A Palaeoproterozoic puzzle
Near Lake Onega in the Republic of Karelia, Russia, lies a massive deposit of a curious, carbon-rich rock known as shungite. These deposits are ancient, dating back approximately 2 billion years to the Paleoproterozoic Era. The total carbon reserve within the Shunga deposit is estimated to be over 250 gigatonnes, spread across an area of roughly 9,000 square kilometers. Shungite is not a mineral but a mineraloid, as it lacks a defined crystal structure. Its composition is primarily non-crystalline carbon, with some varieties containing up to 98% carbon.
The origin of this immense carbon deposit is a scientific debate. The prevailing theory asserts a biological origin, suggesting the carbon is the metamorphosed remains of vast blooms of ancient microorganisms, like algae or bacteria, from a brackish lagoon. These organisms would have been deposited in shallow water sediments and then transformed by heat and pressure over geological time. An alternative hypothesis suggests an abiogenic origin, where the carbon formed through non-biological processes deep within the Earth's crust or was even delivered by a meteorite. While the biological origin theory is now more widely accepted, the exact mechanisms that led to such a huge and concentrated carbon deposit remain a subject of study.