What Happened to the Giant ‘Kings of Apes’ That Once Roamed Southern China?

Artist’s impression of a group of G. blacki.
Artist’s impression of a group of Gigantopithecus blacki in a forest in southern China. (Image: Garcia/Joannes-Boyau (Southern Cross University))

Giant creatures are usually associated with dinosaurs, woolly mammoths, or mystical beasts. But if you go back though the human lineage, you’ll find a very distant relative that stood three meters tall and weighed around 250 kilograms. This was Gigantopithecus blacki, the mightiest of all the apes and one of the biggest unresolved mysteries in paleontology.

Despite surviving for nearly 2 million years in what is now the Guangxi Zhuang Autonomous Region of southern China, the entire species of giant apes is represented in the fossil record only by a few thousand teeth and four jawbones. Nothing from the neck down.

Added to that is its mysterious disappearance from the fossil record at a time when other primates were flourishing. Where did these giant apes go and what brought them down?

Since 2015, a team of Chinese, Australian, and U.S. scientists has been chasing this mighty beast in the distinctive terrains of southern China. Our findings are published in Nature and reveal a story of seasonality, stress, and vulnerability.

A karst landscape panorama in southern China.
A karst landscape panorama in southern China. (Image: Renaud Joannes-Boyau)

Finding the window of extinction of the giant apes

Extensive exploration and excavations in hundreds of caves over a five-year period has been narrowed down into evidence from 22 caves in two regions of Guangxi: Chongzuo, near the Vietnamese border, and Bubing Basin, close to Nanning. Eleven of these caves contain evidence of G. blacki and the other 11 — of a similar age range — do not.

Our team applied several dating techniques to sediments from the caves: luminescence dating of feldspars (a common rock-forming mineral), electron spin resonance dating of quartz, and uranium series dating of stalagmites and similar deposits, as well as fossils. Altogether, we ended up with a staggering 157 radiometric ages.

Excavations of giant apes in Ma Feng Cave in Guangxi Zhuang Autonomous Region of southern China.
Excavations of giant apes in Ma Feng Cave in Guangxi Zhuang Autonomous Region of southern China. (Image: Kira Westaway)

We used these data sets to establish exactly when G. blacki dropped out of the fossil record, to define a “window of extinction.” This window allowed us to target a period of time to look closely at the environmental changes.

Next, we looked at eight sources of environmental and behavioral evidence, including ancient pollen grains, other animal bones, and micro details in the sediments.

The closest primate relative of G. blacki is the critically endangered orangutan. (Image: christels via Pixabay)

Furthermore, we gained a wealth of information from G. blacki teeth themselves — from isotopic signatures, trace elements, and the wear patterns on the surface of the teeth. This evidence can indicate diet, migration patterns, habitat preferences, diversity of food sources, and stress.

This data represents the largest collection of well-dated evidence for the giant apes and for the first time is supported by well-documented environmental and behavioral changes. It reveals the rise and fall of G. blacki in comparison to its closest primate relative — the orangutans.

Stronger seasons

Surprisingly, G. blacki went extinct between 295,000 and 215,000 years ago, much more recently than previously assumed. Before this time, G. blacki flourished in a rich and diverse forest.

But between 600,000 and 300,000 years ago, the environment became more variable. An increase in the strength of the seasons caused a change in the structure of the forest plant communities. By 200,000 years ago, the forests started to deteriorate.

Differences in trace elements such as barium, strontium, and calcium were mapped across the inside of G. blacki and orangutan teeth. At earlier sites, clear banding in both species’ teeth suggests diverse food sources and a flourishing population. Diffuse or no banding in later G. blacki suggests less varied food sources and chronic stress. The orangutan tooth suggests a less stressed population than G. blacki at this time. (Image: Yingqi Zhang et al. via Nature)

Despite being a close relative of G. blacki, orangutans could adapt their size, behavior, and habitat preferences to accommodate these forest changes. Their fossils display a flexible and balanced diet with very little stress during this period.

But G. blacki made the fatal mistake of relying on less nutritious backup food like twigs and bark when their favorite food sources, such as fruit-bearing plants, were unavailable. This meant the diversity of the giant apes’ food decreased, and their less mobile body size compared to the more agile orangutans restricted their geographic range for foraging.

Surprisingly, G. blacki also increased in body size over this period, contributing to food source problems and causing immense chronic stress to the species. This stress can be seen in the trace element mapping of their teeth, providing an insight into a species on the brink of extinction.

Pollen records from caves in the region showing the change in plant communities over time. (Image: Yingqi Zhang et al. via Nature)

Failure to adapt

As a direct consequence, G. blacki numbers dwindled as the species was placed under increasing environmental stress.

It would seem that by having such specific food and habitat preferences, G. blacki was vulnerable to environmental and habitat changes. Its size and food choice hampered its adaptation compared to more agile and mobile species like orangutans.

The story of G. blacki is a lesson in extinction — how some species are more equipped to survive change and others are more vulnerable. We must take this lesson on board with the looming threat of a sixth mass extinction event.

Trying to understand past extinctions is a good starting point to understand primate resilience. It may offer clues to the fate of other large animals, both in the past and in the future.

Kira Westaway, Associate Professor, School of Natural Sciences, Macquarie University; Marian Bailey, PhD Candidate, Geoarchaeology, Southern Cross University; Renaud Joannes-Boyau, Associate Professor, Southern Cross University; Simon Haberle, Professor, Australian National University, and Yingqi Zhang, Research professor in palaeontology, Chinese Academy of Sciences

This article is republished from The Conversation under a Creative Commons license. Read the original article.

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