Global Climate Change and Coral Reefs: Implications for People and Reefs
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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. -
In Soils of Niue Island, South Pacific
Geochemical Journal, Vol. 24, pp. 371 to 378, 1990 Anomalous Hg contents in soils of Niue Island, South Pacific NEIL E. WHITEHEAD', JOHN BARRIE2 and PETER RANKIN3 Nuclear Sciences Group, Division of Physical Sciences, D.S.I.R. P.O.Box 31-312, Lower Hutt, New Zealand', Avian Mining Ltd., 24 Jindvik Place, Canberra, A.C.T., Australia2 and Division of Land and Soil Sciences, D.S.I.R., Private Bag, Taita, New Zealand3 (Received September 10, 1990; Accepted December 29, 1990) Niue Island, a raised coralline atoll in the South Pacific, has soils that have long been known to have strongly anomalous radioactivity. We now show that there is also a highly anomalous Hg content in the soils. It is associated with the radioactivity and the goethite/gibbsite content and the values are as high as those in soils over known Hg-mineralisation in volcanic settings, though no mineralisation is known on Niue and such an occurrence on this coral island would be geochemically unusual. INTRODUCTION GEOLOGY AND SOILS OF NIUE ISLAND Niue Island in the South Pacific is a raised A detailed description of the geological set coral atoll, located at 19° S and 169° W. The in ting of Niue Is. may be found in Schofield (1959) terior of the island is dolomitised, and is covered and a summary follows. by reddish-brown soils rich in Fe, Al and Niue Island is a raised coral atoll consisting phosphate in the form of goethite, gibbsite and of seaward cliffs rising steeply from the sea but crandallite respectively (the mean soil P205 is girded by a terrace on which sits Alofi, the 4%; Whitehead et al. -
Challenges in Freshwater Management in Low Coral Atolls
Journal of Cleaner Production 15 (2007) 1522e1528 www.elsevier.com/locate/jclepro Challenges in freshwater management in low coral atolls Ian White a,*, Tony Falkland b, Pascal Perez c, Anne Dray c, Taboia Metutera d, Eita Metai e, Marc Overmars f a Centre for Resource and Environmental Studies, Institute of Advanced Studies, Australian National University, Canberra, ACT 0200, Australia b Ecowise Environmental, ACTEW Corporation, PO Box 1834, Fyshwick ACT 2609, Australia c CIRAD Montpellier France and Resource Management in the Asia-Pacific Program, Research School of Pacific and Asian Studies, Institute of Advanced Studies, Australian National University, Canberra, ACT 0200, Australia d Public Utilities Board, Betio, Tarawa, Republic of Kiribati e Water Engineering Unit, Public Works Department, Betio, Tarawa, Republic of Kiribati f South Pacific Applied Geoscience Commission, Suva, Fiji Received 13 January 2005; accepted 31 July 2006 Available online 13 October 2006 Abstract Population centres in low atoll islands have water supply problems that are amongst the most critical in the world. Fresh groundwater, the major source of water in many atolls, is extremely vulnerable to natural processes and human activities. Storm surges and over-extractions cause seawater intrusion, while human settlements and agriculture can pollute shallow groundwaters. Limited land areas restrict freshwater quantities, particularly in frequent ENSO-related droughts. Demand for freshwater is increasing and availability is extremely limited. At the core of many groundwater management problems are the traditional water ownership rights inherent in land tenure and the conflict between the requirements of urbanised societies and the traditional values and rights of subsistence communities living on groundwater reserves. -
Evaporation Rates for a Coral Island by Field Observation and Simulation
23rd International Congress on Modelling and Simulation, Canberra, ACT, Australia, 1 to 6 December 2019 mssanz.org.au/modsim2019 Evaporation rates for a coral island by field observation and simulation S. Han ab, S. Liu bc, S. Hu b, X. Mo bc and X. Song bc a University of Chinese Academy of Sciences, Beijing 100049, PR China, b Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, PR China, c College of Resources and Environment, Sino- Danish Center, University of Chinese Academy of Sciences, Beijing 100049, PR China. Email: [email protected] Abstract: Evaporation in coral islands influences their limited freshwater recharge and plays an important role in coral reefs ecology protection under the background of climate changes. From June 20th to August 16th, 2018, a field experiment was carried out in Zhaoshu Island, Xisha Islands, China, using a self-made micro- lysimeter and pan evaporation dish. To understand the whole process of evaporations at the annual scale, we used the Penman-Monteith model and crop coefficient (Kc) method to estimate potential evaporation (ETo) and actual evaporation (ETc) using meteorological data and leaf area index (LAI). The results show (1) ETo reached its peak value earlier than precipitation, causing island vegetations to suffer the highest water stress at the end of the dry season. (2) in the wet season, ETc rose as the precipitation increased, however, the ETo presented a tendency of slowly declining. These phenomena indicate that the vegetation could suffer from strong drought at the end of the dry season because of the maximum ETo and extended low rate of precipitation. -
