RESEARCH BASE
Search 3,721 documents across 34 fields — every claim tier-rated by evidence
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.
3,692 results for "G protein" — page 27 of 185
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
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
ZF_4_09 — Seagrass and Coastal Carbon Sequestration (Blue Carbon)
Blue carbon refers to the carbon captured and stored by coastal and marine ecosystems — primarily seagrass meadows, mangrove forests, and salt marshes — which sequester carbon at rates per unit area far exceeding terrest
ZF_1_12 — El Niño and ENSO: Pacific Oscillation and Global Climate Impact
The El Niño–Southern Oscillation (ENSO) is the most powerful year-to-year climate fluctuation on Earth — a coupled ocean-atmosphere phenomenon centered in the tropical Pacific that affects weather patterns, agriculture,
ZF_1_13 — Continental Shelves: Submerged Geography and Ice Age Coastlines
Continental shelves — the shallow, gently sloping underwater extensions of continental landmasses — represent some of the most biologically productive, economically valuable, and archaeologically significant terrain on E
ZF_1_14 — Ocean-Atmosphere Coupling: Heat Exchange, Evaporation, and Weather
The ocean-atmosphere interface — the boundary between Earth's two great fluid envelopes — is the planet's most important energy exchange surface. The ocean absorbs approximately 93% of the excess heat trapped by anthropo
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
ZF_1_02 — Tidal Science: Lunar Cycles, Tidal Locking, and Tidal Energy
Tides — the rhythmic rise and fall of ocean surfaces — are among the most predictable natural phenomena on Earth, driven primarily by the gravitational attraction of the Moon (accounting for ~68% of tidal forcing) and th
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
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
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
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
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
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
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
ZF_1_16 — Paleoceanography and Foraminifera: Reconstructing Ancient Oceans from Microfossil Archives
Paleoceanography — the study of the history of the oceans and their role in Earth's climate system through geological time — relies fundamentally on the geochemical analysis of foraminifera (single-celled protists with c
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
Z_5_12 — Splicing: RNA Processing and Alternative Splicing
RNA splicing — the process by which intervening sequences (introns) are removed from precursor messenger RNA (pre-mRNA) and the remaining sequences (exons) are joined together to form the mature mRNA — is a fundamental s
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
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
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