Diplurus

In this article we will explore various facets related to Diplurus, a topic that has captured the attention and interest of people around the world. Since its emergence, Diplurus has sparked curiosity and debate, and its impact has been felt in different areas of society. Throughout this writing, we will immerse ourselves in the analysis and reflection on Diplurus, addressing its implications, its evolution over time and its relevance today. Through this article, we seek to provide a comprehensive and enriching view on Diplurus, with the goal of giving the reader a deeper and more nuanced understanding of this highly relevant topic.

Diplurus
Temporal range: Norian-Pliensbachian
Fossil
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Sarcopterygii
Class: Actinistia
Order: Coelacanthiformes
Family: †Mawsoniidae
Genus: †Diplurus
Newberry, 1878
Species
  • D. longicaudatus
  • D. newarki
  • D. uddeni
  • D. enigmaticus

Diplurus is a genus of prehistoric mawsoniid coelacanth fish which lived during the Late Triassic-Early Jurassic period in North America.[1] The fossils of this genus are common on the eastern North American Margin, being a key taxon of the Newark Supergroup, and recovered from units such as the Bull Run Formation (Norian, Virginia), Lockatong Formation (Norian, Pennsylvania), Stockton Formation (Norian, New Jersey), Solite Quarry (Norian, North Carolina-Virginia), Midland Formation (Hettangian, Virginia), East Berlin Formation (Hettangian, Connecticut), Boonton Formation (Sinemurian, New Jersey) and the Portland Formation (Hettangian-Pliensbachian, Connecticut).[2] Three species are know, the type D. longicaudatus (Newberry, 1878), the youngest and biggest, D. newarki, (Bryant in 1934) the oldest, followed then by "D. uddeni" (Eastman), also from older rocks and considered dubious. A recent work has recovered a 3rd or 4th species, D. enigmaticus, from the Late Triassic of New Jersey, representing another small-bodied form living in sympatry with the similarly sized D. newarki.[2] This genus ranges in size from 15 cm of D. newarki and D. enigmaticus in New Jersey to the larger 60 cm specimens of Diplurus longicaudatus found in the Connecticut River Valley, which indicates a considerable growth and likely a change in the ecological position of the genus to a possible apex predatory niche.[3]

Paleoenvironment

Diplurus represents a freshwater taxon that inhabited the fluvial, palustrine and lacustrine environments that filled the Valley incisions of the Newark Supergroup, mostly fed by the coeval activity of the North American CAMP.[4] This units represented several types of freshwater settings, from rivers and wetlands to deep lakes, with a notorious diversity of fauna and flora.[4] Late Triassic D. newarki and D. enigmaticus lived along a great invertebrate diversity, including Hyriinae, Unionidae and Corbiculidae clams, freshwater crayfishes (Cytioclopsis), ostracods (Darwinula spp.), clam-shrimps (Cyzicus spp.), insects (Belostomatidae, Coleoptera) and Notostracan crustaceans (Triops spp), then vertebrates such as the hybodont shark Carinacanthus and the bony fishes Turseodus, Synorichthys, Cionichthys, Semionotus and another coelacanth, Pariostegus.[4] The larger Lower Jurassic D. longicaudatus shared its environment with Unionidae clams, freshwater snails (Hydrobia and Gyraulus) insects (Diptera and Coleoptera larvae, such as Mormolucoides), clam-shrimps (Cyzicus spp.) and ostracods (Darwinula spp.) invertebrates, then also with fishes such as Hybodus, Redfieldius, Ptycholepis, Acentrophorus and Semionotus.[4] Linked with both Late Triassic and Early Jurassic, abundant terrestrial vertebrate ichnosites and body fossils are found, including those of Archosaurs and Synapsids.[4]

References

  1. ^ Schaeffer, Bobb (1952). "The Triassic coelacanth fish Diplurus, with observations on the evolution of the Coelacanthini". Bulletin of the AMNH. hdl:2246/416.
  2. ^ a b Brownstein, C.D.; Bissell, I.C. (2022). "Species delimitation and coexistence in an ancient, depauperate vertebrate clade". BMC Ecology and Evolution. 22 (1): 90. doi:10.1186/s12862-022-02043-4. PMC 9277872. PMID 35820797.
  3. ^ Abrams, J.; Riley, E. (2002). "A reconstruction of the biodiversity of the Connecticut River valley usingfossil and geological history evidence". The Traprock. 1 (2): 18–22. Retrieved 11 October 2023.
  4. ^ a b c d e Olsen, P. E. (1988). "Paleontology and paleoecology of the Newark Supergroup (early Mesozoic, eastern North America)". Developments in Geotectonics. 22 (1): 185–230. doi:10.1016/B978-0-444-42903-2.50013-0. ISBN 9780444429032. Retrieved 11 October 2023.