Kabuh Formation

Geologic formation from Central Java From Wikipedia, the free encyclopedia

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]

Unit ofKendeng Group
Coordinates7.5°S 110.0°E / -7.5; 110.0
Quick facts Type, Unit of ...
Kabuh Formation
Stratigraphic range: ZancleanChibanian
~5.333–0.126 Ma
TypeGeological formation
Unit ofKendeng Group
Lithology
PrimarySandstone, mudstone
Location
Coordinates7.5°S 110.0°E / -7.5; 110.0
Approximate paleocoordinates7.6°S 110.4°E / -7.6; 110.4
RegionJava
CountryIndonesia
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Fauna

Gastropoda

More information Genus, Species ...
Genus Species Group Material Notes
Calyptraea (Bicatillus)[1] morbidum Kendeng
Cerithium[1] bioekense
Cerithidea (Cerithideopsilla)[1] cf. microptera
cheribonensis
jenkinsi
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Reptilia

More information Genus, Species ...
Genus Species Location Material Notes
Orlitia[1] borneensis Sambungmacan Right first costal, isolate[7] Geoemydid turtle
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Mammalia

More information Genus, Species ...
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
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References

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