Reef Check Australia – GBR Project Report
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7 Day Gbr Itinerary
7 DAY & 7 NIGHT GREAT BARRIER REEF ITINERARY PORT DOUGLAS | GREAT BARRIER REEF | COOKTOWN | LIZARD ISLAND PORT DOUGLAS Port Douglas is a town on the Coral Sea in the tropical far north of Queensland, Australia. Located a scenic 50 minute drive north of Cairns International airport, It's known for its luxury beach resorts and as a base for visits to both the Great Barrier Reef, the world's largest reef system, and Daintree National Park, home to biodiverse rainforest. In town, Macrossan Street is lined with boutique shops and restaurants. Curving south is popular Four Mile Beach. THE RIBBON REEFS - GREAT BARRIER REEF - Characteristically no wider than 450m, the Ribbon Reefs are part of the Great Barrier Reef Marina Park and are covered in colorful corals that attract a plethora of reef life big and small, with sandy gullies separating them, themselves containing interesting critters. The Ribbons reef host several of Australia’s most spectacular dive sites, as well as arguably the most prolific Black Marlin fishing in the world at certain times of year -with general fishing topping the list also. LIZARD ISLAND Lizard Island hosts Australia’s northernmost island resort. It is located 150 miles north of Cairns and 57 miles north east off the coast from Cooktown. Lizard Island is an absolute tropical paradise, a haven of isolation, gratification and relaxation. Accessible by boat and small aircraft, this tropical haven is a bucket list destination. Prominent dives spots on the Ribbon Reefs are generally quite shallow, with bommies coming up to as high as 5 metres below the surface from a sandy bottom that is between 15-20 metres below the surface. -
Australia's Coral Sea - How Much Do We Know?
Proceedings of the 12 th International Coral Reef Symposium, Cairns, Australia, 9-13 July 2012 18E The management of the Coral Sea reefs and sea mounts Australia's Coral Sea - how much do we know? Daniela M. Ceccarelli 1 1PO Box 215, Magnetic Island QLD 4819 Australia Corresponding author: [email protected] Abstract. Recent efforts to implement management zoning to Australia’s portion of the Coral Sea have highlighted the need for a synthesis of information about the area’s physical structure, oceanography and ecology. Current knowledge is hampered by large geographic and temporal gaps in existing research, but nevertheless underpins the determination of areas of ecological value and conservation significance. This review draws together existing research on the Coral Sea’s coral reefs and seamounts and evaluates their potential function at a regional scale. Only four coral reefs, out of a potential 36, have been studied to the point of providing information at a community level; this information exists for none of the 14 mapped seamounts. However, the research volume has increased exponentially in the last decade, allowing a more general analysis of likely patterns and processes. Clear habitat associations are emerging and each new study adds to the’ Coral Sea species list’. Broader research suggests that the reefs and seamounts serve as dispersal stepping stones, potential refugia from disturbances and aggregation hotspots for pelagic predators. Key words: Isolated reefs, Dispersal, Community structure, Refugia. Introduction Australia’s Coral Sea lies to the east of the Great Barrier Reef (GBR) within the Australian EEZ boundaries. Geologically, it is dominated by large plateaux that rise from the abyssal plain and cover approximately half of the seabed area (Harris et al. -
Coral Reef Education and Australian High School Students
