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967 result(s) for "Great Barrier Reef"
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The Great Barrier Reef
One of the world's natural wonders, the Great Barrier Reef stretches more than 2000 kilometres in a maze of coral reefs and islands along Australia's north-eastern coastline. Now unfolding the fascinating story behind its mystique this 2002 book provides for the first time a comprehensive cultural and ecological history of European impact, from early voyages of discovery to developments in Reef science and management. Incisive and a delight to read in its thorough account of the scientific, social and environmental consequences of European impact on the world's greatest coral reef system, this extraordinary book is sure to become a classic.
Where is the Great Barrier Reef?
Introduces the Great Barrier Reef off the coast of Australia, [which] is the world's largest coral reef system. Stretching more than 1,400 miles, it provides a home to a wide diversity of creatures\"--Amazon.com.
Elevated land runoff after European settlement perturbs persistent foraminiferal assemblages on the Great Barrier Reef
Coral reefs are under pressure from a variety of human-induced disturbances, but demonstration of ecosystem changes and identification of stressors are often difficult. We tested whether global change or increased agricultural runoff after European settlement of Northeast Australia (ca. 1860) has affected inshore reefs of the Great Barrier Reef. Eleven sediment cores were retrieved from inner reefs, intermediate reefs, and outer-island reefs, and benthic foraminiferal assemblages were analyzed in dated ( 14 C, 210 Pb, 137 Cs) core sections ( N = 82 samples). Data were grouped into six age bands (<55, 55-150, 150-500, 500-1000, 1000-1500, and >1500 yr). Principal component analysis and two-factor (Zone and Age) permutational analysis of variance (PERMANOVA) suggested that assemblages from the three zones were significantly different from each other over several millennia, with symbiont-bearing (mixotrophic) species dominating the outer reefs. A significant interaction term indicated that within-zone patterns varied. Assemblages in outer reefs unaffected from increased land runoff were persistent until present times. In both other zones, assemblages were also persistent until 150 yr ago, suggesting that benthic foraminiferal assemblages are naturally highly persistent over long (>2000 yr) timescales. Assemblages in core sections < 55 yr old from inner reefs were significantly (post hoc t test) different from those older than 150 yr. Similarly, assemblages < 55 yr old from intermediate reefs were significantly different compared to older assemblages. A multivariate regression tree (environmental variables: Zone and Age) explained 56.8% of the variance in foraminiferal assemblages and confirmed patterns identified by PERMANOVA. With some exceptions, changes on the inner and intermediate reefs were consistent with a model predicting that increased nutrients and higher turbidity enhance relative abundance of heterotrophic species. Given that assemblages did not change in outer-island reefs (not impacted by runoff) we argue that changes in assemblages due to global change can be rejected as an explanation. Thus, the findings are more consistent with the hypothesis that agricultural runoff since European settlement altered foraminiferal assemblages than with the hypothesis that global forcing caused changes.
Supply-Side Ecology Works Both Ways: The Link between Benthic Adults, Fecundity, and Larval Recruits
\"Supply-side\" ecology recognizes the potential role that recruitment plays in the local population dynamics of open systems. Apart from the applied fisheries literature, the converse link between adults and the production of cohorts of recruits has received much less attention. We used a hierarchical sampling design to investigate the relationships between adult abundance, fecundity, and rates of larval recruitment by acroporid corals on 33 reefs in five sectors (250-400 km apart) stretching from north to south along the length of the Great Barrier Reef, Australia. Our goal was to quantify patterns of recruitment at multiple scales, and to explore the underlying mechanisms. Specifically, we predicted that large-scale patterns of recruitment could be driven by changes in the abundance of adults and/or their fecundity, i.e., that corals exhibit a stock-recruitment relationship. The amount of recruitment by acroporids in each of two breeding seasons varied by more than 35-fold among the five sectors. Adult density varied only twofold among sectors and was not correlated with recruitment at the sector or reef scale. In contrast, fecundity levels (the proportion of colonies on each reef that contained ripe eggs) varied from 15% to 100%, depending on sector, year, and species. Spatial and temporal variation in the fecundity of each of three common Acropora species explained most of the variation (72%) in recruitment by acroporids, indicating that the production of larvae is a major determinant of levels of recruitment at large scales. Once fecundity was accounted for, none of the other variables we examined (sector, reef area, abundance of adults, or year) contributed significantly to variation in recruitment. The relationship between fecundity and recruitment was nonlinear, i.e., rates of recruitment increased disproportionately when and where the proportion of gravid colonies approached 100%. This pattern is consistent with the hypothesis that enhanced fertilization success and/or predator satiation occurs during mass-spawning events. Furthermore, it implies that small, sublethal changes in fecundity of corals could result in major reductions in recruitment.
The Coral Battleground
The Great Barrier Reef lies off the coast of Queensland: 2000 kilometres of spectacular coral reefs, sand cays and islands, Australia's most precious marine possession. Teeming with life, it covers 350,000 square kilometres. In the late 1960s the Reef was threatened with limestone mining and oil drilling. A small group of dedicated conservationists in Queensland – John Büsst, Judith Wright, Len Webb and others – battled to save the Ellison Reef from coral-limestone mining and the Swain Reefs from oil exploration. The group later swelled to encompass scientists, trade unionists and politicians throughout Australia, and led in 1976 to the establishment of a guardian body: the Great Barrier Reef Marine Park Authority. That it still survives is a legacy of activists, artists, poets, ecologists and students. In 1967 they were branded as 'cranks'; now they should be recognised as 'visionaries'.
Coastal Queensland & the Great Barrier Reef
Lonely Planet Coastal Queensland & the Great Barrier Reef is your passport to the most relevant, up-to-date advice on what to see and skip, and what hidden discoveries await you. Explore the Great Barrier Reef's underwater wonderland, experience the ancient Daintree Rainforest and visit some of Brisbane's vibrant cafes and bars; all with your trusted travel companion. Get to the heart of Queensland & the Great Barrier Reef and begin your journey now! Check out Lonely Planet's East Coast Australia guide for a comprehensive look at all this region has to offer; Discover Australia, a photo-rich guide to the country's most popular attractions.
Submarine Groundwater Discharge: Updates on Its Measurement Techniques, Geophysical Drivers, Magnitudes, and Effects
The number of studies concerning Submarine Groundwater Discharge (SGD) grew quickly as we entered the 21st century. Many hydrological and oceanographic processes that drive and influence SGD were identified and characterized during this period. These processes included tidal effects on SGD, water and solute fluxes, biogeochemical transformations through the subterranean estuary, and material transport via SGD from land to sea. Here we compile and summarize the significant progress in SGD assessment methodologies, considering both the terrestrial and marine driving forces, and local as well as global evaluations of groundwater discharge with an emphasis on investigations published over the past decade. Our treatment presents the state-of-the-art progress of SGD studies from geophysical, geochemical, bio-ecological, economic, and cultural perspectives. We identify and summarize remaining research questions, make recommendations for future research directions, and discuss potential future challenges, including impacts of climate change on SGD and improved estimates of the global magnitude of SGD.