Lord Howe Island Marine Park (Commonwealth Waters)
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ISABEL SANMARTÍN (Uppsala, 2002) There Are Several Conflicting Hypothesis on the Paleogeographic History of the Southern Hemisp
A PALEOGEOGRAPHIC HISTORY OF THE SOUTHERN HEMISPHERE ISABEL SANMARTÍN (Uppsala, 2002) There are several conflicting hypothesis on the paleogeographic history of the Southern Hemisphere continents (Scotese et al., 1988; Kamp, 1980). The following account is my synthesis of ideas presented by Scotese et al. (1988), Veevers (1991), Veevers et al., (1991), Lawver et al., (1992), and McLoughlin (2001), as well as other authors. 140 Myr Figure 1 (I. Sanmartin, 2002) South Africa America SB DR d a New Guinea M India KP Australia Antarctic Antarctica Peninsula East Antarctica Figure 1 (200-120 Myr).- The southern supercontinent Gondwana was formed by the fusion of several cratons during the Late Proterozoic, following the break-up of the Mid-Proterozoic supercontinent Rodinia. In the Early Triassic, Gondwana and its northern counterpart Laurasia became welded together to form a single landmass, Pangea, surrounded by an ocean, Panthalassa. Although geographically connected, the biotas of Gondwana and Laurasia were partly isolated by a tropical continental zone in the west and the equatorial oceanic gulf of Tethys in the east (McLoughlin, 2001). The climate of Gondwana was not uniform. Paleobotanists and zoologists (Brenner, 1976; Amorim and Tozoni, 1994; Karol et al., 2000) recognize the existence of two climatic biotic provinces within Gondwana: a “Northern Tropical Gondwana” (northern South America, Africa, Madagascar, India, New Guinea and northern Australia), and a “Southern Temperate Gondwana” province (southern South America, south Africa, Australia, Antarctica, New Caledonia, and New Zealand). We will use this division here instead of the classic geographic separation into West (Africa + South America) and East Gondwana (Australia + Antarctica). -
Approaching the Prehistory of Norfolk Island
© Copyright Australian Museum, 2001 Records of the Australian Museum, Supplement 27 (2001): 1–9. ISBN 0 7347 2305 9 Approaching the Prehistory of Norfolk Island ATHOLL ANDERSON1 AND PETER WHITE2 1 Department of Archaeology & Natural History, Research School of Pacific and Asian Studies, Australian National University, Canberra ACT 0200, Australia [email protected] 2 Archaeology, University of Sydney, Sydney NSW 2006, Australia [email protected] ABSTRACT. Norfolk Island, on the northeast edge of the Tasman Sea, is of volcanic origin and moderate height. A humid, forested subtropical landmass, it had a diverse range of natural resources, including some food plants such as Cyathea, forest birds such as pigeon and parrot species and substantial colonies of seabirds, notably boobies and procellariids. Its shoreline had few shellfish, but the coastal waters were rich in fish, of which Lethrinids were especially abundant. The island had no inhabitants when discovered by Europeans in A.D. 1774. It was settled by them in A.D. 1788. From the eighteenth century discovery of feral bananas and then of stone adzes, knowledge of the prehistory of Norfolk Island has developed over a very long period. Collections of stone tools seemed predominantly East Polynesian in orientation, but Melanesian sources could not be ruled out. Research on fossil bone deposits established the antiquity of the human commensal Rattus exulans as about 800 B.P. but no prehistoric settlement site was known until one was discovered in 1995 at Emily Bay during the Norfolk Island Prehistory Project. ANDERSON, ATHOLL, AND PETER WHITE, 2001a. Approaching the prehistory of Norfolk Island. -
Explanatory Notes for the Tectonic Map of the Circum-Pacific Region Southwest Quadrant
