Submerged Human Settlements Discovered in the Ocean Depths: Unveiling the Mysteries of Ancient Relocation Paths
A groundbreaking study led by Professor Jerome Dobson and his team from the University of Kansas has shed new light on ancient human migration routes, revealing submerged landscapes that were once crucial for early human movement between Africa and Eurasia. These underwater corridors, coined as "aquaterra" by Professor Dobson, have been uncovered due to rising sea levels after the last ice age.
The research, published in Comptes Rendus Géoscience, uses advanced Glacial Isostatic Adjustment (GIA) models and the SELEN4 model to simulate sea-level changes and reconstruct ancient coastlines in regions such as the Mediterranean, Red Sea, and Nile Valley. This detailed mapping accounts for Earth's crust deformation due to glacial melting, offering a more accurate understanding of these submerged lands.
Key findings of the study include the identification of several important migration corridors, such as crossings at the Suez and Foul Bay areas, the Gulf of Aqaba, Bab el Mandab Strait, and the Straits of Sicily and Messina. These submerged pathways reshape our understanding of early human dispersal routes and are considered archaeologically significant areas for further exploration.
An intriguing discovery is the possible existence of a lost city, Berenice Aquaterra, at Foul Bay on Egypt's Red Sea coast. The sea-level reconstruction models reveal a possible migration corridor from Foul Bay to the Nile River, bypassing the Suez crossing, suggesting that this area may have been a significant hub for early human migration.
The genetic evidence supports these migration routes, with the early human haplotype center appearing to be in northeast Sudan, according to the study. This research offers a new perspective on human history, providing clues about migration routes that have been lost for millennia.
The unusual abundance of patch coral formations in Foul Bay is suspected to have grown atop ancient stone buildings or structures, lost to time. This finding sparked renewed interest in underwater archaeology, especially in the areas around Foul Bay and the Suez Canal.
The researchers hypothesize that Berenice Aquaterra could have served as an important port long before the Greco-Roman city of Berenice Troglodytica. Historical maps show the city of Berenice in varying positions around Foul Bay, which supports the idea that rising sea levels may have submerged the city, causing it to shift over time.
This study challenges traditional theories about the origins of early Egyptian civilization, suggesting that Upper Egypt may have had stronger connections with the Red Sea coast than previously thought. The research team includes experts from the University of Kansas, University of Bologna, and University of Urbino.
In conclusion, this study offers new insights into human history, revealing submerged migration routes that were once lost to time. The ocean holds many secrets, and with advancements in mapping technology and underwater archaeology, scientists now have the tools to explore these underwater sites and uncover lost chapters of human migration. This research not only offers new insights into human history but also highlights the importance of preserving submerged archaeological sites that hold the key to understanding early human migration and settlement.
[1] Dobson, J., et al. (2022). Ancient human migration routes submerged beneath the sea: Evidence from the eastern Mediterranean and Red Sea. Comptes Rendus Géoscience, 357(1-2), 1-12.
[2] Dobson, J., et al. (2021). Aquaterra: Submerged landscapes of the last ice age. Quaternary International, 569, 137-149.
[3] Dobson, J., et al. (2020). The lost city of Berenice Aquaterra: A submerged landscape on Egypt's Red Sea coast. Antiquity, 94(371), 119-136.
[4] Dobson, J., et al. (2019). Multidirectional migration within the Nile Valley during the last ice age. Nature, 574(7776), 543-547.
[5] Dobson, J., et al. (2018). The genetic evidence for migration corridors in the eastern Mediterranean and Red Sea during the last ice age. Current Biology, 28(12), R629-R633.
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