Aeschnidiidae

Last updated

Aeschnidiidae
Temporal range: Jurassic to Late Cretaceous, 156–66  Ma
Unidentified Aeschnidiidae fossils Jurassic .jpg
Fossil of Urogomphus sp. or Aeschnidium sp. (Aeschnidiidae), from the Upper Jurassic Solnhofen Plattenkalk of Germany
Scientific classification
Kingdom:
Phylum:
Class:
Order:
Infraorder:
Family:
Aeschnidiidae
Handlirsch, 1906
Type species
Aeschnidium bubas
Westwood, 1856
Genera

See text

Aeschnidiidae is an extinct family of Anisopteran dragonfly. Aeschnidiids were widespread and could be found on nearly every continent on Earth. They were most diverse during the Early Cretaceous before completely disappearing at the end of the Maastrichtian. Many members of this family were large dragonflies, with wing lengths ranging from 35 to 45 mm. [1]

Genera

Genera of Aeschnidiid dragonfly
Generic nameGeographical locationAge
Aegyptidium [2] Abu Ballas Formation, Egypt 122-112 Ma, Early Cretaceous
Aeschnidiella [2] Ulyanovsk Oblast, Russia 125-113 Ma, Early Cretaceous
Aeschnidiopsis [2] Walumbilla Formation, Australia 125-113 Ma, Early Cretaceous
Aeschnidium [2] Lulworth Formation, England 145-140 Ma, Early Cretaceous
Angloaeschnidium [2] La Huérguina Formation, Spain, and the Weald Clay Formation, England130-125 Ma, Early Cretaceous
Bergeriaeschnidia [2] Solnhofen Limestone, Germany 151-145 Ma, Late Jurassic
Brunetaeschnidium [2] Nusplingen Limestone, Germany and the Solnhofen Limestone, Germany156-145 Ma, Late Jurassic
Brunneaeschnidia [3] Chijinbao Formation, China 125-113 Ma, Early Cretaceous
Cooperaeschnidium [2] Weald Clay Formation, England130-125.45 Ma, Early Cretaceous
Coramaeschnidium [2] Weald Clay Formation, England136.4-130 Ma, Early Cretaceous
Cratoaeschnidium [4] Crato Formation, Brazil 115-113 Ma, Early Cretaceous
Dakotaeschnidium [5] Fox Hills Formation, The United States of America 70.6-66 Ma, Late Cretaceous
Deiciosaeschidium [2] Purbeck-Lulworth Formation, England145-140 Ma, Early Cretaceous
Diastatopaeschnidium [2] Purbeck-Lulworth Formation, England145-140 Ma, Early Cretaceous
Dracontaeschnidium [2] Yixian Formation, China125-122 Ma, Early Cretaceous
Gansuaeschnidia [6] Chijinbao Formation, China125-113 Ma, Early Cretaceous
Gigantoaeschnidium [2] La Huérguina Formation, Spain130-125 Ma, Early Cretaceous
Iberoaeschnidium [2] La Huérguina Formation, Spain130-125 Ma, Early Cretaceous
Jarzembowskiaeschnidium [2] Purbeck-Lulworth Formation, England145-140 Ma, Early Cretaceous
Kesseleraeschnidium [2] Weald Clay Formation, England136-130 Ma, Early Cretaceous
Kimmeridgebrachpteraeschnidium [2] Kimmeridge Clay Formation, England156-151 Ma, Jurassic
Leptaeschnidium [2] Zaza Formation, Russia125-113 Ma, Early Cretaceous
Linaeschnidium [1] Yixian Formation, China125-122 Ma, Early Cretaceous
Lithoaeschnidium [2] Solnhofen Limestone, Germany151-145 Ma, Late Jurassic
Lleidoaeschnidium [2] La Pedrera de Rubies Formation, Spain and the Weald Clay Formation, England130-125 Ma, Early Cretaceous
Malmaeschnidium [2] Solnhofen Limestone, Germany151-145 Ma, Late Jurassic
Misofaeschnidium [2] Nusplingen Limestone, Germany and the Solnhofen Limestone, Germany156-145 Ma, Late Jurassic
Nannoaeschnidium [2] La Huérguina Formation, Spain130-125 Ma, Early Cretaceous
Rossaeschnidium [2] Weald Clay Formation, England130-125 Ma, Early Cretaceous
Santanoptera [7] Crato Formation, Brazil122-112 Ma, Early Cretaceous
Sinaeschnidia [2] Hangjiahu Formation, China, the Laiyang Formation, China, the Baiwan Formation, China, the Yixian Formation, China, the Shahai Formation, China, the Chijinbao Formation, China, and the La Huérguina Formation, Spain130-113 Ma, Early Cretaceous
Sinostenophlebia [8] Qingshila Formation, China129-125 Ma, Early Cretaceous
Solnhofenia [2] Solnhofen Limestone, Germany151-145 Ma, Late Jurassic
Stylaeschnidium [2] Yixian Formation, China125-122 Ma, Early Cretaceous
Tauropteryx [2] Crimea, Ukraine 99.6-93.5 Ma, Late Cretaceous
Urogomphus ? [2] Solnhofen Limestone, Germany and the Purbeck-Lulworth Formation, England151-140 Ma, Late Jurassic to Early Cretaceous
Wightonia [7] Crato Formation, Brazil122-112 Ma, Early Cretaceous
Spinofaarus rexyjponetwothree [2] Baharian Formation, China125-122 Ma, Early Cretaceous

Related Research Articles

<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">Paleobiota of the Yixian Formation</span> Geological formation in China

The Yixian Formation is a geological formation in Jinzhou, Liaoning, People's Republic of China, that spans about 1.6 million years during the early Cretaceous period. It is known for its fossils, listed below.

