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The palaeoenvironmental development of the northeastern Vietnamese Mekong River Delta since the mid Holocene

Bibliographic Data

ID12267283
AuthorsUlrike Proske (0000-0002-3153-7228, University of Bremen, corresponding author), Till J J Hanebuth (0000-0002-2833-3320, University of Bremen), Hermann Behling (0000-0002-5843-8342, University of Göttingen), Van Lap Nguyen (Vietnam Academy of Science and Technology), Van Lap Nguyen Van Lap Nguyen (Vietnamese Academy of Science and Technology, Vietnam), Thi Kim Oanh Ta (Vietnam Academy of Science and Technology), Thi Kim Oanh Ta Thi Kim Oanh Ta (Vietnamese Academy of Science and Technology, Vietnam), Bùi Phát Diệm (Thang Long University), Bui Phat Diem Bui Phat Diem (Provincial Museum Long An, Vietnam)
Year2010
Volume20
Issue8
Pages1257-1268
Publication date2010-07-27
Open AccessYes
TypeARTICLE
VenueThe Holocene (JOURNAL)
Journal identifiersISSN: 0959-6836 • E-ISSN: 1477-0911
PublisherSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683610374884
OpenAlexW2029602345
LanguageEN
Citations received8
References cited27

Three radiocarbon-dated sediment cores from the northeastern Vietnamese Mekong River Delta have been analysed with a multiproxy approach (grain size, pollen and spores, macro-charcoal, carbon content) to unravel the palaeoenvironmental history of the region since the mid Holocene. During the mid-Holocene sea-level highstand a diverse, zoned and widespread mangrove belt (dominated by Rhizophora) covered the extended tidal flats. The subsequent regression and coeval delta progradation led to the rapid development of a back-mangrove community dominated by Ceriops and Bruguiera but also represented locally by e.g. Kandelia, Excoecaria and Phoenix. Along rivers this community seems to have endured even when the adjoining floodplain had already shifted to freshwater vegetation. Generally this freshwater vegetation has a strong swamp signature but locally Arecaceae, Fabaceae, Moraceae/ Urticaceae and Myrsinaceae are important and mirror the geomorphological diversity of the delta plain. The macro-charcoal record implies that natural burning of vegetation occurred throughout the records, however, the occurrence of the highest amounts of macro-charcoal particles is linked with modern human activity

Charcoal · Delta · Geography · Holocene · Mangrove · Marsh · Palynology · Physical geography · Pollen · Radiocarbon dating · Rhizophora · Vegetation (pathology · Wetland · Coastal wetland ecosystem dynamics · Geological formations and processes · Geology and Paleoclimatology Research · Ecology · Geology · Oceanography · Paleontology

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Citations per year0.53
Citation span2011 - 2022 (12)
Highly citedNo

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