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.

8 results for "CO2 degassing"

O_3_09 Verified Earth Anomalies

O_3_09 — Lake Anomalies and Limnic Eruptions

Limnic eruptions (also called "lake overturns") are rare but catastrophic events in which dissolved carbon dioxide (CO₂) erupts suddenly from deep lake water, forming a dense gas cloud that displaces oxygen and can asphy

limnic eruption Lake Nyos Lake Kivu meromixis meromictic lake CO2 degassing
E_5_03 Verified Cataclysms & Chronology

E_5_03 — The End-Triassic Mass Extinction

The End-Triassic mass extinction (c. 201.564 ± 0.015 million years ago) was one of the "Big Five" mass extinctions in Earth's history, eliminating approximately 76% of all species and ~50% of genera, clearing the ecologi

End-Triassic Triassic-Jurassic mass extinction CAMP Central Atlantic Magmatic Province CO2
ZF_4_01 Verified 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_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
E_2_04 Verified Cataclysms & Chronology

E_2_04 — Permian-Triassic Great Dying — The Biggest Mass Extinction

Approximately 252 million years ago, at the boundary between the Permian and Triassic periods, Earth experienced the worst mass extinction in its entire history — an event so devastating it has been called "The Great Dyi

Permian Triassic Great Dying mass extinction Siberian Traps volcanism
O_5_05 Verified Earth Anomalies

O_5_05 — Ice Ages and Milankovitch Cycles: Orbital Forcing of Climate

Ice ages — periods when massive continental ice sheets expand to cover large portions of Earth's surface — are among the most dramatic climate events in the planet's history. The Quaternary glaciation (beginning ~2.6 mil

ice age glacial interglacial Milankovitch orbital eccentricity
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
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