New Distribution Records of Reptant Decapod Crustacea, ^^ Including Descriptions of Three New Species of Pagurus, from the Water
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Examples of Sea Sponges
Examples Of Sea Sponges Startling Amadeus burlesques her snobbishness so fully that Vaughan structured very cognisably. Freddy is ectypal and stenciling unsocially while epithelial Zippy forces and inflict. Monopolistic Porter sailplanes her honeymooners so incorruptibly that Sutton recirculates very thereon. True only on water leaves, sea of these are animals Yellow like Sponge Oceana. Deeper dives into different aspects of these glassy skeletons are ongoing according to. Sponges theoutershores. Cell types epidermal cells form outer covering amoeboid cells wander around make spicules. Check how These Beautiful Pictures of Different Types of. To be optimal for bathing, increasing with examples of brooding forms tan ct et al ratios derived from other microscopic plants from synthetic sponges belong to the university. What is those natural marine sponge? Different types of sponges come under different price points and loss different uses in. Global Diversity of Sponges Porifera NCBI NIH. Sponges EnchantedLearningcom. They publish the outer shape of rubber sponge 1 Some examples of sponges are Sea SpongeTube SpongeVase Sponge or Sponge Painted. Learn facts about the Porifera or Sea Sponges with our this Easy mountain for Kids. What claim a course Sponge Acme Sponge Company. BG Silicon isotopes of this sea sponges new insights into. Sponges come across an incredible summary of colors and an amazing array of shapes. 5 Fascinating Types of what Sponge Leisure Pro. Sea sponges often a tube-like bodies with his tiny pores. Sponges The World's Simplest Multi-Cellular Creatures. Sponges are food of various nudbranchs sea stars and fish. Examples of sponges Answers Answerscom. Sponges info and games Sheppard Software. -
British Columbia Regional Guide Cat
National Marine Weather Guide British Columbia Regional Guide Cat. No. En56-240/3-2015E-PDF 978-1-100-25953-6 Terms of Usage Information contained in this publication or product may be reproduced, in part or in whole, and by any means, for personal or public non-commercial purposes, without charge or further permission, unless otherwise specified. You are asked to: • Exercise due diligence in ensuring the accuracy of the materials reproduced; • Indicate both the complete title of the materials reproduced, as well as the author organization; and • Indicate that the reproduction is a copy of an official work that is published by the Government of Canada and that the reproduction has not been produced in affiliation with or with the endorsement of the Government of Canada. Commercial reproduction and distribution is prohibited except with written permission from the author. For more information, please contact Environment Canada’s Inquiry Centre at 1-800-668-6767 (in Canada only) or 819-997-2800 or email to [email protected]. Disclaimer: Her Majesty is not responsible for the accuracy or completeness of the information contained in the reproduced material. Her Majesty shall at all times be indemnified and held harmless against any and all claims whatsoever arising out of negligence or other fault in the use of the information contained in this publication or product. Photo credits Cover Left: Chris Gibbons Cover Center: Chris Gibbons Cover Right: Ed Goski Page I: Ed Goski Page II: top left - Chris Gibbons, top right - Matt MacDonald, bottom - André Besson Page VI: Chris Gibbons Page 1: Chris Gibbons Page 5: Lisa West Page 8: Matt MacDonald Page 13: André Besson Page 15: Chris Gibbons Page 42: Lisa West Page 49: Chris Gibbons Page 119: Lisa West Page 138: Matt MacDonald Page 142: Matt MacDonald Acknowledgments Without the works of Owen Lange, this chapter would not have been possible. -
3LMANUSCRIPT REPORT SERIES No. 36
