benthic, freshwater detritivores (organisms that obtain nutrients by consuming decomposing plant/animal material), averaging around 30 centimetres (12 in) in length.[2] However, the largest species, B. rex, had an estimated bodylength of 170 centimetres (67 in). Although expansive with over 60 species found worldwide,[3] comparatively Bothriolepis is not unusually more diverse than most modern bottom dwelling species around today.[4]
Classification
Bothriolepis is a genus placed within the placoderm order Antiarchi. The earliest antiarch placoderms first appeared in the
paraphyletic group of the clade Gnathostomata, which includes all jawed vertebrates.[5] It is unclear exactly when gnathostomes emerged, but the scant early fossil record indicates that it was sometime in the Early Palaeozoic era.[6]
The last species of Bothriolepis died out, together with the rest of Placodermi, at the end of the Devonian period.
General anatomy
Head
There are two openings through the head of Bothriolepis: a keyhole opening along the midline on the upper side for the eyes and nostrils and an opening for the mouth on the lower side near the anterior end of the head. A discovery regarding preserved structures that appear to be nasal capsules confirms the belief that the external nasal openings lay on the dorsal side of the head near the eyes.[7] Additionally, the position of the mouth on the ventral side of the skull is consistent with the typical horizontal resting orientation of Bothriolepis. It had a special feature on its skull, a separate partition of bone below the opening for the eyes and nostrils enclosing the nasal capsules called a preorbital recess.
Jaw
A new sample from the Gogo Formation in the Canning Basin of Western Australia has provided evidence regarding the morphological features of the visceral jaw elements of Bothriolepis. Using the sample, it is evident that the mental plate (a dermal bone that forms the upper part of the jaw) of antiarchs is homologous with the suborbital plate found in other placoderms. The lower jawbone consists of a differentiated blade and biting portions. Next to the mandibular joint are the prelateral and infraprelateral plates, which both are canal-bearing bones. The palatoquadrate lacks a high orbital process and was attached only to the ventral part of the mental plate, proving that the ethmoidal region of the braincase (the region of the skull that separates the brain and nasal cavity) was in fact deeper than originally believed.[8] In addition to the above-listed sample from the Gogo Formation, several other specimens have been found with mouthparts held in the natural position by a membrane that covers the oral region and attaches to the lateral and anterior margins of the head.[9]Bothriolepis has a jaw in which the two halves are separate and in the adult are functionally independent.[9]
Trunk
Bothriolepis had a slender trunk that was likely covered in soft skin with no scales or markings. The orientation that appears to have been mostly stable for resting was the dorsal surface up, evidenced by the flat surface on the ventral side.
thoracic shield of Bothriolepis was attached to its heavily armored head. Its box-like body was enclosed in armor plates, providing protection from predators. Attached to the ventral surface of the trunk is a large, thin, circular plate marked by deep-lying lines and superficial ridges. This plate lies just below the opening to the cloaca.[9]
Dermal skeleton
The dermal skeleton is organized in three layers: a superficial lamellar layer, a cancellous spongiosa, and a compact basal lamellar layer. Even in early ontogeny, these layers are apparent in specimen of Bothriolepis canadensis. The compact layers develop first.[10] The superficial layer is speculated to have denticles that may have been made of cellular bone.[11]
Fins and tail
Bothriolepis had a long pair of spine-like
caudal tail was elongated, ending in a narrow band, but is unfortunately rarely preserved in fossils.[9]Bothriolepis lacked pelvic fins. Early antiarchs like Parayunnanolepis had pelvic fins, which implies secondary loss of pelvic fin in Bothriolepis.[14]
Soft anatomy
Structures composed of soft tissue are typically not preserved in fossils because they break down easily and decompose much faster than hard tissues, meaning that the fossil record often lacks information regarding the internal anatomy of fossil species. Preservation of soft tissue structures can sometimes occur, however, if sediments fill the internal structures of an organism upon or after its death. Robert Denison's paper titled "The Soft Anatomy of Bothriolepis" explores the forms and organs of Bothriolepis.[7] These internal structures were preserved when different types of sediments surrounding the exterior of the animal-filled the internal carapaces (only organs that communicate with the exterior could be preserved in this manner). Three different sediment types were identified within the different sections of Bothriolepis: the first a pale greenish-gray medium-textured sandstone largely consisting of calcite; the second similar but finer sediment which preserves many of the organ forms; and the third distinct, fine-grained siltstone consisting of quartz, mica and other minerals but no calcite.[7] These sediments helped preserve the following internal elements:
Alimentary system
In general, the
elasmobranchs and many bony fish and similar to that found in some sharks. A single fold of tissue rolled upon its own axis forms this specialized spiral valve.[7]
Gills
It is inferred that the gills of Bothriolepis are of the primitive type, though their structure is still not well understood. Laterally, they are enclosed by an opercular fold and are found in the space beneath the lateral part of the head shield, extending medially underneath the neurocranium. Compared to the gills of normally-shaped fish, the gill region of Bothriolepis is considered to be placed more dorsally, is anteriorly more crowded, and in general is relatively short and broad.[7]
Paired ventral sacs
Extending posteriorly from the trunk carapace are paired ventral sacs that extend to the anterior end of the spiral intestine. The sacs seem to originate at the pharynx as a single median tube, which then broadens posteriorly and eventually splits into two sacs that may be homologous to the
naris
and mouth, Bothriolepis likely breathed similarly to present-day lungfish, i.e., by placing the mouth above the water's surface and swallowing air.
