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.

609 results for "4.2 ka event" — page 13 of 31

ZF_3_06 Verified Oceanography

ZF_3_06 — Polynesian and Indigenous Ocean Knowledge

Indigenous and Pacific Islander communities have accumulated millennia of empirical ocean knowledge — encompassing navigation, marine ecology, fisheries management, weather prediction, tidal patterns, and ocean-land rela

traditional ecological knowledge TEK Polynesian voyaging Mau Piailug Hokule'a Polynesian Voyaging Society
ZF_3_02 Verified Oceanography

ZF_3_02 — Maritime Archaeology: Shipwrecks, Sunken Cities, and Submerged Structures

Maritime archaeology — the study of human interaction with the sea through material remains — has matured from treasure-hunting salvage into a rigorous scientific discipline that applies the same stratigraphic principles

maritime archaeology shipwreck Uluburun Antikythera Pavlopetri Dwarka
ZF_5_14 Verified Oceanography

ZF_5_14 — Marine Invertebrate Venoms: Cone Snails, Box Jellyfish, and Blue-Ringed Octopus

The oceans harbor an extraordinary diversity of venomous organisms — from the microscopic nematocysts (stinging cells) of cnidarians to the sophisticated venom injection systems of cone snails, blue-ringed octopuses, and

marine venom cone snail Conus conotoxin box jellyfish Chironex fleckeri
ZF_4_15 Verified Oceanography

ZF_4_15 — Ocean Sediments: Deep-Sea Cores, Proxy Records, and Paleoclimate

Ocean sediments are the Earth's most comprehensive climate archive — a continuous record of planetary conditions extending back over 200 million years, slowly accumulated grain by grain on the deep seafloor at rates of m

ocean sediments deep-sea core marine sediment paleoclimate proxy foraminiferal isotopes oxygen isotopes
ZF_4_14 Verified Oceanography

ZF_4_14 — Harmful Algal Blooms: Red Tides, Toxins, and Eutrophication

Harmful algal blooms (HABs) — rapid proliferations of microscopic algae (phytoplankton) or cyanobacteria that produce toxins, deplete oxygen, or otherwise damage marine ecosystems, fisheries, and human health — are incre

harmful algal bloom HAB red tide algal toxin eutrophication paralytic shellfish poisoning
ZF_4_01 Verified Oceanography

ZF_4_01 — Ocean Acidification and Marine Chemistry

The global ocean has absorbed approximately 30% of anthropogenic CO₂ emissions since the Industrial Revolution and over 90% of excess heat from the enhanced greenhouse effect, making it the planet's primary climate buffe

ocean acidification pH carbonate chemistry CO2 absorption ocean carbon sink dissolved oxygen
ZF_1_09 Verified Oceanography

ZF_1_09 — Thermohaline Circulation and Ocean Conveyor

The thermohaline circulation (THC) — often called the "global ocean conveyor belt" — is the large-scale, density-driven system of deep ocean currents that redistributes heat, salt, carbon, and nutrients throughout the wo

thermohaline circulation ocean conveyor belt AMOC Atlantic meridional overturning deep water formation abyssal circulation
ZF_1_11 Verified Oceanography

ZF_1_11 — Rogue Waves, Freak Seas, and Extreme Ocean Events

Rogue waves (also called freak waves, abnormal waves, or episodic waves) are individual ocean surface waves that are at least twice the significant wave height (H_s — the average height of the highest one-third of waves

rogue wave freak wave extreme wave Draupner wave nonlinear wave Benjamin-Feir instability
ZF_1_04 Verified Oceanography

ZF_1_04 — Ocean-Climate Coupling: Paleoceanography

The ocean is Earth's primary climate regulator — absorbing ~93% of the excess heat trapped by greenhouse gases and ~30% of anthropogenic CO₂, storing 50 times more carbon than the atmosphere, and driving glacial-intergla

paleoceanography ice age Milankovitch cycles foraminifera oxygen isotope ocean carbon pump
ZF_1_19 Verified Oceanography

