Download Holocene Sea-level Scenarios in Bangladesh by Towhida Rashid PDF

By Towhida Rashid

ISBN-10: 9814560987

ISBN-13: 9789814560986

ISBN-10: 9814560995

ISBN-13: 9789814560993

This short bargains with the reconstruction of Holocene paleoenvironment within the primary a part of Bangladesh when it comes to relative sea-level (RSL) alterations that's 2 hundred km north from the current beach. Lithofacies features, mangal peat, diatom and paleophysiographical evidences have been thought of to reconstruct the earlier place and C-14 a long time have been used to figure out the time of formation of the relative sea-level throughout the Holocene. With ordinary reference datum the mandatory m.s.l. on the floor of 5 sections are calculate and the RSL curve means that Bangladesh has skilled mid Holocene RSL transgressions punctuated through regressions. The ample marine diatom and mangrove pollens exhibits that the top RSL transgression in Bangladesh is round 6000 cal BP that is attained no less than 4.5 to 5m greater than the trendy m.s.l. After this section, the relative sea-level began to fall and hence a freshwater peat built round 5980―5700 cal BP. The plentiful mangrove pollens in salt-marsh succession indicates the regression round 5500 cal BP and, the peak was once 1―2 m better than the trendy sea point. those and extra fascinating findings are mentioned during this Brief.

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Extra info for Holocene Sea-level Scenarios in Bangladesh

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Bengal Geosyncline is one of the world’s largest geosyncline that includes the Bengal Basin and the Bay of Bengal. The evolution of the Bengal Basin started in the Permo-Carboniferous with the sedimentation in the faulted Gondwana Basins. The break-up of the Gondwanaland in the Cretaceous Period and the marine transgression led to the sedimentation in the Bengal Geosyncline. Bengal Basin, occupied mostly by Bangladesh, is the result of plate collision between the Indian plate and the Asian plate.

In: Warrick RA, Barrow EM, Wigley TML (eds) Climate and sea level change: observation, projection and implication. Cambridge University Press, Britain, pp 25–44 Grindord J (1985) The palynology of mangroves on a prograde shore, Princess Charlotte Bay, North Queensland, Australia. J Biogeogr 12:323–348 Haq BU, Boersma A (1978) Introduction to Marine Micropaleontology. Elsevier, New York, p 376 Higgins CG (1994) Subsurface environment of beaches—temperature and salinity. In: Geologic Society of America, abstracts with programs, Seattle meeting, p A-364 Ireland S (1987) The Holocene sedimentary history of the coastal lagoon of Rio de Janiero state, Brazil.

Longer-term changes are influenced by changes in the Earth’s climates. Consequently, the level is better defined as mean sea level, the height of the sea surface averaged over all stages of the tide over a long period of time (Britanica Concise Encyclopedia). Sea level, the level of the sea, serves as the datum used for measurement of land elevations and ocean depths. Theoretically, one would expect sea level to be a fixed and permanent horizontal surface on the face of the earth, and as a starting approximation, this is true.

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Holocene Sea-level Scenarios in Bangladesh by Towhida Rashid


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