U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP CP-37 U.S. GEOLOGICAL SURVEY Explanatory Notes for the Tectonic Map of the Circum-Pacific Region Southwest Quadrant 1:10,000,000 ICIRCUM-PACIFIC i • \ COUNCIL AND MINERAL RESOURCES 1991 CIRCUM-PACIFIC COUNCIL FOR ENERGY AND MINERAL RESOURCES Michel T. Halbouty, Chairman CIRCUM-PACIFIC MAP PROJECT John A. Reinemund, Director George Gryc, General Chairman Erwin Scheibner, Advisor, Tectonic Map Series EXPLANATORY NOTES FOR THE TECTONIC MAP OF THE CIRCUM-PACIFIC REGION SOUTHWEST QUADRANT 1:10,000,000 By Erwin Scheibner, Geological Survey of New South Wales, Sydney, 2001 N.S.W., Australia Tadashi Sato, Institute of Geoscience, University of Tsukuba, Ibaraki 305, Japan H. Frederick Doutch, Bureau of Mineral Resources, Canberra, A.C.T. 2601, Australia Warren O. Addicott, U.S. Geological Survey, Menlo Park, California 94025, U.S.A. M. J. Terman, U.S. Geological Survey, Reston, Virginia 22092, U.S.A. George W. Moore, Department of Geosciences, Oregon State University, Corvallis, Oregon 97331, U.S.A. 1991 Explanatory Notes to Supplement the TECTONIC MAP OF THE CIRCUM-PACIFTC REGION SOUTHWEST QUADRANT W. D. Palfreyman, Chairman Southwest Quadrant Panel CHIEF COMPILERS AND TECTONIC INTERPRETATIONS E. Scheibner, Geological Survey of New South Wales, Sydney, N.S.W. 2001 Australia T. Sato, Institute of Geosciences, University of Tsukuba, Ibaraki 305, Japan C. Craddock, Department of Geology and Geophysics, University of Wisconsin-Madison, Madison, Wisconsin 53706, U.S.A. TECTONIC ELEMENTS AND STRUCTURAL DATA AND INTERPRETATIONS J.-M. Auzende et al, Institut Francais de Recherche pour 1'Exploitacion de la Mer (IFREMER), Centre de Brest, B. -
Biogenic Habitats on New Zealand's Continental Shelf. Part II
Biogenic habitats on New Zealand’s continental shelf. Part II: National field survey and analysis New Zealand Aquatic Environment and Biodiversity Report No. 202 E.G. Jones M.A. Morrison N. Davey S. Mills A. Pallentin S. George M. Kelly I. Tuck ISSN 1179-6480 (online) ISBN 978-1-77665-966-1 (online) September 2018 Requests for further copies should be directed to: Publications Logistics Officer Ministry for Primary Industries PO Box 2526 WELLINGTON 6140 Email: [email protected] Telephone: 0800 00 83 33 Facsimile: 04-894 0300 This publication is also available on the Ministry for Primary Industries websites at: http://www.mpi.govt.nz/news-and-resources/publications http://fs.fish.govt.nz go to Document library/Research reports © Crown Copyright – Fisheries New Zealand TABLE OF CONTENTS EXECUTIVE SUMMARY 1 1. INTRODUCTION 3 1.1 Overview 3 1.2 Objectives 4 2. METHODS 5 2.1 Selection of locations for sampling. 5 2.2 Field survey design and data collection approach 6 2.3 Onboard data collection 7 2.4 Selection of core areas for post-voyage processing. 8 Multibeam data processing 8 DTIS imagery analysis 10 Reference libraries 10 Still image analysis 10 Video analysis 11 Identification of biological samples 11 Sediment analysis 11 Grain-size analysis 11 Total organic matter 12 Calcium carbonate content 12 2.5 Data Analysis of Core Areas 12 Benthic community characterization of core areas 12 Relating benthic community data to environmental variables 13 Fish community analysis from DTIS video counts 14 2.6 Synopsis Section 15 3. RESULTS 17 3.1 -
Parks Victoria Technical Series No
Deakin Research Online This is the published version: Barton, Jan, Pope, Adam and Howe, Steffan 2012, Marine protected areas of the Flinders and Twofold Shelf bioregions Parks Victoria, Melbourne, Vic. Available from Deakin Research Online: http://hdl.handle.net/10536/DRO/DU:30047221 Reproduced with the kind permission of the copyright owner. Copyright: 2012, Parks Victoria. Parks Victoria Technical Paper Series No. 79 Marine Natural Values Study (Vol 2) Marine Protected Areas of the Flinders and Twofold Shelf Bioregions Jan Barton, Adam Pope and Steffan Howe* School of Life & Environmental Sciences Deakin University *Parks Victoria August 2012 Parks Victoria Technical Series No. 79 Flinders and Twofold Shelf Bioregions Marine Natural Values Study EXECUTIVE SUMMARY Along Victoria’s coastline there are 30 Marine Protected Areas (MPAs) that have been established to protect the state’s significant marine environmental and cultural values. These MPAs include 13 Marine National Parks (MNPs), 11 Marine Sanctuaries (MSs), 3 Marine and Coastal Parks, 2 Marine Parks, and a Marine Reserve, and together these account for 11.7% of the Victorian marine environment. The highly protected Marine National Park System, which is made up of the MNPs and MSs, covers 5.3% of Victorian waters and was proclaimed in November 2002. This system has been designed to be representative of the diversity of Victoria’s marine environment and aims to conserve and protect ecological processes, habitats, and associated flora and fauna. The Marine National Park System is spread across Victoria’s five marine bioregions with multiple MNPs and MSs in each bioregion, with the exception of Flinders bioregion which has one MNP. -
