Passage
During the late Miocene epoch, approximately 5.96 million years ago, the Mediterranean Sea underwent a dramatic transformation known as the Messinian Salinity Crisis. Tectonic uplift in the Gibraltar region, combined with a global drop in sea levels driven by Antarctic glaciation, restricted the inflow of Atlantic water through the Betic and Rifian corridors. Deprived of its primary water source, the Mediterranean Sea, which lies in an arid climate zone, experienced evaporation rates that far exceeded precipitation and river runoff. Consequently, the sea levels plummeted, leaving behind a desiccated basin covered with salt deposits up to three kilometers thick. This massive accumulation of salt withdrew roughly six percent of the oceans' salt content, which directly lowered the salinity of the remaining global oceans. As a result, the freezing point of water in high-latitude regions rose, facilitating the rapid expansion of sea ice around Antarctica and further accelerating global cooling. While tectonic isolation initiated this regional crisis, the resultant global oceanic changes subsequently reinforced the glacial processes that had partially driven the sea-level drop in the first place.
Based on the passage, the rapid expansion of sea ice around Antarctica was directly facilitated by which of the following environmental changes?
- AThe tectonic uplift in the Gibraltar region that restricted Atlantic water inflow through the Betic and Rifian corridors.
- BThe expansion of Antarctic sea ice, which withdrew six percent of the salt content from the global oceans.
- A decrease in the salinity of the global oceans, which raised the freezing point of water in high-latitude regions.Answer
- DAn increase in precipitation and river runoff that lowered the evaporation rate in the Mediterranean basin.