“SEAMOUNT” Database: Recent Updates and Its Potential Use for Ecological Risk Assessment
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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. -
Bathymetry of the New Zealand Region
ISSN 2538-1016; 11 NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 161 BATHYMETRY OF THE NEW ZEALAND REGION by J. W. BRODIE New Zealand Oceanographic Institute Wellington New Zealand Oceanographic Institute Memoir No. 11 1964 This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ Fromispiece: The survey ship HMS Penguin from which many soundings were obtained around the New Zealand coast and in the south-west Pacific in the decade around 1900. (Photograph by courtesy of the Trustees, National Maritime Museum, Greenwich.) This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 161 BATHYMETRY OF THE NEW ZEALAND REGION by J. W. BRODIE New Zealand Oceanographic Institute Wellington New Zealand Oceanographic Institute Memoir No. 11 1964 Price: 15s. This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-nd/3.0/ CONTENTS Page No. ABSTRACT 7 INTRODUCTION 7 Sources of Data 7 Compilation of Charts 8 EARLIER BATHYMETRIC INTERPRETATIONS 10 Carte Gen�rale Bathymetrique des Oceans 17 Discussion 19 NAMES OF OCEAN FLOOR FEATURES 22 Synonymy of Existing Names 22 Newly Named Features .. 23 FEATURES ON THE CHARTS 25 Major Morphological Units 25 Offshore Banks and Seamounts 33 STRUCTURAL POSITION OF NEW ZEALAND 35 The New Zealand Plateau 35 Rocks of the New Zealand Plateau 37 Crustal Thickness Beneath the New Zealand Plateau 38 Chatham Province Features 41 The Alpine Fault 41 Minor Irregularities on the Sea Floor 41 SEDIMENTATION IN THE NEW ZEALAND REGION . -
The Age and Origin of Miocene-Pliocene Fault Reactivations in the Upper Plate of an Incipient Subduction Zone, Puysegur Margin
RESEARCH ARTICLE The Age and Origin of Miocene‐Pliocene Fault 10.1029/2019TC005674 Reactivations in the Upper Plate of an Key Points: • Structural analyses and 40Ar/39Ar Incipient Subduction Zone, Puysegur geochronology reveal multiple fault reactivations accompanying Margin, New Zealand subduction initiation at the K. A. Klepeis1 , L. E. Webb1 , H. J. Blatchford1,2 , R. Jongens3 , R. E. Turnbull4 , and Puysegur Margin 5 • The data show how fault motions J. J. Schwartz are linked to events occurring at the 1 2 Puysegur Trench and deep within Department of Geology, University of Vermont, Burlington, VT, USA, Now at Department of Earth Sciences, University continental lithosphere of Minnesota, Minneapolis, MN, USA, 3Anatoki Geoscience Ltd, Dunedin, New Zealand, 4Dunedin Research Centre, GNS • Two episodes of Late Science, Dunedin, New Zealand, 5Department of Geological Sciences, California State University, Northridge, Northridge, Miocene‐Pliocene reverse faulting CA, USA resulted in short pulses of accelerated rock uplift and topographic growth Abstract Structural observations and 40Ar/39Ar geochronology on pseudotachylyte, mylonite, and other Supporting Information: fault zone materials from Fiordland, New Zealand, reveal a multistage history of fault reactivation and • Supporting information S1 uplift above an incipient ocean‐continent subduction zone. The integrated data allow us to distinguish • Table S1 true fault reactivations from cases where different styles of brittle and ductile deformation happen • Figure S1 • Table S2 together. Five stages of faulting record the initiation and evolution of subduction at the Puysegur Trench. Stage 1 normal faults (40–25 Ma) formed during continental rifting prior to subduction. These faults were reactivated as dextral strike‐slip shear zones when subduction began at ~25 Ma. -
Exploration of New Zealand's Deepwater Frontier * GNS Science
