Biology:Austrolimulus
Austrolimulus fletcheri is an extinct xiphosuran, related to the modern horseshoe crab. The species is only known from the Middle Triassic-aged strata of Brookvale, New South Wales of Australia.[1]
Discovery and naming
Austrolimulus fletcheri is only known from one complete specimen.[2] The specimen was discovered in the Beacon Hill Quarry near the suburb of Brookvale, Sydney, New South Wales of Australia. This quarry represents the Anisian Hawkesbury Sandstone. The fossil was discovered in an 8 m thick shale lens.[3] The Hawkesbury Sandstone was formed in a coastal floodplain composed of high energy braided rivers, lakes and sand dunes. The shale lenses likely represent low-energy shallow water bodies disconnected from the main river channel.[4] The generic name honors Harold Oswald Fletcher, a paleontologist of the Australian Museum.[1]
Description
Austrolimulus fletcheri is 5.75 inches (14.6 cm) long.[1]
The prosoma (head) is wider than the length of both the prosoma and opisthosoma combined, coming in at 7 inches (18 cm) in width, whilst the prosoma and opisthosoma combined only come in at 2.25 inches (5.7 cm) in length. The prosoma is divided into three main areas: a median narrow glabella-like region and two lateral cheek regions. The "cheeks" are themselves composed of two main regions separated by a carina: proximally, the finely tuberculate (covered with small bumps and irregular reliefs) "fixed cheeks" located adjacent to the glabella, and more distally, the "free cheeks". Possible spines extend from both sides of the carina above the inferred position of the eyes. The inner regions of the free cheeks are coarsely and irregularly tuberculate (covered with larger bumps and irregular reliefs), while the marginal regions are thinner, smooth and extend into very long genal spines.[1][2]
The first three segments of the opisthosoma (abdomen) are consolidated whereas the following three segments are distinct. The three segments of the anterior region taper markedly posteriorly, the posterior segments are similar in width. At the front of the opisthosoma is a pair of well developed free lobes extending as far as the width of the posterior margin of the prosoma (excluding the genal spines). Last segment pointed postero-laterally. The central axis of the opisthosoma is similar in width to the "glabella" but tapers toward the rear. The telson (rear-facing spike) is longer than the body.[1][2]
Classification
Cladogram after Bicknell (2019).[5]
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Wikidata ☰ Q4825667 entry
References
- ↑ 1.0 1.1 1.2 1.3 1.4 Riek, E. F. (1955-09-01). "A new Xiphosuran from the Triassic sediments at Brookvale, New South Wales" (in en). Records of the Australian Museum 23 (5): 281–282. doi:10.3853/j.0067-1975.23.1955.637. ISSN 0067-1975. https://journals.australian.museum/riek-1955-rec-aust-mus-235-281282/.
- ↑ 2.0 2.1 2.2 Riek, E. F. (1968-12-23). "Re-examination of two arthropod species from the Triassic of Brookvale, New South Wales" (in en). Records of the Australian Museum 27 (17): 313–321. doi:10.3853/j.0067-1975.27.1968.451. ISSN 0067-1975. https://journals.australian.museum/riek-1968-rec-aust-mus-2717-313321/.
- ↑ Bicknell, Russell D. C.; Smith, Patrick M.; Birch, Sienna A.; Bevitt, Joseph J. (2022-04-22). "An earliest Triassic age for Tasmaniolimulus and comments on synchrotron tomography of Gondwanan horseshoe crabs" (in en). PeerJ 10. doi:10.7717/peerj.13326. ISSN 2167-8359. PMID 35480564.
- ↑ Bicknell, Russell D. C.; Smith, Patrick M. (2021-10-02). "The first fossil scorpion from Australia" (in en). Alcheringa: An Australasian Journal of Palaeontology 45 (4): 419–422. doi:10.1080/03115518.2021.1983874. ISSN 0311-5518. Bibcode: 2021Alch...45..419B. https://www.tandfonline.com/doi/full/10.1080/03115518.2021.1983874.
- ↑ Bicknell, Russell D.C. (2019-10-13). "Xiphosurid from the Upper Permian of Tasmania confirms Palaeozoic origin of Austrolimulidae" (in en). Palaeontologia Electronica. doi:10.26879/1005. https://palaeo-electronica.org/content/2019/2758-a-permian-austrolimulid. Retrieved 2026-05-06.
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