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Sustainable Seas Expeditions and Recognizes the Capabilities of BACKGROUND INFORMATION Deepworker
INVESTIGATION 3 Planning an Expedition Club-tipped anemone LAURA FRANCIS lzlzlzlzlzlzlzlzlz n this Investigation, students design LEARNING OBJECTIVES I their own scientific expedition to the Students will: sea using the goals of Sustainable Seas • Conduct a simulated vertical transect Expeditions as a guide. They begin by in the sea as one method of doing conducting a simulated vertical transect research; as an example of one method scientists • Plan and design a scientific investiga- tion that meets the goals of use in oceanic research. Sustainable Seas Expeditions and recognizes the capabilities of BACKGROUND INFORMATION DeepWorker. Exploring—For Answers Sustainable Seas Expeditions Research STANDARDS Meet DeepWorker Geography Standard 3 NOAA’s National Marine Sanctuaries How to analyze the spatial organization National Marine Sanctuary Sites of people, places, and environments on the Earth’s surface ACTIVITIES Geography Standard 18 Sample Mission: Vertical Transect How to apply geography to interpret Planning Your SSE Mission the present and plan for the future Science Education Standards Recognizing and developing abilities necessary to design and conduct scientific investigations •47• INVESTIGATION 3 Sample Mission: ACTIVITY Vertical Transect Guiding Question In this activity, students conduct a simulated vertical transect, providing them with an example What is a vertical transect? How do scientists use of one sampling method that they may consider this method to determine the layering system of for their scientific investigations. The data repre- physical and biological parts in the ocean? sents a vertical transect in Monterey Bay, but may be replaced with data from other locations. Discussion Materials Scientists often face the problem of trying to ac- curately interpret a natural system based upon ❑ Dive Mission Cards, one set for the class the limited data they are able to collect in the ❑ Water Sample Cards, one set for the class field. -
History of Scuba Diving About 500 BC: (Informa on Originally From
History of Scuba Diving nature", that would have taken advantage of this technique to sink ships and even commit murders. Some drawings, however, showed different kinds of snorkels and an air tank (to be carried on the breast) that presumably should have no external connecons. Other drawings showed a complete immersion kit, with a plunger suit which included a sort of About 500 BC: (Informaon originally from mask with a box for air. The project was so Herodotus): During a naval campaign the detailed that it included a urine collector, too. Greek Scyllis was taken aboard ship as prisoner by the Persian King Xerxes I. When Scyllis learned that Xerxes was to aack a Greek flolla, he seized a knife and jumped overboard. The Persians could not find him in the water and presumed he had drowned. Scyllis surfaced at night and made his way among all the ships in Xerxes's fleet, cung each ship loose from its moorings; he used a hollow reed as snorkel to remain unobserved. Then he swam nine miles (15 kilometers) to rejoin the Greeks off Cape Artemisium. 15th century: Leonardo da Vinci made the first known menon of air tanks in Italy: he 1772: Sieur Freminet tried to build a scuba wrote in his Atlanc Codex (Biblioteca device out of a barrel, but died from lack of Ambrosiana, Milan) that systems were used oxygen aer 20 minutes, as he merely at that me to arficially breathe under recycled the exhaled air untreated. water, but he did not explain them in detail due to what he described as "bad human 1776: David Brushnell invented the Turtle, first submarine to aack another ship. -
The Evolution of Siphonophore Tentilla for Specialized Prey Capture in the Open Ocean