CORAL REEF EDUCATION AND AUSTRALIAN HIGH SCHOOL STUDENTS by Carl M. Stepath, MEd PhD Candidate: School of Education, and School of Tropical Environment Studies & Geography; James Cook University, Cairns, Qld 4878, Australia, [email protected] In proceedings of the Marine Education Society of Australasia 2004 Conference, Noosa, Queensland, October 2-3, 2004. Keywords: tropical marine education, environmental and marine experiential education, environmental awareness and attitudes, ecological agency, coral reef education Abstract: This paper reports on a PhD research project investigating marine education in coral reef environments along the Queensland coast. The study explored relationships between awareness, attitudes and ecological skills of high school students who were trained in coral reef ecology and monitoring in offshore sites along the Great Barrier Reef in 2002 and 2003. The research investigated the question of whether experiential marine education can change the reported environmental knowledge, attitudes and ecological agency of student participants. Some key data outcomes are presented and implications for effective marine education strategies discussed. Introduction Educational programs that focus on humans and their relationship to coral reefs are becoming necessary, as reef structures along the Queensland coast come under mounting ecological pressure (GBRMPA, 2003; Hughes et al., 2003; Talbot, 1995). Marine education has been defined by Roseanne Fortner (1991) as that part of the total educational process that enables people to develop sensitivity to and a general understanding of the role of the seas in human affairs and the impact of society on the marine and aquatic environments. Improving pedagogical techniques concerning aquatic environments is valuable since continuing intensification of human activity near coastline areas adversely affects marine and coastal ecosystems worldwide (NOAA, 1998). -
Great Barrier Reef Marine Park Authority Technical Memorandun Gbrmpa - Tm-5
GREAT BARRIER REEF MARINE PARK AUTHORITY TECHNICAL MEMORANDUN GBRMPA - TM-5 REPORT OF SCIENTIFIC DISCUSSION MEETING ON THE PHYSICAL OCEANOGRAPHYOF THE GREAT BARRIER REEF REGION Held at the University of New South Wales 5-6 July 1982 with support from the Great Barrier Reef Marine Park Authority and the Australian Academy of Science i. _. JASON H. MIDDLETON SUMMARY A scientific discussion meeting was held in July 1982 to generate a statement concerning the physical oceanography of the Great Barrier Reef region. The statement was to be framed by answering the questions below: .. (a) What is the present state of knowledge? (b) What appear to be the most important unanswered questions? (c) With regard to (a) and (b), what methods would be‘mogt effective in answering the questions posed in (b)? (d) What routine monitoring measurements would appear to be of most scientific value in increasing our knowledge of the region? This report summarises the discussions of the meeting. Technical Memoranda are of a preliminary nature, representing the views of the author and do not necessarily represent the views of the Great Barrier Reef Marine Park Authority. Postal Address: The Chairman, Great Barrier Reef Marine Park Authority, P.O. Box 1379, TOWNSVILLE. QLD. 4810 -l- 1. SUMMARYOF IMPORTANT SCIENTIFIC QUESTIONS The meeting identified a number of important scientific questions. These were of two types: (i) What is the description of certain events? and (ii) Which model is needed to predict these events. Considering events in decreasing time scale, the following . I statements summarize the important questions addressed in the body of the report. -
Cairns Outer Great Barrier Reef
CAIRNS OUTER GREAT BARRIER REEF Cairns fastest, most spacious and luxurious vessel From $165 + $20 LEVY Full Day Reef Cruise Unlimited Snorkelling and up to three Certified Dives! Adventure awaits on board the fastest, award-winning Adult Child Family $ $ $ luxury vessel EVOLUTION, the best value tour to the 185 95 485 Outer Great Barrier Reef in Cairns. TOUR INCLUDES *INCLUDES $20 LEVY PAYABLE ON BOARD TWO OUTER REEF SITES FASTEST REEF VESSEL SNORKEL HIRE HOT BBQ CHEESE & FRUIT PLATTER, WINE FIVE HOURS REEF TIME BUFFET LUNCH LIVE ENTERTAINMENT EXPERIENCED DIVE MODERN AIR SPACIOUS SUN DECKS INSTRUCTORS CONDITIONED BOAT FOR SUNBATHING DEPARTS CAIRNS REEF FLEET TERMINAL DAILY RETURN TRANSFERS DAILY FROM CAIRNS CBD ($17) CHECK IN 7:15am DEPARTS 8:15am RETURNS 4:30pm. AND NORTHERN BEACHES ($24). CAPE TRIBULATION Agincourt Reef C o nti n e Two Outerntal Reef Sites Undine Reef S St Crispin Reef h e Locations selected for lfclarity of water Opal Reef Rudder Reef & abundance of Marine Life Tongue Reef PORT DOUGLAS Norman Reef Saxon Reef Batt Reef Hastings Reef Pixie Reef Breaking Patches Michaelmas Cay Oyster Reef Vlasoff Cay Upolo Cay Double PALM COVE Island Green Island Arlington Reef KURANDA Moore Reef Skyrail Kuranda Scenic Rail CAIRNS Fitzroy Island MAP NOT TO SCALE Extras Prebooked Only Only $50 $10 $25 INTRO & CERTIFIED DIVES SEMI-SUBMERSIBLE TOURS MARINE BIOLOGY TOURS Scuba Dive without any previous experience, or Enjoy the spectacular coral formations without Learn the secrets of the reef from our Marine use your Scuba Certification to explore the Great getting wet on our semi submersible tour with Biologist and then explore the coral gardens Barrier Reef. -
