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	<title>Newly Published Articles - Encyclopedia of Earth</title>
	<link>http://www.eoearth.org/</link>
	<lastBuildDate>Thu, 01 Jan 1970 00:00:00 GMT</lastBuildDate>
	<ttl>15</ttl>
	<language>en-us</language>
	<managingEditor>cutler@bu.edu</managingEditor>
	<description></description>
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		<title>Encyclopedia of Earth</title>
		<link>http://www.eoearth.org/</link>
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		<title>Climate Change Authors</title>
		<link>http://www.eoearth.org/article/Climate_Change_Authors</link>
		<description>&lt;a href='http://www.eoearth.org/article/Climate_Change_Authors'&gt;&lt;img border='0' src='/media/approved/a/a3/John.bruno_100px.jpg' width='100'/&gt;&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;a href='http://www.eoearth.org/article/Climate_Change_Authors'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Climate_Change_Authors</guid>
		<pubDate>Fri, 09 May 2008 18:04:24 GMT</pubDate>
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		<title>Hansen, James E.</title>
		<link>http://www.eoearth.org/article/Hansen,_James_E.</link>
		<description>&lt;a href='http://www.eoearth.org/article/Hansen,_James_E.'&gt;&lt;img border='0' src='/upload/thumb/c/cf/Lg-hansen.jpg/180px-Lg-hansen.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;p&gt;James E. Hansen (1941- ) is an American physicist known for his research in the field of climatology and his testimony on climate change to congressional committees in the 1980s that helped raise broad awareness of the climate change issue. Hansen heads the NASA Institute for Space Studies in New York City, which is a division of Goddard Space Flight Center&amp;#39;s (Greenbelt, MD), Earth Sciences Directorate. He is currently an adjunct professor in the Department of Earth and Environmental Sciences at Columbia University, and also serves as Al Gore&amp;#39;s science advisor.&lt;/p&gt;&lt;p&gt;Hansen was elected to the National Academy of Sciences in 1996 and he received the Heinz Environment Award for his research on &lt;a href=&quot;/article/Global_warming&quot;&gt;global warming&lt;/a&gt; in 2001. He was listed as one of Time Magazine&amp;#39;s 100 Most Influential People in the Time 100 (2006) list and, in 2007, he was awarded the Dan David Prize. On April 5, 2008, Hansen received the PNC Bank Common Wealth Award of Distinguished Service for his outstanding achievements in science.&lt;/p&gt;&lt;p&gt;Hansen was trained in physics and astronomy in the space science program of Dr. James Van Allen at the University of Iowa. His early research on the properties of clouds of Venus led to their identification as sulfuric acid. Since the late 1970s, he has worked on studies and computer simulations of the Earth&amp;#39;s climate, for the purpose of understanding the human impact on global climate&lt;/p&gt;&lt;p&gt;In 1981 Hansen and a team of scientists at Goddard stated that &lt;a href=&quot;/article/Carbon_dioxide&quot;&gt;carbon dioxide&lt;/a&gt; in the &lt;a href=&quot;/article/Atmospheric_composition&quot;&gt;atmosphere&lt;/a&gt; would lead to global warming sooner than previously predicted. While other climatologists had already predicted that a trend would be apparent by 2020, Hansen predicted that the change was already occurring and that there would be record high &lt;a href=&quot;/article/Temperature&quot;&gt;temperatures&lt;/a&gt; as early as 1990. He also predicted that it would be difficult to convince politicians and the public to react.&lt;/p&gt;&lt;p&gt;In 2003 Hansen argued that human-caused forces on the climate are now greater than natural ones, and that this, over a long time period, can cause large climate changes. He further states that a lower limit on “dangerous anthropogenic interference” is set by the stability of the Greenland and &lt;a href=&quot;/article/Antarctica&quot;&gt;Antarctic&lt;/a&gt; ice sheets. His view on actions to mitigate climate change is that &amp;quot;halting global warming requires urgent, unprecedented international cooperation, but the needed actions are feasible and have additional benefits for human health, agriculture and the environment.&amp;quot;&lt;/p&gt;&lt;p&gt;Hansen has been a critic of both the Clinton and current Bush Administration&amp;#39;s stances on climate change.  In 2005 and 2006, Hansen claimed in interviews with the Washington Post and the New York Times that NASA administrators have tried to influence his public statements about the causes of climate change. Hansen claims that NASA public relations staff were ordered to review his public statements and interviews after a December 2005 lecture at the American Geophysical Union in San Francisco, claims which were denied by NASA administrator Michael Griffin.&lt;/p&gt;&lt;p&gt;Hansen has also appeared on 60 Minutes stating that the White House edited climate-related press releases reported by federal agencies to make &lt;a href=&quot;/article/Global_warming&quot;&gt;global warming&lt;/a&gt; seem less threatening. He claimed that he was unable to speak &amp;quot;freely&amp;quot;, without the backlash of other government officials. &amp;quot;In my more than three decades in the government I&amp;#39;ve never witnessed such restrictions on the ability of scientists to communicate with the public.”  Spokespersons for the federal agencies involved denied that Hansen was pressured to alter his public remarks on climate change.&lt;/p&gt;&lt;p&gt;&lt;strong&gt;Further reading&lt;/strong&gt;&lt;/p&gt;&lt;ul&gt;&lt;li&gt;&lt;a href=&quot;http://www.giss.nasa.gov/&quot; class='external text' title=&quot;http://www.giss.nasa.gov/&quot;&gt;NASA Goddard Institute for Space Studies&lt;/a&gt;&lt;/li&gt;&lt;li&gt;&lt;a href=&quot;http://www.cooperativeresearch.org/entity.jsp?entity=james_e._hansen_1&quot; class='external text' title=&quot;http://www.cooperativeresearch.org/entity.jsp?entity=james e. hansen 1&quot;&gt;James E. Hansen Timeline at the Cooperative Research History Commons&lt;/a&gt;&lt;/li&gt;&lt;li&gt;&lt;a href=&quot;http://www.giss.nasa.gov/staff/jhansen.html&quot; class='external text' title=&quot;http://www.giss.nasa.gov/staff/jhansen.html&quot;&gt;NASA GISS Biography&lt;/a&gt;&lt;/li&gt;&lt;li&gt;&lt;a href=&quot;http://www.columbia.edu/~jeh1/&quot; class='external text' title=&quot;http://www.columbia.edu/~jeh1/&quot;&gt;James E. Hansen Homepage&lt;/a&gt;&lt;/li&gt;&lt;/ul&gt;&lt;br /&gt;&lt;p&gt;&lt;strong&gt;Copyright&lt;/strong&gt;&lt;/p&gt;&lt;p&gt;This article contains content from &lt;a href=&quot;/contributor/Wikipedia&quot;&gt;Wikipedia&lt;/a&gt;.  The text of the article is available under the terms of the the &lt;a href=&quot;http://en.wikipedia.org/wiki/Wikipedia:Text_of_the_GNU_Free_Documentation_License|&quot; class='external text' title=&quot;http://en.wikipedia.org/wiki/Wikipedia:Text of the GNU Free Documentation License|&quot;&gt;GNU Free Documentation License&lt;/a&gt;.&lt;/p&gt;
&lt;p&gt;&lt;a href='http://www.eoearth.org/article/Hansen,_James_E.'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Hansen,_James_E.</guid>
		<pubDate>Fri, 09 May 2008 14:23:37 GMT</pubDate>
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		<title>Support and opposition of public-private partnerships</title>
		<link>http://www.eoearth.org/article/Support_and_opposition_of_public-private_partnerships</link>
		<description>&lt;a href='http://www.eoearth.org/article/Support_and_opposition_of_public-private_partnerships'&gt;&lt;img border='0' src='/upload/thumb/5/50/Gains_in_efficiency_from_public-private_partnerships_table.GIF/400px-Gains_in_efficiency_from_public-private_partnerships_table.GIF' width='100'/&gt;&lt;/a&gt;

&lt;p&gt;There are numerous reasons why the international and policy community has supported private participation in water services.  Public-private partnerships have gained support due to the improvements in financing, pricing, efficiency, risk distribution, environmental compliance, human resource management, and service they can provide. Moreover, successful partnerships such as those in Milwaukee, Paris, Buenos Aries, and Mexico City have fostered support for public-private partnerships as a solution to the prevalent problems in &lt;a href=&quot;/article/Water_governance&quot;&gt;water governance&lt;/a&gt;. 
