Emplastus Gurnetensis BMNHP9755 Whole
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''Emplastus'' is an
extinct Extinction is the termination of a kind of organism or of a group of kinds (taxon), usually a species. The moment of extinction is generally considered to be the death of the last individual of the species, although the capacity to breed and ...
morphogenus Form classification is the classification of organisms based on their morphology (biology), morphology, which does not necessarily reflect their biological relationships. Form classification, generally restricted to palaeontology, reflects uncer ...
of ants in the subfamily
Dolichoderinae Dolichoderinae is a subfamily of ants, which includes species such as the Argentine ant (''Linepithema humile''), the erratic ant, the odorous house ant, and the cone ant. The subfamily presents a great diversity of species throughout the world ...
, known from fossils found in Asia and Europe. The genus contains twelve species described from sites in England, Eastern Europe and Far Eastern Russia.


Distribution

''Emplastus'' is known from a number of adult fossil specimens which are composed of partial adult males, female workers and queens. The first specimens described were preserved as compression fossils in
sedimentary rock Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles ...
from the
Radoboj Radoboj is a village and municipality in Krapina-Zagorje County in Croatia. In the 2011 census, the total population was 3,387, in the following settlements: * Bregi Radobojski, population 445 * Gorjani Sutinski, population 145 * Gornja Šemn ...
area of what is now Croatia. The deposits are the result of sedimentation in an
inland sea An inland sea (also known as an epeiric sea or an epicontinental sea) is a continental body of water which is very large and is either completely surrounded by dry land or connected to an ocean by a river, strait, or "arm of the sea". An inland se ...
basin, possibly a shallow lagoon environment, during the
Burdigalian The Burdigalian is, in the geologic timescale, an age (geology), age or stage (stratigraphy), stage in the early Miocene. It spans the time between 20.43 ± 0.05 annum, Ma and 15.97 ± 0.05 Ma (million years ago). Preceded by the Aquitanian (sta ...
of the Early Miocene. Along with the ''Emplastus'' species, a diverse assemblage of several hundred species of insects have been preserved in the sediments, along with fish and algae. The fossil impressions are preserved in
micrite Micrite is a limestone constituent formed of calcareous particles ranging in diameter up to four μm formed by the recrystallization of lime mud. Flügel, Erik, ''Microfacies of Carbonate Rocks: Analysis, Interpretation and Application,'' Springe ...
limestones, resulting in low quality preservation of fine details. Another series of species were described from compression fossils found in thin layers and concretions of micrite from the "insect bed" and older stratum of the
Bembridge Marls The Bouldnor Formation is a geological formation in the Hampshire Basin of southern England. It is the youngest formation of the Solent Group and was deposited during the uppermost Eocene and lower Oligocene. Stratotype and occurrence The Boul ...
. The
marl Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part o ...
s are exposed at a number of locations along the north coast of the
Isle of Wight The Isle of Wight ( ) is a county in the English Channel, off the coast of Hampshire, from which it is separated by the Solent. It is the largest and second-most populous island of England. Referred to as 'The Island' by residents, the Isle of ...
in England. Part of the
Bouldnor Formation The Bouldnor Formation is a geological formation in the Hampshire Basin of southern England. It is the youngest formation of the Solent Group and was deposited during the uppermost Eocene and lower Oligocene. Stratotype and occurrence The Boul ...
, the marls have been dated to the Late Eocene in age. The marls have not preserved any
Symphyta Sawflies are the insects of the suborder Symphyta within the order Hymenoptera, alongside ants, bees, and wasps. The common name comes from the saw-like appearance of the ovipositor, which the females use to cut into the plants where they lay ...
hymenopterans such as
Tenthredinoidea The Tenthredinoidea are the dominant superfamily of sawflies within the Symphyta, containing some 8,400 species worldwide, primarily in the family Tenthredinidae. All known larvae are phytophagous, and a number are considered pests. The included ...
species, suggesting that the paleotemperature of the marls was as warm or possibly warmer than either the
Baltic amber The Baltic region is home to the largest known deposit of amber, called Baltic amber or succinite. It was produced sometime during the Eocene epoch, but exactly when is controversial. It has been estimated that these forests created more than 1 ...
or Florissant Formation forests, while the presence of the wasp family
Scelionidae The hymenopteran family Scelionidae is a very large cosmopolitan group (over 3000 described species in some 176 genera) of exclusively parasitoid wasps, mostly small (0.5–10 mm), often black, often highly sculptured, with (typically) elbowe ...
suggests generally mesic moisture conditions. Since the genus and first species descriptions, another series of species have been described from fossils found in Russia. The three species were described from compression fossils preserved in diatomite deposits of the Bol’shaya Svetlovodnaya site. Located in the
Pozharsky District Pozharsky District (russian: Пожа́рский райо́н) is an administrativeLaw #161-KZ and municipalLaw #191-KZ district (raion), one of the twenty-two in Primorsky Krai, Russia. It is located in the northern and northwestern parts of t ...
, on the Pacific Coast of Russia, the fossil bearing rocks preserve possibly
Priabonian The Priabonian is, in the ICS's geologic timescale, the latest age or the upper stage of the Eocene Epoch or Series. It spans the time between . The Priabonian is preceded by the Bartonian and is followed by the Rupelian, the lowest stage of t ...
plants and animals which lived in a small lake near a volcano. The site has been attributed to either the Maksimovka or Salibez Formations and compared to the Bembridge Marls and Florissant Formation, both of which are Priabonian in age.


