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Ifm-Geomar Report
FS Sonne Fahrtbericht / Cruise Report SO201-1b KALMAR Kurile-Kamchatka and ALeutian MARginal Sea-Island Arc Systems: Geodynamic and Climate Interaction in Space and Time Yokohama, Japan - Tomakomai, Japan 10.06. - 06.07.2009 IFM-GEOMAR REPORT Berichte aus dem Leibniz-Institut für Meereswissenschaften an der Christian-Albrechts-Universität zu Kiel Nr. 32 November 2009 FS Sonne Fahrtbericht / Cruise Report SO201-1b KALMAR Kurile-Kamchatka and ALeutian MARginal Sea-Island Arc Systems: Geodynamic and Climate Interaction in Space and Time Yokohama, Japan - Tomakomai, Japan 10.06. - 06.07.2009 Berichte aus dem Leibniz-Institut für Meereswissenschaften an der Christian-Albrechts-Universität zu Kiel Nr. 32 November 2009 ISSN Nr.: 1614-6298 Das Leibniz-Institut für Meereswissenschaften The Leibniz-Institute of Marine Sciences is a ist ein Institut der Wissenschaftsgemeinschaft member of the Leibniz Association Gottfried Wilhelm Leibniz (WGL) (Wissenschaftsgemeinschaft Gottfried Wilhelm Leibniz). Herausgeber / Editor: Reinhard Werner & Folkmar Hauff IFM-GEOMAR Report ISSN Nr.: 1614-6298 Leibniz-Institut für Meereswissenschaften / Leibniz Institute of Marine Sciences IFM-GEOMAR Dienstgebäude Westufer / West Shore Building Düsternbrooker Weg 20 D-24105 Kiel Germany Leibniz-Institut für Meereswissenschaften / Leibniz Institute of Marine Sciences IFM-GEOMAR Dienstgebäude Ostufer / East Shore Building Wischhofstr. 1-3 D-24148 Kiel Germany Tel.: ++49 431 600-0 Fax: ++49 431 600-2805 www.ifm-geomar.de 1 CONTENTS Page Summary..........................................................................................................................................................2 -
Sixteenth Meeting of the GEBCO Sub-Committee on Undersea Feature Names (SCUFN) Met at the International Hydrographic Bureau, Monaco, Under the Chairmanship of Dr
Distribution : limited IOC-IHO/GEBCO SCUFN-XV1/3 English only INTERGOVERNMENTAL INTERNATIONAL OCEANOGRAPHIC HYDROGRAPHIC COMMISSION (of UNESCO) ORGANIZATION International Hydrographic Bureau Monaco, 10-12 April 2003 SUMMARY REPORT IOC-IHO/GEBCO SCUFN-XVI/3 Page 2 Page intentionally left blank IOC-IHO/GEBCO SCUFN-XVI/3 Page 1 Notes: A list of acronyms, used in this report, is in Annex 3. An alphabetical index of all undersea feature names appearing in this report is in Annex 6. 1. INTRODUCTION – APPROVAL OF AGENDA The sixteenth meeting of the GEBCO Sub-Committee on Undersea Feature Names (SCUFN) met at the International Hydrographic Bureau, Monaco, under the Chairmanship of Dr. Robert L. FISHER, Scripps Institution of Oceanography (SIO), USA. Attendees were welcomed by Capt. Hugo GORZIGLIA, IHB Director. He mentioned that the IHB had invited IHO Member States to make experts available to SCUFN and was pleased to see new faces at this meeting. The meeting welcomed Dr. Hans-Werner SCHENKE (AWI, Germany), Mr. Kunikazu NISHIZAWA (Japan Hydrographic Department), Mrs. Lisa A. TAYLOR (NGDC, USA), Captain Vadim SOBOLEV (HDNO, Russian Federation) and Mr Norman CHERKIS (USA) as new members of SCUFN. The list of participants is in Annex 1. The draft agenda was approved without changes (see Annex 2). Mr. Desmond P.D. SCOTT kindly accepted to serve as Rapporteur for the meeting. 2. MATTERS REMAINING FROM PREVIOUS MEETINGS 2.1 From SCUFN-XIII (Dartmouth, Nova Scotia, Canada, June 1999) Ref: Doc. IOC-IHO/GEBCO SCUFN-XIII/3 2.1.1 Southwest Pacific region The following four features and names in this area, still pending, were reviewed: • Paragraph 3.1.5 - Proposed names for two seamounts located at (18°56’S – 169°27’W) and (19°31’S – 167°36’W) were still awaited from Dr Robin FALCONER, NIWA, New Zealand. -