PRESS RELEASE –Embargoed Until February 13, 2020 Cancun, Mexico * Belize City, Belize * Guatemala City, Guatemala * Tegucigalpa, Honduras
Melanie McField Director-Healthy Reefs Initiative /Smithsonian Institution Cell: (754) 610 9311, [email protected], Skype: melaniemcfield -------------------------------------------------------------- PRESS RELEASE –embargoed until February 13, 2020 Cancun, Mexico * Belize City, Belize * Guatemala City, Guatemala * Tegucigalpa, Honduras CARIBBEAN’S LARGEST BARRIER CORAL REEF SYSTEM FACES NEW THREATS, BUT ALSO TESTS NEW SOLUTIONS (Mesoamerican Reef – February 13th, 2020) -- The Healthy Reefs for Healthy People Initiative (HRI) today released its 2020 Mesoamerican Reef Health Report Card. For the first time in 12 years of tracking the health of the largest barrier reef in the Western Hemisphere, the overall condition of this vital ecosystem has deteriorated. The Reef Health Index (RHI), which synthesizes ecological data into a “Dow Jones” style index, decreased from 2.8 in 2016 to 2.5 in 2018. Despite the recent decline, reef health still shows improvement compared to 2006 when the HRI monitoring efforts began. A similar report released last summer for Australia’s Great Barrier Reef also marked a dramatic reduction in reef condition, signaling a worrisome outlook for two of the world’s most important reef systems in different hemispheres of the globe. ”Over the past decade we have documented a slow but positive recovery of the Mesoamerican Barrier Reef System,” according to Dr. Melanie McField, Director of the Healthy Reefs Initiative and marine scientist with the Smithsonian Institution, “but this recent decline highlights the need to step up local actions to improve water quality and increase fish populations and accelerate international commitments to reduce carbon emissions in order to halt climate change impacts on reefs.” The report is based on a new study of 286 coral reef sites along 1000 km of the Caribbean coasts of Mexico, Belize, Guatemala, and Honduras. -
SEDIMENTARY FRAMEWORK of Lmainland FRINGING REEF DEVELOPMENT, CAPE TRIBULATION AREA
GREAT BARRIER REEF MARINE PARK AUTHORITY TECHNICAL MEMORANDUM GBRMPA-TM-14 SEDIMENTARY FRAMEWORK OF lMAINLAND FRINGING REEF DEVELOPMENT, CAPE TRIBULATION AREA D.P. JOHNSON and RM.CARTER Department of Geology James Cook University of North Queensland Townsville, Q 4811, Australia DATE November, 1987 SUMMARY Mainland fringing reefs with a diverse coral fauna have developed in the Cape Tribulation area primarily upon coastal sedi- ment bodies such as beach shoals and creek mouth bars. Growth on steep rocky headlands is minor. The reefs have exten- sive sandy beaches to landward, and an irregular outer margin. Typically there is a raised platform of dead nef along the outer edge of the reef, and dead coral columns lie buried under the reef flat. Live coral growth is restricted to the outer reef slope. Seaward of the reefs is a narrow wedge of muddy, terrigenous sediment, which thins offshore. Beach, reef and inner shelf sediments all contain 50% terrigenous material, indicating the reefs have always grown under conditions of heavy terrigenous influx. The relatively shallow lower limit of coral growth (ca 6m below ADD) is typical of reef growth in turbid waters, where decreased light levels inhibit coral growth. Radiocarbon dating of material from surveyed sites confirms the age of the fossil coral columns as 33304110 ybp, indicating that they grew during the late postglacial sea-level high (ca 5500-6500 ybp). The former thriving reef-flat was killed by a post-5500 ybp sea-level fall of ca 1 m. Although this study has not assessed the community structure of the fringing reefs, nor whether changes are presently occur- ring, it is clear the corals present today on the fore-reef slope have always lived under heavy terrigenous influence, and that the fossil reef-flat can be explained as due to the mid-Holocene fall in sea-level. -
