Morphodynamic characteristics and genetic mechanism of the submarine sandbanks in Xuande Atoll, Xisha Islands

HE Qijiang; SHEN Aisi; LIU Gang; DING Dong; QU Hongbao; LIU Gen; GOU Pengfei

doi:10.16562/j.cnki.0256-1492.2022041101

2023 Vol. 43, No. 1

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HE Qijiang, SHEN Aisi, LIU Gang, DING Dong, QU Hongbao, LIU Gen, GOU Pengfei. Morphodynamic characteristics and genetic mechanism of the submarine sandbanks in Xuande Atoll, Xisha Islands[J]. Marine Geology & Quaternary Geology, 2023, 43(1): 1-12. doi: 10.16562/j.cnki.0256-1492.2022041101

Citation:

HE Qijiang, SHEN Aisi, LIU Gang, DING Dong, QU Hongbao, LIU Gen, GOU Pengfei. Morphodynamic characteristics and genetic mechanism of the submarine sandbanks in Xuande Atoll, Xisha Islands[J]. Marine Geology & Quaternary Geology, 2023, 43(1): 1-12. doi: 10.16562/j.cnki.0256-1492.2022041101

Morphodynamic characteristics and genetic mechanism of the submarine sandbanks in Xuande Atoll, Xisha Islands

1.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Key Laboratory of Marine Geology Resources and Environment of Hainan Province, Haikou 570206, China
3.
Marine Geological Survey Institute of Hainan Province, Haikou 570206, China
4.
Third Institute of Oceanography, Ministry of Natural Resources, Xiamen 361005, China

More Information

Corresponding author: GOU Pengfei, Goupeng-fei@163.com

Received Date: 11 April 2022

Revised Date: 21 June 2022

Accepted Date: 21 June 2022

Publish Date: 28 February 2023

Abstract

Abstract

Submarine geomorphology can reveal the topographic characteristics of seafloor, which is helpful to understand the composition, formation, evolution, and distribution of the sediment. The hydrologic elements and hydrodynamic conditions in Xuande Atoll, Xisha, Islands, South China Sea were quantitatively investigated by the combination of single beam sounding, single-channel seismology, sampling of surface sediments, and hydrodynamic measurements. Furthermore, the morphodynamic characteristics and genetic mechanism of submarine sandbanks were discussed in detail. Results show that the coral reef frame and buried corals that developed in water depth of 50～55 m and 60 m in the atoll lagoon were formed in the same period of typical landforms that formed in the 50～60 m depth during the lower sea level period of the Holocene in South China Sea. It is likely that the boundary of the submarine geomorphology developed in water depth of 50～55 m retained the paleo-lagoon reef morphology of the Early Holocene. Five types of submarine sandbanks with own morphodynamic characteristics were identified in the atoll lagoon where tidal currents at the bottom are the main modern dynamic factors that shape the submarine sandbanks. Under normal weather condition, tidal currents in the study area are strong to transport sandy sediments and shape the geomorphology of present submarine sandbanks on the previous topography formed during sea level fluctuations. The sea level fluctuations are induced by climate change, followed by topographic foundation (coral frame, reef shoreline, reef gate) and tidal currents, and are the main factors that control the development of submarine sandbanks in the study area.
- submarine sandbanks /
- morphodynamic /
- hydrodynamic conditions /
- genetic mechanism /
- Xuande Atoll

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References

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