Zeszyt 10. Morza I Oceany
Uwaga: Niniejsza publikacja została opracowana według stanu na 2008 rok i nie jest aktualizowana. Zamieszczony na stronie internetowej Komisji Standaryzacji Nazw Geograficznych poza Granica- mi Rzeczypospolitej Polskiej plik PDF jest jedynie zapisem cyfrowym wydrukowanej publikacji. Wykaz zalecanych przez Komisję polskich nazw geograficznych świata (Urzędowy wykaz polskich nazw geograficznych świata), wraz z aktualizowaną na bieżąco listą zmian w tym wykazie, zamieszczo- ny jest na stronie internetowej pod adresem: http://ksng.gugik.gov.pl/wpngs.php. KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju NAZEWNICTWO GEOGRAFICZNE ŚWIATA Zeszyt 10 Morza i oceany GŁÓWNY URZĄD GEODEZJI I KARTOGRAFII Warszawa 2008 KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju Waldemar Rudnicki (przewodniczący), Andrzej Markowski (zastępca przewodniczącego), Maciej Zych (zastępca przewodniczącego), Katarzyna Przyszewska (sekretarz); członkowie: Stanisław Alexandrowicz, Andrzej Czerny, Janusz Danecki, Janusz Gołaski, Romuald Huszcza, Sabina Kacieszczenko, Dariusz Kalisiewicz, Artur Karp, Zbigniew Obidowski, Jerzy Ostrowski, Jarosław Pietrow, Jerzy Pietruszka, Andrzej Pisowicz, Ewa Wolnicz-Pawłowska, Bogusław R. Zagórski Opracowanie Kazimierz Furmańczyk Recenzent Maciej Zych Komitet Redakcyjny Andrzej Czerny, Joanna Januszek, Sabina Kacieszczenko, Dariusz Kalisiewicz, Jerzy Ostrowski, Waldemar Rudnicki, Maciej Zych Redaktor prowadzący Maciej -
Vulnerable Marine Ecosystems – Processes and Practices in the High Seas Vulnerable Marine Ecosystems Processes and Practices in the High Seas
ISSN 2070-7010 FAO 595 FISHERIES AND AQUACULTURE TECHNICAL PAPER 595 Vulnerable marine ecosystems – Processes and practices in the high seas Vulnerable marine ecosystems Processes and practices in the high seas This publication, Vulnerable Marine Ecosystems: processes and practices in the high seas, provides regional fisheries management bodies, States, and other interested parties with a summary of existing regional measures to protect vulnerable marine ecosystems from significant adverse impacts caused by deep-sea fisheries using bottom contact gears in the high seas. This publication compiles and summarizes information on the processes and practices of the regional fishery management bodies, with mandates to manage deep-sea fisheries in the high seas, to protect vulnerable marine ecosystems. ISBN 978-92-5-109340-5 ISSN 2070-7010 FAO 9 789251 093405 I5952E/2/03.17 Cover photo credits: Photo descriptions clockwise from top-left: Acanthagorgia spp., Paragorgia arborea, Vase sponges (images courtesy of Fisheries and Oceans, Canada); and Callogorgia spp. (image courtesy of Kirsty Kemp, the Zoological Society of London). FAO FISHERIES AND Vulnerable marine ecosystems AQUACULTURE TECHNICAL Processes and practices in the high seas PAPER 595 Edited by Anthony Thompson FAO Consultant Rome, Italy Jessica Sanders Fisheries Officer FAO Fisheries and Aquaculture Department Rome, Italy Merete Tandstad Fisheries Resources Officer FAO Fisheries and Aquaculture Department Rome, Italy Fabio Carocci Fishery Information Assistant FAO Fisheries and Aquaculture Department Rome, Italy and Jessica Fuller FAO Consultant Rome, Italy FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2016 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
