Isotope signature of sand calcites in the Paris Basin: a proxy for permafrost/groundwater paleoconditions

International audience Sand calcites occurring as rhombohedral crystals and spherolitic concretions in several Tertiary sandstone formations in the Paris basin have been dated to the cooling periods of the four last glacial stages, using 14C and U-Th methods. Sand calcites constitute a novel proxy t...

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Bibliographic Details
Published in:Procedia Earth and Planetary Science
Main Authors: Thiry, Médard, Innocent, Christophe, Franke, Christine
Other Authors: Centre de Géosciences (GEOSCIENCES), Mines Paris - PSL (École nationale supérieure des mines de Paris), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), Bureau de Recherches Géologiques et Minières (BRGM)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2015
Subjects:
France
Fontainebleau
paleo-permafrost
paleo-groundwater
isotopes
sand calcite
datation
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
permafrost
Online Access:https://minesparis-psl.hal.science/hal-01236662
https://minesparis-psl.hal.science/hal-01236662/document
https://minesparis-psl.hal.science/hal-01236662/file/Thiry%26al_2015_sand_calcites_Paris_Basin_isotopes.pdf
https://doi.org/10.1016/j.proeps.2015.07.005
Description
Summary:International audience Sand calcites occurring as rhombohedral crystals and spherolitic concretions in several Tertiary sandstone formations in the Paris basin have been dated to the cooling periods of the four last glacial stages, using 14C and U-Th methods. Sand calcites constitute a novel proxy to estimate paleo-groundwater levels and the extension of permafrost conditions. The δ13C and δ18O compositions of sand calcites are a function of precipitation depth in relation with the warming of surface water during infiltration. Sand calcites appear as precious markers for Pleistocene paleo-landscape reconstructions.

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