RESEARCH BASE

Search 3,721 documents across 34 fields — every claim tier-rated by evidence

3,721 documents 34 sections 43,623 citations 34,854 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.

2,480 results for "Brú na Bóinne" — page 64 of 124

ZF_4_08 Verified Oceanography

ZF_4_08 — Ocean Acidification Paleoclimate Record

Ocean acidification — the decrease in seawater pH caused by absorption of atmospheric CO₂ — is not only a modern phenomenon but has occurred repeatedly throughout Earth's history, leaving distinctive signals in the geolo

ocean acidification pH paleoclimate PETM Paleocene-Eocene Thermal Maximum carbonate compensation depth
ZF_4_13 Verified Oceanography

ZF_4_13 — Ocean Noise Pollution: Anthropogenic Sound and Marine Life

Ocean noise pollution — the introduction of excessive or harmful human-generated sound into the marine environment — has emerged as one of the most pervasive and least visible threats to marine ecosystems. Sound travels

ocean noise pollution underwater noise anthropogenic sound marine acoustics shipping noise sonar
ZF_4_06 Verified Oceanography

ZF_4_06 — Ocean Remote Sensing and Satellite Oceanography

Satellite oceanography — the use of Earth-orbiting sensors to observe ocean properties from space — has transformed ocean science since the 1970s from a data-sparse field reliant on sparse ship transects to a globally co

satellite oceanography remote sensing altimetry TOPEX Jason Sentinel
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_18 Verified Oceanography

ZF_4_18 — Deep Ocean Microplastics

Deep ocean microplastics — synthetic polymer particles smaller than 5 mm that have infiltrated the deepest marine environments on Earth — represent one of the most alarming and poorly understood dimensions of global plas

microplastics nanoplastics deep sea ocean floor Mariana Trench sediment
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_05 Verified Oceanography

ZF_4_05 — Marine Pharmacology and Drug Discovery

Marine pharmacology explores the ocean's vast biodiversity as a source of bioactive compounds for drug development — a field that has yielded several approved drugs and thousands of promising leads since the pioneering w

marine pharmacology marine natural products drug discovery bioprospecting marine toxin cone snail
ZF_4_04 Verified Oceanography

ZF_4_04 — Ocean Acoustics and Sound Channels

Ocean acoustics — the study of sound propagation in the sea — is fundamental to marine science, military applications, and understanding marine life. Sound travels approximately 4.5× faster in seawater (~1,500 m/s) than

ocean acoustics SOFAR channel sound propagation underwater sound deep sound channel acoustic thermometry
ZF_4_01 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_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_01 Oceanography

ZF_1_01 — Physical Oceanography: Thermohaline Circulation, Currents, and ENSO

Physical oceanography studies the motion, properties, and dynamics of the global ocean — a system containing 97% of Earth's water, covering 71% of the surface, and storing over 90% of the excess heat from anthropogenic c

thermohaline circulation AMOC ENSO El Niño La Niña ocean currents
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_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_17 Credible Oceanography

ZF_1_17 — Abyssal Trench Biogeography

Hadal trenches — oceanic depressions exceeding 6,000 m depth, formed by tectonic subduction — represent Earth's deepest and least explored biomes, harboring unique ecosystems under extreme pressures (600–1,100 atm), perp

hadal-zone ocean-trenches abyssal-ecology deep-sea-biogeography barophiles piezophiles
ZF_1_03 Oceanography

ZF_1_03 — Seafloor Spreading, Plate Tectonics and Marine Geology

The discovery that the ocean floor is not ancient and static but young, dynamic, and continuously recycled revolutionized Earth science in the 20th century. Seafloor spreading — proposed by Harry Hess (1962) and confirme

seafloor spreading plate tectonics mid-ocean ridge subduction zone Mariana Trench seamount
ZF_1_07 Verified Oceanography

ZF_1_07 — Submarine Geology and Ocean Trenches

The submarine geology of the ocean floor encompasses a vast range of geological features — from abyssal plains (the flattest surfaces on Earth, at 3,000–6,000 m depth, covered by fine sediment) to mid-ocean ridges (the l

ocean trench submarine geology abyssal plain mid-ocean ridge subduction Mariana Trench
Z_5_10 Verified Molecular Biology

Z_5_10 — Genome Editing Beyond CRISPR: TALENs, Base Editors, Prime Editors, and Next-Generation Tools

While CRISPR-Cas9 (covered in Z_1_02) dominates the genome editing landscape, it is neither the first nor the only precision genome editing technology. The field began with zinc finger nucleases (ZFNs) in the early 2000s

genome editing TALENs zinc finger nucleases ZFN base editing prime editing
Z_5_20 Verified Molecular Biology

Z_5_20 — Proteomics: The Complete Protein Landscape of Life

Proteomics — the large-scale study of the complete protein complement (proteome) of a cell, tissue, or organism — emerged in the 1990s as the necessary counterpart to genomics. While the human genome contains ~20,000 pro

proteomics mass spectrometry protein expression protein-protein interactions post-translational modifications two-dimensional gel electrophoresis
Z_5_21 Verified Molecular Biology

Z_5_21 — Mobile Genetic Elements: Transposons, Retrotransposons, and Genomic Plasticity

Mobile genetic elements (MGEs) — DNA sequences capable of moving within and between genomes — constitute a staggering ~45% of the human genome, far exceeding the ~1.5% that encodes proteins. Discovered by Barbara McClint

transposons mobile genetic elements jumping genes retrotransposons barbara mcclintock LINE elements