The Change of Specific Term of Marine Geographical Names in Old Sea Charts
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Equinor Environmental Plan in Brief
Our EP in brief Exploring safely for oil and gas in the Great Australian Bight A guide to Equinor’s draft Environment Plan for Stromlo-1 Exploration Drilling Program Published by Equinor Australia B.V. www.equinor.com.au/gabproject February 2019 Our EP in brief This booklet is a guide to our draft EP for the Stromlo-1 Exploration Program in the Great Australian Bight. The full draft EP is 1,500 pages and has taken two years to prepare, with extensive dialogue and engagement with stakeholders shaping its development. We are committed to transparency and have published this guide as a tool to facilitate the public comment period. For more information, please visit our website. www.equinor.com.au/gabproject What are we planning to do? Can it be done safely? We are planning to drill one exploration well in the Over decades, we have drilled and produced safely Great Australian Bight in accordance with our work from similar conditions around the world. In the EP, we program for exploration permit EPP39. See page 7. demonstrate how this well can also be drilled safely. See page 14. Who are we? How will it be approved? We are Equinor, a global energy company producing oil, gas and renewable energy and are among the world’s largest We abide by the rules set by the regulator, NOPSEMA. We offshore operators. See page 15. are required to submit draft environmental management plans for assessment and acceptance before we can begin any activities offshore. See page 20. CONTENTS 8 12 What’s in it for Australia? How we’re shaping the future of energy If oil or gas is found in the Great Australian Bight, it could How can an oil and gas producer be highly significant for South be part of a sustainable energy Australia. -
Introduction to Co2 Chemistry in Sea Water
INTRODUCTION TO CO2 CHEMISTRY IN SEA WATER Andrew G. Dickson Scripps Institution of Oceanography, UC San Diego Mauna Loa Observatory, Hawaii Monthly Average Carbon Dioxide Concentration Data from Scripps CO Program Last updated August 2016 2 ? 410 400 390 380 370 2008; ~385 ppm 360 350 Concentration (ppm) 2 340 CO 330 1974; ~330 ppm 320 310 1960 1965 1970 1975 1980 1985 1990 1995 2000 2005 2010 2015 Year EFFECT OF ADDING CO2 TO SEA WATER 2− − CO2 + CO3 +H2O ! 2HCO3 O C O CO2 1. Dissolves in the ocean increase in decreases increases dissolved CO2 carbonate bicarbonate − HCO3 H O O also hydrogen ion concentration increases C H H 2. Reacts with water O O + H2O to form bicarbonate ion i.e., pH = –lg [H ] decreases H+ and hydrogen ion − HCO3 and saturation state of calcium carbonate decreases H+ 2− O O CO + 2− 3 3. Nearly all of that hydrogen [Ca ][CO ] C C H saturation Ω = 3 O O ion reacts with carbonate O O state K ion to form more bicarbonate sp (a measure of how “easy” it is to form a shell) M u l t i p l e o b s e r v e d indicators of a changing global carbon cycle: (a) atmospheric concentrations of carbon dioxide (CO2) from Mauna Loa (19°32´N, 155°34´W – red) and South Pole (89°59´S, 24°48´W – black) since 1958; (b) partial pressure of dissolved CO2 at the ocean surface (blue curves) and in situ pH (green curves), a measure of the acidity of ocean water. -
HIKING TRAILS SOUTH SUNSHINE COAST Sunshinecoastcanada.Com
HIKING TRAILS SOUTH SUNSHINE COAST sunshinecoastcanada.com Local Favourites ROBERTS CREEK heritage graveyard on the Sechelt First Nations band land at the east end. CLIFF GILKER PARK TRAILS ACCESS: From Highway 101 in Sechelt, access the walk- LENGTH & DIFFICULTY: 7 km of trails | 15 min to 2.5 hrs | way from Shorncliffe, Ocean, Trail, Inlet, or Wharf Avenues. GIBSONS Moderate Trails are colour coded and easy to follow and all loop back BURNETT FALLS GIBSONS SEAWALL to the parking lot. The park is a largely advanced second LENGTH & DIFFICULTY: 10-15 min one way | Very Easy LENGTH & DIFFICULTY: 20-30 min one way | Easy growth Douglas Fir forest. Roberts Creek and Clack Creek A short walk with a bit of an incline