Lochkovian Age (419-411 Ma) is in the Early Devonian Epoch. It occurs after the Pridoli (of the Silurian Period) and before the Pragian Age.
419.62±1.36–413.02±1.91 Ma
In North America the Lochkovian Stage is represented by Gedinnian or Helderbergian time
Above: Fig 2 of Matsunaga and Tomescu 2016, showing root arrangement and variable preservation of root-bearing axes and attached roots
Above: Fig 4 of Matsunaga and Tomescu 2016, showing roots of the Cottonwood Canyon lycophyte
Bryophytes such as Sporogonites † are on the landscape
Eophytes and horneophytes, which both probably appeared in the Silurian, populate the water edges
Eophytes are only known from Lochkovian sediments of the Welsh Borderland, but may represent the final days for this group, which probably appeared in the Ordovician Period based upon cryptospores
Early tracheophytes, such as rhyniophytes and cooksonioids, continue to inhabit wet areas
Rhyniophytes: Aberlemnia †, Cooksonia †, Eocooksonia † (=Cooksonella), Culullitheca †, Fusitheca † (=Fusiformitheca), Grisellatheca †, Pertonella †, Resilitheca †, Salopella †, Sporathylacium †, Tarrantia †, Tortilicaulis †, Uskiella †
Ancestral lycophytes continue to diversify
Zosterophyllopsida: Deheubarthia †, Gosslingia †, Hicklingia †, Jugumella †, Sawdoniales, Thrinkophyton †, Xitunia †, Zosterophyllum †
Lycopods such as Drepanophycales diversify
Barinophytes like Protobarinophyton †
Early Devonian lycophyte from Cottonwood Canyon (Wyoming) shows evidence for a rooting system preserved in growth position (Matsunaga & Tomescu, 2016)
Ancestral trimerophytes, such as Psilophyton †, also appear on the land.
Other unclassified plants include: Balchaschella †, Bowerophylloides †, Hostinella †, Isidrophyton †, Juliphyton †, Mointina †, Pseudosajania †, Psilophytites †, Salairia †, Stolophyton †, Taeniocrada †, Tastaephyton †, Uksunaiphyton †