Journal of Tropical Oceanography ›› 2020, Vol. 39 ›› Issue (2): 44-53.doi: 10.11978/2019041CSTR: 32234.14.2019041

Special Issue: 南海专题

• Marine Geology • Previous Articles     Next Articles

Characteristics and morphodynamics of newly-formed coral debris deposits on the Niu’e and Ximen Reefs, Jiuzhang Atoll, South China Sea

Mouying XU1(), Shu GAO2(), Chendong GE1, Mei HUANG1   

  1. 1. Key Laboratory of Coast & Island Development of Ministry of Education, School of Geographic and Oceanographic Science, Nanjing University, Nanjing 210023, China;
    2. Stake Key Laboratory of Estuarine and Coastal Research, School of Marine Sciences, East China Normal University, Shanghai 200241, China
  • Received:2019-04-22 Revised:2019-10-15 Online:2020-03-10 Published:2020-03-10
  • Supported by:
    Key Project of the National Natural Science Foundation of China(41530962);Academician Consulting Project of the Chinese Academy of Sciences(2016ZWH005A-005)

Abstract:

Coral reefs over the Nansha Islands have characteristic geomorphological patterns; they exist in the form of atolls. The Niu’e (also known as Mckennan) and Ximen (Whitsum) reefs of the Jiuzhang Giant Atoll are two secondary atolls with newly-formed debris deposits, which may represent an important stage of landform evolution from a submerged atoll towards a reef island. Grain-size analysis of the surficial sediment samples collected from the two reefs shows that gravel-sized coral debris is the main component of the deposit. Medium grain sizes of the samples (measured by the long axis) range from 14 to 45 mm. Sorting coefficients range from 4.5 (being poorly sorted) to 31 with a sphericity value of 0.52 to 0.68 (far from a sphere shape). Medium grain sizes show a trend of increasing away from the shoreline. Medium grain sizes of the sediment samples are positively correlated with sorting coefficients, whereas they are more or less negatively correlated with sphericity values. Based on an analysis of historical records and satellite images, these beach ridge- or sand bar-like deposits represent modern accumulation landforms; their formations are related to storm waves and to some extent to the winter monsoon waves. The sand bar on the Niu’e reef had been extending towards the southeast and at the same time moving towards the north. The sand bar on the Ximen reef had an overall migration towards the southeast, with recurved sand spits on both sides. The mechanisms for the formulation of these features, in terms of changes in coral material supply and storm wave pattern, need further investigations.

Key words: newly-formed reef top deposits, grain size, coral debris, storm wave, Jiuzhang Atoll, South China Sea

CLC Number: 

  • P737.11