catatomic
Gold Member
- Nov 28, 2012
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And I'd say Chat GPT gave a great answer though I haven't verified any of this myself!
:
how did the CO2 levels go back down after their peak 50 million years ago?
Want a visual timeline or a breakdown of how this compares to today's COâ‚‚ changes?
:
how did the CO2 levels go back down after their peak 50 million years ago?
ChatGPT said:
Great question! COâ‚‚ levels were indeed much higher during the Eocene Epoch, peaking around 50 million years ago. Since then, they gradually declined. Here's how it happened:1.
- Around that time, major tectonic changes occurred — for example, the collision of India with Asia began building the Himalayas and the Tibetan Plateau.
- Mountain building increases rock weathering, a natural process that pulls COâ‚‚ from the atmosphere.
- Silicate rocks (like granite) react with COâ‚‚ and water to form carbonates, locking the carbon away in sediments.
2.
- Weathering of uplifted silicate rocks consumes atmospheric COâ‚‚.
- This process increases with warm temperatures and rain — both abundant during the Eocene.
- The byproducts (like bicarbonates) get washed into the oceans and eventually form limestone, sequestering carbon for millions of years.
3.
- Marine plankton and other organisms use carbon to form calcium carbonate shells.
- When they die, their remains sink to the ocean floor, forming limestone and other sediments, trapping carbon long-term.
4.
- Over time, volcanic COâ‚‚ emissions decreased.
- Volcanic outgassing is a major long-term source of COâ‚‚, so less volcanism means slower input of COâ‚‚ into the atmosphere.
5.
- As COâ‚‚ dropped, Earth's climate gradually cooled.
- This led to the formation of polar ice sheets around 34 million years ago (Oligocene), which increased Earth's reflectivity (albedo) and further reinforced cooling.
- Cooler climates further reduced COâ‚‚ through more efficient weathering and biological processes.
Want a visual timeline or a breakdown of how this compares to today's COâ‚‚ changes?