exploration of New Zealand’s deepwater frontier The New Zealand Exclusive Economic Zone (EEZ) is the 4th largest in the world at about GNS Science Petroleum Research Newsletter 4 million square kilometres or about half the land area of Australia. The Legal Continental February 2008 Shelf claim presently before the United Nations, may add another 1.7 million square kilometres to New Zealand’s jurisdiction. About 30 percent of the EEZ is underlain by sedimentary basins that may be thick enough to generate and trap petroleum. Although introduction small to medium sized discoveries continue to be made in New Zealand, big oil has so far This informal newsletter is produced to tell the eluded the exploration companies. industry about highlights in petroleum-related research at GNS Science. We want to inform Exploration of the New Zealand EEZ has you about research that is going on, and barely started. Deepwater wells will be provide useful information for your operations. drilled in the next few years and encouraging We welcome your opinions and feedback. results would kick start the New Zealand deepwater exploration effort. Research Petroleum research at GNS Science efforts have identified a number of other potential petroleum basins around New Our research programme on New Zealand's Zealand, including the Pegasus Sub-basin, Petroleum Resources receives $2.4M p.a. of basins in the Outer Campbell Plateau, the government funding, through the Foundation of deepwater Solander Basin, the Bellona Basin Research Science and Technology (FRST), between the Challenger Plateau and Lord and is one of the largest research programmes in GNS Science. -
The Gondwana Margin: Proterozoic to Mesozoic
CORE Metadata, citation and similar papers at core.ac.uk Provided by EPrints Complutense The Gondwana margin: Proterozoic to Mesozoic The longevity and extent of the oceanic southern of '--'H��'.JAJ.J.'u., E. I.M. Gonzalez-Casado and I.A. Dahlquist Gondwana have made it the of intense study for more on "The Maz terrane: a Mesoproterozoic domain in the western than 70 years. It was one of the cradles of terrane and Sierras equivalent to the remains a proving ground for theories of Antofalla block of southern Peru? for West LL.L�""".LE, """'.LJL.LU''-'H and Investigation on this Gondwana evolution" sheds new light on the Middle margin, such as accretionary orogenesis and terrane analysis, is and Late Proterozoic evolution of the western Amazonia margin vital to our understanding of the Proterozoic and Phanerozoic that preceded final amalgamation of West Gondwana in the Late evolution of the continental crust. In this issue of Cambrian. The Maz terrane Gondwana Research, entitled "The West Gondwana Margin: Sierras Pampeanas) is recognised as a new continental terrane Proterozoic to Mesozoic", we have assembled 9 research papers that underwent Grenvillian-age orogeny and was thoroughly various of the evolution of the West the Ordovician Famatinian orogeny. Nd- and Gondwana margin, frrst at the international .L.Ln-''-'�'J.�F. allows correlation of Maz metasedi 'Gondwana 12 (Geological and Biological Heritage of Gond- rnp'nt�n"\T rocks with the Mesoproterozoic northern part of the wana)', held in in November 2005. Many -'-'J.�V.L<-"HU craton, of pre-Andean basement in concern southern South which has a continuous southern Peru. -
Paper Is Divided Into Two Parts
Earth-Science Reviews 140 (2015) 72–107 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Geologic and kinematic constraints on Late Cretaceous to mid Eocene plate boundaries in the southwest Pacific Kara J. Matthews a,⁎, Simon E. Williams a, Joanne M. Whittaker b,R.DietmarMüllera, Maria Seton a, Geoffrey L. Clarke a a EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia b Institute for Marine and Antarctic Studies, University of Tasmania, TAS 7001, Australia article info abstract Article history: Starkly contrasting tectonic reconstructions have been proposed for the Late Cretaceous to mid Eocene (~85– Received 25 November 2013 45 Ma) evolution of the southwest