DFO - L bra y MPOBibio heque II 1 111111 11 11 11 V I 1 120235441 3LMANUSCRIPT REPORT SERIES No. 36 Some If:eat/viz& 3,5,unamia, Olt the Yacific ettadt of South and ✓ cuith anwitica, T. S. Murty, S. 0. Wigen and R. Chawla Marine Sciences Directorate 975 Department of the Environment, Ottawa Marine Sciences Directorate Manuscript. Report Series No. 36 SOME FEATURES OF TSUNAMIS ON THE PACIFIC COAST OF SOUTH AND NORTH AM ERICA . 5 . Molly S . O. Wigen and R. Chawla 1975 Published by Publie par Environment Environnement Canada Canada I' Fisheries and Service des !Aches Marine Service et des sciences de la mer Office of the Editor Bureau du fiedacteur 116 Lisgar, Ottawa K1 A Of13 1 Preface This paper is to be published in Spanish in the Proceedings of the Tsunami Committee XVII Meeting, Lima, Peru 20-31 Aug. 1973, under the International Association of Seismology and Physics of the Earth Interior. 2 Table of Contents Page Abstract - Resume 5 1. Introduction 7 2. Resonance characteristics of sonic inlets on the Pacific Coast of Soulh and North America 13 3. Secondary undulations 25 4. Tsunami forerunner 33 5. Initial withdrawal of water 33 6. Conclusions 35 7. References 37 3 4 i Abstract In order to investigate the response of inlets to tsunamis, the resonance characteristics of some inlets on the coast of Chile have been deduced through simple analytical considerations. A comparison is made with the inlets of southeast Alaska, the mainland coast of British Columbia and Vancouver Island. It is shown that the general level of intensif yy of secondary undulations is highest for Vancouver Island inlets, and least for those of Chile and Alaska. -
Crabs and Their Relatives of British Columbia by Josephine Hart 1984 British Columbia Provincial Museum Handbook 40
Crabs and their relatives of British Columbia by Josephine Hart 1984 British Columbia Provincial Museum Handbook 40. Victoria, British Columbia. 267 pp. Extracted from the publication (now out of print) SECTION MACRURA Superfamily Thalassinidea Key to Families 1. Shrimp-like. Integument soft and pleura on abdomen large. Live in burrows……………………………………………………………………………..……….……Axiidae 1. Shrimp-like. Integument soft and pleura small. Live in burrows………………………………………………………………………………………………….2 2. Rostrum distinct, ridged and setose. Eyestalks cylindrical and cornea terminal. Chelipeds subchelate and subequal…………………………………………………………………….Upogebiidae 2. Rostrum minute and smooth. Eyestalks flattened with mid-dorsal corneal pigment or cylindrical without dark pigment. Chelipeds chelate and unequal in size and shape.......Callianassidae Family AXIIDAE The thin-shelled shrimp-like animals in this family are all burrowers and are found from shallow subtidal habitats to great depths. Recently Pemberton, Risk and Buckley (1976) determined that one species found off Nova Scotia makes burrows more than 2.5 m into the substrate. Obviously in abyssal regions the collection of these animals under such circumstances in particularly haphazard. Thus the number of specimens obtained is few and often these are damaged. Four species of this family are known to occur in the waters off British Columbia. All have one or two small hollow knobs of apparently unknown function on the mid-dorsal ridge of the carapace. These species have been assigned to the genera Axiopsis, Calastacus and Calocaris. The definitions of these genera were made when few species had been studied and recent discoveries indicate that the criteria used are not satisfactory. New genera will have to be created and the taxonomy of the Family revised. -
Northisle Copper and Gold Inc
