Abstract
The evolution of mangroves in response to sea-level rise will partially depend on the availability of accommodation space, which is influenced by the hydrodynamic setting. Here, we reconstruct mangrove evolution in a paleochannel of Sungei Jurong (i.e., Jurong River), Singapore via litho-, bio-, and chrono-stratigraphical analyses. Paleochannels are a commonly-occurring, but under-studied hydrodynamic setting in mangroves. Our results show a stratigraphy of a pre-Holocene basal unit of light grey clayey silt with no recorded microfossils (Unit I), overlain by dark grey clayey silt with 45–58% mangrove pollen (e.g.,
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