Study links deep-time dust with major impacts on carbon cycl
Wed Nov 18, 2015 4:03 pm
Science Daily Geology
A new study links vast amounts of iron-rich dust deposits from the late Paleozoic period of 300 million years ago with implications for major ecosystem fertilization and a massive drawdown of atmospheric carbon. Understanding iron fertilization and other deep-time events may explain present and future climate change and aid scientists and policymakers when making decisions related to geoengineering Earth.
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A new study links vast amounts of iron-rich dust deposits from the late Paleozoic period of 300 million years ago with implications for major ecosystem fertilization and a massive drawdown of atmospheric carbon. Understanding iron fertilization and other deep-time events may explain present and future climate change and aid scientists and policymakers when making decisions related to geoengineering Earth.
Read more