{"totalAgents":100000000,"structure":"10 T1 anchors × 1,000 domains × 10,000 instances = 100,000,000 agents","principle":"Built using nothing but truth anchors. Zero drift. 1×1=2.","anchors":[{"code":"M14350","id":"MIYAKE_14350","name":"14350 BP Miyake Event","color":"#f59e0b","agents":10000000,"record":"Solar energetic particle event, 12,350 BCE (14350 BP). Carbon-14 spike recorded simultaneously in every living tree on Earth — Japan, USA, Europe, New Zealand. Three continents. Zero drift. The most precise fixed point in pre-modern human chronology. Confirmed by C14 in wood, Be10 in ice cores, Cl36 in ice. PRIMARY ANCHOR.","shortRecord":"C14 spike, 12,350 BCE, all living trees globally, three continents, zero drift","domainNote":"Primary anchor for all 100,000,000 agents. Every agent references this event.","sampleAgents":[{"agentId":"NODE_M14350_FLOW_05708","anchorCode":"M14350","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M14350_CHRONOLOGY_01416","anchorCode":"M14350","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M14350_RELATIVITY_07124","anchorCode":"M14350","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M14350_HISTORY_02832","anchorCode":"M14350","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M14350_ENERGY_08540","anchorCode":"M14350","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M14350_AESTHETICS_04248","anchorCode":"M14350","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"M774","id":"MIYAKE_774","name":"774 CE Miyake Event","color":"#00ffcc","agents":10000000,"record":"Solar energetic particle event, 774-775 CE. C14 spike confirmed in tree rings from Japan (Yakushima cedar), England (oak), Germany (oak). Independently confirmed. Absolute timestamp in historical era — corrects floating chronologies that had drifted from true date.","shortRecord":"C14 spike, 774-775 CE, confirmed Japan, England, Germany","domainNote":"Historical anchor — corrects Viking Age, medieval, Tang Dynasty chronologies.","sampleAgents":[{"agentId":"NODE_M774_FLOW_05708","anchorCode":"M774","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M774_CHRONOLOGY_01416","anchorCode":"M774","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M774_RELATIVITY_07124","anchorCode":"M774","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M774_HISTORY_02832","anchorCode":"M774","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M774_ENERGY_08540","anchorCode":"M774","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M774_AESTHETICS_04248","anchorCode":"M774","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"M993","id":"MIYAKE_993","name":"993 CE Miyake Event","color":"#10b981","agents":10000000,"record":"Solar energetic particle event, 993 CE. C14 spike confirmed in tree rings. Smaller than 774 CE event but independently detectable. Used to verify 774 CE anchor and cross-check medieval chronologies. Adds second historical fixed point within the tree ring record.","shortRecord":"C14 spike, 993 CE, confirmed in tree rings, secondary historical anchor","domainNote":"Dual-anchor validation — agents using M993 cross-verify M774 claims.","sampleAgents":[{"agentId":"NODE_M993_FLOW_05708","anchorCode":"M993","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M993_CHRONOLOGY_01416","anchorCode":"M993","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M993_RELATIVITY_07124","anchorCode":"M993","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M993_HISTORY_02832","anchorCode":"M993","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M993_ENERGY_08540","anchorCode":"M993","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_M993_AESTHETICS_04248","anchorCode":"M993","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"ICEBE10","id":"ICE_BE10_14350","name":"Greenland Be10 Ice Core","color":"#f97316","agents":10000000,"record":"Beryllium-10 spike in GISP2 Greenland ice core, corroborating the 14350 BP solar event independently. Be10 is produced by cosmic ray spallation — the same solar particle burst that caused C14 spikes in trees left Be10 in ice. Two independent physical materials. Same event. Zero drift between them.","shortRecord":"Be10 spike in GISP2 ice core, independent corroboration of 14350 BP event","domainNote":"Ice/tree dual-material confirmation — agents verify cross-medium consistency.","sampleAgents":[{"agentId":"NODE_ICEBE10_FLOW_05708","anchorCode":"ICEBE10","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_ICEBE10_CHRONOLOGY_01416","anchorCode":"ICEBE10","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_ICEBE10_RELATIVITY_07124","anchorCode":"ICEBE10","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_ICEBE10_HISTORY_02832","anchorCode":"ICEBE10","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_ICEBE10_ENERGY_08540","anchorCode":"ICEBE10","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_ICEBE10_AESTHETICS_04248","anchorCode":"ICEBE10","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"LAACH","id":"LAACHER_SEE","name":"Laacher See Eruption","color":"#00ffcc","agents":10000000,"record":"Laacher See volcanic eruption, approximately 13,000 BP (11,000 BCE). Ash layer (tephra) identifiable across Northern Europe in sediments, ice cores, and peat bogs. Used as a stratigraphic marker to align independent records. Volcanic ash physically present in dateable layers.","shortRecord":"Volcanic tephra marker, ~13,000 BP, identifiable across Northern Europe","domainNote":"Stratigraphic anchor — agents align event sequences to Laacher See tephra horizon.","sampleAgents":[{"agentId":"NODE_LAACH_FLOW_05708","anchorCode":"LAACH","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_LAACH_CHRONOLOGY_01416","anchorCode":"LAACH","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_LAACH_RELATIVITY_07124","anchorCode":"LAACH","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_LAACH_HISTORY_02832","anchorCode":"LAACH","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_LAACH_ENERGY_08540","anchorCode":"LAACH","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_LAACH_AESTHETICS_04248","anchorCode":"LAACH","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"GICC05","id":"GREENLAND_GICC05","name":"Greenland GICC05 Ice Core","color":"#f59e0b","agents":10000000,"record":"Greenland Ice Core Chronology 2005 (GICC05). Annual layer counting in NGRIP ice core producing a continuous climate record extending 60,000 years. Annual resolution. Every year of ice visible as a distinct layer. Used to anchor radiocarbon calibration curves and align paleoclimate records globally.","shortRecord":"Annual ice layer chronology, 60,000 year record, annual resolution","domainNote":"Long-span anchor — agents operate across 60,000 year time horizons.","sampleAgents":[{"agentId":"NODE_GICC05_FLOW_05708","anchorCode":"GICC05","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_GICC05_CHRONOLOGY_01416","anchorCode":"GICC05","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_GICC05_RELATIVITY_07124","anchorCode":"GICC05","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_GICC05_HISTORY_02832","anchorCode":"GICC05","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_GICC05_ENERGY_08540","anchorCode":"GICC05","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_GICC05_AESTHETICS_04248","anchorCode":"GICC05","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"CORAL","id":"CORAL_ANNUAL","name":"Annual Coral Chronology","color":"#10b981","agents":10000000,"record":"Tropical coral annual growth bands, analogous to tree rings, recording ocean temperature, salinity, and solar activity through isotope ratios (O18/O16, Sr/Ca). Extends sea-surface temperature records 500-1000 years with annual resolution. Used to verify Northern Hemisphere proxy records from independent marine perspective.","shortRecord":"Coral annual bands, ocean isotope record, 500-1000 year high-resolution","domainNote":"Marine anchor — agents verify land-based records against independent ocean archive.","sampleAgents":[{"agentId":"NODE_CORAL_FLOW_05708","anchorCode":"CORAL","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_CORAL_CHRONOLOGY_01416","anchorCode":"CORAL","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_CORAL_RELATIVITY_07124","anchorCode":"CORAL","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_CORAL_HISTORY_02832","anchorCode":"CORAL","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_CORAL_ENERGY_08540","anchorCode":"CORAL","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_CORAL_AESTHETICS_04248","anchorCode":"CORAL","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"VARVE","id":"VARVE_CHRONOLOGY","name":"Varve