ZF_1_19 — AMOC Collapse Risk

The Atlantic Meridional Overturning Circulation (AMOC) — a system of ocean currents carrying warm surface water northward through the Atlantic and returning cold, dense water at depth — is one of Earth's most critical cl

AMOC Atlantic Meridional Overturning Circulation thermohaline Gulf Stream climate tipping point Rahmstorf
ZF_1_05 Verified Oceanography

ZF_1_05 — Tsunami Science and Warning Systems

Tsunamis — long-wavelength ocean waves generated by sudden displacement of the water column — are among the most destructive natural hazards, capable of crossing entire ocean basins and devastating coastlines thousands o

tsunami seismic sea wave warning system subduction zone megathrust earthquake run-up height
Z_5_13 Verified Molecular Biology

Z_5_13 — Molecular Clocks: Timing Evolution at the Sequence Level

Molecular clocks — the observation that DNA and protein sequences accumulate substitutions (mutations that become fixed in a lineage) at approximately regular rates over long periods of evolutionary time, enabling the es

molecular clock neutral theory substitution rate Zuckerkandl Pauling calibration
Z_3_02 Verified Molecular Biology

Z_3_02 — Epigenetic Inheritance & Transgenerational Effects

Epigenetic inheritance refers to the transmission of phenotypic information across generations through mechanisms other than changes in DNA sequence. The three primary molecular mechanisms — DNA methylation, histone modi

epigenetics transgenerational inheritance DNA methylation histone modification Dutch Hunger Winter Överkalix
Z_2_10 Verified Molecular Biology

Z_2_10 — Genetics of Aging and Progeria

Aging — the progressive decline in physiological function leading to increased vulnerability to disease and death — has a substantial genetic component: twin studies estimate heritability of human lifespan at ~25–30% (He

aging genetics progeria Hutchinson-Gilford progeria HGPS LMNA lamin A
Z_2_21 Verified Molecular Biology

Z_2_21 — Epigenetic Aging Clocks

Epigenetic aging clocks are mathematical models that use patterns of DNA methylation at specific CpG dinucleotides across the genome to estimate an individual's biological age with remarkable accuracy — typically within

epigenetic clock DNA methylation biological age Horvath clock GrimAge aging
Z_2_14 Verified Molecular Biology

Z_2_14 — Genetics of Longevity and Blue Zones

The genetics of human longevity — why some individuals live past 100 while most do not — is a field where heritability is modest, effect sizes are small, and environmental factors dominate, yet several genetic pathways h

longevity genetics aging centenarians Blue Zones telomeres telomerase
Z_1_07 Verified Molecular Biology

Z_1_07 — Genetic Recombination and Crossing Over

Genetic recombination — the physical exchange of DNA segments between homologous chromosomes during meiosis — is a fundamental biological process that generates genetic diversity, ensures proper chromosome segregation, a

recombination crossing over meiosis chiasma homologous recombination linkage
Z_1_02 Verified Molecular Biology

Z_1_02 — Human Chromosome 2 Fusion — Evidence of Primate Ancestry

Humans possess 46 chromosomes (23 pairs), while all other great apes — chimpanzees, gorillas, and orangutans — possess 48 chromosomes (24 pairs). This discrepancy was explained in the 1980s–1990s when molecular cytogenet

chromosome 2 chromosome fusion telomere-telomere ancestral chromosomes primate karyotype great ape
Z_4_02 Verified Molecular Biology

Z_4_02 — Stem Cells and Pluripotency

Stem cells — defined by the dual capacity for self-renewal (division producing at least one daughter cell retaining stemness) and differentiation (specialization into distinct cell types) — are the foundational building

stem cell pluripotency embryonic stem cell induced pluripotent stem cell iPSC Yamanaka factors
Z_4_23 Verified Molecular Biology

Z_4_23 — Memory as Physical and Molecular Phenomenon

What is a memory made of? The question has driven neuroscience from Santiago Ramón y Cajal's 1894 hypothesis that learning strengthens connections between neurons, through Donald Hebb's 1949 postulate that "neurons that

molecular memory memory engram synaptic plasticity long-term potentiation LTP Eric Kandel