Fig. 1: Location of the study area.
From: Foraminiferal environmental DNA reveals late Holocene sea-level changes
The study area is located in the Pearl River Delta (PRD) (a) and in Deep Bay (b). Location of surface sampling transects (MP_A, MP_B, and SK), sediment core MPSC01, the nearest tide gauge at Tsim Bei Tsui, and the land surface elevation as represented by the LiDAR digital elevation model provided by the Hong Kong S.A.R government in Mai Po and Sha Kiu (c). Historical boundaries of mangrove in Mai Po Nature Reserve inferred from aerial images47 are indicated by the black dashed line.
