Chishi Era (地支代, Chishidai)

The Chishi Era marks a dramatic fracturing of the continents following the Gogyō Era. For the first time in Erthas’s history, over a dozen distinct landmasses drifted into separate evolutionary trajectories. Elven natural philosophers of the Classical Period referred to this time as the Era of Earthly BranchesChishi(地支) — associating each landmass with one of the Twelve Terrestrial Signs. Though poetic and imprecise, the number reflected an early awareness of the scale of fragmentation. Later scientific consensus recognizes fourteen major continental plates during this era.  

Continental Overview & Dominant Families

 

Archaeo-Daiin(Thadh, Kiin, Chūin)

Climate: Polar (Thadh, Kiin), Boreal (Chūin)  
  • Plant Families:
  • Pinaceae — adapted to extreme cold, forming boreal forests
  • Ginkgoaceae — hardy, deciduous forms in protected valleys
  • Cupressaceae — cold-tolerant conifers gaining foothold
  • Animal Families:
  • Morganucodontidae — shrew-like early mammals adapted to freezing climates
  • Ceratodontidae — lungfish persisting in glacial meltwater
  • Capitosauridae — relic amphibians surviving in thermal springs
 

Archaeo-Daishin(Shinyū, Shinbō)

Climate: Temperate (Shinyū), Subtropical (Shinbō)  
  • Plant Families:
  • Podocarpaceae, Araucariaceae — conifer dominance in uplands
  • Ginkgoaceae — common in temperate valleys
  • Polypodiaceae — fern thickets in riparian zones
  • Animal Families:
  • Tritylodontidae — small, herbivorous mammaliforms
  • Protosuchidae — early croc-line archosaurs
  • Salticidae-like spiders — widespread across leaf litter
 

Archaeo-Konchuu(Konchū)

Climate: Tropical  
  • Plant Families:
  • Zamiaceae — dominant in evergreen tropical forest canopy
  • Polypodiaceae — diverse epiphytes and ground ferns
  • Animal Families:
  • Chiniquodontidae — arboreal cynodonts in dense forests
  • Blattidae, Curculionidae — rapid radiation of insects
  • Araneidae — web-building spiders adapting to high moisture
 

Archaeo-Bomi(Bōkō, Teishin, Gohyō, Teigō)

Climate: Tropical (Bōkō–Teishin–Gohyō), Subtropical (Teigō)  
  • Plant Families:
  • Zamiaceae, Cycadaceae — dominant in canopy and upland forest
  • Matoniaceae, Osmundaceae — tropical ferns
  • Animal Families:
  • Tritheledontidae, Docodontidae — emerging mammaliaformes
  • Euparkeriidae — agile archosauriforms expanding into new niches
  • Rhynchocephalians — diversifying lepidosaurians
 

Archaeo-Saizai(Jinchū, Jinshi)

Climate: Temperate (Jinchū), Subtropical (Jinshi)  
  • Plant Families:
  • Ginkgoaceae — prominent throughout
  • Podocarpaceae — forming highland conifer forests
  • Polypodiaceae — widespread ferns
  • Animal Families:
  • Tritylodontidae — herbivorous generalists
  • Coelophysidae — early small-bodied theropod dinosaurs
  • Formicidae-like ants — eusocial behavior likely emerging
 

Archaeo-Daisai(Shinshi, Kyōshi, Chishi, Kōbō, Chichū, Tōsai, Shinchū)

Climate: Tropical to Subtropical  
  • Plant Families:
  • Zamiaceae, Cycadaceae — main canopy components
  • Polypodiaceae, Gleicheniaceae — widespread fern diversity
  • Podocarpaceae — upland and seasonal forest zones
  • Animal Families:
  • Chiniquodontidae, Cynognathidae — mid-sized cynodonts
  • Sauropodomorph families — early herbivorous dinosaurs emerging
  • Tenebrionidae, Curculionidae — beetle lineages expanding across niches
 

Archaeo-Lomba(Lomba)

Climate: Boreal  
  • Plant Families:
  • Pinaceae, Cupressaceae — conifer dominance
  • Ginkgoaceae — surviving in seasonal valleys
  • Animal Families:
  • Morganucodontidae — basal mammaliaformes
  • Procolophonidae — lingering herbivores
 

Archaeo-Ndali(Ndali)

Climate: Subtropical  
  • Plant Families:
  • Zamiaceae, Podocarpaceae — dominant in upland forests
  • Polypodiaceae — dominant in valleys and riverways
  • Animal Families:
  • Protosuchidae — early croc-line reptiles
  • Docodontidae — diverse early mammals
 

Archaeo-Zhamo(Zhamo)

Climate: Boreal  
  • Plant Families:
  • Pinaceae, Ginkgoaceae — boreal forests
  • Glossopteridaceae — final relict pockets
  • Animal Families:
  • Tritheledontidae — cold-adapted insectivores
  • Temnospondyls — declining amphibian groups
 

Archaeo-Boyuu(Boshi, Teigai, Boshu)

Climate: Subtropical to Temperate  
  • Plant Families:
  • Podocarpaceae — conifers common in uplands
  • Zamiaceae, Osmundaceae — warm lowland forests
  • Animal Families:
  • Docodontidae — thriving in cooler forests
  • Coelophysidae — lightweight theropods in open plains
 

Archaeo-Chishu(Chishu)

Climate: Boreal  
  • Plant Families:
  • Pinaceae, Cupressaceae — conifer forests
  • Ginkgoaceae — valley specialists
  • Animal Families:
  • Morganucodontidae — high-latitude mammals
  • Erythrosuchidae — late-surviving basal archosaurs
 

Archaeo-Heiyū(Heiyū)

Climate: Polar  
  • Plant Families:
  • Cupressaceae, Ginkgoaceae — small, hardy groves
  • Animal Families:
  • Tritylodontidae — cold-adapted grazers
  • Temnospondyli — clinging to thermal streams
 

Shinshin(Shinshin)

Climate: Tropical  
  • Plant Families:
  • Zamiaceae, Polypodiaceae — dominate thick jungle biomes
  • Animal Families:
  • Chiniquodontidae — fast, nimble insectivores
  • Rhynchocephalia — lizard-like reptiles with diverse feeding strategies
 

Kyougai(Kyougai)

Climate: Tropical  
  • Plant Families:
  • Zamiaceae, Osmundaceae — established endemic forms
  • Animal Families:
  • Tritheledontidae — relic mammal-forms
  • Archosauriformes — island-radiated specialists
 

Legacy

The Chishi Era established the modern tectonic map of Erthas. Each landmass bore its own evolutionary pressures, climates, and endemic lineages. This increasing separation would set the stage for the explosive radiations of the Kairetsu and Shinrin Eras to follow — and for the rise of truly modern ecosystems across the globe.