Late Quaternary environmental changes in the Pearl River mouth region, China |
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| Authors: | Y Zong WW-S Yim F Yu G Huang |
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| Institution: | aDepartment of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong SAR, China;bDepartment of Geography, University of Durham, South Road, Durham DH1 3LE, UK;cGuangzhou Institute of Geography, 100 Xian Lie Road, Guangzhou 510070, China |
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| Abstract: | This study presents findings concerning Late Quaternary environmental changes in the Pearl River mouth region, China based on the study of over 300 boreholes. Out of these, 35 boreholes are selected for the reconstruction of transects across the deltaic plain and estuary. 39 radiocarbon dates obtained from these boreholes are used to help define the chronology of stratigraphic units present including two terrestrial units (T1 and T2) and two marine units (M1 and M2). Diatom assemblages are studied in 6 boreholes revealing similarities and differences between the two marine units. Before the area was inundated by the last interglacial sea (MIS 5), an older terrestrial unit of sand and gravel (T2) was laid down in a number of palaeo-valleys. During the last interglacial period, an older marine unit of silt and clay (M2) was laid down which was subsequently subaerially exposed when sea-level regressed during the last glacial period (MIS 4-2) causing the uppermost section to be weathered. During the same period, a younger terrestrial unit of sand and gravel (T1) was deposited along palaeo-river channels. Around the early Holocene before 8.2 cal. ka BP, the postglacial rise in sea level initiated a new phase of sedimentation in the outer part of the estuary, characterised by the high percentages of marine diatoms in the sediments. In the early Holocene, strong monsoon freshwater discharge resulted in sedimentation of a fine-sand layer in the inner part of the estuary. After 8.2 cal. ka BP, rapid rises in sea level caused widespread marine inundation and sedimentation. The diatom data suggest that the relative sea level associated with the M2 and M1 units were both at similar levels. Because the M2 unit is typically recorded at altitudes of 15 m and 20 m below the present sea level, this is likely to be a result of long-term subsidence. Although numerical dating of the pre-M1 units has not been made in the present study, the chronology of these units can be inferred from uranium-series ages and optically stimulated luminescence dating obtained from the adjacent coastal waters of Hong Kong. The T1 unit has yielded ages of about 30.0 cal. ka BP while the M2 unit has yielded ages about 130.0 cal. ka BP confirming their MIS 4-2 and MIS 5 ages respectively. |
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