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 |