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		<title>Ocean on EARTH Magazine</title>
		<link>https://www.earthmagazine.org/tags/ocean/</link>
		<description>Recent content in Ocean on EARTH Magazine</description>
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		<language>en-US</language>
		
		
		
			<copyright>American Geosciences Institute. All rights reserved.</copyright>
		
		
			<lastBuildDate>Thu, 08 Nov 2018 09:27:50 -0500</lastBuildDate>
		
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				<title>Down to Earth With: Coastal scientist Gary Griggs</title>
				<link>https://www.earthmagazine.org/article/down-earth-coastal-scientist-gary-griggs/</link>
				<pubDate>Thu, 08 Nov 2018 09:27:50 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/down-earth-coastal-scientist-gary-griggs/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/down-earth-coastal-scientist-gary-griggs/GARYSKYE.jpg&#34; alt=&#34;Coastal scientist Gary Griggs has been teaching at the University of California, Santa Cruz, for the past 50 years. An advocate for ocean science, conservation, policy and education, he has studied coasts around the world, including the beach pictured here, Coral Beach on the Isle of Skye, Scotland. Credit: courtesy of Gary Griggs.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Coastal scientist Gary Griggs has been teaching at the University of California, Santa Cruz, for the past 50 years. An advocate for ocean science, conservation, policy and education, he has studied coasts around the world, including the beach pictured here, Coral Beach on the Isle of Skye, Scotland. Credit: courtesy of Gary Griggs.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Maybe it was the summer camping trips with his family along the Pacific coast, or perhaps surfing off Santa Barbara, Calif., during college, but &lt;a href=&#34;https://campusdirectory.ucsc.edu/cd_detail?uid=griggs&#34;&gt;Gary Griggs&lt;/a&gt; always gravitated to the ocean. He turned that love into a career and has spent the last 50 years teaching about the oceans and coasts at the University of California, Santa Cruz (UCSC).&lt;/p&gt;</description>
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				<title>Surfactants slow oceanic carbon dioxide uptake  </title>
				<link>https://www.earthmagazine.org/article/surfactants-slow-oceanic-carbon-dioxide-uptake/</link>
				<pubDate>Mon, 10 Sep 2018 11:28:54 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/surfactants-slow-oceanic-carbon-dioxide-uptake/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/surfactants-slow-oceanic-carbon-dioxide-uptake/Atlantic_Ocean_Sunset_panoramio.jpg&#34; alt=&#34;Across the Atlantic Ocean, researches sampled the surfactant layer across several sites. Credit: Michael A. Orlando, CC BY-SA 3.0&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Across the Atlantic Ocean, researches sampled the surfactant layer across several sites. Credit: Michael A. Orlando, CC BY-SA 3.0&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;The oceans are the largest long-term carbon sink on Earth, absorbing about a quarter of all anthropogenic carbon dioxide emissions. The rate of exchange of carbon dioxide between the oceans and the atmosphere is thought to be primarily controlled by wind-driven turbulence at the sea surface. More turbulence leads to increasing gas exchange and higher rates of carbon uptake by the ocean. But in a new &lt;a href=&#34;https://www.nature.com/articles/s41561-018-0136-2&#34;&gt;study&lt;/a&gt;, published in Nature Geoscience, scientists found that biomolecules called surfactants floating at the sea surface may significantly reduce carbon dioxide exchange with the atmosphere — reducing the uptake of carbon dioxide by up to 50 percent. &amp;ldquo;As surface temperatures rise, so too do surfactants, which is why this is such a critical finding,&amp;rdquo; said lead author &lt;a href=&#34;https://www.hw.ac.uk/staff/uk/egis/ryan-pereira.htm&#34;&gt;Ryan Pereira&lt;/a&gt; of Heriot-Watt University in Scotland in a &lt;a href=&#34;https://www.ncl.ac.uk/press/articles/latest/2018/05/surfactants/&#34;&gt;statement&lt;/a&gt;.&lt;/p&gt;</description>
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				<title>Radium levels suggest Arctic Ocean chemistry is changing</title>
				<link>https://www.earthmagazine.org/article/radium-levels-suggest-arctic-ocean-chemistry-changing/</link>
				<pubDate>Tue, 10 Apr 2018 11:44:26 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/radium-levels-suggest-arctic-ocean-chemistry-changing/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/radium-levels-suggest-arctic-ocean-chemistry-changing/illustration1_map_renier_edit.jpg&#34; alt=&#34;In 2015, researchers measured radium in the Arctic Ocean from the Chukchi Shelf (where the voyage started) to the North Pole. Elevated radium levels (shown in bright yellow along the cruise route) were found near the North Pole, possibly as a result of transport from the East Siberian Arctic Shelf. Credit: Natalie Renier, Woods Hole Oceanographic Institution.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;In 2015, researchers measured radium in the Arctic Ocean from the Chukchi Shelf (where the voyage started) to the North Pole. Elevated radium levels (shown in bright yellow along the cruise route) were found near the North Pole, possibly as a result of transport from the East Siberian Arctic Shelf. Credit: Natalie Renier, Woods Hole Oceanographic Institution.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Rising temperatures have already caused changes in the Arctic environment, like diminishing sea ice and thawing permafrost. Now, it appears that sea-ice loss could be throwing Arctic Ocean chemistry out of whack.&lt;/p&gt;</description>
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				<title>Gyres spin up, currents get muddled</title>
				<link>https://www.earthmagazine.org/article/gyres-spin-currents-get-muddled/</link>
