The formation comprises a succession of lenticular bodies showing two main facies; clayey sands rich in frequently pyritisedlignite, together with amber and grey clayey sands with less lignite (1 to 12% of the sediment), with continental vertebrate fauna. These facies, the rarity of mollusk shells and charophytes, probably due to decarbonatation and the presence of pyrrhotite (FeS4), reflect a hypoxic environment.
The strata were deposited at the bottom of two channels cutting into underlying Thanetian marine green sands. The channels prograde toward the northeast and were discovered under Oise RiverQuaternary deposits.
Fossil content
The formation has provided among others the following fossils:[1]
Bronnert, C.; Gheerbrant, E.; Godinot, M.; Métais, G. (2019), "First European 'Isectolophidae' (Mammalia, Perissodactyla): Chowliia europea, sp. nov., from the lower Eocene of Le Quesnoy, France", Journal of Vertebrate Paleontology, 38 (4): 1–9, doi:10.1080/02724634.2018.1487448
Solé, F.; Gheerbrant, E.; Godinot, M. (2013b), "Sinopaninae and Arfianinae (Hyaenodontida, Mammalia) from the Early Eocene of Europe and Asia; evidence for dispersal in Laurasia around the Paleocene/Eocene boundary and for an unnoticed faunal turnover in Europe", Geobios, 46 (4): 313–327, Bibcode:2013Geobi..46..313S, doi:10.1016/j.geobios.2013.02.003
Nel, A (2006), "Oldest records of Bombyliidae: Phthiriinae and Mythicomyiidae: Glabellulinae from the Lowermost Eocene amber of France (Diptera: Bombylioidea)", European Journal of Entomology, 103: 109–114, doi:10.14411/eje.2006.016
Nel, A.; de Plöeg, G.; Dejax, J.; Duthiel, D.; Franceschi, D.; Gheerbrant, E.; Godinot, M.; Hervet, S.; Menier, J.J.; Augé, M.; Bignot, G.; Cavagnetto, C.; Duffaud, S.; Gaudant, J.; Hua, S.; Jossang, A.; Lapparent Broin, F.; Pozzi, J.P.; Paicheler, J.C.; Beuchet, F.; Rage, J.C. (1999), "Un gisement sparnacien exceptionnel à plantes, arthropodes et vertébrés (Éocène basal, MP7): Le Quesnoy (Oise, France)", Comptes Rendus de l'Académie des Sciences, Série IIA, 329 (1): 65–72, Bibcode:1999CRASE.329...65N, doi:10.1016/S1251-8050(99)80229-8