Temporal range: Early to mid Cambrian: Chengjiang–Burgess shale
|Image of the first complete Anomalocaris fossil found, residing in the Royal Ontario Museum|
Anomalocaris ("abnormal shrimp") is an extinct genus of anomalocaridid, a family of animals thought to be closely related to ancestral arthropods. The first fossils of Anomalocaris were discovered in the Ogygopsis Shale by Joseph Frederick Whiteaves, with more examples found by Charles Doolittle Walcott in the Burgess Shale. Originally several fossilized parts discovered separately (the mouth, feeding appendages and tail) were thought to be three separate creatures, a misapprehension corrected by Harry B. Whittington and Derek Briggs in a 1985 journal article. Anomolocaris is thought to be one of the earliest examples of an apex predator, though others have been found in older Cambrian lagerstätten deposits.
Anomalocaris has been misidentified several times, in part due to its makeup of a mixture of mineralized and unmineralized body parts; the mouth and feeding appendage was considerably harder and more easily fossilized than the delicate body. Its name originates from a description of a detached 'arm', described by Joseph Frederick Whiteaves in 1892, as a separate crustacean-like creature due to its resemblance to the tail of a lobster or shrimp. The first fossilized anomalocaridid mouth was discovered by Charles Doolittle Walcott, who mistook it for a jellyfish and placed it in the genus Peytoia. Walcott also discovered a second feeding appendage, but failed to realize the similarities to Whiteaves' discovery and instead identified it as feeding appendage or tail of the extinct Sidneyia.
The body was discovered separately and classified as a sponge in the genus Laggania; a mouth was found with the body, but was interpreted by its discoverer Simon Conway Morris as an unrelated Peytoia that had through happenstance settled and been preserved with Laggania. Later, while clearing what he thought was an unrelated specimen, Harry B. Whittington removed a layer of covering stone to discover the unequivocally connected arm thought to be a shrimp tail and mouth thought to be a jellyfish. Whittington linked the two species, but it took several more years for researchers to realize that the continuously juxtaposed Peytoia, Laggania and feeding appendage actually represented a single, enormous creature. The two genera are now placed into the family Anomalocaridae. Because Peytoia was named first, it became the correct name for the entire animal. The original feeding arm, however, came from a larger species distinct from Peytoia and "Laggania", which retains the name Anomalocaris.
In 2011, six fossils of compound eyes, the first for Anomalocaris, were recovered from an paleontological dig at Emu Bay on Kangaroo Island, Australia, proving that Anomalocaris was indeed an arthropod as had been suspected. The find also indicated that advanced arthropod eyes had evolved very early, before the evolution of jointed legs or hardened exoskeletons.
Stephen Jay Gould cites Anomalocaris as one of the fossilized extinct species he believed to be evidence of a much more diverse set of phyla that existed in the Cambrian Period, discussed in his book Wonderful Life, a conclusion disputed by other paleontologists.
For the time in which it lived, Anomalocaris was gigantic, up to 1 metre (3.3 feet) long. It propelled itself through the water by undulating the flexible lobes on the sides of its body. Each lobe sloped below the one more posterior to it, and this overlapping allowed the lobes on each side of the body to act as a single "fin", maximizing the swimming efficiency. The construction of a remote-controlled model showed this mode of swimming to be intrinsically stable, implying that Anomalocaris would not have needed a complex brain to manage balance while swimming. The body was widest between the third and fifth lobe and narrowed towards the tail; it had at least 11 lobes in total. It is difficult to distinguish lobes near the tail, making an accurate count difficult.
Anomalocaris had an unusual disk-like mouth. The mouth was composed of several plates organized in triradially. 3 of the plates were quite large. 3-4 medium sized plates could be found between each of the large plates, and several small, wrinkled plates between them. The mouth resembled a pineapple ring with the center replaced by a series of serrated prongs. The mouth could constrict to crush prey, but never completely close; there was always an opening about 5 millimeters in diameter when the mouth was shut; a centimetres in exceptionally large individuals. Two large Great Appendages (up to 18 centimetres (7.1 inches) in length when extended) were positioned in front of the mouth, at the front of the head. Along with all other known Anomalocarids, Anomalocaris possessed a sclerite on the top of its head, called a head shield, or dorsal carapace. The head shield of Anomalocaris was shaped like an oval, with a distinct rim on the outer edge.