that ends at a spectacular Paved waterfront walkway with views of Gibsons Marina, flow through this park. The trails cross them at various view of the waterfall. points on rustic wooden bridges and the waterfall is a high- Gibsons Harbour, Keats Island and North Shore moun- ACCESS: 5396 Burnett Rd. From Sechelt, go north on light (especially in the winter time). Wheelchair accessible tains. Just steps away from shops and restaurants in Lower Wharf Ave. At the 4-way stop, turn right onto East Porpoise viewing platform. Gibsons. Bay Rd. Take a right turn on Burnett Rd. and park at the end. ACCESS: There are access points along Marine Drive and ACCESS: Follow Hwy 101 west from Gibsons for 10 km or Trailhead will be visible. Gower Point Road in Gibsons, including Armours Beach, drive east on Hwy 101 from Sechelt. -
Status of Pacific Island Coral Reef Fisheries by Tim Adams1, Paul Dalzell1 and Richard Farman2
Status of Pacific Island coral reef fisheries by Tim Adams1, Paul Dalzell1 and Richard Farman2 1. SPC Coastal Fisheries Programme 2. Service de la mer, Province Sud, Nouméa, New Caledonia (paper presented at 8th International Coral Reef Symposium, Panama, 1996) Abstract It is difficult to determine the status of fisheries on Pacific Islands coral reefs. The region is economically undeveloped, sparsely populated and its coral reefs are scattered over a vast area. Resultant constraints on monitoring and investigation mean that quantitative information is rare. The few available quantitative indicators are summarised here alongside opinions based on extensive practical experience. Most anecdotal reports about exploitation of Pacific Island marine life that reach the global press concern adverse aspects of fisheries and this, in context with the definite crises being experienced in other global fisheries, particularly southeast Asian reef-fisheries, has led to a general feeling of pessimism about the broad impact of fishing on Pacific Island reefs. However, the available evidence suggests that Pacific Island reef fisheries as a whole do not exert an excessive pressure on reefs and that (high) local protein nutritional demands can be sustained at least for the immediate future. However, it is urgent that this apparent overall sustainability be consolidated through state-recognised management arrangements; it is necessary that some specific overfishing problems be addressed; and it is particularly important that the adverse influence of terrestrial activities and run-off on the carrying capacity of coral reefs fisheries be mitigated. Introduction Fisheries on Pacific Island coral reefs, despite the increasing pace of outside influence, are still overwhelmingly subsistence fisheries. -
GEOG 101 PLACE NAME LIST for EXAM THREE
GEOG 101 PLACE NAME LIST for EXAM THREE Each exam will have a place name location map section based on the list below, plus countries and political units. Consult the appropriate maps in the atlas and textbook to locate these places. The atlas has a detailed INDEX. Exam III will focus on place names from Asia and Oceania. This section of the exam will be in the form of a matching question. You will match the names to numbers on a map. ________________________________________________________________________________ I. CONTINENTS Australia Asia ________________________________________________________________________________ II. OCEANS Pacific Indian Arctic ________________________________________________________________________________ III. ASIA Seas/Gulfs/Bays/Lakes: Caspian Sea Sea of Japan Arabian Sea South China Sea Red Sea Aral Sea Lake Baikal East China Sea Bering Sea Persian Gulf Bay of Bengal Sea of Okhotsk ________________________________________________________________________________ Islands: New Guinea Taiwan Sri Lanka Singapore Maldives Sakhalin Sumatra Borneo Java Honshu Philippines Luzon Mindanao Cyprus Hokkaido ________________________________________________________________________________ Straits/Canals: Str. of Malacca Bosporas Dardanelles Suez Canal Str. of Hormuz ________________________________________________________________________________ Rivers: Huang Yangtze Tigris Euphrates Amur Ob Mekong Indus Ganges Brahmaputra Lena _______________________________________________________________________________ Mountains, Plateaus, -
