Mid Holocene palaeoenvironments from Lake Nhlange, northern Kwazulu-Natal, South Africa

CI Wright, Andrew Cooper, RN Kilburn

Research output: Contribution to journalArticle

14 Citations (Scopus)

Abstract

Palaeoenvironments are described from 5 vibracores taken from within Lake Nhlange, the largest waterbody within the Kosi system which comprises a series of lakes linked to the sea via a large tidal sand-flat. The mid to late Holocene lagoonal palaeoenvironment has undergone minimal sedimentation since the Last Glacial Maximum (18,000 BP, oxygen-isotope stage 2). Shelf-margin gravity slumping has transported typical shallow water, intertidal molluscan assemblages into deeper subtidal environments. The lake bathymetry exhibits a drowned Last Glacial Maximum palaeofluvial channel topography, preserved by the post-last Glacial Maximum (Flandrian) transgression which formed a large coastal dune barrier, trapping the lakes behind it. The palaeoestuary mouth was located at Bhanga Nek, until approximately 3,000 BP, but has been relocated 13 km north, approximately 1,500 BP, to where it now maintains an open inlet through the coastal barrier. An abundant Holocene molluscan assemblage combined with detailed sedimentological descriptions indicate that the conditions within Nhlange have changed over the last 5,000 years from a deep coastal estuarine/lagoonal system, with free tidal exchange to a predominantly freshwater lake. The molluscan assemblages indicate a subtropical, temperate lagoonal environment similar to Durban Bay (prior to anthropogenic changes) with a number of species including Paphia textile indicating a warmer climate. A modern analogy of the palaeoenvironment would be that of the inside edge of Bazaruto Archipelago, Mozambique.
LanguageEnglish
Pages991-1001
JournalJournal of Coastal Research
Volume15
Issue number4
Publication statusPublished - 1999

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paleoenvironment
Holocene
Last Glacial Maximum
lake
Flandrian
subtidal environment
slumping
bathymetry
transgression
archipelago
oxygen isotope
trapping
dune
shallow water
Africa
topography
sedimentation
gravity
climate

Cite this

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title = "Mid Holocene palaeoenvironments from Lake Nhlange, northern Kwazulu-Natal, South Africa",
abstract = "Palaeoenvironments are described from 5 vibracores taken from within Lake Nhlange, the largest waterbody within the Kosi system which comprises a series of lakes linked to the sea via a large tidal sand-flat. The mid to late Holocene lagoonal palaeoenvironment has undergone minimal sedimentation since the Last Glacial Maximum (18,000 BP, oxygen-isotope stage 2). Shelf-margin gravity slumping has transported typical shallow water, intertidal molluscan assemblages into deeper subtidal environments. The lake bathymetry exhibits a drowned Last Glacial Maximum palaeofluvial channel topography, preserved by the post-last Glacial Maximum (Flandrian) transgression which formed a large coastal dune barrier, trapping the lakes behind it. The palaeoestuary mouth was located at Bhanga Nek, until approximately 3,000 BP, but has been relocated 13 km north, approximately 1,500 BP, to where it now maintains an open inlet through the coastal barrier. An abundant Holocene molluscan assemblage combined with detailed sedimentological descriptions indicate that the conditions within Nhlange have changed over the last 5,000 years from a deep coastal estuarine/lagoonal system, with free tidal exchange to a predominantly freshwater lake. The molluscan assemblages indicate a subtropical, temperate lagoonal environment similar to Durban Bay (prior to anthropogenic changes) with a number of species including Paphia textile indicating a warmer climate. A modern analogy of the palaeoenvironment would be that of the inside edge of Bazaruto Archipelago, Mozambique.",
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Mid Holocene palaeoenvironments from Lake Nhlange, northern Kwazulu-Natal, South Africa. / Wright, CI; Cooper, Andrew; Kilburn, RN.

In: Journal of Coastal Research, Vol. 15, No. 4, 1999, p. 991-1001.

Research output: Contribution to journalArticle

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AB - Palaeoenvironments are described from 5 vibracores taken from within Lake Nhlange, the largest waterbody within the Kosi system which comprises a series of lakes linked to the sea via a large tidal sand-flat. The mid to late Holocene lagoonal palaeoenvironment has undergone minimal sedimentation since the Last Glacial Maximum (18,000 BP, oxygen-isotope stage 2). Shelf-margin gravity slumping has transported typical shallow water, intertidal molluscan assemblages into deeper subtidal environments. The lake bathymetry exhibits a drowned Last Glacial Maximum palaeofluvial channel topography, preserved by the post-last Glacial Maximum (Flandrian) transgression which formed a large coastal dune barrier, trapping the lakes behind it. The palaeoestuary mouth was located at Bhanga Nek, until approximately 3,000 BP, but has been relocated 13 km north, approximately 1,500 BP, to where it now maintains an open inlet through the coastal barrier. An abundant Holocene molluscan assemblage combined with detailed sedimentological descriptions indicate that the conditions within Nhlange have changed over the last 5,000 years from a deep coastal estuarine/lagoonal system, with free tidal exchange to a predominantly freshwater lake. The molluscan assemblages indicate a subtropical, temperate lagoonal environment similar to Durban Bay (prior to anthropogenic changes) with a number of species including Paphia textile indicating a warmer climate. A modern analogy of the palaeoenvironment would be that of the inside edge of Bazaruto Archipelago, Mozambique.

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