				<pubDate>Thu, 08 Mar 2018 11:37:13 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/gyres-spin-currents-get-muddled/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/gyres-spin-currents-get-muddled/Cantner_WeddellGyre_map.jpg&#34; alt=&#34;In the Weddell Sea Gyre, one of two clockwise-spinning circulation patterns in the Southern Ocean, warming has accelerated the spinning. Recent research suggests this acceleration — and the warmer, faster-moving Antarctic Circumpolar Currrent and Circumpolar Deepwater that result — may trigger the development of smaller, shorter-lived polynyas like those observed over the past two years. Credit: K. Cantner, AGI.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;In the Weddell Sea Gyre, one of two clockwise-spinning circulation patterns in the Southern Ocean, warming has accelerated the spinning. Recent research suggests this acceleration — and the warmer, faster-moving Antarctic Circumpolar Currrent and Circumpolar Deepwater that result — may trigger the development of smaller, shorter-lived polynyas like those observed over the past two years. Credit: K. Cantner, AGI.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;In addition to polynya formation and warming-induced surface freshening, other factors may also impact open-ocean convection in the Southern Ocean. The warming atmosphere is shifting global climatic zones and their associated wind fields poleward in both hemispheres. In the Weddell Sea Gyre, one of two clockwise-spinning circulation patterns in the Southern Ocean, this shift has resulted in a dramatic increase in wind stress curl (the strength of the wind&amp;rsquo;s influence on ocean water flow) over the past two years.&lt;/p&gt;</description>
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				<title>Disrupting the deep: Ocean warming reaches the abyss</title>
				<link>https://www.earthmagazine.org/article/disrupting-deep-ocean-warming-reaches-abyss/</link>
				<pubDate>Thu, 08 Mar 2018 11:29:52 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/disrupting-deep-ocean-warming-reaches-abyss/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/disrupting-deep-ocean-warming-reaches-abyss/OceanIce_SOCCUM_HannahZanowski.jpg&#34; alt=&#34;SOCCUM Project, Hannah Zanowski, CC BY 2.0&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;SOCCUM Project, Hannah Zanowski, CC BY 2.0&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Seventy-one percent of our planet is covered by ocean, and these basins contain 97 percent of Earth&amp;rsquo;s near-surface water. The ocean lies at the heart of the global climate system, shaping all parts of our environment, even in the deepest continental interiors. So as the ocean goes, so goes the planet — and the ocean is warming.&lt;/p&gt;</description>
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				<title>Heating up Enceladus&#39; ice-covered ocean</title>
				<link>https://www.earthmagazine.org/article/heating-enceladus-ice-covered-ocean/</link>
				<pubDate>Tue, 27 Feb 2018 13:20:21 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/heating-enceladus-ice-covered-ocean/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/heating-enceladus-ice-covered-ocean/PIA19656-16.jpg&#34; alt=&#34;Friction produced by tidal forces acting on Enceladus&amp;#39; highly fragmented, porous core could produce enough heat to sustain the moon&amp;#39;s liquid ocean. Credit: NASA/JPL-Caltech.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Friction produced by tidal forces acting on Enceladus&amp;#39; highly fragmented, porous core could produce enough heat to sustain the moon&amp;#39;s liquid ocean. Credit: NASA/JPL-Caltech.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Saturn&amp;rsquo;s sixth-largest moon, Enceladus, is covered by ice, but just beneath its icy surface lies an ocean of liquid water. New &lt;a href=&#34;https://www.nature.com/articles/s41550-017-0289-8&#34;&gt;research&lt;/a&gt; suggests that this internal ocean may be maintained in a liquid state by heat generated by tidal friction within the moon&amp;rsquo;s fragmented, rocky core.&lt;/p&gt;</description>
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				<title>Driftwood reveals ancient Arctic currents and sea-ice levels</title>
				<link>https://www.earthmagazine.org/article/driftwood-reveals-ancient-arctic-currents-and-sea-ice-levels/</link>
				<pubDate>Thu, 28 Dec 2017 12:37:35 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/driftwood-reveals-ancient-arctic-currents-and-sea-ice-levels/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/driftwood-reveals-ancient-arctic-currents-and-sea-ice-levels/DriftwoodPhippsoya.jpg&#34; alt=&#34;Driftwood frozen into sea ice can be transported around the Arctic, eventually collecting on distant shores such as on the island of Phippsøya in Svalbard, which lies to the east of northern Greenland. Credit: Marc Macias-Fauria&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Driftwood frozen into sea ice can be transported around the Arctic, eventually collecting on distant shores such as on the island of Phippsøya in Svalbard, which lies to the east of northern Greenland. Credit: Marc Macias-Fauria&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Arctic driftwood up to 12,000 years old is giving scientists a better understanding of how ocean currents and sea ice in the far north have changed through the Holocene. In a new &lt;a href=&#34;http://onlinelibrary.wiley.com/doi/10.1002/2017JC013126/abstract&#34;&gt;study&lt;/a&gt;, published in the Journal of Geophysical Research: Oceans, scientists at the University of Oxford in England studied more than 900 pieces of driftwood collected from Arctic shorelines since the 1950s to investigate how shifting Arctic Ocean currents help melt or fortify sea ice.&lt;/p&gt;</description>
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				<title>Ancient wildfires suggest rising atmospheric oxygen helped end past ocean anoxia</title>
				<link>https://www.earthmagazine.org/article/ancient-wildfires-suggest-rising-atmospheric-oxygen-helped-end-past-ocean-anoxia/</link>
				<pubDate>Thu, 17 Aug 2017 17:15:07 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/ancient-wildfires-suggest-rising-atmospheric-oxygen-helped-end-past-ocean-anoxia/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/ancient-wildfires-suggest-rising-atmospheric-oxygen-helped-end-past-ocean-anoxia/PrescribedFire_JaxStrong_CCBY2.jpg&#34; alt=&#34;Rising atmospheric oxygen levels may have spurred wildfire activity and helped bring an end to a bout of ocean anoxia about 180 million years ago. Credit: Chuck Hanlon, South Florida Water Management District, CC BY 2.0&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Rising atmospheric oxygen levels may have spurred wildfire activity and helped bring an end to a bout of ocean anoxia about 180 million years ago. Credit: Chuck Hanlon, South Florida Water Management District, CC BY 2.0&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Many times throughout Earth&amp;rsquo;s history, oxygen levels in the world&amp;rsquo;s oceans have decreased dramatically in episodes called oceanic anoxic events (OAEs), which have caused massive marine die-offs. In the Early Jurassic, for example, the Toarcian OAE has been linked with the extinction of many ammonite species and other sea life. However, how such episodes end remains largely unclear to scientists.&lt;/p&gt;</description>