&lt;/p&gt;
 &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Support_and_opposition_of_public-private_partnerships'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Support_and_opposition_of_public-private_partnerships</guid>
		<pubDate>Fri, 09 May 2008 05:42:34 GMT</pubDate>
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		<title>Yellow Sea large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Yellow_Sea_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Yellow_Sea_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/e/e6/Yellowsea.jpg/250px-Yellowsea.jpg' width='100'/&gt;&lt;/a&gt;
&lt;p class=&quot;MsoNormal&quot;&gt; &lt;/p&gt;  &lt;p&gt; A monsoon regime prevails over this Large Marine Ecosystem (LME). Intensive fishing is the primary force driving the LME, with climate as the secondary driving force. The Global Environment Facility (GEF) is supporting an LME project in the Yellow Sea to address critical threats to the coastal and marine environment, and to promote ecosystem-based management of coastal and marine resources. China, North Korea and South Korea are the 3 countries bordering the semi-enclosed Yellow Sea LME. Book chapters and articles pertaining to this LME include She, 1999; Tang, 1989; Tang et al, 1999; and Zhang and Kim, 1999.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Yellow_Sea_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Yellow_Sea_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:54:22 GMT</pubDate>
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		<title>West-Central Australian Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/West-Central_Australian_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/West-Central_Australian_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/4/43/West-central.jpg/250px-West-central.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;h1&gt;Introduction&lt;br /&gt;         &lt;/h1&gt; &lt;p&gt;The West-Central Australia Large Marine Ecosystem (LME) extends from   Cape   Leeuwin,   at Australia’s southwest edge, to NorthWest Cape. The LME  owes   its unity  to the West Australia Current, a north-flowing current  coming  from the circulation   pattern of the counter-clockwise Indian Ocean  gyre  and West Wind Drift. But  it also has a southward-bound band of warm  water  known as the Leeuwin Current,  thanks to which tropical reefs flourish  further  south than anywhere else in the world.  The LME has an extremely  narrow  shelf. It has cool, temperate  waters and it includes seagrass beds  and diverse  and abundant algal communities.  &lt;br /&gt;            &lt;/p&gt;          &lt;h1&gt;Productivity&lt;br /&gt;&lt;/h1&gt;                             &lt;p&gt;For an analysis of the  role of oceanic fronts as highly  productive areas, see Menon, 1998. The West-Central Australian Shelf LME  is considered a Class II, moderately high (150-300 gC/m&lt;sup&gt;2&lt;/sup&gt;-yr) productivity  ecosystem based on SeaWiFS global primary productivity estimates. Because  of its latitudinal range it encompasses diverse pelagic and coastal ecosystems.  The West Wind Drift carries water eastward to the coast of Australia, where  it then flows north as the West Australia Current. The southbound warm water  Leeuwin Current marks a boundary between this warm temperate LME and the tropical waters to the North, but this boundary is variable. See CSIRO for more information on the Leeuwin    Current and its influence on this LME. &lt;a href=&quot;/article/Ocean&quot;&gt;Ocean&lt;/a&gt; current and wind systems   along the coast of this LME inhibit the development of large, highly productive,    Ekman-forced upwelling systems like those that occur along the western margins   of North America, South America and Africa. Shark Bay along the coastline  is an inverse estuary: along the arid coastline, the high evaporation rate  from shallow embayments without significant freshwater inflows and with restricted  tidal exchange creates an environment with a salinity that exceeds that of the seawater. For a general understanding of oceanographic processes affecting  the nutrient dynamics and productivity of Australian marine ecosystems, read  the State of the Environment Report.  For more information on productivity, see Furnas.    For information on Western Australian ocean surface environmental data (currents,  temperatures, salinity, winds), as well as a study of ocean dispersal of Western rock lobster larvae, see a CSIRO report.&lt;/p&gt;          &lt;p&gt;&lt;a href='http://www.eoearth.org/article/West-Central_Australian_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/West-Central_Australian_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:50:51 GMT</pubDate>
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		<title>West Greenland Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/West_Greenland_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/West_Greenland_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/b/b7/West-greenland.jpg/200px-West-greenland.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;p&gt;The West Greenland Shelf Large Marine Ecosystem (LME) begins at Eirik Ridge on the southern tip of Greenland and extends along Greenland’s west &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coast&lt;/a&gt;. It encompasses a number of banks, including the Fyllas Bank. The waters of the West Greenland Current come from Greenland’s south coast, the Labrador Sea, and from East Greenland’s strong Irminger &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;current&lt;/a&gt;. There is a strong link to the East Greenland Shelf LME (#19) because of the clockwise direction of the system of currents. The Davis Strait separates West Greenland from Canada. Changes in sea and &lt;a href=&quot;/article/Atmospheric_composition&quot;&gt;air&lt;/a&gt; &lt;a href=&quot;/article/Temperature&quot;&gt;temperature&lt;/a&gt; appear to be the driving force of this LME.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/West_Greenland_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/West_Greenland_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:47:14 GMT</pubDate>
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		<title>Sulu-Celebes Sea large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Sulu-Celebes_Sea_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Sulu-Celebes_Sea_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/5/5c/Sulu-celebes_sea.jpg/250px-Sulu-celebes_sea.jpg' width='100'/&gt;&lt;/a&gt;
  &lt;p class=&quot;MsoNormal&quot;&gt; &lt;/p&gt;&lt;p class=&quot;MsoNormal&quot;&gt;The Sulu-Celebes Sea Large Marine Ecosystem (LME) is characterized by its tropical climate. It is a semi-enclosed sea bounded by northern Borneo (Malaysia), the southwest &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coast&lt;/a&gt; of the Philippines, and Sulawesi Island (northern coast of Indonesia). It has an area of about 900,000 square &lt;a href=&quot;/article/Meter&quot;&gt;kilometers&lt;/a&gt; (km&lt;sup&gt;2&lt;/sup&gt;), and is comprised of the Sulu Sea and the Celebes Sea (sometimes referred to as the Sulawesi Sea). The LME contains many islands, surrounded by narrow shelf areas. Much of the LME has a depth greater than 3,000 &lt;a href=&quot;/article/Meter&quot;&gt;meters&lt;/a&gt; (m). The LME is oceanographically well defined and is limited by the Palawan trough to the North and by the Sulawesi Island to the South. There is a deeper area, and a chain of islands known as the Sulu Archipelago, separating the two seas. The Global Environment Facility (GEF) has funded the development of a Transboundary Diagnostic Analysis and the preliminary framework for a Strategic Action Programme for this LME (see GEF/UNDP). An article pertaining to this LME is &lt;a href=&quot;/article/Food_and_Agriculture_Organization_%28FAO%29&quot;&gt;Food and Agriculture Organization (FAO)&lt;/a&gt; of the United States (FAO), 2002.&lt;/p&gt;     &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Sulu-Celebes_Sea_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Sulu-Celebes_Sea_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:41:18 GMT</pubDate>
