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.

135 results for "marine sediment" — page 7 of 7

ZF_5_07 Verified Oceanography

ZF_5_07 — Upwelling Systems: Coastal Productivity and Fisheries Foundations

Upwelling — the wind-driven or current-driven ascent of cold, nutrient-rich deep water to the sunlit surface layer — is the foundation of the ocean's most productive ecosystems and the world's most valuable fisheries. Th

upwelling coastal upwelling Ekman transport wind-driven eastern boundary current nutrient enrichment
ZF_5_17 Verified Oceanography

ZF_5_17 — Oil Spill Ecotoxicology: Environmental Fate, Biological Effects, and Ecosystem Recovery

Oil spills — the release of petroleum hydrocarbons into marine and coastal environments — represent among the most visible and ecologically damaging forms of anthropogenic pollution, triggering toxic effects across multi

oil spill ecotoxicology Deepwater Horizon Exxon Valdez PAH polycyclic aromatic hydrocarbons
ZF_4_07 Verified Oceanography

ZF_4_07 — Deep Ocean Mining and Mineral Resources

Deep-sea mining — the extraction of mineral resources from the ocean floor at depths of 200–6,000 m — is one of the most consequential and contested environmental issues in contemporary oceanography. Three primary resour

deep-sea mining polymetallic nodules manganese nodules seafloor massive sulfides cobalt-rich crusts ISA
ZF_4_00 Oceanography

ZF_4_00 — Ocean Chemistry Climate: Subfolder Summary

ZF_4_12 Verified Oceanography

ZF_4_12 — Underwater Acoustics and the SOFAR Channel

Sound is the dominant long-range information carrier in the ocean — electromagnetic radiation (light, radio) is rapidly absorbed in seawater, but sound can travel thousands of kilometers with remarkably little loss, maki

underwater acoustics SOFAR channel sound propagation deep sound channel sonar SOSUS
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_1_20 Verified Oceanography

ZF_1_20 — Ocean Stratification

Ocean stratification — the formation of stable density layers in the water column due to gradients in temperature, salinity, and pressure — is one of the most fundamental physical characteristics of the global ocean and

ocean stratification thermocline pycnocline halocline density gradient mixed layer
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_18 Verified Oceanography

ZF_1_18 — Mesopelagic Zone Ecology

The mesopelagic zone (200–1,000 m depth) — the ocean's "twilight zone" — is emerging as one of the most ecologically and biogeochemically important yet poorly understood habitats on Earth. [KEY FINDING] Despite receiving

mesopelagic twilight-zone diel-vertical-migration biological-carbon-pump deep-scattering-layer micronekton
E_1_13 Credible Cataclysms & Chronology

E_1_13 — Cosmic Impact Markers: Nanodiamonds, Microspherules, Platinum

Cosmic impact markers are distinctive mineralogical, geochemical, and textural features preserved in geological strata that provide evidence for extraterrestrial impact events — including asteroid/comet impacts and airbu

impact marker nanodiamond microspherule platinum iridium cosmic spherule
E_5_05 Verified Cataclysms & Chronology

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

mass extinction Devonian Kellwasser Hangenberg reef collapse anoxia
ZB_3_14 Verified Ecology & Biology

ZB_3_14 — Kelp Forests and Seagrass Meadows: Underwater Gardens of Productivity

Kelp forests and seagrass meadows are the two major groups of marine macrophyte-dominated ecosystems — structurally complex, highly productive underwater habitats that provide essential services including nursery habitat

kelp forest seagrass macroalgae blue carbon urchin barren trophic cascade
ZB_3_13 Verified Ecology & Biology

ZB_3_13 — Estuary and Mangrove Ecology: Where Rivers Meet the Sea

Estuaries — semi-enclosed coastal water bodies where freshwater river discharge meets and mixes with saline ocean water — and mangrove forests — tropical and subtropical intertidal forests dominated by salt-tolerant tree

estuary mangrove salt marsh salinity gradient nursery habitat blue carbon
O_2_15 Verified Earth Anomalies

O_2_15 — Moeraki Boulders & Septarian Concretions

The Moeraki Boulders (Te Kaihinaki in Māori) are a group of approximately 50 large, near-spherical septarian concretions exposed on Koekohe Beach, near Moeraki on the Otago coast of New Zealand's South Island. Ranging fr

Moeraki Boulders septarian concretion spheroidal weathering diagenesis mudstone calcite
O_3_16 Verified Earth Anomalies

O_3_16 — Underwater Anomaly Catalog

Underwater anomalies range from confirmed submerged archaeological sites (Pavlopetri, Dwarka, Heracleion) to ambiguous geological/archaeological features (Yonaguni, Bimini Road, Baltic Sea Anomaly) to outright unexplaine

underwater-anomaly-catalog baltic-sea-anomaly bimini-road yonaguni submerged-structures uso