Evaluating the Environmental Impacts of Fracking in New Zealand: an Interim Report
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NIWA Client Report No: WLG2013-44 Report Date: August 2013 NIWA Project: TTR11301
Geological Desktop Summary Active Permit areas 50753 (55581), 54068 and 54272, South Taranaki Bight Prepared for Trans-Tasman Resources Limited August 2013 20 August 2013 2.07 p.m. Authors/Contributors: Alan R. Orpin For any information regarding this report please contact: Alan Orpin Marine Sedimentologist Ocean Sediments +64-4-386 0356 [email protected] National Institute of Water & Atmospheric Research Ltd 301 Evans Bay Parade, Greta Point Wellington 6021 Private Bag 14901, Kilbirnie Wellington 6241 New Zealand Phone +64-4-386 0300 Fax +64-4-386 0574 NIWA Client Report No: WLG2013-44 Report date: August 2013 NIWA Project: TTR11301 © All rights reserved. This publication may not be reproduced or copied in any form without the permission of the copyright owner(s). Such permission is only to be given in accordance with the terms of the client’s contract with NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. Whilst NIWA has used all reasonable endeavours to ensure that the information contained in this document is accurate, NIWA does not give any express or implied warranty as to the completeness of the information contained herein, or that it will be suitable for any purpose(s) other than those specifically contemplated during the Project or agreed by NIWA and the Client. 20 August 2013 2.07 p.m. Contents Executive summary ..................................................................................................... 6 1 Overview ............................................................................................................ -
ABSTRACTS Deep-Sea Biology Symposium 2018 Updated: 18-Sep-2018 • Symposium Page
ABSTRACTS Deep-Sea Biology Symposium 2018 Updated: 18-Sep-2018 • Symposium Page NOTE: These abstracts are should not be cited in bibliographies. SESSIONS • Advances in taxonomy and phylogeny • James J. Childress • Autecology • Mining impacts • Biodiversity and ecosystem • Natural and anthropogenic functioning disturbance • Chemosynthetic ecosystems • Pelagic systems • Connectivity and biogeography • Seamounts and canyons • Corals • Technology and observing systems • Deep-ocean stewardship • Trophic ecology • Deep-sea 'omics solely on metabarcoding approaches, where genetic diversity cannot Advances in taxonomy and always be linked to an individual and/or species. phylogenetics - TALKS TALK - Advances in taxonomy and phylogenetics - ABSTRACT 263 TUESDAY Midday • 13:30 • San Carlos Room TALK - Advances in taxonomy and phylogenetics - ABSTRACT 174 Eastern Pacific scaleworms (Polynoidae, TUESDAY Midday • 13:15 • San Carlos Room The impact of intragenomic variation on Annelida) from seeps, vents and alpha-diversity estimations in whalefalls. metabarcoding studies: A case study Gregory Rouse, Avery Hiley, Sigrid Katz, Johanna Lindgren based on 18S rRNA amplicon data from Scripps Institution of Oceanography Sampling across deep sea habitats ranging from methane seeps (Oregon, marine nematodes California, Mexico Costa Rica), whale falls (California) and hydrothermal vents (Juan de Fuca, Gulf of California, EPR, Galapagos) has resulted in a Tiago Jose Pereira, Holly Bik remarkable diversity of undescribed polynoid scaleworms. We demonstrate University of California, Riverside this via DNA sequencing and morphology with respect to the range of Although intragenomic variation has been recognized as a common already described eastern Pacific polynoids. However, a series of phenomenon amongst eukaryote taxa, its effects on diversity estimations taxonomic problems cannot be solved until specimens from their (i.e. -
Tracking Submarine Volcanic Activity at Monowai: Constraints from Long-Range Hydroacoustic Measurements