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		<title>Southwest Australian Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Southwest_Australian_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Southwest_Australian_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/3/37/Southwest-australian.jpg/250px-Southwest-australian.jpg' width='100'/&gt;&lt;/a&gt;
&lt;p class=&quot;MsoNormal&quot;&gt; &lt;/p&gt;  &lt;p&gt;The Southwest Australia Large Marine Ecosystem (LME) is characterized  by its temperate climate. The LME extends from the estuary of the Murray-Darling  river to Australia’s southwest edge at Cape Leeuwin. The LME has a narrow  shelf. It borders the Southern Ocean and includes the Great Australian Bight.  Western boundary &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;currents&lt;/a&gt; flow into the West Wind Drift, which circulates  around the continent of &lt;a href=&quot;/article/Antarctica&quot;&gt;Antarctica&lt;/a&gt;. It is bordered by the states of South  Australia and Western Australia. &lt;/p&gt;             &lt;h1&gt;Productivity &lt;br /&gt;  &lt;/h1&gt;                          &lt;p&gt;The Southwest Australian Shelf LME is considered a Class  II, moderately high (150-300 grams of &lt;a href=&quot;/article/Carbon&quot;&gt;carbon&lt;/a&gt; per square &lt;a href=&quot;/article/Meter&quot;&gt;meter&lt;/a&gt; per year) productivity ecosystem based on SeaWiFS  global primary productivity estimates. This LME has small latitudinal range.  It borders on the Southern Ocean and is a haven to thousands of fish and &lt;a href=&quot;/article/Marine_biomes&quot;&gt;marine&lt;/a&gt; species including humpback whales, sea lions, penguins and dolphins. Locally significant upwelling of nutrient-enriched waters is known to occur at sites along the &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coast&lt;/a&gt; of South Australia. Zonation in this LME is evidenced by shallow-water reef fish. Three &lt;a href=&quot;/article/Ecology&quot;&gt;ecological&lt;/a&gt; barriers appear to inhibit dispersal:  a sharp &lt;a href=&quot;/article/Temperature&quot;&gt;temperature&lt;/a&gt; gradient around Albany near the cessation of the Leeuwin  Current; and two interruptions in the nearshore &lt;a href=&quot;/article/Composition_of_rocks&quot;&gt;rocky&lt;/a&gt; reef area: in the center  of the Great Australian Bight, and at the mouth of the Murray River. For a general understanding of oceanographic processes affecting nutrient dynamics  and the productivity of Australian marine ecosystems, see the State of the Environment Report. For more information on productivity, see Furnas. &lt;/p&gt;                          &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Southwest_Australian_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
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		<pubDate>Fri, 09 May 2008 02:36:29 GMT</pubDate>
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		<title>Southeast Australian Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Southeast_Australian_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Southeast_Australian_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/f/f7/Australia_map2.jpg/250px-Australia_map2.jpg' width='100'/&gt;&lt;/a&gt;
  &lt;p class=&quot;MsoNormal&quot;&gt; &lt;/p&gt;  &lt;p&gt; The Southeast Australia Large Marine Ecosystem (LME) extends from Cape Howe, at the southern end of the state of New South Wales, to the estuary of the &lt;a href=&quot;/article/Murray-Darling_woodlands_and_mallee&quot;&gt;Murray-Darling&lt;/a&gt; river system in the State of South Australia. It borders the Southern Ocean and the western boundary &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;currents&lt;/a&gt; flowing into the West Wind Drift, which circulates around the continent of &lt;a href=&quot;/article/Antarctica&quot;&gt;Antarctica&lt;/a&gt;. It contains the island of Tasmania and the Bass Strait, which separates the island from the Victoria State mainland in the Tasmanian Sea. The LME has a diversity of habitats such as seagrass beds, mud flats, intertidal and sub-tidal &lt;a href=&quot;/article/Composition_of_rocks&quot;&gt;rocky&lt;/a&gt; reefs, mangrove kelp forests and pelagic systems. The Murray-Darling river system has a large catchment area, and it transports nutrients and sediments from the land into the &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coastal&lt;/a&gt; waters. The climate is temperate.  &lt;br /&gt;           &lt;/p&gt;                &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Southeast_Australian_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Southeast_Australian_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:32:34 GMT</pubDate>
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		<title>South Brazil Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/South_Brazil_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/South_Brazil_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/9/91/LMEsouthbrazilshelf2.jpg/250px-LMEsouthbrazilshelf2.jpg' width='100'/&gt;&lt;/a&gt;
                                            &lt;p class=&quot;MsoNormal&quot;&gt; &lt;/p&gt;  &lt;p&gt;The South Brazil Shelf Large Marine Ecosystem is characterized by its mixed climate. The &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;Brazil Current&lt;/a&gt; flows parallel to this &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coast&lt;/a&gt; and is an offshoot of the &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;South Equatorial Current&lt;/a&gt;. The continental shelf is wide, reaching 220 kilometers  (km) in some areas. This Large Marine Ecosystem (LME) has a composite structure of environmental conditions, with high water &lt;a href=&quot;/article/Temperature&quot;&gt;temperatures&lt;/a&gt; at least in some periods of the year. It is subjected to relatively intense shelf edge and wind-driven &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;upwellings&lt;/a&gt; of nutrient rich waters in the summer (see Hubold, 1980a,b; and Bakun and Parrish, 1991). It is controlled by shelf topography. It has material sources from land. It sustains moderately diverse &lt;a href=&quot;/article/Food_web&quot;&gt;food webs&lt;/a&gt; and higher production than the East Brazil LME to the north. LME book chapters and articles pertaining to the South Brazil Shelf include Bakun, 1993, and Ekau and Knoppers, 2003.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/South_Brazil_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/South_Brazil_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:28:39 GMT</pubDate>
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		<title>Somali Coastal Current large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Somali_Coastal_Current_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Somali_Coastal_Current_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/e/ee/LME31location.jpg/250px-LME31location.jpg' width='100'/&gt;&lt;/a&gt;
              &lt;p&gt;This Large Marine Ecosystem (LME) is characterized  by its tropical climate. It is a monsoon-influenced Indian Ocean ecosystem,  which lies off the northeastern margin of the African continent. It includes  the continental shelf areas of Yemen,  Somalia, Kenya and Tanzania. In the summer, its dominant oceanographic feature  is the strong, northerly flowing Somali Current. In the winter the Somali  Current reverses its flow. Book chapters and articles pertaining to this  LME include Alexander, 1998, Baars et al, 1998, Bakun et al, 1998, Dwivedi  and Choubey, 1998, Mailu, 1998, Nguta, 1998, Okemwa, 1998, Pollock, 1998 and Weru, 1998. The Global International Waters Assessment (GIWA) has a Somali Coastal Current  page.&lt;/p&gt;              &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Somali_Coastal_Current_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
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		<pubDate>Fri, 09 May 2008 02:26:13 GMT</pubDate>
