GREAT SOUTH BASIN CHECKSHOT SURVEY Marine Mammal
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Greenpeace Deep Sea Oil Briefing
May 2012 Out of our depth: Deep-sea oil exploration in New Zealand greenpeace.org.nz Contents A sea change in Government strategy ......... 4 Safety concerns .............................................. 5 The risks of deep-sea oil ............................... 6 International oil companies in the dock ..... 10 Where is deep-sea oil exploration taking place in New Zealand? ..................... 12 Cover: A view from an altitude of 3200 ft of the oil on the sea surface, originated by the leaking of the Deepwater Horizon wellhead disaster. The BP leased oil platform exploded April 20 and sank after burning, leaking an estimate of more than 200,000 gallons of crude oil per day from the broken pipeline into the sea. © Daniel Beltrá / Greenpeace Right: A penguin lies in oil spilt from the wreck of the Rena © GEMZ Photography 2 l Greenpeace Deep-Sea Oil Briefing l May 2012 The inability of the authorities to cope with the effects of the recent oil spill from the Rena cargo ship, despite the best efforts of Maritime New Zealand, has brought into sharp focus the environmental risks involved in the Government’s decision to open up vast swathes of the country’s coastal waters for deep-sea oil drilling. The Rena accident highlighted the devastation that can be caused by what in global terms is actually still a relatively small oil spill at 350 tonnes and shows the difficulties of mounting a clean-up operation even when the source of the leaking oil is so close to shore. It raised the spectre of the environmental catastrophe that could occur if an accident on the scale of the Deepwater Horizon disaster in the Gulf of Mexico were to occur in New Zealand’s remote waters. -
J. Mar. Biol. Ass. UK (1958) 37, 7°5-752
J. mar. biol. Ass. U.K. (1958) 37, 7°5-752 Printed in Great Britain OBSERVATIONS ON LUMINESCENCE IN PELAGIC ANIMALS By J. A. C. NICOL The Plymouth Laboratory (Plate I and Text-figs. 1-19) Luminescence is very common among marine animals, and many species possess highly developed photophores or light-emitting organs. It is probable, therefore, that luminescence plays an important part in the economy of their lives. A few determinations of the spectral composition and intensity of light emitted by marine animals are available (Coblentz & Hughes, 1926; Eymers & van Schouwenburg, 1937; Clarke & Backus, 1956; Kampa & Boden, 1957; Nicol, 1957b, c, 1958a, b). More data of this kind are desirable in order to estimate the visual efficiency of luminescence, distances at which luminescence can be perceived, the contribution it makes to general back• ground illumination, etc. With such information it should be possible to discuss. more profitably such biological problems as the role of luminescence in intraspecific signalling, sex recognition, swarming, and attraction or re• pulsion between species. As a contribution to this field I have measured the intensities of light emitted by some pelagic species of animals. Most of the work to be described in this paper was carried out during cruises of R. V. 'Sarsia' and RRS. 'Discovery II' (Marine Biological Association of the United Kingdom and National Institute of Oceanography, respectively). Collections were made at various stations in the East Atlantic between 30° N. and 48° N. The apparatus for measuring light intensities was calibrated ashore at the Plymouth Laboratory; measurements of animal light were made at sea. -
Grazing by Pyrosoma Atlanticum (Tunicata, Thaliacea) in the South Indian Ocean