The evolution of siphonophore tentilla for specialized prey capture in the open ocean Alejandro Damian-Serranoa,1, Steven H. D. Haddockb,c, and Casey W. Dunna aDepartment of Ecology and Evolutionary Biology, Yale University, New Haven, CT 06520; bResearch Division, Monterey Bay Aquarium Research Institute, Moss Landing, CA 95039; and cEcology and Evolutionary Biology, University of California, Santa Cruz, CA 95064 Edited by Jeremy B. C. Jackson, American Museum of Natural History, New York, NY, and approved December 11, 2020 (received for review April 7, 2020) Predator specialization has often been considered an evolutionary makes them an ideal system to study the relationships between “dead end” due to the constraints associated with the evolution of functional traits and prey specialization. Like a head of coral, a si- morphological and functional optimizations throughout the organ- phonophore is a colony bearing many feeding polyps (Fig. 1). Each ism. However, in some predators, these changes are localized in sep- feeding polyp has a single tentacle, which branches into a series of arate structures dedicated to prey capture. One of the most extreme tentilla. Like other cnidarians, siphonophores capture prey with cases of this modularity can be observed in siphonophores, a clade of nematocysts, harpoon-like stinging capsules borne within special- pelagic colonial cnidarians that use tentilla (tentacle side branches ized cells known as cnidocytes. Unlike the prey-capture apparatus of armed with nematocysts) exclusively for prey capture. Here we study most other cnidarians, siphonophore tentacles carry their cnidocytes how siphonophore specialists and generalists evolve, and what mor- in extremely complex and organized batteries (3), which are located phological changes are associated with these transitions. -
Trophic Ecology of Gelatinous Zooplankton in Oceanic Food Webs of the Eastern Tropical Atlantic Assessed by Stable Isotope Analysis
Limnol. Oceanogr. 9999, 2020, 1–17 © 2020 The Authors. Limnology and Oceanography published by Wiley Periodicals LLC on behalf of Association for the Sciences of Limnology and Oceanography. doi: 10.1002/lno.11605 Tackling the jelly web: Trophic ecology of gelatinous zooplankton in oceanic food webs of the eastern tropical Atlantic assessed by stable isotope analysis Xupeng Chi ,1,2* Jan Dierking,2 Henk-Jan Hoving,2 Florian Lüskow,3,4 Anneke Denda,5 Bernd Christiansen,5 Ulrich Sommer,2 Thomas Hansen,2 Jamileh Javidpour2,6 1CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China 2Marine Ecology, GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany 3Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, Vancouver, British Columbia, Canada 4Institute for the Oceans and Fisheries, University of British Columbia, Vancouver, British Columbia, Canada 5Institute of Marine Ecosystem and Fishery Science (IMF), Universität Hamburg, Hamburg, Germany 6Department of Biology, University of Southern Denmark, Odense M, Denmark Abstract Gelatinous zooplankton can be present in high biomass and taxonomic diversity in planktonic oceanic food webs, yet the trophic structuring and importance of this “jelly web” remain incompletely understood. To address this knowledge gap, we provide a holistic trophic characterization of a jelly web in the eastern tropical Atlantic, based on δ13C and δ15N stable isotope analysis of a unique gelatinous zooplankton sample set. The jelly web covered most of the isotopic niche space of the entire planktonic oceanic food web, spanning > 3 tro- phic levels, ranging from herbivores (e.g., pyrosomes) to higher predators (e.g., ctenophores), highlighting the diverse functional roles and broad possible food web relevance of gelatinous zooplankton. -
Order BERYCIFORMES ANOPLOGASTRIDAE Anoplogaster
click for previous page 2210 Bony Fishes Order BERYCIFORMES ANOPLOGASTRIDAE Fangtooths by J.R. Paxton iagnostic characters: Small (to 16 cm) Dberyciform fishes, body short, deep, and compressed. Head large, steep; deep mu- cous cavities on top of head separated by serrated crests; very large temporal and pre- opercular spines and smaller orbital (frontal) spine in juveniles of one species, all disap- pearing with age. Eyes smaller than snout length in adults (but larger than snout length in juveniles). Mouth very large, jaws extending far behind eye in adults; one supramaxilla. Teeth as large fangs in pre- maxilla and dentary; vomer and palatine toothless. Gill rakers as gill teeth in adults (elongate, lath-like in juveniles). No fin spines; dorsal fin long based, roughly in middle of body, with 16 to 20 rays; anal fin short-based, far posterior, with 7 to 9 rays; pelvic fin abdominal in juveniles, becoming subthoracic with age, with 7 rays; pectoral fin with 13 to 16 rays. Scales small, non-overlap- ping, spinose, cup-shaped in adults; lateral line an open groove partly covered by scales. No light organs. Total vertebrae 25 to 28. Colour: brown-black in adults. Habitat, biology, and fisheries: Meso- and bathypelagic. Distinctive caulolepis juvenile stage, with greatly enlarged head spines in one species. Feeding mode as carnivores on crustaceans as juveniles and on fishes as adults. Rare deepsea fishes of no commercial importance. Remarks: One genus with 2 species throughout the world ocean in tropical and temperate latitudes. The family was revised by Kotlyar (1986). Similar families occurring in the area Diretmidae: No fangs, jaw teeth small, in bands; anal fin with 18 to 24 rays. -
