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    "results": [
        {
            "id": 20006,
            "url": "https://svs.gsfc.nasa.gov/20006/",
            "result_type": "Animation",
            "release_date": "2003-11-05T12:00:00-05:00",
            "title": "Carbon Cycle",
            "description": "The Carbon  Cycle - The carbon cycle on land, acted out here show a tree  taking in carbon dioxide from the atmosphere, and combined with water  and nutrients from the soil, growing. In the fall and winter, parts  of the growth die off and release some carbon back into the system.  At some point, the tree is no longer able to take in carbon and  begins to die. When that happens, all the carbon absorbed in its body  is released back into the cycle as it decomposes. Fire can accelerate  this, sending plumes of carbon-laden aerosols into the atmosphere, as  well as leaving carbon-rich ash deposits on the ground for further  decomposition and recycling. || ",
            "hits": 48
        },
        {
            "id": 20007,
            "url": "https://svs.gsfc.nasa.gov/20007/",
            "result_type": "Animation",
            "release_date": "2003-11-05T12:00:00-05:00",
            "title": "Carbon Cycle",
            "description": "Carbon And The Ocean — The Slow Cycle - The oceans are vast, and their processes as complex as their waters are deep.Phytoplankton absorbs carbon dioxide from the atmosphere and nutrient rich waters and grows in wide colonies called blooms. These blooms are highly dependent on surrounding environmental conditions.As phytoplankton grows, it forms the foundation for the food chain, thus passing carbon up to higher life forms. But just as on land, links in the ocean's chain of life also break, and stored carbon settles out of the top layers of water. A portion of it gets swept back to the surface as upwellings, only to begin again, but a major portion sinks to the bottom, becoming what oceanographers call 'marine snow.' This decomposing biological matter literally precipitates through the water and builds up on the ocean bottom, essentially sequestered from the rest of the Earth for geologically long periods of time. || ",
            "hits": 328
        }
    ]
}