RESEARCH BASE

Search 3,721 documents across 34 fields — every claim tier-rated by evidence

3,721 Documents 34 Sections 43,625 Citations 34,852 Keywords Indexed 4 Evidence Tiers

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.

3,665 results for "P vs NP" — page 124 of 184

K_5_08 Verified Consciousness

K_5_08 — Metacognition: Thinking About Thinking

Metacognition — literally "cognition about cognition" or "thinking about thinking" — refers to the human capacity to monitor, evaluate, and regulate one's own cognitive processes. When you realize you don't understand a

metacognition metamemory meta-awareness thinking about thinking monitoring control
K_5_13 Credible Consciousness

K_5_13 — Integrated World Models: Bayesian Brain and Consciousness

The Bayesian brain hypothesis proposes that the brain is fundamentally a prediction machine — it constructs and maintains internal generative models of the world (including the body), uses these models to generate predic

Bayesian brain predictive processing predictive coding free energy principle Friston Helmholtz
K_5_11 Credible Consciousness

K_5_11 — Synaesthesia and Consciousness: Cross-Modal Binding

Synaesthesia (British spelling; "synesthesia" in American English) is a neurological condition in which stimulation of one sensory or cognitive pathway automatically triggers an involuntary experience in a second, unstim

synaesthesia synesthesia cross-modal grapheme-color sound-color chromesthesia
E_3_21 Verified Cataclysms & Chronology

E_3_21 — The 5.9 Kiloyear Event: Saharan Desiccation & the Birth of River Civilizations

The 5.9 kiloyear event (c. 3900 BCE) marks the terminal phase of the African Humid Period — a 6,000-year interval during which the Sahara was a grassland savanna supporting abundant lakes, rivers, and human populations.

5900-year-event green-sahara african-humid-period saharan-desiccation neolithic-subpluvial orbital-forcing
E_3_18 Verified Cataclysms & Chronology

E_3_18 — Black Mat: Younger Dryas Boundary Layer Geochemistry

The "black mat" is a thin, dark, organic-rich sedimentary layer found at dozens of archaeological and geological sites across North America, dating to the onset of the Younger Dryas stadial (~12,800 cal BP). First system

black mat Younger Dryas boundary carbonaceous layer nanodiamonds magnetic spherules iridium
E_3_22 Verified Cataclysms & Chronology

E_3_22 — Historic Mega-Earthquakes: Cascadia, New Madrid, and the Seismic Record

The seismic record of North America reveals two mega-earthquake systems that challenge the common assumption that destructive earthquakes are confined to well-known plate boundaries like the San Andreas Fault: the Cascad

mega-earthquake Cascadia New Madrid seismology subduction zone paleoseismology
E_3_09 Verified Cataclysms & Chronology

E_3_09 — Messinian Salinity Crisis

The Messinian Salinity Crisis (MSC) — approximately 5.96–5.33 million years ago (late Miocene) — was one of the most dramatic geological events in the Cenozoic: the near-complete desiccation (drying up) of the Mediterran

Messinian Salinity Crisis Mediterranean evaporite Gibraltar Strait of Gibraltar Zanclean flood
E_2_09 Verified Cataclysms & Chronology

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

Heinrich events Bond cycles ice-rafted debris Dansgaard-Oeschger thermohaline circulation AMOC
E_2_12 Verified Cataclysms & Chronology

E_2_12 — Great Oxygenation Event

The Great Oxygenation Event (GOE) — approximately 2.4–2.1 billion years ago — was one of the most transformative events in Earth's history: the first permanent rise of free molecular oxygen (O₂) in the atmosphere, from n

Great Oxygenation Event GOE oxygen crisis cyanobacteria photosynthesis Paleoproterozoic
E_2_15 Verified Cataclysms & Chronology

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

Azolla event Azolla fern Arctic Ocean Eocene carbon sequestration CO₂ drawdown
E_4_19 Verified Cataclysms & Chronology

E_4_19 — Mono Lake and Gothenburg Excursions: Short Geomagnetic Events

Geomagnetic excursions are brief, extreme departures of the Earth's magnetic field from its normal dipolar configuration — events during which the virtual geomagnetic pole (VGP) deviates by more than 40–45° from the geog

geomagnetic excursion Mono Lake Gothenburg Laschamp paleomagnetic virtual geomagnetic pole
E_4_10 Verified Cataclysms & Chronology

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

ice cores GRIP GISP2 NGRIP EPICA Vostok
E_4_24 Verified Cataclysms & Chronology

E_4_24 — Quaternary Science: Integrating Ice Ages, Extinctions, and Migrations

Quaternary science is the interdisciplinary study of Earth's most recent geological period — the Quaternary (2.58 Ma to present), encompassing the Pleistocene (2.58 Ma to 11,700 BP) and the Holocene (11,700 BP to present

Quaternary Pleistocene Holocene ice age glaciation megafaunal extinction
E_4_22 Verified Cataclysms & Chronology

E_4_22 — Varve Chronology: Annual Lake Sediment Records

Varve chronology is a dating and paleoclimate method based on counting and analyzing varves — annually laminated sediment layers deposited in lakes (and occasionally in marine or estuarine settings). Each varve typically

varve annual lamination lacustrine lake sediment glaciolacustrine clastic varve
E_1_09 Verified Cataclysms & Chronology

E_1_09 — Solar Storms and Miyake Events

The Sun periodically releases enormous bursts of energy — coronal mass ejections (CMEs) and solar proton events (SPEs) — that interact with Earth's magnetosphere and can have devastating consequences for technology-depen

solar storm Carrington Event coronal mass ejection CME Miyake event solar proton event
E_5_03 Verified Cataclysms & Chronology

E_5_03 — The End-Triassic Mass Extinction

The End-Triassic mass extinction (c. 201.564 ± 0.015 million years ago) was one of the "Big Five" mass extinctions in Earth's history, eliminating approximately 76% of all species and ~50% of genera, clearing the ecologi

End-Triassic Triassic-Jurassic mass extinction CAMP Central Atlantic Magmatic Province CO2
E_5_06 Verified Cataclysms & Chronology

E_5_06 — Holocene Sixth Mass Extinction: Current Biodiversity Crisis

The Holocene "Sixth Mass Extinction" hypothesis holds that current species loss rates are 100–1,000 times the normal background extinction rate, driven primarily by human activity: habitat destruction, overexploitation,

sixth extinction Holocene Anthropocene biodiversity loss IUCN Red List background extinction rate
E_5_02 Verified Cataclysms & Chronology

E_5_02 — The Ordovician-Silurian Mass Extinction

The Late Ordovician mass extinction (c. 445–444 million years ago, at the Ordovician-Silurian boundary) was the second-most severe extinction event in Earth's history in terms of percentage of species lost — approximatel

Ordovician Silurian mass extinction Hirnantian glaciation Late Ordovician graptolites
E_5_05 Verified Cataclysms & Chronology

E_5_05 — Late Devonian Mass Extinction: Kellwasser and Hangenberg Events

The Late Devonian mass extinction (~372–359 Ma) was not a single catastrophe but a series of extinction pulses spanning approximately 25 million years, making it unique among the "Big Five" mass extinctions. The two most

mass extinction Devonian Kellwasser Hangenberg reef collapse anoxia
ZG_2_06 Verified Linguistics & Communication

ZG_2_06 — Historical Linguistics and Language Family Classification

Historical linguistics is the scientific study of how languages change over time, how they are related to each other, and how they can be grouped into language families descended from common ancestors. The discipline's c

historical linguistics comparative method language family proto-language sound change Grimm's law