If you haven't noticed, a recurring theme in all my previous entries is that all the species are from the continent of Tuaisceart. And as we go through each post and more is added. We briefly go through biomes of tuaisceart, as a result. And strike deeper into it's "heart". The massive Loch sea.
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| What guards the massive Loch sea is the Temperate denseforest of Tuaisceart . Otherwise known as An Coillthiubh , supported by the lake, whose is protected by precipitation on the lake itself, and the massive, ash consuming Ashcatchers, or Coilleanas, a group of species specialised by consuming the massive clouds suspended by Eile's lower gravity and wind patterns, which may not feel like much, being 30% less. But it makes a massive difference for small particles like volcanic ash, and the ability to develop structures to catch volcanic ash. |
Ash contains molecules , nutrients necessary to maintain massive size for the Coilleneas. The coillean has selectively developed extended ends off it's upper leaves to reach up into the sky. Large Ash clouds are maintained via wind patterns, and it's particles consumed and stripped bare by these trees. The ends are electrically charged, nutrient molecules launch into the trees system from the top into the leaves, into the branches, into the trunk. Sometimes, volcanoes may only erupt only a few hundred or thousand years, so the coillean are switch up and sustain themselves on other nutrient and water sources.
You may notice the distance of some volcanoes to actual denseforests. There are a few explanations, ashes, due to the lower gravity of Eile, are easily suspended in it's atmosphere. Allowing it travel for hundreds of thousands of kilometers, considering the fact that all things considered, Tuaisceart is a massive continent. Another reason is plategrass, the denseforest is in a constant "war" with the plategrass, which is indeed, an invasive species. The reason of existence for TDTLFs on large continents is that they are outgrowth of denseforests, some photoid species can be found both on TDTLFS and in the cluttered, tight, denseforests. Even shrubland species, which evolved from denseforest undergrowth. It is an evolutionary arms race, with both sides launching parasitic species , adapted to the environments on either sides ,that is the reason why some TDTLF areas are trapped being TDTLFs whilst sorrounded by volcanoes. Or plategrass securing a victory by sorrounding it with plategrass species adapted to volcanoe habitats. Thus why Denseforests looked squeezed in along the end of the Tuaiscartean river deltas and yet spread out for hundreds of kilometers at the north and center loch region.