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		<title>Sea of Japan large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Sea_of_Japan_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Sea_of_Japan_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/4/41/LME50location.jpg/300px-LME50location.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;p&gt;The Sea of Japan Large Marine Ecosystem (LME) is a semi-enclosed sea with an area of approximately 978,000 square kilometers (km&lt;sup&gt;2&lt;/sup&gt;), a volume of 1,713,000 cubic kilometers (km&lt;sup&gt;3&lt;/sup&gt;), and a mean depth of 1,350 &lt;a href=&quot;/article/Meter&quot;&gt;meters&lt;/a&gt; (m). The Sea of Japan is connected to the Sea of Okhotsk, the Northern Pacific Ocean and the East China Sea through four shallow straits. The Tsushima Current, a small branch of the warm Kuroshio Current, enters the Sea of Japan through the Tsushima Strait between Kyushu and Korea and flows out to the Pacific through the Tsugaru and Soya Straits. Climate is the primary force driving the LME, with intensive fishing as the secondary driving force. LME book chapters and articles pertaining to this LME include Terazaki, 1999.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Sea_of_Japan_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Sea_of_Japan_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:23:11 GMT</pubDate>
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		<title>Red Sea large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Red_Sea_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Red_Sea_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/3/35/LME33location.jpg/250px-LME33location.jpg' width='100'/&gt;&lt;/a&gt;
                &lt;p&gt;This Large Marine Ecosystem (LME) is characterized by its tropical  climate. This semi-enclosed LME is situated between the continents of Africa  and Asia, and it links the Mediterranean Sea and the Indian Ocean. Its width  varies from 30 to 280 &lt;a href=&quot;/article/Meter&quot;&gt;kilometers&lt;/a&gt; (km). The Global Environment Facility (GEF) is supporting an LME project aimed  at protecting the unique &lt;a href=&quot;/article/Coral_reef&quot;&gt;coral reefs&lt;/a&gt; of this LME, and sustaining its valuable  &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coastal&lt;/a&gt; and &lt;a href=&quot;/article/Marine_biomes&quot;&gt;marine&lt;/a&gt; resources. LME book chapters and articles pertaining to  this LME include Baars et al, 1998, and Getahun, 1998.&lt;br /&gt;          &lt;/p&gt;                               &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Red_Sea_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Red_Sea_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:18:41 GMT</pubDate>
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		<title>Patagonian Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Patagonian_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Patagonian_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/8/8b/LMEpatagonian1.JPG/250px-LMEpatagonian1.JPG' width='100'/&gt;&lt;/a&gt;
                                          &lt;p class=&quot;MsoNormal&quot;&gt; &lt;/p&gt;  &lt;p&gt;The Patagonian Shelf Large Marine Ecosystem (LME) extends from Uruguay to the    Strait of Magellan. It has a total area of about 2.7 million sqaure kilometers. The continental    shelf is relatively narrow in the north but widens progressively to the  south,  where it reaches a width of about 850 kms. The LME has a distinctive  bathymetry  and hydrography. It is influenced by two major &lt;a href=&quot;/article/Wind&quot;&gt;wind&lt;/a&gt;-driven currents:  the northward flowing Falklands/Malvinas Current and the southward flowing  Brazil Current (Bakun, 1993). The two currents provide the LME with a  distinctive ecological boundary to the east. The LME is a composite area with a unique combination of characteristics. &lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Patagonian_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Patagonian_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:16:25 GMT</pubDate>
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		<title>Oyashio Current large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Oyashio_Current_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Oyashio_Current_large_marine_ecosystem'&gt;&lt;img border='0' src='/media/approved/0/08/LME51location.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;p&gt;The Oyashio Current Large Marine Ecosystem (LME) is characterized by its sub-arctic climate. It is influenced by the cold Oyashio Current (“parent current”), also known as the Kurile Current. The Oyashio Current originates in the Sea of Okhotsk and flows south along the southern &lt;a href=&quot;/article/South_Sakhalin-Kurile_mixed_forests&quot;&gt;Kurile Islands&lt;/a&gt;. It meets the warmer Kuroshio Current off the coast of Japan’s Honshu Island. The topography of the LME includes the Kuril-Kamchatka Trench and Rise. The countries bordering the LME are Russia and Japan. LME book chapters and articles include Minoda, 1989 &lt;span class=&quot;reference&quot;&gt;&lt;sup id=&quot;ref_1&quot; class=&quot;plainlinksneverexpand&quot;&gt;&lt;a href=&quot;#endnote_1&quot; class='external autonumber' title=&quot;#endnote 1&quot;&gt;[1]&lt;/a&gt;&lt;/sup&gt;&lt;/span&gt;.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Oyashio_Current_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Oyashio_Current_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:14:12 GMT</pubDate>
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		<title>Norwegian Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Norwegian_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Norwegian_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/9/95/Norwegian-shelf.jpg/200px-Norwegian-shelf.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;p&gt;The Norwegian Shelf Large Marine Ecosystem (LME) is characterized by its Subarctic climate. It is a western boundary ecosystem situated off the West &lt;a href=&quot;/article/Coastal_zone&quot;&gt;Coast&lt;/a&gt; of Norway. The Iceland-Faroe Ridge separates the relatively warm waters of the Northeast North Atlantic from the cold Arctic deep water of the Norwegian Sea. A boundary current flows along the edge of the Norwegian Shelf into the Arctic &lt;a href=&quot;/article/Region&quot;&gt;region&lt;/a&gt;. The cold and low salinity East Icelandic &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;Current&lt;/a&gt; flows southeast towards the Norwegian Basin. Climate is the primary force driving the LME, with intensive fishing as the secondary driving force. LME book chapters and articles pertaining to this LME include Ellertsen, et al, 1990; and Blindheim and Skjoldal, 1993.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Norwegian_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Norwegian_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:12:10 GMT</pubDate>
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		<title>Northwest Australian Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Northwest_Australian_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Northwest_Australian_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/media/approved/5/51/Northwest.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;p&gt;The Northwest Australia Large Marine Ecosystem (LME) is characterized by its   tropical climate. It extends from North West Cape to the vicinity of the  Timor Sea. The LME has a wide continental shelf and it includes topographical   features such as the Exmouth Plateau, the Rowley Shelf and the Sahul Shelf.   