Human Earth LabPeople · Soil · Landscapes · Time
Tell, destruction and hidden stratigraphy

Tel Burna

Tel Burna in the southern Levant shows how archaeological layers can be read even where they are not macroscopically visible. Geochemistry, pOSL and biomolecular analysis distinguish floors, mudbrick, destruction horizons and post-depositional change.

Tel Burna map and reconstruction
Regional location of Tel Burna and reconstruction of the fortified settlement in the Shephelah.
WhereShephelah, Israel
Site typemulti-period tell
ChronologyBronze Age to Iron Age
AreaArea G, gate and fortifications
MethodspXRF, pOSL, ORA, DNA

What we study here

Tel Burna is a model case for contexts where stratigraphy is unclear but its record remains preserved in chemistry, luminescence and biomolecular content.

1 / Stratigraphy

Layers without clear boundaries

Analyses help distinguish construction, destruction and post-depositional phases.

2 / Material

Mudbrick and chalk floors

Potassium points to mudbrick architecture, while high Ca reflects chalk and carbonate floors.

3 / Processes

Erosion and degradation

pOSL, lipids and DNA indicate preservation, erosion and organic degradation.

How to read invisible layers

Area G combines three main geochemical signals: P, Ca and K.

P

Activity and destruction

Phosphorus indicates occupation horizons, waste, burning and destruction sediments.

Ca

Chalk-based floors

High Ca corresponds to chalk or carbonate floors, especially in Strata II and III.

K

Mudbrick and architectural collapse

Potassium is the main proxy for mudbrick and collapsed earthen architecture.

Geoarchaeology 2025

Geoarchaeology in the Absence of Layers

Large-Scale Sampling From an Iron Age Urban Context in the Southern Levant

The study integrates pXRF, pOSL, organic residue analysis and DNA to reconstruct Area G where visible layers are ambiguous due to erosion and post-depositional processes.

pXRFpOSLIRSLORADNAP / Ca / Kmudbrick

Figures and analytical layers

From regional context to Area G stratigraphy, geochemistry, luminescence and biomolecular signals.

Map and reconstruction
Regional position and reconstruction.
Harris Matrix
Harris Matrix of the main strata.
Area G
Area G with sampled contexts.
P Ca K profile
Depth profiles of P, Ca and K.
pOSL
pOSL and IRSL signals increase with depth.
Lipids and DNA
Lipids and DNA decrease with depth.