History and classification

In 1849, some ant fossils from Radoboj were studied by
Oswald Heer Oswald Heer (or Oswald von Heer) (31 August 1809 – 27 September 1883), Swiss geologist and naturalist, was born at Niederuzwil in Canton of St. Gallen and died in Lausanne. Biography Oswald Heer was educated as a clergyman at Halle and ...
, then a professor with the University of Zürich. He placed the single species he described in the living genus ''
Formica ''Formica'' is a genus of ants of the family Formicidae, commonly known as wood ants, mound ants, thatching ants, and field ants. ''Formica'' is the type genus of the Formicidae, and of the subfamily Formicinae. The type species of genus ''For ...
'' as ''Formica ocella'' and in the same paper, a single male was described as ''Formica ocella'' var. ''paulo major'' based the large size of the abdomen. The species was retained in ''Formica'' by Gustav Mayr in 1867 and
Anton Handlirsch Anton Handlirsch or Anton Peter Josef Handlirsch (20 January 1865, Vienna – 28 August 1935, Vienna) was an Austrian entomologist. He worked on many groups including Hemiptera, Hymenoptera and Neuroptera. His most significant work was in the stu ...
in 1907. Mayr named two species ''Liometopum antiquum'' and ''Hypoclinea haueri'' in an 1867 publication on the ant fossils of Radoboj. The species ''Hypoclinea haueri'' was moved in 1893 by
Karl Wilhelm von Dalla Torre Karl Wilhelm von Dalla Torre (14 July 1850 – 6 April 1928) was an Austrian taxonomist, entomologist and botanist. Dalla Torre was born in Kitzbühel, Tyrol. He studied natural sciences at the University of Innsbruck. He then worked in the ...
from ''Hypoclinea'' to the combination ''Iridomyrmex haueri'', a placement that was not changed until 2014. The species and many of the type specimens were reexamined and redescribed in 2014 by paleoentomologists Gennady Dlussky and Tatyana Putyatina. When Dlussky, Rasnitsyn, and Perfilieva described the species ''E. biamoensis'', they gave it the name ''E. dubious'', but that name had already been used the year prior for a species from Radoboj. As such Perfilieva and Rasnitsyn proposed the replacement name ''E. biamoensis'' in a 2015 paper. They derived the name from "Biamo", the older name of the type locality at Bol’shaya Svetlovodnaya. A number of ''E. britannicus'' fossils are known and were described under three different names. The oldest descriptions are that of
Theodore Cockerell Theodore Dru Alison Cockerell (1866–1948) was an American zoology, zoologist, born at Norwood, England, and brother of Sydney Cockerell. He was educated at the Middlesex Hospital Medical School, and then studied botany in the field in Colorad ...
who named both ''Dolichoderus britannicus'' and ''Dolichoderus ovigerus'', citing small wing differences tentatively separating the two species. A third species, ''Emplastus emeryi'', was named by Horace Donisthorpe in 1920, and was the type species of the genus ''Emplastus''. In the time since the initial descriptions of the species, a number of additional queens and several males have been found, and a group of over twenty body fossils plus twenty seven wing fossils were studied by Dlussky and Perfilieva and published in 2014. The fossils showed a spectrum of wing morphology that bridged all three species, and as such they deemed both ''D. ovigerus'' and ''E. emeryi'' to be synonyms of the first published species name ''D. britannicus''. However the
propodeum The propodeum or propodium is the first abdominal segment in Apocrita Hymenoptera (wasps, bees and ants). It is fused with the thorax to form the mesosoma. It is a single large sclerite, not subdivided, and bears a pair of spiracles. It is strongl ...
is different than that of ''Dolichoderus'' species, being rounded in profile, and as such the species was retained in the genus ''Emplastus''. A second ''Emplastus'' species was described by Cockerell from the Bembridge Marls as ''Ponera hypolitha''. It was moved in 1964 to the fossil genus ''Poneropsis'', and finally to ''Emplastus'' in 2014.