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by OceanRep Tracking submarine volcanic activity at Monowai: Constraints from long-range hydroacoustic measurements Authors: D. Metz1*, A. B. Watts1, I. Grevemeyer2, M. Rodgers3 1Department of Earth Sciences, South Parks Road, Oxford OX1 3AN, United Kingdom 2GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany 3School of Geosciences, University of South Florida, Tampa, Florida, USA * Now at: Research and Development Center for Earthquake and Tsunami, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Kanagawa, Japan Corresponding Author: Dirk Metz ([email protected]) Highlights - Volcanic activity at Monowai is detected by an IMS hydrophone array at Juan Fernández Islands, Southeast Pacific Ocean - 82 discrete episodes of activity have been identified in a 3.5-year record - Monowai is one of the most active submarine arc volcanoes currently known Index Terms: Monowai, submarine volcanism, hydroacoustics, Pacific Ocean, IMS, CTBTO This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process which may lead to differences between this version and the Version of Record. Please cite this article as doi: 10.1029/2018JB015888 © 2018 American Geophysical Union. All rights reserved. Abstract Monowai is a submarine volcanic center in the Kermadec Arc, Southwest Pacific Ocean. In the past, activity at the volcano had been intermittently observed in the form of fallout at the sea surface, discolored water, changes in seafloor topography, and T phase seismicity, but there is no continuous record for more recent years. -
Abbot Ice Shelf, Structure of the Amundsen Sea Continental 10.1002/2014GC005570 Margin and the Southern Boundary of the Bellingshausen Plate
PUBLICATIONS Geochemistry, Geophysics, Geosystems RESEARCH ARTICLE Abbot Ice Shelf, structure of the Amundsen Sea continental 10.1002/2014GC005570 margin and the southern boundary of the Bellingshausen Plate Key Points: seaward of West Antarctica Abbot Ice Shelf is underlain by E-W rift basins created at 90 Ma James R. Cochran1, Kirsty J. Tinto1, and Robin E. Bell1 Amundsen shelf shaped by subsidence, sedimentation, and 1Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York, USA passage of the ice sheet Bellingshausen plate boundary is located near the base of continental Abstract Inversion of NASA Operation IceBridge airborne gravity over the Abbot Ice Shelf in West Ant- slope and rise arctica for subice bathymetry defines an extensional terrain made up of east-west trending rift basins formed during the early stages of Antarctica/Zealandia rifting. Extension is minor, as rifting jumped north of Correspondence to: J. R. Cochran, Thurston Island early in the rifting process. The Amundsen Sea Embayment continental shelf west of the [email protected] rifted terrain is underlain by a deeper, more extensive sedimentary basin also formed during rifting between Antarctica and Zealandia. A well-defined boundary zone separates the mildly extended Abbot extensional Citation: terrain from the deeper Amundsen Embayment shelf basin. The shelf basin has an extension factor, b,of Cochran, J. R., K. J. Tinto, and R. E. Bell 1.5–1.7 with 80–100 km of extension occurring across an area now 250 km wide. Following this extension, (2015), Abbot Ice Shelf, structure of the Amundsen Sea continental margin and rifting centered north of the present shelf edge and proceeded to continental rupture. -
Cruise Report SONNE 192/2 MANGO
Schwarz-Schampera, U., Botz, R., Hannington, M., Adamson, R., Anger, V., Cormany, D., Evans, L., Gibson, H., Haase, K., Hirdes, W., Hocking, M., Juniper, K., Langley, S., Leybourne, M., Metaxas, A., Mills, R., Ostertag-Henning, Chr., Rauch, M., Rutkowski, J., Schmidt, M., Shepherd, K., Stevens, C., Tamburri, K., Tracey, D., Westernstroer, U. Cruise Report SONNE 192/2 MANGO Marine Geoscientific Research on Input and Output in the Tonga-Kermadec Subduction Zone Marine Geowissenschaftliche Untersuchungen zum In- und Output der Tonga-Kermadec Subduktionszone Auckland, New Zealand – Suva, Fiji 26 April – 17 May 2007 TABLE OF CONTENTS 1 Summary………………………………………………………………………………. 