Pacific Reef Assessment and Monitoring Program Benthic Monitoring Summary: American Sāmoa 2015
Pacific Reef Assessment and Monitoring Program Benthic monitoring summary: American Sāmoa 2015 About this summary The purpose of this document is to provide a brief summary of the most recent survey efforts conducted in the islands of American Sāmoa by the Coral Reef Ecosystem Division (CRED) of the NOAA Pacific Islands Fisheries Science Center as part of the Pacific Reef Assessment and Monitoring Program (Pacific RAMP). A more detailed assessment of coral populations and reef community structure in American Sāmoa will be summarized in a forthcoming annual report. Sampling effort - Ecological monitoring in American Sāmoa was conducted from February 15 – March 30, 2015. Figure 2. Mean density of all juvenile coral colonies (Scleractinia, < 5 cm) at survey sites. - Surveys were conducted at 188 sites across 5 islands and atolls: Ofu-Olosega, Rose, Swains, Ta‘ū, and Tutuila. - Coral demography, partial mortality, and condition were surveyed using belt transects; benthic community structure will be assessed using photoquadrats. Overview of data collected Figure 3. Mean density of adult (dark) and juvenile (light) coral colonies (± standard error) grouped by island within three depth categories: shallow (0–6 m), mid (>6–18 m), and deep (>18–30 m). Figure 1. Mean density of all adult coral colonies (Scleractinia, ≥ 5 cm) at survey sites. Overview of data collected (cont.) colonies measured, two colonies were identified as Pavona diffluens and 813 colonies identified as Isopora sp. The threatened species Isopora crateriformis was not consistently identified to species throughout our survey efforts in American Samoa due to the similarity to I. cuneata when both have an encrusting morphology. -
BBP in Brief
IO AS" COM M P A LE H X I A T " Y 0 R O J E C T BBP in Brief A NEWSLETTER OF THE BAHAMAS BIOCOMPLEXITY PROJECT Produced by the American Museum of Natural History’s Center for Biodiversity and Conservation (AMNH-CBC) Issue 8 Spring, 2007 Welcome… This is the newsletter of the Bahamas Biocomplexity Project, or “BBP,” also available at http://bbp.amnh.org/bbpinbrief/. Here you can learn about the activities and progress of the BBP team and its partners. We welcome your submissions about research progress, upcoming field plans, meetings, or any other information you feel would be of interest to project partners. Submissions for consideration in future newsletters may be made to Kate Holmes or Christine Engels ([email protected]). In this Issue: Marine Reserves and Coral Recovery: BBP Publications Demonstrate How Reserves Can Facilitate Reef Recovery Kate Holmes, Dan Brumbaugh (AMNH-CBC), and Steve Vollmer (Northeastern University) A Swimming Cash Crop Two recent research articles by BBP researchers have revealed Page 2 important information about how marine protected areas (MPAs) can contribute to the recovery of Caribbean corals. The first paper, published in the Journal of Heredity in January BBP General Meeting 2007, addresses the maximum spacing among reefs that would 2007 allow for reef recovery via an adequate supply of coral recruits Page 3 (coral larvae that disperse, settle, and grow to become small new coral colonies). That is, how close should damaged reefs be to healthy reefs for them to be able to benefit from a supply of new corals? This information is particularly needed in Bahamian Voices the Caribbean where the two once-dominant shallow water at the 15th UN corals, staghorn coral (Acropora cervicornis) and elkhorn Commission coral (A. -
Pacific Ocean Coral Island Reveals How Human Settlement Affects Water Quality 17 February 2014, by Niall Byrne
Pacific Ocean coral island reveals how human settlement affects water quality 17 February 2014, by Niall Byrne sites close to and far from human populations and fishing. They found that greater levels of fishing were associated with bigger differences in dead and live shell types. "At more heavily fished sites, the living population was dominated by foraminifera that thrive in high- nutrient conditions," Jessica says. The relationship suggests that fishing can lead to higher nutrients in the water column, which is generally bad for corals, supporting other research that shows healthy fish populations are important for healthy coral reefs. Kirimati Island was settled in the 1970s when a re- population program in the Republic of Kiribati moved