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Evidence of Sphagnum-like remains
Evidence of Sphagnum-like remains
The Sandbian Epoch (459-453 Ma) occurs during the Late Ordovician Period, that occurs after the Darriwilian, and before the Katian.
Geologic Age
Geologic Age
458.4±0.9–453.0±0.7 Ma
Eon / Era / Period / Epoch
Eon / Era / Period / Epoch
What happened during this time?
What happened during this time?
These Ordovician sediments possess 15 species of miospores
Naked laevigate monads; naked fused dyads (i.e. Pseudodyadospora); naked fused tetrads (i.e. Tetrahedraletes); naked unfused tetrads (i.e. Stegambiquadrella); smooth envelope enclosed dyads (i.e. Segestrespora); envelope enclosed ornamented tetrads; naked unfused dyads (i.e.Dyadospora); ornamented envelope enclosed dyads (i.e. Segestrespora); smooth envelope enclosed tetrads (i.e. Velatitetras); ornamented envelope enclosed tetrads (i.e. Velatitetras); envelope enclosed monads (i.e. Sphaerasaccus);
Many are bryophyte-like spores found in these Middle Ordovician sediments
Other possible miospore types
naked monads with pseudo-trilete mark (i.e. Imperfectotriletes)
Macrofossils of plants are found as smooth tubes, similar to hydroids.
Peat moss–like vegetative remains found in 455 Ma sediments from Wisconsin (Cardona-Correa et al. 2016)
Above: Multicellular organic fragments similar to Sphagnum found in 455 Ma sediments from Wisconsin (Cardona-Correa et al. 2016)
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