A study reconstructed the global mean sea level over the past 4.5 million years.
Sea levels were about 20 m higher than today 4.5-3 million years ago.
Sea levels decreased 3-2.5 million years ago with intensifying ice ages.
The study suggests 100,000-year ice age cycles arose from internal climate feedbacks, not Earth's orbit changes.
Detailed Insights:
The reconstruction utilized oxygen isotope data from marine sediments to determine past sea levels.
Higher sea levels in the past indicate significantly warmer global temperatures and reduced ice volume.
The intensification of ice ages led to a drop in sea levels as water was stored in ice sheets.
Internal climate feedbacks involve complex interactions within the Earth's climate system, such as changes in greenhouse gas concentrations and ocean currents.
Scientific/Technical Concepts Involved:
Oxygen Isotopes: Variants of oxygen atoms with different numbers of neutrons, used to determine past temperatures.
Marine Sediments: Accumulated particles on the ocean floor, preserving records of past environmental conditions.
Ice Ages: Periods of long-term reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental ice sheets.