people from the overcrowded capital, Tarawa, to under-populated outer islands. Provided by ANSTO A Pacific Ocean coral island, populated around 40 years ago, reveals how human settlement can quickly degrade water quality and affect the health of coral reefs, Sydney scientists say. Jessica Carilli, of the Australian Nuclear Science and Technology Organisation, and Sheila Walsh, of the Nature Conservancy, used Kirimati Island to examine the shells made by an organism that thrives in high-nutrient conditions, which is considered detrimental to coral. "We used a unique metric to estimate water quality before and after people arrive by comparing types of dead and live microscopic shells in reef sand made by organisms called foraminifera," says Jessica, an ANSTO postdoctoral fellow. Jessica and Shelia collected sand underwater at 1 / 2 APA citation: Pacific Ocean coral island reveals how human settlement affects water quality (2014, February 17) retrieved 29 September 2021 from https://phys.org/news/2014-02-pacific-ocean-coral- island-reveals.html This document is subject to copyright. -
Research and Monitoring in Australia's Coral Sea: a Review
Review of Research in Australia’s Coral Sea D. Ceccarelli DSEWPaC Final Report – 21 Jan 2011 _______________________________________________________________________ Research and Monitoring in Australia’s Coral Sea: A Review Report to the Department of Sustainability, Environment, Water, Population and Communities By Daniela Ceccarelli, Oceania Maritime Consultants January 21st, 2011 1 Review of Research in Australia’s Coral Sea D. Ceccarelli DSEWPaC Final Report – 21 Jan 2011 _______________________________________________________________________ Research and Monitoring in Australia’s Coral Sea: A Review By: Oceania Maritime Consultants Pty Ltd Author: Dr. Daniela M. Ceccarelli Internal Review: Libby Evans-Illidge Cover Photo: Image of the author installing a temperature logger in the Coringa-Herald National Nature Reserve, by Zoe Richards. Preferred Citation: Ceccarelli, D. M. (2010) Research and Monitoring in Australia’s Coral Sea: A Review. Report for DSEWPaC by Oceania Maritime Consultants Pty Ltd, Magnetic Island. Oceania Maritime Consultants Pty Ltd 3 Warboys Street, Nelly Bay, 4819 Magnetic Island, Queensland, Australia. Ph: 0407930412 [email protected] ABN 25 123 674 733 2 Review of Research in Australia’s Coral Sea D. Ceccarelli DSEWPaC Final Report – 21 Jan 2011 _______________________________________________________________________ EXECUTIVE SUMMARY The Coral Sea is an international body of water that lies between the east coast of Australia, the south coasts of Papua New Guinea and the Solomon Islands, extends to Vanuatu, New Caledonia and Norfolk Island to the east and is bounded by the Tasman Front to the south. The portion of the Coral Sea within Australian waters is the area of ocean between the seaward edge of the Great Barrier Reef Marine Park (GBRMP), the limit of Australia’s Exclusive Economic Zone (EEZ) to the east, the eastern boundary of the Torres Strait and the line between the Solitary Islands and Elizabeth and Middleton Reefs to the south. -
Niue Integrated Strategic Plan – 2003 - 2008
HHaallaavvaakkaa kkee hhee MMoonnuuiinnaa Governance Financial Stability Social Economic Environment Development Niue Integrated Strategic Plan – 2003 - 2008 Niue Ke Monuina – A Prosperous Niue COUNTRY PROFILE Geography Niue is a single coral island of 259 square kilometers in the South Pacific Ocean at latitude 19 south and longitude 169 west. Niue has an Exclusive Economic Zone of 293,988 sq km. It is the largest raised coral island in the world and is known for its unspoilt environment and pristine coastal waters. People, culture and tradition Niueans are of Polynesian descent and are said to be amongst the friendliest people in the world. They speak Niuean, which has close links to other Polynesian languages. Culture, tradition, spirituality and social values play an integral part in the unique Niuean culture. Population In March 2002 the population was 1707. This compares with 20,145 residents of New Zealand who claimed to be of Niuean descent in the 2001 Census. The declining population has created difficulties in maintaining adequate public services but more importantly threatens the existence of Niue’s cultural heritage and sovereignty. The Government Since 1974 Niue has been self-governing in free association with New Zealand. Under this constitutional arrangement New Zealand is responsible for defense and external affairs as well as providing necessary economic and administrative assistance. General elections are held once every three years for the 20 members of the Legislative Assembly. Since 2001 Niue has full diplomatic representation in New Zealand. Economy In 2002 GDP was $14.2m, which equates to $7,470 per capita. The Government is the major employer in Niue. -
What Is an Atoll ?
