Question

The phenomenon commonly designated as the "Classic Maya collapse," which unfolded over the terminal ninth century, has long served as an intellectual crucible for anthropological archaeology. Early interpretations were heavily reliant on an ecological determinist framework, most prominently advanced by Aris, which posited that abrupt environmental catastrophes—namely, severe, prolonged droughts—precipitated a catastrophic agricultural failure. While Aris's model beneficially highlights the fragile interdependence of Maya urban centers and their surrounding microenvironments, it ultimately founders on its own mechanistic reductionism. By attributing the disintegration of complex state systems solely to climatic exogenous shocks, the ecological determinist model strips the Maya of their historical agency, offering a narrative that is more a cautionary tale for the modern Anthropocene than a rigorous reconstruction of ninth-century realities.

In contrast, the sociopolitical fragmentation model, articulated by Vance, rightly redirects scholarly focus toward endogenous mechanisms of decline. Vance meticulously documents the escalating frequency of internecine warfare, the hypertrophy of elite competition, and the eventual dissolution of divine kingship networks. This paradigm offers a compellingly textured view of political decay, capturing the intense internal pressures that fractured Maya polities. However, its explanatory power remains circumscribed; by treating political structures as hermetically sealed arenas, Vance's model fails to adequately integrate the very real demographic and ecological variables that catalyzed these political crises. It is a necessary but profoundly incomplete theoretical apparatus.

More recently, Lira has championed the trade disruption hypothesis, arguing that the collapse was primarily a function of shifting macro-regional economic networks that bypassed the central lowlands. Unfortunately, this framework represents a regression in Maya historiography. Lira's analysis relies on a tenuous extrapolation of scant obsidian and jade distribution patterns, demanding an evidentiary leap that the current archaeological record simply cannot support. Worse still, it anachronistically projects contemporary anxieties regarding globalized supply chains onto pre-Columbian societies, rendering it theoretically suspect and empirically hollow.

Conversely, the emerging resilience and transformation paradigm, pioneered by Chen, offers a necessary corrective to the teleological pessimism of earlier models. Chen convincingly argues that the events of the terminal Classic period should be conceptualized not as a monolithic collapse, but rather as a profound structural reorganization. Through rigorous settlement pattern analysis, Chen demonstrates that while southern centers depopulated, northern and coastal regions experienced simultaneous florescence. This paradigm masterfully integrates ecological adaptability with sociopolitical dynamism, recognizing the enduring continuity of Maya civilization. It stands as the most sophisticated and empirically robust framework yet articulated, demanding a fundamental recalibration of how archaeologists approach societal transformation.

Based on the text above, pair each scholarly framework regarding the Classic Maya collapse on the left with the description on the right that best characterizes the author's overall attitude toward it.