| Atane Formation | |
|---|---|
|  Stratigraphic range: Albian-Coniacian  ~  | |
| Type | Formation | 
| Sub-units | Skansen Member | 
| Underlies | Kome Formation | 
| Overlies | Slibestensfjeldet Formation | 
| Lithology | |
| Primary | Mudstone | 
| Other | Sandstone, coal | 
| Location | |
| Coordinates | 69°24′N52°48′W / 69.4°N 52.8°W | 
| Approximate paleocoordinates | 55°06′N16°54′W / 55.1°N 16.9°W | 
| Region | Ivnanguit | 
| Country | Greenland | 
| Extent | Nuussuaq Basin | 
The Atane Formation is a geologic formation in Greenland. It preserves fossil insects of Elytrulum multipunctatum , [1] dating back to the Albian to Coniacian stages of the Cretaceous period. [2]
The carbonaceous mudstones, sandstones and coal seams are interpreted as freshwater lake or swamp deposits representing the vertical aggradation of a subaerial to shallow, limnic floodplain to upper delta plain. There are no indications –neither palynological evidence nor the presence of pyrite– to suggest marine or brackish-water conditions. [2]