Chapter 5: Biostratigraphy
1 • PETROLEUM GEOLOGY OF SOUTH AUSTRALIA Volume 5: Great Australian Bight Biostratigraphy R Morgan1, AI Rowett2 and MR White3 5INTRODUCTION . 2 TERTIARY . 21 REFERENCES . 31 MIDDLE JURASSIC TO CRETACEOUS . 2 Palynology . .21 PLATE Palynology . .2 Zonation . .21 5.1 Horologinella sp. A, B, C and D, History of zonation . .2 Wells . .21 Jerboa 1 cuttings, 2400–05 m . 12 Zonation framework . .5 Western Bight Basin: FIGURES Wells . .8 Eyre Sub-basin . .21 5.1. Major features and well locations, Great Western Bight Basin: Central Bight Basin: Australian Bight . 4 central Ceduna Sub-basin . .22 Eyre Sub-basin . .10 5.2 Middle Jurassic to Cretaceous North–central Bight Basin: Eastern Bight Basin: Duntroon and biostratigraphic zonation of the Madura Shelf . .13 eastern Ceduna Sub-basins . .22 Bight and Polda Basins. 7 Central Bight Basin: central Foraminifera . .25 5.3 Middle Jurassic to Cretaceous Ceduna Sub-basin . .14 Zonation . .25 biostratigraphy (and older stratigraphy) Polda Basin . .14 Wells . .25 of wells in the Bight and Polda Basins . 9 Eastern Bight Basin: Duntroon Western Bight Basin: 5.4 Tertiary biostratigraphic zonation of the and eastern Ceduna Sub-basins . .15 Eyre Sub-basin . 25 portion of the Eucla Basin which overlies North–central Bight Basin: Foraminifera . .18 the Bight Basin and Tertiary foraminiferal Madura Shelf . .28 events recognised in southern Australia. 26 Summary . .19 Central Bight Basin: central 5.5 Integrated microfossil and palynological Permian to Middle Jurassic . .19 Ceduna Sub-basin . .29 Tertiary biostratigraphy of wells Cretaceous . .19 Eastern Bight Basin: Duntroon and penetrating the Eucla and Bight Basins 27 eastern Ceduna Sub-basins . -
Cleaning Symbiosis Among California Inshore Fishes
CLEANING SYMBIOSIS AMONG CALIFORNIA INSHORE FISHES EDMUNDS. HOBSON' ABSTRACT Cleaning symbiosis among shore fishes was studied during 1968 and 1969 in southern California, with work centered at La Jolla. Three species are habitual cleaners: the seAoriF, Ozyjulis californica; the sharpnose seaperch, Phanerodon atripes; and the kelp perch, Brachyistius frenatus. Because of specific differences in habitat, there is little overlap in the cleaning areas of these three spe- cies. Except for juvenile sharpnose seaperch, cleaning is of secondary significance to these species, even though it may be of major significance to certain individuals. The tendency to clean varies between in- dividuals. Principal prey of most members of these species are free-living organisms picked from a substrate and from midwater-a mode of feeding that favors adaptations suited to cleaning. Because it is exceedingly abundant in a variety of habitats, the seiiorita is the predominant inshore cleaning fish in California. Certain aspects of its cleaning relate to the fact that only a few of the many seiioritas present at a given time will clean, and that this activity is not centered around well-defined cleaning stations, as has been reported for certain cleaning fishes elsewhere. Probably because cleaners are difficult to recognize among the many seiioritas that do not clean, other fishes.generally do not at- tempt to initiate-cleaning; rather, the activity is consistently initiated by the cleaner itself. An infest- ed fish approached by a cleaner generally drifts into an unusual attitude that advertises the temporary existence of the transient cleaning station to other fish in need of service, and these converge on the cleaner. -