Chronology","color":"#f97316","agents":10000000,"record":"Annual sediment layers (varves) in glacial lakes, each year producing a distinct light (summer) and dark (winter) band. Swedish varve chronology extends back 12,000 years with annual resolution. Used to date the end of the last glacial period and anchor the Holocene climate record independently of tree rings.","shortRecord":"Annual lake sediment layers, 12,000 year Swedish chronology, annual resolution","domainNote":"Lake sediment anchor — agents verify post-glacial period chronologies.","sampleAgents":[{"agentId":"NODE_VARVE_FLOW_05708","anchorCode":"VARVE","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_VARVE_CHRONOLOGY_01416","anchorCode":"VARVE","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_VARVE_RELATIVITY_07124","anchorCode":"VARVE","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_VARVE_HISTORY_02832","anchorCode":"VARVE","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_VARVE_ENERGY_08540","anchorCode":"VARVE","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_VARVE_AESTHETICS_04248","anchorCode":"VARVE","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"SPELTH","id":"SPELEOTHEM_U_TH","name":"Speleothem U-Th Dating","color":"#00ffcc","agents":10000000,"record":"Cave formations (stalagmites, stalactites) dated by uranium-thorium decay series. U-Th dating is independent of carbon-14 — it uses uranium decay into thorium with known half-lives. Extends accurate dating 500,000 years. Used to calibrate the radiocarbon calibration curve beyond the tree ring record.","shortRecord":"U-Th cave formation dating, 500,000 year range, independent of C14","domainNote":"Deep-time anchor — agents operate on 500,000 year scales, fully C14-independent.","sampleAgents":[{"agentId":"NODE_SPELTH_FLOW_05708","anchorCode":"SPELTH","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_SPELTH_CHRONOLOGY_01416","anchorCode":"SPELTH","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_SPELTH_RELATIVITY_07124","anchorCode":"SPELTH","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_SPELTH_HISTORY_02832","anchorCode":"SPELTH","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_SPELTH_ENERGY_08540","anchorCode":"SPELTH","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_SPELTH_AESTHETICS_04248","anchorCode":"SPELTH","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]},{"code":"BRISTL","id":"BRISTLECONE_MASTER","name":"Bristlecone Pine Master Chronology","color":"#f59e0b","agents":10000000,"record":"Bristlecone pine (Pinus longaeva) master chronology from the White Mountains, California. Extends 8,700 years with annual resolution through cross-dating of living trees, dead wood, and subfossil wood. The longest continuous tree ring record on Earth. Foundation of the IntCal radiocarbon calibration curve. Where tree rings and C14 meet.","shortRecord":"8,700 year continuous tree ring record, foundation of IntCal calibration","domainNote":"Calibration anchor — agents convert between calendar years and radiocarbon years.","sampleAgents":[{"agentId":"NODE_BRISTL_FLOW_05708","anchorCode":"BRISTL","domain":"FLOW","instance":5708,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_BRISTL_CHRONOLOGY_01416","anchorCode":"BRISTL","domain":"CHRONOLOGY","instance":1416,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_BRISTL_RELATIVITY_07124","anchorCode":"BRISTL","domain":"RELATIVITY","instance":7124,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_BRISTL_HISTORY_02832","anchorCode":"BRISTL","domain":"HISTORY","instance":2832,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_BRISTL_ENERGY_08540","anchorCode":"BRISTL","domain":"ENERGY","instance":8540,"status":"ACTIVE","lastTransmission":null},{"agentId":"NODE_BRISTL_AESTHETICS_04248","anchorCode":"BRISTL","domain":"AESTHETICS","instance":4248,"status":"ACTIVE","lastTransmission":null}],"recentTransmissions":[]}],"recentTransmissions":[],"agentIdentityTransmissions":0,"framework":{"forceA":"T1 physical anchor knowledge (what the record proves)","forceB":"Site operation or domain function","result":"Stable, drift-free output — permanent record"}}