2. Geophysics and the Structure of the Lesser Antilles Forearc1
2. GEOPHYSICS AND THE STRUCTURE OF THE LESSER ANTILLES FOREARC1 G. K. Westbrook, Department of Geological Sciences, University of Durham and A. Mascle and B. Biju-Duval, Institut Français du Pétrole2 ABSTRACT The Barbados Ridge complex lies east of the Lesser Antilles volcanic arc along the eastern margin of the Caribbean Plate. The complex dates in part from the Eocene, and elements of the arc system have been dated as Late Cretaceous and Late Jurassic, although most of the volcanic rocks date from the Tertiary, particularly the latter part. It is probable that the arc system was moved a considerable distance eastward with respect to North and South America during the Tertiary. The accretionary complex can be divided into zones running parallel to the arc, starting with a zone of initial accre- tion at the front of the complex where sediment is stripped from the ocean floor and the rate of deformation is greatest. This zone passes into one of stabilization where the deformation rate is generally lower, although there are localized zones of more active tectonics where the generally mildly deformed overlying blanket of sediment is significant dis- turbed. Supracomplex sedimentary basins that are locally very thick are developed in the southern part of the complex. The Barbados Ridge Uplift containing the island of Barbados lies at the western edge of the complex; between it and the volcanic arc lies a large forearc basin comprising the Tobago Trough and Lesser Antilles Trough. There are major longitudinal variations in the complex that are broadly related to the northward decrease in sedi- ment thickness away from terrigenous sources in South America and that are locally controlled by ridges in the oceanic igneous crust passing beneath the complex. -
Shona and Discovery Seamount Chains
Goldschmidt Conference Abstracts 2009 A229 Shona and Discovery seamount Uranium-lead dating of speleothems: chains, South Atlantic: Prospects and limitations Superplume source constraints R.A. CLIFF 1 2 C. CLASS * AND A.P. LE ROEX School of Earth & Environment, University of Leeds 1Lamont-Doherty Earth Observatory of Columbia University, In recent year several studies have shown that U-Pb Palisades, NY 10964, USA isotopic dating is a promising option for dating speleothems (*correspondence: [email protected]) from the early Pleistocene and earlier which has otherwise 2University of Cape Town, Rondebosch 7701, South Africa presented a difficult challenge. ([email protected]) The integrity of the U-Pb system has been confirmed by comparison of U-Pb and U-Th data on a speleothem from the The effectively un-sampled major bathymetric anomalies Spannagel Cave in the Austrian Alps. Disequilibrium- of the Shona Ridge – Meteor Rise – Agulhas Ridge – Cape corrected U-Pb ages date growth from 340 ka to 267 ka. High Rise and Discovery seamounts in the South Atlantic have been resolution sampling of one short growth interval yielded U-Pb attributed to the activity of the Shona and Discovery mantle and U-Th ages in close agreement at 266 ka with ± 1 ka error plumes based solely on geochemical signatures measured in on the U-Pb age. These results confirm closed system Mid-Ocean Ridge basalts from the adjacent Mid-Atlantic behaviour throughout the uranium decay chain even in such Ridge and a single Discovery Seamount sample. Here we U-rich samples. present new Sr-Nd-Pb-Hf isotope data on dredge samples Speleothems from the Wilder Mann and Wildmahd caves from these seamount chains collected by the ANT XXIII/5 in the Allgäu Alps, western Austria encapsulate a detailed cruise of the FS Polarstern. -
