''Micropholis'' (Greek mikros''
' = small and '
''pholis''
' = scale) is an extinct
genus
Genus (; : genera ) is a taxonomic rank above species and below family (taxonomy), family as used in the biological classification of extant taxon, living and fossil organisms as well as Virus classification#ICTV classification, viruses. In bino ...
of
dissorophoid temnospondyl
Temnospondyli (from Greek language, Greek τέμνειν, ''temnein'' 'to cut' and σπόνδυλος, ''spondylos'' 'vertebra') or temnospondyls is a diverse ancient order (biology), order of small to giant tetrapods—often considered Labyrinth ...
.
Fossil
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserve ...
s have been found from the
''Lystrosaurus'' Assemblage Zone of the
Karoo Basin in
South Africa
South Africa, officially the Republic of South Africa (RSA), is the Southern Africa, southernmost country in Africa. Its Provinces of South Africa, nine provinces are bounded to the south by of coastline that stretches along the Atlantic O ...
and are dated to the
Induan
The Induan is the first age of the Early Triassic epoch in the geologic timescale, or the lowest stage of the Lower Triassic series in chronostratigraphy. It spans the time between 251.9 Ma and 249.9 Ma (million years ago). The Induan is so ...
(
Early Triassic
The Early Triassic is the first of three epochs of the Triassic Period of the geologic timescale. It spans the time between 251.9 Ma and Ma (million years ago). Rocks from this epoch are collectively known as the Lower Triassic Series, which ...
). Fossils have also been found from the lower
Fremouw of Antarctica. ''Micropholis'' is the only post-Permian dissorophoid and the only dissorophoid in what is presently the southern hemisphere and what would have been termed
Gondwana
Gondwana ( ; ) was a large landmass, sometimes referred to as a supercontinent. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia (continent), Australia, Zea ...
during the amalgamation of
Pangea
Pangaea or Pangea ( ) was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. It assembled from the earlier continental units of Gondwana, Euramerica and Siberia (continent), Siberia during the Carboniferous period ...
.
History of study
''Micropholis'' was one of the first dissorophoids to be named by English paleontologist
Thomas Huxley in 1859 based on a partial skull. ''Micropholis stowii'' (properly ''Micropholis stowi'')'','' the
type species
In International_Code_of_Zoological_Nomenclature, zoological nomenclature, a type species (''species typica'') is the species name with which the name of a genus or subgenus is considered to be permanently taxonomically associated, i.e., the spe ...
, is named for
George William Stow, the South African geologist and ethnologist who discovered the specimen and who proposed that it represented some extinct
amphibian
Amphibians are ectothermic, anamniote, anamniotic, tetrapod, four-limbed vertebrate animals that constitute the class (biology), class Amphibia. In its broadest sense, it is a paraphyletic group encompassing all Tetrapod, tetrapods, but excl ...
. English paleontologist
Richard Owen
Sir Richard Owen (20 July 1804 – 18 December 1892) was an English biologist, comparative anatomy, comparative anatomist and paleontology, palaeontologist. Owen is generally considered to have been an outstanding naturalist with a remarkabl ...
later named a new genus and species, ''Petrophryne granulata'', for a better-known skull, also from the Karoo Basin, that he suggested might be the same animal as ''M. stowi''; this synonymy was eventually accepted by other workers. Additional description was furnished by German paleontologists
Ferdinand Broili and Joachim Schröder in 1937.
The taxon was most recently revised by German paleontologist Jürgen Boy in 1985
and again in 2005 by German paleontologist Rainer Schoch and South African paleontologist Bruce Rubidge.
''Micropholis'' has been repeatedly incorporated in phylogenetic analyses of temnospondyls and dissorophoids. In 2015, American paleontologist Julia McHugh published a description of histological patterns in ''Micropholis''.
Description
Practically the entire skeleton of ''Micropholis'' is now known. Many specimens have been found, a number of which are on blocks preserving partial to complete skeletons of multiple individuals in close association,
and two distinct morphotypes are evident, differing in skull width and palatal dentition.
The "slender-headed" morph is defined by corresponding narrowing of many features and cranial elements, differences in dentition on the vomer, and possibly by smaller and more numerous maxillary teeth when compared with the "broad-headed" morph. Additionally, a wide size range of individuals are known, ranging from skull lengths around 20 mm to over 40 mm. There remains some uncertainty about whether the slender-headed morph is an advanced ontogenetic stage, as the largest individuals all exhibit this skull morphology. Schoch & Milner (2014) identified 10 features in the diagnosis of ''Micropholis'':
: (1) dermal ornament, with irregularly spaced pustules;
: (2) accessory fangs on the vomer;
: (3) unpaired anterior palatal fenestra (sometimes 'fontanelle');
: (4) palatine and ectopterygoid reduces to struts along medial maxillary margin;
: (5) short basipterygoid ramus of pterygoid;
: (6) basal plate with prominent posterolateral horns;
: (7) hyobranchial skeleton well ossified;
: (8) short tail;
: (9) elongate skull table (plesiomorphy); and
:(10) postparietal much longer than tabular (plesiomorphy).
Phylogenetic relationships
When it was first described, ''Micropholis'' was recognized as a '
labyrinthodont,' an outdated term used to refer to extinct 'amphibians' in a broad sense. However, Huxley remarked that it did not show close affinities with any of the known Triassic labyrinthodonts of the time. Its uncertain affinities continued to plague paleontologists who remarked that "no types really closely allied to it have been found". As a result, it was placed within its own family, Micropholidae, and sometimes within its own superfamily, Micropholoidea.
Although it was suggested in the 1930s that ''Micropholis'' might be allied with dissorophoids by comparison with the
dissorophid ''
Broiliellus'', this idea was not widely adopted
until the 1960s. Subsequent discovery of
amphibamiforms, either referred to monotaxic families such as Doleserpetontidae or to Dissorophidae, has further strengthened the placement of ''Micropholis'' among dissorophoids, which has since been maintained by computer-assisted phylogenetic analyses.
''Micropholis'' now belongs to the recently resurrected family Micropholidae,
which is included in what was historically termed
Amphibamidae (now Amphibamiformes). However, its placement has long been perplexing because it retains numerous plesiomorphies and is usually recovered as one of the earlier diverging amphibamiforms despite being tens of millions of years younger than all other dissorophoids.
Below is a phylogeny from Schoch (2018)
showing the position of ''Micropholis''.
References
External links
''Micropholis''in the
Paleobiology Database
{{Taxonbar, from=Q6839869
Amphibamids
Triassic temnospondyls of Africa
Early Triassic amphibians of Africa
Taxa named by Thomas Henry Huxley
Fossil taxa described in 1859
Prehistoric amphibian genera