Draft:Macromyzon

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Draft:Macromyzon

Macromyzon
Temporal range: Llandovery Epoch (Telychian-Lower Sheinwoodian) 438.5–433.4 Ma
Fossil holotype of M. siluricus (UWGM 7056)
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Annelida
Clade: Pleistoannelida
Clade: Sedentaria
Class: Clitellata
Subclass: Hirudinea
Genus: †Macromyzon
De Carle et al., (2025)
Species:
†M. siluricus
Binomial name
†Macromyzon siluricus
De Carle et al., (2025)

Macromyzon (meaning "large sucker") is a genus of basal hirudinean (leech) annelid known from the lower Silurian aged Waukesha Biota. A single species is currently known, Macromyzon siluricus, which was discovered in strata belonging to the Telychian aged Brandon Bridge Formation in Wisconsin. Originally discovered alongside the Waukesha Biota in 1985, this taxon wouldn't be properly described until 2025. The description paper, which was published by De Carle et al., (2025), found that this taxon was a member of the hirudinean stem-group, splitting off before crown-group leeches evolved.

This taxon is rather significant, as not only does it represent the oldest known leech in the fossil record, but it also represents the oldest known complete body fossil from the group, as well as the earliest uncontested appearance of the clitellata in general. This taxon also represents the first time that any of the worms from the Waukesha Biota have been properly described in detail and helps to further increase the known diversity of organisms from the site. Its discovery also pushes back the origins of the hirudinea by more than a hundred million years, showing that they originated in marine environments. De Carle et al., (2025) also found that instead of being hematophagous, this taxon most likely hunted, and consumed live prey, in contrast to previous assumptions on hirudinean evolution, in that they fed on the blood of early vertebrates.

Background

The Brandon Bridge Formation is a geologic formation within the state of Wisconsin that dates to the Lower Silurian (more specifically the Telychian and Sheinwoodian stages).[1][2] Within the formation exists the smaller Waukesha Biota, a Konservat-Lagerstätten fossil site known for its exceptional preservation of soft-bodied and lightly sclerotized organisms that are not normally found in Silurian strata.[3] The biota itself is found within a 12 cm (4.7 in) layer of thinly-laminated, fine-grained, shallow marine sediments consisting of mudstone and dolomite deposited within a sedimentary trap at the end of an erosional scarp over the eroded dolomites of the Schoolcraft and Burnt Bluff Formations.[2] The site itself is known from two quarries; one in Waukesha county, and the other in the city of Franklin, in Milwaukee County.[3][1] The two faunas are almost identical to one another, with the exception being that the Franklin quarry lacks any fossils of trilobites.[3][4] A unique trait of the biota is its taphonomy, being that the majority of hard-shelled organisms (which are normally found in Silurian strata), are poorly preserved, or entirely absent.[3] With the exceptions to this being the various trilobites and conulariids (a group of cnidarians with pyramidal theca) from the site.[3] The exceptional preservation of non-biomineralized and lightly sclerotized remains of the Waukesha Biota is generally attributed to a combination of favorable conditions, including the transportation of organisms to a sediment trap that helped to protect from scavengers, and promoted the buildup of organic films that coated the surfaces of the dead organisms, which inhibited decay, sometimes enhanced by promoting precipitation of a thin phosphatic coating, which is observed on many of the fossils.[5][6] However, some of the fossils are also coated with other materials, including pyrite and calcium carbonate.[3][4][7]

Ironically, Macromyzon was not the first vermiform taxon from the Waukesha Biota to be labeled as a leech, as another fossil (UWGM 2422) was also placed within the hirudinea in multiple papers.[1][2][8] However, more recent studies, including Shcherbakov et al. (2020) and Braddy, Gass & Tessler (2023), instead interpreted the fossil as molted remains belonging to an unidentified member of the cycloneuralia, and that the 'suckered end' seen in the specimen was instead a breakage point in the molt.[9][10]

Discovery and naming

The type specimen of M. siluricus, including close ups of the fossil, the pattern of segmentation (E), and comparisons to the extant genera Myxobdella and Haementeria (F and G respectively).

The holotype, and only known specimen of Macromyzon, catalogued as UWGM 7056, was discovered within the 'West Quarry' near the city of Waukesha, which is owned and operated by the Waukesha Lime and Stone Company.[1] Like with the majority of the fossils known from the site, the holotype specimen is housed within the collections of the UW Madison Geology Museum.[1][4] However, as with the majority of the taxa known from the Waukesha fauna, this species wouldn't be properly described for several decades.[1] Its description marks the first time that any of the worm fossils from the site have been properly named and analyzed thoroughly.[1][10] According to the description study, the fossil was prepared using a freeze-thaw method to help split the dolostone containing the holotype.[1] Curiously, it seems several earlier studies that predate the annelids description in 2025 suggested that it may have been a poriferan, or a poriferan-like organism, before its more confident placement in the hirudinea stem-group.[11]