SCUFN-XVIII/3 English Only
Distribution Limited IOC-IHO/GEBCO SCUFN-XVIII/3 English Only INTERGOVERNMENTAL INTERNATIONAL OCEANOGRAPHIC HYDROGRAPHIC COMMISSION (of UNESCO) ORGANIZATION International Hydrographic Bureau Monaco, 3-6 October 2005 FINAL REPORT IOC-IHO/GEBCO SCUFN-XVIII/3 Page 2 Page intentionally left blank IOC-IHO/GEBCO SCUFN-XVIII/3 Page 3 Notes: A list of acronyms, used in this report, is in Annex 5. An alphabetical index of all undersea feature names appearing in this report is in Annex 6. 1. INTRODUCTION – APPROVAL OF AGENDA Docs: SCUFN18-1A List of Documents (also Annex 1) SCUFN18-1B rev.1 List of Participants (also Annex 2) SCUFN18-1C rev.3 Agenda (also Annex 3) The eighteenth meeting of the GEBCO Sub-Committee on Undersea Feature Names (SCUFN) met at the International Hydrographic Bureau (IHB) in Monaco under the Chairmanship of Dr. Hans Werner Schenke, Alfred Wegener Institute (AWI), Germany. Dr. Schenke opened the meeting by thanking the IHB for hosting the meeting and expressing his appreciation for their hospitality. Admiral Maratov, president of the IHB, offered opening remarks and welcomed the participants to Monaco. Mr. Michel Huet (IHB), secretary of SCUFN, reviewed the logistics of the meeting and presented the documentation to be addressed by the meeting. A list of documents is included in Annex 1. Attendees included SCUFN members Dr. Hans-Werner Schenke (AWI, Germany), Dr. Galina V. Agapova (Geological Institute of the Russian Academy of Sciences), LCdr. Harvinder AVTAR (NHO, India), Mr. Norman Z. Cherkis (Five Oceans Consultants, USA), Lic. José Luis Frias Salazar (INEGI, Mexico), Mr. Michel Huet (IHB, Monaco), Dr. Yasuhiko Ohara (Hydrographic and Oceanographic Department of Japan), Captain Vadim Sobolev (HDNO, Russian Federation), Ms. -
Limited IOC-IHO/GEBCO SCUFN-XIV/3 English Only
Distribution : limited IOC-IHO/GEBCO SCUFN-XIV/3 English only INTERGOVERNMENTAL INTERNATIONAL OCEANOGRAPHIC HYDROGRAPHIC COMMISSION (of UNESCO) ORGANIZATION Japan Oceanographic Data Center Tokyo, Japan 17-20 April 2001 SUMMARY REPORT IOC-IHO/GEBCO SCUFN-XIV/3 Page intentionally left blank IOC-IHO/GEBCO SCUFN-XIV/3 Page i ALPHABETIC INDEX OF UNDERSEA FEATURE NAMES CONSIDERED AT SCUFN XIV AND APPEARING IN THIS REPORT (*=new name approved) Name Page Name Page ABY Canyon * 19 ARS Canyon * 94 AÇOR Bank * 26 ATHOS Canyon * 93 AÇOR Fracture Zone 26 'ATI'APITI Seamount 98 AÇORES ESTE Fracture Zone * 26 AUDIERNE Canyon * 90 AÇORES NORTE Fracture Zone 26 AUDIERNE Levee * 90 AÇORES-BISCAY Cordillera 26 AVON Canyon * 78 AEGIR Ridge 23 BAOULÉ Canyon * 19 AEGIS Spur * 87 BEAUGÉ Promontory * 85 AGOSTINHO Seamount * 26 BEIJU Bank * 58 AIGUILLON Canyon * 94 BEIRAL DE VIANA Escarpment * 6 AIX Canyon * 94 BELLE-ILE Canyon * 92 AKADEMIK KURCHATOV 12 BERTHOIS Spur * 86 Fracture Zone * AKE-NO-MYOJO Seamount * 52 BIJAGÓS Canyon * 11 ALBERT DE MONACO Ridge * 27 BIR-HAKEIM Bank 96 ALVARO MARTINS Hill * 27 BLACK Hole * 71 AMAMI Rise 62 BLACK MUD Canyon * 86 AMANOGAWA Seamounts * 69 BLACK MUD Levee * 89 AN-EI Seamount * 74 BLACK MUD SUPERIEUR 95 Seachannel ANITA CONTI Seamounts * 18 BLACK MUD INFERIEUR 95 Seachannel ANNAN Seamount 10 BOGDANOV Fracture Zone * 81 ANTON LEONOV Seamount * 11 BORDA Seamount * 27 ANTONIO DE FREITAS Hill * 27 BOREAS Abyssal Plain 23 ARAKI Seamount * 65 BOURCART Spur 97 ARAMIS Canyon * 93 BOURÉE Hole * 27 ARCACHON Canyon * 92 BRENOT Spur -
Insights Into the Origin and Evolution of Intraplate Magmatism in the Caribbean
