Makarkinia

Last updated

Contents

Makarkinia
Temporal range: Aptian
~115–113  Ma
O
S
D
C
P
T
J
K
Pg
N
Makarkinia irmae by THSpike.jpg
Life restoration of M. irmae
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Class: Insecta
Order: Neuroptera
Family: Kalligrammatidae
Genus: Makarkinia
Martins-Neto 1997
Species
  • M. adamsi
  • M. kerneri
  • M. irmae

Makarkinia is an extinct genus of lacewings in the family Kalligrammatidae described by Martins-Neto in 1997 from fossils found in the Crato Formation of the Araripe Basin in northeastern Brazil. The genus contains three species dating to the Late Aptian, Makarkinia adamsi, Makarkinia kerneri and Makarkinia irmae. [1]

History and classification

When first described, Makarkinia was known from a single fossil wing which is a compression-impression fossil preserved in layers of soft sedimentary rock. [2] Along with other well-preserved insect fossils, the Makarkinia specimens were collected from layers of the Upper Aptian Crato Formation. The formation is composed of unweathered grey and oxidized yellow limestones, which preserved numerous insects, fish, birds and reptiles as a notable lagerstätten. The area is a preserved inland lake or one of a series of lakes, though the nature as a fresh or salt-water body is uncertain. The depth of the basin has been suggested as either shallow or fairly deep. The basin formed near the center of the supercontinent Gondwana during the early part of the diversification of flowering plants. [3]

The M. adamsi holotype specimen was preserved in the National Museum of Brazil paleontological collection when first studied. [4] The fossil was described by R. G. Martins-Neto in a 1992 paper on the neuropterans of the Crato Formation, with the species named in it. [2] At the time of description the species was placed into the extinct family Panfiloviidae as Panfilovia adamsi. This placement was changed in a 1997 by Martins-Neto who moved the species to a new genus, Makarkinia and new subfamily "Makarkiniinae" in Panfiloviidae. Three years later Martins-Neto elevated the subfamily to a full family as Makarkiniidae, though this change was not widely used. It was suggested by Makarkin and Archibald in 2003 and subsequent authors that the genus was closely related to Kalligrammatidae, and moved into the family in 2016 by Günter Bechly and Vladimir Makarkin. [2]

The second species described, M. kerneri, is known from the single holotype specimen residing in the Staatliches Museum für Naturkunde collections at the time of description. The fossil was first studied by Günter Bechly and Vladimir Makarkin who erected the species in a Cretaceous Research paper published in 2016. They coined the specific epithet kerneri to honor Andreas Kerner, who owned the fossil until its donation to the Staatliches Museum für Naturkunde. [2]

When M. kerneri was described, Makarkinia was the only Kalligrammatidae genus known from the Americas, the other members of the family having been described from Asian and European fossils. Like other kalligrammatids, the environment of Makarkinia was subtropical to tropical in temperature, and color patterning of the fossils indicates they were daytime fliers. To lessen predation by other animals, large eye spots are found on the hindwings. The genus is the youngest member of the family to be described, living slightly after the last Eurasian genera from the early Aptian of China. Makarkinia also had the largest wing size of any living or fossil lacewing (indeed of any member of the order Neuroptera) and had an estimated maximum wing length of approximately 160 millimetres (6.3 in). [2]

Description

Makarkinia species are distinguished from other genera by the subcostal veinlets which notably curve towards the wing tip. The veinlets are forked with one to four small branches. The hindwings have a large distinct eye spot centered in the wing and surrounded by three concentric circles. [2]

M. adamsi

The holotype wing is partially preserved and thought to be a possible forewing, though it is not whole enough to confirm. The estimated wing length is approximately 140–160 mm (5.5–6.3 in). [2] However, no information was provided as how that inference was obtained, since it is only known from fairly partial fossil not enough to reconstruct whole wing, and wing length-width ratio is completely unknown since that is quite different among kalligrammatids. [1]

M. kerneri

The overall size of the M. kerneri hindwing is smaller than M. adamsi, being 78 mm (3.1 in) and estimated between 100–120 mm (3.9–4.7 in) in full length. The costal vein starts fairly thick in the basal section of the wing and tapers down as it progresses towards the wing tip. The subcostal veinlets below the costa curve towards the wing tip and are fairly widely spaced. Between the major veins on most of the wing are many densely spaced crossveins, with the exception of between the veins at the wings tip end. The wing is covered in a coating of setae, very thick on the outer margins and major veins. On the thin veins running lengthwise along the wing and the crossveins the setae are thinner, arranged into three rows on the veins. The wing membrane has a coating of setae that thins out approaching the wing tip. The color pattering consists of a notable eye-spot that is 11 mm (0.43 in) in diameter, several darker longitudinal stripes and darkening of the costal area. [2]