Anomalocaris canadensis possessed 14 segments on each appendage, each one tipped with two barb-like ventral spines. The ventral spines themselves were both equipped with 2 smaller auxiliary spines, which branches off from the main spine at the center of its length. The tail was large and fan-shaped, composed of three large fin-shaped lobes, and along with undulations of the lobes, was probably used to propel the creature through Cambrian waters. The gills of the animal, in the form of long, thin, hair-like structures, were attached to setal blades. The steal blades were attached by their margin to the top side of the animal, two setal blades per lobe pair. A divide ran down the middle, separating the gills.
Based on fossilized eyes from the Emu Bay Shale, which belonged to Anomalocaris briggsi (Which, based on morphological and phylogenetic evidence, was more closely related to Tamisiocaris) were 30 times as powerful as those of trilobites, long thought to have had the most advanced eyes of any contemporary species. With 16,000 lenses, the resolution of the 3-centimetre-wide (1.2 in) eyes would have been rivalled only by that of the modern dragonfly, which has 28,000 lenses in each eye.
A long-standing view holds that Anomalocaris fed on hard-bodied animals, including trilobites—making it one of the first predators—and its mid-gut glands strongly suggest a predatory lifestyle. However, its ability to penetrate mineralised shells has been questioned. Some Cambrian trilobites have been found with round or W-shaped "bite" marks, which were identified as being the same shape as the mouthparts of Anomalocaris. Stronger evidence that Anomalocaris ate trilobites comes from coprolite, which contain trilobite parts and are so large that the anomalocarids are the only known organism from that period large enough to have produced them. However, since Anomalocaris lacks any mineralised tissue, it seemed unlikely that it would be able to penetrate the hard, calcified shell of trilobites. Rather, the coprolites may have been produced by a different organisms, such as the trilobites of the genus Redlichia.
The lack of wear on anomalocaridid mouthparts suggests they did not come into regular contact with mineralised trilobite shells, and were possibly better suited to feeding on smaller, soft-bodied organisms by suction, since they would have experienced structural failure if they were used against the armour of trilobites. A. canadensis may have been capable of feeding on organisms with hard exoskeletons due to the short, robust spines on its appendages. However, as opposed to Peytoia whose mouthpiece is more rectangular with short protruding spines, the mouthpiece of A. canadensis has a smaller and more irregular diamond-shaped opening, not permitting strong biting motions, and indicating a suction-feeding behavior to suck in softer organisms.
One suggested possibility is that anomalocaridids fed by grabbing one end of their prey in their jaws while using their appendages to quickly rock the other end of the animal back and forth. This produced stresses that exploited the weaknesses of arthropod cuticles, causing the prey's exoskeleton to rupture and allowing the predator to access its innards. This behaviour was originally thought to have provided an evolutionary pressure for trilobites to roll up, to avoid being flexed until they snapped.
Anomalocaris canadensis lived in the Burgess Shale in relatively great numbers, though comparable fossils have been found elsewhere, suggesting a more expansive range over the Laurentian continent. In the Burgess Shale, Anomalocaris is more common in the older sections, notably the Mount Stephen trilobite beds. However, in the younger sections, such as the Phyllopod bed, Anomalocaris could reach much greater sizes; roughly twice the size of its older, trilobite bed relatives. These rare giant specimens have previously been referred to a separate species, Anomalocaris gigantea; however, the validity of this species has been called into question, and is currently dubious.
Other species attributed to Anomalocaris live in vastly different environments. Anomalocaris saron and Anomalocaris kunmingensis lived in the Maotianshan Shales, a shallow tropical sea in what is now modern China. Anomalocaris briggsi lived in a comparable environment; the shallow, tropical waters of Cambrian Australia. The Maotianshan Shale and the Emu Bay Shale are very close in proximity, being separated by a small landmass, far from the Burgess Shale.
- 8564 Anomalocaris, an asteroid named after this animal
- Cambrian explosion
- Aegirocassis, a giant filter-feeding anomalocarid from Ordovician Morocco
- Daley, A. C.; Peel, J. S. (2010). "A Possible Anomalocaridid from the Cambrian Sirius Passet Lagerstätte, North Greenland". Journal of Paleontology. 84 (2): 352–355. doi:10.1666/09-136R1.1.
- Conway Morris, S. (1998). The crucible of creation: the Burgess Shale and the rise of animals. Oxford [Oxfordshire]: Oxford University Press. pp. 56–9. ISBN 978-0-19-850256-2.
- Whittington, H.B.; Briggs, D.E.G. (1985). "The largest Cambrian animal, Anomalocaris, Burgess Shale, British Columbia". Philosophical Transactions of the Royal Society B. 309 (1141): 569–609. Bibcode:1985RSPTB.309..569W. doi:10.1098/rstb.1985.0096.
- Gould, Stephen Jay (1989). Wonderful life: the Burgess Shale and the nature of history. New York: W.W. Norton. pp. 194–206. ISBN 978-0-393-02705-1.
