Formation of sedimentary rocks in present-day western Greenland. Examined by Shidlowski in 1988 AD, they showed increased values of the isotope 12C, suggesting a probable organic origin, for example, due to photosynthesis.
Formation of sedimentary rocks in present-day western Greenland. Examined by Shidlowski in 1988 AD, they showed increased values of the isotope 12C, suggesting a probable organic origin, for example, due to photosynthesis.