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10 results for "strontium isotopes"
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,
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
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
ZF_1_16 — Paleoceanography and Foraminifera: Reconstructing Ancient Oceans from Microfossil Archives
Paleoceanography — the study of the history of the oceans and their role in Earth's climate system through geological time — relies fundamentally on the geochemical analysis of foraminifera (single-celled protists with c
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
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
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
R_1_09 — The Great Oxidation Event: Oxygen, Cyanobacteria, and Earth's Atmospheric Transformation
The Great Oxidation Event (GOE), occurring approximately 2.4–2.1 billion years ago during the Paleoproterozoic, was the most dramatic chemical transformation in Earth's history — atmospheric oxygen rose from trace levels
F_2_06 — Tin Sources and the Bronze Age Mystery
The Bronze Age (c. 3300–1200 BCE) depended fundamentally on tin — the scarce metal alloyed with copper to produce bronze (typically 88–92% copper, 8–12% tin). While copper was widely available across the Mediterranean, N
ZA_5_08 — Atomic Clocks: The Most Precise Instruments Ever Built
Atomic clocks — timekeeping devices that use the invariant frequencies of atomic transitions as their oscillation reference — are the most precise measuring instruments ever constructed, achieving fractional frequency un
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