Pacific, reflecting sparse and ambiguous data. Furthermore, uncertainty in Accepted 30 October 2014 the timing of and motion at plate boundaries in the region has led to controversy around how to implement a Available online 7 November 2014 robust southwest Pacific plate circuit. It is agreed that the southwest Pacific comprised three spreading ridges during this time: in the Southeast Indian Ocean, Tasman Sea and Amundsen Sea. However, one and possibly Keywords: two other plate boundaries also accommodated relative plate motions: in the West Antarctic Rift System Southwest Pacific fi Lord Howe Rise (WARS) and between the Lord Howe Rise (LHR) and Paci c. Relevant geologic and kinematic data from the South Loyalty Basin region are reviewed to better constrain its plate motion history during this period, and determine the time- Late Cretaceous dependent evolution of the southwest Pacific regional plate circuit. A model of (1) west-dipping subduction Subduction and basin opening to the east of the LHR from 85–55 Ma, and (2) initiation of northeast-dipping subduction Plate circuit and basin closure east of New Caledonia at ~55 Ma is supported. -
Proposal to Study Subduction Initiation in Northern Zealandia Tim Stern1
Proposal to study subduction initiation in northern Zealandia Tim Stern1, Rupert Sutherland2 1 Victoria University of Wellington; 2 GNS Science, Lower Hutt [email protected] Back-arc regions of subduction zones contain sedimentary records that hold clues to the subduction initiation process, and provide complementary insights to fore-arc studies (e.g. Izu-Bonin-Mariana and Tonga). The basins and sedimentary platforms northwest of New Zealand record onset of the Tonga –Kermadec (TK) system during the Eocene- Oligocene (see Gurnis et al. white paper). We propose (mainly) marine geophysical studies that will reveal clues as to how and why TK, and Hikurangi, subduction started. Key features that require study are: Norfolk Ridge (NR); New Caledonia Trough (NCT); Taranaki-Wanganui basins; and Three Kings Ridge (TKR). The NR is where surface convergence was associated with initial subduction. What was the vergence and timing of thrusting, what vertical motions took place, and how do these observations compare and discriminate alternate geodynamic model predictions? The New Caledonia Trough lies adjacent to Norfolk Ridge, was deformed in the subduction initiation event and subsided with large magnitude (Sutherland and al., 2010) that is precisely quantified (1.5 km) at its southern end near the north end of Taranaki Basin (Baur et al., 2013). What was the regional timing of NCT subsidence in relation to other aspects of subduction initiation, and what is its significance? Does the 1.5 km of Oligocene “platform subsidence” seen in oil company drill hole data from South Taranaki Basin at ~ 30 Ma (Stern and Holt, 1994) have a common cause as that in the NCT ? If so, the process occurs on a ~1000 km scale and is clearly geodynamically significant. -
Chapter 36D. South Pacific Ocean
Chapter 36D. South Pacific Ocean Contributors: Karen Evans (lead author), Nic Bax (convener), Patricio Bernal (Lead member), Marilú Bouchon Corrales, Martin Cryer, Günter Försterra, Carlos F. Gaymer, Vreni Häussermann, and Jake Rice (Co-Lead member and Editor Part VI Biodiversity) 1. Introduction The Pacific Ocean is the Earth’s largest ocean, covering one-third of the world’s surface. This huge expanse of ocean supports the most extensive and diverse coral reefs in the world (Burke et al., 2011), the largest commercial fishery (FAO, 2014), the most and deepest oceanic trenches (General Bathymetric Chart of the Oceans, available at www.gebco.net), the largest upwelling system (Spalding et al., 2012), the healthiest and, in some cases, largest remaining populations of many globally rare and threatened species, including marine mammals, seabirds and marine reptiles (Tittensor