Description

Species in ''Emplastus'' are not preserved well enough to place in formal genera, but a suite of characteristics is found in all the species which comprise the morphogenus. All the species have a similar size range, considered medium for ant species. The fossils have generally rectangular heads bearing triangular toothed mandibles and rounded
occipital The occipital bone () is a cranial dermal bone and the main bone of the occiput (back and lower part of the skull). It is trapezoidal in shape and curved on itself like a shallow dish. The occipital bone overlies the occipital lobes of the cereb ...
corners. In profile, the propodeum has a round upper surface and the gaster is smooth, with no constriction between the first and second segments. In gynes the petioles are enlarged, while in males, the outline is triangular. In the forewings there are 4 well formed cells enclosed by the veins, 1+2r, 3r, rm and mcu. The 3r cell has an elongated outline that extends to the upper wing margin. Of the wing veins, the 1RS runs perpendicular or slightly angled to the R vein.


''E. antiquus''

The neotype fossil is a long gyne preserved as a partial dorsal impression. This species is distinguished by the distinct but weakly concave ocular margin at the rear of the head. All other ''Emplastus'' species from Radoboj have slightly convex margins. While ''E. britannicus'' also has a concave rear to the head capsule, it is a larger species than ''E. antiquus'' and the antenna scape of ''E. britannicus'' is much shorter. Due to the poor wing preservation the species was moved from ''Liometopum'', though the preserved areas have a vein structure indicating relation to genera of the subfamily Dolichoderinae.


''E. biamoensis''

The single known queen of ''E. biamoensis'' is the only ''Emplastus'' gyne described from Bol’shaya Svetlovodnaya. Overall the species has a body length of The queen is distinct from the other Bol’shaya Svetlovodnaya species due to the forward set smallish eyes, whereas the two other species have large eyes. The species is smaller than the queens from the Bembridge Marls and Radoboj which range between . The petiole is smaller than that of ''E. britannicus'' and ''E. gurnetensis''.


''E. britannicus''

Females of ''E. britannicus'' range between with a forewing length between . The head is broader than it is long, giving a rectangular outline, and like ''E. antiquus'' of Radoboj it has a convex curve to the rear head margin. While Emery in his description asserted the mandibles to have a smooth margin, further specimens have shown that the robust mandibles have several blunt teeth on the chewing margin. The legs are usually short and thick. The petiole flared in width being up to three times as wide across as it is from front to back. The gaster is typically oval in outline. Males are smaller, at only approximately in length for the few described specimens. They have a small head, with similar mandibles to the females, and likewise similar short antenna scapes. Unlike the females, the legs of the males are long and fairly thin. The species names ''britannicus'' and ''ovigerus'' were not given etymologies by Cockerell, while the name ''emeryi'' was coined by Donisthorpe as a patronym honoring the Italian entomologist Carlo Emery, who gave input Donisthorpe on the Isle of Wight fossils, and for his work on Sicilian amber ants. Overall individuals of ''E. britannicus'' are the most numerous ant fossils in the Bembridge Marls.


''E. dubius''

The ''E. dubius'' queen is separated from the other species due to the distinct structure of the forewing cells. The wings have a triangular RM cell, while other species have a rectangular RM cell. Also the RM cell has a peduncle, while the RM cell of other species do not. The head is just slightly rectangular, being a little longer than wide. Similarly, the mesosoma is nearly one-and-a-half times longer than its height. The gaster, however, is an oval shape in outline. Dlussky and Putyatina coined the species name from the Latin " dubius", meaning uncertain. The queen was originally identified by Heer as a specimen of ''Formica globularus''.


