During the transition from the Pleistocene to the Holocene epoch, the sudden return to glacial conditions known as the Younger Dryas was triggered by a complex interplay of hydro-glacial and oceanic mechanisms. As the Laurentide Ice Sheet rapidly retreated due to increasing global temperatures, vast quantities of fresh meltwater accumulated in proglacial Lake Agassiz. The catastrophic breaching of the lake's eastern ice dam redirected this massive freshwater pulse from the Mississippi River drainage system into the North Atlantic Ocean. Because freshwater is significantly less dense than saltwater, this influx stratified the surface waters of the North Atlantic, fundamentally disrupting the thermohaline circulation—the 'global ocean conveyor belt' driven by the sinking of cold, highly saline water. The resultant weakening of the Atlantic meridional overturning circulation drastically reduced the northward transport of equatorial heat. Consequently, despite the broader planetary warming trend, atmospheric temperatures in the Northern Hemisphere plummeted, initiating the millennium-long cooling phase of the Younger Dryas.
According to the passage, which one of the following explicitly caused the stratification of the surface waters in the North Atlantic?
- The introduction of a massive volume of freshwater that possesses a lower density than saltwaterCevap
- BThe fundamental disruption of the global ocean conveyor belt driven by sinking cold water
- CThe rapid retreat of the Laurentide Ice Sheet triggered by an overarching planetary warming trend
- DThe catastrophic accumulation of glacial meltwater within the Mississippi River drainage system
- EThe melting of northern polar sea ice resulting from rapidly increasing global temperatures