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.
25 results for "Holocene flooding" — page 1 of 2
M_5_23 — Post-Glacial Flooding and Submerged Archaeological Landscapes
Between the Last Glacial Maximum (LGM, c. 26,500–19,000 years ago) and approximately 6,000 years ago, global mean sea level rose by approximately 120–130 m, drowning continental shelves that had been habitable land. The
M_4_16 — Sundaland & Southeast Asian Lost Continent Hypothesis
Sundaland is the geological term for the exposed continental shelf of Southeast Asia that connected the present-day islands of Borneo, Java, Sumatra, and the Malay Peninsula into a single landmass during the Last Glacial
M_1_17 — Underwater City Discoveries (Dwarka, Yonaguni, Pavlopetri)
The discovery and investigation of submerged archaeological sites — cities, harbors, temples, and infrastructure now lying beneath coastal waters due to post-glacial sea level rise, tectonic subsidence, or local geologic
ZF_3_01 — Sea-Level History: Glacial Cycles, Meltwater Pulses, and Coastal Archaeology
Sea level has varied by over 120 meters between glacial and interglacial periods, repeatedly reshaping coastlines, exposing and flooding continental shelves, and creating or destroying land bridges that directed human mi
E_4_11 — The Holocene Climate Optimum and Mid-Holocene Transition
The Holocene Climate Optimum (also called the Holocene Thermal Maximum or Hypsithermal) designates a prolonged warm interval roughly spanning 9,000–5,000 years before present, during which Northern Hemisphere summer temp
D_2_21 — Black Sea Deluge: Archaeological Evidence for Rapid Flooding
The Black Sea Deluge Hypothesis proposes that the Black Sea — now a large saline body connected to the Mediterranean via the Bosporus Strait — was once a significantly smaller, lower freshwater lake during the Last Glaci
E_5_06 — Holocene Sixth Mass Extinction: Current Biodiversity Crisis
The Holocene "Sixth Mass Extinction" hypothesis holds that current species loss rates are 100–1,000 times the normal background extinction rate, driven primarily by human activity: habitat destruction, overexploitation,
Y_4_15 — Sensory Overload and Information Flooding: Excess as Altered State
Sensory overload — the state that arises when sensory input exceeds the brain's capacity for orderly processing — represents the mirror image of sensory deprivation as a pathway to altered consciousness. While deprivatio
F_4_26 — The Green Sahara: African Humid Period Civilizations
The "Green Sahara" — also known as the African Humid Period (AHP) — refers to a period of profound climatic transformation that turned the Sahara Desert into a lush, habitable landscape of grasslands, lakes, rivers, and
M_4_11 — Göbekli Tepe Climate Reconstruction: What Supported Its Builders?
Göbekli Tepe (~9600-8000 BCE), the monumental stone pillar sanctuary in southeastern Turkey, presents a fundamental puzzle: how did pre-agricultural hunter-gatherers — people who had not yet domesticated crops or animals
ZF_5_08 — Coastal Geomorphology: Erosion, Beaches, and Barrier Islands
Coastal geomorphology is the study of landforms at the interface of land and sea — a dynamic zone shaped by the constant interaction of waves, tides, currents, wind, rivers, geology, biology, and increasingly by human ac
E_3_15 — Sea-Level Curves: Eustatic Change from LGM to Present
Sea-level curves — graphical reconstructions of how global mean sea level has changed through time — represent one of the most important datasets in Quaternary science, recording the waxing and waning of continental ice
E_3_04 — Doggerland and Sundaland — Drowned Continental Shelves
Doggerland and Sundaland represent two of the most significant landmasses lost to post-glacial sea level rise, together encompassing hundreds of thousands of square kilometers of habitable terrain that was progressively
E_3_13 — Storegga Slide: Mega-Tsunami and Mesolithic Europe
The Storegga Slide (Norwegian: Storegga-raset; Store = "great," egga = "edge") — a series of submarine landslides on the continental slope off western Norway at approximately 64°N — constitutes one of the largest known m
E_3_06 — The 8.2 Kiloyear Event: Sudden Cooling and Neolithic Disruption
The 8.2 kiloyear event (~6200 BCE) was the most severe abrupt climate oscillation of the Holocene, triggered by a catastrophic outburst flood from glacial Lakes Agassiz and Ojibway into the North Atlantic via Hudson Bay.
E_2_07 — The 4.2 Kiloyear Event — Bronze Age Climate Catastrophe
The 4.2 kiloyear event (~2200 BCE) was a severe, century-scale aridification episode that constitutes one of the most significant abrupt climate changes of the Holocene. Identified through speleothem, marine sediment, an
E_4_17 — Palynology: Pollen Records and Vegetation History
Palynology — the study of pollen grains and spores (and other organic-walled microfossils collectively termed palynomorphs) — is one of the most widely applied techniques in Quaternary science, archaeology, and paleoclim
E_4_24 — Quaternary Science: Integrating Ice Ages, Extinctions, and Migrations
Quaternary science is the interdisciplinary study of Earth's most recent geological period — the Quaternary (2.58 Ma to present), encompassing the Pleistocene (2.58 Ma to 11,700 BP) and the Holocene (11,700 BP to present
E_4_22 — Varve Chronology: Annual Lake Sediment Records
Varve chronology is a dating and paleoclimate method based on counting and analyzing varves — annually laminated sediment layers deposited in lakes (and occasionally in marine or estuarine settings). Each varve typically
ZB_5_19 — The Anthropocene: Human Dominance of Earth Systems and Epoch Dating
The Anthropocene — a proposed geological epoch defined by the dominant influence of human activity on Earth's geology, climate, and ecosystems — has become one of the most consequential and contentious concepts in modern
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