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				<title>A new — and more toxic — normal? Harmful algal blooms find new habitats in changing oceans</title>
				<link>https://www.earthmagazine.org/article/new-and-more-toxic-normal-harmful-algal-blooms-find-new-habitats-changing-oceans/</link>
				<pubDate>Fri, 13 Jan 2017 13:06:09 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/new-and-more-toxic-normal-harmful-algal-blooms-find-new-habitats-changing-oceans/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/new-and-more-toxic-normal-harmful-algal-blooms-find-new-habitats-changing-oceans/2__A_southern_summer_bloom.jpg&#34; alt=&#34;An Envisat image of a phytoplankton bloom in the South Atlantic Ocean east of the Falkland Islands on Dec. 2, 2011. Chlorophyll pigment detected by ocean-color sensors on Earth-observing satellites can help identify species in algal blooms and their toxicity. Credit: ESA.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;An Envisat image of a phytoplankton bloom in the South Atlantic Ocean east of the Falkland Islands on Dec. 2, 2011. Chlorophyll pigment detected by ocean-color sensors on Earth-observing satellites can help identify species in algal blooms and their toxicity. Credit: ESA.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;In May 2015, a seizure-wracked sea lion hauled itself ashore on a beach in southern Washington. Testing confirmed it was suffering from domoic acid poisoning, an illness that causes disorientation, seizures and sometimes death that stems from the consumption of fish or shellfish contaminated by a toxic species of algae called &lt;em&gt;Pseudo-nitzschia&lt;/em&gt;. To the south, in warm California waters where localized toxic blooms of &lt;em&gt;Pseudo-nitzschia&lt;/em&gt; are a near-annual occurrence, sea lion illnesses caused by exposure to domoic acid are common — however, this was a first in Washington. The sick sea lion was euthanized, but its stranding in Washington alerted coastal communities to the massive algae bloom that was engulfing coastal waters from Santa Barbara, Calif., all the way to British Columbia.&lt;/p&gt;</description>
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				<title>Pluto may still have liquid ocean</title>
				<link>https://www.earthmagazine.org/article/pluto-may-still-have-liquid-ocean/</link>
				<pubDate>Wed, 19 Oct 2016 16:29:01 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/pluto-may-still-have-liquid-ocean/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/pluto-may-still-have-liquid-ocean/118140_web.jpg&#34; alt=&#34;Deep fractures revealing tectonic activity suggests that Pluto may have a liquid ocean. Credit: Credit: NASA/JHUAPL/SwRI.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Deep fractures revealing tectonic activity suggests that Pluto may have a liquid ocean. Credit: Credit: NASA/JHUAPL/SwRI.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Last year, images from NASA&amp;rsquo;s New Horizons flyby of Pluto revealed geologic activity that suggested a liquid ocean may have once lurked beneath the dwarf planet&amp;rsquo;s icy crust. But whether it still exists in that state, or had frozen, remained a question. According to a new &lt;a href=&#34;http://onlinelibrary.wiley.com/doi/10.1002/2016GL069220/full&#34;&gt;study&lt;/a&gt; published in Geophysical Research Letters, it may still be partially liquid.&lt;/p&gt;</description>
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				<title>Tiny ocean bacteria could play big role in climate</title>
				<link>https://www.earthmagazine.org/article/tiny-ocean-bacteria-could-play-big-role-climate/</link>
				<pubDate>Tue, 16 Aug 2016 16:36:11 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/tiny-ocean-bacteria-could-play-big-role-climate/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/tiny-ocean-bacteria-could-play-big-role-climate/Credit__Ben_Temperton.jpg&#34; alt=&#34;Stephen Giovannoni&amp;#39;s team samples for Pelagibacterales off Bermuda. Credit: Ben Temperton.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Stephen Giovannoni&amp;#39;s team samples for Pelagibacterales off Bermuda. Credit: Ben Temperton.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;In the 1990s, researchers identified the most abundant group of organisms in the ocean as Pelagibacterales, a class of free-living bacteria that live in surface waters as a microscopic but major part of the phytoplankton community. Now, a new &lt;a href=&#34;http://www.nature.com/articles/nmicrobiol201665&#34;&gt;study&lt;/a&gt; suggests that Pelagibacterales could play an important role in the global climate cycle by producing dimethylsulfide (DMS), an organosulfur compound that stimulates cloud formation when it gets into the atmosphere.&lt;/p&gt;</description>
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				<title>Drilling for gold inside a submarine volcano</title>
				<link>https://www.earthmagazine.org/article/drilling-gold-inside-submarine-volcano/</link>
				<pubDate>Thu, 14 Jul 2016 15:12:35 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/drilling-gold-inside-submarine-volcano/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/drilling-gold-inside-submarine-volcano/Joides_0.jpg&#34; alt=&#34;In 2018, researchers aboard International Ocean Discovery Program&amp;#39;s JOIDES Resolution ship will drill into an active submarine volcano — Brothers Volcano, part of the Kermadec Arc north of New Zealand — for the first time. Credit: William Crawford, IODP JRSO/TAMU&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;In 2018, researchers aboard International Ocean Discovery Program&amp;#39;s JOIDES Resolution ship will drill into an active submarine volcano — Brothers Volcano, part of the Kermadec Arc north of New Zealand — for the first time. Credit: William Crawford, IODP JRSO/TAMU&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Earth scientists have been given the green light to drill into an active submarine volcano for the first time, with the hope of discovering substantial new reserves of valuable metals, as well as new forms of extreme life.&lt;/p&gt;</description>
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				<title>Benchmarks: March 1961: Project Mohole undertakes the first deep-ocean drilling</title>
				<link>https://www.earthmagazine.org/article/benchmarks-march-1961-project-mohole-undertakes-first-deep-ocean-drilling/</link>
