### Younger Dryas Cooling
The Younger Dryas was a period of abrupt global cooling that occurred approximately years ago. Scientists debate the primary cause of this cooling event.
Hypothesis 1
A massive release of freshwater from Lake Agassiz flowed into the North Atlantic Ocean. Because freshwater is less dense than saltwater, this influx capped the warm ocean currents of the thermohaline circulation, halting the transport of heat to the Northern Hemisphere and triggering rapid cooling.
Hypothesis 2
A large comet entered Earth's atmosphere and exploded over North America. The heat and shockwaves from this impact event destabilized the Laurentide Ice Sheet and ignited widespread wildfires, throwing immense dust and soot into the atmosphere that blocked sunlight and caused global cooling.
New Evidence
Researchers analyze marine sediment cores and find that the influx of freshwater into the North Atlantic Ocean—indicated by a distinct drop in salinity and freshwater-associated oxygen isotopes (such as )—occurred approximately to years *after* Northern Hemisphere temperatures had already rapidly dropped.
Based on this information, how does the new evidence affect the two hypotheses?
- AIt supports Hypothesis 1 because it confirms that a freshwater influx did occur, and it weakens Hypothesis 2.
- BIt has no effect on Hypothesis 1 because a freshwater influx is still documented, but it weakens Hypothesis 2.
- It weakens Hypothesis 1 because the freshwater influx did not precede the cooling, but it does not weaken Hypothesis 2.Cevap
- DIt weakens Hypothesis 2 because the impact would have caused an immediate freshwater influx, but it supports Hypothesis 1.