. I 41 ~:;~.. ,,:i, ~""".' to\\y 1. l'.-

Similar documents
Technical Reports Nos. 142, 143, 144, 145, 146, 147, 148, and 149. and

Bulletin Zoölogisch Museum

CHAPTER IV THE RELATIONSHIP BETWEEN OCEANOGRAPHY AND METEOROLOGY

A note on the lectotype of Ammonites galicianus FAVRE, 1869

12. ARCHAEOMONADS AS EOCENE AND OLIGOCENE GUIDE FOSSILS IN MARINE SEDIMENTS

Chapter 02 The Sea Floor

History of Plate Tectonics

Chapter 20. Plate Tectonics. Scientific Method. This is a repeatable measurement or experiment. One or more possible explanations to link observations

Small area of the ocean that is partially surrounded by land. The Ocean Basins. Three Major Oceans. Three Major Oceans. What is a SEA?

TWO NEW FOSSIL DEMOSPONGES FROM WES ONGUL ISLAND, LUTZOW-HOLM BAY, ANTA.

Two new species of Cryptophagus HERBST, 1792 (Coleoptera: Cryptophagidae) from New Mexico (United States of America)

Chapter 20. Plate Tectonics

Sediment Acoustics LONG-TERM GOAL

60% water. Big Bang: 14,000 millions years ago The Earth originated about 4,500 millions years ago its orbit allows water to exist in a liquid state!

Essentials of Oceanography Eleventh Edition

First Record of Boccardiella ligerica (Ferronniere) (Polychaeta: Spionidae) from the East Coast of North America

I. Earth s Layers a. Crust: Earth s outside layer. Made of mostly rock. i. Continental: er; made of mostly granite, forms the continents and shallow

On the world-wide circulation of the deep water from the North Atlantic Ocean

2015 Record breaking temperature anomalies

Geography IIN. Exploration of Polymetallic Nodules

READING QUESTIONS: Chapter 11, Plate Tectonics GEOL 131 Fall pts

SEDIMENTARY ROCKS FROM THE CONTINENTAL SHELF AND SLOPE OFF THE CENTRAL COAST OF OREGON. By Neil J. Maloney and John V. Byrne

Introduction to Oceanography. Chapter 2: Plate Tectonics Overview

The Growth of Oceanography

Plate Tectonics. entirely rock both and rock

1. Name at least one place that the mid-atlantic Ridge is exposed above sea level.

OS 1 The Oceans Fall 2007

Crustal Activity. Plate Tectonics - Plates - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones

Diversity, Change and Continuity. History of Life

Geology Project 1 Plate Motions

ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017

CRUSTAL STRUCTURE AND SURFACE-WAVE DISPERSION. PART II SOLOMON ISLANDS EARTHQUAKE OF JULY 29, 1950* By MAURICE EWING and FRANK PRESS

Plate Tectonics. In 1912 Alfred Wegener ( ) proposed that: the continents were once compressed into a single protocontinent which he called

16. TRIPYLEAN RADIOLARIANS FROM THE SUBANTARCTIC ATLANTIC 1. Hsin Yi Ling 2

AGY 514 Marine Geology COURSE PARTICULARS COURSE INSTRUCTORS COURSE DESCRIPTION COURSE OBJECTIVES

Alfred Wegener gave us Continental Drift. Fifty years later...

Grand Unifying Theory of everything... for the Geosciences, at least!

Lab Activity Mid-Atlantic Ridge

Science in the News - Plate Tectonics 1. Story

NATURAL SCIENCES & TECHNOLOGY RESOURCE PACK GRADE 4 TERM 4

Our Dynamic Earth Unit Unit 5

3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.

