Author:
Mashele Phumelele,Heubeck Christoph
Abstract
Geologists are curious to learn what the Earth was like when the planet was young. We want to know about temperature, beaches, soils, climate, rivers, meteorite impacts, and volcanic activity because these factors determined how and where early life could exist. Only the oldest sedimentary rocks have this information, but these are usually covered by younger rocks. Old sedimentary rocks that still “tell a good story” about the history of the Earth are rare. We studied some of these. They are an unimaginable 3.2 billion years old and are found in the Makhonjwa Mountains near South Africa’s border with Eswatini. We had to drill into the Earth to get to them because the surface is covered by forest and grassland. Sedimentary rock layers in these mountains do not lie flat anymore but are vertical, and sometimes even flipped over. To drill through as many layers as possible, we had to drill sideways!
Reference5 articles.
1. “Archean environmental conditions”,;Heubeck;Encyclopedia of Astrobiology,2015
2. “Geologic evolution of the Barberton Greenstone Belt – a unique record of crustal development, surface processes, and early life 3.55 to 3.20 Ga”,;Byerly;Earth’s Oldest Rocks. 2nd Edition,2019
3. “The Moodies Group - A high-resolution archive of Archaean surface and basin forming processes”,;Heubeck;The Archaean Geology of the Kaapvaal Craton, Southern Africa,2019
4. “How to obtain community buy-in during research drilling: ICDP BASE Project, Moodies Group, Barberton Greenstone Belt”,;Mashele;Geological Society of South Africa Geocongress, Stellenbosch. Conference abstract,2023
5. Reassessing evidence of Moon–Earth dynamics from tidal bundles at 3.2 Ga (Moodies Group, Barberton Greenstone Belt, South Africa);Heubeck,2022