Monday, 2 June 2014

Dating the Haasgat Cave Deposits.

The Malmani Dolomite to the west of Johannesburg and Pretoria is host to a large number of cave systems that have formed from about 5.3 million years ago onwards. These caves are noted for a large volume of fossiliferous material, including many Hominin (species more closely related to modern Humans than to modern Chimpanzees) fossils considered to be of great palaeoanthropolgical significance. However dating these deposits can be extremely difficult, due to extensive kartsification in the area. 

Karstification is a form of erosion affecting exposed limestones, whereby water dissolution creates caves in the limestone, which then are filled in by eroded material (either from elsewhere or by collapse of the cave system, and frequently by a combination of the two), with new caves then forming which often partially overlap with previous caves. Over time non-limestone material (e.g. sandstone or siltstone layers) within the deposits are both concentrated and broken up to form breccias, while the limestone disappears, making accurate reconstruction of the original deposits extremely difficult.

The Haasgat Cave is located within the Monte Christo Formation in the Schurveberg Mountain Range, about 20 km to the northeast of the well-documented Sterkfontein, Swartkrans and Kromdraai cave systems. It was extensively worked by limestone miners in the early twentieth century, and recognised as a site of palaeontological importance in the 1980s, having produced a large number of Primate and hooved Mammal remains. The mining was carried out by artisanal miners looking for limestone for local building works. A large volume of flowstone, stalagmites and stalactites were removed, but left the original structure of the cave (floors, walls, ceilings) intact.

In a paper published in the South African Journal of Science on 27 March 2014, a team of scientists led by Andy Herries of the Australian Archaeomagnetism Laboratory of the Department of Archaeology, Environment and Community Planning at La Trobe University attempt to date the Haasgat Cave Deposits using a combination of biostratigraphic and palaeomagnetic methods.

The location of Haasgat within the Cradle of Humankind World Heritage site and its relation to other fossil sites mentioned in the text. Sites with larger font are Hominin-bearing sites (except Haasgat) and those with smaller font are vertebrate fossil sites. Herries et al. (2014).

Biostratigraphy uses fossils from sites with known dates to extrapolate similar dates for sites with similar fossils. This most commonly uses abundant microscopic fossils such as pollen or marine plankton, but for recent deposits larger Mammal species can sometimes be utilized.

The Haasgat cave has produced remains of two Zebra species, Equus capensis and Equus cf. quagga. Since the oldest known specimens of any Equus species on the African continent are from the Omo Shungura deposits, where they can be dated to between 2.27 and 2.19 million years old by isotope dating of volcanic layers above and below the fossil bearing strata, this is taken as an oldest possible age for the Haasgat Cave Equus specimens.

The cave has also produced two Suid (Pig) skulls, which appear similar to Metridiochoerus andrewsi specimens from Gondolin, dated to between 1.95 and 1.78 million years old, and Metridiochoerus andrewsi and Phacochoerus specimens from Swartkrans, dated to between 2.25 and 1.80 million years old, but probably more than 1.96 million years old. They appear more derived than the Metridiochoerus specimens from the Makapansgat Limeworks, dated to between 2.85 and 2.58 million years old, but more primitive than the Metridiochoerus and Phacochoerus specimens from Cornelia-Uitzoek, dated to between 1.07 and 0.99 million years old.

The most abundant fossil at Haasgat Cave is the Klipspringer, Oreotragus sp., which forms 15.6% of the total assemblage and 38.0% of the Bovid fossils in the assemblage. These most closely resemble Oreotragus specimens from the Makapansgat Limeworks, dated to between 2.85 and 2.58 million years old than specimens from Gondolin dated to between 1.95 and 1.78 million years old.

Taken together Herries et al.  conclude that these fossils indicate an age of between 2.3 and 1.98 million years old for the Haasgat Cave deposits.

Major features of the Western Deposits of the Haasgat mine and its palaeocave deposits looking west from beneath the Bridge. Herries et al. (2014).

Palaeomagnetic dating relies on the fact that the Earth’s magnetic field undergoes periodic reversals to provide dates for strata. In deposits where iron rich minerals are able to settle slowly in liquids these will settle in alignment with the Earth’s magnetic field. Since this field reverses periodically, but irregularly, and these reversals have been mapped for many well dated deposits, these reversals can be used to date suitable deposits. 

Before this can be done it is necessary to establish that the deposits being studied do in fact contain iron minerals that have settled in a liquid medium. In order to do this Herries et al. carried out X-ray fluorescence microscopy at the Australian Synchrotron in Melbourne, which established that the majority of iron minerals occurred in discrete horizontal bands within flowstone from the Haasgat  Cave. This suggests that deposition was periodic, probably coinciding with warmer, more humid periods with increased erosion. The iron-rich layers also show raised arsenic levels and are strontium poor, suggesting they are formed by the deposition of minerals released by dissolution of the dolomite.

Synchrotron X-ray fluorescence microscopy data showing the negative correlation between iron (Fe) and strontium (Sr) in a flowstone at Haasgat. The Fe distribution (lighter in the figure) is dominated by the layering of the calcite in the flowstone and is likely detrital from flooding events between flowstone formation. However, it appears that some Fe also occurs along crystal growth boundaries between these laminated layers and may have been introduced into the flowstone during calcite formation. Areas of higher strontium are lighter. Herries et al. (2014).

The majority of the sampled flowstone in the Haasgat Cave appears to have been laid down in an extended period of reversed magnetic polarity, with the last of the material in a period of normal polarity. The reversed polarity material has a declination of 176–216° and inclinations between +50° and +64°, suggesting that the deposits have not moved greatly since they were formed (all rocks are laid down on the surface of a sphere, which palaeomagnitists try to orientate to a bar magnet running between the Earth’s poles; over time these rocks can be moved by uplift or subsidence, or the movement of the continents, making this task harder).

Based the fossil evidence and the extended period of magnetic reversal seen in the flowstone deposits, Herries et al. conclude that the Hassgat Cave deposits were laid down during the late Early Matuyama Chron (2.58-1.95 million years ago). During the Matayuma Chron the Earth had an extended period of reversed polarity, with several shorter periods of normal polarity (subchrons) towards the end of the early part of the chron. These were the RĂ©union at 2.21-2.14 million years ago, the Huckleberry Ridge at 2.05-2.02 million years ago, the Pre-Olduvai at about 1.98 million years ago, and the Olduvai at about 1.95-1.78 million years ago, which was followed by the Late Matuyama Chron (reversed polarity) from 1.78 million years ago onwards. The extent of the normal polarity at the top of the sample suggests that this was probably an extended period of normality, ruling out the pre-Olduvai event, and making the RĂ©union and Huckleberry Ridge less likely, while the fossils point towards the end of this time-gap, leading Herries et al. to conclude that the shift in polarity seen in the rocks represents the end of the Early Matuyama Chron and beginning of the Olduvai Subchron, giving a date of 1.95 million years for this event.

The age of Haasgat on the geomagnetic polarity timescale compared with other Hominin and Vertebrate fossil bearing sites. Herries et al. (2014).

See also…

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 A new species of Fox from the Pleisticene of Gauteng Province, South Africa.

Foxes (Vulpini) are a subgroup of the Dog Family, Canidae, found in North America, Eurasia and Africa (South American Foxes are a separate group, more closely related to True Dogs than to other...


 The diet of the Langebaanweg Hyaenids.

Modern Hyenas are among the most highly specialized durophagous (adapted to eating tough food) Mammals ever to live, with powerfully constructed teeth and jaws and enlarged masticatory...



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