Pachycondyla oligocenica

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Pachycondyla oligocenica
Temporal range: Priabonian
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Scientific classification Red Pencil Icon.png
Kingdom: Animalia
Clade: Euarthropoda
Class: Insecta
Order: Hymenoptera
Family: Formicidae
Genus: Pachycondyla
Species:P. oligocenica
Binomial name
Pachycondyla oligocenica
Dlussky, Rasnitsyn & Perfilieva, 2015

Pachycondyla oligocenica is an extinct species of formicid in the ant subfamily Ponerinae known from a fossil found in eastern Asia.

In biology, a species ( ) is the basic unit of classification and a taxonomic rank of an organism, as well as a unit of biodiversity. A species is often defined as the largest group of organisms in which any two individuals of the appropriate sexes or mating types can produce fertile offspring, typically by sexual reproduction. Other ways of defining species include their karyotype, DNA sequence, morphology, behaviour or ecological niche. In addition, paleontologists use the concept of the chronospecies since fossil reproduction cannot be examined. While these definitions may seem adequate, when looked at more closely they represent problematic species concepts. For example, the boundaries between closely related species become unclear with hybridisation, in a species complex of hundreds of similar microspecies, and in a ring species. Also, among organisms that reproduce only asexually, the concept of a reproductive species breaks down, and each clone is potentially a microspecies.

Ponerinae subfamily of insects

Ponerinae is a subfamily of ants in the Poneromorph subfamilies group, with about 1,600 species in 47 extant genera, including Dinoponera gigantea - one of the world's largest species of ant. Mated workers have replaced the queen as the functional egg-layers in several species of ponerine ants. In such queenless species, the reproductive status of workers can only be determined through ovarian dissections.

Contents

History and classification

P. oligocenica is known from a single ant found in Russia. [1] The specimen was described from a compression fossil preserved in diatomite deposits of the Bol’shaya Svetlovodnaya site. The site is exposed on the bank of Barachek Creek 3 km (3,000 m) upstream from the creeks confluence with the Bol’shaya Svetlovodnaya River [2] in the Pozharsky District, on the Pacific Coast of Russia. The fossil-bearing rocks preserve possibly Priabonian plants and animals which lived in and around 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. [1]

Compression fossil

A compression fossil is a fossil preserved in sedimentary rock that has undergone physical compression. While it is uncommon to find animals preserved as good compression fossils, it is very common to find plants preserved this way. The reason for this is that physical compression of the rock often leads to distortion of the fossil.

Pozharsky District District in Primorsky Krai, Russia

Pozharsky District is an administrative and municipal district (raion), one of the twenty-two in Primorsky Krai, Russia. It is located in the northern and northwestern parts of the krai and borders with Khabarovsk Krai in the north, Terneysky District in the east and southeast, Krasnoarmeysky District in the south, Dalnerechensky District in the southwest, and with China in the west. The area of the district is 22,570.3 square kilometers (8,714.4 sq mi). Its administrative center is the urban locality of Luchegorsk. Population: 31,086 (2010 Census); 34,120 (2002 Census); 35,826 (1989 Census). The population of Luchegorsk accounts for 67.6% of the district's total population.

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 37.8 and33.9 Ma. The Priabonian is preceded by the Bartonian and is followed by the Rupelian, the lowest stage of the Oligocene.

At the time of description, the holotype male specimen, number PIN 3429/1112 was preserved in the A. A. Borissiak Paleontological Institute collections, part of the Russian Academy of Sciences. [1] The fossil was first described by the trio of paleomyrmecologists Gennady Dlussky, Alexandr Rasnitsyn and Ksenia Perfilieva. In the type description, Dlussky, Rasnitsyn and Perfilieva named the species P. oligocenica, with the specific epithet derived "Oligocene" the possible age of the site. [1]

Holotype single physical example (or illustration) of an organism, known to have been used when the species (or lower-ranked taxon) was formally described

A holotype is a single physical example of an organism, known to have been used when the species was formally described. It is either the single such physical example or one of several such, but explicitly designated as the holotype. Under the International Code of Zoological Nomenclature (ICZN), a holotype is one of several kinds of name-bearing types. In the International Code of Nomenclature for algae, fungi, and plants (ICN) and ICZN the definitions of types are similar in intent but not identical in terminology or underlying concept.

