The Langeberg Quartzose Sand Member has not been directly dated as yet, although attempts are currently underway to get a direct date from this horizon. The Langebaanweg Suidae enable us to infer a relative date however, as the abundance of
Nyanzachoerus australis in the Langeberg Quartzose Sand Member and its presence in eastern Africa at 5.2 million years ago establishes this as the relative age for the Langeberg Quartzose Sand Member.
Nyanzachoerus australis is therefore important for the
Biochronology:
Biochronology is the dating of biological events using biostratigraphic or palaeontological methods.
of the Langeberg Quartzose Sand Member (see
'How old is it anyway?' for more information on how animals may be used to work out the age of deposits which cannot be directly dated).
Acknowledgements: Our thanks to Dr Yohannes Haile-Selassie for supplying the above information.