				<pubDate>Wed, 06 Jul 2016 13:15:34 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/benchmarks-march-1961-project-mohole-undertakes-first-deep-ocean-drilling/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/benchmarks-march-1961-project-mohole-undertakes-first-deep-ocean-drilling/5574190251_9a2cdebcf0_o.jpg&#34; alt=&#34;Early near-shore trials of the CUSS I drillship occurred off La Jolla, Calif., where the writer John Steinbeck noted that the barge, with its drilling derrick rising amidship, had the &amp;#34;sleek race lines of an outhouse standing on a garbage scow.&amp;#34; Credit: Willard Bascom, National Academy of Sciences.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Early near-shore trials of the CUSS I drillship occurred off La Jolla, Calif., where the writer John Steinbeck noted that the barge, with its drilling derrick rising amidship, had the &amp;#34;sleek race lines of an outhouse standing on a garbage scow.&amp;#34; Credit: Willard Bascom, National Academy of Sciences.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Since its inception in the 1960s, the ocean drilling program — an international research program that explores the world&amp;rsquo;s ocean basins — has logged hundreds of thousands of hours of ship time traveling the world&amp;rsquo;s oceans, drilling boreholes and retrieving cores of sediment and rock that have revealed Earth&amp;rsquo;s deep history and structure.&lt;/p&gt;</description>
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				<title>Benchmarks: January 23, 1960: Humans reach the deepest point on Earth</title>
				<link>https://www.earthmagazine.org/article/benchmarks-january-23-1960-humans-reach-deepest-point-earth/</link>
				<pubDate>Mon, 20 Jun 2016 14:40:15 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/benchmarks-january-23-1960-humans-reach-deepest-point-earth/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/benchmarks-january-23-1960-humans-reach-deepest-point-earth/Bathyscaphe_Trieste_Piccard-Walsh.jpg&#34; alt=&#34;Jacques Piccard and Don Walsh in the crew cabin as the Trieste descends to Challenger Deep. Credit: NOAA.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Jacques Piccard and Don Walsh in the crew cabin as the Trieste descends to Challenger Deep. Credit: NOAA.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;More than 9,000 meters underwater, a window buckles, sending a spider web of cracks across the glass. The entire submersible shakes, but no water rushes into the Trieste. Out of vocal contact with the main ship on the surface above them, Swiss oceanographer and engineer Jacques Piccard and U.S. Navy Lt. Don Walsh decide to continue their descent despite the new danger. After all, at more than nine kilometers below the sea surface, the explorers were too close to their goal to turn around. They were only 2,000 meters away from the deepest spot on Earth: Challenger Deep. On Jan. 23, 1960, they reached that fabled point 10,916 meters below the surface of the Pacific Ocean.&lt;/p&gt;</description>
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				<title>The softer side of hydrothermal vents</title>
				<link>https://www.earthmagazine.org/article/softer-side-hydrothermal-vents/</link>
				<pubDate>Tue, 19 Apr 2016 15:34:36 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/softer-side-hydrothermal-vents/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/softer-side-hydrothermal-vents/VDVF_Credit_NOCS.jpg&#34; alt=&#34;A 3-meter-tall talc spire tops the main hydrothermal vent in the Von Damm Vent Field. Credit: National Oceanography Center Southampton.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;A 3-meter-tall talc spire tops the main hydrothermal vent in the Von Damm Vent Field. Credit: National Oceanography Center Southampton.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Seafloor chimneys belching dark plumes of superheated, acidic fluids into the ocean, called &amp;ldquo;black smokers,&amp;rdquo; are the most common kind of submarine hydrothermal vent known. But recently scientists discovered a vent system, of a seemingly gentler nature, unlike any observed before.&lt;/p&gt;</description>
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				<title>North Sea uplift caused Jurassic cooling event</title>
				<link>https://www.earthmagazine.org/article/north-sea-uplift-caused-jurassic-cooling-event/</link>
				<pubDate>Wed, 30 Mar 2016 19:02:35 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/north-sea-uplift-caused-jurassic-cooling-event/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/north-sea-uplift-caused-jurassic-cooling-event/ncomms10015-f1_kc_0.jpg&#34; alt=&#34;The Laurasian Seaway (a) connected the Boreal Sea to the Tethys Ocean to the south during the Jurassic. Uplift of the North Sea Dome (b) beginning in the Early Jurassic might have blocked the northward flow of warm Tethyan waters through the seaway, causing an abrupt cooling event about 174 million years ago. Credit: Korte et al., Nature Communications, December 2015, CC BY 4.0.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;The Laurasian Seaway (a) connected the Boreal Sea to the Tethys Ocean to the south during the Jurassic. Uplift of the North Sea Dome (b) beginning in the Early Jurassic might have blocked the northward flow of warm Tethyan waters through the seaway, causing an abrupt cooling event about 174 million years ago. Credit: Korte et al., Nature Communications, December 2015, CC BY 4.0.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;The climate of the Jurassic, long envisioned as ubiquitously warm from the equator to the poles, was actually more dynamic, sometimes cooling dramatically, according to a new &lt;a href=&#34;http://www.nature.com/ncomms/2015/151211/ncomms10015/full/ncomms10015.html&#34;&gt;study&lt;/a&gt;. The research joined isotopic and sedimentological data to suggest that an abrupt cooling event occurred in the midlatitudes early in the Middle Jurassic as a result of changing ocean currents associated with a feature known as the North Sea Dome.&lt;/p&gt;</description>
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				<title>No laughing matter: Ocean nitrous oxide emissions greater than thought</title>
				<link>https://www.earthmagazine.org/article/no-laughing-matter-ocean-nitrous-oxide-emissions-greater-thought/</link>
