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Hikurangi Plateau: Crustal Structure, Rifted Formation, and Gondwana Subduction History
Article Geochemistry 3 Volume 9, Number 7 Geophysics 3 July 2008 Q07004, doi:10.1029/2007GC001855 GeosystemsG G ISSN: 1525-2027 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Click Here for Full Article Hikurangi Plateau: Crustal structure, rifted formation, and Gondwana subduction history Bryan Davy Institute of Geological and Nuclear Sciences, P.O. Box 30368, Lower Hutt, New Zealand ([email protected]) Kaj Hoernle IFM-GEOMAR, Wischhofstraße 1-3, D-24148 Kiel, Germany Reinhard Werner Tethys Geoconsulting GmbH, Wischhofstraße 1-3, D-24148 Kiel, Germany [1] Seismic reflection profiles across the Hikurangi Plateau Large Igneous Province and adjacent margins reveal the faulted volcanic basement and overlying Mesozoic-Cenozoic sedimentary units as well as the structure of the paleoconvergent Gondwana margin at the southern plateau limit. The Hikurangi Plateau crust can be traced 50–100 km southward beneath the Chatham Rise where subduction cessation timing and geometry are interpreted to be variable along the margin. A model fit of the Hikurangi Plateau back against the Manihiki Plateau aligns the Manihiki Scarp with the eastern margin of the Rekohu Embayment. Extensional and rotated block faults which formed during the breakup of the combined Manihiki- Hikurangi plateau are interpreted in seismic sections of the Hikurangi Plateau basement. Guyots and ridge- like seamounts which are widely scattered across the Hikurangi Plateau are interpreted to have formed at 99–89 Ma immediately following Hikurangi Plateau jamming of the Gondwana convergent margin at 100 Ma. Volcanism from this period cannot be separately resolved in the seismic reflection data from basement volcanism; hence seamount formation during Manihiki-Hikurangi Plateau emplacement and breakup (125–120 Ma) cannot be ruled out. -
Hoplostethus Atlanticus Fisheries Relating to the South Pacific Regional Fishery Management Organisation
SP-07-SWG-INF-09 Chile 13 May 2009 Information describing orange roughy Hoplostethus atlanticus fisheries relating to the South Pacific Regional Fishery Management Organisation WORKING DRAFT 04 MAY 2007 1. Overview ................................................................................................................ 2 2. Taxonomy .............................................................................................................. 3 2.1 Phylum ............................................................................................................. 3 2.2 Class ................................................................................................................. 3 2.3 Order ................................................................................................................ 3 2.4 Family .............................................................................................................. 3 2.5 Genus and species ............................................................................................ 3 2.6 Scientific synonyms ......................................................................................... 3 2.7 Common names ............................................................................................... 3 2.8 Molecular (DNA or biochemical) bar coding .................................................. 3 3. Species characteristics ........................................................................................... 4 3.1 Global distribution and depth range -
Mahimahi (Coryphaenamahimahi Hippurus)
