Prehistoric settlement activities changed soil pH, nutrient availability, and growth of contemporary crops in Central Europe

Background and aims

How prehistoric human settlement activities have changed soil chemical properties, plant nutrition and growth of contemporary crops is a question that has not been satisfactorily addressed. The aim of this paper was to study to what extent nutrient availability in the soil, together with nutrition and growth of spring barley (Hordeum vulgare), improved on sites of former sunken buildings (cropmarks) in comparison to their surroundings (controls) 1,700 years after abandonment of the buildings.

Methods

In the Czech Republic, a unique prehistoric settlement with many sunken buildings was discovered during aerial reconnaissance from cropmarks in stands of cereals. Soil and biomass samples were collected from cropmarks and controls in a barley crop in June 2012.

Results

A substantially higher content of organic matter, higher pH and concentrations of plant-available (Mehlich III) P, Ca, Mg, Cu and Zn were recorded in the sub-soil layer in cropmarks compared with controls, indicating the accumulation of wood ash and organic waste. In the arable layer, pH and concentrations of P, Ca and Mg were generally very high in both positions. Cropmarks were characterised by barley plants that were twice as tall as the controls, with significantly higher Ca, Mg and P concentrations.

Conclusions

Prehistoric settlement activity affected nutrient availability and plant growth in the previously settled area even after 1,700 years. We conclude that the chemical signature of prehistoric settlement activity can be detected from chemical analysis of the sub-soil layer as well as analysis of the contemporary arable layer and crop biomass.