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212 results for "climate change" — page 2 of 11

M_4_11 Verified Forbidden Archaeology

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

Göbekli Tepe climate Younger Dryas early Holocene archaeobotany archaeozoology
C_5_28 Verified Global Traditions

C_5_28 — Ritual Sacrifice: Blood, Fire, and the Sacred Exchange

Ritual sacrifice — the deliberate destruction or offering of something valuable (animal, human, agricultural produce, wealth) to a divine or supernatural power — is one of the most universal and oldest documented human p

ritual sacrifice human sacrifice animal sacrifice scapegoat Aztec Inca
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_10 Verified Oceanography

ZF_4_10 — Coral as Climate Archive — Paleoceanographic Proxies

Coral paleoclimatology uses the geochemical and physical properties of coral skeletons as high-resolution archives of past ocean conditions — providing some of the most detailed tropical climate records available for the

coral proxy paleoclimate coral core Sr/Ca δ¹⁸O sea surface temperature
ZF_4_15 Verified Oceanography

ZF_4_15 — Ocean Sediments: Deep-Sea Cores, Proxy Records, and Paleoclimate

Ocean sediments are the Earth's most comprehensive climate archive — a continuous record of planetary conditions extending back over 200 million years, slowly accumulated grain by grain on the deep seafloor at rates of m

ocean sediments deep-sea core marine sediment paleoclimate proxy foraminiferal isotopes oxygen isotopes
ZF_4_14 Verified Oceanography

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

harmful algal bloom HAB red tide algal toxin eutrophication paralytic shellfish poisoning
E_3_19 Verified Cataclysms & Chronology

E_3_19 — Volcanic Aerosol Forcing and Historical Climate Disruption

Explosive volcanic eruptions inject sulfur dioxide (SO₂) into the stratosphere, where it converts to sulfate aerosol particles (H₂SO₄) that reflect incoming solar radiation and cool Earth's surface for 1–3 years. This pr

volcanic-aerosol climate-forcing sulfate-aerosol volcanic-winter tambora toba
E_2_20 Verified Cataclysms & Chronology

E_2_20 — Medieval Warm Period: Climate Optimum and Civilizational Flourishing

The Medieval Warm Period (MWP) — increasingly referred to in scientific literature as the Medieval Climate Anomaly (MCA) to emphasize its complex spatial patterns — was a period of relatively warm climatic conditions acr

Medieval Warm Period MWP Medieval Climate Anomaly MCA Little Ice Age climate optimum
E_2_04 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
E_4_21 Verified Cataclysms & Chronology

E_4_21 — Oxygen Isotope Stages: Marine Isotope Record and Climate Cycles

The marine oxygen isotope record — constructed from measurements of the ratio of oxygen-18 to oxygen-16 (δ¹⁸O) in the calcium carbonate (CaCO₃) shells of foraminifera (single-celled marine organisms) preserved in deep-se

oxygen isotope δ18O marine isotope stage MIS benthic foraminifera planktonic
E_4_10 Cataclysms & Chronology

E_4_10 — Ice Core Science: Greenland and Antarctic Climate Records

Ice cores drilled from the Greenland and Antarctic ice sheets constitute one of the most powerful archives of past climate on Earth. Greenland cores (GRIP, GISP2, NGRIP, NEEM) provide high-resolution records extending ba

ice cores GRIP GISP2 NGRIP EPICA Vostok
E_4_11 Cataclysms & Chronology

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

Holocene Thermal Maximum Holocene Climate Optimum Green Sahara African Humid Period Milankovitch obliquity
E_1_17 Verified Cataclysms & Chronology

E_1_17 — Toba Supereruption: Genetic Bottleneck and Climate Catastrophe

The Toba supereruption — occurring approximately 74,000 years ago (74 ka) on the island of Sumatra, Indonesia — was the largest volcanic eruption of the last 2 million years and one of the most catastrophic events in hum

Toba supereruption VEI-8 volcanic winter genetic bottleneck Homo sapiens
ZC_5_06 Verified Social Science

ZC_5_06 — Environmental Sociology: Risk, Justice, and Ecological Modernization

Environmental sociology studies the reciprocal relationships between human societies and their natural environments — how social structures, economic systems, political institutions, cultural beliefs, and power relations

environmental sociology environmental justice risk society ecological modernization treadmill of production Beck
ZC_2_17 Credible Social Science

ZC_2_17 — Institutional Change Theory: How Organizations, States, and Systems Transform

Institutional change theory — the study of how formal and informal rules, norms, and organizations originate, persist, transform, and collapse — is central to understanding political, economic, and social development. Th

institutional change Douglass North institutional economics path dependence critical junctures Acemoglu
O_4_05 Earth Anomalies

O_4_05 — Desertification, Green Sahara & Landscape Transformation

Between approximately 11,000 and 5,000 years BP, the Sahara — today the world's largest hot desert — was a green, well-watered landscape of lakes, rivers, and grasslands supporting hippopotami, crocodiles, fish, and larg

Green Sahara African Humid Period desertification Holocene Gobero orbital forcing
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
O_5_13 Verified Earth Anomalies

O_5_13 — Paleosols and Ancient Soils: Climate Records in Earth

Paleosols — ancient soils preserved in the geological record — are among the most valuable but often overlooked records of past environmental conditions. When soils are buried by subsequent sedimentation (flooding, volca

paleosol ancient soil pedogenesis climate proxy carbon isotope carbonates
R_5_02 Biology & Evolution

R_5_02 — Megafauna Extinction: Quaternary Losses and the Overkill Debate

Between ~50,000 and 10,000 years ago, Earth lost the majority of its large-bodied animals (megafauna >44 kg) — woolly mammoths, ground sloths, saber-toothed cats, giant wombats, moa, and dozens of other spectacular speci

megafauna extinction Pleistocene extinction Quaternary extinction overkill hypothesis climate change woolly mammoth
S_4_01 Future Technology

S_4_01 — Existential Risk Taxonomy

Existential risk (x-risk) refers to any event that could permanently curtail humanity's long-term potential — including extinction, civilizational collapse without recovery, or irreversible loss of value (e.g., permanent

existential risk x-risk global catastrophic risk GCR extinction Bostrom