mahimahi (CoryphaenaMahimahi hippurus) Mahimahi is the Hawaiian of Hawaii’s commercial landings Quality name that has become the common of mahimahi. Trollers catch nearly market name for this fish. It is also 40% of the landings. Schools of ma- Fresh mahimahi has a shelf life of known as dorado or dolphin (the himahi are common around flotsam 10 days if properly cared for. The fish, not the mammal) in other parts drifting at sea and near fish aggre- fish caught by trolling are only one of the country. When a mahimahi gation buoys. or two days on ice when landed and are typically fresher than the ma- takes the hook, its colors are bril- Although mahimahi have been liant blue and silver dappled with himahi caught by longline boats on raised successfully in tanks from extended trips. yellow. These fade quickly when the eggs to adults, the high cost has fish dies. made commercial aquaculture un- The first external evidence of de- Seasonality & How feasible to date. terioration in a whole mahimahi is They Are Caught softening and fading of bright skin Distribution: colors. In a dressed fish, discolor- Availability and Seasonality: The popularity of fresh mahimahi ation of the flesh exposed around Locally-caught mahimahi is avail- in the tourist industry and with resi- the collar bone would indicate a loss able most of the year, with peak dents has created a steady demand of quality. Mahimahi retains better catches usually March to May and for this fish and consistently good quality if it is not filleted until short- from September to November. -
Consumption Impacts by Marine Mammals, Fish, and Seabirds on The
83 Consumption impacts by marine mammals, fish, and seabirds on the Gulf of Maine–Georges Bank Atlantic herring (Clupea harengus) complex during the years 1977–2002 W. J. Overholtz and J. S. Link Overholtz, W. J. and Link, J. S. 2007. Consumption impacts by marine mammals, fish, and seabirds on the Gulf of Maine–Georges Bank Atlantic herring (Clupea harengus) complex during the years 1977–2002. ICES Journal of Marine Science, 64: 83–96. A comprehensive study of the impact of predation during the years 1977–2002 on the Gulf of Maine–Georges Bank herring complex is presented. An uncertainty approach was used to model input variables such as predator stock size, daily ration, and diet composition. Statistical distributions were constructed on the basis of available data, producing informative and uninformative inputs for estimating herring consumption within an uncertainty framework. Consumption of herring by predators tracked herring abundance closely during the study period, as this important prey species recovered following an almost complete collapse during the late 1960s and 1970s. Annual consumption of Atlantic herring by four groups of predators, demersal fish, marine mammals, large pelagic fish, and seabirds, averaged just 58 000 t in the late 1970s, increased to 123 000 t between 1986 and 1989, 290 000 t between 1990 and 1994, and 310 000 t during the years 1998–2002. Demersal fish consumed the largest proportion of this total, followed by marine mammals, large pelagic fish, and seabirds. Sensitivity analyses suggest that future emphasis should be placed on collecting time-series of diet composition data for marine mammals, large pelagic fish, and seabirds, with additional monitoring focused on the abundance of seabirds and daily rations of all groups. -
Benthic Invertebrate Bycatch from a Deep-Water Trawl Fishery, Chatham Rise, New Zealand
AQUATIC CONSERVATION: MARINE AND FRESHWATER ECOSYSTEMS, VOL. 7, 27±40 (1997) CASE STUDIES AND REVIEWS Benthic invertebrate bycatch from a deep-water trawl fishery, Chatham Rise, New Zealand P. KEITH PROBERT1, DON G. MCKNIGHT2 and SIMON L. GROVE1 1Department of Marine Science, University of Otago, PO Box 56, Dunedin, New Zealand 2National Institute of Water and Atmospheric Research Ltd, PO Box 14-901, Kilbirnie, Wellington, New Zealand ABSTRACT 1. Benthic invertebrate bycatch was collected during trawling for orange roughy (Hoplostethus atlanticus) at water depths of 662±1524 m on the northern and eastern Chatham Rise, New Zealand, in July 1994. Seventy-three trawl tows were examined, 49 from `flat' areas and 24 from two groups of `hills' (small seamounts). Benthos was recorded from 82% of all tows. 2. Some 96 benthic species were recorded including Ophiuroidea (12 spp.), Natantia (11 spp.), Asteroidea (11 spp.), Gorgonacea (11 spp.), Holothuroidea (7 spp.), and Porifera (6 spp.). 3. Cluster analysis showed the bycatch from flats and hills to differ significantly. Dominant taxa from flats were Holothuroidea, Asteroidea and Natantia; whereas taxa most commonly recorded from hills were Gorgonacea and Scleractinia. Bycatch from the two geographically separate groups of hills also differed significantly. 