ACOUSTIC ASSESSMENT OF BAITFISH STOCKS IN PUGET SOUND. Final Report Service Contract No. 501 Washington Department of Fisheries 1973

Buried nodules from the Central Indian Ocean Basin

HARMONIC CLOSE-TO-CONVEX MAPPINGS

by the Bartlett Expedition near the Azores at 37 13'18" N 28 lj'j, 30" W, proved that a related form existed during the Pleistocene ice ages.

Introduction To Plate Tectonics Evolution. (Continents, Ocean Basins, Mountains and Continental Margins)

From VOA Learning English, this is SCIENCE IN THE NEWS, in Special English. I m Kelly Jean Kelly.

Map Skills Test. 1. What do we call a person who makes maps? a. mapographer b. cartographer c. geologist d. archaeologist

Bi/GE105: Evolution Homework 2 Due Date: Tuesday, January 21, 2013

PLATE TECTONICS THEORY

El Niño Seasonal Weather Impacts from the OLR Event Perspective

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

Plate Tectonics GEOL 101 Lecture 22 How Are Mountains Built?

12. The diagram below shows the collision of an oceanic plate and a continental plate.

Title The Fauna of Akkeshi Bay : XXII. Phoronidea (With 2. Author(s)Uchida, Tohru; Iwata, Fumio

Almost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean.

The Sea Floor. Chapter 2

Evidence for Continental Drift and The Theory of Plate Tectonics

Marine benthic habitats of the George V Land shelf, Antarctica

General Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea

Inside Earth Review Packet

Chapter Overview. Evidence for Continental Drift. Plate Tectonics. Evidence for Continental Drift. Evidence for Continental Drift 9/28/2010

Two representatives of the genus Mindarus (Homoptera, Aphidoidea, Mindaridae) in Baltic amber

Impacts of Deep Sea Mining. Phil Weaver Seascape Consultants Romsey, UK

Chapter Two. Figure 02_02. Geography of the Ocean Basins. The Sea Floor

Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel Nr. 14

First Record of the Rudist Bivalve Mitrocaprina tschoppi (Palmer) from the Maastrichtian of Jamaica

Introduction to Geology Spring 2008

Table of Contents. Introduction 4. Chapter 1 Research and the Deep Oceans 6. Chapter 2 Physical Characteristics of the Ocean 10

What does Evolution Explain?

Plate Tectonics Practice Test

Full file at CHAPTER 2 The Way the Earth Works: Plate Tectonics

The Moving Story of Plate Tectonics

CONTENT. A. Changes in the Crust Facts Changes Construction and Destruction. B. Continental Drift What is it? Evidence

Physiography Ocean Provinces p. 1 Dimensions p. 1 Physiographic Provinces p. 2 Continental Margin Province p. 2 Deep-Ocean Basin Province p.

BIOLOGY. General Instructions. James Ruse Agricultural High School. Total marks for this paper: 61

PROCESSING RECORD SCRIPPS INSTITUTION OF OCEANOGRAPHY ARCHIVES. Scripps Institution of Oceanography. Office of the Director (Sverdrup)

Downloaded from

NAME Lab TA. Introduction to Oceanography, EPSS15 Practice Lecture Exam #1, Fall 2017 Exam#

ISSUED BY KENDRIYA VIDYALAYA - DOWNLOADED FROM

Tezula funebralis Shell height variance in the Intertidal zones

SMART NOTES ON INDIAN GEOGRAPHY - 1

Full file at

Introduction. Learning Outcomes. Exercise 1 Plates and Plate Boundaries. GEO 101 The Solid Earth Week 2 Plate Tectonics Lab (25 points)

Delta-lognormal linear models applied to standardised CPUE abundance indices (1994 to 2003) for orange roughy off Namibia.

Out of the doldrums: Campylaspis stephenseni Just, 1970 revived (Crustacea, Cumacea, Nannastacidae)

Questions and Topics

Continental Drift. Wegener theory that the crustal plates are moving and once were a super continent called Pangaea.

