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.
212 results for "CEA" — page 7 of 11
K_3_11 — Animal Consciousness and Sentience
The question of whether non-human animals possess conscious experience — subjective awareness, felt pain, emotions, and self-recognition — has moved from philosophical speculation to a major neuroscientific research prog
K_5_07 — Psychophysics: Measuring the Relationship Between Mind and World
Psychophysics — literally "the physics of the soul/mind" — is the scientific study of the quantitative relationship between physical stimuli and the sensations and perceptions they produce. Founded by Gustav Theodor Fech
E_2_14 — Deccan Traps and Large Igneous Provinces
Large Igneous Provinces (LIPs) are the most voluminous volcanic features on Earth: enormous outpourings of basalt lava and associated intrusions that cover areas of up to millions of square kilometers and release colossa
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_04 — Permian-Triassic Great Dying — The Biggest Mass Extinction
Approximately 252 million years ago, at the boundary between the Permian and Triassic periods, Earth experienced the worst mass extinction in its entire history — an event so devastating it has been called "The Great Dyi
Q_3_09 — Astrobiology and Origin of Life in Space
Astrobiology — the study of the origin, evolution, distribution, and future of life in the universe — sits at the intersection of biology, chemistry, planetary science, and astronomy. The central question — "Are we alone
INTERDOC_17 — Navigation, Seafaring, and the Lost Maritime Web
The Austronesian expansion — beginning ~3500 BCE from Taiwan and reaching Madagascar (~500 CE), Hawaii (~1000 CE), and New Zealand (~1250 CE) — represents the greatest sustained maritime achievement of the pre-modern wor
ZB_5_23 — Bioacoustics & Animal Communication
Bioacoustics — the study of biological sound production, transmission, and reception — reveals a hidden world of communication systems of extraordinary sophistication. Humpback whale songs contain hierarchical structure
ZB_3_23 — Coral Reef Ecosystem Dynamics
Coral reefs are among Earth's most biodiverse and economically valuable ecosystems, occupying less than 0.1% of the ocean floor yet supporting approximately 25% of all marine species (~830,000 species). Built over millen
ZB_3_20 — Kelp Forest Ecology
Kelp forests are underwater ecosystems formed by dense stands of large brown macroalgae (Order Laminariales), predominantly species of Macrocystis (giant kelp, reaching heights of 45–60 meters — among the fastest-growing
ZB_3_02 — Coral Reef Ecology: Symbiosis, Bleaching, and Biodiversity Hotspots
Coral reefs, built by tiny colonial cnidarians over millennia, harbor approximately 25% of all marine species while covering less than 0.1% of the ocean floor — earning the title "rainforests of the sea." The ecological
O_2_19 — Expanding Earth Theory
The expanding Earth hypothesis proposes that the planet has significantly increased in radius (and possibly mass) over geological time, with continental drift and ocean basin formation being consequences of this expansio
O_2_04 — Geological Hotspots and Mantle Plumes
Geological hotspots are locations where anomalously high volcanic activity occurs away from tectonic plate boundaries — the dominant hypothesis explains them as surface expressions of mantle plumes, columns of hot, buoya
O_2_09 — The Mohorovičić Discontinuity and Earth's Internal Structure
The Mohorovičić Discontinuity (the "Moho") — the boundary between Earth's crust and upper mantle — is one of the most fundamental structural features of our planet and a cornerstone of solid-Earth geophysics. It was disc
O_2_03 — Plate Tectonics, Continental Drift, and Deep Earth
Plate tectonics — the theory that Earth's outer shell (lithosphere) is divided into rigid plates that move, collide, and separate atop a convecting asthenosphere — is one of the great unifying theories of modern science.
O_2_01 — Volcanism, Supervolcanoes, and Geological Catastrophism
Volcanic eruptions are among the most powerful forces on Earth, capable of altering global climate, triggering mass extinctions, collapsing civilizations, and imprinting themselves on human mythology for millennia. The T
O_4_15 — Rogue Waves: Extreme Ocean Waves and the Physics of the Improbable
Rogue waves (also called freak waves, monster waves, or abnormal waves) — individual ocean waves that are exceptionally large relative to the surrounding sea state, typically defined as waves whose height exceeds 2.2 tim
O_5_12 — Volcanic Islands: Surtsey, Hawaii, and Emergent Land
Volcanic islands — landmasses formed by submarine volcanic eruptions that build up from the ocean floor until they breach the sea surface — represent some of the most dynamic and scientifically informative geological fea
O_5_05 — Ice Ages and Milankovitch Cycles: Orbital Forcing of Climate
Ice ages — periods when massive continental ice sheets expand to cover large portions of Earth's surface — are among the most dramatic climate events in the planet's history. The Quaternary glaciation (beginning ~2.6 mil
T_1_08 — Personality Psychology and the Big Five
Personality psychology seeks to understand individual differences in characteristic patterns of thinking, feeling, and behaving — and why these patterns remain relatively stable across time and situations.
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