The Tarsophlebiidae 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 ...
family
Family (from la, familia) is a Social group, group of people related either by consanguinity (by recognized birth) or Affinity (law), affinity (by marriage or other relationship). The purpose of the family is to maintain the well-being of its ...
of medium-sized
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 preserved ...
odonates from the
Upper Jurassic
The Late Jurassic is the third epoch of the Jurassic Period, and it spans the geologic time from 163.5 ± 1.0 to 145.0 ± 0.8 million years ago (Ma), which is preserved in Upper Jurassic strata.Owen 1987.
In European lithostratigraphy, the name ...
and
Lower Cretaceous
Lower may refer to:
*Lower (surname)
*Lower Township, New Jersey
*Lower Receiver (firearms)
*Lower Wick
Lower Wick is a small hamlet located in the county of Gloucestershire, England. It is situated about five miles south west of Dursley, eight ...
period
Period may refer to:
Common uses
* Era, a length or span of time
* Full stop (or period), a punctuation mark
Arts, entertainment, and media
* Period (music), a concept in musical composition
* Periodic sentence (or rhetorical period), a concept ...
of
Eurasia
Eurasia (, ) is the largest continental area on Earth, comprising all of Europe and Asia. Primarily in the Northern and Eastern Hemispheres, it spans from the British Isles and the Iberian Peninsula in the west to the Japanese archipelago a ...
. They are either the most basal member of the damsel-dragonfly grade ("anisozygopteres") within the
stem group
In phylogenetics, the crown group or crown assemblage is a collection of species composed of the living representatives of the collection, the most recent common ancestor of the collection, and all descendants of the most recent common ancestor. ...
of
Anisoptera
A dragonfly is a flying insect belonging to the infraorder Anisoptera below the order Odonata. About 3,000 extant species of true dragonfly are known. Most are tropical, with fewer species in temperate regions. Loss of wetland habitat threate ...
, or the sister group of all Recent odonates. They are characterized by the basally open discoidal cell in both pairs of wings, very long legs, paddle-shaped male
cerci, and a hypertrophied
ovipositor
The ovipositor is a tube-like organ used by some animals, especially insects, for the laying of eggs. In insects, an ovipositor consists of a maximum of three pairs of appendages. The details and morphology of the ovipositor vary, but typical ...
in females.
Description
Adult
Body
![Tarsophlebia eximia holotype BSPGM AS VI 44b right hind leg](https://upload.wikimedia.org/wikipedia/commons/b/b2/Tarsophlebia_eximia_holotype_BSPGM_AS_VI_44b_right_hind_leg.png)
The head is similar to that of Recent
Gomphidae
The Gomphidae are a family of dragonflies commonly referred to as clubtails or club-tailed dragonflies. The family contains about 90 genera and 900 species found across North and South America, Europe, Asia, and Australia. The name refers to the ...
with two large and globular
compound eye
A compound eye is a visual organ found in arthropods such as insects and crustaceans. It may consist of thousands of ommatidia, which are tiny independent photoreception units that consist of a cornea, lens, and photoreceptor cells which disti ...
s that are distinctly separated, but closer together than in damselflies (
Zygoptera). There are also two cephalic sutures.
The pterothorax seems to be even more strongly skewed than in damselflies. The legs are extremely long with short and strong spines, and with very elongate tarsi. There are three tarsal segments (
tarsomeres), of which the most basal one is twice as long as the others. The pair of tarsal claws lack the ventro-apical hook of modern odonates.
Wings and wing venation
The largest species ''Turanophlebia sinica'' reached a wingspan of about , while the smallest species ''Tarsophlebia minor'' reached only a wingspan of about .
