Soru

For decades, the prevailing explanation for the collapse of the Classic Maya civilization in the ninth century has been the "megadrought" hypothesis. This theory posits that a series of exceptionally severe, multi-decade droughts devastated the agricultural foundation of Maya city-states, leading to widespread famine, political instability, and ultimately, a catastrophic demographic collapse. Proponents of this established view rely heavily on paleoclimatic records—such as sediment cores extracted from Lake Chichancanab and stalagmite data from regional caves—which show a stark, sudden decrease in rainfall precisely aligning with the period of systemic societal breakdown. According to these researchers, the agricultural deficit caused by this climate shift was insurmountable for a society heavily dependent on seasonal rains.

Recently, however, archaeological evidence has complicated this unipolar narrative. Extensive excavations in the northern Yucatán Peninsula reveal that several major Maya centers, such as Chichén Itzá and Mayapán, not only survived but actively flourished during the very centuries when the supposedly ubiquitous drought was at its peak. Furthermore, advanced isotopic analysis of human remains recovered from these northern sites indicates that local populations maintained diverse and nutritionally adequate diets throughout the most severe dry periods. If an unmitigated drought were indeed the sole monolithic engine of collapse, one would expect a far more uniform pattern of abandonment across the entirety of the Maya lowlands.

While climate data undeniably confirms that a severe regional drought occurred during the Terminal Classic period, framing this ecological stressor as the singular cause of the collapse is reductive. Rather than invalidating the drought hypothesis entirely, the survival of the northern cities suggests that the climate shift acted as a catalyst within a complex, pre-existing web of geopolitical and economic vulnerabilities. The southern lowlands, where the societal collapse was most absolute, were already suffering from endemic warfare, the disruption of critical obsidian and jade trade networks, and deep-seated institutional rigidities that prevented rapid adaptation. The northern cities, conversely, had previously shifted their economic reliance to maritime trade routes, which were considerably less affected by inland agricultural scarcity.

Therefore, a more accurate and comprehensive model of the Classic Maya collapse must be inherently multi-causal. The megadrought was not an isolated executioner, but rather a profound environmental shock that exposed and exploited the distinct structural weaknesses of specific city-states.

Which of the following most accurately describes the primary argumentative function of the first sentence of the third paragraph ("While climate data... reductive")?