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future As more and more states are incorporating projections of sea-level rise into coastal planning efforts, the states of California, Oregon, and Washington asked the National Research Council to project sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account the many factors that affect sea-level rise on a local scale. The projections show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections; north of that point, sea-level rise is projected to be less than global projections because seismic strain is pushing the land upward. ny significant sea-level In compliance with a rise will pose enor- 2008 executive order, mous risks to the California state agencies have A been incorporating projec- valuable infrastructure, devel- opment, and wetlands that line tions of sea-level rise into much of the 1,600 mile shore- their coastal planning. This line of California, Oregon, and study provides the first Washington. For example, in comprehensive regional San Francisco Bay, two inter- projections of the changes in national airports, the ports of sea level expected in San Francisco and Oakland, a California, Oregon, and naval air station, freeways, Washington. housing developments, and sports stadiums have been Global Sea-Level Rise built on fill that raised the land Following a few thousand level only a few feet above the years of relative stability, highest tides. The San Francisco International Airport (center) global sea level has been Sea-level change is linked and surrounding areas will begin to flood with as rising since the late 19th or to changes in the Earth’s little as 40 cm (16 inches) of sea-level rise, a early 20th century, when climate. -
Relative Gut Lengths of Coral Reef Butterflyfishes (Pisces
Relative gut lengths of coral reef butterflyfishes (Pisces: Chaetodontidae) ML Berumen1, 2 *, MS Pratchett3, BA Goodman4 1. Red Sea Research Center, King Abdullah University of Science and Technology, Thuwal, 23955, Kingdom of Saudi Arabia 2. Biology Department, Woods Hole Oceanographic Institution, Woods Hole, MA, 02543, USA 3. ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, QLD 4811, Australia 4. Department of Ecology and Evolutionary Biology, University of Colorado, Boulder, CO, 80309 * Corresponding author: Email: [email protected] Phone: +966 544700019 Keywords: Chaetodontidae; corallivory; Papua New Guinea; relative gut length Abstract Variation in gut length of closely related animals is known to generally be a good predictor of dietary habits. We examined gut length in 28 species of butterflyfishes (Chaetodontidae), which encompass a wide range of dietary types (planktivores, omnivores, corallivores). We found general dietary patterns to be a good predictor of relative gut length, although we found high variation among groups and covariance with body size. The longest gut lengths are found in species that exclusively feed on the living tissue of corals, while the shortest gut length is found in a planktivorous species. Although we tried to control for phylogeny, corallivory has arisen multiple times in this family, confounding our analyses. The butterflyfishes, a speciose family with a wide range of dietary habits, may nonetheless provide an ideal system for future work studying gut physiology associated with specialisation and foraging behaviours. Introduction Relative gut lengths of vertebrates have long been studied and compared within and among species (e.g., Al-Hussaini 1949). The most common explanations for relatively longer guts in herbivores focus on the chemical defences of plants (e.g., Levin 1976; Hay and Fenical 1988), the indigestibility of plant fibre (e.g., Stevens 1989; Karasov and Martinez del Rio 2007), or the poor nutritional quality of plants as food. -
Our Ocean Backyard –– Santa Cruz Sentinel Columns by Gary Griggs, Director, Institute of Marine Sciences, UC Santa Cruz