Submarine Geology of the Tasman Sea
JIM C. STANDARD Dept. Geology and Geophysics, University of Sydney, Sydney, N.S.W., Australia Submarine Geology of the Tasman Sea Abstract: The physiographic features of the con- mum eastward development of the Australian tinental margin of eastern Australia, the Tasman continent. Lord Howe Rise is considered orogenic Basin, Lord Howe Rise, and the Coral Sea Platform in origin and probably of Early Paleozoic age. The are described and discussed geologically. Three Tasman Basin is a stable area underlain by per- guyots, each having more than 14,000 feet of relief manent ocean-type crust which may have acted as and a platform depth of less than 150 fathoms, are a nucleus for the eastward growth of the island mapped and described. arcs which lie between the Tasman Basin and the The present continental slope of southeastern South Pacific Basin. Australia west of the Tasman Basin marks the maxi- CONTENTS Introduction 1777 Figure Acknowledgments . 1777 1. Location map of the physiographic features of Bathymetry 1778 the Tasman Sea 1778 Physiographic features 1779 2. Profile from southeastern Australian coast to Continental margin 1779 Lord Howe Island; north-south profile of Tasman Basin 1781 guyots and east-west profile of Lord Howe Lord Howe Rise 1782 Rise 1780 Coral Sea Platform 1782 3. Profiles of continental shelf and slope of south- Geological interpretation 178? eastern Australia 1781 Tasman Basin 1783 4. East-west profile of Derwent Hunter Guyot . 1782 Seamounts and guyots 1784 Volcanic islands and reefs 1784 Plate Facing Lord Howe Rise and Coral Sea Platform 1785 1. Bathymetric map of the middle part of the Conclusions 1785 Tasman Sea 1782 References cited 1786 Table 1. -
A Revision of the Labrid Fish Genus Anampses
A Revision of the Labrid Fish Genus Anampses JoHN E. RANDALL1 Abstract The tropical Indo-Pacific wrasse genus Anampses is distinctive in possessing a single pair of broad· projecting incisiform teeth at the front of the jaws, scaleless head, smooth preopercular margin, complete lateral line, IX, 12 dorsal rays, and III, 12 anal rays. It is represented by two subgenera, Pseudanampses with 48 to 50 lateral-line scales (one species, A. geographicus) and Anampses with 26 or 27 lateral-line scales (11 species). Anampses femininus is described as new from specimens collected at Easter Island, Pitcairn, Rapa, New Caledonia, and Lord Howe Island. The female, bright orange with dark-edged blue stripes and a blue caudal peduncle and fin, is unusual in being even more colorful than the male, which is dusky yellow to blackish with vertical blue lines on the scales. The following pairs of nominal Anampses are here recognized as males and females of the same species (the first name of each pair has priority): 1) A. caeruleopunctatus Riippell 2) A. diadematus Riippell (male) 1) A. cuvier Quoy and Gaimard 2) A. godeffroyi Gunther (male) 1) A. chrysocephalus Randall (male) 2) A. rubrocaudatus Randall 1) A. neoguinaicus Bleeker (male) 2) A. fidjensis Sauvage 1) A. meleagrides Cuvier and Valenciennes 2) A. amboinensis Bleeker (male) More evidence is needed for the last pair in the above list, however, to be certain of conspecificity. A. tinkhami Fowler (1946) from the Ryukyu Islands is placed in the synonymy of A. caeruleopunctatus, the species with the broadest distribution of the genus: Red Sea to Easter Island, but not Hawaii. -
Annotated Checklist of the Fishes of Lord Howe Island
AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Allen, Gerald R., Douglass F. Hoese, John R. Paxton, J. E. Randall, C. Russell, W. A. Starck, F. H. Talbot, and G. P. Whitley, 1977. Annotated checklist of the fishes of Lord Howe Island. Records of the Australian Museum 30(15): 365–454. [21 December 1976]. doi:10.3853/j.0067-1975.30.1977.287 ISSN 0067-1975 Published by the Australian Museum, Sydney naturenature cultureculture discover discover AustralianAustralian Museum Museum science science is is freely freely accessible accessible online online at at www.australianmuseum.net.au/publications/www.australianmuseum.net.au/publications/ 66 CollegeCollege Street,Street, SydneySydney NSWNSW 2010,2010, AustraliaAustralia ANNOTATED CHECKLIST OF THE FISHES OF LORD HOWE ISLAND G. R. ALLEN, 1,2 D. F. HOESE,1 J. R. PAXTON,1 J. E. RANDALL, 3 B. C. RUSSELL},4 W. A. STARCK 11,1 F. H. TALBOT,1,4 AND G. P. WHITlEy5 SUMMARY lord Howe Island, some 630 kilometres off the northern coast of New South Wales, Australia at 31.5° South latitude, is the world's southern most locality with a well developed coral reef community and associated lagoon. An extensive collection of fishes from lord Howelsland was made during a month's expedition in February 1973. A total of 208 species are newly recorded from lord Howe Island and 23 species newly recorded from the Australian mainland. The fish fauna of lord Howe is increased to 447 species in 107 families. Of the 390 species of inshore fishes, the majority (60%) are wide-ranging tropical forms; some 10% are found only at lord Howe Island, southern Australia and/or New Zealand. -
Late Cretaceous to Present-Day Opening of the Southwest Pacific Constrained by Numerical Models and Seismic Tomography
University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers: part A Faculty of Science, Medicine and Health 1-1-2012 Late Cretaceous to present-day opening of the southwest Pacific constrained by numerical models and seismic tomography Kara J. Matthews University of Sydney Maria Seton University of Sydney Nicolas Flament University of Sydney, [email protected] R. Dietmar Muller University of Sydney Follow this and additional works at: https://ro.uow.edu.au/smhpapers Part of the Medicine and Health Sciences Commons, and the Social and Behavioral Sciences Commons Recommended Citation Matthews, Kara J.; Seton, Maria; Flament, Nicolas; and Muller, R. Dietmar, "Late Cretaceous to present-day opening of the southwest Pacific constrained by numerical models and seismic tomography" (2012). Faculty of Science, Medicine and Health - Papers: part A. 4387. https://ro.uow.edu.au/smhpapers/4387 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Late Cretaceous to present-day opening of the southwest Pacific constrained by numerical models and seismic tomography Abstract The southwest Pacific is a frontier region for petroleum exploration. A complex series of subduction and back-arc basin forming episodes characterises the late Cretaceous to present day evolution of the region. Controversial aspects of the regional tectonic history include the presence or lack of subduction between 83 and 43 Ma, the polarity of subduction, the timing of back-arc basin formation, and whether or not Pacific plate motion can be tied ot the motion of Australia via spreading in the Tasman Sea during the late Cretaceous-early Cenozoic. -
Historic Hybridization and Introgression Between Two Iconic Australian Anemonefish and Contemporary Patterns of Population Connectivity M
Historic hybridization and introgression between two iconic Australian anemonefish and contemporary patterns of population connectivity M. H. van der Meer12,G.P.Jones23, J.-P. A. Hobbs4 & L. van Herwerden1,2 1Molecular Ecology and Evolution Laboratory, Australian Tropical Sciences and Innovation Precinct, James Cook University, Townsville 4811, Australia 2School of Marine and Tropical Biology, James Cook University, Townsville 4811, Australia 3ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia 4The Oceans Institute and School of Plant Biology, The University of Western Australia, Crawley 6009, Australia Keywords Abstract Amphiprion, coral reef fish, endemism, extinction risk, Great Barrier Reef, isolated Endemic species on islands are considered at risk of extinction for several reasons, islands, Lord Howe Island. including limited dispersal abilities, small population sizes, and low genetic diver- sity. We used mitochondrial DNA (D-Loop) and 17 microsatellite loci to explore Correspondence the evolutionary relationship between an endemic anemonefish, Amphiprion mccul- M. H. van der Meer, Molecular Ecology and lochi (restricted to isolated locations in subtropical eastern Australia) and its more Evolution Laboratory, Australian Tropical widespread sister species, A. akindynos.AmitochondrialDNA(mtDNA)phylogram Sciences and Innovation Precinct, James Cook University, Townsville 4811, Australia. showed reciprocal monophyly was lacking for the two species, with two supported Tel: +61 (07)4871 5423; groups, each containing representatives of both species, but no shared haplotypes E-mail: [email protected] and up to 12 species, but not location-specific management units (MUs). Population genetic analyses suggested evolutionary connectivity among samples of each species Funded by Australian Department of the (mtDNA), while ecological connectivity was only evident among populations of the Environment and Water Resources, and endemic, A. -
