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Holocene Sea-level Scenarios in Bangladesh (Paperback, 2014)
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Holocene Sea-level Scenarios in Bangladesh (Paperback, 2014)
Series: SpringerBriefs in Oceanography
Expected to ship within 10 - 15 working days
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This Brief deals with the reconstruction of Holocene
paleoenvironment in the central part of Bangladesh in relation to
relative sea-level (RSL) changes which is 200 km north from the
present coastline. Lithofacies characteristics, mangal peat, diatom
and paleophysiographical evidences were considered to reconstruct
the past position and C-14 ages were used to determine the time of
formation of the relative sea-level during the Holocene. With
standard reference datum the required m.s.l. at the surface of five
sections are calculate and the RSL curve suggests that Bangladesh
has experienced two mid Holocene RSL transgressions punctuated by
regressions. The abundant marine diatom and mangrove pollens
indicates that the highest RSL transgression in Bangladesh is
around 6000 cal BP which is attained at least 4.5 to 5m higher than
the modern m.s.l. After this phase, the relative sea-level started
to fall and consequently a freshwater peat developed around 5980
5700 cal BP. The abundant mangrove pollens in salt-marsh succession
shows the regression around 5500 cal BP and, the height was 1 2 m
higher than the modern sea level. These and more interesting
findings are discussed in this Brief.
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