M. irmae

M. irmae is known from 77 millimetres (3.0 in) long hindwing fragment which preserves eye spot patterning. [1]

Related Research Articles

<span class="mw-page-title-main">Crato Formation</span> Geologic formation of Early Cretaceous age in northeastern Brazil

The Crato Formation is a geologic formation of Early Cretaceous (Aptian) age in northeastern Brazil's Araripe Basin. It is an important Lagerstätte for palaeontologists. The strata were laid down mostly during the Aptian age, about 113 million years ago. It thought to have been deposited in a semi-arid lacustrine wetland environment.

<span class="mw-page-title-main">Neuroptera</span> Order of insects

The insect order Neuroptera, or net-winged insects, includes the lacewings, mantisflies, antlions, and their relatives. The order consists of some 6,000 species. Neuroptera is grouped together with the Megaloptera and Raphidioptera (snakeflies) in the unranked taxon Neuropterida.

<span class="mw-page-title-main">Snakefly</span> Order of insects

Snakeflies are a group of predatory insects comprising the order Raphidioptera with two extant families: Raphidiidae and Inocelliidae, consisting of roughly 260 species. In the past, the group had a much wider distribution than it does now; snakeflies are found in temperate regions worldwide but are absent from the tropics and the Southern Hemisphere. Recognisable representatives of the group first appeared during the Early Jurassic. They are a relict group, having reached their apex of diversity during the Cretaceous before undergoing substantial decline.

<span class="mw-page-title-main">Hemerobiidae</span> Family of insects

Hemerobiidae is a family of Neuropteran insects commonly known as brown lacewings, comprising about 500 species in 28 genera. Most are yellow to dark brown, but some species are green. They are small; most have forewings 4–10 mm long. These insects differ from the somewhat similar Chrysopidae not only by the usual coloring but also by the wing venation: hemerobiids differ from chrysopids in having numerous long veins and forked costal cross veins. Some genera are widespread, but most are restricted to a single biogeographical realm. Some species have reduced wings to the degree that they are flightless. Imagines (adults) of subfamily Drepanepteryginae mimic dead leaves. Hemerobiid larvae are usually less hairy than chrysopid larvae.

<span class="mw-page-title-main">Berothidae</span> Family of insects

The Berothidae are a family of winged insects of the order Neuroptera. They are known commonly as the beaded lacewings. The family was first named by Anton Handlirsch in 1906. The family consists of 24 genera and 110 living species distributed discontinuously worldwide, mostly in tropical and subtropical regions. Numerous extinct species have also been described. Their ecology is poorly known, but in the species where larval stages have been documented, the larvae are predators of termites.

<span class="mw-page-title-main">Nymphidae</span> Family of insects

Nymphidae, sometimes called split-footed lacewings, are a family of winged insects of the order Neuroptera. There are 35 extant species native to Australia and New Guinea.

<span class="mw-page-title-main">Psychopsidae</span> Family of insects

Psychopsidae is a family of winged insects of the order Neuroptera. They are commonly called silky lacewings.

<i>Undulopsychopsis</i> Extinct genus of insects

Undulopsychopsis is an extinct genus of lacewing in the silky lacewing family Psychopsidae. The genus is solely known from a Cretaceous fossil found in China. Currently the genus is composed of a single species, Undulopsychopsis alexi.

<span class="mw-page-title-main">Stenophlebiidae</span> Extinct family of insects

The Stenophlebiidae is an extinct family of medium-sized to large fossil odonates from the Upper Jurassic and Cretaceous period that belongs to the damsel-dragonfly grade ("anisozygopteres") within the stem group of Anisoptera. They are characterized by their long and slender wings, and the transverse shape of the discoidal triangles in their wing venation.

<i>Elektrithone</i> Extinct genus of insects

Elektrithone is an extinct genus of lacewing in the moth lacewings family Ithonidae. The genus is solely known from an Eocene fossil forewing found in Europe. At the times of description the genus was composed of a single species, Elektrithone expectata.