Marine Communities Associated with the Frigate Canterbury and on Nearby Shores, Eastern Bay of Islands, 2012
Marine communities associated with the frigate Canterbury and on nearby shores, eastern Bay of Islands, 2012 Fish Forever Images ©Paihia Dive A report prepared for Ngati Kuta and Patukeha December 2012 1 Marine communities associated with the frigate Canterbury and on nearby shores, eastern Bay of Islands, 2012 Fish Forever* December 2012 Abstract The communities of animals and plants associated with the scuttled HMNZS Canterbury, and with the natural reefs of Maunganui Bay and other nearby shores in the eastern Bay of Islands, were examined by scuba divers and with still and video photography between 15 April and 26 May 2012. This sampling continued the time-series of observations required under the resource consent issued to the local Hapu to enable the sinking of the vessel in Maunganui Bay (Mountain Harte 2009a). The results of this sampling need to be considered in the light of the 2-year Rahui (ban on all fishing, except for the harvesting of kina) that was placed on Maunganui Bay in November 2009. Not all the sampling of previous years was repeated in 2012—for logistic reasons and because some was seen as unnecessary. On the other hand, new sampling—both method and area—was introduced. Most importantly, baited underwater video (BUV) drops gave standardised relative-abundance estimates of fish for sites within Maunganui Bay as well as on the nearby open coast. The percentage cover by sessile organisms of both the vertical and horizontal surfaces of the Canterbury increased significantly between July 2011 and April 2012, reaching the full coverage possible. (Note though that more than a quarter of the horizontal surfaces were covered in non-living material.) Although ‘species richness’ (more accurately, taxon richness) changed little, there were large changes in community structure. -
Comparative Phylogeography of Three Host Sea Anemones in the Indo-Pacific
Comparative phylogeography of three host sea anemones in the Indo-Pacific Item Type Article Authors Emms, Madeleine; Saenz-Agudelo, Pablo; Giles, Emily C.; Gatins, Remy; Nanninga, Gerrit B.; Scott, Anna; Hobbs, Jean-Paul A.; Frisch, Ashley J.; Mills, Suzanne C.; Beldade, Ricardo; Berumen, Michael L. Citation Emms, M. A., Saenz-Agudelo, P., Giles, E. C., Gatins, R., Nanninga, G. B., Scott, A., … Berumen, M. L. (2019). Comparative phylogeography of three host sea anemones in the Indo-Pacific. Journal of Biogeography. doi:10.1111/jbi.13775 Eprint version Post-print DOI 10.1111/jbi.13775 Publisher Wiley Journal Journal of Biogeography Rights Archived with thanks to Journal of Biogeography Download date 28/09/2021 17:55:44 Link to Item http://hdl.handle.net/10754/660912 1 COMPARATIVE PHYLOGEOGRAPHY OF THREE HOST SEA ANEMONES IN 2 THE INDO-PACIFIC 3 Running Title: Phylogeography of host sea anemones 4 5 MADELEINE A. EMMS1,2, PABLO SAENZ-AGUDELO3, EMILY C. GILES3, 6 REMY GATINS1,4, GERRIT B. NANNINGA2,8, ANNA SCOTT5, JEAN-PAUL A. 7 HOBBS6, ASHLEY J. FRISCH7, SUZANNE C. MILLS8,9, RICARDO BELDADE8,10 8 & MICHAEL L. BERUMEN1 9 1Red Sea Research Center, King Abdullah University of Science and Technology, 10 Thuwal, 23955-6900, Saudi Arabia. 2Department of Zoology, University of 11 Cambridge, Cambridge, CB2 3EJ, United Kingdom. 3Instituto de Ciencias 12 Ambientales y Evolutivas, Universidad Austral de Chile, Valdivia, 5090000, Chile. 13 4Department of Ecology and Evolutionary Biology, University of California Santa 14 Cruz115 McAllister Way, Santa Cruz, CA 95060, USA. 5National Marine Science 15 Centre and Marine Ecology Research Centre, School of Environmental Science and 16 Engineering, Southern Cross University, PO Box 4321, Coffs Harbour, New South 17 Wales 2450, Australia.