Libo–Maolan Pod

The Libo–Maolan pod is an inferred torpor pod located inside the forested ridge-mass of southern Guizhou's Libo karst zone, centred near Longmoshan at approximately 25.22°N, 107.98°E, roughly 45 km southeast of the Luodian–Hongshuihe locus. It is the archive's proposed "interior chamber" pod: a site whose concealment is not achieved through village-integration like Luodian, nor through infrastructure-erasure like Longgong, but through multiple folds of topographic and vegetative isolation that make the terrain itself act as containment.

Among the four southern pod proposals, Libo–Maolan is distinguished by the presence of a named textual corpus — the Shui script tradition — resident within the karst field itself. This makes it the strongest southern analogue to the Wuling north's gazetteer-based cultural archive, though the archive's ability to read Shui script cycle-records is presently limited.

Claims

c0001 — Geographic isolation within a multi-fold karst ridge-mass

The pod locus sits behind multiple folded limestone ridges within the Libo karst zone, approximately coincident with the named Longmoshan feature. Three-dimensional terrain imagery shows the site is not accessible from valley floors by direct sightline; any approach requires ridge-crossing over a nontrivial horizontal distance. The archive treats this topographic isolation as the primary concealment mechanism, distinct from the village-integration mechanism documented at Luodian.

c0002 — Shui script cultural layer provides a textual channel for cycle memory

The Shui ethnic community resident in the Libo–Maolan zone maintains an active textual tradition in Shui script, a logographic system with continuous documented use that predates contact with Han Chinese orthography. The presence of a script-bearing culture resident in a candidate pod locality raises the possibility that cycle-period observations were encoded in Shui textual tradition in a form functionally analogous to the Qing-period Shizhu county gazetteer record. The archive's Shui-language analytical capacity is currently insufficient to read the corpus for tremor-cadence signals, and the claim is flagged as a research priority rather than a completed finding.

c0003 — Longmoshan as a named topographic anchor

The feature labelled Longmoshan ("Dragon Mother Mountain") sits near the centre of the proposed pod locus. Named dragon-toponymy above a candidate pod is not decisive evidence of a resident specimen — the same toponym cluster appears across unrelated sites in the Dragon-Lore Caves corpus — but the coincidence of named topography with the inferred pod position is more consistent with the archive's expectation of cultural-marker overlay at active pods than with the absence of such marking.

c0004 — Paired-pod relationship with Luodian proposed rather than peer siting

The 45 km separation between Libo–Maolan and Luodian–Hongshuihe is too small to treat them as independent field candidates but too large for them to share a single youngest-tier column. The archive's working interpretation is that the two sites are a paired substructure within the same southern corridor extension: Luodian as the outer river-karst approach and Libo as the inner forested chamber. If this reading is correct, both sites share a single founder-scale substrate lineage with bifurcated descendant tiers, rather than representing two unrelated pod formations.

c0005 — No documented MSS instrumentation presence

As with Luodian–Hongshuihe, neither remote sensing nor the GDCC's access-pathway intelligence places MSS instrumentation at the Libo–Maolan locus. The site is under UNESCO World Heritage protection, which complicates any future emplacement of state-run monitoring infrastructure; passive observation through ecological-survey channels is the most plausible current monitoring mechanism. The archive treats the instrumentation gap as both a limitation for predictive modelling and as a structural feature of the pod's concealment — the Heritage designation itself acts as a protective layer over the site.

c0006 — Specimen count estimated at approximately 15-25 across the youngest tier

The interior-chamber topography constrains the pod's physical volume compared to the broader river-karst corridor at Luodian, so the archive's provisional specimen-count estimate for the Libo-Maolan youngest tier is lower at approximately 15-25 specimens distributed across cycle cohorts A through E. Cohort A (cycles 15-16) is estimated at 2-3 specimens at 50-200 m depth. Under the paired-substructure reading with Luodian at c0004, the combined Luodian-Libo youngest-tier specimen total approaches the Wuling figure of 32, with the corridor carrying a single pod of comparable magnitude split across two sub-loci.