Overview

Puddlespore is a floating lava mollusk of the Magmoor Caverns on Tallon IV. Its body remains sealed inside an impenetrable shell while it drifts in molten channels. At a distance it can resemble a dark stone mass on the lava surface; its identity becomes clear when the shell opens, exposing a mantle beneath a patterned upper surface.

The organism does not open as a feeding display. When another body approaches, it expands the shell opening to appear larger. If that approach continues, the shell snaps shut and ejects harmful energy globules. Its behavior is defensive and positional: it holds its place in the lava while turning the surrounding basin into an intermittent range hazard.

Puddlespore is distinct from superficially similar plantlike records. It is a mollusk, not a fungus or a rooted spore organism. The closest useful comparisons are the shell-bearing Dark Phlogus and the large Brinstar Spore Spawn, but their appearances do not establish a shared species or tissue structure.

Shell And Mantle

The shell is the defining protective structure. When closed it is effectively impenetrable in the documented environment, allowing the animal to float through severe heat without presenting an obvious vulnerable surface. The foul odor reported from within the shell is a reliable identification cue, but its composition and biological purpose have not been confirmed.

The mantle is exposed only when the animal opens. A direct impact there can overturn the body into a defensive inverted position. That inversion does not destroy the mollusk; it changes the shell orientation for a short interval and exposes a flat enough upper surface to alter a hazardous crossing. Once the animal rights itself, the route changes again.

Magmoor Range

Confirmed range is restricted to Magmoor lava pools and geothermal corridors rather than the full Tallon IV biosphere. The organism is closely tied to liquid lava and has been observed in crossing basins where a stable path is otherwise absent. It should therefore be treated as part of the local physical landscape, not as a roaming predator moving between dry areas.

The nearby Magmoor record helps define the wider thermal environment, but it should not be used to infer the Puddlespore diet or lifecycle. Extreme heat explains where the mollusk can remain; it does not explain what resources it uses or how a new individual reaches a separate lava channel.

Defensive Behavior

The opening display is a warning and should not be read as a willingness to pursue. Puddlespore stays in the lava and reacts to a close threat by closing hard enough to send energy globules across the surface. That pattern creates an interval of risk around the body rather than a long chase behavior.

A field team should record shell state, mantle exposure, lava current, and the viable route around the animal before modifying the encounter. The animal is most useful as an environmental indicator when left undisturbed; repeatedly provoking the opening display converts a stable obstacle into a recurrent projectile source.

Evidence And Limits

The archive supports a Tallon IV Magmoor range, lava flotation, impenetrable shell, foul internal odor, opening display, mantle exposure, defensive inversion, and harmful energy globules. It does not support an inferred diet, a reproductive cycle, a universal social behavior, or a claim that the organism actively seeks prey.

Future analysis should sample residue from an unoccupied shell surface and observe a free-floating specimen over a complete thermal cycle. Until then, Puddlespore is best treated as a specialized lava mollusk whose shell mechanics create a precise and changing environmental hazard.