et al., 2010). The South Pacific Ocean surrounds and is bordered by 23 countries and territories (for the purpose of this chapter, countries west of Papua New Guinea are not considered to be part of the South Pacific), which range in size from small atolls (e.g., Nauru) to continents (South America, Australia). Associated populations of each of the countries and territories range from less than 10,000 (Tokelau, Nauru, Tuvalu) to nearly 30.5 million (Peru; Population Estimates and Projections, World Bank Group, accessed at http://data.worldbank.org/data-catalog/population-projection-tables, August 2014). Most of the tropical and sub-tropical western and central South Pacific Ocean is contained within exclusive economic zones (EEZs), whereas vast expanses of temperate waters are associated with high seas areas (Figure 1). -
32-1 Arculus.Pdf
OceTHE OFFICIALa MAGAZINEn ogOF THE OCEANOGRAPHYra SOCIETYphy CITATION Arculus, R.J., M. Gurnis, O. Ishizuka, M.K. Reagan, J.A. Pearce, and R. Sutherland. 2019. How to cre- ate new subduction zones: A global perspective. Oceanography 32(1):160–174, https://doi.org/ 10.5670/oceanog.2019.140. DOI https://doi.org/10.5670/oceanog.2019.140 PERMISSIONS Oceanography (ISSN 1042-8275) is published by The Oceanography Society, 1 Research Court, Suite 450, Rockville, MD 20850 USA. ©2019 The Oceanography Society, Inc. Permission is granted for individuals to read, download, copy, distribute, print, search, and link to the full texts of Oceanography articles. Figures, tables, and short quotes from the magazine may be republished in scientific books and journals, on websites, and in PhD dissertations at no charge, but the materi- als must be cited appropriately (e.g., authors, Oceanography, volume number, issue number, page number[s], figure number[s], and DOI for the article). Republication, systemic reproduction, or collective redistribution of any material in Oceanography is permitted only with the approval of The Oceanography Society. Please contact Jennifer Ramarui at [email protected]. Permission is granted to authors to post their final pdfs, provided byOceanography , on their personal or institutional websites, to deposit those files in their institutional archives, and to share the pdfs on open-access research sharing sites such as ResearchGate and Academia.edu. DOWNLOADED FROM HTTPS://TOS.ORG/OCEANOGRAPHY SPECIAL ISSUE ON SCIENTIFIC OCEAN DRILLING: LOOKING TO THE FUTURE HOW TO CREATE NEW SUBDUCTION ZONES A Global Perspective By Richard J. Arculus, Michael Gurnis, Osamu Ishizuka, Mark K. -
Avian Evolution, Gondwana Biogeography and the Cretaceous
doi 10.1098/rspb.2000.1368 Avian evolution, Gondwana biogeography and the Cretaceous±Tertiary mass extinction event Joel Cracraft Department of Ornithology, American Museum of Natural History, Central Park West at 79th Street, NewYork, NY 10024, USA ( [email protected]) The fossil record has been used to support the origin and radiation of modern birds (Neornithes) in Laurasia after the Cretaceous^Tertiary mass extinction event, whereas molecular clocks have suggested a Cretaceous origin for most avian orders.These alternative views of neornithine evolution are examined using an independent set of evidence, namely phylogenetic relationships and historical biogeography. Phylogenetic relationships of basal lineages of neornithines, including ratite birds and their allies (Palaeognathae), galliforms and anseriforms (Galloanserae), as well as lineages of the more advanced Neoaves (Gruiformes, Caprimulgiformes, Passeriformes and others) demonstrate pervasive trans- Antarctic distribution patterns.The temporal history of the neornithines can be inferred from fossil taxa and the ages of vicariance events, and along with their biogeographical patterns, leads to the conclusion that neornithines arose in Gondwana prior to the Cretaceous^Tertiary extinction event. Keywords: Neornithes; avian evolution; biogeography; Gondwana; Cretaceous^Tertiary extinction marker of neornithine beginnings.The fact that the 1. INTRODUCTION preponderance of the fossils are found in North America The relationships of modern birds, or Neornithes, to non- and Europe is taken as evidence that most higher taxa of avian theropods and Mesozoic pre-neornithine avian birds diversi¢ed on the Laurasian landmass and had lineages, is now well established (Chiappe 1995; Padian little, if anything, to do with Gondwana (Feduccia 1995). & Chiappe 1998; Chiappe et al. -