3 2 Acknowledgements…………………………………………………………………… 8 3 Participants……………………………………………………………………………. 9 4 Cruise Narrative ……………………………………………………………………… 10 5 Structure, Bathymetry and Sampling of the Tonga-Kermadec Arc………............. 15 5.1 Objectives of the Tonga-Kermadec Arc Hydrothermal and Volcanological Program. 15 5.2 Bay of Plenty, Calypso Vent Sites…………………………………………………… 16 5.2.1 Bathymetry and Structure………………………………………………………….. 16 5.2.2 ROPOS Operations………………………………………………………………… 19 5.2.3. Sampling…………………………………………………………………………....24 5.3 Monowai Seamount, Northern Kermadec Arc………………………………………. 26 5.3.1 Bathymetry and Structure………………………………………………………….. 26 5.3.2 ROPOS Operations………………………………………………………………… 30 5.3.3 Sampling…………………………………………………………………………….34 5.4 Volcano U (#21), Northern Kermadec Arc…………………………………………... 37 5.4.1 Bathymetry and Structure…………………………………………………………... 37 5.4.2 -
Subduction of the Oceanic Hikurangi Plateau and Its Impact on the Kermadec Arc
ARTICLE Received 1 Apr 2014 | Accepted 6 Aug 2014 | Published 17 Sep 2014 DOI: 10.1038/ncomms5923 Subduction of the oceanic Hikurangi Plateau and its impact on the Kermadec arc Christian Timm1, Bryan Davy1, Karsten Haase2, Kaj A. Hoernle3, Ian J. Graham1, Cornel E.J. de Ronde1, Jon Woodhead4, Dan Bassett5, Folkmar Hauff3, Nick Mortimer6, Hannu C. Seebeck1, Richard J. Wysoczanski7, Fabio Caratori-Tontini1 & John A. Gamble8 Large igneous province subduction is a rare process on Earth. A modern example is the subduction of the oceanic Hikurangi Plateau beneath the southern Kermadec arc, offshore New Zealand. This segment of the arc has the largest total lava volume erupted and the highest volcano density of the entire Kermadec arc. Here we show that Kermadec arc lavas south of B32°S have elevated Pb and Sr and low Nd isotope ratios, which argues, together with increasing seafloor depth, forearc retreat and crustal thinning, for initial Hikurangi Plateau—Kermadec arc collision B250 km north of its present position. The combined data set indicates that a much larger portion of the Hikurangi Plateau (the missing Ontong Java Nui piece) than previously believed has already been subducted. Oblique plate convergence caused southward migration of the thickened and buoyant oceanic plateau crust, creating a buoyant ‘Hikurangi’ me´lange beneath the Moho that interacts with ascending arc melts. 1 GNS Science, PO Box 30-368, Lower Hutt 5040, New Zealand. 2 Geozentrum Nordbayern, Universita¨t Erlangen-Nu¨rnberg, Schlossgarten 5, 91054 Erlangen, Germany. 3 GEOMAR Helmholtz Centre for Ocean Research, FB4, Wischhofstrasse 1-3, 24148 Kiel, Germany. -
SCUFN30-03.1A LIST of DECISIONS and ACTIONS from SCUFN-29
SCUFN30-03.1A LIST of DECISIONS and ACTIONS from SCUFN-29 (Status at the date of 16 August 2017) Note: DECISIONS have been kept in the list and highlighted in light grey when implemented (names now available in the GEBCO Gazetteer, for instance). Status & Decision/ Agenda Details Comments Action Item (Aug 2017) 1 Opening and Administrative Arrangements Done for IOC to replace N. Cherkis – K. IHO and IOC Secretariats to prepare calls for SCUFN Dobrolyubova Membership possible vacancies as appropriate and no selected. SCUFN29/01 later than September 2017 so new nominees can Call for investigate possibility of participating in SCUFN31 vacancies by (2018). e-mail from Sec 31 May 2017. SCUFN Sec. to circulate the Excel spreadsheet Complete depicting the status and future plans/deadlines of SCUFN29/02 SCUFN Membership to SCUFN Members and IOC Secretariat’s representative. SCUFN Members agreed to add Marine Regions’ Complete SCUFN29/03 SCUFN point of contact (Mr Simon Claus) in the SCUFN Membership List as an Observer. Sec. to update the SCUFN Membership List with Ms Complete SCUFN29/04 Jennifer Jencks as new NOAA’s point of contact for the GEBCO Gazetteer. 2 Introduction by SCUFN Chair - Approval of Agenda SCUFN Chair invited SCUFN Members in general, to Done. See give top priority consideration to short specific names SCUFN29-06A, that are in relation with marine geophysics, §II.A.1 & II.A.4. SCUFN29/05 hydrographic and oceanographic sciences. Subsequent amendment to emphasize this statement, to be considered for inclusion in the future new Edition of B-6. 3 Matters remaining from Previous Meetings Review of Actions from SCUFN-28 and transfer to the 3.1 relevant agenda items SCUFN30-03.1A Status & Decision/ Agenda Details Comments Action Item (Aug 2017) Following action SCUFN28/94, SCUFN Members SCUFN29/06 agreed not to submit an article in Hydro International. -
