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Pakistan Stratigraphy
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Paleozoic • Cambrian In GSP lexicon

Kussak Formation

Early to early Middle Cambrian

Cambrian in the time scale →

Cited in 8 sources Last reviewed Aug 20, 2026

Unit summary
Rank
Not recorded
Status
Published
Age
Paleozoic · Cambrian · Series 2Early to early Middle Cambrian
Named by
Wynne (1878) 'Obolus/Siphonotreta beds'; Waagen & Wynne (1895) 'Neobolus beds'; Noetling (1894) 'Kussak group'; formalized as Kussak Formation, Fatmi (1973)
Type locality
Kussak Fort, eastern Salt Range
Thickness
50-100 m
Lithology
Glauconitic and micaceous sandstone, siltstone, dolomite interbeds
Synonyms
Neobolus Shales

A glauconitic, micaceous Cambrian sandstone and dolomite unit deposited on tidal flats and a shallow shelf; it is rich in trilobites and burrows.

Named after Kussak Fort in eastern Salt Range. Contains thin lenses of fossil asphalt (gilsonite). Rich in trilobites including Redlichia noetlingi. Part of the Khewra Group.

Fossils

Contacts

In the Salt Range column
SandstoneLimestoneShale / mudFossils recordedUnconformityConformable

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type (wavy = unconformity inferred from a missing period). True scale makes height ∝ recorded thickness; hatched = thickness not recorded. Ages approximate, for ordering.

This unit (highlighted) within its province column; faded ends continue above and below. Line style marks the contact type.

Distribution & setting

Basin
Not recorded
Region
Not recorded
Depositional environment
tidal flat, shallow marine
Coordinates
Not recorded

Correlation

Not recorded. Compare this unit against other basins on the correlation panel →

Economic significance

Not recorded

Remarks

A glauconitic, trilobite-bearing Cambrian unit whose intense and diverse bioturbation (Cruziana and Skolithos ichnofacies across intertidal to shallow-subtidal settings) records well-established tidal-flat ecosystems during the Cambrian 'agronomic revolution'.

Sources (9)

Reviewer confidence: high

Every fact on this page is source-cited. This entry is part of the peer-archived Pakistan Stratigraphy Dataset (doi.org/10.5281/zenodo.21363991, CC‑BY‑4.0).

Lexicon status: Name attested in the Shah (1977/2009) Geological Survey of Pakistan compilation — the national stratigraphic lexicon. This records where the name is documented; it is not an endorsement of the unit’s definition, age or figures.

Cite this unit
APA

Qudsi, L. (2026). Kussak Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@misc{stratigraphypk_kussakformation,
  author    = {Qudsi, Lareb},
  title     = {{Kussak Formation} --- Pakistan Stratigraphy Dataset},
  year      = {2026},
  publisher = {Zenodo},
  doi       = {10.5281/zenodo.21363991},
  url       = {https://doi.org/10.5281/zenodo.21363991}
}

Archived dataset: doi.org/10.5281/zenodo.21363991 (CC‑BY‑4.0) · Direct link to this entry: https://stratigraphy.pk/formation/kussak-formation (accessed August 30, 2026).

To cite the unit's original definition instead, see: Wynne (1878) 'Obolus/Siphonotreta beds'; Waagen & Wynne (1895) 'Neobolus beds'; Noetling (1894) 'Kussak group'; formalized as Kussak Formation, Fatmi (1973).

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