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.
3,434 results for "51 Pegasi b" — page 76 of 172
K_2_13 — Attention Networks: Dorsal, Ventral, and Salience Systems
Attention — the selective allocation of processing resources to particular stimuli, locations, or tasks — is among the most studied phenomena in cognitive neuroscience and is intimately linked to consciousness: what we a
K_5_10 — Theories of Self: No-Self, Minimal Self, Narrative Self
The self — the sense of being a unified, continuous subject of experience — is one of the most fundamental yet puzzling features of consciousness. Who or what is the "I" that sees, thinks, remembers, and acts? Theories o
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_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_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
E_3_10 — Clathrate Gun Hypothesis
The clathrate gun hypothesis proposes that warming of ocean waters or thawing of permafrost can destabilize methane clathrates (also called methane hydrates) — ice-like crystalline structures in which methane molecules a
E_2_27 — Mega-Tsunami History: Evidence for Catastrophic Wave Events
Mega-tsunamis — wave events with initial amplitudes of tens to hundreds of meters, far exceeding the 10–30 m waves generated by typical seismic tsunamis — are produced by catastrophic mechanisms including volcanic flank
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_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_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_12 — Dendrochronology: Tree-Ring Science and Precise Ancient Dating
Dendrochronology — the science of dating based on the analysis of tree-ring growth patterns — is one of the most precise dating methods available to archaeology, climatology, and ecology. Pioneered by Andrew Ellicott Dou
E_1_16 — Thera/Santorini Eruption: Detailed Analysis of the Minoan Catastrophe
The eruption of Thera (modern Santorini, Greece) was one of the largest volcanic events in the Holocene — estimated at VEI 6–7 (Volcanic Explosivity Index), ejecting approximately 30–80 km³ of magma (dense rock equivalen
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
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
ZG_2_15 — Language Attrition: How First Languages Are Lost
Language attrition — the process by which a previously acquired language is gradually lost by an individual speaker due to reduced use and exposure — is one of the most fascinating and practically important phenomena in
ZG_5_06 — Lexicography: Dictionary Making from Johnson to Digital
Lexicography — the art and science of dictionary making — is among the oldest scholarly enterprises concerned with language, stretching from ancient Mesopotamian word lists (Sumerian-Akkadian bilingual glossaries, c. 230
ZG_5_21 — Indus Valley Script: The Undeciphered Writing System
The Indus Valley Script (also called the Harappan script) remains one of the last major undeciphered writing systems from the ancient world. [KEY FINDING] Used by the Indus Valley Civilization (c. 2600–1900 BCE) — one of
ZG_1_09 — Writing Materials — Clay, Papyrus, Parchment, Paper
The history of writing materials is the material history of human knowledge itself — the physical substrates on which civilizations recorded thought, law, literature, science, and commerce determined what could be writte
ZG_4_10 — Code-Switching and Multilingual Discourse
Code-switching is the practice of alternating between two or more languages (or language varieties) within a single conversation, sentence, or even a single word — a phenomenon observed wherever multilingual speakers int
ZG_3_02 — FOXP2 and the Genetics of Language
FOXP2 (Forkhead Box Protein P2) is the first gene directly linked to human speech and language ability, located on chromosome 7q31 and encoding a transcription factor that regulates hundreds of downstream genes involved
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