Ryl Madol is able to support a large amount of amphibious and aquatic life thanks to its many pools, ponds and streams which pay tribute to large lakes and rivers. For many of the tetrapods and arthropods, these are vital for their reproduction, as their eggs and larvae lack shells and need to be laid in water. However, many of these breeding pools are not necessarily provided by the island topography. They are made by the wildlife itself, though, ironically, not by amphibians.
Encountered in almost every waterway are waterlogged wooden structures, which early explorers at first mistook as as bridges or fish-traps created by the island’s intelligent natives. But no. These are dams built by an aquatic reptile called Castorosaurus, whose name literally translated to “beaver-lizard”. Castorosaurs are derived members of the Captorhinidae, a group of Palaeozoic reptiles that, on account of missing postorbital windows, were traditionally grouped with the “Anapsida” alongside the turtles, though recent work has recovered them as being eureptiles close to the Diapsida. Even more recent work has declared them stem-amniotes, though this remains controversial.
Just like beavers, castorosaurs are
ecosystem-engineers who prolifically build dams along narrow waterways,
creating many pools throughout the island in which other organisms can thrive
and reproduce. Their dams usually have a hollow chamber that can only be
accessed from underwater. Here the castorosaurs lay their eggs and raise their
young. The dam structure prevents terrestrial or aerial predators from easily gaining access to the nest, though the parents still tend to be on the look-out for any of the creeping amphibians that may dive and slither below.
Unlike the terrestrial captorhinids of the Palaeozoic, castorosaurs feature many aquatic adaptations such as webbed feet and a dorso-ventrally flattened tail like a platypus. This tail-shape is of course quite curious, as reptiles usually swim through sideways undulation and so one would expect a laterally flattened tail, but the tail seems to be mainly used as a sort of hammer in dam-building. What castorosaurs have retained from their ancestors are the long, kinked snouts with specialised teeth at the front. Said teeth have become quite large and spiky. Many people easily make the mistake of assuming that castorosaurs used their large front-teeth just like beavers to gnaw at wood, but that is in fact incorrect. They are entirely unsuited for such a task and are instead used to capture fish.
If they cannot gnaw at trees and branches, where do castorosaurs get the wood for their dams then? The answer is that they simply pick it up from the forest or lake floor and so do not need to saw up fresh wood. But why it is that simple for them is actually interesting. Vast areas of Ryl Madol are covered in thick carpets of wood-litter that degrade into smaller pieces over time as animals trample over them, but never truly rot and decay. Some pools and moors have as a consequence devolved into large, malignant peat bogs in which unwary animals may stumble and get trapped. It is highly unusual and not something seen in any other forests in the world. Only recently has the reason behind this been revealed by botanists and microbiologists: Ryl Madol entirely lacks any organisms, be they bacteria or fungi, that can digest lignin, the main polymer that makes up wood. This used to be true for all of Earth in the Carboniferous period, from which huge coal deposits still survive. While it explains the primordial nature of Ryl Madol’s forests, it just opens up many more questions. Why has lignin-digestion never evolved or arrived on Ryl Madol? Or did it exist here once but the respective microorganisms have since somehow gone extinct? The lack of notable coal deposits in the island’s geological formations may be evidence of the latter, pointing towards this being a fairly recent development. It seems almost like time on the island is moving backwards.
