''Acinocricus'' is a genus of extinct worm belonging to the group
Lobopodia
The lobopodians, members of the informal group Lobopodia (from the Greek language, Greek, meaning "blunt feet"), or the formally erected phylum Lobopoda Cavalier-Smith (1998), are panarthropods with stubby legs called lobopods, a term which may ...
and known from the middle
Cambrian
The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million ...
Spence Shale
The Spence Shale is the middle member of the Langston Formation in southeastern Idaho and northeastern Utah. It is exposed in the Bear River Range, the Wasatch Range and the Wellsville Mountains. It is known for its abundant Cambrian trilobites ...
of Utah, United States. As a
monotypic
In biology, a monotypic taxon is a taxonomic group (taxon) that contains only one immediately subordinate taxon. A monotypic species is one that does not include subspecies or smaller, infraspecific taxa. In the case of genera, the term "unispec ...
genus, it has one species ''Acinocricus stichus''. The only lobopodian discovered from the Spence Shale, it was described by
Simon Conway Morris
Simon Conway Morris (born 1951) is an English palaeontologist, evolutionary biologist, and astrobiologist known for his study of the fossils of the Burgess Shale and the Cambrian explosion. The results of these discoveries were celebrated in ...
and Richard A. Robison in 1988.
Owing to the original fragmentary fossils discovered since 1982, it was initially classified as an alga, but later realised to be an animal belonging to Cambrian fauna.
Discovery
The first specimen of ''Acinocricus'' was discovered by American palaeontologist Lloyd Gunther in 1982 from the Spence Shale in Miners Hollow,
Wellsville Mountains
The Wellsville Mountains are located in northern Utah, United States and are often considered part of the Wasatch Mountains.
Description
The mountains separate Cache Valley from the Wasatch Front (Bear River Valley), as well as form a portion of ...
, Utah. It was embedded in hardened mud and was incomplete with some of its body part missing. More than a dozen fragmentary fossils were later recovered from the same site and the surrounding areas.
Simon Conway Morris
Simon Conway Morris (born 1951) is an English palaeontologist, evolutionary biologist, and astrobiologist known for his study of the fossils of the Burgess Shale and the Cambrian explosion. The results of these discoveries were celebrated in ...
of the
University of Cambridge
, mottoeng = Literal: From here, light and sacred draughts.
Non literal: From this place, we gain enlightenment and precious knowledge.
, established =
, other_name = The Chancellor, Masters and Schola ...
and Richard A. Robison of the
University of Kansas
The University of Kansas (KU) is a public research university with its main campus in Lawrence, Kansas, United States, and several satellite campuses, research and educational centers, medical centers, and classes across the state of Kansas. Tw ...
jointly published the systematic description and scientific name in 1988. The generic name is derived from two Greek words, ''akaina'', meaning thorn or spine, and ''krikos,'' meaning ring or circle, for the circular spines on its body; the specific name ''stichos'' means row or line, referring to the arrangement of the spines.
Morris and Robison made an erroneous classification by assigning it as an alga (in the phylum
Chlorophyta
Chlorophyta or Prasinophyta is a taxon of green algae informally called chlorophytes. The name is used in two very different senses, so care is needed to determine the use by a particular author. In older classification systems, it refers to ...
) as they were convinced that it had no particular resemblance to any known animal fossils (
medusoid) known at the time.
The correct identification as an animal came only after a series of discoveries of Cambrian fossils (
Maotianshan Shales
The Maotianshan Shales are a series of Cambrian, Early Cambrian deposits in the Chiungchussu Formation, famous for their ''Lagerstätte, Konservat Lagerstätten'', deposits known for the exceptional preservation of fossilized organisms or traces. ...
) in
Chengjian, China. A variety of lobopods were discovered in the early 1990s that showed important shared features with ''Acinocricus''. Comparison of the Chengjian lobopods and ''Acinocricus'' revealed their similarities.
In 1998, Jun-yuan Chen (Nanjing Institute of Geology and Palaeontology,
Chinese Academy of Sciences
The Chinese Academy of Sciences (CAS); ), known by Academia Sinica in English until the 1980s, is the national academy of the People's Republic of China for natural sciences. It has historical origins in the Academia Sinica during the Republ ...
) and Lars Ramsköld (
Uppsala University
Uppsala University ( sv, Uppsala universitet) is a public university, public research university in Uppsala, Sweden. Founded in 1477, it is the List of universities in Sweden, oldest university in Sweden and the Nordic countries still in opera ...
, Sweden) made assessment of all available Cambrian lobopod fossils and came to the conclusion that ''Acinocricus'' belongs to Lobopodia.
Description
''Acinocricus'' is a soft-bodies worm-like animal having numerous stumpy legs called lobopods. It is most easily distinguished from spiral spines on its back.
It is for this appearance that it was originally believed as having body whorls that give a
thallus
Thallus (plural: thalli), from Latinized Greek (), meaning "a green shoot" or "twig", is the vegetative tissue of some organisms in diverse groups such as algae, fungi, some liverworts, lichens, and the Myxogastria. Many of these organisms wer ...
-like structure and classified as an alga.
It is similar to other lobopods such as ''Luolishania longicruris,
Collinsovermis monstruosus,
Collinsium ciliosum'' in having several pairs of legs and spines on each body segment (
somite
The somites (outdated term: primitive segments) are a set of bilaterally paired blocks of paraxial mesoderm that form in the embryonic stage of somitogenesis, along the head-to-tail axis in segmented animals. In vertebrates, somites subdivide in ...
). It is for these reasons that it also classified under the family
Luolishaniidae
The Luolishaniidae or Luolishaniida are a group of Cambrian and Ordovician lobopodians with anterior 5 or 6 pairs of setiferous lobopods. Most luolishaniids also have posterior lobopods each with a hooked claws, and thorn-shaped sclerites arran ...
. Its major difference is that its spines are arranged in multiple rows on each somite, unlike in single pairs in other lobopods. The spines are arranged in rows, and each row contains alternating large and small spines. The large spines measure up to 1.5. cm long, while the small spines are in at least two different sizes of less than 0.1 cm long.
The exact number of the rows of spine and lobopods is difficult to make out due to fragmentary fossils. There are at least 12 pairs of lobopods, and the first five pairs are different from the rest in being longer and slender. The total length of the body can be up to 10 cm long. It is considered as lacking hardened body covering (
sclerite
A sclerite (Greek , ', meaning "hard") is a hardened body part. In various branches of biology the term is applied to various structures, but not as a rule to vertebrate anatomical features such as bones and teeth. Instead it refers most commonly ...
). It is regarded as characteristically most closely related to ''Collinsovermis,'' with the major differences being its larger size, less number of anterior legs, absence of sclerites and its numerous rows of back spines.
References
{{Taxonbar, from1=Q110393899, from2=Q110393902
Fossil taxa described in 1988
Lobopodia
Cambrian geology of Utah