The LME is positioned on the path of the Indonesian Throughflow, a warm-water   current flowing from the Pacific into the Indian Ocean. This current warms   the LME’s sea surface and increases rainfall over Western Australia. Rainfall   however is irregular, with occasional cyclonic disturbances and flash flooding   resulting in brown sediments. The tropical waters are warm, and the coast   includes reefs and extensive mangrove forests. Tropical cyclones are common   seasonal events in this LME. Cyclones exert pronounced effects on the continental    shelf and on coastal marine ecosystems. The rainfall that accompanies cyclonic    weather systems can be a major source of freshwater to the region, causing    widespread though episodic flooding. &lt;br /&gt;      &lt;/p&gt;                                  &lt;h1&gt;Productivity&lt;br /&gt;&lt;/h1&gt;                                         &lt;p&gt;      The Northwest Australian Shelf Large Marine Ecosystem is considered a  Class  III, low productivity (&amp;lt; 150 gC/m2-yr) ecosystem based  on SeaWiFS  global primary productivity estimates. &lt;a href=&quot;/article/Temperature&quot;&gt;Temperature&lt;/a&gt; and salinity  measurements of the Indonesian Throughflow and the South Equatorial Current  were made as part of the World Ocean Circulation Experiment (WOCE). More information is provided in CSIRO    Marine Research. The Northwest Australian Shelf system is characterized   by a high-energy tidal regime. Tidally induced mixing is a major contributor   to nutrient dynamics. Bottom friction acts in a manner analogous to wind  stress on the surface to mix the water column. Shelf upwelling and cyclonic  disruptions also contribute to nutrient inputs that support the productivity  of this LME. The warm tropical waters are the home of corals, fish, starfish, sponges, turtles and shells. The continental shelf supports a diverse demersal  fish community. For a general understanding of oceanographic processes affecting    nutrient dynamics and the productivity of Australian marine ecosystems,  see the State of the Environment  Report,  and Furnas.    &lt;br /&gt;                     &lt;/p&gt;                                  &lt;h1&gt;Fish and Fisheries&lt;br /&gt;&lt;/h1&gt;                                         &lt;p&gt;      Australian waters are relatively nutrient-poor and unable to sustain  large  fish populations. In the Northwest Australian Shelf LME, fish stocks  are quite small. The level of endemicity in northern Australian LMEs is low,  with most species distributed widely in the Indo-West Pacific region. Reef  fisheries occur in the Rowley Shoals, a chain of coral atolls at the edge  of the LME’s wide continental shelf. Demersal species that are fished in this LME include Lethrinus, Nemipterus, Saurida, and Lutjanus. These demersal species  have historically been fished by foreign fleets. A small domestic trap fishery  for Lethrinus, Lutjanus, and Epinephelus   exists in areas subjected to little trawling. Until recently, fisheries resources were usually managed in separate fishery units. Under the Environment Protection and Biodiversity Conservation Act 1999 (the EPBC Act), the Commonwealth Government now has a framework that helps it to respond effectively to current and emerging environmental problems, and to ensure that any harvesting of marine species is managed for &lt;a href=&quot;/article/Ecology&quot;&gt;ecological&lt;/a&gt; &lt;a href=&quot;/article/Sustainability&quot;&gt;sustainability&lt;/a&gt;. After examining several possible management regimes for this LME, the government of Australia divided the area into three zones and closed two of them to trawling. It is thought that there will be an expansion of trap fishing in the two closed areas after the species composition changes induced by trawling are reversed. For detailed fish catch statistics for this LME, see data collected by the University of British Columbia   Fisheries Center. A graphic representation of 12 fishing groups is shown   below. The &lt;a href=&quot;/article/Food_and_Agriculture_Organization_%28FAO%29&quot;&gt;Food and Agriculture Organization (FAO)&lt;/a&gt;   website provides information on Australia’s fisheries industry. &lt;/p&gt;                                     &lt;p&gt;&amp;nbsp;&lt;/p&gt;                                      &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Northwest_Australian_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/Northwest_Australian_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:10:20 GMT</pubDate>
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		<title>Northeast Australian Shelf/Great Barrier Reef large marine ecosystem</title>
		<link>http://www.eoearth.org/article/Northeast_Australian_Shelf_Great_Barrier_Reef_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/Northeast_Australian_Shelf_Great_Barrier_Reef_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/8/89/Northeast-australia1.jpg/250px-Northeast-australia1.jpg' width='100'/&gt;&lt;/a&gt;
                  &lt;p class=&quot;MsoNormal&quot;&gt;The Northeast Australia Large Marine Ecosystem (LME) is characterized by its tropical climate. It lies in the Pacific Ocean along the eastern margin of Australia. The LME is bounded by the Coral Sea to the East, and by the Torres Strait to the North. It is characterized by the South Equatorial Current, a part of the Pacific Ocean counterclockwise gyre, and by the &lt;a href=&quot;/article/Great_Barrier_Reef_World_Heritage_Area%2C_Australia&quot;&gt;Great Barrier Reef&lt;/a&gt; (GBR), a system of &lt;a href=&quot;/article/Coral_reef&quot;&gt;coral reefs&lt;/a&gt; that stretches 2,000 &lt;a href=&quot;/article/Meter&quot;&gt;kilometers&lt;/a&gt; (km) along Australia’s northeast &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coast&lt;/a&gt;. It is the largest system of corals and related life forms in the world. Nutrient enrichment and mixing in this LME are due to &lt;a href=&quot;/article/Tide&quot;&gt;tidal&lt;/a&gt; effects. Intensive &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fishing&lt;/a&gt; is the primary force driving the LME, with climate as the secondary driving force. LME book chapters and articles pertaining to this LME include Bradbury and Mundy, 1989, Kelleher, 1993, and Brodie, 1999. &lt;/p&gt;  &lt;h1&gt;&lt;strong&gt;Productivity&lt;/strong&gt;&lt;/h1&gt;                 &lt;p class=&quot;MsoNormal&quot;&gt;&lt;a href=&quot;/article/Tropical_weather_and_hurricanes&quot;&gt;Tropical cyclones&lt;/a&gt; are common seasonal events in this &lt;a href=&quot;/article/Region&quot;&gt;region&lt;/a&gt;. There is high &lt;a href=&quot;/article/Biodiversity&quot;&gt;biological diversity&lt;/a&gt; in this LME, with high numbers of rare species. 350 species of hard coral are found on the &lt;a href=&quot;/article/Great_Barrier_Reef_World_Heritage_Area%2C_Australia&quot;&gt;Great Barrier Reef&lt;/a&gt; (GBR), along with 1,500 species of fish, 240 species of seabirds, and at least 4,000 species of mollusks (see Brodie, 1999). The physical and biological structure of the GBR is complex. For a map of the GBR region, see Kelleher, 1993, p. 273. Tidally-induced mixing in the GBR is a major contributor to the nutrient dynamics of this &lt;a href=&quot;/article/Marine_biomes&quot;&gt;marine&lt;/a&gt; ecosystem. For more information on oceanographic  processes in this LME, see Furnas. For large-scale shifts in biomass of the  GBR, see Bradbury and Mundy, 1989. There has been a steady accumulation of  knowledge and understanding of the structure and dynamics of this system. For more information about the large-scale effects of Crown-of-thorns starfish  outbreaks on the benthic community, and for the propagation of effects into the fish and &lt;a href=&quot;/article/Plankton&quot;&gt;plankton&lt;/a&gt; communities, see Bradbury and Mundy, 1989. The hard corals are at least halved in abundance in the parts of the system where there is intense starfish activity. For detailed information on the corals in this LME, see data collected by the University of British Columbia Fisheries Center. The Northeast Australian Shelf LME is considered a Category II, moderately high (150-300 grams of &lt;a href=&quot;/article/Carbon&quot;&gt;carbon&lt;/a&gt; per square &lt;a href=&quot;/article/Meter&quot;&gt;meter&lt;/a&gt; per year) productivity ecosystem, according to SeaWiFS global primary productivity estimates. &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;Ocean currents&lt;/a&gt; and &lt;a href=&quot;/article/Wind&quot;&gt;wind&lt;/a&gt; systems along this &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coast&lt;/a&gt; inhibit the development of highly productive upwelling systems like those occurring along the western margins of North America, South America and Africa. Sources of nutrients to the LME are Coral Sea surface water, Coral Sea upwellings of deep sea water, &lt;a href=&quot;/article/Terrestrial_biome&quot;&gt;terrestrial&lt;/a&gt; &lt;a href=&quot;/article/Surface_runoff_of_water&quot;&gt;runoff&lt;/a&gt;, and &lt;a href=&quot;/article/Atmospheric_composition&quot;&gt;atmospheric&lt;/a&gt; inputs. &lt;/p&gt;  &lt;h1&gt;&lt;strong&gt;Fish and Fisheries&lt;/strong&gt;&lt;/h1&gt;  &lt;p class=&quot;MsoNormal&quot;&gt;These waters are relatively nutrient-poor and unable to sustain large fish populations. The &lt;a href=&quot;/article/Food_and_Agriculture_Organization_%28FAO%29&quot;&gt;Food and Agriculture Organization (FAO)&lt;/a&gt; 10-year trend shows a total catch of 10,000 tons in 1990, 14,000 tons in 1996, and 11,000 tons in 1999 (see FAO, 2003). The average yearly catch is 12,000 tons. Catch trends are very diverse. There is a very high percentage of crustacean catches (more than half), and mollusks. On this narrow continental shelf, production depends on nutrient runoff and nutrient-rich upwellings. The trawl &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fishery&lt;/a&gt; (see Brodie, 1999) targets tiger prawns, banana prawns and king prawns. The annual catch for scallops and prawns is about 8,000 tons. Scallops are caught in the southern section of the GBR Marine Park. The Torres Strait Prawn is a fully-exploited fishery. The Torres Strait Lobster is still somewhat underexploited. The Northeast Australia LME is driven by a predator, the Crown-of-Thorns starfish (&lt;em&gt;Acanthaster planci&lt;/em&gt;), a coral-eating echiderm that has devastated &lt;a href=&quot;/article/Coral_reef&quot;&gt;reefs&lt;/a&gt; (see Kelleher, 1993). The starfish has few &lt;a href=&quot;/article/Predation&quot;&gt;predators&lt;/a&gt; in the environment. There is uncertainty as to whether the outbreaks are human induced or are a natural part of the &lt;a href=&quot;/article/Ecology&quot;&gt;ecological&lt;/a&gt; variability of the GBR (see Brodie, 1999). Possible anthropogenic causes are the overfishing of Crown-of-Thorns predators such as fish or the triton shell, and enhanced nutrient runoff from coastal development. Until recently, fisheries resources were usually managed in separate fishery units. Under the Environment Protection and &lt;a href=&quot;/article/Biodiversity&quot;&gt;Biodiversity&lt;/a&gt; Conservation Act 1999 (the EPBC Act), the Commonwealth Government now has a framework that helps it to respond effectively to current and emerging environmental problems, and to ensure that any harvesting of marine species is managed for ecological &lt;a href=&quot;/article/Sustainability&quot;&gt;sustainability&lt;/a&gt;. For sustainable fishing issues in the GBR, see Kelleher, 1993. The FAO provides information on Australia’s fisheries and the characteristics of the industry. The University  of British Columbia Fisheries Center has detailed fish catch statistics for this LME. The data can be viewed in the graph above.&lt;br /&gt; &lt;/p&gt;          &lt;h1&gt;&lt;strong&gt;Pollution and Ecosystem Health&lt;/strong&gt;&lt;/h1&gt;                  &lt;p class=&quot;MsoNormal&quot;&gt;The Crown-of-Thorns starfish (&lt;em&gt;Acanthaster planci&lt;/em&gt;) has devastated &lt;a href=&quot;/article/Coral_reef&quot;&gt;reefs&lt;/a&gt; (see Kelleher, 1993). The starfish has few predators in the environment. Outbreaks of this starfish may be human induced or are a natural part of the ecological variability of the GBR (see Brodie, 1999). Possible anthropogenic causes are the overfishing of Crown-of-Thorns predators such as fish or the triton shell, and enhanced nutrient runoff from coastal development. For more information about the large-scale effects of Crown of thorns starfish outbreaks on the benthic community, see Bradbury and Mundy, 1989. See the State of the Environment Report. The &lt;a href=&quot;/article/Great_Barrier_Reef_World_Heritage_Area%2C_Australia&quot;&gt;GBR&lt;/a&gt; is also threatened by increased shipping. A number of substantial ports line the GBR coastline (see Brodie, 1999), and navigation in the Torres Strait is intense. Ballast water introductions of &lt;a href=&quot;/article/Toxicity&quot;&gt;toxic&lt;/a&gt; dinoflagellates have caused serious ecological problems in other parts of Australia but so far no undesirable introduction has been detected in the GBR region. One significant anthropogenic impact on the GBR region is the change in the water quality of &lt;a href=&quot;/article/Terrestrial_biome&quot;&gt;terrestrial&lt;/a&gt; &lt;a href=&quot;/article/Surface_runoff_of_water&quot;&gt;runoff&lt;/a&gt; (see Brodie, 1999). Excess nutrients can have a number of effects on coral and coral reef systems (see Kinsey, 1991b). There is considerable evidence that reefs, particularly inshore fringing reefs, are now muddier and have less coral cover and more algal cover (see Brodie, 1999). There are environmental impacts on the GBR caused by tourism. Large numbers of people are engaged in recreational &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fishing&lt;/a&gt;, SCUBA diving and boating. Activities associated with the use of this kind of equipment have the potential to affect the environment through the pollution of water by boats and the disturbance of species and habitats (including mangroves). Recreational fishermen tend to target reef ecosystems and remove larger &lt;a href=&quot;/article/Predation&quot;&gt;predatory&lt;/a&gt; species. The effects of this selective removal of fish are largely unknown. Shore-based recreational fishing can have effects on shore populations of invertebrates that are collected for bait in intensively visited areas. A major source of environmental impacts is the provision of infrastructure to support tourism (airports, power generation facilities, accommodation, sewage treatment and disposal facilities, moorings, and marine transport, including high-speed ferries). Often the infrastructure is required in fragile or pristine environments that are susceptible to disturbance and fragmentation. For more information on pollution control in the GBR, see Kelleher, 1993. &lt;/p&gt;  &lt;h1&gt;&lt;strong&gt;Socioeconomics&lt;/strong&gt;&lt;/h1&gt;                       &lt;p&gt;The &lt;a href=&quot;/article/Food_and_Agriculture_Organization_%28FAO%29&quot;&gt;FAO&lt;/a&gt; provides information on Australia’s &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fisheries&lt;/a&gt; and the socioeconomic benefits of the industry. &lt;br /&gt;&lt;a href=&quot;/article/Marine_biomes&quot;&gt;Marine&lt;/a&gt; and &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coastal&lt;/a&gt;-based tourism is the main industry of the GBR, an internationally recognized tourist site and one of Australia’s 6 World Heritage Areas (see Brodie, 1999). In the 1980s, tourism in the GBR was evaluated at 150,000 visitor-days. In the late 1990s, tourism was worth $1 billion, with 1.5 million visitor-days). Whale-watching occurs off the coast of Queensland. Shipping  in the LME is a major activity. Extracting petroleum from the &lt;a href=&quot;/article/Coral_reef&quot;&gt;reef&lt;/a&gt; is permissible but not mining. With this level of usage, continuing tourism clearly depends on &lt;a href=&quot;/article/Sustainability&quot;&gt;sustaining&lt;/a&gt; environmental and heritage values. Tourism can affect the lifestyle of community residents in ways they perceive as intrusive. Negative social impacts may include real or perceived increases in crowding, prices, or crime. Increased tourism may also result in increasing conflict between various uses of the marine and coastal areas. In terms of fisheries, for instance, there can be tensions between recreation, commercial and indigenous interests. Traditional fishing by Aborigines and Torres Strait islanders is confined to areas close to Aboriginal communities (see Brodie, 1999). For more information about human uses of the &lt;a href=&quot;/article/Great_Barrier_Reef_World_Heritage_Area%2C_Australia&quot;&gt;Great Barrier Reef&lt;/a&gt;, see Kelleher, 1993.