E_3_05 — Megafauna Extinction — Overkill, Climate, or Cosmic Impact?

The late Quaternary megafauna extinction represents one of the most dramatic biodiversity losses in the last 66 million years, eliminating approximately 178 species of large-bodied mammals (≥44 kg) across six continents

E_2_07 — The 4.2 Kiloyear Event — Bronze Age Climate Catastrophe

The 4.2 kiloyear event (~2200 BCE) was a severe, century-scale aridification episode that constitutes one of the most significant abrupt climate changes of the Holocene. Identified through speleothem, marine sediment, an

E_2_05 — Late Antiquity Little Ice Age (536–660 CE) and the Fall of Antiquity

The period 536–660 CE represents one of the most catastrophic environmental and civilizational crises in recorded human history, now termed the Late Antiquity Little Ice Age (LALIA). It began in 536 CE — described by his

E_2_00 — Volcanic Climate Events: Subfolder Summary

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

E_2_01 — 536 CE Climate Catastrophe

This document examines 536 CE Climate Catastrophe, a topic within the Cataclysms and Chronology research area. Key areas of investigation include "The Worst Year to Be Alive", Historical Eyewitness Accounts, The Volcanic

E_0_00 — Cataclysms & Chronology: Section Summary

E_5_07 — Post-Extinction Recovery Patterns: Adaptive Radiation After Mass Dying

Mass extinctions are not merely episodes of destruction — they fundamentally reshape the trajectory of life through the recovery dynamics that follow. Post-extinction recovery is typically slow (5–10 million years for fu

E_5_06 — Holocene Sixth Mass Extinction: Current Biodiversity Crisis

The Holocene "Sixth Mass Extinction" hypothesis holds that current species loss rates are 100–1,000 times the normal background extinction rate, driven primarily by human activity: habitat destruction, overexploitation,

E_5_05 — Late Devonian Mass Extinction: Kellwasser and Hangenberg Events

The Late Devonian mass extinction (~372–359 Ma) was not a single catastrophe but a series of extinction pulses spanning approximately 25 million years, making it unique among the "Big Five" mass extinctions. The two most

INTERDOC_52 — Distributed Cognition: Decentralized Information Networks Across Biology

Cognition — defined functionally as adaptive information processing, decision-making, and memory — is implemented across biology in many architectures other than the centralized animal nervous system. Mycorrhizal fungal

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

ZB_2_18 — Phage-Bacteria Coevolution: Arms Races in the Microbial World

Bacteriophages (phages) — viruses that infect and replicate within bacteria — are the most abundant biological entities on Earth (~10³¹ total particles, outnumbering bacteria ~10:1 in most environments), and their coevol

ZB_2_00 — Organismal Biology Physiology: Subfolder Summary

ZB_2_17 — Mycology: Kingdom Fungi

Kingdom Fungi — the second-largest kingdom of eukaryotes after animals, with an estimated 2.2–3.8 million species (only ~150,000 described) — encompasses organisms that obtain nutrition by absorbing dissolved organic mol

ZB_1_14 — Animal Architecture: Nests, Webs, Mounds, and Biological Engineering

Animal architecture — the construction of physical structures by non-human organisms for shelter, reproduction, thermoregulation, prey capture, mate attraction, or environmental modification — represents one of the most

ZB_1_00 — Animal Behavior Cognition: Subfolder Summary

ZB_1_11 — Predator-Prey Dynamics and Coevolution

Predator-prey dynamics are among the most fundamental processes structuring ecological communities, driving evolutionary arms races, and shaping biodiversity. The Lotka-Volterra equations (Lotka, 1925; Volterra, 1926) pr

ZB_1_13 — Sexual Selection and Mate Choice

Sexual selection — first articulated by Darwin (1871) in The Descent of Man, and Selection in Relation to Sex — is the evolutionary process by which traits that increase mating success are favored, even when they decreas

ZB_1_15 — Infrasound Communication in Wildlife

Infrasound (frequencies below 20 Hz) and low-frequency communication (<100 Hz) are used by elephants, whales, okapi, cassowaries, alligators, and other species for long-range signaling across distances exceeding 10 km. K