Calcitine: Difference between revisions
Jump to navigation
Jump to search
Content added Content deleted
imported>Mnidjm No edit summary |
imported>Mnidjm (→top: Eukaryota) |
||
Line 15: | Line 15: | ||
|diet = Lithovore (Calcite) |
|diet = Lithovore (Calcite) |
||
|reproduction= Binary Fission |
|reproduction= Binary Fission |
||
|domain = |
|domain = Eukaryota |
||
|kingdom = |
|kingdom = |
||
|phylum = |
|phylum = |
Revision as of 21:55, 2 March 2021
Calcitine | ||
---|---|---|
(Cryoutine calcitine) | ||
23/149, Outcompeted | ||
Information | ||
Creator | OpDDay2001 Other | |
Week/Generation | 18/118 | |
Habitat | Sublyme Limestone Caves | |
Size | Microscopic | |
Primary Mobility | Unknown | |
Support | Unknown | |
Diet | Lithovore (Calcite) | |
Respiration | Unknown | |
Thermoregulation | Unknown | |
Reproduction | Binary Fission | |
Taxonomy | ||
Domain Genus Species | Eukaryota Cryoutine Cryoutine calcitine |
Ancestor: | Descendants: |
---|---|
Calcitine has split from it's ancestor. Having spread to the Sublyme Limestone Caves, the tealspot cryoutine needed alternate means of nutrition, as there was little to no sunlight and no other lifeforms to infect parasitically. Eventually, tealspot cryoutine evolved to use calcite, a major part of limestone, as an energy source. As such, the calcitine has spread throughout the entire cave system. Calcitine live on rocks, and stalagmites. They've yet to spread to stalactites and the cave ceiling. Calcitine use the carbon from carbon-dioxide as a carbon-source, producing oxygen as a waste product.