Uncovering Shantou’s Erosive Neritic Zone in the NE South China Sea Since MIS 5 Through OSL Core Dating

An erosive neritic area of Shantou in coastal NE South China Sea since at least MIS 5 revealed by OSL dating of cores – Frontiers

Unveiling the Erosional Dynamics of Shantou: Fresh Perspectives from the Northeastern South China Sea Coast

Recent advancements in geological research have illuminated the complex erosional history of the neritic zone off Shantou’s coastline, situated in the northeastern sector of the South China Sea. By applying state-of-the-art Optically Stimulated Luminescence (OSL) dating to sediment core samples, scientists have reconstructed coastal evolution extending back to Marine Isotope Stage 5 (MIS 5), roughly between 130,000 and 75,000 years ago. Published in Frontiers, this study offers a nuanced understanding of how natural forces and sea-level fluctuations have shaped this region over millennia. As researchers continue to analyze sedimentary deposits beneath Shantou’s waters, their findings are poised to inform adaptive strategies addressing ongoing climate change challenges and accelerating coastal erosion.

Decoding Erosion Patterns in Shantou’s Coastal Waters Using OSL Techniques

The neritic environment adjacent to Shantou has been identified as a hotspot for significant erosive activity persisting since at least MIS 5. Through meticulous OSL dating on sediment cores extracted up to depths of 15 meters, researchers established a detailed chronology revealing multiple phases of sediment loss and redeposition. These insights highlight not only natural climatic influences but also underscore increasing human-induced pressures exacerbating erosion rates—recently estimated at approximately 2 centimeters annually.

Key revelations from this analysis include:

Parameter Observation
Date Range of Sediments Up to ~120,000 years old
Sediment Core Depths Analyzed Reaching depths near 15 meters
Erosion Rate (Recent Decades) Around 2 cm per year on average

Tracing Historical Coastal Transformations Across the South China Sea Basin

Employing OSL dating methods has enabled scientists to revisit assumptions about stability along parts of the South China Sea coastline near Shantou. Contrary to earlier beliefs that these zones were relatively static over long timescales, data now reveal substantial shoreline recession linked closely with MIS 5 climatic oscillations—an epoch marked by pronounced glacial-interglacial cycles affecting global sea levels.

This research highlights several critical outcomes: