Miaolingian Epoch (Series 3)
Geologic Age
509–497 Ma
Subdivisions
Guzhangian: 500.5–497 Ma
Drumian: 504.5–500.5 Ma
Wuliuan: 509–504.5 Ma
Eon / Era / Period / Epoch
What happened during this time?
Possible evidence for land-based spores during the Middle Cambrian, although the affinities of these spores are unknown (Taylor & Strother, 2008, 2009; Strother, 2016)
There may be land plants, or possibly algae, or even transitional embryophyte-charophyte organisms
Indirect evidence of Cambrian land plants also comes from carbon isotopic composition of carbonaceous debris and sediments (Tomescu & Rothwell, 2006; Tomescu et al., 2009) and chemical and textural profile differentiation of clayey Cambrian paleosols (Retallack, 2008, 2009, 2015).
Parafunaria sinensis
An alleged moss-like fossil from China dating to this period (Yang et al., 2004)
This fossil is interpreted as having whorled leaves and other features similar to the living moss Funaria hygrometrica
This fossil is 20-30 million years earlier than the expected origin of bryophytes as a whole
Most researchers assume the earliest bryophytes were thalloid, retaining some of those ancestral algal morphologies.
This fossil appears quite sophisticated, and leaf-like organs have already evolved.
Substantial skepticism exists about this fossil representing an authentic Middle Cambrian moss