				<pubDate>Thu, 12 Nov 2015 08:46:09 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/no-laughing-matter-ocean-nitrous-oxide-emissions-greater-thought/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/no-laughing-matter-ocean-nitrous-oxide-emissions-greater-thought/shutterstock_181535864_MancoraPeru_SvenSchermer.jpg&#34; alt=&#34;High productivity ecosystems like the upwelling zone off the coast of Peru, which once supported an abundant anchovy fishery before overfishing collapsed it in the 1970s and ‘80s, also create oxygen minimum zones where high fluxes of nitrous oxide are produced. Credit: ©Shutterstock.com/Sven Schermer.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;High productivity ecosystems like the upwelling zone off the coast of Peru, which once supported an abundant anchovy fishery before overfishing collapsed it in the 1970s and ‘80s, also create oxygen minimum zones where high fluxes of nitrous oxide are produced. Credit: ©Shutterstock.com/Sven Schermer.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Nitrous oxide is a potent greenhouse gas and, since the banning of chlorofluorocarbons in 1987, it has become the main driver of ozone loss from the stratosphere. Most atmospheric nitrous oxide is emitted from agricultural land and soils, but roughly a third is thought to come from the ocean. However, marine sources and sinks of the gas are not well understood.&lt;/p&gt;</description>
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				<title>Enceladus&#39; extremely alkaline underground ocean</title>
				<link>https://www.earthmagazine.org/article/enceladus-extremely-alkaline-underground-ocean/</link>
				<pubDate>Mon, 02 Nov 2015 11:58:47 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/enceladus-extremely-alkaline-underground-ocean/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/enceladus-extremely-alkaline-underground-ocean/Enceladus_credit_NASA_JPL-Caltech.jpg&#34; alt=&#34;A diagram illustrating the possible interior of Saturn&amp;#39;s moon Enceladus, including the ocean and plumes in the south polar region. Credit: NASA/JPL-Caltech.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;A diagram illustrating the possible interior of Saturn&amp;#39;s moon Enceladus, including the ocean and plumes in the south polar region. Credit: NASA/JPL-Caltech.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Saturn&amp;rsquo;s moon Enceladus is home to a vast underground ocean that erupts to the surface at the moon&amp;rsquo;s south pole in a giant plume of gas, ice and dust. Scientists studying observational data of this plume collected by the Cassini spacecraft, which has been orbiting Saturn since 2004, have recently learned more about the chemistry of Enceladus&amp;rsquo; hidden ocean.&lt;/p&gt;</description>
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				<title>Ancient asteroids boiled Earth&#39;s oceans</title>
				<link>https://www.earthmagazine.org/article/ancient-asteroids-boiled-earths-oceans/</link>
				<pubDate>Mon, 21 Sep 2015 11:28:06 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/ancient-asteroids-boiled-earths-oceans/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/ancient-asteroids-boiled-earths-oceans/LoweByerly.jpg&#34; alt=&#34;Donald Lowe and Gary Byerly examine Archean rocks that preserve evidence of impacts in South Africa. Credit: Donald Lowe.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Donald Lowe and Gary Byerly examine Archean rocks that preserve evidence of impacts in South Africa. Credit: Donald Lowe.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;The asteroid that wiped out the remaining dinosaurs — save for the avian variety — 66 million years ago was roughly 10 kilometers wide. Long before that, however, early Earth was bombarded by many larger impactors, which pulverized Earth&amp;rsquo;s surface time and again. Now, a new &lt;a href=&#34;http://geology.gsapubs.org/content/early/2015/05/07/G36665.1.abstract&#34;&gt;study published in Geology&lt;/a&gt; suggests that two asteroids, dating to Archean times and estimated to be 50 to 100 kilometers in diameter, released enough energy to boil the oceans and reduce sea level by as much as 100 meters or more.&lt;/p&gt;</description>
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				<title>Southbound icebergs off the hook for ice-age cooling</title>
				<link>https://www.earthmagazine.org/article/southbound-icebergs-hook-ice-age-cooling/</link>
				<pubDate>Fri, 17 Jul 2015 09:27:00 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/southbound-icebergs-hook-ice-age-cooling/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/southbound-icebergs-hook-ice-age-cooling/Iceberg_kaet44.jpg&#34; alt=&#34;A new study suggests that southbound icebergs probably arrived too late to be the trigger for Pleistocene cooling events in the North Atlantic. Credit: ©kaet44, CC BY 2.0.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;A new study suggests that southbound icebergs probably arrived too late to be the trigger for Pleistocene cooling events in the North Atlantic. Credit: ©kaet44, CC BY 2.0.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;During the Late Pleistocene, changes in North Atlantic Ocean circulation triggered abrupt changes in global climate: In some locations in the Northern Hemisphere, average temperatures dropped by as much as 10 degrees Celsius within a few decades. Scientists have long thought that freshwater from melting icebergs traveling south from the Arctic may have instigated the circulation shifts that contributed to cooling feedback loops. But now, scientists looking at seafloor sediments collected near Iceland have found that pulses of icebergs typically arrived after the onset of cooling episodes, too late to be primary drivers of climate change.&lt;/p&gt;</description>
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				<title>A pair of moons with underground oceans</title>
				<link>https://www.earthmagazine.org/article/pair-moons-underground-oceans/</link>
				<pubDate>Mon, 06 Jul 2015 13:34:09 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/pair-moons-underground-oceans/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/pair-moons-underground-oceans/Credit__NASA_JPL-Caltech_promo.jpg&#34; alt=&#34;Interactions between deep ocean water and hot rock on Saturn&amp;#39;s moon Enceladus are thought to result in hydrothermal plumes that erupt through the moon&amp;#39;s icy crust. Credit: NASA/JPL-Caltech.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Interactions between deep ocean water and hot rock on Saturn&amp;#39;s moon Enceladus are thought to result in hydrothermal plumes that erupt through the moon&amp;#39;s icy crust. Credit: NASA/JPL-Caltech.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Jupiter and Saturn are both gas giants boasting multiple moons. Now, two separate studies have identified another similarity: Each appears to have a moon with hidden underground oceans.&lt;/p&gt;</description>
