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Pohlsepia mazonensis is a species of fossil organism with unknown affinity. Although it was originally identified as an extinct cephalopod,[1] later studies denied that interpretation.[2][3] The species is known from a single exceptionally preserved fossil discovered in the late Carboniferous (Pennsylvanian) Francis Creek Shale (Mazon Creek fossil beds) of the Carbondale Formation, north-east Illinois, United States.[1]
| Pohlsepia Temporal range: | |
|---|---|
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Genus: | †Pohlsepia |
| Species: | †P. mazonensis |
| Binomial name | |
| †Pohlsepia mazonensis Kluessendorf & Doyle, 2000 | |
Pohlsepia mazonensis is named after its discoverer, James Pohl, and the type locality, Mazon Creek. Its habitat was the shallows seawards of a major river delta in what at that time was an inland ocean between the Midwest and the Appalachians. In its initial description, it was considered to be the oldest known octopus,[1] but later studies have considered this classification dubious.[2] In 2022, it was even suggested that it may not be a mollusk.[3]
The type specimen is reposited at the Field Museum of Natural History in Chicago, Illinois.[1]
The Pohlsepia mazonensis fossil found by James Pohl is the only known example of the species. Most notably, the fossil has ten arms. The extra two arms are shorter, while the other eight are similar in length.[4]
The 3.5 cm (1.4 in) wide fossil is “sack-shaped” with indistinct features including a poorly defined head. While it is unclear, one of these features could be an ink sac. The fossil lacks arm hooks and suckers and all of these factors combine to make the assigning of the order Cirroctopoda controversial.[5]
Genus name Pohlsepia is came from its discoverer James Pohl. He is the son of Joe Pohl and together they have collected fossils in the Mazon Creek area. Originally from Wisconsin and Minnesota, Pohl is a native Midwesterner. He and his father have donated their fossils to museums in the area, including Pohlsepia mazonensis to the Field Museum.[4]
In 2000, Joanne Kluessendorf assigned Pohlsepia mazonensis to the order Cirroctopoda. Many other researchers disagreed, citing the lack of internal structure. The possible evidence of fins and the huge time difference between the Pohlsepia mazonensis fossil and first confirmed cirrate octopus fossils is problematic. However, the species can be classified as an octopod. Despite the number of arms being unclear, the fact that the fossil has an indistinct head, sac like body and similar fins to cirrate octopods gives enough evidence to classify Pohlsepia mazonensis in the order Cirroctopoda.[5]
When looking at the groups Teudopsidae, Trachyteuthididae, the Vampyromorpha, cirrate octopods, incirrate octopods and the fossil Loligosepiina, the describing authors proposed that Pohlsepia mazonensis would be most closely related to the octopods based on its lack of a shell.[5]
However, later studies found the placement within Octopoda to be dubious, due to the fossils poor preservation, and the fact that other fossils have now shown true octopuses to have first arisen in the Jurassic.[2] In 2021, it is considered that is even unlikely to be cephalopod or mollusk. Lack of a shell is a highly unlikely combination in a Carboniferous cephalopod. In addition, its appendages lack hooks, suckers, cirri, an arm web, and the characteristic 8/10 arm count. There is neither a beak, unambiguous ink sac, nor radula. The bulbous body outline and presence of appendages more likely to show the affinity as a cnidarian, a phylum of invertebrate animals including jellyfish and sea anemones.[3] In 2019, fossils included some fossils including ones from Mazon Creek like vertebrates, Tullimonstrum, and Pohlsepia are examined, to consider affinity of Tullimonstrum. Although this study treated Pohlsepia as cephalopod, melanosomes cannot be identified from its eyespot.[6]
Located in what is currently northern Illinois, the Mazon Creek preserved the Pohlsepia mazonensis fossil extraordinarily. The Pohlsepia mazonensis fossil was found specifically in the Pit 11 region, within the Francis Creek Shale Member.[7] Like most soft tissue fossils found in Mazon Creek, it is preserved as a 2D light-on-dark discolouration of the matrix.[8] The Francis Creek Shale Member of the Carbon Formation has a diverse array of preserved plants and animals.[9]
Previously, it was thought that these organisms were immediately killed and buried in storm surges, where bursts of water would submerge the organisms in sediments, creating an environment where their remains were protected from scavengers before most decomposition could start.[9] However, there is limited geological evidence for the hypothesis of storm surges, and the kill mechanism in the Mazon Creek is not fully understood but high sedimentation could have choked, killed, and buried organisms rapidly [8]
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