The Emsian Age (411-393.5 Ma) is the last age in the Early Devonian epoch, which occurs after the Pragian Age, and before the Eifelian Age of the Middle Devonian Epoch
410.62±1.95–393.47±0.99 Ma
Many vascular and non-vascular plants on the landscape, but terrestrial landscapes are still considered primitive (Hotton et al., 2001)
Nematophytes such as Spongiophyton † and Prototaxites †
Bryophytes such as Sporogonites †
Rhyniophytes, Cooksonia †, and early Tracheophytes such as Aarabia †, Amplectosporangium †, Aphyllopteris †, Bitelaria †, Changwuia †, Chakassiophyton †, Dawsonites †, Eogaspesia †, Hostinella †, Hsüa †, Huia †, Huvenia †, Margophyton †, Minusia †, Pectinophyton †, Psilophytites †, Renalia, Stockmansella †, Rhabdophyton †, Taeniocrada †, Sciadocillus †, Sciadophyton †, Thursophyton †, Uskiella †, and Yarravia †
Plants like Huvenia † and Sciadophyton † occupy areas farther away from the channel margins
Zosterophyllophytes such as Crenaticaulis †, Danziella †, Distichophytum †, Estinnophyton? †, Forgesia †, Guangnania †, Hicklingia †, Oricilla †, Sawdonia †, and Zosterophyllum †
These plants occupy low-energy, water-saturated habitats such as marshes and back swamps (Hotton et al., 2001), which are stressful and low in dissolved oxygen
Plants had adaptations to this stressful environment, such as resistant cuticle, growth after producing spores, and numerous buds for regrowth
Lycopods such as Baragwanathia †, Cyclostigma †, Drepanophycus †, Kaulangiophyton †, and Leclercqia †
Barinophytes such as Bracteophyton †, Krithodeophyton †, and Omniastrobus †
Early euphyllophytes such as Chaleuria †, Oocampsa †, Psilophyton †, Trimerophyton †, and Wilhowia † were all present
Most of these plants occupy higher-energy, ephemeral habitats such as crossbar channels in rivers (Hotton et al., 2001), although Psilophyton forbesii † existed in back swamp conditions
These plants lived in high-disturbance environments with high reproductive output and short life spans
Psilophyton diakanthon † is an Emsian species that possesses fibers in the inner cortex and enations/prickles, which are the earliest possible evidence of anti-herbivore defense
Cladoxylopsids
Foozia minuta †, a possible early cladoxylopsid, is also found at this time (Gerrienne, 1992)
Paracladophyton kespekianum † found in Quebec, Canada (Chu et al., 2024)
In addition, Pertica † was probably the tallest plant around at this time, although woody growth in Franheuberia gerriennei † may have allowed for tall growth
Franhueberia (Hoffman and Tomescu 2013), Gmujij tetraxylopteroides † (Pfeiler & Tomescu, 2020), and Armoricaphyton † (Strullu-Derrien et al., 2014) axes exhibiting secondary xylem are found in the mid-late Emsian
These are the oldest evidence of wood production in the fossil record
Heterospory originated approximately 407 Ma (Traverse, 1988)
Isolated mega- and microspores are the oldest evidence in the fossil record
Omniastrobus dawsonii †, a lycophyte from the Early Emsian, shows a gradation of small to large spores, with median-sized spores, as well.
Chaleuria †, a euphyllophyte found in the Emsian, also shows heterospory with sporangia that exhibit small, large, or mixed spores.
Above: Anatomy of Franhueberia †, one of the earliest plants to show secondary growth