Periglacial morphogenesis in the Paris basin: insight from geophysical survey and consequences for the fate of soil pollution

Geophysical survey by Automatic Resistivity Profiling (ARP©) system of the Pierrelaye–Bessancourt area revealed remarkable conductive polygon patterns of 20- to 30-m diameter detected between 0.5- and 1.7-m depth. Trenches dug down to the limestone substrate allowed detailing of the pedological and lithological units that compose such polygonal features. The patterns are formed by greenish glauconite and carbonated sand hollows where clay-rich pedological horizons bend downward, forming narrow tongs extending up to 2- to 3-m depth. Such structures were interpreted as a buried polygonal ice-wedge network (thermokarst depressions). Geometrical relationships between the lithological units and consecutive erosional surfaces allowed the identification of successive landscape events and a landscape chronology. The sequence started during the Saalian glaciation with (1) the development of patterned grounds by thermokarstic cryoturbation; (2) the consecutive deflation/erosion during post-permafrost aridity; (3) the loess and eolian sand deposits; (4) the weathering of the former deposits with development of pedogenic horizons during the Eemian interglacial; (5) the recurrent cryoturbation and thermal cracking leading to infolding of the pedogenic horizons during the Pleniglacial optimum (Weichselian); and finally (5) the erosion that levelled the periglacial microreliefs, most probably during the last glacial stage (Weichselian), leading to the modern landscape. In this agricultural area, urban waste water has been spread for more than 100years by flooding irrigation for food crop production and has led to high levels of metal pollution in the surface horizons of the soils. The polygonal cryogenic structures have major impacts on soil hydrology and dispersion/distribution of heavy metals toward the geological substrate. Such structures are essential to consider when conceiving proposals for future soil management of this polluted area. Artist view of the cryogenic infolded clay structures below the black strip of the polluted soils of the dismal Pierrelaye Plain, by the author (MT) [Display omitted] •Geophysical survey revealed a 20- to 30-m-wide polygon pattern in a Luvisol soil cover.•Periglacial cryoturbation led to clay sink structures and fragmented limestone zones.•Millennial cryogenic structures highly influence the fate of centennial soil pollution.•Leaching of heavy metals into the substrate was higher in fragmented limestone zones.