MARINE ECOLOGY PROGRESS SERIES Vol. 330: 1–11, 2007 Published January 25 Mar Ecol Prog Ser OPENPEN ACCESSCCESS FEATURE ARTICLE Grazing by Pyrosoma atlanticum (Tunicata, Thaliacea) in the south Indian Ocean R. Perissinotto1,*, P. Mayzaud2, P. D. Nichols3, J. P. Labat2 1School of Biological & Conservation Sciences, G. Campbell Building, University of KwaZulu-Natal, Howard College Campus, Durban 4041, South Africa 2Océanographie Biochimique, Observatoire Océanologique, LOV-UMR CNRS 7093, BP 28, 06230 Villefranche-sur-Mer, France 3Commonwealth Scientific and Industrial Research Organisation (CSIRO), Marine and Atmospheric Research, Castray Esplanade, Hobart, Tasmania 7001, Australia ABSTRACT: Pyrosomas are colonial tunicates capable of forming dense aggregations. Their trophic function in the ocean, as well as their ecology and physiology in general, are extremely poorly known. During the ANTARES-4 survey (January and February 1999) their feeding dynamics were investigated in the south Indian Ocean. Results show that their in situ clearance rates may be among the highest recorded in any pelagic grazer, with up to 35 l h–1 per colony (length: 17.9 ± 4.3 [SD] cm). Gut pigment destruction rates, estimated for the first time in this tunicate group, are higher than those previously measured in salps and appendiculari- ans, ranging from 54 to virtually 100% (mean: 79.7 ± 19.8%) of total pigment ingested. Although individual colony ingestion rates were high (39.6 ± 17.3 [SD] µg –1 The pelagic tunicate Pyrosoma atlanticum conducts diel pigment d ), the total impact on the phytoplankton vertical migrations. Employing continuous jet propulsion, its biomass and production in the Agulhas Front was rela- colonies attain clearance rates that are among the highest in tively low, 0.01 to 4.91% and 0.02 to 5.74% respec- any zooplankton grazer. -
Planktonic Foraminifera As Oceanographic Proxies: Comparison of Biogeographic Classifications Using Some Southwest Pacific Core-Top Faunas
Hindawi Publishing Corporation ISRN Oceanography Volume 2013, Article ID 508184, 15 pages http://dx.doi.org/10.5402/2013/508184 Review Article Planktonic Foraminifera as Oceanographic Proxies: Comparison of Biogeographic Classifications Using Some Southwest Pacific Core-Top Faunas G. H. Scott GNS Science, 1 Fairway Drive, Lower Hutt 5010, New Zealand Correspondence should be addressed to G. H. Scott; [email protected] Received 29 April 2013; Accepted 17 June 2013 Academic Editors: M. Elskens and M. T. Maldonado Copyright © 2013 G. H. Scott. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The distribution of planktonic foraminifera, as free-floating protists, is largely controlled by hydrography. Their death assemblages in surficial sediments provide proxy data on upper water mass properties for paleoceanography. Techniques for mapping faunal distributions for this purpose are compared in a study of 35 core-top samples that span the Subtropical Front in the Southwest Pacific. Faunas are analyzed by taxon composition, order of dominant taxa, and abundance. Taxon composition (presence-absence data) and dominant taxa (ordinal data) recognize groups of sites that approximate major water mass distributions (cool subtropical water, subantarctic water) and clearly define the location of the Subtropical Front. Quantitative data (relative abundances) more closely reflect the success of taxa in upper water mass niches. This information resolves groups of sites that reflect differences in intrawater mass hydrography. Comparisons suggest that abundance data should provide much better oceanographic resolution globally than the widely used ordinal biogeographic classification that identifies only Tropical, Subtropical Transitional, Subpolar and Polar provinces. -
Stomach Content Analysis of Short-Finned Pilot Whales
f MARCH 1986 STOMACH CONTENT ANALYSIS OF SHORT-FINNED PILOT WHALES h (Globicephala macrorhynchus) AND NORTHERN ELEPHANT SEALS (Mirounga angustirostris) FROM THE SOUTHERN CALIFORNIA BIGHT by Elizabeth S. Hacker ADMINISTRATIVE REPORT LJ-86-08C f This Administrative Report is issued as an informal document to ensure prompt dissemination of preliminary results, interim reports and special studies. We recommend that it not be abstracted or cited. STOMACH CONTENT ANALYSIS OF SHORT-FINNED PILOT WHALES (GLOBICEPHALA MACRORHYNCHUS) AND NORTHERN ELEPHANT SEALS (MIROUNGA ANGUSTIROSTRIS) FROM THE SOUTHERN CALIFORNIA BIGHT Elizabeth S. Hacker College of Oceanography Oregon State University Corvallis, Oregon 97331 March 1986 S H i I , LIBRARY >66 MAR 0 2 2007 ‘ National uooarac & Atmospheric Administration U.S. Dept, of Commerce This report was prepared by Elizabeth S. Hacker under contract No. 84-ABA-02592 for the National Marine Fisheries Service, Southwest Fisheries Center, La Jolla, California. The statements, findings, conclusions and recommendations herein are those of the author and do not necessarily reflect the views of the National Marine Fisheries Service. Charles W. Oliver of the Southwest Fisheries Center served as Contract Officer's Technical Representative for this contract. ADMINISTRATIVE REPORT LJ-86-08C CONTENTS PAGE INTRODUCTION.................. 