Hurdia

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Hurdia
Temporal range: Mid Cambrian, 518–505  Ma
20210619 Hurdia.png
Reconstruction of H. victoria (top) and H. triangulata
Hurdia disarticulated assemblages.jpg
Disarticulated fossils
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Order: Radiodonta
Family: Hurdiidae
Genus: Hurdia
Walcott, 1912
Type species
Hurdia victoria
Walcott, 1912
Other species
  • H. triangulataWalcott, 1912
  • ?H. hospesChlupach and Kordule, 2002
Synonyms
  • ?Huangshandongia yichangensisShicheng and Zhilin, 1990
  • ?Liantuoia inflataShicheng and Zhilin, 1990

Hurdia is an extinct genus of hurdiid radiodont that lived 505 million years ago during the Cambrian Period. Fossils have been found in North America, China, and the Czech Republic.

Contents

Description

Hurdia was one of the largest organisms in the Cambrian oceans, H. victoria reached between 18.3–30.5 cm (7.2–12.0 in) in length, while H. triangulata reached up to just 8.1 cm (3.2 in) long. [1] Its head bore a pair of frontal appendages. These frontal appendages had 9 or more rarely 10 or 11 segments/podomeres, which were approximately rectangular and decreased in size towards the end of the appendage. The upper surface of the appendage was convexly curved. Podomeres 2 to 6 bore long downward pointing spines (ventral spines) with forward-curving tips. These ventral spines themselves bore up to 9 equally spaced forward-facing spines dubbed auxiliary spines, with podomeres 7 and 8 bearing shorter, smooth forward curving spines. The frontal appenages were used to bring food to its ring-shaped mouth (oral cone), in which four large plates are present, with inner rows of spines inside the main cone. [2] Like other hurdiids, Hurdia bore a large frontal carapace protruding from its head composed of three sclerites: a central component known as the H-element and two lateral components known as P-elements. Originally, it is estimated that body flaps ran along the sides of the organisms, from which large gills were suspended. [3] However, anatomy of Aegirocassis clarified that Hurdia had both ventral and dorsal flaps, and gills were on trunk segments. [4]

Ecology

Hurdia is either suggested to have used its frontal appendages to sift small prey from sediment, or to have used them as a trap to capture larger benthic (seafloor dwelling) prey. [5]

Distribution

Hurdia had cosmopolitan distribution; two described species has been recovered from the Burgess Shale in British Columbia, Canada. In addition, H. victoria is also known from the Spence Shale in Utah, USA. [6] Unnamed species are known from Qingjiang biota in Hubei, China, Pioche Shale in Nevada, USA, and Wheeler Shale in Utah, USA. [6] [7] Huangshandongia yichangensis and Liantuoia inflata from the Shuijingtuo Formation in Hubei, China, and Proboscicaris hospes from the Jince Formation of the Czech Republic (which is identified as Hurdia hospes in some papers [8] ), and unnamed fossil from Ordovician Fezouata Formation could represent species of Hurdia as well. [3] [2]

Taxonomic history

Hurdia was named in 1912 by Charles Walcott, with two species, the type species H. victoria and a referred species, H. triangulata. [9] The genus name refers to Mount Hurd. [9] It is possible that Walcott had described a specimen the year prior as Amiella, but the specimen is too fragmentary to identify with certainty, so Amiella is a nomen dubium . [10] Walcott's original specimens consisted only of H-elements of the frontal carapace, which he interpreted as being the carapace of an unidentified type of crustacean. P-elements of the carapace were described as a separate genus, Proboscicaris, in 1962.

In 1996, then-curator of the Royal Ontario Museum Desmond H. Collins erected the taxon Radiodonta to encompass Anomalocaris and its close relatives, and included both Hurdia and Proboscicaris in the group. [11] He subsequently recognized that Proboscicaris and Hurdia were based on different parts of the same animal, and recognized that a specimen previously assigned to Peytoia was also a specimen of the species. [10] He presented his ideas in informal articles, [12] [13] and it was not until 2009, after three years of painstaking research, that the complete organism was reconstructed. [3] [14] [15] [16]

Sixty-nine specimens of Hurdia are known from the Greater Phyllopod bed, where they comprise 0.13% of the community. [17]

See also

Related Research Articles

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<i>Anomalocaris</i> Extinct genus of cambrian radiodont

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<i>Peytoia</i> Extinct genus of radiodont

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<i>Peytoia infercambriensis</i> Extinct species of arthropod

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<i>Stanleycaris</i> Extinct genus of basal hurdiid radiodonts

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<i>Ursulinacaris</i> Extinct genus of hurdiid radiodonts

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<i>Cambroraster</i> Extinct genus of radiodonts

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<i>Titanokorys</i> Extinct genus of giant hurdiid radiodont

Titanokorys is a genus of extinct hurdiid (peytoiid) radiodont that existed during the mid Cambrian. It is the largest member of its family from the Cambrian, with a body length of 50 cm (20 in) long, making it one of the largest animals of the time. It bears a resemblance to the related genus Cambroraster. Fossils of T. gainesi were first found within the Marble Canyon locality within the Burgess Shale in 2018. The fossils were not named until 2021 because they were assumed to be giant specimens of Cambroraster.

<i>Laminacaris</i> Genus of extinct arthropods

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<i>Pahvantia</i> Extinct genus of radiodonts

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<i>Cordaticaris</i> Genus of extinct stem-group arthropods

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<i>Buccaspinea</i> Extinct genus of radiodont

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<i>Zhenghecaris</i> Genus of enigmatic Cambrian arthropod

Zhenghecaris is an extinct genus of enigmatic arthropods from the Lower Cambrian Maotianshan Shales, tentatively classified as a hurdiid (peytoiid) radiodont, and originally as a thylacocephalan. The genus contains a single species, Zhenghecaris shankouensis, known from several specimens mostly preserving the carapace and eyes. These specimens measure roughly 15 cm (5.9 in) in width, making it one of the largest thylacocephalans, behind Ostenocaris, Dollocaris and Ainiktozoon, as well as the earliest since all other thylacocephalans are Ordovician or younger. Better preserved fossils show that it was more similar to the domed sclerites of radiodonts such as Cambroraster, with two lateral spine processes on either side of the carapace, the eyes apparently fitting into the posterior notches. Additional isolated sclerites from the Chengjiang have been described as the lateral sclerites of Zhenghecaris due to their broad similarity to the P-elements of hurdiids (peytoiids), and because of their similar construction, ornamentation, and possession of two-pronged lateral spine processes. It has also been classified conservatively as Arthropoda incertae sedis, as the fragmentary remains cannot confidently be classified further due to the lack of associated appendages of trunk elements.

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References

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