| Palaeoaplysina Temporal range: | |
|---|---|
| Scientific classification | |
| Clade: | Archaeplastida |
| Division: | Rhodophyta |
| Class: | Florideophyceae |
| Stem group: | Corallinales |
| Order: | † Archaeolithophyllales (?) |
| Family: | † Palaeoaplysinaceae |
| Genus: | † Palaeoaplysina |
Palaeoaplysina is a genus of tabular, calcified fossils that are a component of many Late Palaeozoic reefs. [1] The fossil acted as a baffle to trap sediment. Historically interpreted as a sponge or hydrozoan, [2] recent studies are converging to its classification in the coralline stem group, placing it among the red algae. [1]
The thalloid organism had a series of internal canals opening on one side of the body (presumably the upper side), and volcano-like protuberances on that same side inviting comparison to filter-feeding organisms. On the other hand, it seems to have had a calcified cellular make up akin to that of the coralline reds, suggesting that it was either a stem-group coralline or a coralline-encrusted filter feeder. [3]
The organism is widespread in the tropical and near-tropical margin of the Laurentian continent (45–15°N), but is not found elsewhere. [4] Its oldest reported occurrence is Middle Pennsylvanian (mid- to late Moscovian) [5] and youngest is the late Sakmarian. [3] It acts as an important reservoir rock for oil deposits. [3]