Principiala is an extinct genus of lacewing in the moth lacewings family Ithonidae. The genus is known from Cretaceous fossils found in South America, Europe, and possibly Asia. The genus is composed of two species, the type species Principiala incerta, and Principiala rudgwickensis.

Wesmaelius mathewesi is an extinct species of lacewing in the neuropteran family Hemerobiidae known from an Eocene fossil found in North America

Cretomerobius is an extinct genus of lacewings in the neuropteran family Hemerobiidae known from fossils found in Asia. The genus currently contains a single species, the Aptian C. disjunctus.

<span class="mw-page-title-main">Kalligrammatidae</span> Extinct family of insects

Kalligrammatidae, sometimes known as kalligrammatids or kalligrammatid lacewings, is a family of extinct insects in the order Neuroptera (lacewings) that contains twenty genera and a number of species. The family lived from the Middle Jurassic to the early Late Cretaceous before going extinct. Species of the family are known from Europe, Asia, and South America. The family has been occasionally described as "butterflies of the Jurassic" based on their resemblance to modern butterflies in morphology and ecological niche.

Araripenymphes is an extinct genus of lacewing in the family Nymphidae known from fossils found in the Crato Formation of the Araripe Basin in South America. The genus contains a single species, Araripenymphes seldeni. The genus was named after the basin.

Rafaelnymphes is an extinct genus of lacewing in the family Nymphidae known from a fossil found in South America. The genus contains a single species, Rafaelnymphes cratoensis.

Prosisyrina is an extinct genus of lacewing in the neuropteran family Sisyridae. The genus contains two described species, Prosisyrina sphinga and Prosisyrina sukachevae. Prosisyrina is known from a group of Late Cretaceous fossils which were found in Asia.

<span class="mw-page-title-main">Babinskaiidae</span> Extinct family of insects

Babinskaiidae is an extinct family of neuropterans known from the Cretaceous period. They are part of the superfamily Myrmeleontoidea. Their distinguishing characters include: "long filiform antennae, narrowly elongated wings, with features such as trichosors, and presectorial cross veins present in both wings, and absence of forewing oblique vein". They are considered transitional between Nymphidae and more derived myrmeleontodoids, such as antlions.

<i>Palaeopsychops</i> Extinct genus of lacewings

Palaeopsychops is an extinct genus of lacewing in the moth lacewings family Ithonidae. The genus is known from Early Eocene fossils found in Europe, and North America and is composed of ten species. The ten species can be informally separated into two species groups based on veination of the forewings, the "European" and "North American" groups. When first described, the genus was placed in the family Psychopsidae, but later was moved to Polystoechotidae, which itself is now considered a subgroup of the moth lacewings.

<i>Polystoechotites</i> Extinct genus of lacewings

Polystoechotites is an extinct parataxon of lacewings in the moth lacewing family Ithonidae. The taxon is a collective group for fossil polystechotid giant lacewing species whose genus affiliation is uncertain, but which are distinct enough to identify as segregate species. Polystoechotites species are known from Eocene fossils found in North America and is composed of four named species Polystoechotites barksdalae, Polystoechotites falcatus, Polystoechotites lewisi, and Polystoechotites piperatus, plus two unnamed species. Three of the described species are known from fossils recovered from the Eocene Okanagan Highlands of Washington State, while the fourth is from Colorado.

References

  1. 1 2 3 Machado, Renato J. P.; Freitas, André V. L.; Ribeiro, Guilherme C. (2021-04-01). "A new giant species of the remarkable extinct family Kalligrammatidae (Insecta: Neuroptera) from the Lower Cretaceous Crato Formation of Brazil". Cretaceous Research. 120: 104724. Bibcode:2021CrRes.12004724M. doi:10.1016/j.cretres.2020.104724. ISSN   0195-6671. S2CID   230637153.
  2. 1 2 3 4 5 6 7 8 Bechly, G.; Makarkin, V. N. (2016). "A new gigantic lacewing species (Insecta: Neuroptera) from the Lower Cretaceous of Brazil confirms the occurrence of Kalligrammatidae in the Americas". Cretaceous Research. 58: 135–140. Bibcode:2016CrRes..58..135B. doi:10.1016/j.cretres.2015.10.014.
  3. Martill, David M.; Bechly, Günter; Loveridge, Robert F. (2007). The Crato Fossil Beds of Brazil: Window into an Ancient World. Cambridge University Press. pp. 1–4. ISBN   978-1-139-46776-6.
  4. "Fossilworks: Makarkinia adamsi" . Retrieved 17 December 2021.