This leeches genus name, Macromyzon, is derived from the greek words, makros, meaning "large", and myzon, meaning "sucker".[1] The species name siluricus, is derived from the Silurian period, when the taxa of the Waukesha Biota were deposited.[1]

Significance

Macromyzon represents a unique discovery, as it casts doubt on many long-held theories on the evolution of leeches, including their environmental origins and their lifestyles. For one, this taxon represents not only the oldest confirmed member of the hirudinea yet known, but also of the clitellata in general, and pushes back the origins of the group by more than a hundred million years earlier than their previously oldest uncontested occurrences in the Permian of South Africa and Kazakhstan.[1][12][13] However, De Carle et al., (2025) speculates that the hirudinea may have originated earlier on in the Paleozoic.[1] Macromyzon also represents the oldest confirmed body fossil from the group, as many of the other fossil specimens known represent egg carrying cocoons, and thus are harder to confidently be assigned as belonging to leeches and not from other clitellate groups.[1][14] This taxon also shows that early leeches seemingly evolved from more basal annelids in marine environments before transitioning to freshwater areas, meaning that crown leeches living in freshwater areas most likely represents a derived condition for the group.[1] It also helps strengthen the theory that the acanthobdellida and branchiobdellida, two groups of clitellates that branched off before true leeches evolved, may represent transitions into freshwater that are independent to that of the euhirudineans (true leeches).[1][15] The diet of this Silurian taxon is also of great importance, as it was once assumed that early leeches were already hematophagous, and targeted early vertebrates.[1] However, the lack of crown-group vertebrates from the Waukesha Biota, and the rare occurrence of jawless vertebrates like conodonts from the site, indicates that Macromyzon was either most likely hunting live prey, or was a parasite to the various contemporary invertebrates.[1][16] This seemingly lines up with most modern taxa being primarily carnivorous, and the groups that are blood-feeding ectoparasites seemingly represent a derived condition in true leeches.[1][17]

Paleobiology and paleoecology

Life reconstruction of M. siluricus

Macromyzon held a very curious niche within the shallow lagoons of Silurian Waukesha, as instead of being a blood feeding parasite of early gnathostomes like what was once believed, this basal leech was most likely a carnivorous predator within its environment. Considering its size, it's likely that this annelid held a niche as a dominant predator within its environment, due to the relatively small size of the majority of the contemporary fauna. Its appearance in shallow marine areas, while not unique among hirudineans, indicates that this leech was acclimated to living in fully saltwater areas, and that the appearance of leeches in freshwater and terrestrial areas was a more derived radiation later on in the group's evolution.

During the lower Silurian, the area that would become the Waukesha Biota was a shallow peritidal environment.[2][3] The preservational area of the region was most likely anoxic, and in combination with oceanic currents, helped to preserve the organisms from the ecosystem.[3] The conditions of the sediments were similar to a Winogradsky column, as the various levels of bacteria within the sediments helped entomb and preserve the fossils free of the risk of scavenging.[3] Some notable contemporary organisms include various arthropods (phyllocarids, thylacocephalans, etc.) paleoscolecids, lobopodians, other annelids, poriferans, conodonts, and various other groups.[2][16][18]



