Archaeology / Stable Isotope Paleodiet (δ13C & δ15N)
FREE TO EXPLORE
LABORATORY 14 · ARCHAEOLOGY

Paleodietary Reconstruction: Collagen Stable Isotopes (δ13C & δ15N Mass Spectrometry)

Reconstruct prehistoric human and faunal dietary trophic levels and marine vs C3/C4 terrestrial plant intake using collagen stable isotope ratio mass spectrometry. Explore interactive archaeometric simulation, survey geophysics, and material science analysis.

FIELD SURVEY · GEOPHYSICS · ARCHAEOMETRY · CERAMICS · BIOARCHAEOLOGY · GEOARCHAEOLOGY

Your virtual archaeology laboratory.

BONE COLLAGEN STABLE NITROGEN ISOTOPE RATIO Δ15N—
CALIBRATED FIELD TELEMETRY

Ready to sample with Carbon Isotope Ratio δ13C = -18.0 ‰ VPDB.

-18.0 ‰ VPDB
Standardized archaeometric baseline calibration protocol.

Adjust Carbon Isotope Ratio δ13C, then execute archaeometric acquisition.

Archaeometric measurements are captured using calibrated digital transducers and 64-bit IEEE 754 floating-point logging under controlled conditions. Residuals reflect ordinary least-squares regression across successive observations. Continuous data structures support comprehensive archaeological, geophysical, and geochemical evaluation.

Archaeological continuum and boundary limits

All artifact specimens, stratigraphic units, and geochemical matrices are evaluated under standardized laboratory protocols. Linear constitutive models reflect small-strain mechanics, ideal radioactive decay kinetics, and standard geochemical fractionation limits.

Laboratory apparatus & testing equipment.

Stable Isotope Paleodiet (δ13C & δ15N) Workstation & Field Sensor Rig

Provides rigid calibrated mounting, standardized environmental control, and precise positioning for c3 vs c4 photosynthetic pathways, marine protein enrichment, trophic level nitrogen fractionation (~3–5‰).

Calibrated Digital Archaeometric Transducer & Sensor Head

Quantifies physical, chemical, or optical responses with high baseline sensitivity and ±0.05% measurement accuracy.

Multi-Channel Digital Telemetry Data Logger (Class 0.2)

Samples resistance, potential, magnetic flux, optical absorbance, and temperature at 1 kHz with 24-bit resolution.

Precision Specimen Preparation & Thin-Section Polishing Rig

Prepares microscopic petrographic sections, resin-embedded blocks, or powder samples under controlled thickness (30 μm).

Certified Archaeological & Geological Reference Standards Set

Provides verified isotopic, elemental, or dimensional benchmarks before establishing carbon isotope ratio δ13c setpoints.

Grounded Shielded Instrumentation Leads & Environmental Enclosure

Eliminates stray electromagnetic interference, electrostatic charge drift, and thermal fluctuations in field laboratories.

FOLLOW THE METHOD

A reason behind every step.

Reconstruct prehistoric human and faunal dietary trophic levels and marine vs C3/C4 terrestrial plant intake using collagen stable isotope ratio mass spectrometry. Standardized parameter settings: -22.0, -20.0, -18.0, -16.0, -14.0, -12.0 ‰ VPDB.

  1. Apparatus Calibration & Baseline Standard Verification: Inspect all optical, electrical, and radiometric sensors. Verify instrument calibration against certified reference materials and perform electronic zero tare.
  2. Specimen Conditioning & Matrix Preparation: Clean, dry, or prepare the archaeological sample according to standardized micro-analytical protocols to eliminate modern surface contamination.
  3. Sensor Alignment & Baseline Datum Acquisition: Mount the specimen securely within the sensor housing or establish spatial grid coordinates. Verify alignment of the carbon isotope ratio δ13c with primary excavation datum.
  4. Systematic Parameter Variation & Acquisition: Increment the carbon isotope ratio δ13c systematically across the designated domain (-22.0 to -12.0 ‰ VPDB), permitting full signal equilibration at each measurement station.
  5. Multi-Channel Telemetry Recording & Signal Integration: Record the primary dependent variable (Bone Collagen Stable Nitrogen Isotope Ratio δ15N) alongside auxiliary environmental monitors. Validate signal stability and confirm low noise thresholds.
  6. Post-Test Verification & Digital Archive Export: Cycle the sensor through a verification standard to confirm zero baseline drift, de-energize primary drives, and export all digital telemetry observations to the persistent laboratory database.
YOUR NOTEBOOK · 0 OBSERVATIONS

Turn measurements into archaeological insight.

See a complete example report ↗

Points are your recorded observations. The solid regression line validates Stable Isotope Paleodiet (δ13C & δ15N) mathematical scaling.

LINEAR REGRESSION FIT · y = mx + b
δ15N = 0.5500 · δ13C + 21.2000
#Bone Collagen Stable Carbon Isotope Ratio δ13C (‰ VPDB)Bone Collagen Stable Nitrogen Isotope Ratio δ15N (‰ AIR)Carbon isotope ratio δ13C (‰ VPDB)Nitrogen isotope ratio δ15N (‰ AIR)

No readings yet. Execute an archaeometric trial and record it.

CHECK YOUR UNDERSTANDING

Explain what the archaeological metrics mean.

Question 1: In the experimental study of Stable Isotope Paleodiet (δ13C & δ15N), the primary dependent variable measured is:

Question 2: The governing mathematical constitutive equation for Stable Isotope Paleodiet (δ13C & δ15N) is modeled as:

Question 3: The target benchmark parameter derived from regression analysis is:

Question 4: Why is sample pre-treatment essential in archaeological laboratory analysis?

THEORY AND STRATIGRAPHIC CONTEXT

Archaeology background & physical principles.

Reconstruct prehistoric human and faunal dietary trophic levels and marine vs C3/C4 terrestrial plant intake using collagen stable isotope ratio mass spectrometry.

δ15N = 0.5500 · δ13C + 21.2000

Archaeological science principles build upon nuclear physics, geophysics, mineralogy, organic geochemistry, and biological skeletal anthropology.