Haasgat
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Haasgat is a fossiliferous South African paleocave located in the Cradle of Humankind
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Area, northeast of the
hominin The Hominini form a taxonomic tribe of the subfamily Homininae ("hominines"). Hominini includes the extant genera ''Homo'' (humans) and '' Pan'' (chimpanzees and bonobos) and in standard usage excludes the genus ''Gorilla'' (gorillas). The ...
-bearing sites of Sterkfontein and
Swartkrans Swartkrans is a fossil-bearing cave designated as a South African National Heritage Site, located about from Johannesburg. It is located in the Cradle of Humankind World Heritage Site and is notable for being extremely rich in archaeological ma ...
and approx. north-northwest of the City of
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. It is located on private land and is not accessible by the public. The cave system formed on the western slope of a narrow, north-south valley excised by a southeastern tributary of the Witwatersrandspruit River. As is the case with many of the dolomitic paleocaves in the region, the system was extensively mined for lime during the early 20th century. Although this mining obliterated the original cave entrance and parts of the system, the miners largely followed the original contours of the system. As a result, Haasgat is somewhat unusual in maintaining both the original roof and parietal contours, as well as remnant fossiliferous bands of calcified sediments throughout the ~100m long tunnel that comprises the modern cave.


History of investigations

While Haasgat was long known to residents of the Kalkheuvel West region (who named the cave Haasgat 'Afrikaans: hare hole''after a resident red rock hare), the system was first mapped during a survey of regional caves by Martini and Keyser in 1987. The extensive ''
ex situ Svalbard GLOBAL SEED BANK, an ''ex situ'' conservation. ''Ex situ'' conservation literally means, "off-site conservation". It is the process of protecting an endangered species, variety or breed, of plant or animal outside its natural habitat; ...
'' calificied sediment miner's dumps at Haasgat were sampled by Andre Keyser in the late 1980s, yielding a fossil assemblage that was partially described in a series of publications. The site was abandoned after this single phase of sampling and data from the site has rarely been incorporated into studies of South African Plio-Pleistocene fossil record. Since 2010, an international interdisciplinary team has initiated a new phase of ''ex situ ''and ''
in situ ''In situ'' (; often not italicized in English) is a Latin phrase that translates literally to "on site" or "in position." It can mean "locally", "on site", "on the premises", or "in place" to describe where an event takes place and is used in ...
'' excavation, geological sampling, and faunal analysis.Adams, 2011; Kegley et al., 2011; } Currently, this research program integrates researchers from the
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(South Africa; Stephany Potze, Lazarus Kgasi),
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(Australia; Justin W. Adams),
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(Australia; Andy I.R. Herries), Grand Valley State University (USA; Anthony D.T. Kegley),
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(Australia; Robyn Pickering), and the School of Anatomical Sciences at the
University of the Witwatersrand The University of the Witwatersrand, Johannesburg (), is a multi-campus South African public research university situated in the northern areas of central Johannesburg. It is more commonly known as Wits University or Wits ( or ). The university ...
(South Africa; Jason Hemingway).


Geology and age of deposits

Original interpretations of the formation of the Haasgat cave system (speleogenesis) emphasised development along a typical low-topographic relief pattern, where progressive erosion and deepening of the valley into the surface dolomites drained the phreatic cave, allowing for internal collapse and expansion of the system. Simultaneously, Keyser and Martini also suggested that the elevation of the system (near 1500m) and erosional deroofing prior to mining might indicate that the fossil deposits at Haasgat might have formed as early as the terminal Pliocene. Subsequent biostratigraphic interpretations of the fauna processed from the ''ex situ ''dumpsites produced two different proposed age ranges. An evaluation of the extinct baboon (''Papio'' ''angusticeps)'' sample, a species currently only known across African Pleistocene deposits in the Kromdraai A assemblage, were taken to suggest that the Haasgat fossils were roughly contemporaneous (~1.9-1.8 million years ago). In contrast, a description of the non-primate faunas from the ''ex situ ''dumpsite emphasised the largely modern ungulate sample and suggested a more recent depositional age of maximally 1.5 – 0.5 million years ago. The recent analysis by of all the ''ex-situ'' fauna from the cave suggests an age later than the first occurrence of ''Equus'' in Africa at ~2.3 Ma and an age prior to ~1.8 Ma also undertook a palaeomagnetic analysis of the cave deposits, indicating that the main ''in-situ'' fossil beds were older than the end of the Olduvai SubChron at 1.95 Ma and younger than the Gauss-Matuyama Boundary at 2.58 Ma. This suggests an age between 2.3 and 1.95 Ma for the majority of fossils from the site.


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External links


SpeleomagnetismResearch Protocol: Haasgat Fossil Site
{{Greater Johannesburg, natural Caves of South Africa Paleoanthropological sites Archaeological sites of Southern Africa Archaeological history of Southern Africa