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				<title>Some coral reefs bounce back after bleaching</title>
				<link>https://www.earthmagazine.org/article/some-coral-reefs-bounce-back-after-bleaching/</link>
				<pubDate>Wed, 08 Apr 2015 15:34:56 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/some-coral-reefs-bounce-back-after-bleaching/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/some-coral-reefs-bounce-back-after-bleaching/IMG_1587_smaller.jpg&#34; alt=&#34;This recovering coral reef in the Seychelles is dominated by structurally complex Acropora and Porites corals, which provide shelter for fish and other organisms. Credit: Nicholas Graham&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;This recovering coral reef in the Seychelles is dominated by structurally complex Acropora and Porites corals, which provide shelter for fish and other organisms. Credit: Nicholas Graham&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Ocean temperatures that rise too much or for too long can harm coral reefs, sometimes causing mass die-offs that leave reefs nearly barren of live corals. But scientists don&amp;rsquo;t know if or under what conditions reefs — which provide habitat for a wide array of marine species, as well as food for millions of people around the world — can recover from such catastrophes, in part because of a lack of long-term studies tracking damaged reefs. Now, a new study suggests that, given time and the right conditions, even once-decimated reefs can recoup their losses.&lt;/p&gt;</description>
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				<title>Did three convicts survive their escape from Alcatraz? Modern modeling adds to a decades-old mystery</title>
				<link>https://www.earthmagazine.org/article/did-three-convicts-survive-their-escape-alcatraz-modern-modeling-adds-decades-old-mystery/</link>
				<pubDate>Wed, 14 Jan 2015 10:11:00 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/did-three-convicts-survive-their-escape-alcatraz-modern-modeling-adds-decades-old-mystery/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/did-three-convicts-survive-their-escape-alcatraz-modern-modeling-adds-decades-old-mystery/Alcatraz11.JPEG&#34; alt=&#34;The former Alcatraz Federal Penitentiary on Alcatraz Island in San Francisco Bay. Credit: Jon Sullivan, public domain&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;The former Alcatraz Federal Penitentiary on Alcatraz Island in San Francisco Bay. Credit: Jon Sullivan, public domain&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Twenty-first century science is shedding new light on a 53-year-old mystery involving one of the country&amp;rsquo;s most notorious prisons: Did three convicted bank robbers survive their escape attempt from Alcatraz Island? &lt;a href=&#34;http://www.dutchwatersector.com/news-events/news/12586-agu-fall-meeting-2014-high-performance-3di-hydraulic-software-visualizes-route-of-legendary-alcatraz-escape.html&#34;&gt;New results&lt;/a&gt;, presented at the &lt;a href=&#34;http://fallmeeting.agu.org/2014/&#34;&gt;American Geophysical Union&amp;rsquo;s (AGU) annual meeting&lt;/a&gt; in San Francisco last December, suggest there&amp;rsquo;s a chance they did.&lt;/p&gt;</description>
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				<title>Pliocene tropical oceans were warmer after all</title>
				<link>https://www.earthmagazine.org/article/pliocene-tropical-oceans-were-warmer-after-all/</link>
				<pubDate>Tue, 04 Nov 2014 10:08:07 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/pliocene-tropical-oceans-were-warmer-after-all/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/pliocene-tropical-oceans-were-warmer-after-all/shutterstock_71518945_sea_beach_wave_holbox.jpg&#34; alt=&#34;Credit: ©Shutterstock.com/holbox.&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Credit: ©Shutterstock.com/holbox.&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Scientists may have overturned the idea that Earth&amp;rsquo;s tropical oceans were the same temperature during the Early to Middle Pliocene — between about 5 million and 3 million years ago — as they are today, despite the world being a far warmer place then.&lt;/p&gt;</description>
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				<title>Bare Earth Elements: Search the seafloor firsthand (and live!)</title>
				<link>https://www.earthmagazine.org/article/bare-earth-elements-search-seafloor-firsthand-and-live/</link>
				<pubDate>Thu, 25 Sep 2014 11:38:35 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/bare-earth-elements-search-seafloor-firsthand-and-live/</guid>
				<description>&lt;p&gt;If you&amp;rsquo;ve ever wanted to take a dive into the ocean depths and explore the seafloor below the waves, but just haven&amp;rsquo;t had the time (or financing) to build your own deep-sea submersible, here&amp;rsquo;s another solution. &lt;a href=&#34;http://www.noaa.gov&#34;&gt;NOAA&lt;/a&gt;&amp;rsquo;s 68-meter &lt;a href=&#34;http://www.moc.noaa.gov/oe/&#34;&gt;Okeanos Explorer&lt;/a&gt; — the only federally funded ship dedicated to &amp;ldquo;solely to exploration&amp;rdquo; — is currently trolling the Atlantic Ocean on the three-week third leg of a mission dubbed &lt;a href=&#34;http://oceanexplorer.noaa.gov/okeanos/explorations/ex1404/welcome.html&#34;&gt;&amp;ldquo;Our Deepwater Backyard: Exploring Atlantic Canyons and Seamounts 2014,&amp;quot;&lt;/a&gt; and it&amp;rsquo;s offering to take guests along for part of the ride.&lt;/p&gt;</description>
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				<title>XPRIZE offers new ocean health awards</title>
				<link>https://www.earthmagazine.org/article/xprize-offers-new-ocean-health-awards/</link>
				<pubDate>Tue, 29 Oct 2013 18:45:35 -0400</pubDate>
				<guid>https://www.earthmagazine.org/article/xprize-offers-new-ocean-health-awards/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/xprize-offers-new-ocean-health-awards/Coral_Reef.jpg&#34; alt=&#34;The newest XPRIZE will be awarded for studying ocean acidification. Jerry Reid, U.S. Fish and Wildlife Service&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;The newest XPRIZE will be awarded for studying ocean acidification. Jerry Reid, U.S. Fish and Wildlife Service&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;&lt;a href=&#34;http://www.xprize.org/&#34;&gt;XPRIZE&lt;/a&gt;, the organization that used competition&#xA;to propel the development of private space travel and super-efficient&#xA;vehicles, is now making a commitment to improving ocean health.&lt;/p&gt;</description>
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				<title>Tracking plastic in the oceans</title>
