Mangrove encroachment of salt marsh in Western Port Bay, Victoria: The role of sedimentation, subsidence, and sea level rise |
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Authors: | K Rogers N Saintilan H Heijnis |
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Institution: | 1. School of Arts and Sciences, Australian Catholic University, Post Office Box 968, 2059, North Sydney, NSW, Australia 2. Environment Division, Australian Nuclear Science and Technology Organisation, PMB1, 2234, Menai, NSW, Australia
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Abstract: | Surface elevation tables, feldspar marker horizons, and210Pb analysis of core profiles were implemented at four sites in Western Port Bay, Victoria, Australia, to provide information
on the role of sedimentation, subsidence or compaction, and enhanced sea-level rise in contributing to salt marsh decline.
Photogrammetric surveys indicate that the rate of salt marsh decline that is attributable to mangrove encroachment is lower
in Western Port Bay than in comparable sites in New South Wales. Differences in the rate of mangrove encroachment at Western
Port Bay may be attributed to the inverse relationship found between the degree of mangrove encroachment and surface elevation
increase. While sedimentation contributes to surface elevation changes, surface elevation is not solely explained by sedimentation;
factors including autocompaction and changes in the water table also play a significant role in Western Port Bay. Historic
sedimentation rates measured using210Pb dating techniques corresponded to contemporary sedimentation rates determined from feldspar marker horizons. Core sediment
profiles show no change in sedimentation rates at three sites. A fourth site (French Island) was the only site that exhibited
high rates of sedimentation, which appears to be related to local land-use changes in the area. All sites maintained their
elevation with respect to sea level over the study period. Historic sedimentation exceeded sea-level rise for the past 32
yr, but it is difficult to determine the extent to which belowground processes affect surface elevation, causing deviations
between surface elevation and sedimentation over longer periods. |
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