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.

85 results for "isotope dating" — page 3 of 5

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
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_1_04 Verified Oceanography

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

paleoceanography ice age Milankovitch cycles foraminifera oxygen isotope ocean carbon pump
E_3_15 Verified Cataclysms & Chronology

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

sea level eustatic LGM Last Glacial Maximum post-glacial transgression
E_3_11 Verified Cataclysms & Chronology

E_3_11 — Earthquake Archaeology and Seismic Catastrophes

Archaeoseismology — the study of past earthquakes using archaeological evidence — reveals that seismic catastrophes have repeatedly destroyed, reshaped, and sometimes permanently ended ancient urban centers and entire ci

archaeoseismology earthquake seismic destruction ancient earthquake Troy Jericho
E_3_10 Credible Cataclysms & Chronology

E_3_10 — Clathrate Gun Hypothesis

The clathrate gun hypothesis proposes that warming of ocean waters or thawing of permafrost can destabilize methane clathrates (also called methane hydrates) — ice-like crystalline structures in which methane molecules a

clathrate gun methane hydrate gas hydrate methane release abrupt warming continental shelf
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_03 Verified Cataclysms & Chronology

E_2_03 — Santorini/Thera Eruption and Minoan Collapse

Around 1600 BCE (revised range: 1628–1600 BCE), the volcanic island of Thera (modern Santorini) in the southern Aegean Sea experienced one of the largest volcanic eruptions in recorded human history — a VEI-7 event that

Santorini Thera Minoan eruption VEI-7 Akrotiri
E_2_19 Verified Cataclysms & Chronology

E_2_19 — Volcanism and Human Evolution: Eruptions That Shaped Our Species

The relationship between volcanism and human evolution operates on multiple scales and through multiple mechanisms — from the geological forces that created the landscapes where hominins evolved, to the catastrophic erup

volcanism human evolution Toba volcanic winter bottleneck tephra
E_4_13 Verified Cataclysms & Chronology

E_4_13 — Milankovitch Cycles and Orbital Forcing

Milankovitch cycles are periodic variations in Earth's orbital geometry that modulate the distribution and intensity of solar radiation reaching Earth's surface, driving the glacial-interglacial cycles that have dominate

Milankovitch cycles orbital forcing eccentricity obliquity precession ice age
E_4_00 Cataclysms & Chronology

E_4_00 — Dating Chronological Science: Subfolder Summary

E_4_02 Credible Cataclysms & Chronology

E_4_02 — Radiocarbon Calibration & Chronology Shifts

This document examines Radiocarbon Calibration & Chronology Shifts, a topic within the Cataclysms and Chronology research area. Key areas of investigation include The Physics , Key Parameters, What Can Be Dated. Notable

radiocarbon C-14 IntCal20 dendrochronology Hallstatt Plateau reservoir effect
E_1_03 Credible Cataclysms & Chronology

E_1_03 — Moon Formation & Artificial Moon Theory

This document examines Moon Formation & Artificial Moon Theory, a topic within the Cataclysms and Chronology research area. Key areas of investigation include The "Ringing Like a Bell" Phenomenon, Low Density and Mass Di

Moon Theia giant impact hollow moon isotope ratios Apollo
G_4_10 Verified Modern Frameworks

G_4_10 — Paleoclimatology Methods: Proxies, Models, and Reconstruction

Paleoclimatology reconstructs Earth's climate history using natural archives—physical, chemical, and biological proxies preserved in geological and biological materials. Speleothems (cave formations) record precipitation

paleoclimatology climate proxies speleothems pollen analysis palynology foraminifera
G_1_14 Verified Modern Frameworks

G_1_14 — Archaeometry — Physical Science Methods in Archaeology

Archaeometry — the application of physical and chemical science methods to archaeological materials — encompasses a broad range of analytical techniques used to determine the composition, provenance, manufacturing techno

archaeometry XRF NAA ICP-MS Raman FTIR
G_2_10 Verified Modern Frameworks

G_2_10 — Zooarchaeology — Animal Bones as Cultural Evidence

Zooarchaeology (also called archaeozoology) is the study of animal remains — primarily bones, teeth, antler, horn, and shell — recovered from archaeological sites, to reconstruct past human-animal relationships, includin

zooarchaeology faunal analysis animal bone archaeozoology taphonomy butchery
G_2_17 Verified Modern Frameworks

G_2_17 — Biogeochemistry and Ancient Environmental Reconstruction

Biogeochemistry — the study of chemical, physical, geological, and biological processes that govern the composition and cycling of elements and compounds in natural environments — provides essential tools for reconstruct

biogeochemistry paleoenvironment proxy isotope sediment core pollen
O_3_07 Verified Earth Anomalies

O_3_07 — Coral Reefs as Ancient Climate Archives

Coral skeletons serve as high-resolution natural archives of past ocean and climate conditions, recording temperature, salinity, ocean chemistry, and volcanic events in their calcium carbonate growth bands — much like tr

coral paleoclimate Porites Sr/Ca δ¹⁸O sea surface temperature PAGES 2k