Passage:
For decades, paleoclimatologists investigating the African Humid Period (11,000–5,000 years ago) attributed the expansion of Saharan vegetation primarily to orbital forcing—specifically, increased summer insolation that intensified the West African monsoon. However, climate researcher Dr. Elena Vance asserts that orbital forcing alone was insufficient to sustain deep-inland precipitation. Vance contends that a vegetation-albedo feedback loop was the essential driver: initial modest precipitation promoted early plant growth, which lowered surface albedo and increased evapotranspiration, thereby self-amplifying regional rainfall. As evidence, Vance notes that Saharan paleolake sediment cores display abrupt, non-linear shifts in pollen density during periods when insolation changes were virtually non-existent.
Statement:
Discovering that fossilized plant stomata densities in Saharan paleolake sediments remained unchanged throughout the initial two millennia of the African Humid Period would weaken Dr. Vance's assertion regarding the primary mechanism of Saharan greening.
Cevap: Cevap