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Blue carbon in human-dominated estuarine and shallow coastal
Blue carbon in human-dominated estuarine and shallow coastal

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Carbon cycle implications of terrestrial weathering changes since
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... Bryden, 1982]. The NAC follows the boundary between the North Atlantic subpolar gyre (SPG) and the subtropical gyre (STG), and its density and flow are modulated by the SPG [Hátún et al., 2005]. During periods when the SPG is enhanced (elongated E-W with strong outgrowth into the eastern Atlantic), t ...
Chapter 51. Biological Communities on Seamounts and Other
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Geological Society, London, Special Publications
Geological Society, London, Special Publications

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... enhanced DFe concentrations (up to 10 nM) immediately under the ash plume. Bioassay experiments performed with ash collected at sea under the plume also demonstrated the potential for associated Fe release to stimulate phytoplankton growth and nutrient drawdown. Combining Fe dissolution measurements ...
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Tide Pools on Cavendish Beach – A Lesson in Survival

... environment of tide pools to students in elementary school. The activities can be done individually or in groups of varying sizes, depending on the nature of the class and availability of technology facilities. It is recommended that teachers familiarize themselves with the sites before starting the ...
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Sailing through Changing Oceans

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Gulf of Maine Strategic Regional Ocean Science Plan
Gulf of Maine Strategic Regional Ocean Science Plan

... Initiative evolved from an awareness of the importance of integrated approaches to addressing ecological, environmental, and social influences in coastal and marine ecosystems at the regional level. In response to a call for regional coordination of research by the U.S. Commission on Ocean Policy, t ...
PDF
PDF

... correlated with regional primary production and sea-ice duration [75]. Similarly, organic matter is transferred within sinking water generated from rejected brine during ice formation and is suspected to act as an important source of food for benthic species creating locations of high species richne ...
Salinity (Marine) - Canadian Environmental Quality Guidelines
Salinity (Marine) - Canadian Environmental Quality Guidelines

... estuary (Kistritz 1978), but stenohaline marine species, such as eelgrass and shellfish, are found in the adjacent, more saline area that is isolated from the river flow behind the two long jetties to the south of the river. In many coastal areas, salinity fluctuations limit the distributions of org ...
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Ocean acidification



Ocean acidification is the ongoing decrease in the pH of the Earth's oceans, caused by the uptake of carbon dioxide (CO2) from the atmosphere. An estimated 30–40% of the carbon dioxide from human activity released into the atmosphere dissolves into oceans, rivers and lakes. To achieve chemical equilibrium, some of it reacts with the water to form carbonic acid. Some of these extra carbonic acid molecules react with a water molecule to give a bicarbonate ion and a hydronium ion, thus increasing ocean acidity (H+ ion concentration). Between 1751 and 1994 surface ocean pH is estimated to have decreased from approximately 8.25 to 8.14, representing an increase of almost 30% in H+ ion concentration in the world's oceans. Since current and projected ocean pH levels are above 7.0, the oceans are technically alkaline now and will remain so; referring to this effect as ""decreasing ocean alkalinity"" would be equally correct if less politically useful. Earth System Models project that within the last decade ocean acidity exceeded historical analogs and in combination with other ocean biogeochemical changes could undermine the functioning of marine ecosystems and disrupt the provision of many goods and services associated with the ocean.Increasing acidity is thought to have a range of possibly harmful consequences, such as depressing metabolic rates and immune responses in some organisms, and causing coral bleaching. This also causes decreasing oxygen levels as it kills off algae.Other chemical reactions are triggered which result in a net decrease in the amount of carbonate ions available. This makes it more difficult for marine calcifying organisms, such as coral and some plankton, to form biogenic calcium carbonate, and such structures become vulnerable to dissolution. Ongoing acidification of the oceans threatens food chains connected with the oceans. As members of the InterAcademy Panel, 105 science academies have issued a statement on ocean acidification recommending that by 2050, global CO2 emissions be reduced by at least 50% compared to the 1990 level.Ocean acidification has been called the ""evil twin of global warming"" and ""the other CO2 problem"".Ocean acidification has occurred previously in Earth's history. The most notable example is the Paleocene-Eocene Thermal Maximum (PETM), which occurred approximately 56 million years ago. For reasons that are currently uncertain, massive amounts of carbon entered the ocean and atmosphere, and led to the dissolution of carbonate sediments in all ocean basins.
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