Basic info | Taxonomic history | Classification | Included Taxa |
Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Kalotermes disruptus
Taxonomy
Sisyra disrupta was named by Cockerell (1917). Its type specimen is NHML I.8644, a wing (apical fragment), and it is a compression fossil. Its type locality is Bembridge Marls (Brodie coll), which is in a Priabonian lagoonal/restricted shallow subtidal lime mudstone in the Bouldnor Formation of the United Kingdom.
It was recombined as Kalotermes disruptus by Jarzembowski (1980), Nel and Paicheler (1993), Krishna et al. (2013).
It was recombined as Kalotermes disruptus by Jarzembowski (1980), Nel and Paicheler (1993), Krishna et al. (2013).
Synonymy list
Year | Name and author |
---|---|
1917 | Sisyra disrupta Cockerell p. 381 figs. pl. 31, fig.13 |
1980 | Kalotermes disruptus Jarzembowski p. 249 figs. 8-13 16-19 |
1993 | Kalotermes disruptus Nel and Paicheler p. 120 |
2013 | Kalotermes disruptus Krishna et al. p. 509 |
Is something missing? Join the Paleobiology Database and enter the data
|
|
If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Kalotermes disruptus Cockerell 1917
show all | hide all
Diagnosis
No diagnoses are available
Measurements
No measurements are available
|
|
||||
|
|||||
|
|
||||
Source: c = class, p = phylum | |||||
References: Kiessling 2004, Bush and Bambach 2015 |
Age range: Priabonian or 37.71000 to 33.90000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Priabonian | United Kingdom (England) | Sisyra disrupta (type locality: 123959) |