				<link>https://www.earthmagazine.org/article/tracking-plastic-oceans/</link>
				<pubDate>Tue, 24 Jan 2012 07:34:25 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/tracking-plastic-oceans/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.earthmagazine.org/archive/tracking-plastic-oceans/siocomm_A_SEAPLEX-09-336_hu_2759fc9bc3cc4e61.webp&#34; srcset=&#34;https://www.earthmagazine.org/archive/tracking-plastic-oceans/siocomm_A_SEAPLEX-09-336_hu_592f79d050bf0b41.webp 480w, https://www.earthmagazine.org/archive/tracking-plastic-oceans/siocomm_A_SEAPLEX-09-336_hu_2759fc9bc3cc4e61.webp 600w&#34; sizes=&#34;(min-width: 992px) 760px, 100vw&#34; width=&#34;600&#34; height=&#34;902&#34; alt=&#34;Researchers found this net and other debris floating in the Great Pacific Garbage Patch. ©Scripps Institution of Oceanography&#34; loading=&#34;eager&#34; decoding=&#34;async&#34; fetchpriority=&#34;high&#34;&gt;&#xA;&#xA;&#xA;&lt;figcaption&gt;Researchers found this net and other debris floating in the Great Pacific Garbage Patch. ©Scripps Institution of Oceanography&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/tracking-plastic-oceans/siocomm_A_SEAPLEX-09-307.jpg&#34; alt=&#34;The garbage patches floating in the oceans are not solid, giant floating islands of trash. In fact, most of the plasticsx are tiny fragments called microplastics. ©Scripps Institution of Oceanography&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;The garbage patches floating in the oceans are not solid, giant floating islands of trash. In fact, most of the plasticsx are tiny fragments called microplastics. ©Scripps Institution of Oceanography&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/tracking-plastic-oceans/siocomm_R_SEAPLEX-09-459.jpg&#34; alt=&#34;Plastic can affect everything from tiny invertebrates to fish to large marine mammals. ©Scripps Institution of Oceanography&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Plastic can affect everything from tiny invertebrates to fish to large marine mammals. ©Scripps Institution of Oceanography&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Despite worldwide efforts to curtail plastic use &amp;mdash; to ban plastic&#xA;grocery bags, to switch to reusable water bottles instead of disposable&#xA;plastic bottles, and to get rid of the microplastics in cosmetics, for&#xA;example &amp;mdash; we still produce more than 260 million tons of plastic each&#xA;year. Almost a third of that plastic goes into disposable, one-time-use&#xA;items. Only about 1 percent of it is recycled globally, so much ends up&#xA;in landfills. Worse still, some of the plastic winds up in the world&amp;rsquo;s&#xA;oceans.&lt;/p&gt;</description>
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				<title>Blogging on EARTH: First dispatches from EGU</title>
				<link>https://www.earthmagazine.org/article/blogging-earth-first-dispatches-egu/</link>
				<pubDate>Thu, 05 Jan 2012 06:41:58 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/blogging-earth-first-dispatches-egu/</guid>
				<description>&lt;p&gt;EARTH&amp;rsquo;s Carolyn Gramling is taking in the &lt;a href=&#34;http://www.egu.eu/home/egu-general-assembly-2011-at-a-glance.html&#34;&gt;European Geophysical Union&#xA;meeting&lt;/a&gt;&#xA;this week in Vienna, Austria. Here are some of the sessions that have&#xA;caught her interest so far.&lt;/p&gt;&#xA;&lt;h3 id=&#34;how-many-thunderstorms-are-there-around-the-world-at-any-point-in-time&#34;&gt;How many thunderstorms are there around the world at any point in time?&lt;/h3&gt;&#xA;&lt;p&gt;About a century ago, scientists thought that number was about 2,000,&#xA;based on an estimated number of lightning flashes per second (back then,&#xA;thought to be about 100). Nowadays, of course, we have much better&#xA;estimates of lightning flashes &amp;mdash; satellite observations suggest there&#xA;are actually only 45 flashes per second.&lt;/p&gt;</description>
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				<title>Natural dust may be harmful to ocean organisms</title>
				<link>https://www.earthmagazine.org/article/natural-dust-may-be-harmful-ocean-organisms/</link>
				<pubDate>Thu, 05 Jan 2012 06:41:58 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/natural-dust-may-be-harmful-ocean-organisms/</guid>
				<description>&lt;p&gt;Although human-made aerosols sometimes are toxic, natural aerosols from&#xA;deserts and volcanoes are important contributors to ocean fertilization.&#xA;Now, new research suggests that natural aerosols have their downside too&#xA;&amp;mdash; and the impact of natural aerosols on ocean organisms could&#xA;influence predictions of future climate change.&lt;/p&gt;</description>
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				<title>Of sounds and cetaceans: Quieting a noisy underwater world</title>
				<link>https://www.earthmagazine.org/article/sounds-and-cetaceans-quieting-noisy-underwater-world/</link>
				<pubDate>Thu, 05 Jan 2012 06:41:58 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/sounds-and-cetaceans-quieting-noisy-underwater-world/</guid>
				<description>&lt;p&gt;Marine mammals live in a world of sound. In the open ocean, whales and&#xA;dolphins depend on sound waves, using echolocation to navigate, find&#xA;food, attract mates and communicate. But their clicks and calls are not&#xA;the only noises underwater: Oil and gas exploration, seafloor mapping,&#xA;and ship and submarine navigation have increased dramatically over the&#xA;past few decades, making the world&amp;rsquo;s oceans noisier than ever.&lt;/p&gt;</description>
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				<title>Sea sprawl: Into the blue frontier of ocean development</title>
				<link>https://www.earthmagazine.org/article/sea-sprawl-blue-frontier-ocean-development/</link>
				<pubDate>Thu, 05 Jan 2012 06:41:58 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/sea-sprawl-blue-frontier-ocean-development/</guid>
				<description>&lt;p&gt;&lt;strong&gt;Picture it:&lt;/strong&gt; Dozens of kilometers off the coast of Texas, a giant&#xA;polygon-shaped cage constructed of steel ribs and mesh netting floats 30&#xA;or so meters beneath the waves. The cage, moored to the seafloor, is&#xA;filled with tens of thousands of teeming, silvery fish. Several&#xA;kilometers away, offshore wind turbines sprout from the sea surface in a&#xA;curving line, their spindly white arms churning the atmosphere. Still&#xA;farther along the horizon, a massive oil platform squats heavily on four&#xA;stumpy legs over its parcel of ocean, pipes plunging 11 kilometers into&#xA;deep reservoirs within the seafloor. In the open waters between these&#xA;industries, tankers and commercial fishermen follow snaking shipping&#xA;lanes that lead them toward the coast.&lt;/p&gt;</description>
