### Tectonic Gateways vs. Atmospheric Carbon Dioxide
About years ago, Earth's climate transitioned from a warm "greenhouse" state to a cold "icehouse" state, resulting in the rapid glaciation of Antarctica. Two scientists debate the primary cause of this cooling event.
Scientist 1
The primary driver of the Eocene-Oligocene transition (EOT) cooling was the opening of tectonic gateways, specifically the Drake Passage and the Tasmanian Gateway. As Australia and South America drifted away from Antarctica, a continuous Antarctic Circumpolar Current (ACC) was established. This current thermally isolated Antarctica by preventing warm tropical waters from reaching high southern latitudes. The resulting drop in regional temperature initiated the growth of the Antarctic ice sheet, which increased Earth's albedo and triggered global cooling. Atmospheric drawdown occurred as a consequence, rather than the primary driver, of this glaciation due to changes in ocean circulation patterns.
Scientist 2
The opening of tectonic gateways played a negligible role in the EOT cooling. Instead, the transition was driven primarily by a significant decline in global atmospheric concentrations, which fell below a critical threshold of approximately (parts per million). This decline was caused by increased silicate weathering of continental rocks, which absorbed carbon dioxide from the atmosphere and deposited it in marine sediments. As levels dropped, the greenhouse effect weakened globally, allowing temperatures at both poles to fall sufficiently for continental glaciation to begin. The establishment of the ACC was an effect of the cooling and ice sheet growth, which rearranged surface winds and ocean currents, rather than its cause.
Based on the passage, which of the following statements best describes the core claim of Scientist 1 regarding the factor that directly initiated Antarctic glaciation?
- The tectonic separation of Antarctica from other landmasses, which established the Antarctic Circumpolar Current and thermally isolated the continent.Cevap
- BA decrease in atmospheric carbon dioxide levels below driven by the weathering of continental silicate rocks.
- CAn increase in Earth's albedo that resulted from altered global wind patterns and ocean circulation changes.
- DA global reduction in the greenhouse effect that caused both polar regions to cool simultaneously.