- Daley, A. and Bergström, J. (2012). "The oral cone of Anomalocaris is not a classic 'peytoia'." Naturwissenschaften, doi:10.1007/s00114-012-0910-8
- Paterson, J. R.; García-Bellido, D. C.; Lee, M. S. Y.; Brock, G. A.; Jago, J. B.; Edgecombe, G. D. (2011). "Acute vision in the giant Cambrian predator Anomalocaris and the origin of compound eyes". Nature. 480 (7376): 237–240. Bibcode:2011Natur.480..237P. doi:10.1038/nature10689. PMID 22158247.
- Usami, Yoshiyuki (2006). "Theoretical study on the body form and swimming pattern of Anomalocaris based on hydrodynamic simulation". Journal of Theoretical Biology. 238 (1): 11–17. doi:10.1016/j.jtbi.2005.05.008. PMID 16002096.
- Whittington, H.B.; Briggs, D.E.G. (1985). "The Largest Cambrian Animal, Anomalocaris, Burgess Shale, British Columbia". Philosophical Transactions of the Royal Society B (free full text). 309 (1141): 569–609. Bibcode:1985RSPTB.309..569W. doi:10.1098/rstb.1985.0096.
- Briggs, Derek E. G. (1994). "Giant Predators from the Cambrian of China". Science. 264 (5163): 1283–4. Bibcode:1994Sci...264.1283B. doi:10.1126/science.264.5163.1283. PMID 17780843.
- "The Anomalocaris homepage". Archived from the original on 4 April 2008. Retrieved 2008-03-20.
- Hagadorn, James W. (August 2009). "Taking a Bite out of Anomalocaris" (PDF). In Smith, Martin R.; O'Brien, Lorna J.; Caron, Jean-Bernard (eds.). Abstract Volume. International Conference on the Cambrian Explosion (Walcott 2009). Toronto, Ontario, Canada: The Burgess Shale Consortium (published 31 July 2009). ISBN 978-0-9812885-1-2.
- Nedin, C. (1999). "Anomalocaris predation on nonmineralized and mineralized trilobites". Geology. 27 (11): 987–990. Bibcode:1999Geo....27..987N. doi:10.1130/0091-7613(1999)027<0987:APONAM>2.3.CO;2.
- Daley, A. C.; Paterson, J. R.; Edgecombe, G. D.; García-Bellido, D. C.; Jago, J. B. (2013). Donoghue, Philip (ed.). "New anatomical information on Anomalocaris from the Cambrian Emu Bay Shale of South Australia and a reassessment of its inferred predatory habits". Palaeontology: n/a. doi:10.1111/pala.12029.
- Daley, A. C.; Bergström, J. (2012). "The oral cone of Anomalocaris is not a classic peytoia". Naturwissenschaften. 99 (6): 501–504. Bibcode:2012NW.....99..501D. doi:10.1007/s00114-012-0910-8. PMID 22476406.
- Vinther, J.; Stein, M.; Longrich, N. R.; Harper, D. A. T. (2014). "A suspension-feeding anomalocarid from the Early Cambrian". Nature. 507 (7493): 496–499. Bibcode:2014Natur.507..496V. doi:10.1038/nature13010. PMID 24670770.
- Van Roy, P.; Daley, A. C.; Briggs, D. E. G. (2015). "Anomalocaridid trunk limb homology revealed by a giant filter-feeder with paired flaps". Nature. 522 (7554): 77–80. Bibcode:2015Natur.522...77V. doi:10.1038/nature14256. PMID 25762145.
- Lerosey-Aubril, R.; Hegna, T.A.; Babcock, L.E.; Bonino, E.; Kier, C. (2014-05-19). "Arthropod appendages from the Weeks Formation Konservat-Lagerstätte: new occurrences of anomalocaridids in the Cambrian of Utah, USA". Bulletin of Geosciences: 269–282. doi:10.3140/bull.geosci.1442. ISSN 1802-8225.
- "Anomalocaris, the largest known Cambrian arthropod | The Palaeontological Association". www.palass.org. Retrieved 2019-09-16.
- Jeanes, Graphic: Jacquie. "Mapping the world's Burgess Shale-type deposits". www.virtualmuseum.ca. Retrieved 2019-09-16.
|Wikimedia Commons has media related to Anomalocaris.|
- "Anomalocaris canadensis". Burgess Shale Fossil Gallery. Virtual Museum of Canada. 2011.
- Anomalocaris 'homepage' with swimming animation
- Burgess Shale: Anomalocaris canadensis (proto-arthropod), Smithsonian.