Passage
The gradual formation of the Isthmus of Panama—a narrow strip of land connecting North and South America that closed approximately three million years ago—fundamentally restructured global ocean currents and climate systems. Prior to this geological event, the Atlantic and Pacific Oceans exchanged water freely at the equator. However, persistent tectonic collision slowly forced the seafloor upward, eventually creating a continuous land bridge. This new barrier completely blocked the inter-oceanic passage, forcing the warm, saline equatorial waters of the Atlantic to redirect northward. This diversion dramatically intensified the Gulf Stream, which began transporting significantly more warmth and moisture to high northern latitudes. As this warm, humid air encountered the colder atmospheric conditions of the Arctic and Northern Europe, it resulted in vastly increased snowfall across those regions. The persistent accumulation of snow, combined with a cyclical drop in summer solar radiation, prevented the winter snowpack from melting. Consequently, massive ice sheets expanded across the northern continents, initiating the Pleistocene Ice Age.
Question
Based on the passage, arrange the following events in order of their cause-and-effect relationship, starting with the primary geological event and ending with the final climatic consequence.
- 1Tectonic collision forces the seafloor upward, creating the Isthmus of Panama.
- 2The free exchange of water between the Atlantic and Pacific Oceans is blocked.
- 3Warm, salty Atlantic waters are diverted northward, strengthening the Gulf Stream.
- 4Increased moisture is carried to high northern latitudes and precipitates as snow.
- 5Snowpack accumulates over time, leading to the growth of continental ice sheets.