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.

107 results for "HLA diversity" — page 6 of 6

ZG_3_16 Credible Linguistics & Communication

ZG_3_16 — Sign Language Typology: Structure, Diversity, and the Linguistics of Gesture

Sign languages — natural human languages that use the visual-gestural modality rather than the vocal-auditory channel — are among the most powerful demonstrations that human linguistic capacity is not bound to speech. Th

sign language ASL BSL Stokoe phonology iconicity
ZB_2_14 Verified Ecology & Biology

ZB_2_14 — Photosynthesis Evolution and Diversity

Photosynthesis — the conversion of light energy into chemical energy — is arguably the most important biochemical process on Earth, responsible for virtually all atmospheric oxygen and the primary energy input for nearly

photosynthesis oxygenic photosynthesis anoxygenic chloroplast endosymbiosis Great Oxidation Event
R_1_13 Verified Biology & Evolution

R_1_13 — Archaea: The Third Domain and Extremophilic Diversity

Archaea constitute the third domain of life — neither Bacteria nor Eukarya — recognized as a distinct lineage by Carl Woese and George Fox in 1977 through revolutionary 16S ribosomal RNA phylogenetic analysis. For decade

Archaea third domain Carl Woese extremophile thermophile halophile
ZF_2_22 Verified Oceanography

ZF_2_22 — Hadal Zone & Deep-Sea Trench Ecology

The hadal zone — the deepest region of the ocean, comprising trenches and troughs exceeding 6,000 meters — represents Earth's last great frontier of biological exploration. Named after Hades, the Greek underworld, the ha

hadal zone deep-sea trenches Mariana Trench Challenger Deep barophilic amphipods
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
L_2_17 Verified Genetics & Origins

L_2_17 — Pacific Islander Genetics: Austronesian Ancestry, Denisovan Introgression, and Oceanian Genomics

Pacific Islander populations — spanning Melanesia, Micronesia, and Polynesia — harbor some of the most genetically complex and scientifically informative genomes in human biology. Their genetic history records multiple d

Pacific Islander genetics Oceanian genomics Denisovan introgression Polynesian motif Austronesian ancestry Melanesian genetics
L_3_14 Verified Genetics & Origins

L_3_14 — Genetic Bottleneck Recovery and Founder Effects

A genetic bottleneck occurs when a population's size is drastically reduced, causing a random loss of genetic variation (alleles) that cannot be recovered through subsequent population growth. Founder effects are a speci

genetic-bottleneck founder-effect population-genetics toba-catastrophe effective-population-size heterozygosity