Tips for Success on a Test

11. THE OBLIQUE SEISMIC EXPERIMENT ON DEEP SEA DRILLING PROJECT LEG 70 1


Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent

EARTH S INTERIOR, EVIDENCE FOR PLATE TECTONICS AND PLATE BOUNDARIES

Magnetism. Geology. Size and Shape Relationships

Department of Geography is a Government Depository for maps. 3bP. 3aP. 3bP. Area needs improvement. 3bP. 3bP. 2bP. 3bP. 3bP. 3aP

New Chemistry of Gold

Chapter Nineteen: Changing Earth

Directed Reading. Section: The Water Planet. surface is called the a. Earth s ocean. b. Pacific Ocean. c. salt-water ocean. d. global ocean.

Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building

Transcription:

~:;~.. t,,:i,,. ~""".'. I 41 to\\y 1 l'.- 05

UNIVERSITY OF WASHINGTON DEPARTMENT OF OOEANOORAPHY Seattle, Washington 98105 Technical Reports Nos. 136, 137, 138, 139, 140, and 141 A COMPILATION OF ARTICLES REPORTING Im>EARCH SPONSORED BY --. THE OFFICE OF NAVAL RESFARCH Office of Naval Research Contracts Nonr-477(10) and Nonr-477(37) Project NR 083 012 Reference M66-1 January 1966 Reproduction in whole or in part is permitted for any purpose of the United States Government

iii ARTICLES REPORTmG RESEARCH SPONSORED BY THE OFFICE OF NAVAL RESEARCH Technical Report No. 136 ON THE VERTICAL DISTRIBUTION OF ZOO~ON IN THE SEA, by K. Banse. pp. 55-125 in Progress in OCeanography, vol. II (Mary Sears, ed.). Pergamon Press, London. 1964. Technical Report No. 137 SYNONYMS OF PRa.rODORVILLEA EGENA (EHLERS) (EUNICIDAE, POLYCHAETA), by K. Banse and G. Hartmann-SchrOder. Proceedings of the Biological Society of' Washington, 77:241-242. 30 December 1964. Technical Report No. 138 THE INFLUENCE OF VARIABLE DEPrH ON STEADY ZONAL BARarROPIC FLGl, by Gene H. Porter and Maurice Rattray, Jr. Deutsche Hydrographische Zeitschrift, 17(4):164-174. 1964. Technical Report No. 139 THE MESOPEIAGIC CARIDEAN SHRIMP NOTOOTCHUS JAPONICUS BATE IN THE NORTH FASTERN PACIFIC, by Belle A. Stevens and Fenner A. Chace, Jr. Crustaceana,!!(pt. 3):277-284. 1965. Technical Report No. 140 CARBONIFEROUS GIACIAL ROCKS FRCM THE WERRIE BASIN, NEW SOUTH WALES, AUSTRALIA, by Jolm T. Whetten. Geological Society of' America Bulletin, 76:43-56. January 1965. Technical Report No. 141 THE ORIGIN OF MANGANESE NODULES ON THE OCEAN FLOOR, by Enrico Bonatti and Y. Rammohanroy Nayudu. American Journal of Science, 263:17-39. January 1965. -