On the Fate of Pumice Rafts Formed During the 2012 Havre Submarine Eruption
ARTICLE Received 9 Oct 2013 | Accepted 14 Mar 2014 | Published 22 Apr 2014 DOI: 10.1038/ncomms4660 OPEN On the fate of pumice rafts formed during the 2012 Havre submarine eruption Martin Jutzeler1,2, Robert Marsh3, Rebecca J. Carey4, James D.L. White2, Peter J. Talling1 & Leif Karlstrom5 Pumice rafts are floating mobile accumulations of low-density pumice clasts generated by silicic volcanic eruptions. Pumice in rafts can drift for years, become waterlogged and sink, or become stranded on shorelines. Here we show that the pumice raft formed by the impressive, deep submarine eruption of the Havre caldera volcano (Southwest Pacific) in July 2012 can be mapped by satellite imagery augmented by sailing crew observations. Far from coastal interference, the eruption produced a single 4400 km2 raft in 1 day, thus initiating a gigantic, high-precision, natural experiment relevant to both modern and prehistoric oceanic surface dispersal dynamics. Observed raft dispersal can be accurately reproduced by simulating drift and dispersal patterns using currents from an eddy-resolving ocean model hindcast. For future eruptions that produce potentially hazardous pumice rafts, our technique allows real- time forecasts of dispersal routes, in addition to inference of ash/pumice deposit distribution in the deep ocean. 1 National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK. 2 Department of Geology, University of Otago, PO Box 56, Dunedin 9056, New Zealand. 3 Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton, European Way, Southampton SO14 3ZH, UK. 4 CODES—ARC Centre of Excellence in Ore Deposits, University of Tasmania, PO Box 79, Hobart 7005, Australia. -
Proceedings of Kermadec Discoveries and Connections
Proceedings of Kermadec Discoveries and Connections Science Symposium April 11-12, 2016 Academy Galleries, Queens Wharf, Wellington PROCEEDINGS OF KERMADEC – DISCOVERIES AND CONNECTIONS ISBN: 978-0-473-36137-2 Edited by: Bronwen Golder and Amelia Connell, The Pew Charitable Trusts PO Box 25459 Wellington New Zealand Kermadec – Discoveries and Connections, Wellington, New Zealand, 11-12 April 2016 Suggested citation: Author Name(s). 2016, Article title. In B Golder and A Connell (Eds.) Proceedings of Kermadec – Discoveries and Connections. Paper presented at Kermadec – Discoveries and Connections, Wellington, New Zealand (inclusive page numbers). The Pew Charitable Trusts. The Pew Charitable Trusts is driven by the power of knowledge to solve today’s most challenging problems. Pew applies a rigorous, analytical approach to improve public policy, inform the public, and invigorate civic life. Cover images: ©2016 Jason O’Hara DISCOVERIES AND CONNECTIONS – these are words that excite our imagination and inspire scientific endeavour. The Kermadec region of New Zealand Readers of this Proceedings Document will BRONWEN GOLDER, represents the last frontier in marine and find the descriptors ‘unique’, ‘never before DIRECTOR, KERMADEC island exploration. The near pristine waters seen’, ‘first record’, ‘new species’, and INITIATIVE, GLOBAL OCEAN and island ecology of the Kermadecs offer ‘distinct’ used frequently in the papers LEGACY, THE PEW scientists and conservation agencies a presented – yet further scientific CHARITABLE TRUSTS unique research and management confirmation that the habitats, species and [email protected] opportunity. oceanic processes and connections of the Kermadec region are a globally significant. In 2010 The Pew Charitable Trusts hosted the first ever Kermadec Science Symposium Scientists presenting to the Symposium also - DEEP – Talks and Thoughts Celebrating explored the opportunities for scientific Diversity in New Zealand’s Untouched research that the recently proposed Kermadecs. -