MEESO Survey to the North Atlantic Ocean, 1-30 June 2021
MEESO survey to the North Atlantic Ocean, 1-30 June 2021 R/V “G.O. Sars”, surveying the North Atlantic Ocean mesopelagic sone during the light summer nights. Photo: Chris Lindemann. As part of the MEESO field campaign, the Norwegian Research Vessel, G. O. Sars, is sur- veying the mesopelagic ecosystem of the North-East Atlantic and the Norwegian Sea. The cruise started in Bergen, Norway, 1 June and ends there 30 June. Scientists from the University of Bergen and the Institute of Marine Research in Bergen, Nor- way, are using new technology, partly developed in MEESO, like non-graded trawls and un- derwater towed systems with optical sensors and broadband multifrequency acoustics to in- vestigate the mesopelagic ecosystem and map the biomass distribution of the mesopelagic community and its possible drivers. So far we have identified more than 90 species of fish and the diversity of crustaceans, gelati- nous plankton and cephalopods has proven to be high as well. A marked fall in diversity and the vertical extent of the mesopelagic deep scattering layers were observed as we moved from the Iceland Basin, south of Iceland and west of the Faroe Islands, into the Norwegian Sea. Download from meeso.org 1 The Common fangtooth Anoplogaster cornuta (127 mm SL) is not only the fish species with the long- est teeth in relation to body length, it also has an amazing pattern of bony ridges on its head. Photo: Rupert Wienerroither. The Mirror lanternfish Lampadena speculigera (97 mm SL) has a large heart-shaped luminous gland on top and an oval luminous gland below its caudal peduncle. -
Updated Checklist of Marine Fishes (Chordata: Craniata) from Portugal and the Proposed Extension of the Portuguese Continental Shelf
European Journal of Taxonomy 73: 1-73 ISSN 2118-9773 http://dx.doi.org/10.5852/ejt.2014.73 www.europeanjournaloftaxonomy.eu 2014 · Carneiro M. et al. This work is licensed under a Creative Commons Attribution 3.0 License. Monograph urn:lsid:zoobank.org:pub:9A5F217D-8E7B-448A-9CAB-2CCC9CC6F857 Updated checklist of marine fishes (Chordata: Craniata) from Portugal and the proposed extension of the Portuguese continental shelf Miguel CARNEIRO1,5, Rogélia MARTINS2,6, Monica LANDI*,3,7 & Filipe O. COSTA4,8 1,2 DIV-RP (Modelling and Management Fishery Resources Division), Instituto Português do Mar e da Atmosfera, Av. Brasilia 1449-006 Lisboa, Portugal. E-mail: [email protected], [email protected] 3,4 CBMA (Centre of Molecular and Environmental Biology), Department of Biology, University of Minho, Campus de Gualtar, 4710-057 Braga, Portugal. E-mail: [email protected], [email protected] * corresponding author: [email protected] 5 urn:lsid:zoobank.org:author:90A98A50-327E-4648-9DCE-75709C7A2472 6 urn:lsid:zoobank.org:author:1EB6DE00-9E91-407C-B7C4-34F31F29FD88 7 urn:lsid:zoobank.org:author:6D3AC760-77F2-4CFA-B5C7-665CB07F4CEB 8 urn:lsid:zoobank.org:author:48E53CF3-71C8-403C-BECD-10B20B3C15B4 Abstract. The study of the Portuguese marine ichthyofauna has a long historical tradition, rooted back in the 18th Century. Here we present an annotated checklist of the marine fishes from Portuguese waters, including the area encompassed by the proposed extension of the Portuguese continental shelf and the Economic Exclusive Zone (EEZ). The list is based on historical literature records and taxon occurrence data obtained from natural history collections, together with new revisions and occurrences. -
New Zealand Fishes a Field Guide to Common Species Caught by Bottom, Midwater, and Surface Fishing Cover Photos: Top – Kingfish (Seriola Lalandi), Malcolm Francis
