This chapter demonstrates that the molecular clock can be mathematically decoupled from the Out-of-Africa hypothesis by (1) replacing African-root calibration with fossil-anchored Eurasian calibration (Tianyuan, Xuchang), (2) correcting mutation rates for purifying selection in cold-adapted populations, and (3) substituting the replacement model with regional continuity. This recalibration produces divergence times compatible with the LSED framework—but it does not replace LSED's physical veto. A recalibrated clock that still places migration events in the LGM window (26–19 ka) remains subject to the Sinai dehydration equation (summer transit, death by Day 4–5) and the Red Sea hydrodynamic barrier (50–55 psu, Bab el-Mandeb sill depth <20 m). The molecular clock is a chronometric tool; it is not a physical feasibility simulator. The LSED framework absorbs the recalibrated clock's timeline, but the clock's timeline must still pass through the Death Zone—and the Death Zone has no mathematical loopholes. Glacial isotherms do not recognize mutation rates; salt crusts do not read phylogenetic trees. Beyond the physical veto, however, lies a positive question: if the southern routes were sealed, what happened to the populations that remained in the temperate zone? The answer is metabolic-behavioral coupling. The extreme cold of the Last Glacial Maximum imposed not only a physiological filter—favoring high-efficiency mitochondrial haplotypes (M/N lineages)—but also a behavioral filter. High metabolic thermogenesis demands high caloric intake; high caloric intake in a resource-scarce environment demands high-intensity labor and forward-planning behavior. The EDAR V370A allele, which underwent positive selection during the LGM window, provides independent genetic evidence of this coupling. The same glacial cycles that made the Sinai crossing physically impossible also forged, in the mid-latitude tempering zone, a behavioral phenotype of high activity, foresight, and cooperative resource management—the metabolic-behavioral signature of survival under thermodynamic constraint. This chapter pushes the temporal zero point of the argumentation even further back. The continuous Late Pleistocene stratigraphic sequences of the Bashan site cluster in Shandong and the Nihewan Basin provide evidence of cultural continuity extending approximately 200,000 years. This timeframe corresponds to a critical period of physiological remodeling for the human thermoregulatory system—specifically, the loss of body hair and the increase in sweat gland density. Furthermore, during the low sea levels of the Last Glacial Period, the alluvial fan of the lower Yellow River was exposed as a vast terrestrial expanse, constituting a stable resource base for water and food. These three distinct anchors constitute the irreversible spatiotemporal zero point of the LSED framework.
Jing Zhang (Thu,) studied this question.