The temporal lobes of Homo erectus were proportionally smaller than in H. sapiens

The temporal lobes of Homo erectus were proportionally smaller than in H. sapiens

The CENIEH has contributed to a paleoneurological study published in the journal Quaternary International, on the brain of Homo erectus, which analyzes its temporal lobes and compares these with other species like H. ergaster and H. sapiens
temporal lobes erectus sapiens ergaster
Pearson at al.

Emiliano Bruner, a paleoneurologist at the Centro Nacional de Investigación sobre la Evolución Humana (CENIEH), has participated in a study published in the journal Quaternary International, on the anatomy of the temporal lobes in the brain of Homo erectus, which establishes that they were proportionally smaller than in modern humans.

In H. sapiens, the temporal lobes are relatively more highly developed than in other primates, although little is known about their anatomy in extinct human species, because they are housed in a very delicate region of the cranium known as the middle cranial fossa, which is often not conserved in fossil individuals.

An earlier study by the same team had shown that the size of the middle cranial fossa can be used to deduce the volume of the temporal lobes. In this new study, three anatomical diameters were analyzed in fossils of H. erectus and H. ergaster, and compared with the corresponding measurements for 51 modern humans. The results suggest that both fossil species had temporal lobes proportionally smaller than in humans today.

Moreover, “The Asiatic individuals, namely Homo erectus, had larger temporal lobes than in the African ones, Homo ergaster, although the scanty fossil record does not allow us to tell whether this is due to chance or a paleoneurological difference between the two species”, says Bruner.

As the temporal lobe is a brain region involved in the integration of many cognitive functions, such as memory, the emotions, hearing, social relations and language, any change in their sizes or proportions is of transcendent importance, as this could reveal variations in the development of their neurons or their connections, and therefore in the cognitive functions associated to this region of the cerebral cortex.

This study has been conducted by Alannah Pearson, a doctoral student of Emiliano Bruner at the Australian National University in Canberra (Australia), in collaboration with Professor David Polly, of Indiana University (USA).

 

Full bibliographic information

Pearson, A., Polly, P. D., & Bruner, E. (2020). Temporal lobe evolution in Javanese Homo erectus and African Homo ergaster: inferences from the cranial base. Quaternary International (0). doi: 10.1016/j.quaint.2020.07.048.

 

Press release from CENIEH


Historic logging site shows first human-caused bedrock erosion along an entire river

Historic logging site shows first human-caused bedrock erosion along an entire river

The author's 45-pound dog gives a sense of the size of the bedrock boulders being eroded from the side of the Teanaway River. The previous floodplain is just visible at the top of the frame. Credit: Sarah Schanz/Indiana University

Geologic time is supposed to be slow, and the most solid object should be bedrock. But new University of Washington research upends both concepts: Effects of logging show that human activity can significantly erode bedrock, causing geology to fast forward.

The study, published April 15 in the Proceedings of the National Academy of Sciences, focuses on the Teanaway River, a picturesque river in central Washington state.

"In the last century, we have more river incision in this area than expected. Something caused these rivers to start eroding a lot more," said lead author Sarah Schanz, a former UW doctoral student who is now a postdoctoral researcher at Indiana University. "We know the Teanaway River has eroded into bedrock before, naturally -- it has some terraces that are 1,800 years old. But this current cycle is anthropogenic, or human-driven."

Results show that practices related to logging caused bedrock incision of up to 2 meters (6 feet) along the riverbed. As much as a half of what had been a floodplain was transformed into a new terrace abutting the river.

"This is the first time that we've been able to pinpoint erosion into bedrock due to human action," Schanz said. "Most rivers are eroding at about a tenth of a millimeter per year. This is about 100 times that amount."

The discovery means this beautiful riverbank resulted from human action, not natural forces. It could change how geologists think about landscapes in other parts of the world, such as Taiwan, with its long history of intense human activity.

The study began 20 years ago when co-author Brian Collins, a UW senior lecturer in river geology, was curious why there was so much exposed bedrock in the Teanaway.

Collins also noticed unusual river terraces, the stepped structures along the river bank resulting from cycles of the river flooding and then running more quickly, cutting a new channel deeper into the sediment. He led a 2016 study that calculated short-term changes in the Teanaway's western fork and suggested logging may have caused the river to cut a new channel.

This site in a community forest offered good access for regular visits by the research team and undergraduate assistants to all three forks. By combining newspaper records, material from the UW Libraries Special Collections, Central Washington University and the local Kittitas County historical society, the researchers were able to piece together and confirm the full history.

This 1920 photo of the Teanaway River shows how logs traveled down the river to the mills and railway. Credit: Frederick Krueger Photographs 376/Central Washington University Archives

Before logging roads existed, companies built temporary "splash dams" high up on the slope with all the logs and then broke up the dam with tools or explosives. Released water helped send logs shooting down to the mills.

"It was such an event that schools closed, and newspaper records show it really well," Schanz said. "People who are still alive today, some of their earliest memories are of going to see it."

Key to the process is that loggers would clear away debris to give the logs a clear shot down the river. This removed barriers that held back sediment and cleared out much of the gravel from the riverbed. Such events, the authors believe, caused the erosion to change dramatically.

"If you have too much sediment, you're basically protecting the river from erosion. But if you have not enough sediment, as that sediment is moving along, it starts to hit the bedrock and erode it," Schanz said.

David Montgomery, a UW professor of Earth and space sciences, and the other two co-authors used many techniques to analyze the four youngest terraces on the river's edge, including LIDAR maps, carbon dating of rocks and computer models. In 1999 the team even hammered nails into the bedrock and measured the erosion rates directly.

Many rivers, including the Teanaway, have individual features that show evidence of human impact on areas of bedrock. But this is the first time an entire river basin is found to have been transformed by human activity.

"This is a direct topographic signature of the Anthropocene, the 'age of humans' that we now live in," Montgomery said. "The finding that terrace surfaces in the Teanaway are recently-abandoned floodplains suggests that similar landforms around the world may also reflect the influence of human activity."

The UW team recently published an overview paper looking at where river terraces have formed worldwide over the past 4,000 years. The authors showed that in many cases, river terrace formation coincided with deforestation.

"It's sort of a hand-wavey linkage at this point, but I think this could be prevalent worldwide," said Schanz. "It's just not a signal that we've known to look for before."

Schanz will start a faculty position in August at Colorado College, where she plans also to explore what the finding means for how river canyons form through natural processes.

"I think the human part is really interesting, but what has broader implications, for me, is the proof that if you change how sediment moves through a river, you can change erosion rates," Schanz said.

erosion Teanaway River
This photo shows fluting and pothole formation in the bed of the channel. The survey rod in the foreground is 1.1 meters long. Credit: Brian Collins/University of Washington

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The research was funded by the National Science Foundation.

 

Press release from the University of Washington