Open /app/sandbox/deep-time Needs Palaeo-GIS Workspace

Deep-Time Palaeo-GIS Explorer

The Deep-Time Palaeo-GIS Explorer is a specialised spatial reconstruction module for analyzing long-term environmental change, palaeoclimate shifts, hydrological transformations, and prehistoric human engagement with the landscape in the Dead Sea Basin and Southern Levant.

Spanning time horizons from the Last Glacial Maximum (20,000 BP) through the Pre-Pottery Neolithic (PPN) to the Middle Bronze Age (3,500 BP), the module enables researchers to reconstruct ancient lake shorelines (Lake Lisan), iso-hyet shifts, vegetation biomes, and prehistoric settlement distributions.

Access: The Deep-Time Palaeo-GIS module requires the Palaeo-GIS workspace unlock. Request access on your Account page.

When to use it


Anatomy of the interface

The Palaeo-GIS workspace integrates a Palaeo-Environmental Control Sidebar on the left with a 3D terrain-enabled Palaeo-Map Canvas on the right.

Deep-Time Palaeo-GIS Dead Sea basin spatial explorer interface with reference tags A1 to A5
Figure 1 — The Deep-Time Palaeo-GIS workspace.
TagControlWhat it does
A1Time Horizon & Epoch PickerSelect climate epoch: Last Glacial Maximum, Terminal Pleistocene, Early Holocene Pluvial, or Mid-Holocene Arid.
A2Hydrological ReconstructionSet Dead Sea / Lake Lisan water level ($-160\text{ m}$ to $-400\text{ m}$ MSL) and precipitation offset sliders ($+50%$ to $-30%$).
A3Archaeological FiltersToggle settlement distribution layers by period: Natufian, PPNA/PPNC, Ghassulian Chalcolithic, EB I-III, and MB II.
A4Palaeo Lake Lisan PolygonReconstructed water body extent corresponding to the selected lake level (e.g. $-290\text{ m}$ during the Early Holocene).
A5Archaeological Site MarkersGeoreferenced prehistoric settlement points with popups displaying site area (ha), radiocarbon dates, and material culture attributes.

Supported palaeo-climate epochs

Critical to this approach is the understanding that ancient landscapes were not static baselines. Considering as many environmental variables as possible — lake level, precipitation, and biome expansion — can only increase the credibility of any inferences drawn.

Climate EpochHorizonLake Lisan LevelRegional RainVegetation & Biome
Last Glacial Maximum (LGM)24,000 – 18,000 BP$-160\text{ m}$ (Highstand)$+60%$ vs presentSteppe / Conifer Woodland in Highlands
Terminal Pleistocene (Natufian)15,000 – 11,700 BP$-240\text{ m}$ (Regressing)$+30%$ vs presentOak-Pistacia Open Park Forest
Early Holocene Pluvial (PPN)11,700 – 8,200 BP$-290\text{ m}$ (Pluvial)$+40%$ vs presentMediterranean Evergreen Forest Expansion
Mid-Holocene Desiccation (EB)6,000 – 4,200 BP$-390\text{ m}$ (Desiccating)Present baselineMediterranean Scrub / Desert Steppe

Walkthrough: Reconstructing the Early Holocene Pluvial

Follow these steps to conduct a palaeo-environmental reconstruction:

1. Select the Early Holocene Epoch

  1. Open the Time Horizon Picker (A1).
  2. Select Early Holocene Pluvial (10,000 – 8,000 BP).

2. Configure Lake Lisan Water Level

  1. In Hydrological Reconstruction (A2), verify the lake level is set to -290 m MSL.
  2. Observe how the map canvas (A4) updates to draw the expanded Lake Lisan shoreline covering the Jordan Rift Valley.

3. Overlay Pre-Pottery Neolithic Sites

  1. Expand Archaeological Filters (A3).
  2. Check PPNB / PPNC Settlements (N=142).
  3. Click on Jericho (Tell es-Sultan) (A5) to inspect its early agricultural catchment parameters.