During palynological slide scanning i have find some unusual structures. Which I am uploading for your opinion. This is from the mesoproterozoic carbonaceous shale.
In my opinion, the pictures shown as atypical form could be represented as remains of either fragment of 'mat-like' coccoid cynobacteria colony(or aggregation), or some contaminant organic material.
MOCZYDLOWSKA 1991 (Acritarch biostratigraphy of the Lower Cambrian and the Precambrian-Cambrian boundary in southeastern Poland) figure a similar object on Plate 15:H as an "organic envelope after growth of framboidal pyrite on a fragment of organic matter."