Cave Ferrumtime: Difference between revisions
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imported>Mnidjm No edit summary |
imported>Mnidjm (→top: Eukaryota) |
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|diet = Lithovore (Iron, Other Minerals) |
|diet = Lithovore (Iron, Other Minerals) |
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|reproduction= Binary Fission |
|reproduction= Binary Fission |
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|domain = |
|domain = Eukaryota |
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|kingdom = |
|kingdom = |
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|phylum = |
|phylum = |
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Revision as of 21:57, 2 March 2021
| Cave Ferrumtime | ||
|---|---|---|
| (Ferrumteproutine trabaunda) | ||
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| 23/148, Integrated into Tepoflora | ||
| Information | ||
| Creator | Clarke Other | |
| Week/Generation | 19/129 | |
| Habitat | Blood Lava Tube Sea Caves | |
| Size | Microscopic | |
| Primary Mobility | Unknown | |
| Support | Unknown | |
| Diet | Lithovore (Iron, Other Minerals) | |
| Respiration | Unknown | |
| Thermoregulation | Unknown | |
| Reproduction | Binary Fission | |
| Taxonomy | ||
| Domain Genus Species | Eukaryota Ferrumteproutine Ferrumteproutine trabaunda | |
| Ancestor: | Descendants: |
|---|---|
The cave ferrumtime split from its ancestor, the ferrumtine, and has moved to the Wright sea caves and water tables. Its four flagellum have spaced out, and are now used to anchor the organism to the walls of the caves and to absorb nutrients. If an area is to crowded, though, the cave ferrumtime will use its flagellum to push off of the wall and into the water, moving to new locations, feeding on the iron in the water until it runs into rock.