Rock hyraxes, known in southern Africa more often as “dassies”, are furry, thickset creatures with short legs and no discernible tails. They spend much of their time sunning themselves on rocky outcrops.
Another thing they sometimes do is drag their butts along the ground. Dog owners know that this behaviour can be a sign of parasitic infections; in hyraxes the reason seems to be less clear, but this action leaves distinctive traces in sandy areas.
Traces and tracks – ancient, fossilised ones – are what we study at the African Centre for Coastal Palaeoscience through the Cape south coast ichnology project. Over the past few decades, we have found almost 400 vertebrate tracksites on this coast, some as old as 400,000 years, in cemented dunes known as aeolianites from the Pleistocene epoch. This epoch lasted from about 2.58 million years ago to about 11,700 years ago.
We’re building up a picture of the environment during that period and how the animals and plants of that time lived.
Among our latest finds are two fossilised traces that appear to have been made by rock hyraxes long ago. One is a tracksite and the other is a butt-drag impression with what may be a fossilised dropping in it.
The probable tracksite was brought to our attention from a site near Walker Bay on the Cape south coast by an ardent tracker, Mike Fabricius. It is around 76,000 years old. We found the probable butt-drag impression east of Still Bay on the same coast, and it is most likely around 126,000 years old.
The butt-drag impression is the first fossil of its kind to be described from anywhere in the world. In addition, these are the only possible fossilised hyrax tracks ever to be identified. In the world of palaeontology, anything this unusual is important and we feel privileged to be able to interpret them.
Interpreting the drag mark
Dating on our sites has been done through a technique known as optically stimulated luminescence, which works by analysing when materials like sand were last exposed to light.
The butt-drag impression is 95cm long and 13cm wide. It contains five parallel striations. Its outer margins are slightly raised, and within it there is a 2cm-high raised feature, 10cm by 9cm. Clearly something was dragged across the surface when it consisted of loose sand.
We considered possible causes other than hyrax buttocks. These included a leopard or an ancestral human dragging prey, or perhaps an elephant dragging its trunk. Firstly, however, these would be expected to leave tracks, and secondly in such interpretations the raised feature could not be explained.
But if it was a hyrax, it would make sense, because the buttock trace would have come after the tracks and wiped them out. And the raised feature might be a coprolite: a fused fossilised mass of hyrax droppings.
Old dung and urine
Rock hyraxes leave much more than just tracks and butt-drag traces. Because they prefer rocky areas, their tracks are not often found, but they polish rock surfaces to a shiny finish. This is similar to what buffalo on the North American prairie do, creating “buffalo rubbing stones”.
Hyraxes also leave deposits of urine and dung. Urea and electrolytes are concentrated in their urine, and they excrete large amounts of calcium carbonate. This becomes cemented and forms extensive whitish deposits on rock surfaces. Due to their communal habits, hyraxes often urinate in the same preferred localities over multiple generations.
Their urine and dung often mix to form a substance known as hyraceum – a rock-like mass that can accumulate into extensive, dark, tarry deposits. Hyraceum has been used as a traditional medication to treat a variety of ailments, including epilepsy, and for gynaecological purposes.
Hyraceum may be tens of thousands of years old, and can be regarded as a threatened, non-renewable resource. The middens, being sensitive to environmental changes and containing fossil pollen and other evidence of ancient life, form valuable natural archives for interpreting past climates, vegetation and ecology.
Thinking of hyraceum as a trace fossil, something which apparently has not been done before, can help in the protection of this underappreciated resource.
Although fossilised urine is globally uncommon, there is a word to describe it: “urolite”, to distinguish it from “coprolite” (fossilised poop). It seems that hyraxes contribute the lion’s share of the world’s urolite. At palaeontology conferences, students can be seen sporting T-shirts that brazenly state: “coprolite happens”. In southern Africa, a more appropriate term might be “urolite happens”.
Through appreciating the importance of butt-drag impressions, urolites, coprolites and hyraceum, and learning about the environment of rock hyraxes and other animals during the Pleistocene, we will never view these endearing creatures in the same light again.
Mathilde Stuart contributed to this research.
Lynne Quick receives funding from the National Research Foundation of South Africa African Origins Platform (grant no: 136507)
Charles Helm does not work for, consult, own shares in or receive funding from any company or organisation that would benefit from this article, and has disclosed no relevant affiliations beyond their academic appointment.
