RESEARCH BASE
Search 3,721 documents across 34 fields — every claim tier-rated by evidence
3,633 are the core, quality-scored corpus (34 lettered sections — see How We Work); the remaining 88 are cross-corpus synthesis documents (68 InterDocs, 12 Connections, 8 Theories) also indexed here.
3,018 results for "li" — page 10 of 151
E_3_01 — Rise and Fall of Civilizations
Every complex civilization in recorded history has collapsed or been transformed beyond recognition. The Bronze Age collapse (~1177 BCE) destroyed the interconnected civilizations of the eastern Mediterranean within a si
E_3_13 — Storegga Slide: Mega-Tsunami and Mesolithic Europe
The Storegga Slide (Norwegian: Storegga-raset; Store = "great," egga = "edge") — a series of submarine landslides on the continental slope off western Norway at approximately 64°N — constitutes one of the largest known m
E_3_20 — Dansgaard-Oeschger Events: Rapid Climate Oscillations
Dansgaard-Oeschger (D-O) events are rapid climate oscillations first identified in Greenland ice cores, characterized by abrupt warming of 8–16°C over Greenland within decades, followed by gradual cooling over centuries
E_3_17 — Environmental Catastrophe–Civilization Correlation Timeline
Systematic cross-referencing of paleoclimate proxy records (ice cores, speleothems, tree rings, marine sediments) with archaeological and historical records reveals repeated correlations between abrupt environmental shif
E_3_06 — The 8.2 Kiloyear Event: Sudden Cooling and Neolithic Disruption
The 8.2 kiloyear event (~6200 BCE) was the most severe abrupt climate oscillation of the Holocene, triggered by a catastrophic outburst flood from glacial Lakes Agassiz and Ojibway into the North Atlantic via Hudson Bay.
E_3_12 — Agriculture: Origins, Spread, and Civilizational Impact
Agriculture — the deliberate cultivation of plants and domestication of animals for food, fiber, and other products — is arguably the single most consequential technological and social transformation in human history, se
E_2_07 — The 4.2 Kiloyear Event — Bronze Age Climate Catastrophe
The 4.2 kiloyear event (~2200 BCE) was a severe, century-scale aridification episode that constitutes one of the most significant abrupt climate changes of the Holocene. Identified through speleothem, marine sediment, an
E_2_26 — Lake Agassiz: Drainage, Climate Disruption, and the Younger Dryas
Glacial Lake Agassiz was the largest proglacial lake in North American history — a vast freshwater body that existed from approximately 13,000 to 8,200 years ago at the southern margin of the retreating Laurentide Ice Sh
E_2_05 — Late Antiquity Little Ice Age (536–660 CE) and the Fall of Antiquity
The period 536–660 CE represents one of the most catastrophic environmental and civilizational crises in recorded human history, now termed the Late Antiquity Little Ice Age (LALIA). It began in 536 CE — described by his
E_2_09 — Heinrich Events and Bond Cycles: Millennial-Scale Climate Oscillations
Heinrich events are episodes of massive iceberg discharge from the Laurentide Ice Sheet through Hudson Strait into the North Atlantic, depositing distinctive layers of ice-rafted debris (IRD) across the ocean floor. Firs
E_2_15 — Azolla Event and Eocene Arctic Cooling
The Azolla Event (c. 49 Ma, Middle Eocene) refers to a period of approximately 800,000 years during which the floating freshwater fern _Azolla_ bloomed prolifically across the semi-enclosed Arctic Ocean, sequestering mas
E_2_10 — Volcanic Winter and Civilizational Effects
Large volcanic eruptions can inject sulfate aerosols into the stratosphere, where they reflect incoming solar radiation, producing global cooling lasting 1–3 years — a phenomenon known as volcanic winter. The most severe
E_2_22 — Dansgaard-Oeschger Events: Rapid Climate Oscillations of the Last Ice Age
Dansgaard-Oeschger (D-O) events are rapid climate oscillations that occurred during the last glacial period (~120,000–11,700 years BP), characterized by abrupt warmings of 8–16°C over Greenland within decades (as few as
E_2_20 — Medieval Warm Period: Climate Optimum and Civilizational Flourishing
The Medieval Warm Period (MWP) — increasingly referred to in scientific literature as the Medieval Climate Anomaly (MCA) to emphasize its complex spatial patterns — was a period of relatively warm climatic conditions acr
E_2_18 — Minoan Eruption Expanded: Tsunami, Ashfall, and Civilization Collapse
The Minoan eruption of Thera (modern Santorini, Greece) was one of the largest volcanic eruptions of the Holocene — a VEI 6–7 event that ejected approximately 60–100 km³ of magma (DRE; some estimates reach 40 km³ DRE wit
E_4_21 — Oxygen Isotope Stages: Marine Isotope Record and Climate Cycles
The marine oxygen isotope record — constructed from measurements of the ratio of oxygen-18 to oxygen-16 (δ¹⁸O) in the calcium carbonate (CaCO₃) shells of foraminifera (single-celled marine organisms) preserved in deep-se
E_4_10 — Ice Core Science: Greenland and Antarctic Climate Records
Ice cores drilled from the Greenland and Antarctic ice sheets constitute one of the most powerful archives of past climate on Earth. Greenland cores (GRIP, GISP2, NGRIP, NEEM) provide high-resolution records extending ba
E_4_11 — The Holocene Climate Optimum and Mid-Holocene Transition
The Holocene Climate Optimum (also called the Holocene Thermal Maximum or Hypsithermal) designates a prolonged warm interval roughly spanning 9,000–5,000 years before present, during which Northern Hemisphere summer temp
E_4_25 — Bayesian Age Modeling: Statistical Frameworks for Archaeological Chronology
Bayesian age modeling — the application of Bayesian statistical inference to combine radiocarbon dates with prior archaeological knowledge (stratigraphy, typology, historical constraints) to produce refined chronological
E_1_17 — Toba Supereruption: Genetic Bottleneck and Climate Catastrophe
The Toba supereruption — occurring approximately 74,000 years ago (74 ka) on the island of Sumatra, Indonesia — was the largest volcanic eruption of the last 2 million years and one of the most catastrophic events in hum
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