1 METHODS....................... 2 Sample Collection........ 2 Sample Identification.... 2 Sample Analysis.......... 3 RESULTS....................... 3 Globicephala macrorhynchus 3 Mirounga angustirostris... 4 DISCUSSION.................... 6 ACKNOWLEDGEMENTS.............. 11 REFERENCES.............. 12 i LIST OF TABLES TABLE PAGE 1 Collection data for Globicephala macrorhynchus examined from the Southern California Bight........ 19 2 Collection data for Mirounga angustirostris examined from the Southern California Bight........ 20 3 Stomach contents of Globicephala macrorhynchus examined from the Southern California Bight....... -
Campbell Plateau: a Major Control on the SW Pacific Sector of The
Ocean Sci. Discuss., doi:10.5194/os-2017-36, 2017 Manuscript under review for journal Ocean Sci. Discussion started: 15 May 2017 c Author(s) 2017. CC-BY 3.0 License. Campbell Plateau: A major control on the SW Pacific sector of the Southern Ocean circulation. Aitana Forcén-Vázquez1,2, Michael J. M. Williams1, Melissa Bowen3, Lionel Carter2, and Helen Bostock1 1NIWA 2Victoria University of Wellington 3The University of Auckland Correspondence to: Aitana ([email protected]) Abstract. New Zealand’s subantarctic region is a dynamic oceanographic zone with the Subtropical Front (STF) to the north and the Subantarctic Front (SAF) to the south. Both the fronts and their associated currents are strongly influenced by topog- raphy: the South Island of New Zealand and the Chatham Rise for the STF, and Macquarie Ridge and Campbell Plateau for the SAF. Here for the first time we present a consistent picture across the subantarctic region of the relationships between front 5 positions, bathymetry and water mass structure using eight high resolution oceanographic sections that span the region. Our results show that the northwest side of Campbell Plateau is comparatively warm due to a southward extension of the STF over the plateau. The SAF is steered south and east by Macquarie Ridge and Campbell Plateau, with waters originating in the SAF also found north of the plateau in the Bounty Trough. Subantarctic Mode Water (SAMW) formation is confirmed to exist south of the plateau on the northern side of the SAF in winter, while on Campbell Plateau a deep reservoir persists into the following 10 autumn. -
Geophysical Structure of the Southern Alps Orogen, South Island, New Zealand
Regional Geophysics chapter 15/04/2007 1 GEOPHYSICAL STRUCTURE OF THE SOUTHERN ALPS OROGEN, SOUTH ISLAND, NEW ZEALAND. F J Davey1, D Eberhart-Phillips2, M D Kohler3, S Bannister1, G Caldwell1, S Henrys1, M Scherwath4, T Stern5, and H van Avendonk6 1GNS Science, Gracefield, Lower Hutt, New Zealand, [email protected] 2GNS Science, Dunedin, New Zealand 3Center for Embedded Networked Sensing, University of California, Los Angeles, California, USA 4Leibniz-Institute of Marine Sciences, IFM-GEOMAR, Kiel, Germany 5School of Earth Sciences, Victoria University of Wellington, Wellington, New Zealand 6Institute of Geophysics, University of Texas, Austin, Texas, USA ABSTRACT The central part of the South Island of New Zealand is a product of the transpressive continental collision of the Pacific and Australian plates during the past 5 million years, prior to which the plate boundary was largely transcurrent for over 10 My. Subduction occurs at the north (west dipping) and south (east dipping) of South Island. The deformation is largely accommodated by the ramping up of the Pacific plate over the Australian plate and near-symmetric mantle shortening. The initial asymmetric crustal deformation may be the result of an initial difference in lithospheric strength or an inherited suture resulting from earlier plate motions. Delamination of the Pacific plate occurs resulting in the uplift and exposure of mid- crustal rocks at the plate boundary fault (Alpine fault) to form a foreland mountain chain. In addition, an asymmetric crustal root (additional 8 - 17 km) is formed, with an underlying mantle downwarp. The crustal root, which thickens southwards, comprises the delaminated lower crust and a thickened overlying middle crust. -