New Zealand fishes A field guide to common species caught by bottom, midwater, and surface fishing Cover photos: Top – Kingfish (Seriola lalandi), Malcolm Francis. Top left – Snapper (Chrysophrys auratus), Malcolm Francis. Centre – Catch of hoki (Macruronus novaezelandiae), Neil Bagley (NIWA). Bottom left – Jack mackerel (Trachurus sp.), Malcolm Francis. Bottom – Orange roughy (Hoplostethus atlanticus), NIWA. New Zealand fishes A field guide to common species caught by bottom, midwater, and surface fishing New Zealand Aquatic Environment and Biodiversity Report No: 208 Prepared for Fisheries New Zealand by P. J. McMillan M. P. Francis G. D. James L. J. Paul P. Marriott E. J. Mackay B. A. Wood D. W. Stevens L. H. Griggs S. J. Baird C. D. Roberts‡ A. L. Stewart‡ C. D. Struthers‡ J. E. Robbins NIWA, Private Bag 14901, Wellington 6241 ‡ Museum of New Zealand Te Papa Tongarewa, PO Box 467, Wellington, 6011Wellington ISSN 1176-9440 (print) ISSN 1179-6480 (online) ISBN 978-1-98-859425-5 (print) ISBN 978-1-98-859426-2 (online) 2019 Disclaimer While every effort was made to ensure the information in this publication is accurate, Fisheries New Zealand does not accept any responsibility or liability for error of fact, omission, interpretation or opinion that may be present, nor for the consequences of any decisions based on this information. Requests for further copies should be directed to: Publications Logistics Officer Ministry for Primary Industries PO Box 2526 WELLINGTON 6140 Email: [email protected] Telephone: 0800 00 83 33 Facsimile: 04-894 0300 This publication is also available on the Ministry for Primary Industries website at http://www.mpi.govt.nz/news-and-resources/publications/ A higher resolution (larger) PDF of this guide is also available by application to: [email protected] Citation: McMillan, P.J.; Francis, M.P.; James, G.D.; Paul, L.J.; Marriott, P.; Mackay, E.; Wood, B.A.; Stevens, D.W.; Griggs, L.H.; Baird, S.J.; Roberts, C.D.; Stewart, A.L.; Struthers, C.D.; Robbins, J.E. -
A Link to the Report Hv 2021-22
HV 2021-22 ISSN 2298-9137 HAF- OG VATNARANNSÓKNIR MARINE AND FRESHWATER RESEARCH IN ICELAND Sampling for the MEESO project during the International Ecosystem Summer Survey in Nordic Seas on the R/V Arni Fridriksson in July 2020 Ástþór Gíslason, Klara Jakobsdóttir, Kristinn Guðmundsson, Svanhildur Egilsdóttir, Teresa Silva HAFNARFJÖRÐUR - MAÍ 2021 Sampling for the MEESO project during the International Ecosystem Summer Survey in Nordic Seas on the R/V Arni Fridriksson in July 2020 Ástþór Gíslason, Klara Jakobsdóttir, Kristinn Guðmundsson, Svanhildur Egilsdóttir, Teresa Silva Haf‐ og vatnarannsóknir Marine and Freshwater Research in Iceland Upplýsingablað Titill: Sampling for the MEESO project during the International Ecosystem Summer Survey in Nordic Seas on the R/V Arni Fridriksson in July 2020 Höfundar: Ástþór Gíslason, Klara Jakobsdóttir, Kristinn Guðmundsson, Svanhildur Egilsdóttir, Teresa Silva Skýrsla nr: Verkefnisstjóri: Verknúmer: HV‐2021‐22 Ástþór Gíslason 12471 ISSN Fjöldi síðna: Útgáfudagur: 2298‐9137 26 7. maí 2021 Unnið fyrir: Dreifing: Yfirfarið af: Hafrannsóknastofnun Opin Anna Heiða Ólafsdóttir Ágrip Gagnasöfnun fyrir alþjóðlegt rannsóknaverkefni um lífríki miðsjávarlaga (MEESO), sem styrkt er af Evrópusambandinu, fór fram í rannsóknaleiðangri Hafrannsóknastofnunar á uppsjávarvistkerfi norðurhafa að sumarlagi sumarið 2020. Tilgangurinn var að rannsaka magn, dreifingu og samsetningu miðsjávarfánu í tengslum við umhverfisþætti og vöxt og viðgang plöntsvifs. Meginsvæði rannsóknarinnar fylgdi sniði sem liggur nokkurn veginn eftir 61°50’N‐breiddarbaug, frá 38°49’V og að 16°05’V, þ.e. frá Grænlandshafi yfir Reykjaneshrygg og inn í Suðurdjúp, sem og á stöð í Grindavíkurdýpi. Eftir endilöngu sniðinu var u.þ.b. 50 m þykkt blöndunarlag sem svifgróður virtist dafna í. Samkvæmt bergmálsmælingum voru tvö meginlög miðsjávarlífvera. -
For Creative Minds
For Creative Minds The For Creative Minds educational section may be photocopied or printed from our website by the owner of this book for educational, non-commercial uses. Cross-curricular teaching activities, interactive quizzes, and more are available online. Go to ArbordalePublishing.com and click on the book’s cover to explore all the links. Deep Ocean Habitats Things change the deeper you go in the ocean: light disappears, temperatures grow increasingly colder, and pressure gets much higher. The amount of oxygen in the water sunlight zone decreases with depth but then gets higher again at the bottom! Because these changes twilight zone affect the types of organisms that can survive there, the ocean is divided into five layers by depth called life zones. Only the sunlight zone receives enough sunlight for algae to convert light into energy midnight zone (photosynthesis). Because almost all food webs start with plants or algae, this is the zone where the most animals live. The twilight zone still gets some sunlight, but not enough for photosynthesis. The animals that live here either travel to the sunlight zone to feed or depend on food falling from above. There is no light in the midnight zone. Most abyssal zone of the animals that live here produce their own light through bioluminescence. The abyssal zone is pitch black, almost freezing cold, and has little oxygen and incredibly high pressure, yet animals still live here. In the deep trenches is the hadal zone. It is like the abyssal zone, except with even more hadal zone immense -
