Sedimentologic, biostratigraphic and diagenetic studies made on Middle Aale
nian to Lowermost Bathonian deposits in 25 outcrops of the Burgundy High (s
outheastern Paris basin) lead to a sequence stratigraphy subdivision of the
early Dogger record into 7 third order depositional sequences. These seque
nces make up a second-order transgressive phase whose lower limit is a tect
onically enhanced unconformity (the Mid-Cimmerian unconformity), associated
with a large scale uplift during the Upper Toarcian and the Lower Aalenian
. In the largest outcrops, where the geometry of sedimentary bodies is obse
rvable at the hectometre to kilometre scale, the combination of diagenetic,
biostratigraphical, spatial and sedimentologic studies is useful to unders
tand the evolution of sediment distribution in the sequences. This approach
also allows the measurement of sea level falls at the origin of the sequen
ce boundaries. For example, we show that Lower Bajocian sequences end with
decreases of accomodation space < 10 m in amplitude, leading to temporary e
mergences of some reef complexes. Without interrupting the sedimentation on
submarine peri-reef pediments during lowstands, these decreases of a few m
etres of accomodation space can be related to either tectono-eustatic event
s or thermo-eustatic events.