
Paul Voosen
Reporter at Science Magazine
Earth, climate, and planetary science reporter @ScienceMagazine. This account is no longer active. Now at @[email protected].
Articles
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2 weeks ago |
science.org | Paul Voosen
The assault on climate science by President Donald Trump’s administration has been taken to a new level, as NASA has terminated the contract that supports two dozen technical staff at the U.S. Global Change Research Program (USGCRP), the White House office that coordinates research among the federal agencies.
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1 month ago |
science.org | Paul Voosen
NASA’s Curiosity rover has detected what could be a chemical relic of long-ago life on Mars: long-chain organic molecules. Found after painstaking reanalysis of data on a sample drilled from a lake that dried up billions of years ago, the molecules likely derived from fatty acids, a common building block of cell membranes on Earth.
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1 month ago |
science.org | Paul Voosen
The Woodlands, Texas—For nearly as long as Earth has existed, the Moon has been with it. That’s the conclusion of several studies suggesting the Moon formed some 65 million years after the start of the Solar System—and only tens of millions of years after Earth.
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1 month ago |
science.org | Paul Voosen
NASA announced today it will eliminate its Office of the Chief Scientist, along with offices advising the agency on technology, strategy, and coordinating its diversity, equity, inclusion, and accessibility (DEIA) efforts. The reductions, which will eliminate two dozen jobs, come as part of the agency’s “reduction in force,” mandated by the White House.
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1 month ago |
science.org | Paul Voosen
Earth’s atmosphere, the veneer of gases that makes most life possible, has changed dramatically over time. Bubbles of ancient air trapped in polar ice cores provide reliable archives of the past 6 million years—but that’s less than 0.002% of Earth’s history. For the eons before that, which saw the origin and proliferation of life, researchers have had to infer the atmosphere’s composition from evidence of its chemical effects on metals and minerals preserved in ancient rocks.
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