Further to “Researchers: Chemical evidence of life on Earth 3.2 billion years ago?”:
An upcoming lecture (March 11, 2015, New York, registration but no charge) by OOL researcher Robert Hazen will advance the thesis that:
Earth’s geological and biological evolution are intertwined in remarkable ways that are coming into sharper focus thanks to studies of the diversity and distribution of minerals. Robert Hazen will explore the emerging field of ‘mineral evolution’ and reveal how Earth, which is unique among known worlds in its biosphere, is unique in its geosphere as well.
In this lecture, Robert Hazen will examine how Earth’s near-surface environment has evolved as a consequence of selective physical, chemical and biological processes — an evolution that is preserved in the mineralogical record. Recent studies of mineral diversification through time reveal correlations with major geochemical, tectonic and biological events, including large changes in ocean chemistry, the supercontinent cycle, the origins of life, the increase in atmospheric oxygen and the rise of the terrestrial biosphere. Growing data resources also point to new opportunities for applying statistical methods and visualization strategies for deep-time — or geologic time — data. Among our most provocative findings: Earth is mineralogically unique in the cosmos.
If Earth is indeed mineralogically unique in the cosmos, theses re life on exoplanets must address the findings.
Does nature just “naturally” produce life?
Don’t let Mars fool you. Those exoplanets teem with life!
Looking for planets in all the wrong places?
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