4. The largest bycatch volumes comprised corals from hills: Scleractinia (Goniocorella dumosa), Stylasteridae (Errina chathamensis) and Antipatharia (?Bathyplates platycaulus). Such large sessile epifauna may significantly increase the complexity of benthic habitat and trawling damage may thereby depress local biodiversity. Coral patches may require 4100 yr to recover. 5. Other environmental effects of deep-water trawling are briefly reviewed. 6. There is an urgent need to assess more fully the impact of trawling on seamount biotas and, in consequence, possible conservation measures. -
Order ZEIFORMES PARAZENIDAE Parazens P.C
click for previous page Zeiformes: Parazenidae 1203 Order ZEIFORMES PARAZENIDAE Parazens P.C. Heemstra, South African Institute for Aquatic Biodiversity, South Africa iagnostic characters: Small to moderate-sized (to 30 cm) oblong fishes, the head and body com- Dpressed; body depth slightly less than head length, contained 2.6 to 2.9 times in standard length; head naked, the bones thin and soft; opercular bones weakly serrate; mouth large, terminal, the upper jaw extremely protrusile; maxilla widely expanded posteriorly, and mostly exposed when mouth is closed; no supramaxilla; jaws with 1 or 2 rows of small, slender, conical teeth; vomer with a few short stout teeth;gill rakers (including rudiments) 2 on upper limb, 8 on lower limb.Eye diameter about 1/3 head length and slightly less than snout length.Branchiostegal rays 7.Dorsal fin divided, with 8 slender spines and 26 to 30 soft rays; anal fin with 1 minute spine and 30 to 32 soft rays; dorsal-, anal-, and pectoral-fin rays un- branched; caudal fin forked, with 11 principal rays and 9 branched rays; pectoral fin with 15 or 16 rays, shorter than eye diameter; pelvic fins with 1 unbranched and 5 or 6 branched soft rays, but no spine, fin origin posterior to a vertical at pectoral-fin base. Scales moderate in size, weakly ctenoid, and deciduous; 2 lateral lines originating on body at upper end of operculum and running posteriorly about 4 scale rows apart, gradually converging to form a single line on caudal peduncle. Caudal peduncle stout, the least depth about equal to its length and slightly less than eye diameter.Vertebrae 34.Colour: body reddish or silvery; large black blotch on anterior margin of dorsal fin. -
Charactensation of the Alfonsino (Beryx Splendens) Fishery in BYX 3
ISSN 1175-1584 MINISTRY OF FISHERIES Te Tautiaki i nga lid a Tangaroa Charactensation of the alfonsino (Beryx splendens) fishery in BYX 3 A. D. Langley N. A Walker New Zealand Fisheries Assessment Report 2002129 July 2002 Characterisation of the alfonsino (Beryx spZendm) fishery in BYX 3 A D. Langley N. A Walker Trophia Ltd PO Box 60 Kaikoura New Zealand Fisheries Assessment Report 2002129 July 2002 Published by Ministry of Fisheries Wellington 2002 ISSN 1175-1584 0 Ministry of Fisheries 2002 Citation: Langley, A.D.; Walker, N.A. (2002). Characterisation of the alfonsino (Beysplendens) fishery in BYX 3. New Zealand Fisheries Assessment Report 2002/29.40 p. This series continues the informal New Zealand Fisheries Assessment Research Document series which ceased at the end of 1999. EXECUTIVE SUMMARY Langley, A.D.; Walker, N.A. (2002). Characterisation of the alfonsino (Beryx splendem) fishery in BYX 3. New Zealand Fisheries Assessment Report 2002B9.40 p. Alfonsino, Belyx splendens, are distributed worldwide in temperate and bopical waters with the exception of the northeastern Pacific. The commercial fishery in New Zealand fishes seamounts and underwater ridges at depths ranging from 200 to 1000 m. In BYX 3, the alfonsino fishery off the east coast of the south island of New Zealand, a target trawl fishery has developed recently, particularly to the southeast of the Chatham Islands, which has resulted in a large increase in catches and a concomitant increase in bycatch of bluenose, EfypezogIypJze antarctica. These developments prompted concerns regarding the status of the stocks and the Ministry of Fisheries commissioned a review of the fishery. -
Oceanography and Marine Zoology of the New Zealand Subantarctic