Benthic Community Structure and Environmental Drivers on Monowai Seamount, Kermadec Volcanic Arc
Benthic community structure and environmental drivers on Monowai Seamount, Kermadec volcanic arc Niharika Dutt Long A thesis submitted for the degree of Master of Science At University of Otago, Dunedin, New Zealand 26 June 2014 ABSTRACT Seamounts are spatially isolated, underwater topographical features that extend more than 1 km above the seafloor. They are products of geological processes, and exhibit diverse forms of venting as a result of volcanism due to plate tectonics. Environmental factors vary greatly on seamounts, due to which they support communities of specialist chemosynthetic invertebrates, suspension-feeding fauna, and large mobile megafauna including many commercially-important fish species. In addition to threats from benthic trawling, seamounts are now viewed as repositories for Seafloor Massive Sulphide (SMS) deposits, owing to their venting activity. The seamounts of the 2500 km-long Tonga-Kermadec volcanic arc are diverse in their hydrothermal activity and, therefore, are potentially of mining interest. Species diversity and abundances differ within and between seamounts of the Kermadec volcanic arc, according to prevailing environmental factors. Three abiotic variables (i.e. water depth, substrate type, proximity to vent sites) were chosen in order to examine their effect on taxa richness, abundances, and benthic community structure for the current study on Monowai Seamount, northern Kermadec volcanic arc. Monowai Caldera was explored as part of the 2005 New Zealand-American Pacific Ring of Fire, using the submersible Pisces V. 4500 still images and 16 hours of video footage for three dives were acquired for recording data on substrate type, water depth, proximity to vent sites, taxa abundance, and composition. -
Talk S and Though T S Celebr a T Ing D Iversit Y in N Ew Zeal And's U N T
TALKS AND THOUGHTS CELEBRATING DIVERSITY IN NEW ZEALand’s UNTOUCHED KERMADECS From the earliest Polynesian voyagers, to whalers and pioneers, sailors and conservationists, the Kermadec region has attracted those who are keen to push the boundaries, to see what lies beyond the horizon. INTO THE UNKNOWN. A 0 kilometres 400 0 nautical miles 200 FRONTIER WILDERNESS DEEP – these are words that excite our imagination and inspire scientific endeavour. Straddling the known and unknown of our The papers presented at DEEP, and now knowledge and understanding, frontiers published here, represent the work and have always inspired enthusiasm for scientific knowledge of today’s Kermadec explorers. exploration and discovery. Frontiers are They range across the disciplines of geology, where the unknown draws attention and biology, history and anthropology. Each paper propels curious explorers off on new and is a detailed profiling of specific places, species DEEP Talks and Thoughts Celebrating inspiring journeys. and patterns of life across the Kermadec region. Diversity in New Zealand’s Read as a collection, they provide us with our Untouched Kermadecs. New Zealand’s Kermadec region is such a first opportunity to understand how the features frontier – a place that has drawn explorers HOSTED BY of this region come together and interact in one from all corners of the globe for generations. Pew Environment Group of the world’s great ocean wilderness areas. and Te Papa Tongarewa From the earliest Polynesian voyagers AUGUST 2010 to whalers and pioneers, sailors and Discovery, connection, collaboration – more conservationists, the Kermadec region has words to excite and inspire. attracted those who are keen to push the DEEP provided a unique opportunity to explore boundaries, to see what lies beyond the a remarkable place.