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4 results for "U-Th"

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
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
E_1_15 Verified Cataclysms & Chronology

E_1_15 — Uranium-Thorium Dating: Methodology and Applications in Deep Time

Uranium-thorium (U-Th) dating, also called uranium-series disequilibrium dating, is a radiometric technique that measures the decay of ²³⁴U to ²³⁰Th (half-life: ~245,620 years) in materials such as speleothems (cave form

uranium-thorium-dating U-Th radiometric-dating speleothem coral-dating uranium-series
O_3_07 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