2007
DOI: 10.11646/zootaxa.1660.1.4
|View full text |Cite
|
Sign up to set email alerts
|

A new Middle Triassic genus and species of Mylacridae (Blattodea) from China

Abstract: Shaanxi Entomofauna is important in the study of insect’s evolution from Paleozoic to Mesozoic. A new genus and species, Cathayiblatta longata gen. et sp. nov., of Mylacridae (Blattodea) from Middle Triassic is described. The new genus and species was found in Tongchuan City, Shaanxi Province of China, and the fossil referred to a new member of Tongchuan Entomassemblage of Shaanxi Entomofauna. The ultrastructure of wing was observed through scanning electron microscope. Comparison was made between the new genu… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
2
1

Citation Types

0
7
0

Year Published

2015
2015
2024
2024

Publication Types

Select...
4

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(7 citation statements)
references
References 0 publications
0
7
0
Order By: Relevance
“…The upper part is composed of greyish green or red fine sandstone and siltstone, interbedded with greyish green or black shale with black oil-shale at the top. The Tongchuan Formation yields bivalves, spinicaudatans, ostracods, insects, tadpole shrimps, fish, reptiles, sporopollen and plants (IGCAGS, 1980; Wu, Liu & Li, 2001; Hong, 2007, 2009; Li, Hong & Yang, 2007; Sun & Hong, 2011), and has a total thickness of c. 596 m. The layers bearing the insect fauna are considered to be Ladinian in age while the Tongchuan Formation is assigned an Anisian – early Carnian age in the present paper (see below).…”
Section: Geological Settingmentioning
confidence: 99%
See 4 more Smart Citations
“…The upper part is composed of greyish green or red fine sandstone and siltstone, interbedded with greyish green or black shale with black oil-shale at the top. The Tongchuan Formation yields bivalves, spinicaudatans, ostracods, insects, tadpole shrimps, fish, reptiles, sporopollen and plants (IGCAGS, 1980; Wu, Liu & Li, 2001; Hong, 2007, 2009; Li, Hong & Yang, 2007; Sun & Hong, 2011), and has a total thickness of c. 596 m. The layers bearing the insect fauna are considered to be Ladinian in age while the Tongchuan Formation is assigned an Anisian – early Carnian age in the present paper (see below).…”
Section: Geological Settingmentioning
confidence: 99%
“…The Tongchuan Formation was established in the Qishuihe outcrop of Shaanxi Province, northwestern China, by IGCAGS (1980), yielding abundant fossils. The age of the Tongchuan Formation was traditionally considered to be either Middle Triassic or Middle–Late Triassic (IGCAGS, 1980; Wu, Liu & Li, 2001; Hong, 2007, 2009; Li, Hong & Yang, 2007; Sun & Hong, 2011). In this formation, both the bivalve and plant assemblages indicate a Middle Triassic age, and the sporopollen assemblage resembles that in the underlying Lower–Middle Triassic Ermaying Formation (IGCAGS, 1980).…”
Section: Stratigraphic Implicationsmentioning
confidence: 99%
See 3 more Smart Citations