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 . -
(Cciea) California Current Ecosystem Status Report, 2020
Agenda Item G.1.a IEA Team Report 2 March 2020 SUPPLEMENTARY MATERIALS TO THE CALIFORNIA CURRENT INTEGRATED ECOSYSTEM ASSESSMENT (CCIEA) CALIFORNIA CURRENT ECOSYSTEM STATUS REPORT, 2020 Appendix A LIST OF CONTRIBUTORS TO THIS REPORT, BY AFFILIATION NWFSC, NOAA Fisheries SWFSC, NOAA Fisheries Mr. Kelly Andrews Dr. Eric Bjorkstedt Ms. Katie Barnas Dr. Steven Bograd Dr. Richard Brodeur Ms. Lynn deWitt Dr. Brian Burke Dr. John Field Dr. Jason Cope Dr. Newell (Toby) Garfield (co-lead editor) Dr. Correigh Greene Dr. Elliott Hazen Dr. Thomas Good Dr. Michael Jacox Dr. Chris Harvey (co-lead editor) Dr. Andrew Leising Dr. Daniel Holland Dr. Nate Mantua Dr. Kym Jacobson Mr. Keith Sakuma Dr. Stephanie Moore Dr. Jarrod Santora Dr. Stuart Munsch Dr. Andrew Thompson Dr. Karma Norman Dr. Brian Wells Dr. Jameal Samhouri Dr. Thomas Williams Dr. Nick Tolimieri (co-editor) University of California-Santa Cruz Ms. Margaret Williams Ms. Rebecca Miller Dr. Jeannette Zamon Dr. Barbara Muhling Pacific States Marine Fishery Commission Dr. Isaac Schroeder Ms. Amanda Phillips Humboldt State University Mr. Gregory Williams (co-editor) Ms. Roxanne Robertson Oregon State University California Department of Public Health Ms. Jennifer Fisher Ms. Christina Grant Ms. Cheryl Morgan Mr. Duy Trong Ms. Samantha Zeman Ms. Vanessa Zubkousky-White AFSC, NOAA Fisheries California Department of Fish and Wildlife Dr. Stephen Kasperski Ms. Christy Juhasz Dr. Sharon Melin CA Office of Env. Health Hazard Assessment NOAA Fisheries West Coast Region Dr. Rebecca Stanton Mr. Dan Lawson Oregon Department of Fish and Wildlife Farallon Institute Dr. Caren Braby Dr. William Sydeman Mr. Matthew Hunter Point Blue Conservation Science Oregon Department of Agriculture Dr. -
Distribution, Associations and Role in the Biological Carbon Pump of Pyrosoma Atlanticum (Tunicata, Thaliacea) Off Cabo Verde, N
www.nature.com/scientificreports OPEN Distribution, associations and role in the biological carbon pump of Pyrosoma atlanticum (Tunicata, Thaliacea) of Cabo Verde, NE Atlantic Vanessa I. Stenvers1,2,3*, Helena Hauss1, Karen J. Osborn2,4, Philipp Neitzel1, Véronique Merten1, Stella Scheer1, Bruce H. Robison4, Rui Freitas5 & Henk Jan T. Hoving1* Gelatinous zooplankton are increasingly acknowledged to contribute signifcantly to the carbon cycle worldwide, yet many taxa within this diverse group remain poorly studied. Here, we investigate the pelagic tunicate Pyrosoma atlanticum in the waters surrounding the Cabo Verde Archipelago. By using a combination of pelagic and benthic in situ observations, sampling, and molecular genetic analyses (barcoding, eDNA), we reveal that: P. atlanticum abundance is most likely driven by local island- induced productivity, that it substantially contributes to the organic carbon export fux and is part of a diverse range of biological interactions. Downward migrating pyrosomes actively transported an estimated 13% of their fecal pellets below the mixed layer, equaling a carbon fux of 1.96–64.55 mg C m−2 day−1. We show that analysis of eDNA can detect pyrosome material beyond their migration range, suggesting that pyrosomes have ecological impacts below the upper water column. Moribund P. atlanticum colonies contributed an average of 15.09 ± 17.89 (s.d.) mg C m−2 to the carbon fux reaching the island benthic slopes. Our pelagic in situ observations further show that P. atlanticum formed an abundant substrate in the water column (reaching up to 0.28 m2 substrate area per m2), with animals using pyrosomes for settlement, as a shelter and/or a food source. -