[
]
The wing venation is characterized by the following features:
wings hyaline, slender, and not stalked; discoidal cell basally open in both pairs of wings, so that the arculus is incomplete; forewing discoidal cell very acute; large and acute subdiscoidal cell in hindwing; primary antenodal braces Ax1 and Ax2 stronger than the secondary antenodal crossveins; nodus in distal position at 44-47% of wing length; nodus with terminal kink of CP and a strong nodal furrow; pterostigma elongate (covering several cells) and with oblique brace vein; one lestine oblique vein 'O' present between RP2 and IR2; in all wings there are pairs of secondary longitudinal concave intercalary veins anterior and posterior of the convex veins CuA, MA, and IR2, and closely parallel to them (the postero-intercalaries are always longer than the associated antero-intercalaries); hindwings without vein CuAb; crossvein-like remnant of vein CuP is curved and rather looks like a branch of AA.[
]
Sexual dimorphism
Males are distinguished by paddle-like cerci,[ while females are distinguished by very long and thin, hypertrophied ovipositor that projects far beyond the abdomen.][
]
The male secondary genitalia were of a unique primitive type, with a small sperm vesicle on sternite 3, two pairs of small plate-like hamuli on sternite 2, and a very short median ligula on sternite 2. Obviously, none of these structures is hypertrophied as sperm intromittent organ (functional penis). In each of the three suborders of Recent odonates, a different part of this apparatus is enlarged and developed as intromittent organ and device for removal of foreign sperm (sperm competition): in Zygoptera it is the ligula, an median process of sternite 2; in Epiophlebiidae it is the lateral pair of posterior hamuli on segment 2; and in Anisoptera it is the unpaired sperm vesicle on the anterior part of sternite 3. The structure of the apparatus in Tarsophlebiidae is suggestive of an intermediate state between protodonates and modern odonates. An exceptionally well-preserved male specimen of ''Namurotypus sippeli'' showed that protodonate Meganisoptera
Meganisoptera is an extinct order of very large to gigantic insects, informally called griffinflies. The order was formerly named Protodonata, the "proto-Odonata", for their similar appearance and supposed relation to modern Odonata (damselflies ...
completely lacked a secondary genital apparatus on abdominal segments 2 and 3 and still had primary genitalia on segment 9 that strongly resemble those of wingless silverfish, who do not copulate but deposit external spermatophore
A spermatophore or sperm ampulla is a capsule or mass containing spermatozoa created by males of various animal species, especially salamanders and arthropods, and transferred in entirety to the female's ovipore during reproduction. Spermatophores ...
s. Only on the basis of such a mating behaviour is the evolution of the odonate secondary copulation conceivable at all. A first step probably was the attachment of a spermatophore to the basal sternites of the male abdomen instead of a deposition on substrate. The female now had to fetch the spermatophore from the male venter. This created an adaptive pressure to create storage structures for the spermatophore and attachment structures for the female genitalia. Tarsophlebiidae probably represent this state of evolution. The development of liquid sperm and intromittent organs for copulation apparently evolved three times in parallel in the three extant suborders.
Lateral auricles on the sides of the basal abdomen in male ''Tarsophlebia eximia'' had been described by Nel et al. (1993).[ However, Bechly (1996) showed that these alleged male auricles were based on a misinterpretation of the hamuli posteriors,] which was confirmed by Fleck et al. (2004).[
Fleck et al. (2004) demonstrated that male Tarsophlebiidae did possess a unique type of anal appendages. The description of calopterygoid-like appendages of ''Tarsophlebia eximia'', with apparently two pairs of claspers,][ was based on misinterpretations due to artifacts of preservation. The cerci are very long, with a double-barreled basal petiole and a distal plate-like expansion. The broken double-barrelled petioles of the two cerci have been commonly misinterpreted as two pairs of claspers, while the distal plates have been overlooked or regarded as artifacts.][ Indeed, ''Tarsophlebia'' does neither possess zygopteroid- nor anisopteroid-like appendages. There are no visible paraprocts (as in Zygoptera) and no epiproct (as in Epiophlebiidae and Anisoptera). If these structures are secondarily reduced or primarily missing is not clear.
]
Larva
No fossil larvae of this extinct family have yet been discovered.
Classification
The family
Family (from la, familia) is a Social group, group of people related either by consanguinity (by recognized birth) or Affinity (law), affinity (by marriage or other relationship). The purpose of the family is to maintain the well-being of its ...
was established by Handlirsch (1906) on the basis of the type genus ''Tarsophlebia'' Hagen, 1866.
