Cayman Islands, West Indies: regional 4 5 6 implications 7 8 9 10 1 2 3 11 STEPHEN K. DONOVAN *, BRIAN JONES and DAVID A. T. HARPER 12 13 14 15 1Department of Geology, Naturalis Biodiversity Center, Leiden, the Netherlands 16 17 2Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Canada, T6G 2E3 18 For Peer Review 19 3 20 Department of Earth Sciences, Durham University, Durham, UK 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 *Correspondence to: S. K. Donovan, Department of Geology, Naturalis Biodiversity Center, 49 50 Darwinweg 2, 2333 CR Leiden, the Netherlands. 51 52 E-mail: [email protected] 53 54 55 56 57 58 59 60 http://mc.manuscriptcentral.com/gj Geological Journal Page 2 of 40 Page 2 of 32 1 2 3 The first fossil echinoids are recorded from the Cayman Islands. A regular echinoid, Arbacia? sp., the 4 5 spatangoids Brissus sp. cf. B. oblongus Wright and Schizaster sp. cf. S. americanus (Clark), and the 6 7 clypeasteroid Clypeaster sp. are from the Middle Miocene Cayman Formation. Test fragments of the 8 9 mellitid clypeasteroid, Leodia sexiesperforata (Leske), are from the Late Pleistocene Ironshore 10 11 Formation. Miocene echinoids are preserved as (mainly internal) moulds; hence, all species are left 12 13 14 in open nomenclature because of uncertainties regarding test architecture. -
Pennsylvanian Crinoids of New Mexico
Pennsylvanian crinoids of New Mexico Gary D. Webster, Department of Geology, Washington State University, Pullman, WA 99164, and Barry S. Kues, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131 Abstract north of Alamogordo; (2) Morrowan and groups present on the outcrop were sam- Atokan specimens from the La Pasada For- pled, often repeatedly over the years. Crinoids from each of the five Pennsylvanian mation in the Santa Fe area; and (3) a mid- These collections, reposited at the Univer- epochs are described from 26 localities in dle Desmoinesian species from the Alami- sity of New Mexico (UNM), testify to the New Mexico. The crinoid faunas occupied tos Formation, north of Pecos. Bowsher rarity of identifiable crinoid cups and diverse shelf environments around many intermontane basins of New Mexico during and Strimple (1986) described 15 late crowns in these assemblages, even in cases the Pennsylvanian. The crinoids described Desmoinesian or early Missourian crinoid where crinoid stem elements are common. here include 29 genera, 39 named species, species (several not named) from near the In nearly all collections, crinoid cups rep- and at least nine unnamed species, of which top of the Bug Scuffle Member of the Gob- resent only a small fraction of 1% of the one genus and 15 named species are new. bler Formation south of Alamogordo in the total identifiable specimens. The only This report more than doubles the number of Sacramento Mountains. Kietzke (1990) exception is the fauna from the Missourian previously known Pennsylvanian crinoid illustrated a Desmoinesian microcrinoid Sol se Mete Member, Wild Cow Formation, species from New Mexico; 17 of these species from the Flechado Formation near Talpa.