Ministry of Energy, Mines & Petroleum Resources Mining & Minerals Division Assessment Report BC Geological Survey Title Page and Summary TYPE OF REPORT [type of survey(s)]: Archaeological Impact Assessment TOTAL COST: $14,254 AUTHOR(S): Morgan Bartlett, Robbin Chatan, Konstantin Lesnikov SIGNATURE(S): NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): MX-8-271 / December 22, 2011 YEAR OF WORK: 2012 STATEMENT OF WORK - CASH PAYMENTS EVENT NUMBER(S)/DATE(S): 5421553 PROPERTY NAME: Island Copper East Block CLAIM NAME(S) (on which the work was done): Mo 4, Mo 5 COMMODITIES SOUGHT: N/A MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN: 092L 273 MINING DIVISION: Nanaimo NTS/BCGS: 092L/11 / 92L.054 o '" o '" LATITUDE: -127 22 21 LONGITUDE: 50 35 18 (at centre of work) OWNER(S): 1) NorthIsle Copper and Gold Inc. 2) MAILING ADDRESS: #2050-1111 West Georgia Street Vancouver BC V6E 4M3 OPERATOR(S) [who paid for the work]: 1) 2) MAILING ADDRESS: PROPERTY GEOLOGY KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude): Bonanza Volcanics, Quatsino Formation, Karmutsen Formation, Island Plutonic Suite, porphyritic granitoid rocks, granodiorite, andesite, basalt, limestone, Upper Triassic, middle Jurassic, Island Copper Mine REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: AR 2659, 1681, 14393, 15884, 15707, 11460, 15024, 15077, 15367, 16510, 15024, 15077, 15367, 16510, 17368, 32722 Next Page TYPE OF WORK IN EXTENT OF WORK ON WHICH CLAIMS PROJECT COSTS THIS REPORT (IN METRIC UNITS) APPORTIONED (incl. support) -
The Associates of Four Species of Marine Sponges of Oregon and Washington Abstract Approved Redacted for Privacy (Ivan Pratt, Major Professor)
AN ABSTRACT OF THE THESIS OF Edward Ray Long for the M. S. in Zoology (Name) (Degree) (Major) /.,, Date thesis presented ://,/,(//i $» I Ì Ì Title The Associates of Four Species of Marine Sponges of Oregon and Washington Abstract approved Redacted for Privacy (Ivan Pratt, Major Professor) Four species of sponge from the coasts of Oregon and Wash- ington were studied and dissected for inhabitants and associates. All four species differed in texture, composition, and habitat, and likewise, the populations of associates of each species differed, even when samples of two of these species were found adjacent to one another. Generally, the relationships of the associates to the host sponges were of four sorts: 1. Inquilinism or lodging, either accidental or intentional; 2. Predation or grazing; 3. Competition for space resulting in "cohabitation" of an area, i, e. a plant or animal growing up through a sponge; and 4. Mutualism. Fish eggs in the hollow chambers of Homaxinella sp. represented a case of fish -in- sponge inqilinism, which is the first such one reported in the Pacific Ocean and in this sponge. The sponge Halichondria panicea, with an intracellular algal symbiont, was found to emit an attractant into the water, which Archidoris montereyensis followed in behavior experiments in preference to other sponges simultane- ously offered. A total of 6098 organisms, representing 68 species, were found associated with the specimens of Halichondria panic ea with densities of up to 19 organisms per cubic centimeter of sponge tissue. There were 9581 plants and animals found with Microciona prolifera, and 150 with Suberites lata. -
Suberitidae (Demospongiae, Hadromerida) From
Beaufortia INSTITUTE OF TAXONOMIC ZOOLOGY (ZOOLOGICAL MUSEUM) UNIVERSITY OF AMSTERDAM Vol. 43 no. 11 December 31, 1993 Suberitidae (Demospongiae, Hadromerida) from the North Aegean Sea EleniVoultsiadou-Koukoura.*& Rob W. M. van Soest** *Department University ofThessaloniki, 54006 Thessaloniki, Greece **Institute of Taxonomic (Zoological Museum), University ofAmsterdam, P.O.Box 94766, 1090 GTAmsterdam, TheNetherlands Keywords: Sponges, Hadromerida, Suberitidae, North Aegean Sea Abstract Sampling in the North Aegean Sea yielded nine species of the family Suberitidae, four of which, Pseudosuberites sulphureus, P. Suberiles for the fauna ofthe Eastern and three hyalinus, ficus and S. syringella, are new Mediterranean, more, S. carnosus, S. and S. records for the fauna of the Sea. For each of the nine the domuncula, massa, are new Aegean species comments on systematics, as well as geographical and ecological informationis given. A redescription is given of the littleknown species Suberites massa Nardo. A review ofthe distributionof all Mediterranean Suberitidae is also presented, in which it is con- in materialhave been from the Eastern cluded that a further three species not represented our