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New insights on the latest Messinian-to-Piacenzian stratigraphic series from the Dahra Massif (Lower Chelif Basin, Algeria): Lago Mare, reflooding and bio-events
An overview of the Santonian amber-bearing deposits of the Sainte-Baume Massif, southeastern France
Erratum to: Reassessment of amber-bearing deposits of Provence, southeastern France BSGF − Earth Sciences Bulletin 2021, 192, 5 https://doi.org/10.1051/bsgf/2020048
Reassessment of amber-bearing deposits of Provence, southeastern France
Amber, from deposit to inclusions: new data
New fossil assemblage with amber, plants and vertebrates from the lower Cenomanian near Châtellerault (Vienne, western France)
Thai amber: insights into early diatom history?
Exceptional preservation of marine diatoms in upper Albian amber
Anatomie de quelques plates-formes carbonatees progradantes messiniennes de Mediterranee occidentale
Abstract: The Messinian Melilla carbonate platform is composed of five main sedimentary units, from bottom to top: 1) a retrograding marly and conglomeratic unit, 2) a complex conglomeratic then prograding/aggrading carbonate unit, 3) a prograding/aggrading reef-complex unit, 4) an aggrading siliciclastic unit and 5) an aggrading/retrograding siliciclastic and carbonate unit. The platform developed throughout high-frequency relative sea-level rises and Stillstands, and relative sea-level drops are of minor importance. The reef complex mainly contains Porites buildups that exhibit southward progradational geometries. At the base, the reef complex developed on a marine planation surface. The youngest reefs show aggradational geometries and are associated with oolitic deposits. Cross sections constructed by removing late Messinian tectonics and compaction suggest that there was no significant relative fall in sea level during both platform and coral reef development, except at the end of the platform development.
Abstract: Messinian reefs from western Orania occur along a narrow outcrop belt which is several hundred meters wide and tens of kilometers long. The reefs show generally a sequential organization of buildups in a backstepping pattern. Each step of reef-building is represented by a tabular fringing reef with poor internal zonation. Cyclic input of argillaceous sediment produced a rythmic response in coral growth. These well-bedded reefs developed during a general lower Messinian transgressive episode.