Russian Academy of Sciences academy of sciences

The Russian Academy of Sciences consists of the national academy of Russia; a network of scientific research institutes from across the Russian Federation; and additional scientific and social units such as libraries, publishing units, and hospitals.

Alexandr Rasnitsyn Russian scientist

Alexandr Pavlovich Rasnitsyn is a Russian entomologist, expert in palaeoentomology, and Honored Scientist of the Russian Federation (2001). His scientific interests are centered on the palaeontology, phylogeny, and taxonomy of hymenopteran insects and insects in general. He has also studied broader biological problems such as evolutionary theory, the principles of phylogenetics, taxonomy, nomenclature, and palaeoecology. He has published over 300 articles and books in several languages. In August 2008 he was awarded the Distinguished Research Medal of the International Society of Hymenopterists.

At the time of description, only two other Pachycondyla species males had been described from fossils; the males of both P. baltica and P. succinea are known from fossils entombed in Eocene age Baltic amber. [1] P. oligocenica is distinguished from both baltic amber species in that the holotype male is larger than the other males, males of those species with bodies ranging between 3.5–4.5 mm (0.14–0.18 in) long. [1] P. oligocenica is one of two Pachycondyla species that were described by Dlussky, Rasnitsyn and Perfilieva from Bol’shaya Svetlovodnaya, the other species P. aberrans being described from a partial queen or male. [1]

<i>Pachycondyla succinea</i> species of insect (fossil)

Pachycondyla succinea is an extinct species of ant in the formicid subfamily Ponerinae described from fossils found in Europe. P. petrosa is one of three middle Eocene Pachycondyla species found in Baltic amber.

Baltic amber

The Baltic region is home to the largest known deposit of amber, called Baltic amber or succinite. It dates from 44 million years ago. It has been estimated that these forests created more than 100,000 tons of amber. Today, more than 90% of the world's amber comes from Kaliningrad Oblast of Russia. It is a major source of income for the region; the local Kaliningrad Amber Combine extracted 250 tonnes of it in 2014, 400 tonnes in 2015.

Pachycondyla aberrans is an extinct species of formicid in the ant subfamily Ponerinae known from a single fossil found in Russia.

P. succinea male Pachycondyla succinea BMNHP29202 full 01.jpg
P. succinea male

Description

Though incomplete, the P. oligocenica male has an estimated body length of 7 mm (0.28 in), while the alitrunk is 2.3 mm (0.091 in). The head has an almost square outline, being slightly shorter than it is wide, and the rear edge is rounded. The large oval shaped eyes convex in shape, protruding slightly from the head capsule. Neither of the mandibles have any teeth along the edges, and they are placed far apart on the head, preventing touching when they close. The antennae are not preserved from the holotype, so the structure and length was unknown at the time of description. The forewing has a length of 4.1 mm (0.16 in) with the veins fully enclosing and forming the cells 1+2r, 3r, mcu, and rm. The rm cell is not present in the forewing of P. aberrans, distinguishing the two species. [1]

Mesosoma

The mesosoma is the middle part of the body, or tagma, of arthropods whose body is composed of three parts, the other two being the prosoma and the metasoma. It bears the legs, and, in the case of winged insects, the wings.

Antenna (biology) appendages used for sensing in arthropods

Antennae, sometimes referred to as "feelers", are paired appendages used for sensing in arthropods.

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References

  1. 1 2 3 4 5 6 7 8 Dlussky, G.M.; Rasnitsyn, A.P.; Perfilieva, K.S. (2015). "The Ants (Hymenoptera: Formicidae) of Bol'shaya Svetlovodnaya (Late Eocene of Sikhote-Alin, Russian Far East)" (PDF). Caucasian Entomological Bulletin. 11 (1): 131–152.
  2. Rasnitsyn, A. P.; Quicke, D. L., eds. (2006). "Impression fossils". History of insects. Springer Science & Business Media. p. 438.