Bulletin 100, United States National Museum
PYROSOMA.—A TAXONOMIC STUDY, BASED UPON THE COLLECTIONS OF THE UNITED STATES BUREAU OF FISHERIES AND THE UNITED STATES NATIONAL MUSEUM. By Maynard M. Metcalf and Hoyt S. Hopkins, Oj Oberlin, Ohio. INTRODUCTION. The family Pyrosomidae is generally regarded as containing but one genus Pyrosoma. There are, however, two very distinct groups in the family, the Pyrosomata ambulata and the Pyrosomata Jlxata, which might as properly be regarded as two separate genera. In this paper we are treating them as subgenera, although it would be equally well to give each group its own generic name. The members of the family all have the form of free swimming, tubular colonies, and they all emit a strong phosphorescent light. They are said to be the most brilliantly luminous of all marine organisms. Pijrosorna was first described by Peron (1804), and was later more thoroughly studied by Lesueur (1815). The earlier specimens known came from the Atlantic Ocean and Mediterranean Sea, but many have since been collected from all seas, with the exception of the Arctic Ocean. About sixteen species and varieties are now known, including the new forms described in this paper, whereas previous to the year 1895 only three had been described. In that year appeared Seeliger's memoir, "Die Pyrosomen der Plankton Expedition," and this was followed by important memoirs by Neumann and others upon collec- tions made by different oceanographic expeditions. The anatomy, embryology, and budding have been well studied, but little is known of the behavior of the living animals or of their physiology. Our studies are based upon the remarkably rich collections of the United States Fisheries Steamer Albatross in Philippine waters during the years 1908 and 1909 and upon the extensive collections in the United States National Museum, made almost wholly by vessels of the United States Bureau of Fisheries, chiefly the steamer Albatross, which since 1883 has been almost continuously engaged in oceano- graphic studies. -
Seismic Characteristics of Polygonal Fault Systems in the Great South Basin, New Zealand During the Diagenesis Process
Open Geosciences 2020; 12: 851–865 Research Article Sukonmeth Jitmahantakul, Piyaphong Chenrai*, Pitsanupong Kanjanapayont, and Waruntorn Kanitpanyacharoen Seismic characteristics of polygonal fault systems in the Great South Basin, New Zealand https://doi.org/10.1515/geo-2020-0177 during the diagenesis process. Interpretation of the received January 30, 2020; accepted June 12, 2020 polygonal fault in this area is useful in assessing the Abstract: Awell-developed multi-tier polygonal fault migration pathway and seal ability of the Eocene mudstone system is located in the Great South Basin offshore New sequence in the Great South Basin. Zealand’s South Island. The system has been characterised Keywords: seismic interpretation, polygonal fault using a high-quality three-dimensional seismic survey tied system, Great South Basin to available exploration boreholes using regional two- dimensional seismic data. In this study area, two polygonal fault intervals are identified and analysed, Tier 1 and Tier 2. Tier 1 coincides with the Tucker Cove Formation (Late 1 Introduction Eocene) with small polygonal faults. Tier 2 is restricted to ( ) - the Paleocene-to-Late Eocene interval with a great number Since polygonal fault systems PFSs have been dis of large faults. In map view, polygonal fault cells are covered in sedimentary basins worldwide, many PFSs outlined by a series of conjugate pairs of normal faults. The have been studied with respect to petroleum exploration, - polygonal faults are demonstrated to be controlled by such as their seal capacity and as a paleo stress [ – ] ( ) fi depositional facies, specifically offshore bathyal deposits indicator 1 5 . Henriet et al. 1991 rst described PFS characterised by fine-grained clays, marls and muds.