Spatial and temporal variability of Holocene relative sea level along the South China coast
ID:38 View Protection:ATTENDEE Updated Time:2024-10-09 16:29:55 Hits:813 Oral Presentation

Start Time:2025-01-15 14:45(Asia/Shanghai)

Duration:15min

Session:S27 Session 27-Coastal Environment Evolution: From the Past to the Future » S27-2Coastal Environment Evolution: From the Past to the Future

No files

Abstract
Holocene relative sea-level (RSL) data from the South China coast, a far-field location relative to polar ice sheets, have been used to infer ice-equivalent sea-level changes. However, there are notable misfits between geological RSL data and current glacial-isostatic adjustment (GIA) model predictions in the timing and amplitude of the mid-Holocene highstand and temporal variation of RSL over the Holocene. These misfits bring into question: 1) the interpretation and accuracy of proxies; and 2) whether other local- to regional-scale processes may have significantly influenced RSL.

Here, we present an updated, standardized Holocene RSL database with improved quality control. The dataset includes 227 index points and 342 limiting points, covering a geographical range from 119.19°E (Shantou, Guangdong Province) to 105.90°E (Red River Delta, Vietnam) and from 23.63°N (Chaozhou, Guangdong Province) to 16.45°N (Paracel Islands). Sedimentary (mangrove, tidal flat, lagoon), geomorphic (beach ridge, beach rock), fixed biological (oyster), and coral indicators comprise the majority of RSL data in the compilation for the last 12 ka. The database is divided into 10 sub-regions to investigate the influence of tectonics, sediment compaction, and GIA on RSL.

We apply a spatio-temporal empirical hierarchical model to the database to estimate magnitudes and rates of RSL and compare these results with GIA models using ICE-6G_C and ANU-ICE paired with the 3D earth model HetML140. Our findings reveal sub-regional variability on shorter spatial scales than the long-wavelength GIA signal throughout the Holocene. This spatial pattern suggests that some of the misfit with GIA model predictions stem from local- to regional-scale processes influencing RSL. Our analysis lays the foundation for assessing the potential influence of local factors such as sediment compaction and tidal range changes, as well as regional effects from tectonic vertical motion.
 
Keywords
Holocene,Relative sea level,Sea-level change,Database
Speaker
Howard Yu
Mr The University of Hong Kong

Submission Author
Howard Yu The University of Hong Kong
Nicole Khan The University of Hong Kong
Yonghui Qin The University of Hong Kong
Yadian Wang The University of Hong Kong
Tanghua Li Nanyang Technological University
Fangyi Tan Nanyang Technological University
Yucheng Lin Rutgers University
Submit Comment
Verify Code Change Another
All Comments
Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
Contact Information