Vol. 77, pp. 241-242 30 December 1964 PROCEEDINGS OF THE BIOLOGICAL SOCIETY OF WASHINGTON ț SYNONYMS OF PROTODORVILLEA EGENA (EHLERS) (EUNICIDAE, POLYCHAETA) 1 By K. BANSE AND G. HARTMANN-SCHRODER Department of Oceanography, University of Washington, and Zoologisches Staatsinstitut und Zoologisches Museum, Universitiit Hamburg Since we may not have the opportunity to incorporate this note in an appropriate larger paper, we wish to report that we believe now that Dorvillea mandapamae and D. graciloides, described by us, are synonyms of Stauronereis egena Ehlers (1913) from SimonstoWD, South Africa. Following Pettibone (1961) the species is called Protodorvillea egena. Stauronereis egena Ehlers, 1913, p. 501, pl. 35, figs. 1-6. Stauronereis egena Augener, 1917, partim, p. 379. Dorvillea egena Day, 1957, p. 95. Dorvillea mandapamae Banse, 1959, p. 166, fig. 1. Dorvillea graciloides Hartmann-Schroder, 1960, p. 117, figs. 169-172. Protodorvillea egena Pettibone, 1961, p. 180. Protodorvillea egena Day, 1963, p. 412. There are minor deviations in the various descriptions which do not justify maintaining of separate species: the number and position of eyes differ, but the variability of the character during development has been shown for D. mandapamae. The anterior margin of the first segment of the single known specimen of D. graciloide.s is not straight as in the other forms. It is not known whether this is due to contraction or whether its represents nuchal organs not described for any other Protodoroillea species. Variations in relative lengths of the first and the second segments may as well be due to variable states of contraction. None of the later authors has seen two aciculae supporting the two bundles of setae according to Ehlers (1913). A new inspection of a paratype of D. mandapamae (Museum Hamburg No. V.13021) shows that the inner margins of the prongs of the forked setae are not smooth but are feathered (Fig. 1) as in P. egena; Augener (1917) had already 1 Contribution No. 306 from the Department of Oceanography, University of Washington. prepared with partial support by Contract Nonr-477(10), Project NR 083 012, with the Office of Naval Research. We acknowledge also helpful correspondence with Professor J. H. Day in Cape Town. 27-PROC. BIOL. SOC. WASH., VOL. 77, 1964 (241) univ::rs:ty OF WASHINGTON DEPA~TM::NT OF OCEANOGRAPHY TECHNICAL REPORT NO. 13'1

242 Proceedings of the Biological Society of Washington E E q o FIG. 1. Tip of forked seta from juvenile specimen from Mandapam. suggested that Fig. 4 of Ehlers (1913) represents the forked seta but that the caption is wrong. D. graciloides seems to possess smooth forked setae. While some compound bristles with blades having tridentate tips were reported for D. graciloides, the blades of D. mandapamae appear as bidentate under looo-fold magnification. Day (1963) has observed bidentate blades in new material of P. egeoo from the type locality, so Ehlers may have erred in reporting blades with pointed tips. Augener (1917) saw the type of P. egena and added to the original description. However, his own material from Southwest Africa does not represent this species, as also pointed out by Day (1963). Both the single specimens from Swakopmund (Museum Hamburg No. V.8792) and from Liideritzbucht (No. V.8753) belong to Stauronerei.s sensu Pettibone (1961), and seem to be identical with the specimens reported as S. neglecta from many places in South Africa. LITERATURE CITED AucENER, H. 1917. Polychaeta. pp. 65-625 in Michaelsen, W. (Ed.) Beitrage zur Kenntnis der Meeresfauna Westafrikas, 2. BANSE, K. 1959. On marine polychaeta from Mandapam (South India). J. Mar. BioI. Ass. India, 1 (2): 165-177. DAY, J. H. 1957. The polychaet fauna of South Africa. 4. New species and records from Natal and Mo~ambique. Ann. Natal Mus., 14 (1): 59-129. 1963. The polychaete fauna of South Africa. 8. New species and records from grab samples and dredgings. Bull. Brit. Mus. (Nnt. Hist.), 10 (7): 383-445. EHLERS, E. 1913. Die Polychaeten-Sammlungen der Deutschen Siidpolar-Expedition 1901-1903. Dtsch. Siidpolar-Exped., 13: 397-602. HARTMANN-SCHRODER, G. 1960. Polychneten nus dem Roten Meer. Kieler Meeresforsch., 16 (1): 69-125. PETTIBONE, M. 1961. New species of polychaetous WOnDS from the Atlantic Ocean, with a revision of the Dorvilleidae. Proc. BioI. Soc. Wash., 74: 167-185. -...