References

  1. ^ a b c d e f g h i j k l m n o p q r de Carle, D.; Iwama, R. E.; Wendruff, A. J.; Babcock, L. E.; Nanglu, K. (2025). "The first leech body fossil predates estimated hirudinidan origins by 200 million years". PeerJ. 13 e19962. doi:10.7717/peerj.19962. PMC 12495953. PMID 41048386.
  2. ^ a b c d e Mikulic, Donald G.; Briggs, D.E.G.; Kluessendorf, Joanne (1985). "A new exceptionally preserved biota from the Lower Silurian of Wisconsin, U.S.A." Philosophical Transactions of the Royal Society of London B. 311 (1148): 75–85. Bibcode:1985RSPTB.311...75M. doi:10.1098/rstb.1985.0140. JSTOR 2396972.
  3. ^ a b c d e f g h i Wendruff, Andrew J.; Babcock, Loren E.; Kluessendorf, Joanne; Mikulic, Donald G. (2020). "Paleobiology and Taphonomy of exceptionally preserved organisms from the Waukesha Biota (Silurian), Wisconsin, USA". Palaeogeography, Palaeoclimatology, Palaeoecology. 546 109631. Bibcode:2020PPP...54609631W. doi:10.1016/j.palaeo.2020.109631. S2CID 212824469.
  4. ^ a b c Randolfe, E. A.; Gass, K. C. (2024). "Waukeshaaspis eatonae n. gen. n. sp.: a specialized dalmanitid (Trilobita) from the Telychian of southeastern Wisconsin". Journal of Paleontology. 98 (5): 821–829. Bibcode:2024JPal...98..821R. doi:10.1017/jpa.2024.32.
  5. ^ Wendruff, Andrew J.; Babcock, Loren E.; Wirkner, Christian S.; Kluessendorf, Joanne; Mikulic, Donald G. (2020). "A Silurian ancestral scorpion with fossilised internal anatomy illustrating a pathway to arachnid terrestrialisation". Scientific Reports. 10 (14): 14. Bibcode:2020NatSR..10...14W. doi:10.1038/s41598-019-56010-z. PMC 6965631. PMID 31949185.{{cite journal}}: CS1 maint: unflagged free DOI (link)
  6. ^ Jones, Wade T.; Feldman, Rodney M.; Schweitzer, Carrie E. (2015). "Ceratiocaris from the Silurian Waukesha Biota, Wisconsin". Journal of Paleontology. 89 (6): 1007–1021. Bibcode:2015JPal...89.1007J. doi:10.1017/jpa.2016.22. S2CID 131127241.
  7. ^ Gass, Kenneth C.; Braddy, Simon J. (2023). "The Waukesha Biota: a wonderful window into early Silurian life". Geology Today. 39 (5): 169–176. Bibcode:2023GeolT..39..169G. doi:10.1111/gto.12447. ISSN 0266-6979.
  8. ^ Thorp, James H.; Covich, Alan P. (2001). Ecology and Classification of North American Freshwater Invertebrates. Academic Press. p. 466. ISBN 978-0-12-690647-9.
  9. ^ Shcherbakov, Dmitry; Tarmo, Timm; Tzetlin, Alexander B.; Vinn, Olev; Zhuravlev, Andrey (2020). "A probable oligochaete from an Early Triassic Lagerstätte of the southern Cis-Urals and its evolutionary implications". Acta Palaeontologica Polonica. 65 (2): 219–233. doi:10.4202/app.00704.2019. S2CID 219097612.
  10. ^ a b Braddy, Simon J.; Gass, Kenneth C.; Tessler, Michael (2023). "Not the first leech: An unusual worm from the early Silurian of Wisconsin". Journal of Paleontology. 97 (4): 799–804. Bibcode:2023JPal...97..799B. doi:10.1017/jpa.2023.47.
  11. ^ Westberg, Märta (2019). "Enigmatic worm-like fossils from the Silurian Waukesha Lagerstätte, Wisconsin, USA". Dissertations in Geology at Lund University.
  12. ^ Prevec, Rosemary; Nel, André; Day, Michael O.; et al. (2022-10-30). "South African Lagerstätte reveals middle Permian Gondwanan lakeshore ecosystem in exquisite detail". Communications Biology. 5 (1): 1154. doi:10.1038/s42003-022-04132-y. PMC 9618562. PMID 36310243.{{cite journal}}: CS1 maint: unflagged free DOI (link)
  13. ^ Shcherbakov, Dmitry E.; Timm, Tarmo; Dantes, Olga V.; Zhuravlev, Andrey Yu (2025-09-29). "The oldest oligochaete cocoons (former cladocerans) from the upper Permian (Lopingian) freshwater Karaungir Lagerstätte of eastern Kazakhstan". Journal of Paleontology: 1–16. doi:10.1017/jpa.2025.10161. ISSN 0022-3360.
  14. ^ Bomfleur, Benjamin; Kerp, Hans; Taylor, Thomas N.; Moestrup, Øjvind; Taylor, Edith L. (2012-12-18). "Triassic leech cocoon from Antarctica contains fossil bell animal". Proceedings of the National Academy of Sciences of the United States of America. 109 (51): 20971–20974. doi:10.1073/pnas.1218879109. ISSN 1091-6490. PMC 3529092. PMID 23213234.
  15. ^ Tessler, Michael; de Carle, Danielle; Voiklis, Madeleine L.; Gresham, Olivia A.; Neumann, Johannes S.; Cios, Stanisław; Siddall, Mark E. (2018-10-01). "Worms that suck: Phylogenetic analysis of Hirudinea solidifies the position of Acanthobdellida and necessitates the dissolution of Rhynchobdellida". Molecular Phylogenetics and Evolution. 127: 129–134. doi:10.1016/j.ympev.2018.05.001. ISSN 1055-7903.
  16. ^ a b Murdock, Duncan J. E.; Smith, M. Paul (2021). "Panderodus from the Waukesha Lagerstätte of Wisconsin, USA: a primitive macrophagous vertebrate predator". Papers in Palaeontology. 7 (4): 1977–1993. doi:10.1002/spp2.1389. S2CID 237769553.
  17. ^ Phillips, Anna J.; Govedich, Fredric R.; Moser, William E. (2020-09-19). "Leeches in the extreme: Morphological, physiological, and behavioral adaptations to inhospitable habitats". International Journal for Parasitology: Parasites and Wildlife. 12: 318–325. doi:10.1016/j.ijppaw.2020.09.003. PMC 7569739. PMID 33101909.
  18. ^ Gass, Kenneth C.; Braddy, Simon J. (2023). "The Waukesha Biota: a wonderful window into early Silurian life". Geology Today. 39 (5): 169–176. Bibcode:2023GeolT..39..169G. doi:10.1111/gto.12447. ISSN 0266-6979.

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