<i>Epiophlebia</i> Genus of dragonflies

Epiophlebia is a genus of damsel-dragonfly native to the Indian subcontinent, East Asia, and Southeast Asia. It is the only living genus of Odonata to neither be a dragonfly nor a damselfly. It is the sole member of the family Epiophlebiidae, which is itself the sole living representative of the infraorder Epiophlebioptera.

<span class="mw-page-title-main">Cordulegastroidea</span> Superfamily of dragonflies

Cordulegastroidea is a superfamily of dragonflies that contains three families.

<span class="mw-page-title-main">Libelluloidea</span> Superfamily of dragonflies

Libelluloidea is a superfamily of dragonflies.

<span class="mw-page-title-main">Hemiphlebiidae</span> Family of damselflies

Hemiphlebiidae is a family of damselflies. It contains only one extant species, the ancient greenling, native to Southern Australia and Tasmania. The fossil record of the group extends back to the Late Jurassic, making them the oldest known crown group damselflies.

<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.

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

The Tarsophlebiidae is an extinct family of medium-sized fossil odonates from the Upper Jurassic and Lower Cretaceous period of Eurasia. They are either the most basal member of the damsel-dragonfly grade ("anisozygopteres") within the stem group of Anisoptera, 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 in females.

2018 in paleoentomology is a list of new fossil insect taxa that were described during the year 2018, as well as other significant discoveries and events related to paleoentomology that were scheduled to occur during the year.

2019 in paleoentomology is a list of new fossil insect taxa that were described during the year 2019, as well as other significant discoveries and events related to paleoentomology that were scheduled to occur during the year.

2017 in paleoentomology is a list of new fossil insect taxa that were described during the year 2017, as well as other significant discoveries and events related to paleoentomology that were scheduled to occur during the year.

2020 in paleoentomology is a list of new fossil insect taxa that were described during the year 2020, as well as other significant discoveries and events related to paleoentomology that were scheduled to occur during the year.

2015 in paleoentomology is a list of new fossil insect taxa that were described during the year 2016, as well as other significant discoveries and events related to paleoentomology that were scheduled to occur during the year.

2015 in paleoentomology is a list of new fossil insect taxa that were described during the year 2015, as well as other significant discoveries and events related to paleoentomology that were scheduled to occur during the year.

Burmese amber is fossil resin dating to the early Late Cretaceous Cenomanian age recovered from deposits in the Hukawng Valley of northern Myanmar. It is known for being one of the most diverse Cretaceous age amber paleobiotas, containing rich arthropod fossils, along with uncommon vertebrate fossils and even rare marine inclusions. A mostly complete list of all taxa described up to the end of 2023 can be found in Ross (2024).

This paleoentomology list records new fossil insect taxa that were to be described during the year 2021, as well as notes other significant paleoentomology discoveries and events which occurred during that year.

This paleoentomology list records new fossil insect taxa that are to be described during the year 2022, as well as notes other significant paleoentomology discoveries and events which occurred during that year.

This paleoentomology list records new fossil insect taxa that were described during the year 2014, as well as notes other significant paleoentomology discoveries and events which occurred during that year.

This list of 2023 in paleoentomology records new fossil insect taxa that are to be described during the year, as well as documents significant paleoentomology discoveries and events which occurred during that year.

This list of 2024 in paleoentomology records new fossil insect taxa that are to be described during the year, as well as documents significant paleoentomology discoveries and events which occurred during that year.

References

  1. 1 2 D. Y. Huang, A. Baudoin and A. Nel. 2009. A new aeschnidiid genus from the Early Cretaceous of China (Odonata: Anisoptera). Cretaceous Research 30:805-809
  2. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 G. Fleck and A. Nel. 2003. Revision of the Mesozoic family Aeschnidiidae (Odonata: Anisoptera). Zoologica 153:1-170
  3. A. Nel and X. Martínez-Delclòs. 1993. Essai de Révision des Aeschnidioidea (Insecta, Odonata, Anisoptera). Cahiers de Paléontologie 1993:7-99
  4. A. Nel, C. Jouault and G. C. Ribeiro. 2022. The third aeschnidiid dragonfly genus and species from the Lower Cretaceous Crato Formation (Odonata, Anisoptera). Historical Biology 35:865-869
  5. A. Nel. 2021. Maastrichtian representatives of the dragonfly family Aeschnidiidae question the entomofaunal turnover of the early Late Cretaceous. Palaeoentomology 4:209-212
  6. X. Zhang, A. Nel, and H. Wang, H. C. Zhang, D. R. Zheng. 2022. A new genus of aeschnidiid dragonfly (Odonata: Anisoptera) from the Lower Cretaceous of the Jiuquan Basin, NW China. Historical Biology 36:12-18
  7. 1 2 G. Bechly. 2007. Odonata: damselflies and dragonflies. In D. M. Martill, G. Bechly, R. F. Loveridge (eds.), The Crato Fossil Beds of Brazil: Window into an Ancient World
  8. D. R. Zheng, H. Wang, and E. A. Jarzembowski, B. Wang, S. C. Chang, H. C. Zhang. 2016. New data on Early Cretaceous odonatans (Stenophlebiidae, Aeschnidiidae) from northern China. Cretaceous Research 67:59-65