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				<title>Shell-shocked: How different creatures deal with an acidifying ocean</title>
				<link>https://www.earthmagazine.org/article/shell-shocked-how-different-creatures-deal-acidifying-ocean/</link>
				<pubDate>Thu, 05 Jan 2012 06:41:58 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/shell-shocked-how-different-creatures-deal-acidifying-ocean/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-389-7da-3-a.jpg&#34; alt=&#34;Ries and one of his students collect specimens. Justin B. Ries&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Ries and one of his students collect specimens. Justin B. Ries&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-382-7da-3-a.jpg&#34; alt=&#34;An aragonite conch shell reared under current atmospheric carbon dioxide levels (400 ppm) appears normal, but... Justin B. Ries&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;An aragonite conch shell reared under current atmospheric carbon dioxide levels (400 ppm) appears normal, but... Justin B. Ries&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-383-7da-3-a.jpg&#34; alt=&#34;...when reared under elevated (2,850 ppm) levels, it shows clear signs of dissolution, especially at the upper lip of the shell. Justin B. Ries&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;...when reared under elevated (2,850 ppm) levels, it shows clear signs of dissolution, especially at the upper lip of the shell. Justin B. Ries&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-384-7da-3-a.jpg&#34; alt=&#34;An aragonite quahog shell reared at current (400 ppm) atmospheric carbon dioxide levels shows well-formed ridges. Justin B. Ries&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;An aragonite quahog shell reared at current (400 ppm) atmospheric carbon dioxide levels shows well-formed ridges. Justin B. Ries&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-385-7da-3-a.jpg&#34; alt=&#34;Under elevated (2,850 ppm) carbon dioxide, however, the ridges on the shell are nearly dissolved away. Justin B. Ries&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Under elevated (2,850 ppm) carbon dioxide, however, the ridges on the shell are nearly dissolved away. Justin B. Ries&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-386-7da-3-a.jpg&#34; alt=&#34;A tropical pencil urchin (high-magnesium calcite shell) reared under current (400 ppm) atmospheric carbon dioxide conditions still has well-formed spines. Justin B. Ries&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;A tropical pencil urchin (high-magnesium calcite shell) reared under current (400 ppm) atmospheric carbon dioxide conditions still has well-formed spines. Justin B. Ries&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-387-7da-3-a.jpg&#34; alt=&#34;When reared at elevated (2,850 ppm) carbon dioxide, however, another urchin&amp;#39;s spines are nearly dissolved away. Justin B. Ries&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;When reared at elevated (2,850 ppm) carbon dioxide, however, another urchin&amp;#39;s spines are nearly dissolved away. Justin B. Ries&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-380-7da-3-a.jpg&#34; alt=&#34;Justin Ries look at 18 species of marine calcifiers, including crustaceans, corals, bivalves, gastropods, coralline algae and urchins. Justin B. Ries&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Justin Ries look at 18 species of marine calcifiers, including crustaceans, corals, bivalves, gastropods, coralline algae and urchins. Justin B. Ries&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&#xA;&#xA;&#xA;&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/shell-shocked-how-different-creatures-deal-acidifying-ocean/i-381-7da-3-a.jpg&#34; alt=&#34;Staghorn corals, such as these off of Belize, are more vulnerable to ocean acidification because they build their shells from aragonite, not calcite. Castillo, UNC-Chapel Hill&#34; loading=&#34;lazy&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;Staghorn corals, such as these off of Belize, are more vulnerable to ocean acidification because they build their shells from aragonite, not calcite. Castillo, UNC-Chapel Hill&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;To survive in the ocean, soft-bodied organisms must possess one of five&#xA;traits: big teeth, toxic flesh, invisibility, quickness or a hard shell.&#xA;Most marine organisms that employ the latter, called calcifiers, build&#xA;their hard shells from the mineral calcium carbonate. However,&#xA;increasing atmospheric carbon dioxide levels are making the oceans more&#xA;acidic &amp;mdash; which, in turn, is reducing the concentration of carbonate&#xA;ions dissolved in seawater that organisms use to build their protective&#xA;shells and skeletons. Calcifying marine organisms &amp;mdash; such as clams,&#xA;crabs, corals and conchs &amp;mdash; may soon find themselves short on building&#xA;material.&lt;/p&gt;</description>
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				<title>Voyage to the plastic vortex</title>
				<link>https://www.earthmagazine.org/article/voyage-plastic-vortex/</link>
				<pubDate>Thu, 05 Jan 2012 06:41:58 -0500</pubDate>
				<guid>https://www.earthmagazine.org/article/voyage-plastic-vortex/</guid>
				<description>&lt;figure class=&#34;earth-figure&#34;&gt;&#xA;&#xA;&#xA;&lt;img src=&#34;https://www.americangeosciences.org/static/earth/voyage-plastic-vortex/i-26e-7d9-9-3.jpg&#34; alt=&#34;SEAPLEX researchers examine a stuffed toy dog after it was collected along with ghost net debris on Aug. 15, 2009. 2009 Scripps Institution of Oceanography Photo credit: J. Leichter&#34; loading=&#34;eager&#34; decoding=&#34;async&#34;&gt;&#xA;&#xA;&lt;figcaption&gt;SEAPLEX researchers examine a stuffed toy dog after it was collected along with ghost net debris on Aug. 15, 2009. 2009 Scripps Institution of Oceanography Photo credit: J. Leichter&lt;/figcaption&gt;&#xA;&lt;/figure&gt;&#xA;&#xA;&lt;p&gt;Out in the middle of the northern Pacific Ocean, a giant floating mess&#xA;of plastic debris is drifting and bobbing among the waves. Scientists&#xA;call this expanse of litter, which stretches for hundreds of kilometers&#xA;across open sea, the Great Pacific Garbage Patch. But before last&#xA;summer, there was little information about how large the patch really&#xA;is, what types of debris are out there and what kind of impact it is&#xA;having on ocean life.&lt;/p&gt;</description>
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