Passage:
Historians of Mesoamerican agriculture have long debated the factors underlying the abandonment of lowland Maya urban centers during the Terminal Classic period (c. – CE). Traditional hypotheses emphasized environmental degradation, proposing that intensive terrace farming on hillside slopes triggered catastrophic topsoil erosion and nutrient depletion, rendering agricultural hinterlands incapable of supporting dense populations. Recently, however, agro-ecologist Elena Vasquez proposed a revised model: rather than hillside terracing, it was the widespread reliance on lowland wetland agricultural systems—specifically *chinampa*-style raised fields constructed in seasonal swamps—that constituted the primary vulnerability. Vasquez contends that raised-field agriculture required precise, continuous labor input to clear silted canals and maintain water table levels. According to her model, a series of severe multi-year droughts disrupted regional hydrologic regimes, causing water tables to drop below canal beds. This led not to gradual soil exhaustion, but to an immediate, systemic collapse of crop yields across wetland networks, forcing urban abandonment.
To support her assertion that raised fields were the critical failure point, Vasquez points to sediment core samples from lowland basin lakes showing an abrupt drop in *Zea mays* (maize) pollen coinciding precisely with initial drought indicators, whereas terrace-adjacent sediment deposits display a far more gradual decline in agricultural activity.
Question:
Which of the following findings, if true, would most seriously weaken Elena Vasquez's assertion regarding the primary vulnerability that caused the collapse of lowland Maya urban centers?
- Sediment cores from hillside terraces reveal that extensive topsoil erosion and severe nutrient depletion occurred several decades prior to the multi-year droughts, coinciding with the earliest recorded urban population declines.Answer
- BHydrologic simulations of lowland swamp networks demonstrate that even minor drops in the regional water table render raised-field canals functionally useless within a single agricultural season.
- CHighland Maya urban settlements that relied exclusively on rainfall-fed mountain terracing maintained stable population densities for more than a century after lowland cities were abandoned.
- DPaleoclimate data indicate that the severity and duration of multi-year droughts during the Terminal Classic period varied significantly across different sub-regions of the Maya lowlands.
- EArchaeological excavations reveal that the construction of *chinampa*-style raised fields required substantially more labor per hectare than the initial building of hillside agricultural terraces.