Our Ocean Backyard –– Santa Cruz Sentinel columns by Gary Griggs, Director, Institute of Marine Sciences, UC Santa Cruz. #45 January 2, 2010 Why Monterey Submarine Canyon? Monterey Submarine Canyon forms a deep gash beneath the waters of Monterey Bay. At the risk of beating submarine canyons to death, I’m going to try to wrap up this discussion with some final thoughts on why we have one of the world’s largest submarine canyons in our backyard. Monterey Submarine Canyon has been known for over a century, and as with other offshore drainage systems, there has been considerable speculation over the years as to why we have this huge chasm cutting across the seafloor. Most submarine canyons align with river systems, but Elkhorn Slough hardly provides an adequate onshore source for such a massive feature. We do know that prior to 1910 the Salinas River discharged six miles north of its present mouth into Elkhorn Slough, closer to the head of Monterey Submarine Canyons. But even the Salinas River is not of the scale we would expect for an offshore feature as large as the Grand Canyon. Over 50 years ago, two geologists discovered the presence of a deep buried inland canyon beneath the Santa Cruz Mountains from oil company drill holes. This combined with other geological and geophysical observations strongly suggested that this canyon was eroded by an ancient river drainage system that played a critical role in the initial formation of the Monterey Submarine Canyon. This buried canyon, named Pajaro Gorge by some, was the route that the drainage from California’s vast Central Valley followed to the ocean for million of years. -
Marine Mammals and Sea Turtles of the Mediterranean and Black Seas
Marine mammals and sea turtles of the Mediterranean and Black Seas MEDITERRANEAN AND BLACK SEA BASINS Main seas, straits and gulfs in the Mediterranean and Black Sea basins, together with locations mentioned in the text for the distribution of marine mammals and sea turtles Ukraine Russia SEA OF AZOV Kerch Strait Crimea Romania Georgia Slovenia France Croatia BLACK SEA Bosnia & Herzegovina Bulgaria Monaco Bosphorus LIGURIAN SEA Montenegro Strait Pelagos Sanctuary Gulf of Italy Lion ADRIATIC SEA Albania Corsica Drini Bay Spain Dardanelles Strait Greece BALEARIC SEA Turkey Sardinia Algerian- TYRRHENIAN SEA AEGEAN SEA Balearic Islands Provençal IONIAN SEA Syria Basin Strait of Sicily Cyprus Strait of Sicily Gibraltar ALBORAN SEA Hellenic Trench Lebanon Tunisia Malta LEVANTINE SEA Israel Algeria West Morocco Bank Tunisian Plateau/Gulf of SirteMEDITERRANEAN SEA Gaza Strip Jordan Suez Canal Egypt Gulf of Sirte Libya RED SEA Marine mammals and sea turtles of the Mediterranean and Black Seas Compiled by María del Mar Otero and Michela Conigliaro The designation of geographical entities in this book, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN. Published by Compiled by María del Mar Otero IUCN Centre for Mediterranean Cooperation, Spain © IUCN, Gland, Switzerland, and Malaga, Spain Michela Conigliaro IUCN Centre for Mediterranean Cooperation, Spain Copyright © 2012 International Union for Conservation of Nature and Natural Resources With the support of Catherine Numa IUCN Centre for Mediterranean Cooperation, Spain Annabelle Cuttelod IUCN Species Programme, United Kingdom Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the sources are fully acknowledged. -
Modeling Regional Coastal Evolution in the Bight Of
MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA Ondoa Gregoire Abessolo, Magnus Larson, Rafael Almar, Bruno Castelle, Edward Anthony, Johan Reyns To cite this version: Ondoa Gregoire Abessolo, Magnus Larson, Rafael Almar, Bruno Castelle, Edward Anthony, et al.. MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA. Coastal Sediments’19, May 2019, Tampa, United States. 10.1142/9789811204487_0178. hal-02394959 HAL Id: hal-02394959 https://hal.archives-ouvertes.fr/hal-02394959 Submitted on 11 Dec 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA ONDOA GREGOIRE ABESSOLO1,2, MAGNUS LARSON3, RAFAEL ALMAR1, BRUNO CASTELLE4, EDWARD J. ANTHONY5, J. REYNS6,7 1. LEGOS, OMP, UMR 5566 (CNRS/CNES/IRD/Université de Toulouse), 14 Avenue Edouard Belin, 31400, Toulouse, France. [email protected], [email protected]. 2. Ecosystems and Fisheries Resources Laboratory, University of Douala, BP 2701, Douala, Cameroun. 3. Department of Water Resources Engineering, Lund University, Box 118, S-221 00, Lund, Sweden. [email protected]. 4. EPOC, OASU, UMR 5805 (CNRS - Université de Bordeaux), Allée Geoffroy Saint- Hilaire – CS 50023 – 33615, Pessac Cedex, France.