News: Researchers found evidence of microbial life ~3.5 billion years ago in the Singhbhum Craton, eastern India.
Singhbhum Craton:
- Ancient, stable block of continental crust located mainly in Jharkhand & Odisha.
- Contains rocks dating back 3.5–4 billion years.
- Important for studying Earth’s Archaean geological history and early life.
Evidence of Life:
- Found in a carbon-bearing black-and-white chert from Bhatirdari.
- Zircons → geological clocks → indicated age of about 3.497 billion years.
- Carbon isotope signatures → consistent with biological processes.
- Evidence combines rock age + carbon chemistry + geological context.
Geological Significance:
- Singhbhum has ancient greenstone successions and submarine volcanic rocks.
- Features include pillow lava and komatiites.
- Comparable to ancient terrains of South Africa and Western Australia.
Significance:
- Provides a window into early Earth and emergence of life.
- Suggests microbial life may have appeared relatively early after Earth became habitable.
- Helps understand ancient volcanism, tectonics and habitable conditions.