''E. elongatus''

The solitary male specimen of ''E. elongatus'' is , preserved in profile, and with the head twisted so the upper area of the head capsule is showing. The front edge of the clypeus is slightly rounded, unlike that of ''E. macrops''. The angle of the head shows large developed ocelli, but the antennae are not preserved. The compound eyes are large as in ''E. macrops''. The two species are separated by the longer mesosoma of ''E. elongatus'', which also has a more rounded scutum.


''E. gurnetensis''

The head of the ''E. gurnetensis'' is longer than wide, with slightly convex sides and an occipital margin that may be straight or poorly convex. The propodeum is smoothly rounded in profile, and the legs are short and thick. The males are smaller than the queens, with an average body length of . The heads have large, visible ocelli, while the petiole is slightly higher than long with a triangular outline. Both the scutum and scutellum have convex upper surfaces, and the legs are long and thin. While ''E. gurnetensis'' is very similar to both ''E. britannicus'' and ''E. hypolithus'' in several respects, there are notable differences. The female size is smaller, at , than the male ''E. hypolithus'', indicating they are separate species. In the case of ''E. britannicus'', there are features of both the head and petiole structures that indicate they are distinct.


''E. haueri''

The single queen of this species was described by Mayr in 1867. The description provided in the type paper indicated a body length of about and with forewings nearly as long at . The slightly rounded mesosoma is distinct from all the other species being notably long. Since the holotype specimen could not be located for restudy and the one possible male of the species is not well preserved, the species was transferred from ''Iridomyrmex'' to ''Emplastus'' by Dlussky and Putyatina.


''E. hypolithus''

The species was redescribed from fourteen isolated wings and a single long male in 2014. The species is distinguishable by the notably narrow rm cell of the forewing, which mostly takes a triangular shape, but sometimes is quadrangular. The mid-sized cmu cell is trapezoidal and the rs-m cross-vein is usually placed on the wing tip side of the 2r-rs vein. The male has a small head with compound eyes located anterior to the head's midpoint. The scutellum is weakly rounded and about half the length of the mesosoma.


''E. kozlovi''

This Bembridge Marls species was described from a set of five solitary wings from males and females. The female forewings have lengths ranging between while the smaller male wings are generally . The vein structure is similar to that of ''E. britannicus'' though the wing size of the latter is smaller. ''E. kozlovi'' also differs in the proportioning of the triangular rm cell, which is longer than in ''E. britannicus''. One of the paratype wings had initially been identified by Donisthorpe as a wing of ''E. britannicus'', and was not re-identified until the description of ''E. kozlovi'' in 2014. Dlussky and Perfilieva named the species after the finder of the holotype fossil, Mikhail Kozlov.


''E. macrops''

''E. macrops'' was described from a single male preserved in profile. The fossil lacks portions of the antennae, wings, legs, and gaster, resulting in placement of the species into ''Emplastus''. The male has a short antenna scape that does not extend past the head capsule margin. The clypeus has a straight front edge bordering the triangular mandibles. ''E. macrops'' is distinguished from the other species in the genus based on the notably large compound eyes that are oval in outline and cover most of the side of the head. The species name is Latin, meaning, "with large eyes".


''E. miocenicus''

Dlussky and Putyatina described this species from a pair of fossils that had been identified as other species. The holotype queen was originally identified by Heer as ''Ponera fuliginosa'', while the paratype queen was identified by Heer as ''Formica ungeri''. While the queens are similar in appearance to ''E. haueri'', both are double in body length of that species, being long. The queens have heads that are nearly square, compound eyes placed near the midpoint, and a clypeus that is curved on the front margin.


''E. (?) ocellus''

The species was first described by Heer as ''Formica ocella'' from a pair of queens and males that he thought to be mating when entombed in the lake bottom, in addition to an additional solitary male. The type queen has a body length of , while the males range between . The head capsule is rectangular in outline with straight sides and a concave outline to the rear margin. The front edge of the clypeus is straight, bordering the mandibles which have a curving shape. The unique features of the head are distinct to the species, but preservation is poor enough that placement into a new genus or existing genus is problematic.


References


External links

* {{Taxonbar, from=Q18102521 Fossil taxa described in 1849 Fossil taxa described in 1867 Fossil taxa described in 1915 Fossil taxa described in 1920 Fossil taxa described in 2014 Fossil taxa described in 2015 Fossil ant genera Prehistoric insects of Europe Prehistoric insects of Asia Eocene insects