&lt;/p&gt; &lt;h1&gt;&lt;strong&gt;Governance&lt;/strong&gt;&lt;/h1&gt;                                   &lt;p class=&quot;MsoNormal&quot;&gt;The Northeast Australia LME lies off the &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coast&lt;/a&gt; of the State of Queensland. It extends to the Torres Strait, which separates Australia from Papua New Guinea. The main governance issues in this LME pertain to &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fisheries&lt;/a&gt; management and to the Great Barrier Reef Marine Park. Under the offshore constitutional settlement between the Australian states and the federal government, the management of most fisheries within the GBR is the  responsibility of the Queensland government (see Brodie, 1999). For more information on the governance of Australia’s fisheries, see the &lt;a href=&quot;/article/Food_and_Agriculture_Organization_%28FAO%29&quot;&gt;FAO&lt;/a&gt; website. Under the  Environment Protection and &lt;a href=&quot;/article/Biodiversity&quot;&gt;Biodiversity&lt;/a&gt; Conservation Act 1999 (the EPBC Act),  the Commonwealth Government has a framework that helps it to respond effectively to current and emerging environmental problems, and to ensure that any harvesting of marine species is managed for &lt;a href=&quot;/article/Ecology&quot;&gt;ecological&lt;/a&gt; &lt;a href=&quot;/article/Sustainability&quot;&gt;sustainability&lt;/a&gt;. The GBR Marine Park Act was one of the first pieces of legislation in the world to apply the concept of sustainable development to the management of a large natural area. The GBR Marine Park Authority was established in 1975 to manage the  multi-use park. The Authority aims to protect the natural ecosystems of the  GBR, and ensures that &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fishing&lt;/a&gt; does not have unacceptable ecological impacts on the fished areas and the &lt;a href=&quot;/article/Coral_reef&quot;&gt;reefs&lt;/a&gt;. For more information on the history and zoning system of the GBR Marine Park, see Brodie, 1999, and Kelleher, 1993. Compulsory pilotage in the area reduces the risk of collision with reefs. On the national level, the Commonwealth Government developed a National Action Plan for Tourism in 1998. The Plan, which identifies conservation and careful management of the environment as essential to the long-term viability of the tourism industry, makes a commitment to ecologically sustainable tourism development and recognizes that environmental considerations should be an integral part of economic decisions. The marine tourism industry has produced a code of conduct that covers issues such as anchoring, removal of rubbish, fish feeding and preservation of World Heritage values. Australia declared a 200 nautical-mile Exclusive Economic Zone in 1978. Australia is party to the following international agreements: Antarctic-Environmental Protocol, Antarctic Treaty, &lt;a href=&quot;/article/Biodiversity&quot;&gt;Biodiversity&lt;/a&gt;, Climate Change, Endangered Species, Environmental Modification, Hazardous Wastes, Law of the Sea, Marine Dumping, Marine Life Conservation, Nuclear Test Ban, Ozone Layer Protection, Ship Pollution, Tropical Timber 83, &lt;a href=&quot;/article/Wetland&quot;&gt;Wetlands&lt;/a&gt;, and Whaling.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/Northeast_Australian_Shelf_Great_Barrier_Reef_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
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		<pubDate>Fri, 09 May 2008 02:08:27 GMT</pubDate>
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		<title>North Sea large marine ecosystem</title>
		<link>http://www.eoearth.org/article/North_Sea_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/North_Sea_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/2/2d/North-sea.jpg/200px-North-sea.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;p&gt;The North Sea Large Marine Ecosystem (LME) is characterized by a temperate climate and four seasons. It is a semi-enclosed sea situated on the continental shelf of Northwestern Europe, in the Atlantic Ocean. It covers an area of 745,950 &lt;a href=&quot;/article/Meter&quot;&gt;kilometers&lt;/a&gt; (km&lt;sup&gt;2&lt;/sup&gt;) and has a mean depth of 90 &lt;a href=&quot;/article/Meter&quot;&gt;meters&lt;/a&gt; (m). The North Sea includes one of the most &lt;a href=&quot;/article/Biodiversity&quot;&gt;diverse&lt;/a&gt; &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coastal&lt;/a&gt; regions in the world, with a great variety of habitats (fjords, estuaries, deltas, banks, &lt;a href=&quot;/article/Coastal_zone&quot;&gt;beaches&lt;/a&gt;, sandbanks and mudflats, &lt;a href=&quot;/article/Marsh&quot;&gt;marshes&lt;/a&gt;, &lt;a href=&quot;/article/Composition_of_rocks&quot;&gt;rocks&lt;/a&gt; and islands). Intensive fishing is the primary force driving the LME, with climate as the secondary driving force. England, Scotland, Norway, Sweden, Denmark, Germany, the Netherlands, Belgium and France are the 9 countries bordering the North Sea. LME book chapters and articles pertaining to this LME include Dann, 1986, Dann, 1993, and McGlade, 2002.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/North_Sea_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/North_Sea_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:06:49 GMT</pubDate>
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		<title>North Brazil Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/North_Brazil_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/North_Brazil_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/5/55/LMEnorthbrazil1.JPG/250px-LMEnorthbrazil1.JPG' width='100'/&gt;&lt;/a&gt;
                              &lt;p class=&quot;MsoNormal&quot;&gt; &lt;/p&gt;  &lt;p&gt;The North Brazil Shelf Large Marine Ecosystem is characterized by its tropical|climate. It extends in the &lt;a href=&quot;/article/Ocean&quot;&gt;Atlantic Ocean&lt;/a&gt; from the boundary with the Caribbean Sea to the Paraiba River estuary in &lt;a href=&quot;/article/Brazil&quot;&gt;Brazil&lt;/a&gt;. The Large Marine Ecosystem (LME) owes its unity to the North Brazil Current, which flows parallel to Brazil’s coast and is an extension of the &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;South Equatorial Current&lt;/a&gt; coming from the East. The LME is characterized by a wide shelf, and features macrotides and &lt;a href=&quot;/article/Ocean_circulation&quot;&gt;upwellings&lt;/a&gt; along the shelf edge. It has moderately diverse &lt;a href=&quot;/article/Food_web&quot;&gt;food webs&lt;/a&gt; and high production. &lt;/p&gt;&lt;p&gt;   This LME has high levels of nutrients coming from the Amazon and Tocantins &lt;a href=&quot;/article/River&quot;&gt;rivers&lt;/a&gt;, as well as from the smaller rivers of the Amapa and western Para coastal plains. It is bordered by 4 countries: Brazil, French Guiana, Suriname and Guyana. LME book chapters and articles pertaining to the South Brazil Shelf include Bakun, 1993, and Ekau and Knoppers, 2003.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/North_Brazil_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/North_Brazil_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:05:03 GMT</pubDate>
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		<title>North Australian Shelf large marine ecosystem</title>
		<link>http://www.eoearth.org/article/North_Australian_Shelf_large_marine_ecosystem</link>
		<description>&lt;a href='http://www.eoearth.org/article/North_Australian_Shelf_large_marine_ecosystem'&gt;&lt;img border='0' src='/upload/thumb/2/27/North_australian.jpg/250px-North_australian.jpg' width='100'/&gt;&lt;/a&gt;
