Baikuris
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''Baikuris'' is an extinct
genus Genus ( plural genera ) is a taxonomic rank used in the biological classification of living and fossil organisms as well as viruses. In the hierarchy of biological classification, genus comes above species and below family. In binomial nom ...
of
ant Ants are eusocial insects of the family Formicidae and, along with the related wasps and bees, belong to the order Hymenoptera. Ants evolved from vespoid wasp ancestors in the Cretaceous period. More than 13,800 of an estimated total of ...
in the Formicidae subfamily
Sphecomyrminae Sphecomyrminae is an extinct subfamily of ants in family Formicidae known from a series of Cretaceous fossils found in North America, Europe, and Asia. Sphecomyrminae contains eight genera, divided into two tribes Sphecomyrmini and Zigrasimec ...
, and is currently placed in the tribe Sphecomyrmini. The genus contains four described species: the type species ''Baikuris mandibularis'', along with ''Baikuris casei'', ''Baikuris maximus'', and ''Baikuris mirabilis''.


History and classification

The
type species In 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 species that contains the biological type specime ...
''B. mandibularis'' along with ''B. mirabilis'' were identified from adults preserved as
inclusion Inclusion or Include may refer to: Sociology * Social inclusion, aims to create an environment that supports equal opportunity for individuals and groups that form a society. ** Inclusion (disability rights), promotion of people with disabiliti ...
in Taimyr amber. The fossils of both species were collected on an expedition to the Taimyr peninsula. The ambers of the peninsula occur in the upper levels of the Kheta Formation, which is exposed in a number of locations in the Taimyr region. Age estimates of the Kheta Formation are between the Coniacian and
Santonian The Santonian is an age in the geologic timescale or a chronostratigraphic stage. It is a subdivision of the Late Cretaceous Epoch or Upper Cretaceous Series. It spans the time between 86.3 ± 0.7 mya (million years ago) and 83.6 ± 0.7 mya. ...
, and the ambers are found consistently in the upper most units, giving a Santonian age range for the inclusions. Based on the flora and fauna of the
Ledyanaya Ledyanaya (russian: Ледяная, meaning "Icy"), is a peak in the Koryak Mountains. Administratively it is part of the Kamchatka Krai, Russian Federation.Google Earth This high mountain is the highest point of the Koryak Mountains. It is a ...
and Mutino Formations which surround the Kheta formation, the paleoforest likely has a humid and warm temperate climate with the tees growing along river banks. While the resin producing trees have not been identified, the resins were likely dropped into the river systems and buried quickly in deltaic sediments. Both the holotype and the second specimen for ''B. casei'' are adult males which have been preserved as inclusions in transparent chunks of
New Jersey amber New Jersey Amber, sometimes called Raritan amber, is amber found in the Raritan and Magothy Formations of the Central Atlantic (Eastern) coast of the United States. It is dated to the Late Cretaceous, Turonian age, based on pollen analysis of t ...
. The amber specimens were recovered from deposits of the South Amboy Fire Clay, part of the
Raritan Formation The Raritan Formation is a Cretaceous (Turonian) geologic formation. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.Weishampel, et al. (2004). "Dinosaur ...
. New Jersey amber has been dated to approximately 90 to 94 mya, placing it in the
Turonian The Turonian is, in the ICS' geologic timescale, the second age in the Late Cretaceous Epoch, or a stage in the Upper Cretaceous Series. It spans the time between 93.9 ± 0.8 Ma and 89.8 ± 1 Ma (million years ago). The Turonian is preceded b ...
of the
Late Cretaceous The Late Cretaceous (100.5–66 Ma) is the younger of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', ...
. Analysis of the amber composition indicates it originated as cupressaceous resins which were deposited in lagoons and salt water marshes along the Cretaceous eastern seaboard. The fossil of ''B. maximus'' was discovered preserved as an inclusion in a transparent chunk of Charentese amber. The amber is thought to have been formed from resins of the extinct
Pinales The order Pinales in the division Pinophyta, class Pinopsida, comprises all the extant conifers. The distinguishing characteristic is the reproductive structure known as a cone produced by all Pinales. All of the extant conifers, such as cedar, ...
tree family
Cheirolepidiaceae Cheirolepidiaceae is an extinct family of conifers. They first appeared in the Triassic, and were widespread during most of the Mesozoic era. They are united by the possession of a distinctive pollen type assigned to the form genus '' Classopolli ...
and possibly from the living family
Araucariaceae Araucariaceae – also known as araucarians – is an extremely ancient family of coniferous trees. The family achieved its maximum diversity during the Jurassic and Cretaceous periods and the early Cenozoic, when it was distributed almost worldw ...
. Paleoecology based on Charentese amber inclusions indicate a shore line mangrove type forest that was of a subtropical to warm temperate climate, with occasional dry periods. The amber specimens are recovered from deposits exposed in quarries, road constructions, and beach exposures in the
Charente-Maritime Charente-Maritime () is a department in the Nouvelle-Aquitaine region on the southwestern coast of France. Named after the river Charente, its prefecture is La Rochelle. As of 2019, it had a population of 651,358 with an area of 6,864 square kil ...
region of coastal France, notably at Archingeay. Dating of the amber has been done through pollen analysis and it is generally accepted to be approximately 100 million years old. An additional amber specimen with partial fossils of six males of an unidentified species was described in 2013. The amber was recovered from sediments of the
Black Creek Formation The Black Creek Group is a geologic group in North Carolina. It preserves fossils dating back to the Late Cretaceous period. Paleofauna * cf. '' Deinosuchus rugosus'' * cf. '' Coelosaurus antiquus'' * cf. '' Dryptosaurus sp.'' * cf. '' Lophorh ...
along the
Neuse River The Neuse River ( , Tuscarora: Neyuherú·kęʔkì·nęʔ) is a river rising in the Piedmont of North Carolina and emptying into Pamlico Sound below New Bern. Its total length is approximately , making it the longest river entirely contained in ...
in North Carolina. Dating of the formation places the amber age between 83.6 and 72.1 million years old, in the
Campanian The Campanian is the fifth of six ages of the Late Cretaceous Epoch on the geologic timescale of the International Commission on Stratigraphy (ICS). In chronostratigraphy, it is the fifth of six stages in the Upper Cretaceous Series. Campani ...
. These males are the youngest occurrence of ''Baikurus'' identified, and they are of similar age to the Canadian Grassy Lake amber, though ''Baikurus'' has not been found in that amber. Both the North Carolina and ''B. casei'' males are preserved as groups of winged males, indicating that the genus displayed colonial behavior and likely had daytime nuptial fights similar to modern ants.