''Tarsophlebiopsis mayi'' was recognized as valid by most authors until the most recent revision of the family by Fleck et al. (2004), who demonstrated that the holotype of this taxon most probably is only an aberrant specimen of ''Tarsophlebia eximia''.[
The family contains 2 described genera with totally 9 valid species:]
Paleobiology Database entry for Tarsophlebiidae
*Genus ''Tarsophlebia'' Hagen, 1866 (type genus; synonym: ''Tarsophlebiopsis'' Tillyard, 1923)
Diagnosis: cubito-anal areas of forewings and hindwings with four rows of cells or less; 16 or less postnodal crossveins; less than ten secondary antenodal crossveins in hindwing; and IR1 relatively short.
**''Tarsophlebia eximia'' (Hagen, 1862) - (type species; type locality: Eichstätt, Bavaria, Germany; type horizon: Upper Jurassic, Malm zeta 2b, Lower Tithonian / 150 mya, Hybonotum Zone, Solnhofener Plattenkalk Formation; holotype: no. AS VI 44a,b at BSPG Munich Museum; size: forewing 37.1, hindwing 34.7 mm; synonyms: ''Tarsophlebia major'' Handlirsch, 1906, ''Tarsophlebia longissima'' Handlirsch, 1906, ''Tarsophlebiopsis mayi'' Tillyard, 1923[)]
**''Tarsophlebia minor'' Fleck et al., 2004[ - (type locality: Eichstätt, Bavaria, Germany; type horizon: Upper Jurassic, Malm zeta 2b, Lower Tithonian / 150 mya, Hybonotum Zone, Solnhofener Plattenkalk Formation; holotype: no. 55 at MCZ; size: hindwing 26 mm)]
*Genus ''Turanophlebia'' Pritykina, 1968
Diagnosis: wings with more dense venation; presence of more than 25 postnodal crossveins (11-16 in ''Tarsophlebia''); six or more rows of cells between CuA and posterior hindwing margin (less than five rows in ''Tarsophlebia''); more than 10 secondary antenodal crossveins in hindwing (less than 10 in ''Tarsophlebia''); IR1 longer than in ''Tarsophlebia''; presence of long secondary longitudinal not zigzagged veins in area between IR2 and RP2.
**''Turanophlebia anglicana'' Fleck et al., 2004[ - (type locality: Clockhouse (Butterley) Brickworks, England; type horizon: Lower Cretaceous, Upper Hauterivian / 130 mya, Lower ]Weald Clay
Weald Clay or the Weald Clay Formation is a Lower Cretaceous sedimentary rock unit underlying areas of South East England, between the North and South Downs, in an area called the Weald Basin. It is the uppermost unit of the Wealden Group of ro ...
; holotype: no. BMB 018531 at Booth Museum in Brighton / UK; size: hindwing 39.7 mm)
**''Turanophlebia liaoningensis'' Fang & Zheng, 2022 - (type locality: Huangbanjigou Village, western Liaoning, China; type horizon: Lower Cretaceous, Yixian Formation
The Yixian Formation (; formerly transcribed as Yihsien Formation) is a geological formation in Jinzhou, Liaoning, People's Republic of China, that spans the late Barremian and early Aptian stages of the Early Cretaceous. It is known for its ex ...
)
**''Turanophlebia martynovi'' Pritykina, 1968 - (type species; type locality: Karatau-Mikhailovka, Chimkent region, Southern Kazakhstan; type horizon: Upper Jurassic, Callovian- Kimmeridgian or Oxfordian-Kimmeridgian / 163 mya, Karabastau Formation
The Karabastau Formation ( kk, Qarabastaý svıtasy) is a geological formation and lagerstätte in the Karatau Mountains of southern Kazakhstan whose strata date to the Middle to Late Jurassic. It is an important locality for insect fossils that ...
; holotype: no. PIN 2554/210 at Palaeontological Institute Moscow; size: hindwing 41.0 mm)
**''Turanophlebia mongolica'' Fleck et al., 2004[ - (type locality: Bon-Tsagaan, Bayanhongor Aimak, Central Mongolia; type horizon: Lower Cretaceous, Hauterivian-Barremian / 129 mya, Dzun-Bain Formation; holotype: no. PIN 3559/69 at Palaeontological Institute Moscow; size: hindwing 41.0 mm)]
**''Turanophlebia neckini'' (Martynov, 1927) - (type locality: Karatau-Karabastau, Chimkent region, Southern Kazakhstan; type horizon: Upper Jurassic, Callovian- Kimmeridgian or Oxfordian-Kimmeridgian / 163 mya, Karabastau Formation
The Karabastau Formation ( kk, Qarabastaý svıtasy) is a geological formation and lagerstätte in the Karatau Mountains of southern Kazakhstan whose strata date to the Middle to Late Jurassic. It is an important locality for insect fossils that ...