44 ECOLOGY OF SUBANTARCTIC ISLANDS The highest temperatures recorded at Auck- REFERENCES land Is. and at Campbell 1. are much the same, approximately 65°F., and are 12°F. DE LISLE, J. F., 1964. Weather and climate of Campbell higher than that at Macquarie 1. (Table 12). Island. Pacific Ins. Monograph 7: 34-44. The extreme minimum at Macquarie I. is 10°F. lower than that at Port Ross. FABRICIUS, A. F., 1957. Climate of the Subantarctic Islands. In Meteorology of the Antarctic, ed. Van Sea temperatures at Campbell 1. are about Rooy. Weather Bureau, South Africa. 3°F. warmer than the earth temperatures at 12 inches in mid winter and about I!OF. colder FALLA, R. A., 1948. The outlying islands of New Zea- in midsummer (Table 13). land. N.Z. Geographer 4; 127-154. HITCHINGS, M. G., 1949. Campbell Island. A subantarc- TABLE 13. Mean monthly earth and sea tic meteorological station. Weather 4: 389-92. temperatures. Earth temp. Sea temp. MARSHALL, 0., 1909. The Meteorology of Campbell at 1 foot Campbell Auckland Island. In The Subantarctic Islands of New Zea- Campbell L I. Is. land, ed. C. Chilton. Philosophical Institute of Jan. 51.0 49.5 50.8 Canterbury. 2 vols. Feb. 50.3 49.t 51.0 Mar. 48.5 48.5 50.5 MAWSON, D., 1915. The home of the blizzard. Heine- man, London. 2 vols. A~ ~ ~ ~ May 43.2 45.3 47.4 NEWMAN, W., 1929. Tabulated and reduced records of June 40.3 43.2 46.1 the Macquarie Island Station. In Aust. -
Wasted Catch: Unsolved Problems in U.S. Fisheries
© Brian Skerry WASTED CATCH: UNSOLVED PROBLEMS IN U.S. FISHERIES Authors: Amanda Keledjian, Gib Brogan, Beth Lowell, Jon Warrenchuk, Ben Enticknap, Geoff Shester, Michael Hirshfield and Dominique Cano-Stocco CORRECTION: This report referenced a bycatch rate of 40% as determined by Davies et al. 2009, however that calculation used a broader definition of bycatch than is standard. According to bycatch as defined in this report and elsewhere, the most recent analyses show a rate of approximately 10% (Zeller et al. 2017; FAO 2018). © Brian Skerry ACCORDING TO SOME ESTIMATES, GLOBAL BYCATCH MAY AMOUNT TO 40 PERCENT OF THE WORLD’S CATCH, TOTALING 63 BILLION POUNDS PER YEAR CORRECTION: This report referenced a bycatch rate of 40% as determined by Davies et al. 2009, however that calculation used a broader definition of bycatch than is standard. According to bycatch as defined in this report and elsewhere, the most recent analyses show a rate of approximately 10% (Zeller et al. 2017; FAO 2018). CONTENTS 05 Executive Summary 06 Quick Facts 06 What Is Bycatch? 08 Bycatch Is An Undocumented Problem 10 Bycatch Occurs Every Day In The U.S. 15 Notable Progress, But No Solution 26 Nine Dirty Fisheries 37 National Policies To Minimize Bycatch 39 Recommendations 39 Conclusion 40 Oceana Reducing Bycatch: A Timeline 42 References ACKNOWLEDGEMENTS The authors would like to thank Jennifer Hueting and In-House Creative for graphic design and the following individuals for their contributions during the development and review of this report: Eric Bilsky, Dustin Cranor, Mike LeVine, Susan Murray, Jackie Savitz, Amelia Vorpahl, Sara Young and Beckie Zisser. -
Biological Results of the Chatham Islands 1954 Expedition
NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 139 (1) Biological Results of The Chatham Islands 1954 Expedition PART 1 Decapoda Brachyura by R. K. DELL Cumacea by N. S. JONES Decapoda Natantia by J. c, YALDWYN New Zealand Oceanographic Institute Memoir No. 4 1960 BIOLOGICAL RESULTS OF THE CHATHAM ISLANDS 1954 EXPEDITION PART 1 <i Photo: I). Marshall Sorting a trawl haul on the after deek NEW ZEALAND DEPARTMENT OF SCIENTIFIC AND INDUSTRIAL RESEARCH BULLETIN 139 (1) Biological Results of The Chatham Islands 1954 Expedition PART 1 Decapoda Brachyura by R. K. DELL Cumacea by N. S. JONES Decapoda Natantia by J. C. YALDWYN New Zealand Oceanographic Institute Memoir No. 4 Price 10/- 1960 N.Z. Dep. sci. industr. Res. Bull. 139 (1) (N.Z. oceanogr. Inst. Mem. 4) Printed by Wright & Carman Ltd., Wellington, New Zealand—1960 Under authority R. E. Owen, Government Printer, Wellington, N.Z. FOREWORD The Chatham Islands 1954 Expedition was organised and led by Prof. G. A. Knox of the Zoology