Insights into the origin and evolution of intraplate magmatism in the Caribbean (initial stage of the Galápagos hotspot) and the South Atlantic (Discovery and Shona hotspot tracks) DISSERTATION zur Erlangung des Doktorgrades der Mathematisch-Naturwissenschaftlichen Fakultät der Christian-Albrechts-Universität zu Kiel vorgelegt von Antje Dürkefälden Kiel, 2019 Erster Gutachter: ........................................................................................................Prof. Dr. Kaj Hoernle Zweiter Gutachter: .....................................................................................................Prof. Dr. Colin Devey Tag der mündlichen Prüfung: ..................................................................................................12.02.2019 Hiermit erkläre ich, dass die vorliegende Doktorarbeit, abgesehen von der Beratung durch den Betreuer, nach Inhalt und Form eine eigenständige und nur mit den angegebenen Hilfsmitteln verfasste Arbeit ist. Die Arbeit wurde noch nicht an einer anderen Stelle im Rahmen eines Prüfungsverfahrens vorgelegt, veröffentlicht oder zur Veröffentlichung eingereicht. Ferner versichere ich, dass die Arbeit unter Einhaltung der Regeln guter wissenschaftlicher Praxis der Deutschen Forschungsgemeinschaft entstanden ist. Es wurde kein akademischer Grad entzogen. Kiel, den ................................................................................................................................... AntJe Dürkefälden I Preface The following dissertation is composed of five independent -
Ifm-Geomar Report
FS POSEIDON Fahrtbericht / Cruise Report P379/2 Mid-Atlantic-Researcher Ridge Volcanism (MARRVi) Mindelo - Fort-de-France 15.02.-08.03.2009 IFM-GEOMAR REPORT Berichte aus dem Leibniz-Institut für Meereswissenschaften an der Christian-Albrechts-Universität zu Kiel Nr. 29 June 2009 FS POSEIDON Fahrtbericht / Cruise Report P379/2 Mid-Atlantic-Researcher Ridge Volcanism (MARRVi) Mindelo - Fort-de-France 15.02.-08.03.2009 Berichte aus dem Leibniz-Institut für Meereswissenschaften an der Christian-Albrechts-Universität zu Kiel Nr. 29, June 2009 ISSN Nr.: 1614-6298 Das Leibniz-Institut für Meereswissenschaften The Leibniz-Institute of Marine Sciences is a ist ein Institut der Wissenschaftsgemeinschaft member of the Leibniz Association Gottfried Wilhelm Leibniz (WGL) (Wissenschaftsgemeinschaft Gottfried Wilhelm Leibniz). Herausgeber / Editor: Svend Duggen IFM-GEOMAR Report ISSN Nr.: 1614-6298 Leibniz-Institut für Meereswissenschaften / Leibniz Institute of Marine Sciences IFM-GEOMAR Dienstgebäude Westufer / West Shore Building Düsternbrooker Weg 20 D-24105 Kiel Germany Leibniz-Institut für Meereswissenschaften / Leibniz Institute of Marine Sciences IFM-GEOMAR Dienstgebäude Ostufer / East Shore Building Wischhofstr. 1-3 D-24148 Kiel Germany Tel.: ++49 431 600-0 Fax: ++49 431 600-2805 www.ifm-geomar.de Cruise Report POS379/2 (MARRVi) – MAR-Researcher Ridge 15. Feb. – 8. Mrz. 2009 Table of Contents Chapter 1: Scientific Party and Crew 2 Chapter 2: Introduction and Scientific Background 3 Chapter 3: Methods 8 3.1. The ELAC multi-beam system 3.2. The chain sack dredge 3.3. Magnetotellurics Chapter 4: Regional Geology and Preliminary Results 12 4.1. Isolated Seamounts 4.2. Mid-Atlantic Ridge 4.3. Researcher Ridge Chapter 5: Cruise Narrative 17 Chapter 6: Station Summary 23 Chapter 7: Sample Description 25 7.1. -
Fracture Zones and Their Gravity Signal 33
