SUMMARY
Initial results of research on Quaternary sediments and sea
level changes of Tràng An landscape complex(Ninh B́nh)
Trần Tân
Văn, Nguyễn Đại Trung, Vũ Văn Hà, Trịnh
Thị Thúy
Tràng An area has undergone a series of sea transgressions and regressions
corresponding to global glacial and interglacial periods from the Early
Pleistocene to the Late
Holocene, especially the Flandrian sea transgression. The alternating sea
transgressions and regressions affecting the Ninh B́nh area are: Cát Lâm,
Bỉm Sơn and Vĩnh Phúc transgresions in Pleistocene, followed by
Đống Đa transgression (also calledHải
Hưng transgression and corresponding with Flandrian
transgression in countries such as Belgium,
Holland, etc.)
which reached the maximum in Early-Middle Holocene.. Erosion notches in the
limestone mark the Quaternary sea levels at different elevations. The results
of C14 dating of oyster shells in the erosion notches at 2m a.s.l give
the age of 4,300 to 6,500 years BP, corresponding with Early-Middle Holocene
(Hải Hưng transgression - Flandrian transgression). The caves in
Tràng An area are mostly through karst caves and fossil caves formed in four
periods: Period 1 lasted from the end of Early Pleistocene to the beginning of
Middle Pleistocene with the formation of the oldest caves at 60m a.s.l, such as
Trống, Bói, Chợ. Period 2 was in Late Pleistocene with the
formation of the caves at 10-15m, 20-30m a.s.l, such as Thung B́nh and Ṃi. Period
3 was in Early-Middle Holocene with the formation of the caves at 2-9m a.s.l, such as Vàng,
Ông Hay, Ốc, Trâu Bái Đính, Thiên Hà, etc. In period 4 were formed the
caves at below 2m, mainly though caves such as Sinh, Seo, Thuốc,
Địa Linh, Quy Hậu, etc. Stone implements of ancient people have
been found in many caves, such as Ốc, Thiên Hà, Vàng, Ông Hay, Ṃi, which
were used as shelters during Hải Hưng (Đống
Đa)transgression in Early-Middle
Holocene when the seawater submerged the Tràng An area as a whole to the height
of 2 to 10m. Some caves like Trống, Bói and Chợ might have been
occupied by ancient people in the Late Pleistocene (23,000 years BP).
Người biên tập: PGS.TSKH Nguyễn Địch
Dỹ.