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I really hope 2025 is a good year for Hamster’s Paradise.
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What do the Mesoterran bossums of the Middle Temperocene look like?
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I noticed that in the first post detailing the fauna of South Ecatoria, it mentions shearwurms being within the forest canopy, but when I asked you about how the rattile fauna of different landmasses differ from each other, you said that the shearwurms are only found in Mesoterra. Is this a retcon, or did the South Ecatorian shearwurms go extinct within the past 25 million years?
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Is Isla de Oof a continental island or a volcanic one? When did it split from the Arcuterran mainland/ raise from the sea?
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What are the largest podotheres of South Ecatoria?
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What do the Middle Temperocene descendants of the ruffed rath look like?
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Are there plans to make posts for older time periods? I in particular would like to see a post for the life of East Nodera in the Early Glaciocene, around 100 Million years post-establishment, before it fused with North Ecatoria.
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How do flightless pterodents differ from non-pterodent podotheres? Would appreciate an illustration?
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Why didn’t the hammoths and non-podothere drundles spread into Gestaltia through Junctus?
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Why weren’t any dwarf forms of North Ecatorian clades like the podotheres, buffants, and vulwerines present on Isla Centralis during the Glaciocene or Early Temperocene?
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Can you draw the first terrestrial quadriliterian (I don’t know if I’m spelling it right)?
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When did the major clades of pseudosnakes(songs, ophiotauri, quetzals, theriodontophidians, bahumuts, trunksnakes, twintrunks, and windribbons) first evolve?
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Would the Hmu-uwii see the rainbow snimp and wandering nasobeam as races of primitive dwarves and giants, considering how they are some of the Hmu-uwii’s closest living relatives, but respectively much smaller and larger than them?
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