Cryptospores

Cryptospores are fossilised primitive plant spores that first appear in the fossil record during the late Ordovician to early Silurian period.

Contents

Evidence that cryptospores derive from land plants

Occurrence

Cryptospores are generally found in non-marine rocks and decrease in abundance with distance offshore. This suggests that any cryptospores found in the marine environment were transported there by the wind from the land, rather than originating from the marine environment.

Wall Ultrastructure

The walls of cryptospores consist of many lamellae (thin sheets). Liverworts, thought to be the most primitive land plants, also have this spore wall morphology.

Chemical composition

(Some) cryptospores are composed of sporopollenin and have the same chemical makeup as co-occurring trilete spores.[1]

Other information

Recently, fossils of plant sporangia have been found in Oman with cryptospores showing concentric lamellae in their walls, similar to liverworts.

See also

Paleobotany

References

  1. ^ Steemans, P.; Lepot, K.; Marshall, C. P.; Le Hérissé, A.; Javaux, E. J. (2010). "FTIR characterisation of the chemical composition of Silurian miospores (cryptospores and trilete spores) from Gotland, Sweden". Review of Palaeobotany and Palynology 162: 577. doi:10.1016/j.revpalbo.2010.07.006.  edit