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.

9 results for "greenhouse"

O_3_14 Verified Earth Anomalies

O_3_14 — Methane Seeps and Gas Hydrates: Ocean Floor Degassing

Methane seeps (also called "cold seeps") are locations on the ocean floor — particularly along continental margins, in subduction zones, and in deep basins — where methane (CH₄) bubbles or dissolved methane leaks from su

methane seep gas hydrate clathrate cold seep methane CH4
ZF_5_12 Verified Oceanography

ZF_5_12 — Paleocene-Eocene Thermal Maximum: Ancient Anoxic Ocean Crisis

The Paleocene-Eocene Thermal Maximum (PETM), occurring approximately 55.8 million years ago (latest Paleocene), was one of the most dramatic and rapid climate change events in the Cenozoic, offering the closest geologica

PETM Paleocene-Eocene Thermal Maximum hyperthermal carbon isotope excursion CIE ocean acidification
E_2_13 Verified Cataclysms & Chronology

E_2_13 — Paleocene-Eocene Thermal Maximum

The Paleocene-Eocene Thermal Maximum (PETM) — approximately 55.8 million years ago — was the most extreme rapid warming event of the past 66 million years and is widely studied as a deep-time analog for modern anthropoge

PETM Paleocene-Eocene Thermal Maximum hyperthermal carbon isotope excursion CIE methane clathrate
E_2_14 Verified Cataclysms & Chronology

E_2_14 — Deccan Traps and Large Igneous Provinces

Large Igneous Provinces (LIPs) are the most voluminous volcanic features on Earth: enormous outpourings of basalt lava and associated intrusions that cover areas of up to millions of square kilometers and release colossa

Deccan Traps large igneous province LIP flood basalt volcanism mass extinction
E_2_12 Verified Cataclysms & Chronology

E_2_12 — Great Oxygenation Event

The Great Oxygenation Event (GOE) — approximately 2.4–2.1 billion years ago — was one of the most transformative events in Earth's history: the first permanent rise of free molecular oxygen (O₂) in the atmosphere, from n

Great Oxygenation Event GOE oxygen crisis cyanobacteria photosynthesis Paleoproterozoic
E_2_15 Verified Cataclysms & Chronology

E_2_15 — Azolla Event and Eocene Arctic Cooling

The Azolla Event (c. 49 Ma, Middle Eocene) refers to a period of approximately 800,000 years during which the floating freshwater fern _Azolla_ bloomed prolifically across the semi-enclosed Arctic Ocean, sequestering mas

Azolla event Azolla fern Arctic Ocean Eocene carbon sequestration CO₂ drawdown
Q_3_14 Verified Cosmology & Physics

Q_3_14 — Planetary Science: Mars, Venus, and Comparative Planetology

Planetary science studies the formation, composition, atmospheres, surfaces, interiors, and evolution of planets, moons, and other bodies in our solar system and beyond. Comparative planetology — examining how planets wi

planetary science Mars Venus comparative planetology atmosphere climate
ZB_3_19 Verified Ecology & Biology

ZB_3_19 — Permafrost Methane

Permafrost — permanently frozen ground maintained at or below 0°C for at least two consecutive years — underlies approximately 22% of the Northern Hemisphere land surface (about 23 million km²), primarily across Siberia,

permafrost methane thermokarst clathrate greenhouse gas Arctic warming
S_4_20 Credible Future Technology

S_4_20 — Terraforming Technology

Terraforming — the hypothetical process of deliberately modifying a planet's atmosphere, temperature, surface topography, or ecology to make it habitable for Earth life — represents one of the most ambitious long-term en

terraforming Mars Venus planetary engineering atmosphere modification greenhouse gases