Department of Canterbury University. The expedition was planned to explore the distribution of benthic and pelagic animals between the New Zealand coast and the Chatham Islands over the Chatham Rise, and to investigate the faunal affinities of the Chathams group, which lies in the Sub- tropical Convergence zone. A substantial grant towards the cost of the expedition was made by the Council for Scientific and Industrial Research on the recommendation of the N.Z. Oceanographic Committee: further financial support was given by Canterbury University, Canterbury Museum, Dominion Museum and Canterbury and South- land Branches of the Royal Society of New Zealand. -
38. Seismic Stratigraphy and Structure Adjacent to an Evolving Plate Boundary, Western Chatham Rise, New Zealand1
38. SEISMIC STRATIGRAPHY AND STRUCTURE ADJACENT TO AN EVOLVING PLATE BOUNDARY, WESTERN CHATHAM RISE, NEW ZEALAND1 K. B. Lewis, New Zealand Oceanographic Institute D. J. Bennett, Geophysics Division of the Department of Scientific and Industrial Research, New Zealand R. H. Herzer, New Zealand Geological Survey and C. C. von der Borch, Flinders University2 ABSTRACT Seismic profiles obtained from the eastern side of New Zealand, in transit to and from Site 594, illustrate the evolu- tion of the western end of the Chatham Rise and the southern extremity of the Hikurangi Trough. They show several unconformities and several major changes in tectonic and depositional regime. The unconformities represent major changes in oceanic circulation, possibly triggered by large lowerings of sea level in the late Oligocene and late Miocene. Tectonism is exemplified by a Late Cretaceous phase of block faulting, heralding the rift from Gondwanaland, and by Plio-Pleistocene normal faulting on the northern flank of the rise antithetic to the oblique-collision plate boundary in the southern Hikurangi Trough. This active normal faulting may indicate that the northwestern corner of Chatham Rise continental crust is being dragged down with the subducting slab to the north. The depositional regime has changed from Late Cretaceous infilling of fault-angle depressions, through an early Tertiary transgression and mid-Tertiary car- bonate drape, to a late Miocene-Recent sequence recording repeated glacial-interglacial events. This upper stratified unit onlaps a late Miocene erosion/phosphatization unconformity toward the crest of the rise. It is locally truncated by a slope-parallel erosion surface, with downslope buildup, which may indicate either current scour and deposition or mass movement. -
AWI Comments on Resolution on Food Security (IWC/65/10 Rev
AWI Comments on Resolution on Food Security (IWC/65/10 Rev 2). Food security is an important issue globally, nationally, and locally. With the exception of aboriginal subsistence whaling, however, the International Convention for the Regulation of Whaling which established the International Whaling Commission (IWC) is not – and was It has been well documented that marine fish stocks are never – considered a treaty that included food security in crisis. According to the FAO, the share of marine fish as a primary concern. Instead, there are numerous other stocks that are over-exploited has increased from 10 international conventions, declarations, and agencies percent in 1970 to nearly one third in 2009. A further 52 that have, as their primary focus, food security and percent of fish stocks are considered fully exploited. related issues. Such international fora include, inter alia, According to a 2012 report “Pirate Fishing Exposed – The the Food and Agriculture Organization’s Committee on Fight Against Illegal Fishing in West Africa and the EU” by World Food Security, the International Food Security the Environmental Justice Foundation: Treaty (proposed),1 and the Food Assistance Convention2 (formerly the Food Aid Convention3). Losses (globally) due to IUU fishing are estimated to be between US$10 billion and US$23.5 billion In addition, there are numerous reports and declarations per year, representing between 11 and 26 million on the subject, including a report entitled Sustainable tonnes of fish. West African waters are estimated Contribution