...what is an atoll? by Jan Newhouse It is characteristic of humans that we invested by photosynthetic algae (a) Truncation. This theory is based attempt to define precisely and/or (zooxanthellae) which can only survive, on the supposition that a high, categorise all that surrounds us. It is also grow and complete their role(s) within volcanic island has slowly eroded characteristic that such attempts often the euphotic zone — the water layer away because of atmospheric and lead to difficulty and disagreement (e.g., which is penetrated by sufficient radiant ocean-generated forces. After at what height does a hill become a energy to permit these activities. Though complete erosion had taken place, mountain?). So it is with the application the thickness of this water layer varies the resulting surface was covered of terms to reef types. Definitions and from place to place depending on by reef-building corals. Sufficient classifications have often resulted from turbidity, a generally accepted figure is evidence exists to discount this limited personal experience or bias, rather 80 metres. Hence, relatively shallow reefs theory. than from a consideration of the broad (fringing and barrier) bordering volcanic (b) Antecedent platform. This theory range which exists. Thus it seems wise to islands are automatically excluded, as are supposes that, at some time in the seek an operational definition for "atoll". patch reefs found in atoll lagoons. past, the floor of the ocean was, The word atoll is taken from the In any case, since the interest here is or came, within the euphotic Malayalam atolu, "reef, which is the mainly focused on the primarily cal zone. -
Use of High Resolution Pathfinder Sst Data to Document Coral Reef Bleaching*
USE OF HIGH RESOLUTION PATHFINDER SST DATA TO DOCUMENT CORAL REEF BLEACHING* M. A. Toscano NOAA/NESDIS/ORA/ORAD Silver Spring, MD USA K. S. Casey NOAA/NESDIS/NODC Silver Spring, MD USA J. Shannon U. S. Naval Academy Annapolis, MD, USA ABSTRACT Mass coral bleaching has been observed throughout the tropical oceans immediately following periods of thermal stress, in concert with other known causes. While water temperatures monitored in situ best document the relationship of thermal stress to bleaching, most reef sites have limited to no in situ data. For such areas, high-resolution satellite-derived SSTs provide valuable time series data and quantify thermal anomalies and their timing vs. onset of bleaching. The availability of 9km NOAA/NASA Oceans Pathfinder SST data (1985-2001), an internally consistent, calibrated SST database at reef scale resolution, allows us to assess the accuracy and usefulness of satellite SST data to document past conditions in reefs. Statistical analyses of SSTs combined with available in situ temperatures from Caribbean and tropical Pacific locations indicate that 9km SSTs for specific sites, and for the 3x3 pixel means surrounding each site, are highly correlated to in situ temperatures. Biases are tied, wherever possible, to local physical causes. Pathfinder SSTs accurately represent surface field temperatures with predictable exceptions, and therefore have great potential for assessing temperature histories of remote, un-monitored reefs. 1.0 THERMAL STRESS AND CORAL REEF BLEACHING Bleaching is the loss of algal symbionts (zooxanthellae) and/or their pigments from a coral (or other symbiotic animal) host, and occurs in response to environmental stressors which vary regionally and seasonally, and which may act singly or synergistically (Fitt et al. -
"Coral" Islands: Data from the Bahamas and Oceania
ADAPTATION AND EXCHANGES ON "CORAL" ISLANDS: DATA FROM THE BAHAMAS AND OCEANIA Frank R. Thomas This paper constitutes an attempt at delineating similarities and differences among prehistoric cultural traditions in insular tropical environments. While it has often been suggested that the amount and quality of ethnohistoric and linguistic coverage in the Caribbean area are a poor reflection of the types of information available for Oceania, the interest in subsurface investigations in the latter region (on atolls) is barely two decades old. Until the mid-1970s much of Micronesia was terra- incognita, and there are still many islands, particularly in the atoll/ raised coral categories awaiting the spade of the archaeologist. The fact that "true" atolls are absent in the West Indies should not divert us from the potential contributions that might arise in comparing human adaptation to constraints imposed by calcareous environments. On several occasions, Watters (1981, 1982, 1983) drew attention to the advances made by Pacific archaeologists in the area of subsistence; we might also add social organization and social complexity. Because of various limitations in the use of ethnographic data by their Caribbean counterparts and the benign neglect of a "seaward perspective", it was concluded that much could be learned from the work being accomplished in Oceania. THE INSULAR SETTING In order to select geological units that are comparable, one also needs to consider the quality of both ethnographic and archaeological sequences, as well as the areal distribution of coral islands. In effect, this study focuses on three "Coral Clusters" or "Coral Complexes'' for which there is a fairly adequate record of prehistoric and protohistoric cultural develop ments.