reported Mediterranean, and P. the viz. Laxosuberites ectyoninus, Prosuberites longispina, epiphytum. Six suberitids reported from other parts of Mediterra- nean so far have not been found in the Eastern Mediterranean. INTRODUCTION siadou-Koukoura, et al. 1991; Voultsiadou- Koukoura & Van Soest 1991a,b; Voultsiadou- of Eastern Mediterranean is Koukoura & the results of the Knowledge sponges Koukouras, 1993), that of other of the Med- have been and are poor compared to parts sponge collecting being re- iterranean Van 1994: Recent several science and (cf. Soest, Fig. 2). ported; species new to appar- collecting activities in the North Aegean Sea ently endemic to the Eastern Mediterranean been of have been described. -
Toponyms and the Fabric of Provincial History : a Review Article S
Toponyms and the Fabric of Provincial History : A Review Article S. E. READ And Cain knew his wife; and she con ceived, and bare Enoch; and he builded a city, and called the name of the city, after the name of his son, Enoch, (GENESIS 4,17) Place names, as is obvious in this early passage from the Bible, have long been of interest to mankind. Without question, their existence predates recorded history, from the time that man first started to communicate with fellow man; from the moment that someone said, "I live by the Red River," or "I dwell by the Oxen's Ford." For place names exist in all parts of the world and are recorded in all languages. For centuries they have been the subject of scholarly investigation (see, for example, the opening paragraphs of John Stowe's Survey of London, 1598); have stimulated the organization of learned societies and the publication of learned journals; and have given birth to such hard academic terms as "toponym," "toponomy," and toponymie," or "topnymical." In British Columbia place names present a demanding challenge — by no means as yet fully answered. Indians, of many tribes, speaking many dialects, have had their dwellings here for thousands of years. They named places but they kept no written records. Within each of these names is embedded some myth or legend, or some fragment of history but their origins have all too often been lost in the passage of time or obscured by linguistic difficulties. Then, some mere two hundred years ago, came the white explorers — Spanish, English, Scottish, French — first by sea and then by land. -
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Jennifer Galloway's 2010 Paper
Marine Micropaleontology 75 (2010) 62–78 Contents lists available at ScienceDirect Marine Micropaleontology journal homepage: www.elsevier.com/locate/marmicro Research paper A high-resolution marine palynological record from the central mainland coast of British Columbia, Canada: Evidence for a mid-late Holocene dry climate interval Jennifer M. Galloway a,⁎, Lameed O. Babalola a, R. Timothy Patterson a, Helen M. Roe b a Ottawa-Carleton Geoscience Centre and Department of Earth Sciences, Carleton University, 1125 Colonel By Drive, Ottawa, Ontario, Canada KIS 5B6 b School of Geography, Archaeology & Palaeoecology, Queen's University Belfast, Belfast, BT7 1NN, United Kingdom article info abstract Article history: Sediments collected in a 12-m long core (VEC02A04) obtained from Frederick Sound in the Seymour–Belize Received 24 December 2009 Inlet Complex of British Columbia were deposited between ca. 4540 cal. yr BP and ca. 1090 cal. yr BP in Received in revised form 6 March 2010 primarily dysoxic conditions. The sediments are characterized by alternating intervals of fine grained Accepted 8 March 2010 massive and laminated units. Laminated sediments consist of light-coloured diatom-rich layers deposited during summer and dark-coloured mineral-rich layers deposited during winter. Laminated sediments are Keywords: most common in portions of the core deposited between ca. 2840 cal. yr BP and ca. 1820 cal. yr BP, and Climate change correspond to a decline in the relative abundance and pollen accumulation rate of Cupressaceae pollen Late Holocene Coastal Western Hemlock biogeoclimatic between ca. 3190 cal. yr BP and ca. 2250 cal. yr BP. The preservation of laminated units and decline of zone Cupressaceae pollen at this time suggest that a drier and possibly cooler climate punctuated otherwise wet Marine palynology and temperate late Holocene conditions in the Seymour–Belize Inlet Complex. -