; holotype: no. PIN 2452/3 at Palaeontological Institute Moscow; size: hindwing 39.0 mm; originally described in the genus ''Tarsophlebia'')
**''Turanophlebia? sibirica'' Pritykina, 1977 - (type locality: Baissa, Vitim River, Buryat Republik, Siberia / Transbaikalia, Russia; type horizon: Lower Cretaceous, Neocomian-Berriasian / 145-140 mya or Barremian-Aptian / 125 mya, Zaza Formation
The Zaza Formation is a geological formation located in Buryatia (Russia). It dates to the Lower Cretaceous period. It is Aptian in age and consists of Sandstone, sandstones, Siltstone, siltstones, Marl, marls and bituminous Shale, shales, deposi ...
; holotype: no. PIN 1989/1258 at Palaeontological Institute Moscow; estimated size: hindwing 46.9, based on a comparison of the distance between wing base and end of MP, which is 24.7 mm in ''T. sibirica'' and 21.6 mm in ''T. martynovi'' that has a total hindwing length of 41.0 mm)
**''Turanophlebia sinica'' Huang & Nel, 2009 - (type locality: Western Liaoning, PR China; type horizon: Lower Cretaceous, Barremian-Aptian / 125-121 mya, Yixian Formation
The Yixian Formation (; formerly transcribed as Yihsien Formation) is a geological formation in Jinzhou, Liaoning, People's Republic of China, that spans the late Barremian and early Aptian stages of the Early Cretaceous. It is known for its ex ...
; holotype: no. NIGP 148201 at Nanjing Institute of Geology and Palaeontology; size: forewing 49.5 and hindwing 45.5 mm)
**''Turanophlebia vitimensis'' Fleck et al., 2004[ - (type locality: right side of Vitim River downstream Romanovka village, Eravna district, Buryat Republic, Siberia / Transaikalia, Russia; type horizon: Lower Cretaceous, Neocoman / Berriasian / 145-120mya or Barremian-Aptian / 125 mya, ]Zaza Formation
The Zaza Formation is a geological formation located in Buryatia (Russia). It dates to the Lower Cretaceous period. It is Aptian in age and consists of Sandstone, sandstones, Siltstone, siltstones, Marl, marls and bituminous Shale, shales, deposi ...
; holotype: no. PIN 2361/1 at Palaeontological Institute Moscow; estimated size: hindwing 47.0 mm)
All other described taxa are synonyms of the type species ''Tarsophlebia eximia''.[
]
Phylogeny
The monophyly of Tarsophlebiidae is strongly supported by the following set of derived characters (autapomorphies
In phylogenetics, an autapomorphy is a distinctive feature, known as a derived trait, that is unique to a given taxon. That is, it is found only in one taxon, but not found in any others or outgroup taxa, not even those most closely related to t ...
):
hindwings with hypertrophied subdiscoidal cell that is developed as "pseudo discoidal cell"; fusion of veins MAb+MP+CuA for a considerable distance before separation of MP and CuA in hindwing; vein AA strongly bent at insertion of CuP-crossing; extremely acute distal angles of forewing discoidal and subdiscoidal cell. The body characters "distinctly prolonged legs, with very long tarsi" and "male cerci with paddle-like distal expansions" are known from one species of the genus ''Tarsophlebia'' (''T. eximia'') and ''Turanophlebia'' (''T. vitimensis'') respectively, and thus belonged to the common ground plan of all Tarsophlebiidae. The extremely prolonged female ovipositor could be a further synapomorphy for the family, but it is only known from ''T. eximia'' and from a single specimen of ''T. minor'' at the Solnhofen museum.[
Bechly (1996) and Nel et al. (2004: Appendix 2) proposed a long list of putative ]synapomorphies
In phylogenetics, an apomorphy (or derived trait) is a novel character or character state that has evolved from its ancestral form (or plesiomorphy). A synapomorphy is an apomorphy shared by two or more taxa and is therefore hypothesized to have ...
