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131 results for "carbon isotope excursion" — page 1 of 7

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
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
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
G_1_04 Verified Modern Frameworks

G_1_04 — Isotope Analysis and Provenance Studies

Isotope analysis — the measurement of ratios of stable or radiogenic isotopes preserved in human bone, tooth enamel, animal remains, ceramics, metals, and organic residues — has become one of the most powerful tools in m

isotope analysis stable isotopes strontium isotopes oxygen isotopes carbon isotopes nitrogen isotopes
G_1_07 Verified Modern Frameworks

G_1_07 — Stable Isotope Analysis and Ancient Diets

Stable isotope analysis of human and animal remains — primarily the measurement of carbon ($\delta^{13}$C), nitrogen ($\delta^{15}$N), and sulfur ($\delta^{34}$S) isotope ratios in bone collagen, tooth enamel, hair kerat

stable isotopes carbon isotopes nitrogen isotopes sulfur isotopes paleodiet diet reconstruction
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
Q_3_16 Verified Cosmology & Physics

Q_3_16 — Cosmochemistry: Meteorite Analysis, Presolar Grains, and Solar Composition

Cosmochemistry is the study of the chemical composition of the universe and the processes that produced it, with a primary focus on the analysis of meteorites — extraterrestrial rocks that survive passage through Earth's

cosmochemistry meteorite chondrite achondrite iron meteorite carbonaceous chondrite
G_4_09 Modern Frameworks

G_4_09 — Bioarchaeology and Forensic Anthropology: Reading the Dead

Bioarchaeology—the study of human remains from archaeological contexts—transforms skeletons from anonymous objects into biographical records of individual lives. Through stable isotope analysis of bone and tooth enamel,

bioarchaeology isotope analysis strontium carbon isotopes nitrogen isotopes oxygen isotopes
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_09 Verified Oceanography

ZF_4_09 — Seagrass and Coastal Carbon Sequestration (Blue Carbon)

Blue carbon refers to the carbon captured and stored by coastal and marine ecosystems — primarily seagrass meadows, mangrove forests, and salt marshes — which sequester carbon at rates per unit area far exceeding terrest

blue carbon seagrass Posidonia eelgrass Zostera coastal carbon
ZF_1_04 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_4_19 Verified Cataclysms & Chronology

E_4_19 — Mono Lake and Gothenburg Excursions: Short Geomagnetic Events

Geomagnetic excursions are brief, extreme departures of the Earth's magnetic field from its normal dipolar configuration — events during which the virtual geomagnetic pole (VGP) deviates by more than 40–45° from the geog

geomagnetic excursion Mono Lake Gothenburg Laschamp paleomagnetic virtual geomagnetic pole
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
G_1_09 Verified Modern Frameworks

G_1_09 — Provenance Analysis: Strontium, Lead, and Oxygen Isotope Sourcing

Isotopic provenance analysis has revolutionized archaeology by enabling researchers to determine where an artifact was made, where a person grew up, what they ate, and how far they traveled — all from the chemical signat

provenance isotope strontium lead oxygen sourcing
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
S_3_16 Verified Future Technology

S_3_16 — Direct Air Carbon Capture: Technology, Thermodynamics, and Climate Deployment

Direct Air Capture (DAC) — the technological extraction of CO₂ directly from ambient atmospheric air (currently at ~424 ppm, or 0.042%) — represents one of the most critical and technically challenging negative emissions

direct air capture DAC carbon capture negative emissions Climeworks Carbon Engineering
E_4_03 Cataclysms & Chronology

E_4_03 — Paleomagnetism & Geomagnetic Excursions

Earth's magnetic field periodically undergoes dramatic excursions and full polarity reversals, with profound physical consequences including weakened radiation shielding, increased UV exposure, and ozone depletion. The L

paleomagnetism Laschamp Mono Lake Gothenburg geomagnetic excursion Cooper Adams Event
E_4_02 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

TH_05 — The Water-Carbon-Chirality Triple Lock

water carbon chirality fine-structure constant α electron mass