Diplochaetetes longitubus

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Diplochaetetes longitubus
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Annelida
Clade: Pleistoannelida
Subclass: Sedentaria
Order: Terebellida
Family: Cirratulidae
Genus: Diplochaetetes
Species:
D. longitubus
Binomial name
Diplochaetetes longitubus
Weissermel, 1913

Diplochaetetes longitubus is an extinct species of cirratulid polychaete within the genus Diplochaetetes known from Namibian sedimentary rocks dating back to the Eocene. [1] It was initially described as a tabulate coral, but research carried out on present-day Dodecaceria aggregates and Diplochaetetes mexicanus fossils from the pacific coasts of the Americas has led researchers to classify the entire genus as cirratulid polychaetes. [2] [3] [4] For many decades, they've also been erroneously attributed to sponges. [5]

A subspecies named Diplochaetetes longitubus vermicularis was also later described from Eocene Namibian sediments. [6]

Although present-day Dodecaceria and fossil Diplochaetetes aggregates from Peru have been confirmed to show identical double-phased biomineralization characteristics, [7] no detailed analysis has been performed on their Namibian counterparts so it's unclear whether the trait is shared on a broad genus basis.

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Diplochaetetes is an extinct genus of marine polychaete worms in the family Cirratulidae. It was initially described as a tabulate coral, and later classified as a sponge. Later studies provided significant evidence that Diplochaetetes fossils are bioconstructions attributable to cirratulid polychaetes due to their strong similarity with modern Dodecaceria aggregates. Both fossil Diplochaetetes and recent Dodecaceria bioconstructions retain identical double-phased biomineralization characteristics, but the possible synonymity of these genera is currently subject to debate.

<i>Diplochaetetes mexicanus</i> Species of annelid worms

Diplochaetetes mexicanus is an extinct species of cirratulid polychaete within the genus Diplochaetetes from the Pacific coasts of the Americas, found mostly in Oligocene and Miocene sedimentary rocks. Its first reported occurrence was in Baja California sediments, hence the name. Later findings have extended its paleogeographic distribution up to Peru. Initially described as a sponge, the similarity of these aggregates with present-day Dodecaceria bioconstructions from the exact same areas has led researchers to classify these fossils as cirratulid bioconstructions. Both fossil Diplochaetetes and recent Dodecaceria bioconstructions retain identical double-phased biomineralization characteristics, but the possible synonymity of these species is currently subject to debate.

References

  1. Weissermel W (1913). "Uber tertiäre Versteinerungen von den Bogenfelser Diamantfeldern II. Tabulaten und Hydrozoen". Beiträge zur geologischen Erforschung der deutschen Schutzgebiete. 5: 84–111.
  2. Reish DJ (1952). "Discussion of the colonial tube-building polychaetous annelid Dodecaceria fistulicola Ehlers". Bulletin of the Southern California Academy of Sciences. 51: 103–107. doi:10.3160/0038-3872-51.3.103.
  3. Fischer R, Galli Oliver C, Reitner J (1989). "Skeletal structure, growth, and paleoecology of the patch reef-buildingpolychaete worm Diplochaetetes mexicanus wilson, 1986 from the oligocene of baja california (Mexico)". Geobios. 22 (6): 761–775. Bibcode:1989Geobi..22..761F. doi:10.1016/S0016-6995(89)80071-3.
  4. Fischer R, Pernet B, Reitner, J (2000). "Organomineralization of cirratulid annelid tubes-fossil and recent examples". Facies. 42 (1): 35–49. Bibcode:2000Faci...42...35F. doi:10.1007/BF02562565. S2CID   128949856.
  5. Wilson EC (1986). "The first tertiary sclerosponge from the Americas". Palaeontology. 29(3): 577–583.
  6. Weissermel W (1926). "Neues uber Tabulaten, Hydrozoen und eine Hexakoralle aus dem Tertiar der Bogenfelser Diamantenfelder". Die Diamantenwuste Sudwest-Afrikas. (ed Kaiser, H.). 2: 88–106.
  7. Guido A, D'Amico F, DeVries TJ, Kočí T, Collareta A, Bosio G, Sanfilippo R (2024). "Double-phased controlled and influenced biomineralization in marine invertebrates: The example of Miocene to recent reef-building polychaete cirratulids from southern Peru". Palaeogeography, Palaeoclimatology, Palaeoecology. 639: 112060. Bibcode:2024PPP...63912060G. doi:10.1016/j.palaeo.2024.112060. S2CID   267306998.