| Kabuh Formation | |
|---|---|
| Stratigraphic range: Zanclean–Chibanian ~ | |
|   | |
| Type | Geological formation | 
| Unit of | Kendeng Group | 
| Lithology | |
| Primary | Sandstone, mudstone | 
| Location | |
| Coordinates | 7°30′S110°00′E / 7.5°S 110.0°E | 
| Approximate paleocoordinates | 7°36′S110°24′E / 7.6°S 110.4°E | 
| Region | Java | 
| Country | Indonesia | 
The Kabuh Formation is a Plio-Pleistocene geologic formation from Central Java, consisting of several unnamed members belonging to the Kendeng Group. [1] Many of the fossils discovered from Sambungmacan belonging to this group were discovered in an accumulated sediment deposit in a flood-controlling canal near the Solo River, including a series of hominin crania that are similar in anatomy and geologically younger than the Ngandong hominins upstream. This area was excavated throughout the 1970s. [2] [3] [4] [5] [6]
| Genus | Species | Group | Material | Notes | 
|---|---|---|---|---|
| Calyptraea (Bicatillus) [1] | morbidum | Kendeng | ||
| Cerithium [1] | bioekense | |||
| Cerithidea (Cerithideopsilla) [1] | cf. microptera | |||
| cheribonensis | ||||
| jenkinsi | 
| Genus | Species | Location | Material | Notes | 
|---|---|---|---|---|
| Orlitia [1] | borneensis | Sambungmacan | Right first costal, isolate [7] | Geoemydid turtle | 
| Genus | Species | Location | Material | Notes | Images | 
|---|---|---|---|---|---|
| Homo [2] [3] [4] | erectus | Sambungmacan | A tibial shaft and three crania | Late-stage Indonesian hominins |   | 
| erectus newyorkensis [8] | Not accepted [9] | ||||
| Bovidae [5] [6] | indet. | A tooth | Discovered circa 1973 excavations |