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.
70 results for "megafauna extinction" — page 2 of 4
S_2_19 — De-Extinction Technology
De-extinction is the scientific effort to resurrect species that have gone extinct, using techniques ranging from selective back-breeding and cloning to advanced genome editing. What was once pure science fiction moved i
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
ZB_5_05 — Extinction Biology and De-Extinction
Extinction — the complete disappearance of a species — is a permanent event that has shaped life's history as profoundly as origination. Background extinction (the normal, continuous loss of species) proceeds at ~0.1–1 s
ZB_5_06 — Mass Extinction Ecology: Catastrophe, Recovery, and Evolutionary Reset
Mass extinctions — episodes in which >75% of species disappear within a geologically brief interval — have profoundly shaped the history of life on Earth, acting as ecological and evolutionary resets that eliminate domin
H_3_06 — Linguistic Extinction and Lost Knowledge Systems
Of the approximately 7,000 languages spoken today, linguists estimate
R_1_11 — Extinction, Recovery, and Adaptive Radiation
The history of life is punctuated by mass extinction events — catastrophic biodiversity losses that eliminate >75% of species in geologically brief intervals — followed by recovery phases and adaptive radiations during w
R_1_03 — Mass Extinction Events
Life on Earth has endured at least five catastrophic mass extinctions in 540 million years, each eliminating 60–96% of all species. The "Big Five" are: End-Ordovician (~443 Mya, ~85% species lost), Late Devonian (~372 My
S_2_10 — Gene Drives: Ecosystem Engineering and Extinction Technology
Gene drives are genetic engineering systems that bias inheritance in sexually reproducing organisms, causing a modified gene to spread through a wild population at rates far exceeding normal Mendelian inheritance (which
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_1_12 — Impact Winter Theory: Nuclear Winter and Chicxulub Parallels
The impact winter hypothesis describes the catastrophic global darkening and cooling that follows a major asteroid or comet impact, caused by the injection of vast quantities of dust, soot, and aerosols into the Earth's
INTERDOC_44 — Mass Destruction Events: A Chronological Timeline from Earth's Origin to Present
Earth has experienced at least 20 major destruction events across 4.5 billion years, ranging from planetary-scale mass extinctions that eliminated 75–96% of all species to civilization-ending catastrophes that reset huma
O_2_11 — Impact Craters: Chicxulub, Vredefort, Sudbury, and Crater Morphology
Impact craters — circular depressions formed by the hypervelocity collision of asteroids, comets, or meteoroids with planetary surfaces — are among the most geologically significant features on Earth and throughout the s
R_2_13 — Mammalian Radiation: Post-Cretaceous Diversification
The Cretaceous-Paleogene (K-Pg) mass extinction 66 million years ago — triggered by an asteroid impact and possibly exacerbated by Deccan Traps volcanism — eliminated the non-avian dinosaurs and opened vast ecological ni
F_1_29 — Aboriginal Australian First Arrival & Deep-Time Heritage
The first arrival of humans in Australia represents the oldest known maritime colonization in human history and one of the most significant events in the story of Homo sapiens. Reaching the continent now called Australia
M_4_10 — Giants in the Archaeological Record: Separating Fact from Fiction
Claims of giant human skeletons — remains of individuals standing 7, 8, 10, or even 30+ feet tall — are among the most persistent themes in alternative archaeology, appearing in 19th-century newspaper accounts, religious
ZH_5_10 — Naked-Eye Observational Limits: Precision, Techniques, and Ancient Achievement
For all but the last ~400 years of human history, every astronomical observation was made with the unaided eye. Understanding the limits and capabilities of naked-eye observation is therefore essential for evaluating anc
C_4_04 — Tuareg and Saharan Serpent Traditions
The Sahara Desert — the world's largest hot desert at 9.2 million km² — was GREEN, wet, and densely inhabited for most of the last 11,000 years. The "African Humid Period" (AHP, ~11,000-5,000 BP) transformed the Sahara i
ZF_3_10 — Marine Paleontology and the Fossil Record of the Seas
Marine paleontology documents the evolution of life in Earth's oceans over ~3.8 billion years — from the earliest microbial fossils (stromatolites, ~3.5 Ga) to the complex marine ecosystems of the modern ocean. The marin
ZF_5_12 — Paleocene-Eocene Thermal Maximum: Ancient Anoxic Ocean Crisis
The Paleocene-Eocene Thermal Maximum (PETM), occurring approximately 55.8 million years ago (latest Paleocene), was one of the most dramatic and rapid climate change events in the Cenozoic, offering the closest geologica
ZF_5_13 — Coral Paleontology: Fossil Reefs and Ancient Reef Ecosystems
Reef ecosystems have existed for over 3.5 billion years — beginning with Archean microbial stromatolite mounds — making them among the longest-running biological communities on Earth. Yet the organisms that build reefs h
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