Morphology and History of the Kermadec Trench–Arc–Backarc
Marine Geology 159Ž. 1999 35±62 www.elsevier.nlrlocatermargeo Morphology and history of the Kermadec trench±arc±backarc basin±remnant arc system at 30 to 328S: geophysical profile, microfossil and K±Ar data Peter F. Ballance a,), Albert G. Ablaev b, Igor K. Pushchin b, Sergei P. Pletnev b, Maria G. Birylina b, Tetsumaru Itaya c, Harry A. Follas a,1, Graham W. Gibson a,2 a UniÕersity of Auckland, PriÕate Bag 92019, Auckland, New Zealand b Pacific Oceanological Institute, 43 Baltiyskaya Street, VladiÕostok 690041, Russian Federation c Research Institute of Natural Sciences, Okayama UniÕersity of Science, 1-1 Ridai-cho, Okayama 700, Japan Received 8 January 1998; accepted 27 November 1998 Abstract Knowledge of the time span of arc activity, essential for correct tectonic reconstructions, has been lacking for the Kermadec arc system, but is supplied in this paper through study of microfossils contained in dredge samples, and K±Ar ages on dredged basalt clasts. The Kermadec system at south latitudes 30 to 328 in the southwest Pacific comprises from west to east the Colville RidgeŽ. remnant arc , Havre Trough Ž backarc basin . , Kermadec Ridge Ž. active arc and Kermadec TrenchŽ site of west-dipping subduction of Pacific plate lithosphere beneath the Australian plate. Data are presented from two traversesŽ. dredge, magnetic, single-channel seismic across the whole system. An important transverse tectonic boundary, the 328S Boundary, lies between the two traverse lines and separates distinct northernŽ. 32±258S and southern Ž.32±368S sectors. The northern sector is shallower and well sedimented with broad ridges and a diffuse backarc basin. -
Telepresence-Enabled Exploration of The
! ! ! ! 2014 WORKSHOP TELEPRESENCE-ENABLED EXPLORATION OF THE !EASTERN PACIFIC OCEAN WHITE PAPER SUBMISSIONS ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! TABLE OF CONTENTS ! ! NORTHERN PACIFIC! Deep Hawaiian Slopes 7 Amy Baco-Taylor (Florida State University) USS Stickleback (SS-415) 9 Alexis Catsambis (Naval History and Heritage Command's Underwater Archaeology Branch) Sunken Battlefield of Midway 10 Alexis Catsambis (Naval History and Heritage Command's Underwater Archaeology Branch) Systematic Mapping of the California Continental Borderland from the Northern Channel Islands to Ensenada, Mexico 11 Jason Chaytor (USGS) Southern California Borderland 16 Marie-Helene Cormier (University of Rhode Island) Expanded Exploration of Approaches to Pearl Harbor and Seabed Impacts Off Oahu, Hawaii 20 James Delgado (NOAA ONMS Maritime Heritage Program) Gulf of the Farallones NMS Shipwrecks and Submerged Prehistoric Landscape 22 James Delgado (NOAA ONMS Maritime Heritage Program) USS Independence 24 James Delgado (NOAA ONMS Maritime Heritage Program) Battle of Midway Survey and Characterization of USS Yorktown 26 James Delgado (NOAA ONMS Maritime Heritage Program) Deep Oases: Seamounts and Food-Falls (Monterey Bay National Marine Sanctuary) 28 Andrew DeVogelaere (Monterey Bay National Marine Sanctuary) Lost Shipping Containers in the Deep: Trash, Time Capsules, Artificial Reefs, or Stepping Stones for Invasive Species? 31 Andrew DeVogelaere (Monterey Bay National Marine Sanctuary) Channel Islands Early Sites and Unmapped Wrecks 33 Lynn Dodd (University of Southern