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Nanjing Man

life science Maturity 11-13 Next article →

Nanjing Man refers to a significant fossil discovery of an early human species. These fossils belong to Homo erectus, an extinct species of human. Some scientists believe these specimens might even be related to Peking Man. This discovery is vital because it helps researchers understand human history in East Asia. It provides physical evidence of how early humans lived and moved across the continent. By studying these remains, scientists can track the evolution of the genus Homo.

The discovery process began with careful investigation of the local landscape. In 1992, a team from the Nanjing Institute of Geology and Paleontology identified Hulu Cave. This cave is located near the Tangshan hills in the Jiangning District of Nanjing. The team believed the cave was a site containing many mammalian fossils. They organized further excavations with the Institute of Vertebrate Paleontology and Paleoanthropology from Beijing. In March 1993, a local worker named Liu Luhong found the actual fossils. He discovered the remains at a depth of 60 to 97 centimeters within the limestone cave.

The fossils consist of three specific pieces of remains. These include two partial skull fragments, labeled Nanjing 1 and Nanjing 2. The first fragment is notable because it retains most of the face. The second fragment belongs to a different individual, likely a female, while the first was a male. The third piece is a single upper molar tooth, known as Nanjing 3. These fragments belong to the middle Pleistocene epoch. This period is a major chapter in the history of early human development.

Determining the exact age of these fossils required advanced scientific methods. Researchers used mass spectrometric U-series dating to calculate how old the skulls are. This method measures uranium levels to provide a timeline of the past. In 2001, this research estimated the skulls were between 580,000 and 620,000 years old. This was much older than previous estimates using other methods. For example, an earlier study in 1999 estimated one skull was at least 500,000 years old. However, the tooth found at the site was estimated to be only 400,000 years old.

There is a scientific reason for the difference in age between the tooth and the skulls. Researchers proposed that the enamel on the tooth may have different uranium uptake. This means the way the tooth absorbed uranium was not the same as the skulls. Because of this, the dating results for the tooth and the skulls do not match perfectly. Despite this discrepancy, the age of the skulls remains a crucial piece of evidence. It helps scientists build a more accurate timeline for early human presence in China.

The discovery had a massive impact on our understanding of human migration. Before this find, scientists already knew Homo erectus lived in East Asia. However, the new dates pushed the arrival of Homo erectus back by 270,000 years. This suggests that Homo erectus occupied East Asia much earlier than previously thought. It supports the idea that they lived in Asia before pre-modern Homo sapiens existed. This finding added a new layer of complexity to the study of human population dynamics.

Nanjing Man also shows how much variety existed among early humans. The morphological features of these fossils are quite unique. This includes their cranial capacity, which is the volume inside the skull. Their cranial metrics, or specific measurements of the skull, differ from other Chinese hominins. Even with these differences, they still fall within the expected range for Homo erectus. This high diversity shows that different groups of Homo erectus had distinct physical traits.

Today, these important fossils are preserved for the public to see. The skull fragments are displayed at the Nanjing Homo erectus fossil museum. The museum provides educational information about Nanjing Man and the history of China. Visitors can learn about how Homo erectus colonized the region. This site helps connect modern people to the deep history of our ancestors. It serves as a permanent record of a discovery that changed science.

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