Het gebruik van een totale separatiepool in plaats van een halfpool voor de rotatie van de huidige spreidingsrug naar een oude positie is principieel onjuist. De hierdoor veroor- zaakte fout van ongeveer 15 kIn in de positie van de frakturezones in een rekonstruktie door Patriat et ai. (1985) kan van grote invloed zijn op hun konklusie dat frakturezones zich niet stationair gedragen. Patriat Ph., Segoufin J., Goslin J., Beuzart P. - Earth Planet. Sci. Leu .• 75, 204-214, 1985 Dit proefschrift, hoofdstuk 4 Het vulkano-tektonische komplex van Royal Trough en Researcher Ridge & Trough is ontstaan ten gevolge van rek welke samenhangt met de differentie1e beweging tussen Noord- en Zuidamerika. Het feit dat dit komplex zich uitstrekt ten noorden en zuiden van de Fifteen Twenty Fracture Zone vormt een aanwijzing dat frakturezones niet zwakker zijn dan de overige oceaanlithosfeer. Het beschikbaar komen van Seasat-satellietwaarnemingen van de hoogte van het zeeop- pervlak vormt een mijlpaal in het geofysisch onderzoek van de oceaan. Door toepassing van het zwaartekrachtsfilter op de Seasat-satellietwaarnemingen van de gemiddelde hoogte van het zeeoppervlak worden de gegevens in het golflengte bereik van 30-400 kIn bij uitstek geschikt voor het bestuderen van het frakturezonepatroon. De gewoonte om de zgn. stagepolen te bepalen tussen magnetische isochronen komt veelal voort uit een gebrek aan topografische informatie. Ten onrechte zou gekonkludeerd kunnen worden dat er een werkelijke relatie tussen veranderingen in de relatieve beweging van platen en ompolingen in het aardmagneetveld bestaat. Het woord stroomlijn (flowline) dat algemeen wordt gebruikt als men het over de sporen van het aangroeien van de oceaanlithosfeer heeft, is niet gelukkig gekozen aangezien het vervormingen in de oudere oceaanlithosfeer suggereerto Voorzover er al sprake is van stromen, treedt dit op tengevolge van thermische kontraktie in de jonge oceaanlithosfeer en weI Ioodrecht op de "stroomlijnen". -
Nineteenth Meeting of the GEBCO Sub-Committee on Undersea
IOC-IHO/GEBCO SCUFN-XIX English Only INTERGOVERNMENTAL INTERNATIONAL OCEANOGRAPHIC HYDROGRAPHIC COMMISSION (of UNESCO) ORGANIZATION Alfred Wegener Institute for Polar and Marine Research Bremerhaven, Germany 21-23 June 2006 FINAL REPORT Page intentionally left blank IOC-IHO/GEBCO SCUFN-XIX Page 3 Notes: A list of acronyms, used in this report, is in Annex 6. An alphabetical index of all undersea feature names appearing in this report is in Annex 7. 1. OPENING AND ADMINISTRATIVE ARRANGEMENTS Docs: SCUFN19-1A rev.5 List of Documents (also Annex 1) SCUFN19-1B rev.4 List of Participants (also Annex 2) The nineteenth meeting of the GEBCO Sub-Committee on Undersea Feature Names (SCUFN) met at the Alfred Wegener Institute for Polar and Marine Research (AWI) in Bremerhaven, Germany under the Chairmanship of Dr. Hans Werner Schenke (AWI). Dr. Schenke opened the meeting by welcoming the members of SCUFN and the many observers to AWI in Bremerhaven. He stated that the large number of attendees at the meeting was an indication of the increasing interest in the world of topology. The chairman welcomed Dr. Hyun-Chul HAN of the Korea Institute of Geology, Mining and Materials (KIGAM), as a new member of the Sub-Committee. After a round-table of introductions, Dr. Schenke discussed logistical issues and reviewed a list of documents to be addressed during the meeting. A list of documents is included in Annex 1. Attendees included SCUFN chairman, Dr. Hans-Werner Schenke (AWI, Germany), SCUFN secretary, Mr. Michel Huet (IHB, Monaco), and Sub-Committee members LCdr. Harvinder Atvar (NHO, India), Mr.