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            "id": 10358,
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            "release_date": "2009-01-15T00:00:00-05:00",
            "title": "Geochemical Creation of Methane",
            "description": "Conceptual animation depicting how geochemical processes during the course of Mars' history may have produced the methane plumes now seen in Mars' atmosphere. Here, through a process called serpentinization, methane is generated as part of a reaction involving the conversion of liquid water (seen seeping into the planet's crust), iron oxide, and carbon dioxide energized by the planet's internal heat into serpentine minerals. || methane_geo_mpgLG00377_print.jpg (1024x576) [85.2 KB] || methane_geo_mpgLG_web.png (320x180) [184.0 KB] || methane_geo_mpgLG_thm.png (80x40) [16.0 KB] || methane_geo_h264fullres.webmhd.webm (960x540) [3.0 MB] || methane_geo_h264fullres.mov (1280x720) [12.3 MB] || methane_geo_prores.mov (1280x720) [535.3 MB] || methane_geo_YouTube.mov (1280x720) [5.8 MB] || methane_geo_ipodLG.m4v (640x360) [3.5 MB] || methane_geo_mpgLG.mpg (640x360) [4.7 MB] || methane_geo_ipodSM.m4v (320x180) [1.5 MB] || methane_geo_mp4SM.mp4 (320x240) [665.5 KB] || methane_geo_mpgSM.mpg (512x288) [3.1 MB] || ",
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