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245 00 |a Holocene sea levels and palaeoenvironments, Malay-Thai Peninsula, southeast Asia |h [electronic resource].
260        |c 2005.
490        |a The Holocene Volume 15, Number 8 |b Department of Earth and Environmental Science Departmental Papers |y English.
506        |a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
520 3    |a We reveal through sedimentological and palynological investigations of Great Songkhla Lakes, east coast of the Malay-Thai Peninsula, Southeast Asia, sedimentary sequences consisting of very rich palynomorph assemblages dominated by pollen of mangroves and freshwater swamps, but compared with other regions in Southeast Asia are of relatively low diversity. Geochronological data indicate that the Great Songkhla Lakes record one of the earliest mangrove environments in Southeast Asia (8420 to 8190 cal yrs BP), which are subsequently replaced by a freshwater swamp at 7880 to 7680 cal yrs BP due to the decline of marine influence. Sea-level observations from Great Songkhla Lakes and other areas of the Malay-Thai Peninsula reveal an upward trend of Holocene relative sea level from a minimum of -22 m at 9700 - 9250 cal yrs BP to a mid-Holocene high stand of 4850 - 4450 cal yrs BP, which equates to a rise of c. 5.5 mmyr-1. The sea-level fall from the high stand is steady at c. -1.1 mmyr-1. Geophysical modelling shows that hydro-isostasy contributes a significant spatial variation to the sea-level signal between some site locations (3-4 m during the midHolocene), indicating that it is not correct to construct a single relative sea-level history for the Malay-Thai Peninsula.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650    0 |a Climate Change.
650    0 |a Sea Level Rise.
651    0 |a Southeast Asia.
651    0 |a Malay Peninsula.
700 1    |a Horton, Benjamin P..
700 1    |a Morley, R.J..
700 1    |a Gibbard, P.L..
700 1    |a Purintavaragul, C..
700 1    |a Milne, G.M..
700        |a Stargardt,J.M..
773 0    |t Holocene sea levels and palaeoenvironments, Malay-Thai Peninsula, southeast Asia
773 0    |t Holocene sea levels and palaeoenvironments, Malay-Thai Peninsula, southeast Asia
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15061932/00001 |y Click here for full text
856 42 |3 Host material |u http://repository.upenn.edu/ees_papers/38/ |y Holocene sea levels and palaeoenvironments, Malay-Thai Peninsula, southeast Asia
856 42 |3 Host material |u http://dx.doi.org/10.1191/0959683605hl891rp |y Holocene sea levels and palaeoenvironments, Malay-Thai Peninsula, southeast Asia
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/19/32/00001/FI15061932thm.jpg
997        |a Sea Level Rise


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