Protection of Coral Reefs and Related Ecosystems for Sustainable Livelihoods and Development – Australian Submission
Secretary-General’s report: Protection of coral reefs and related ecosystems for sustainable livelihoods and development – Australian submission The United Nations General Assembly (UNGA) Resolution 65/150 “Protection of coral reefs for sustainable livelihoods and development” was initiated by Australia working in close partnership with Pacific countries that may be directly affected by the health of coral reefs and related ecosystems. It was adopted by consensus in the UNGA on 25 November 2010, with co-sponsors comprising 84 States from the Pacific, Caribbean, Africa, the Americas, Asia and Europe. The resolution called for urgent action for the protection of coral reefs and related ecosystems. It also requested the United Nations (UN) Secretary-General to prepare a report on the issue. Australia considers this report as a timely opportunity to highlight the social, economic and environmental benefits of protecting coral reefs and related ecosystems and the urgent need for action to address the alarming trend in threats to the world’s coral reefs and related ecosystems. The United Nations Conference on Sustainable Development (the Rio+20 Conference) will be an important opportunity to secure a strong global outcome for coral reefs and related ecosystems, and recognition of their critical role for securing sustainable livelihoods and development, particularly in small island developing countries. A strong outcome for coral reefs and related ecosystems must be a global response. The main threats to coral reefs and related ecosystems include climate change, catchment runoff, coastal development and under-regulated fishing. For further details see Attachment A . The extent and persistence of damage to coral reef ecosystems will depend on change in the world’s climate and on the resilience of coral reef ecosystems. -
Distinct Benthic Trajectories Call for Monitoring of Mesophotic Reefs
bioRxiv preprint doi: https://doi.org/10.1101/2021.08.01.454664; this version posted August 2, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Hidden in the deep: distinct benthic trajectories 2 call for monitoring of mesophotic reefs 3 4 5 Hernandez-Agreda A1*, Sahit FM2, Englebert N2, Hoegh-Guldberg O2, Bongaerts P1* 6 7 1 California Academy of Sciences, San Francisco, 94118, CA, USA 8 2 Global Change Institute and School of Biological Sciences, The University of Queensland, St 9 Lucia, 4067 QLD, Australia 10 11 * Corresponding authors: [email protected], [email protected] 12 13 14 15 Running title: Urgent call for mesophotic reefs monitoring 16 17 Keywords: benthic communities, coral bleaching, coral reefs, disturbances, ecosystem 18 recovery, long-term monitoring, Mesophotic Coral Ecosystems (MCEs) 19 20 Abstract: 150 words 21 Whole manuscript: 2859 words 22 References: 40 23 Number of figures: 3 24 Number of tables: NA 25 26 27 28 29 30 31 32 33 34 35 36 37 1 bioRxiv preprint doi: https://doi.org/10.1101/2021.08.01.454664; this version posted August 2, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. -
Reef Structures Subject Matter: Recall the Different Types of Reef Structure (E.G
THE REEF AND BEYOND - CORAL REEF DISTRIBUTION Reef Structures Subject matter: Recall the different types of reef structure (e.g. fringing, platform, ribbon, barrier, atolls, coral cays). Recommended reading: Coral Reefs and Climate Change - Patterns of distribution (p.84-85) Zones across the reef (p.92-94) FRINGING REEF Fringing reefs are reefs that grow directly from a shore, with no “true” lagoon (i.e., deep water channel) between the reef and the nearby land. Without an intervening lagoon to effectively buffer freshwater runoff, pollution, and sedimentation, fringing reefs tend to particularly sensitive to these forms of human impact. Fringing reef Tane Sinclair Taylor Tane Tane Sinclair Taylor Tane Planet Dove - Allen Coral Atlas Allen Coral Planet Dove - Coral coast, Fiji Fringing reef in Indonesia. PLATFORM REEFS AND CORAL CAYS Platform reefs begin to form on underwater mountains or other rock-hard