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.
7 results for "eukaryote"
L_3_18 — Horizontal Gene Transfer in Eukaryotes
Horizontal gene transfer (HGT) — the movement of genetic material between organisms through mechanisms other than vertical parent-to-offspring inheritance — was long considered a predominantly prokaryotic phenomenon, cen
R_1_16 — Endosymbiotic Theory: Modern Developments in Organelle Evolution
Endosymbiotic theory — the proposition that mitochondria and chloroplasts originated as free-living bacteria that were engulfed by ancestral eukaryotic cells and subsequently became obligate intracellular symbionts — is
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
ZB_5_21 — Lateral Gene Transfer: Horizontal Exchange and Evolutionary Implications
Lateral gene transfer (LGT), also called horizontal gene transfer (HGT), is the movement of genetic material between organisms by mechanisms other than vertical parent-to-offspring inheritance. First recognized in bacter
R_3_02 — Horizontal Gene Transfer in Complex Life
For decades, the "tree of life" was the central metaphor of evolutionary biology — species branching neatly from common ancestors through vertical gene transmission (parent to offspring). This metaphor is now BROKEN, at
R_1_06 — Symbiogenesis — Lynn Margulis and Cooperative Evolution
Symbiogenesis — the evolutionary origin of new organisms, organelles, or metabolic capabilities through the permanent merger of previously independent life forms — is one of the most consequential biological discoveries
R_1_09 — The Great Oxidation Event: Oxygen, Cyanobacteria, and Earth's Atmospheric Transformation
The Great Oxidation Event (GOE), occurring approximately 2.4–2.1 billion years ago during the Paleoproterozoic, was the most dramatic chemical transformation in Earth's history — atmospheric oxygen rose from trace levels
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