that demonstrate a closer relationship of Tarsophlebiidae with crown group Odonata:
presence of a costal triangle as broad and strong sclerotisation of the basal costal margin; the distal discoidal vein MAb (= distal side of discoidal cell) and the subdiscoidal vein (origin of the CuA on MP) are aligned and dorsally enforced by a strong sclerotisation, so that this structure appears to cross the vein MP and the concave fold along this vein (formation of a “discal brace” sensu Carle 1982); this discal brace is aligned with the arculus in the ground plan (only retained in some taxa with an open discoidal cell and in the forewings of Epiophlebia); the midfork (first fork of RP and base of IR2) is shifted basally, with the RP3/4 generally arising basal of the subnodus (reversed in some Coenagrionoidea) and RP2 arising close to the subnodus (in the ground plan); more derived type of nodus, with a kink in ScP; the oblique basal brace (still present in Protanisoptera and Protozygoptera) is transformed into a transverse “basal bracket” Ax0 which looks like a primary antenodal crossvein; presence of two strong primary antenodal crossveins Ax1 and Ax2 (also present in some Protozygoptera, e.g. specimen PIN 1/276 from the Upper Permian of Russia); pterostigma distinctly braced by an oblique postsubnodal crossvein beneath the basal margin of the pterostigma; presence of a tracheated lestine oblique vein 'O' between RP2 and IR2 (secondarily absent in some taxa); in the median space (= basal space) the convex vestige of the Media-stem (“vestigial CuA” sensu Fraser 1957) is suppressed since it is fused with the cubital stem to a common medio-cubital-stem (the alleged presence of this vestige in the holotype of ''Tarsophlebiopsis'' is a teratology or an artefact of preservation), convergent to some Protanisoptera, Triadophlebiomorpha, and Protozygoptera.
Bechly (1996) proposed that several unique symplesiomorphic features of all Tarsophlebiidae indicate that this family represents the sister group of all Recent Odonata.[ These features are the basally open discoidal cell in the hindwing (instead of closed) which implies an incomplete arculus, the (meanwhile disputed) presence of four tarsomeres of equal length (instead of only three), and the very primitive condition of the male secondary genital apparatus (viz ligula orimentary; vesicula spermalis still very short and flat with a very wide porus) without any intromittent organ. Bechly therefore considered the similarities of Tarsophlebiidae and ]Epiprocta
Epiprocta is one of the two extant suborders of the Odonata (the order (biology), order to which dragonflies and damselflies belong). It was proposed relatively recently, having been created to accommodate the inclusion of the Anisozygoptera. The ...
mentioned by Nel et al. (1993), viz the less separated and relatively large eyes, the presence of two cephalic sutures, and the small leg spines (also present in Meganisoptera[), as symplesiomorphies.
However, based on a cladistic study of 14 characters Fleck et al. (2004) again suggested that Tarsophlebiidae might rather be the sister group of the clade Epiprocta that includes Epiophlebiidae and Anisoptera. Nevertheless, this result has a very low statistical support and might as well be an artefact of the parsimony computer algorithm, because none of the 14 characters represents an unambiguous synapomorphy for Tarsophlebiidae and Epiprocta.][
Huang & Nel (2009) presented convincing evidence from a new fossil Tarsophlebiidae from China that the number of tarsomeres is only three as in modern odonates, but that the first tarsomere is about twice as long as the others.][ Bechly (1996) already discussed this possibility and suggested that such a long basal tarsomere, compared to the short basal tarsomere in protodonates and all Recent odonates, could still be a plesiomorphic state that could have resulted by the fusion of two basal tarsomeres.][ Huang & Nel (2004) state that there is no evidence for such a fusion in the fossils and that the elongation of the first segment could as well be a derived feature (autapomorphy) of Tarsophlebiidae.