 &lt;h1&gt;&lt;strong&gt;Introduction&lt;/strong&gt;&lt;/h1&gt;                 &lt;p class=&quot;MsoNormal&quot;&gt;  &lt;/p&gt;&lt;p class=&quot;MsoNormal&quot;&gt;The North Australia Large Marine Ecosystem (LME) is characterized  by a tropical climate, and is positioned between the Pacific and the Indian  Oceans. Nutrient enrichment and mixing are due to &lt;a href=&quot;/article/Tide&quot;&gt;tidal&lt;/a&gt; mixing, monsoons and &lt;a href=&quot;/article/Tropical_weather_and_hurricanes&quot;&gt;tropical cyclones&lt;/a&gt; in this LME. The Indonesian Throughflow, a warm-water current flowing from the Pacific into the Indian Ocean, plays a vital role in driving the world&amp;#39;s climate system and is also of particular importance to Australia since it helps warm the sea surface of the Indian Ocean. LME articles pertaining to this LME include FAO, 2003.&lt;/p&gt;  &lt;h1&gt;&lt;strong&gt;Productivity&lt;/strong&gt;&lt;/h1&gt;                 &lt;p class=&quot;MsoNormal&quot;&gt; The LME extends from the Timor Sea to the Torres Strait and includes the Arafura Sea and Gulf of Carpentaria. It is bordered by the Timor Trough to the North. A vast continental shelf links Australia with Indonesia and Papua New Guinea. The LME’s Australian &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coastline&lt;/a&gt; is complex and rather poorly known. Supra-tidal mudflats are found along the arid and dry-tropical coastline of the southern Gulf of Carpentaria. The area has a monsoonal climate and tropical cyclones are common seasonal events. High monsoonal summer &lt;a href=&quot;/article/Precipitation_and_fog&quot;&gt;rain&lt;/a&gt; and dry winters result in gray mud sediments inshore and well-developed mangrove creeks. &lt;a href=&quot;/article/Tropical_weather_and_hurricanes&quot;&gt;Tropical cyclones&lt;/a&gt; in this &lt;a href=&quot;/article/Region&quot;&gt;region&lt;/a&gt; have a pronounced effect on the continental shelf and on coastal &lt;a href=&quot;/article/Marine_biomes&quot;&gt;marine&lt;/a&gt; ecosystems. The rainfall that accompanies cyclonic weather systems can be a major source of freshwater to the region, causing widespread though episodic flooding. &lt;a href=&quot;/article/Temperature&quot;&gt;Temperature&lt;/a&gt; and salinity measurements of the Indonesian Throughflow and the South Equatorial Current were made as part of the World Ocean Circulation Experiment (WOCE). Flats in the Gulf of Carpentaria concentrate salt and nutrients for extended periods following tidal inundations and rainfall, then release salty, nutrient-laden water into the &lt;a href=&quot;/article/Coastal_zone&quot;&gt;coastal zone&lt;/a&gt;. The quantitative contribution of these events to the coastal zone is not well known. The North Australia Large Marine Ecosystem is considered a Class I, high productivity (&amp;gt;300 grams of &lt;a href=&quot;/article/Carbon&quot;&gt;carbon&lt;/a&gt; per square &lt;a href=&quot;/article/Meter&quot;&gt;meter&lt;/a&gt; per year) ecosystem based on SeaWiFS global primary productivity estimates. Nutrient discharge from &lt;a href=&quot;/article/River&quot;&gt;rivers&lt;/a&gt; is restricted to the summer wet season and is highly variable. Tidally induced mixing is a major contributor to the nutrient dynamics of this LME. In these systems, bottom friction acts in a manner analogous to &lt;a href=&quot;/article/Wind&quot;&gt;wind&lt;/a&gt; stress on the surface to mix the water column. For information on the marine environment around Australia, see the CSIRO  website. For a general understanding of oceanographic processes affecting the nutrient dynamics and productivity of Australian marine ecosystems, read the State of the Environment Report.  For more information on productivity, see Furnas,  2002.&lt;/p&gt; &lt;h1&gt;&lt;strong&gt;Fish and Fisheries&lt;/strong&gt;&lt;/h1&gt;                  &lt;p class=&quot;MsoNormal&quot;&gt;Fish stocks in the North Australia LME are small but  &lt;a href=&quot;/article/Biodiversity&quot;&gt;diverse&lt;/a&gt;. The level of endemicity in northern Australian LMEs is low, with most species distributed widely in the Indo-West Pacific region. Commercial  &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fisheries&lt;/a&gt; are based on the Northern Prawn (Arafura Sea), mud crab, barramundi,  salmon, shark, Spanish mackerel, as well as snappers and &lt;a href=&quot;/article/Coral_reef&quot;&gt;reef&lt;/a&gt; fish. The Northern Prawn in the Arafura Sea is almost fully exploited. Catch trends are very diverse. The &lt;a href=&quot;/article/Food_and_Agriculture_Organization_%28FAO%29&quot;&gt;Food and Agriculture Organization (FAO)&lt;/a&gt; 10-year trend shows a slight increase from 75,000 tons in  1990 to 80,000 tons in 1999 (see FAO, 2003). There is a very high percentage of crustacean catches (46%), and molluscs (16%). Until recently, fisheries  resources were usually managed in units termed as a fishery. Under the Environment Protection and &lt;a href=&quot;/article/Biodiversity&quot;&gt;Biodiversity&lt;/a&gt; Conservation Act 1999 (the EPBC Act), the Commonwealth Government now has a framework that helps it to respond effectively to current and emerging environmental problems, and to ensure that any harvesting of marine species is managed for &lt;a href=&quot;/article/Ecology&quot;&gt;ecological&lt;/a&gt; &lt;a href=&quot;/article/Sustainability&quot;&gt;sustainability&lt;/a&gt;. For detailed fish catch statistics for this LME, see data collected by the University of British Columbia Fisheries Center. A graphical representation of the data is presented above. FAO also provides information on Australia’s fisheries and the characteristics of the industry.&lt;/p&gt; &lt;h1&gt;&lt;strong&gt;Pollution and Ecosystem Health&lt;/strong&gt;&lt;/h1&gt;                 &lt;p class=&quot;MsoNormal&quot;&gt;The LME is threatened by an increase in shipping and by the transportation of oil. Ships empty of cargo that enter the ports of Northwest Australia are ballasted with water collected in the last port of call. This ballast water has been shown to contain organisms including &lt;a href=&quot;/article/Bacteria&quot;&gt;bacteria&lt;/a&gt;, viruses, algal cells, &lt;a href=&quot;/article/Plankton&quot;&gt;plankton&lt;/a&gt;, and the larval forms of many invertebrates and fish. There are accidental discharges of contaminants, such as &lt;a href=&quot;/article/Oil_spill&quot;&gt;spills&lt;/a&gt; and shipping accidents. The dominant human impacts are related to &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fisheries&lt;/a&gt; and [[terrestrial biome|terrestrial &lt;a href=&quot;/article/Surface_runoff_of_water&quot;&gt;runoff&lt;/a&gt; from deforestation, overgrazing and certain &lt;a href=&quot;/article/Agriculture&quot;&gt;agricultural&lt;/a&gt; practices. Compared with most countries, however, these impacts remain few. Population densities are low in all &lt;a href=&quot;/article/Coral_reef&quot;&gt;coral reef&lt;/a&gt; areas, while the location of many reefs at some distance from the shore further protects them from human impacts. For more information on marine pollution in this LME, see Environment Australia  and a  technical paper from EA on &lt;a href=&quot;/article/Marine_biomes&quot;&gt;marine&lt;/a&gt; disturbances.&lt;/p&gt; &lt;h1&gt;&lt;strong&gt;Socioeconomics&lt;/strong&gt;&lt;/h1&gt;                   &lt;p class=&quot;MsoNormal&quot;&gt;Thousands of people are involved in the &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fisheries&lt;/a&gt;, &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;aquaculture&lt;/a&gt; and processing sectors of the economy. The &lt;a href=&quot;/article/Food_and_Agriculture_Organization_%28FAO%29&quot;&gt;FAO&lt;/a&gt; provides information on the characteristics and socioeconomic benefits of Australia’s &lt;a href=&quot;/article/Fisheries_and_aquaculture&quot;&gt;fishing&lt;/a&gt; industry. There are significant aquaculture activities based on oyster pearls, prawns and barramundi.  Industry, shipping and tourism are major economic  activities. Marine and coastal-based forms of tourism are important in this LME both in terms of domestic and international tourism. A significant proportion  of the Australian population is involved in recreational fishing, surfing, wind surfing, diving, snorkeling, and boating. Tourists from overseas prize the &lt;a href=&quot;/article/Coral_reef&quot;&gt;coral reefs&lt;/a&gt; and the natural and unspoilt marine environment. There are,  however, social, cultural, economic and environmental impacts caused by tourism. Tourism may affect the lifestyle of residents in ways they perceive as intrusive. Negative social impacts may include real or perceived increases in crowding, prices, or crime, as well as increased conflict between commercial, recreational and indigenous interests. Australia’s Aborigines, and the Torres Strait Islanders who occupy parts of the far northeast of the land area, have traditionally made considerable use of reef resources. Arnhem Land is an aboriginal reserve.&lt;/p&gt; &lt;p&gt;&lt;a href='http://www.eoearth.org/article/North_Australian_Shelf_large_marine_ecosystem'&gt;Read Full Article...&lt;/a&gt;&lt;/p&gt;</description>
		<guid>http://www.eoearth.org/article/North_Australian_Shelf_large_marine_ecosystem</guid>
		<pubDate>Fri, 09 May 2008 02:03:24 GMT</pubDate>
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