Description

The genus is known from adult males preserved in amber only. All species of ''Baikuris'' have kidney to oval shaped eyes. The narrow mandibles have a chewing edge that are parallel to each other and lacking teeth. At the base of the outer mandible surface is a ridge and oval area that may be the opening for the mandibular gland. The labial palps, visible on the ''B. casei'' fossil, have four segments, while the maxillary palps are elongated and have six segments each. On both the mid and hind leg sets, the end of the femurs have developed into additional trochantellus segments.


''B. casei''

Adult males of ''B. casei'' are approximately and fore-wings that are . Unlike males of ''B. mandibularis'' and ''B. miribilis'', the compound eyes of ''B. casei'' are oval in shape. Also in contrast, ''B. casei'' fore-wings do not have any crossveins between the cells 1r and 2r. The antennae have 13 segment total, with segment three being the longest and the pedicel being the shortest. The specific epithet ''casei'' was coined in honor of Gerard R. Case, who collected New Jersey amber from a number of localities between 1962 and 1986 and who worked to get the ambers studied in depth.


''B. mandibularis''

The three males described are all included in a single piece of amber labeled PIN 3730/5. The average length of the three is between , the smallest of the described species. The approximately fore wings of the holotype show several areas of folding and deformation. The area of the fore wing extending from the wing tip to the apex of the pterostigma curves away from the body towards the amber surface. The lower edge of the wing on the apical side of the anal vein is curved in towards the body.


''B. maximus''

''B. maximus'' is distinct from the other three species in that the males are distinctly larger at , while the other species are at most . There is also a distinct downward projection on the underside of the petiole node. The antennae are long with a filiform structure to the segments, though only the left antenna is preserved. The clypeus and mandibles are partially obscured and details difficult to distinguish. The mandibles seem to be small, with straight sides and having a small tooth just below the tip end. The species name was taken from the Latin maximus, which translates as "biggest" in reference to the size of the species.


''B. mirabilis''

This Taimyr species is described from a single partial male in amber specimen PIN 3730/8. The holotype has a total length of around , and the petiole is distinctly elongated. The wings are preserved, though the veination is faint in many areas, such as the r-rs vein and the 3cu vein. The fore wings are an estimated long and show distinct darkening in the middle area. As a result of cleavages both the base and tip areas of the left fore wing are missing. The right wing is complete and distinct, despite the inward curving of the wing tip area. There are at least twelve hamuli on the wing, but fissures obscure the wing so a total number cannot be determined.


''Baikuris incertae sedis''

The fossils from North Carolina have a mix of features seen in both the two Taimyr amber species and in ''B. casei''. Like ''B. mirabilis'' and ''B. mandibularis'' the costal vein in the fore wing extends to the pterostigma, while it does not it ''B. casei''. The eyes of the North Carolina fossils are oval in outline though, which is only seen in ''B. casei'' and not the Taimyr amber species. Unlike any of the other ''Baikuris'' species, the North Carolina fossils have short labial and long maxillary palps. The combination of characters is not seen in any of the other species, and they were not placed into a new species in the 2013 paper.


References


External links

* * {{Taxonbar, from=Q9164275 Sphecomyrminae Cretaceous insects Fossil ant genera Fossil taxa described in 1987 Fossil taxa described in 1997 Fossil taxa described in 2015 Prehistoric insects of North America Cretaceous insects of Asia Taimyr amber New Jersey amber