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.

774 results for "sea ice" — page 3 of 39

ZH_2_18 Credible Archaeoastronomy

ZH_2_18 — Angkor Wat Astronomical Alignments

Angkor Wat — the vast Hindu-Buddhist temple complex in Siem Reap, Cambodia, built by King Suryavarman II between approximately 1113 and 1150 CE — is not only the largest religious monument on Earth (covering 162.6 hectar

Angkor Wat astronomical alignment equinox solstice Khmer Suryavarman II
C_4_07 Verified Global Traditions

C_4_07 — Inuit and Arctic Cosmology — Sedna, Shamanic Flight, and Survival Knowledge

The Inuit, Yupik, and Aleut peoples of the Arctic — collectively known as Eskimo-Aleut or Inuit-Yupik-Unangan — developed one of humanity's most extraordinary spiritual-ecological systems in the world's harshest habitabl

Inuit Arctic Sedna Sila angakkuq shaman
C_5_28 Verified Global Traditions

C_5_28 — Ritual Sacrifice: Blood, Fire, and the Sacred Exchange

Ritual sacrifice — the deliberate destruction or offering of something valuable (animal, human, agricultural produce, wealth) to a divine or supernatural power — is one of the most universal and oldest documented human p

ritual sacrifice human sacrifice animal sacrifice scapegoat Aztec Inca
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
ZF_2_01 Verified Oceanography

ZF_2_01 — Deep-Sea Ecosystems: Hydrothermal Vents and Abyssal Biology

The deep ocean — defined as waters below 200 m, encompassing 95% of the ocean's volume and Earth's largest biome — remained virtually unexplored until the mid-20th century. The 1977 discovery of hydrothermal vent ecosyst

hydrothermal vent black smoker white smoker chemosynthesis extremophile tube worm
ZF_2_12 Verified Oceanography

ZF_2_12 — Deep-Sea Gigantism and Abyssal Ecology

Deep-sea gigantism (also called abyssal gigantism) is the observed tendency for certain deep-sea invertebrates and some vertebrates to attain body sizes far exceeding those of their shallow-water relatives — a pattern do

deep-sea gigantism abyssal ecology giant squid giant isopod Bathynomus deep-sea fish
ZF_2_04 Verified Oceanography

ZF_2_04 — Bioluminescence and Deep-Sea Phenomena

In the deep ocean — where sunlight vanishes below ~1,000 m — bioluminescence is the dominant source of light and the most widespread form of communication on Earth. An estimated 76% of all ocean organisms produce or disp

bioluminescence luciferin luciferase counterillumination milky seas anglerfish
ZF_3_01 Verified Oceanography

ZF_3_01 — Sea-Level History: Glacial Cycles, Meltwater Pulses, and Coastal Archaeology

Sea level has varied by over 120 meters between glacial and interglacial periods, repeatedly reshaping coastlines, exposing and flooding continental shelves, and creating or destroying land bridges that directed human mi

sea level meltwater pulse glacial maximum LGM Holocene transgression eustatic change
ZF_5_04 Verified Oceanography

ZF_5_04 — Aquaculture: Fish Farming, Mariculture, and Blue Revolution

Aquaculture — the farming of aquatic organisms including fish, shellfish, crustaceans, and seaweed — has become the fastest-growing food production sector in the world and now provides more seafood for human consumption

aquaculture fish farming mariculture blue revolution salmon farming shrimp farming
ZF_5_09 Verified Oceanography

ZF_5_09 — Whale Falls: Deep-Sea Decomposition and Chemosynthetic Ecosystems

Whale falls — the carcasses of large cetaceans that sink to the deep ocean floor — are among the most remarkable ecosystems in the sea, transforming the nutrient-poor desert of the abyssal plains into oases of biological

whale fall deep sea decomposition chemosynthesis sulfide bone-eating worm
ZF_4_03 Verified Oceanography

ZF_4_03 — Desalination and Ocean Water Resources

Desalination — the removal of dissolved salts from seawater or brackish water to produce freshwater — has become an increasingly critical technology as global freshwater demand rises and climate change intensifies drough

desalination reverse osmosis water scarcity brine discharge membrane technology thermal desalination
ZF_1_06 Verified Oceanography

ZF_1_06 — Arctic and Antarctic Ocean Systems

The Arctic and Antarctic ocean systems — the planet's polar marine environments — play disproportionately critical roles in global ocean circulation, climate regulation, and marine biodiversity. The Arctic Ocean (~14.06

polar ocean Arctic Ocean Southern Ocean sea ice ice sheet thermohaline circulation
ZF_1_08 Verified Oceanography

ZF_1_08 — Submarine Volcanism and Island Formation

Submarine volcanism — volcanic activity occurring beneath the ocean surface — accounts for approximately 75% of the Earth's total volcanic output and is the primary mechanism by which new oceanic crust is created, island

submarine volcano island formation hotspot volcanism volcanic island arc Surtsey Hunga Tonga
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
Z_5_08 Verified Molecular Biology

Z_5_08 — Mitochondrial DNA: Maternal Inheritance, Ancient Lineages, and Disease

Mitochondrial DNA (mtDNA) — the small, circular genome (~16,569 base pairs in humans) contained within mitochondria — encodes 37 genes essential for oxidative phosphorylation (13 protein-coding genes, 22 transfer RNAs, 2

mitochondrial DNA mtDNA maternal inheritance mitochondrial Eve heteroplasmy oxidative phosphorylation
Z_2_11 Verified Molecular Biology

Z_2_11 — Genetics of Immunity and MHC Diversity

The major histocompatibility complex (MHC) — known as the human leukocyte antigen (HLA) system in humans — is the most polymorphic gene region in the human genome, encoding cell-surface glycoproteins essential for adapti

major histocompatibility complex MHC HLA human leukocyte antigen adaptive immunity antigen presentation
Z_4_18 Verified Molecular Biology

Z_4_18 — Protein Misfolding and Prion Diseases

Prion diseases — transmissible spongiform encephalopathies (TSEs) — are fatal neurodegenerative disorders caused by the misfolding and self-propagating aggregation of a normal cellular protein (PrPᶜ) into a pathological

prion protein-misfolding amyloid bse cjd mad-cow-disease
E_2_22 Verified Cataclysms & Chronology

E_2_22 — Dansgaard-Oeschger Events: Rapid Climate Oscillations of the Last Ice Age

Dansgaard-Oeschger (D-O) events are rapid climate oscillations that occurred during the last glacial period (~120,000–11,700 years BP), characterized by abrupt warmings of 8–16°C over Greenland within decades (as few as

Dansgaard-Oeschger events D-O events abrupt climate change ice core Greenland stadial
E_4_21 Verified Cataclysms & Chronology

E_4_21 — Oxygen Isotope Stages: Marine Isotope Record and Climate Cycles

The marine oxygen isotope record — constructed from measurements of the ratio of oxygen-18 to oxygen-16 (δ¹⁸O) in the calcium carbonate (CaCO₃) shells of foraminifera (single-celled marine organisms) preserved in deep-se

oxygen isotope δ18O marine isotope stage MIS benthic foraminifera planktonic