Fluvial response to rapid high‐amplitude lake‐level changes during the L ate W eichselian and early H olocene, A in R iver valley, J ura, F rance

In the present paper the effects of rapid, high‐amplitude base‐level changes during the last glacial‐interglacial transition were studied for the A in R iver in eastern F rance. During the W ürm glacial maximum ( MIS 2) rapid aggradation by deep‐water G ilbert‐type deltas and shallow‐water fan deltas occurred at the margins of a 20 to 50 m deep proglacial lake. A temporal high‐amplitude lake‐level fall of 60 m resulted in gravel deposition by forced‐regressive deltas, followed by rapid lake‐level rise and fine‐grained glaciolacustrine deposition. During the final deglaciation, a rapid base‐level fall of 40 m resulted in a complex fluvial response. Knickpoint formation and headward incision of the highstand deltas and concomitant deposition of gravel sheets by forced‐regressive deltas and braided systems occurred in several depocentres on the former glacial lake floor. Preservation of highstand and falling‐stage deposits and terrace formation in the incised valley depended on vertical incision and lateral channel migration. Terraces are well developed in the former lake‐floor depressions, whereas vertical incision was dominant in the higher lake‐floor areas. The A in terrace staircase was likely formed by autogenic processes during a single allogenic base‐level fall. This case study possibly offers an analogue for the preservation of interglacial highstand coastal deltas during sea‐level fall at warm‐to‐cold climate transitions, although the rates of base‐level fall are different.