Flagellopantopus
| Flagellopantopus Temporal range:
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| Diagrammatic Reconstruction of F. blocki | |
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| World map of the lower Devonian (400 mya), roughly the same age as the Hunsrück Slate | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Arthropoda |
| Subphylum: | Chelicerata |
| Class: | Pycnogonida |
| Genus: | †Flagellopantopus Poschmann & Dunlop, 2006 |
| Species: | †F. blocki
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| Binomial name | |
| †Flagellopantopus blocki Poschmann & Dunlop, 2006
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Flagellopantopus is an extinct genus of pycnogonid (sea spider) arthropod known from the lower Devonian aged Hunsrück Slate. A single species is currently known, Flagellopantopus blocki, which was described from the Emsian aged Kaub Formation in Germany.
F. blocki differs from other members of the pycnogonida by possessing an extremely elongated telson, which was flagelliform in appearance. This animal was fairly large for a pycnogonid, with the whole body of the arthropod measuring around 26 mm (2.6 cm) long, while the telson itself was around 66 millimeters (6.6 cm) long. In it's 2006 description, Poschmann and Dunlop placed Flagellopantopus into the order Pantopoda (which includes modern sea spiders). However, later publications have put doubt on this interpretation, and have suggested a new placement as a member of Pycnogonida incertae sedis. It is currently assumed to have lived a benthic lifestyle, as it lacks the flattened appendages and setae that pelagic species of pycnogonids typically have.
Discovery and naming
[edit]The holotype (and only known) specimen of this pycnogonid, NHMMZ PWL 2004/5024-LS, was first described by Poschmann in 2004 for Project Nahecaris,[a] but was considered a nomen nudum due to the lack of a diagnosis.[1] The specimen would later be given a proper diagnosis and description in 2006.[1] The holotype specimen originates from the Kaub Formation, which is dated to the Emsian stage of the lower Devonian, but the exact locality of origin is uncertain.[2] Poschmann and Dunlop (2006) states that the fossil was recovered from the Wingertshell Member, within the larger Obereschenbach quarry, near the municipality of Bundenbach.[1] However, the administration housing the fossil, the Naturhistorisches Museum Mainz, states that the specimen originates from the Eschenbach-Bocksberg quarry.[2]
The arthropods genus name, Flagellopantopus, is derived from the latin word flagella, meaning "whip", which was named after the elongated telson possessed by the genus, and the pycnogonid order Pantopoda, which is derived from the latin words pant and poda, meaning "all feet".[3][4][1] The specific name, blocki, is in honour of Helmut Block, who donated the holotype for public viewing and research.[1]
Description
[edit]Flagellopantopus was fairly large compared to other pycnogonids, with the whole body of the arthropod measuring around 26 mm (2.6 cm) long.[1] Like most other pycnogonids, this genus possessed four pairs of walking legs that had a 90 mm (9 cm) arm-span.[5][1] The legs follow a similar pattern to other sea spiders, with the chelifores coming first, followed by the pedipalps, and then finally the ovigers (which end in a terminal claw).[6] The proboscis of this taxon is partially obscured, and how it connected to the rest of the cephalic region is uncertain.[2] The proboscis itself had a pyriform appearence, and was roughly 6 mm (0.6 cm) long, and had a width of around 4 mm (0.4 cm) wide.[1] By far the most distinguishing trait of this taxon was its extremely elongated telson, which measured around 66 millimeters (6.6 cm) long, nearly three times longer than the arthropods whole body.[1][2]
Classification
[edit]Although they are often colloquially known as "sea spiders", pycnogonids are not closely related to them and other arachnids.[7] However, their placement as basal members of the Chelicerata subphylum means that they are more closely related to them then to other groups.[7] Flagellopantopus is confidently classified within the Pycnogonida, however its further placement is uncertain.[2] Both Poschmann (2004) and Poschmann and Dunlop (2006) placed this taxon as a relatively basal member of the Pantopoda order (which includes all crown-group sea spiders) on the basis of its long telson, which is lost in more derived taxa.[1] However, they classified this taxon as more derived than another contemporary pycnogonid, Palaeoisopus problematicus, due to Flagellopantopus possessing a less well developed abdomen, which is a derived trait in crown-group pycnogonids.[8][1] However, later studies, including Sabroux et al. (2024) have suggested that not only was Flagellopantopus not a member of Pantopoda, but the entire order did not exist during the Devonian.[2] They instead classified this taxon, and the other known Hunsrück pycnogonids into two different morphological groups separate from the Pantopoda.[2]
Paleoecology
[edit]The Hunsrück Slate is deposited within the regions of Hunsrück and Taunus within the country of Germany.[9] Although debates still stand about the exact depth of the ecosystem during the Devonian, most recent studies have suggested a maximum depth of around 100 meters (328.084 feet) deep, within the Epipelagic zone.[10] Due to the fact that Flagellopantopus possessed chelifores, it is likely that it was not restricted to feeding on sessile organisms, which is common in modern representatives.[10][2] It is also likely that it lived a fully benthic lifestyle, as it lacks the broad legs and long setae usually associated with swimming pycnogonids.[2] The telson of this taxon most likely would've acted as a sensory structure, as it was probably too stiff to help with locomotion in the water column.[2][1]
A plethora of other organisms are known to lived alongside Flagellopantopus, including other arthropods, echinoderms, placoderms, agnathans, and various other groups.[9] Some notable examples of contemporary genera include the peytoiid radiodont Schinderhannes bartelsi,[11] the marrellomorphid arthropods Mimetaster hexagonalis and Vachonisia rogeri,[12] as well as the various placoderms of the bizarre Pseudopetalichthyida order (which are only found at Hunsrück).[13] Also found in the area are various other pycnogonids, including Palaeopantopus maucheri,[14] Pentapantopus vogteli,[8] Palaeothea devonica,[14] and the afformentioned Palaeoisopus problematicus.[14] The level of pycnogonid genera found at the Hunsrück Slate makes it the most diverse assemblage of fossil pycnogonids yet discovered.[2]
Notes
[edit]- ^ Project Nahecaris, which was named after the phyllocarid crustacean Nahecaris, is an internationally funded program dedicated to studying the fauna and overall geologic significance of the Hunsrück Slate.