Dives of the Bathyscaph Trieste, 1958-1963: Transcriptions of Sixty-One Dictabelt Recordings in the Robert Sinclair Dietz Papers, 1905-1994
Dives of the Bathyscaph Trieste, 1958-1963: Transcriptions of sixty-one dictabelt recordings in the Robert Sinclair Dietz Papers, 1905-1994 from Manuscript Collection MC28 Archives of the Scripps Institution of Oceanography University of California, San Diego La Jolla, California 92093-0219: September 2000 This transcription was made possible with support from the U.S. Naval Undersea Museum 2 TABLE OF CONTENTS INTRODUCTION ...........................................................................................................................4 CASSETTE TAPE 1 (Dietz Dictabelts #1-5) .................................................................................6 #1-5: The Big Dive to 37,800. Piccard dictating, n.d. CASSETTE TAPE 2 (Dietz Dictabelts #6-10) ..............................................................................21 #6: Comments on the Big Dive by Dr. R. Dietz to complete Piccard's description, n.d. #7: On Big Dive, J.P. #2, 4 Mar., n.d. #8: Dive to 37,000 ft., #1, 14 Jan 60 #9-10: Tape just before Big Dive from NGD first part has pieces from Rex and Drew, Jan. 1960 CASSETTE TAPE 3 (Dietz Dictabelts #11-14) ............................................................................30 #11-14: Dietz, n.d. CASSETTE TAPE 4 (Dietz Dictabelts #15-18) ............................................................................39 #15-16: Dive #61 J. Piccard and Dr. A. Rechnitzer, depth of 18,000 ft., Piccard dictating, n.d. #17-18: Dive #64, 24,000 ft., Piccard, n.d. CASSETTE TAPE 5 (Dietz Dictabelts #19-22) ............................................................................48 #19-20: Dive Log, n.d. #21: Dr. Dietz on the bathysonde, n.d. #22: from J. Piccard, 14 July 1960 CASSETTE TAPE 6 (Dietz Dictabelts #23-25) ............................................................................57 #23-25: Italian Dive, Dietz, Mar 8, n.d. CASSETTE TAPE 7 (Dietz Dictabelts #26-29) ............................................................................64 #26-28: Italian Dive, Dietz, n.d. -
How Did the Deepwater Horizon Oil Spill Impact Deep-Sea Ecosystems? Charles R
Nova Southeastern University NSUWorks Marine & Environmental Sciences Faculty Articles Department of Marine and Environmental Sciences 9-1-2016 How Did the Deepwater Horizon Oil Spill Impact Deep-Sea Ecosystems? Charles R. Fisher Pennsylvania State University - Main Campus Paul A. Montagna Texas A & M University - Corpus Christi Tracey Sutton Nova Southeastern University, [email protected] Find out more information about Nova Southeastern University and the Halmos College of Natural Sciences and Oceanography. Follow this and additional works at: https://nsuworks.nova.edu/occ_facarticles Part of the Marine Biology Commons, and the Oceanography and Atmospheric Sciences and Meteorology Commons NSUWorks Citation Charles R. Fisher, Paul A. Montagna, and Tracey Sutton. 2016. How Did the Deepwater Horizon Oil Spill Impact Deep-Sea Ecosystems? .Oceanography , (3) : 182 -195. https://nsuworks.nova.edu/occ_facarticles/784. This Article is brought to you for free and open access by the Department of Marine and Environmental Sciences at NSUWorks. It has been accepted for inclusion in Marine & Environmental Sciences Faculty Articles by an authorized administrator of NSUWorks. For more information, please contact [email protected]. OceTHE OFFICIALa MAGAZINEn ogOF THE OCEANOGRAPHYra SOCIETYphy CITATION Fisher, C.R., P.A. Montagna, and T.T. Sutton. 2016. How did the Deepwater Horizon oil spill impact deep-sea ecosystems? Oceanography 29(3):182–195, http://dx.doi.org/10.5670/oceanog.2016.82. DOI http://dx.doi.org/10.5670/oceanog.2016.82 COPYRIGHT This article has been published in Oceanography, Volume 29, Number 3, a quarterly journal of The Oceanography Society. Copyright 2016 by The Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching and research.