B. Bourel, Jean‐David Moreau, Vincent Trincal, Anne-Véronique Walter-Simonnet
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Fossiliferous Holocene tufa of Mende (Lozère, southern France): implication for the Atlantic vegetation of the Causses Basin
Tufas bearing plant macroremains are uncommon in the Causses Basin (southern France). Here, we report a
new fossiliferous tufa deposits at Mende, in Lozere. This palaeontological site is the first Quaternary tufa from the
northern part of the Causses Basin that yields such an abundance of plant macroremains. The radiocarbon dating shows
that these Holocene deposits are related to the Atlantic period. Geomorphology and mineralogy show that the
plant-bearing deposit is a calcareous tufa only composed by calcite, deposited near to an outlet of cool water, linked to
the karstic hydrological system of the Causse de Mende. The flora exposed in this article is dominated by angiosperms.
Leaves and reproductive structures were assigned to Acer platanoides, Corylus sp., Hedera sp., Salix cf. cinerea, and
Tilia cordata. This new palaeobotanical data complements our scarcely knowledge of the Atlantic floras from the Causses
Basin. During the Atlantic period, and in the northern part of the basin, whereas Pinus-dominated forests and oak
groves were probably well-developed, valleys were locally inhabited by diversified wet angiosperm-dominated forests.
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