Publication

Prendergast, M. E.; Rouby, H.; Punnwong, P.; Marchant, R.; Crowther, A.; Kourampas, N.; Shipton, C.; Walsh, M.; Lambeck, K.; Boivin, N. L.: Continental island formation and the archaeology of defaunation on Zanzibar, eastern Africa. PLoS One 11 (2) (2016)

Further Information


Dr. Nicole L. Boivin

School of Archaeology, Oxford University
nicole.boivin@rlaha.ox.ac.uk
Nicole Boivin is based at the University of Oxford. She also leads the Department of Archaeology at the Max Planck Institute for the Science of Human History.

Research is an outcome of the Sealinks Project, funded by the European Research Council. It was conducted in collaboration with the Zanzibar Research Committee, the Zanzibar Department of Museums and Antiquities (DAMA) and took place partly at the National Museums of Kenya.

Media contact

Petra Mader
Phone: +49 3641 686 960
mader@shh.mpg.de
presse@shh.mpg.de

Prehistoric loss of biodiversity

Scientists explore the role of climate change and ancient human activity in the disappearance of Zanzibar’s large fauna

 

February 22, 2016

New research by an international team has revealed that most of Zanzibar’s large fauna were extirpated after the island was reformed by rising sea levels at the end of the last ice age. The study involved a multidisciplinary team of archaeologists, geographers and ecological scientists, and analysed animal remains from a cave site on Zanzibar. The scientists also drew on field data and simulation models to offer a timeline for the formation of Zanzibar as an island.

Archaeological excavation underway at Kuumbi Cave, Zanzibar Zoom Image
Archaeological excavation underway at Kuumbi Cave, Zanzibar

The senior author of the new study is University of Oxford archaeologist Nicole Boivin, who is also the newly appointed director at the Max Planck Institute for the Science of Human History, in Jena, Germany. The study is an outcome of the European Research Council-funded Sealinks Project.

The study provides new insight into processes of extirpation and extinction that followed prehistoric human colonisation of islands globally. "While more work is needed to untangle the human and natural contributions to faunal extirpations on Zanzibar, this is an important step toward better understanding of the ways that humans have shaped the natural world over the long term," says Dr. Boivin.

The researchers from the UK, Spain, France, Kenya, Thailand and Australia compared archaeological data on the history of Zanzibar’s fauna with geographical data obtained by looking at mangrove sediments and simulating sea level rise. The faunal remains were all excavated from Kuumbi Cave, a famous archaeological site that not only documents wildlife changes but also human activities over the long term.

The study covers five periods of time – two stages of the late last Ice Age when Zanzibar was still part of the African mainland, the time of rapid sea level rising as the world subsequently warmed, and the Middle and Late Iron Age after Zanzibar had become an island. During the two latest stages, farmers and herders arrived on the island and brought further changes. The researchers were able to show that over this period, numerous large mammals such as zebra, buffalo, waterbuck and gazelle disappeared from the cave’s faunal record. Cut marks on some bones show that these were hunted by humans, though more work is needed to understand the exact role humans played in their disappearance.

The lead author of the study, Dr. Mary Prendergast from St. Louis University in Madrid observes that "This is a unique case study for understanding land-bridge island formation and human occupation and their long-term effects on animal communities. Such broad perspectives on island formation and defaunation provide insights that can help with efforts to conserve island biodiversity today."

 
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