outcrops between the shore and a barrier reef. Coral cays begin to form when broken coral and sand wash onto these flats; cays can also form on shallow reefs around atolls. Coral cays are small islands, with Platform reef and Coral cay typical length scales between 100 - 1000 m, that form on platform reefs, Dave Logan Heron Island Lady Elliot Island Marine Science Senior Syllabus 8 THE REEF AND BEYOND - CORAL REEF DISTRIBUTION Reef Structures BARRIER REEFS BARRIER REEFS are coral reefs roughly parallel to a RIBBON REEFS are a type of barrier reef and are unique shore and separated from it by a lagoon or other body of to Australia. The name relates to the elongated Reef water.The coral reef structure buffers shorelines against bodies starting to the north of Cairns, and finishing to the waves, storms, and floods, helping to prevent loss of life, east of Lizard Island. -
Spearfishing in Great Barrier Reef Marine Park
· Great • Reef Marine Park Authoiity LAw Bu • Issue Number 18 SPEARFISHING IN GREAT BARRIER REEF MARINE PARK Where am I allowed to spearfish? Seasonal Closure Areas You may spearfish in all gerieral use zones in the Seasonal Closure Areas are areas closed to all access Marine Park, and in all non-zoned sections of the during the breeding or nesting periods of birds or Marine Park. You should note that some Queensland other marine life. The closure of these areas is waters are closed to spearfishing - there are details advertised. of those areas in the Queensland Harbours ahd What equipment can I use? Marine Tide Tables. You may only spearfish using a snorkel and a hand Where am I NOT allowed to spearfish? spear or speargun. You may not use any other You may not spearfish in Marine National Park 'A', underwater breathing equipment (such as scuba or Marine National Park Buffer and Marine National hookah) and you may only use a powerhead for Park 'B' Zones, nor in Scientific Research or protection against a shark attack. Preservation Zones. You also may not spearfish in areas where periodic restrictions are in operation. Can I sell fish I spear? These areas may be Replenishment Areas, Reef Spearfishing for the purpose of sale or trade is not Appreciation Areas, Reef Research Areas or Seasonal allowed in the Marine Park, with one exception, in Closure Areas. the Far Northern Section of the Marine Park it is permitted to spear crayfish for purposes of sale or Replenishment Areas trade (you can also use scuba or hookah in this A Replenishment Area is an area closed for a circumstance - but only for crayfish). -
The Great Barrier Reef and Coral Sea 20 Tom C.L
The Great Barrier Reef and Coral Sea 20 Tom C.L. Bridge, Robin J. Beaman, Pim Bongaerts, Paul R. Muir, Merrick Ekins, and Tiffany Sih Abstract agement approaches that explicitly considered latitudinal The Coral Sea lies in the southwestern Pacific Ocean, bor- and cross-shelf gradients in the environment resulted in dered by Australia, Papua New Guinea, the Solomon mesophotic reefs being well-represented in no-take areas in Islands, Vanuatu, New Caledonia, and the Tasman Sea. The the GBR. In contrast, mesophotic reefs in the Coral Sea Great Barrier Reef (GBR) constitutes the western margin currently receive little protection. of the Coral Sea and supports extensive submerged reef systems in mesophotic depths. The majority of research on Keywords the GBR has focused on Scleractinian corals, although Mesophotic coral ecosystems · Coral · Reef other taxa (e.g., fishes) are receiving increasing attention. · Queensland · Australia To date, 192 coral species (44% of the GBR total) are recorded from mesophotic depths, most of which occur shallower than 60 m. East of the Australian continental 20.1 Introduction margin, the Queensland Plateau contains many large, oce- anic reefs. Due to their isolated location, Australia’s Coral The Coral Sea lies in the southwestern Pacific Ocean, cover- Sea reefs remain poorly studied; however, preliminary ing an area of approximately 4.8 million square kilometers investigations have confirmed the presence of mesophotic between latitudes 8° and 30° S (Fig. 20.1a). The Coral Sea is coral ecosystems, and the clear, oligotrophic waters of the bordered by the Australian continent on the west, Papua New Coral Sea likely support extensive mesophotic reefs.