Depositional evolution of nearshore fringing reefs in the Changpi region, Hainan Island: assessing the role of siliciclastic influx

Maosong Ye ^1* Lijuan Shao ² Ruirui Song ² Weihua Liao ³ Qiaozhu Pang ¹ Hongfei Xu ⁴

• ¹ Hainan Academy of Ocean and Fisheries Sciences, Haikou, China
• ² Shandong Institute of Geophysical and Geochemical Exploration, Jinan, China
• ³ Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences (CAS), Nanjing, Jiangsu Province, China
• ⁴ Key Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, Liaoning Province, China

Abstract：Nearshore fringing reefs have been shown to establish and accrete within sediment-laden coastal environments over millennial timescales. However, the mechanisms governing the evolution of turbid-water reefs remain inadequately understood. This study focuses on a fringing reef in the Changpi (CP) region along the eastern coast of Hainan Island, China. Sedimentological and geochronological analyses of four drill cores provided the first comprehensive growth history for this marginal reef setting through a systematic reconstruction of its developmental chronology, architectural framework, and ecological characteristics.Radiocarbon dating reveals reef initiated at about 7,400 cal yr BP followed by accretion termination around 4,000 cal yr BPand ceased accretion after 4,000 cal yr BP. By integrating core observations, thin-section petrography, and X-ray diffraction results, five distinct lithofacies were identified. These lithofacies exhibit varying degrees of mixing between siliciclastic and carbonate components, revealing that the reef system was periodically influenced by terrigenous siliciclastic input. The vertical accretion of the CP reef underwent three primary stages: (1) colonization stage (7,400-6,400 cal yr BP), characterized by well-preserved coral assemblages in high-energy, clear-water conditions with relatively low accretion rates (~(ca 0.35 mm/yr) and gradual coral diversification; (2) turbid stage (6,400-5,000 500 cal yr BP), marked by rapid terrigenous clastic deposition that produced persistent turbidity, leading to accelerated accretion rates (5.22-up to 6.39 29 mm/yr) and reduced coral diversity; and (3) stabilization stage (5,000-5,500-4,000 cal yr BP), during which stabilized siliciclastic input restored clear-water conditions, supporting renewed coral growth at moderate accretion rates (~(ca 2.70 mm/yr). This case study demonstrates that terrestrial sediment fluxes can exert have a greater influence on nearshore reef trajectories than sea-level changes, particularly in regions or periods characterized by high sediment input. As suggested by the findings, this underscores the necessity of integrated coastal zone management strategies aimed at reducing agricultural runoff and controlling construction sediment to enhance reef resilience.