Despite the original interpretation presented by Denison in 1941, not all paleontologists agree that placoderms like Bothriolepis actually possessed lungs. For example, in his paper "Lungs" in Placoderms, a Persistent Palaeobiological Myth Related to Environmental Preconceived Interpretations, D. Goujet suggests that although traces of some digestive organs may be apparent from the sedimentary structures, there is no evidence supporting the presence of lungs in the samples from the Escuminac formation of Canada upon which the original assertion was based. He notes that the worldwide distribution of Bothriolepis is restricted to strictly marine environments, and thus believes that the presence of lungs in Bothriolepis is uncertain. Further investigation of the fossils is likely necessary to reach a conclusion about the presence of lungs in Bothriolepis.[15]
Feeding
Bothriolepis, as with all other antiarchs, are thought to have fed by directly swallowing mouthfuls of mud and other soft sediments in order to digest detritus, small or microorganisms, algae, and other forms of organic matter in the swallowed sediments. Additionally, the positioning of the mouth on the ventral side of its head further suggests that Bothriolepis was likely a bottom-feeder. The regular presence of "carbonaceous material in the alimentary tract" is believed to indicate that most of its diet consisted of plant material.[7]
orbital fenestra—both of which are characteristics also recognized by Erik Stensio in 1948 in the smallest B. canadensis individuals.[1] Several other features that Stensio marked indicative of young individuals can also be seen exhibited in the Catskill sample. These features include "delicate dermal bones with ornament consisting of continuous anastomosing ridges rather than tubercles, a dorsal trunk shield narrower than long and with a continuous and pronounced dorsal median ridge, and a pre-median plate that is wider than it is long".[1]B. nitida and B. minor are also described from this site.[20]
Species
Vertebrate paleontology is heavily dependent on the ability to differentiate between different species in a way that is consistent both within a particular genus and across all organisms. The genus Bothriolepis is no exception to this principle. Listed below are a few of the notable species within Bothriolepis; more than sixty species have been named in total, and it is likely that a sizeable proportion of them are valid due to the cosmopolitan nature of Bothriolepis.[3]
Bothriolepis canadensis
Bothriolepis canadensis is a taxon that often serves as a model organism for the order Antiarchi because of its enormous sample of complete, intact specimens found at the Escuminac Formation in Quebec, Canada.[1] Because of the vast sample size, this species is often used to compare growth data of newly acquired specimens of Bothriolepis, including those found in the Catskill Formation mentioned above. This comparison allows researchers to determine if newly found samples represent juvenile individuals or new "Bothriolepis" species.
B. canadensis was first described in 1880 by J.F. Whiteaves, using a limited number of disfigured samples. The next to propose a reconstruction of the species was W. Patten, who published his findings in 1904 after a discovery of several specimens that were well preserved in 3-D. In 1948, E. Stensio released a detailed depiction of B. canadensis anatomy using an abundance of material, which eventually became the most widely accepted description of this species. Since Stensio's publication, many others have provided reconstructed models of B. canadensis with modified aspects of the anatomy, including Vezina's modified single dorsal fin and more recently, reconstructions by Arsenault et al from specimens with little taphonomic distortion. Presently, the model of Arsenault et al. is regarded to be the most accurate, while there is still much debate about various aspects of this species' external anatomy. Despite the uncertainty, B. canadensis is still classically considered one of the most well-known species.[13]
The external
heterocercal caudal fin (meaning the notochord extends into the upper lobe of the caudal tail) and a large dorsal fin which likely didn't play an important role in propulsion but instead acted more as a stabilizer.[13]