The two alternative phylogenetic positions of Tarsophlebiidae
Hypothesis of Fleck et al. (2004):
Hypothesis of Bechly (1996, 2007):
]
Biology
Next to nothing is known about the ecology and behavior of Tarsophlebiidae, but it probably was quite similar to Recent odonates. With their very long ovipositor the females probably inserted their eggs into mud in or close to water, similar to modern Cordulegastridae
The Cordulegastridae are a family of Odonata (dragonflies) from the suborder Anisoptera. They are commonly known as spiketails. Some vernacular names for the species of this family are biddie and flying adder. They have large, brown or black bodi ...
. It is remarkable that two other groups of Mesozoic odonates (viz Steleopteridae and Aeschnidiidae) had a similarly elongated ovipositor.
Geographical and geological distribution
The fossil record of this family ranges from Upper Jurassic
The Late Jurassic is the third epoch of the Jurassic Period, and it spans the geologic time from 163.5 ± 1.0 to 145.0 ± 0.8 million years ago (Ma), which is preserved in Upper Jurassic strata.Owen 1987.
In European lithostratigraphy, the name ...
of Kazakhstan and Germany to the Lower Cretaceous
Lower may refer to:
*Lower (surname)
*Lower Township, New Jersey
*Lower Receiver (firearms)
*Lower Wick
Lower Wick is a small hamlet located in the county of Gloucestershire, England. It is situated about five miles south west of Dursley, eight ...
of England, Transbaikalia, Mongolia and China. There are no records of Tarsophlebiidae from any fossil locality outside the Eurasiatic region.[
]
History
The first tarsophlebiid fossils were specimens of ''Tarsophlebia eximia'' from the Upper Jurassic Solnhofen Plattenkalk of Germany described as "''Heterophlebia eximia''" and ''Euphaea longiventris'' by Hagen (1862).[ Larger revisions of this family have been provided by Nel et al. (1993) and Fleck et al. (2004).][
]
Notable specimens
Beside the important type specimens there are also several exceptionally well preserved fossils that contribute to our knowledge of the morphology of Tarsophlebiidae.[ These include the following specimens:][
*female specimen no. SOS 3609 (''Tarsophlebia eximia'') at the Jura-Museum Eichstätt shows the hypertrophied ovipositor
*female specimen without collection number (''Tarsophlebia minor'') at the Bürgermeister Müller Museum in Solnhofen (BMMS), shows the hypertrophied ovipositor (see photo)
*male specimen no. SOS 1720 (''Tarsophlebia eximia'') at the Jura-Museum Eichstätt is the only known specimen that shows under alcohol-cover the crucial structures of the secondary genital apparatus of Tarsophlebiidae
*male specimen no. AS-VI-44b (the holotype of ''Tarsophlebia eximia'') at BSPGM shows an apparent segmentation of the tarsus into four segments on the right hindleg
*specimen no. JME 1960/66K at the Jura-Museum Eichstätt shows an apparent segmentation of the tarsus into four segments on the left foreleg
*male specimen no. 6126 (''Tarsophlebia eximia'') at coll. Carpenter of MCZ shows a perfectly preserved head in dorsal view
*male specimen no. 6222 (''Tarsophlebia eximia'') at coll. Carpenter of MCZ shows well-preserved cerci
*male specimen PIN 2361/1 (holotype of ''Turanophlebia vitimensis'') shows very well-preserved cerci
*male specimen NIGP 148201 (holotype of ''Turanophlebia sinica'') has a well-preserved head and the best preserved legs of all known fossils of Tarsophlebiidae, which show the crucial segmentation of the tarsus. In the original description (Huang & Nel, 2009: Fig. 10) the visible suture between clypeus and labrum is erroneously labeled as "mandibles".][
*male specimen of ''Tarsophlebia eximia'' in private collection Spiegelberg (Heidelberg, Germany) shows perfectly preserved cerci (see photo)
]
References
Further reading
*
*
*
*
External links
Die Fossilien von Solnhofen
(photos of Solnhofen fossils of ''Tarsophlebia'')
Tree of Life Project
(Odonata page)
(by G. Bechly)
(by G. Bechly, 2007)
{{Taxonbar, from=Q1866033
Prehistoric odonates
Prehistoric arthropod families
Jurassic insects
Cretaceous insects
Taxa named by Anton Handlirsch
Late Jurassic first appearances
Early Cretaceous extinctions