References
[edit]- ^ a b c d e f g h i j k l Poschmann, Markus; Dunlop, Jason A. (2006). "A new sea spider (Arthropoda: Pycnogonida) with a flagelliform telson from the Lower Devonian Hunsrück Slate, Germany". Palaeontology. 49 (5): 983–989. Bibcode:2006Palgy..49..983P. doi:10.1111/j.1475-4983.2006.00583.x.
- ^ a b c d e f g h i j k Sabroux, R.; Garwood, R. J.; Pisani, D.; Donoghue, P. C. J.; Edgecombe, G. D. (2024). "New insights into the Devonian sea spiders of the Hunsrück Slate (Arthropoda: Pycnogonida)". PeerJ. 12. e17766. doi:10.7717/peerj.17766. PMC 11485130. PMID 39421419.
- ^ "Pantopoda". Merriam-Webster.com Dictionary. Merriam-Webster.: "taxonomic synonym of Pycnogonida < Neo-Latin, from pant- + -poda"
- ^ "Definition of FLAGELLA". www.merriam-webster.com. Retrieved 2024-11-01.
- ^ Ruppert, Edward E. (1994). Invertebrate Zoology. Barnes, Robert D. (6th ed.). Fort Worth, TX: Saunders College Pub. ISBN 0-03-026668-8. OCLC 30544625.
- ^ Phylogenomic Resolution of Sea Spider Diversification through Integration of Multiple Data Classes
- ^ a b Dunlop, J. A.; Arango, C. P. (2005). "Pycnogonid affinities: A review". Journal of Zoological Systematics and Evolutionary Research. 43: 8–21. CiteSeerX 10.1.1.714.8297. doi:10.1111/j.1439-0469.2004.00284.x.
- ^ a b Kühl, Gabriele; Poschmann, Markus; Rust, Jes (May 2013). "A ten-legged sea spider (Arthropoda: Pycnogonida) from the Lower Devonian Hunsrück Slate (Germany)". Geological Magazine. 150 (3): 556–564. Bibcode:2013GeoM..150..556K. doi:10.1017/S0016756812001033. S2CID 129801458.
- ^ a b Wilkin, Jack T. R. (March 2023). "The Hunsrück Slate Konservat-Lagerstätte: The Hunsrück Slate Konservat-Lagerstätte". Geology Today. 39 (2): 72–76. doi:10.1111/gto.12426. ISSN 0266-6979.
- ^ a b Rust, Jes; Bergmann, Alexandra; Bartels, Christoph; Schoenemann, Brigitte; Sedlmeier, Stephanie; Kühl, Gabriele (2016). "The Hunsrück biota: A unique window into the ecology of Lower Devonian arthropods". Arthropod Structure & Development. 45 (2): 140–151. Bibcode:2016ArtSD..45..140R. doi:10.1016/j.asd.2016.01.004. ISSN 1873-5495. PMID 26826500.
- ^ Gabriele Kühl; Derek E. G. Briggs & Jes Rust (2009). "A great-appendage arthropod with a radial mouth from the Lower Devonian Hunsrück Slate, Germany". Science. 323 (5915): 771–773. Bibcode:2009Sci...323..771K. doi:10.1126/science.1166586. PMID 19197061. S2CID 47555807.
- ^ Stürmer, W; Bergström, J (1976). "The arthropods Mimetaster and Vachonisia from the Devonian Hunsrück Shale". Paläontologische Zeitschrift. 50 (1): 78–111. Bibcode:1976PalZ...50...78W. doi:10.1007/bf03001974.
- ^ Denison, Robert (1978). Placodermi. Handbook of Paleoichthyology. Vol. 2. Stuttgart New York: Gustav Fischer Verlag. pp. 22–23. ISBN 978-0-89574-027-4.
- ^ a b c Bergström, Jan; Stürmer, Wilhelm; Winter, Gerhard (1980-06-01). "Palaeoisopus, Palaeopantopus and Palaeothea, pycnogonid arthropods from the Lower Devonian Hunsrück Slate, West Germany". Paläontologische Zeitschrift. 54 (1–2): 7–54. Bibcode:1980PalZ...54....7B. doi:10.1007/BF02985882. S2CID 86746066.