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| Morphology | Ecology and taphonomy | External Literature Search | Age range and collections |
Panorpidium bimaculatum
Taxonomy
Panorpidium bimaculatum was named by Gorochov et al. (2006). Its type specimen is BMB 016391/-2, a tegmen, and it is a compression fossil. Its type locality is Rudgwick Brickworks, Upper Weald Clay, which is in a Barremian lagoonal/restricted shallow subtidal horizon in the Weald Clay Formation of the United Kingdom.
Synonymy list
| Year | Name and author |
|---|---|
| 2006 | Panorpidium bimaculatum Gorochov et al. p. 645 fig. 7 |
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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.
†Panorpidium bimaculatum Gorochov et al. 2006
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
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| Source: subo = suborder | |||||
| Reference: Tillyard 1921 | |||||
Age range: base of the Late/Upper Hauterivian to the top of the Early/Lower Barremian or 136.40000 to 125.45000 Ma
Collections (4 total)
| Time interval | Ma | Country or state | Original ID and collection number |
|---|---|---|---|
| Late/Upper Hauterivian | United Kingdom (England) | Panorpidium bimaculatum (106281) | |
| Early/Lower Barremian | United Kingdom (England) | Panorpidium bimaculatum (45193 type locality: 104005 118921) |