Gladysvale Cave

Gladysvale is the first cave that Robert Broom visited in the Transvaal in his mid-1930s search for a hominid-bearing cave nearer to Johannesburg than Taung. He visited Gladysvale after a butterfly collector from the Transvaal Museum reported a "human mandible" in the wall of the cave. When Broom arrived at the cave the mandible was gone. Sterkfontein soon lured Broom away from the site. In 1946 Phillip Tobias led a student expedition to the site where a fine baboon fossil was recovered. In 1948 Frank Peabody of the Camp-Peabody expedition from the United States spent several weeks at Gladysvale but failed to find any hominid remains. The site was lost from scientific memory until it was re-opened by Lee Berger and Andre Keyser in 1991. Within a few weeks of excavation the first hominid remains were discovered – two teeth of Australopithecus africanus. This discovery made Gladysvale the first new early hominid site to be discovered in South Africa since 1948 (when the last site – Swartkrans – was discovered by Robert Broom). == Recovered fossils ==

Many thousands of fossils have been recovered from the Gladysvale deposits including rare remains of hominids. From the Gladysvale external deposits, almost a quarter of a million bones have been recovered since excavations began in 1992. There are many millions of bones still in place in the cave. Fossils recovered include antelope, giant zebra, carnivores including extinct wolves, monkeys and hominids attributed to Australopithecus africanus and early Homo. Tools have also been found with the most spectacular being an Acheulean handaxe (pictured), recovered from 1 million year old sediments. Geology Gladysvale has become well known for its exceptional horizontally-bedded stratigraphy and has been the site of the testing of many of the absolute dating techniques which have proved successful on the hard to date breccias of the South African fossil-bearing caves. The site is presently divided into three cave systems with the upper cave holding the Gladysvale Internal Deposits and an External Deposit (pictured in 3-D). Gladysvale was one of the first sites in Africa to be 3-D digitally mapped by Peter Schmid and students from the University of Zurich. Age of the deposits The Gladysvale sequence has been dated using a combination of biostratigraphy, palaeomagnetism (Andy Herries, La Trobe University, Australia), electron spin resonance and uranium series dating (Robyn Pickering, U. Melbourne, Australia). The youngest deposits are thought to be around 54,000 years old while the oldest deposits that are the likely source of the Au. africanus fossils are around 2.4–2.0 million years old. The Gladysvale External deposits contain extensive faunal remains and date to between 780,000 and 530,000 years ago. An Acheulian handaxe was recovered from internal deposits older than the Bruhnes-Matuyama boundary at 780,000 years. == References ==