CHS Index Chart
Fisheries and Oceans Pi'lches et Oceans Canada Canada Canada ••• 137 ° 136 " 134" 133 ° 131° 129 ° ,.. 126 ° 125 " 124 " 123° 122° 119° 124 ° 118 ° GENERAL CHARTS CARTES GENERALES SMALL-CRAFT CHARTS REV ILLAG IGEDO LARGER SCALE CHARTS ISLAND CARTES POUR EMBARCATIONS CARTES A PLUS GRANDE ECHELLE 3050 Kootenay Lake and Rovet 75 000 3311 Sunshtno Coast- Vancouver Ha rbour lo/A 3052 Okanagan Lako so 000 Desolatoon Sound 40 000 3053 Shuswap Lake so 000 331:2 JerviS Intel ond/et Do•o latoon Sound 0 305S Waneta to /~ Hugh Keen leyside Dam 20 000 Vo,ous Scolo•JEche tle• vo"h• > z 3056 Hugh Koon loySido Dam to/A Burlon 40 000 3313 Gull Islands and Ad jacent Watotways/el les Vo1es Navigables Ad1acentes ~ ' 3057 Button IO/~ 1\rrowhood 40 000 Variou• Scale•/Echel le• vo"~"' 3058 Arrowhead lo/6 Rovo lotoko Go «m• 20 000 3488 Fro5er River/F I&uve Fraser, Cre•<ent l5land 3061 " "'"'on Lake and/ol Hamson R1ver '""'' to/~ Hon loon Mills 20 000 Harrison Lake 40 000 3469 Fraser Rovor/Fiouve Fr8set, Pattullo B"dgo Harrison R1ver 30 000 to/a Crescent Is land 20 000 Pitt River and/ot Poll l ak e 25 000 Stuaot L a~e (Not•howniP••rnd•qu o!) 50 000 54 " ~f--- ' ~ 0 "" I < ''"0' 't)Go iUn "?1- Cocoov• 3053 Foo ..o<o o l 0 "' GJ ,. Shu wap .•. Lake CANAOA !'; "'""""'' •·o~ d 130" 125° 120 " •5"omouo .,cocho Cceo> ,... ,. ' GJ ... ' <om l oops ~ DIXON E'N TRANCE' LEGENO/LEGENDE • •• • Scales smaller ttlan 1"40 000 Ectlellas plus petites qua 1:40 000 '' GJ Scales 1:40 000 and larger Ectlelles 1: 40 000 et plus grande& CHART SCALE Chart soale os the rat10 of one umt of d1stance 011 the cha" to the actual d.stance on the Earth's surface expressed on tho same unots. -
Climate Change and Decadal to Centennial-Scale Periodicities Recorded in a Late Holocene NE Pacific Marine Record: Examining the Role of Solar Forcing
Palaeogeography, Palaeoclimatology, Palaeoecology 386 (2013) 669–689 Contents lists available at SciVerse ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Climate change and decadal to centennial-scale periodicities recorded in a late Holocene NE Pacific marine record: Examining the role of solar forcing J.M. Galloway a,⁎, A. Wigston a, R.T. Patterson a, G.T. Swindles b, E. Reinhardt c, H.M. Roe d a Department of Earth Sciences and Ottawa Geoscience Centre, Carleton University, 1125 Colonel By Drive, Ottawa, Ontario K1S 5B6, Canada b School of Geography, University of Leeds, Leeds LS2 9JT, United Kingdom c School of Geography and Earth Sciences, McMaster University, Hamilton, ON L8S 4K1, Canada d School of Geography, Archaeology and Palaeoecology, Queen's University Belfast, Belfast BT7 1NN, United Kingdom article info abstract Article history: We present a decadal-scale late Holocene climate record based on diatoms, biogenic silica, and grain size Received 29 November 2012 from a 12-m sediment core (VEC02A04) obtained from Frederick Sound in the Seymour-Belize Inlet Complex Received in revised form 21 June 2013 of British Columbia, Canada. Sediments are characterized by graded, massive, and laminated intervals. Accepted 22 June 2013 Laminated intervals are most common between c. 2948–2708 cal. yr BP and c. 1992–1727 cal. yr BP. Available online 4 July 2013 Increased preservation of laminated sediments and diatom assemblage changes at this time suggest that cli- mate became moderately drier and cooler relative to the preceding and succeeding intervals. Spectral and Keywords: fi Late Holocene wavelet analyses are used to test for statistically signi cant periodicities in time series of proxies of primary Climate change production (total diatom abundance, biogenic silica) and hydrology (grain size) preserved in the Frederick Diatoms Sound record.