Early Holocene initiation of the Mekong River delta, Vietnam, and the response to Holocene sea-level changes detected from DT1 core analyses

2010 ◽  
Vol 230 (3-4) ◽  
pp. 146-155 ◽  
Author(s):  
Van Lap Nguyen ◽  
Thi Kim Oanh Ta ◽  
Yoshiki Saito
PLoS ONE ◽  
2020 ◽  
Vol 15 (3) ◽  
pp. e0229464 ◽  
Author(s):  
SongYi Paik ◽  
Dung Thi Phuong Le ◽  
Lien Thi Nhu ◽  
Bradford Franklin Mills

2018 ◽  
Vol 28 (3) ◽  
pp. 329-335
Author(s):  
Tạ Thị Kim Oanh ◽  
Nguyễn Văn Lập

Holocene sedimentary facies related to sea-level change of the Vinh Long - Tra Vinh area, Mekong River Delta


1994 ◽  
Vol 42 (2) ◽  
pp. 149-161 ◽  
Author(s):  
Karl Anundsen ◽  
Sally Abella ◽  
Estella Leopold ◽  
Minze Stuiver ◽  
Sheila Turner

AbstractAnalyses of sediments, diatoms, and pollen in a 12.65-m-long sediment core taken from Lake Carpenter in the central Puget Lowland, Washington, provide detailed information regarding the history of deglaciation and late-glacial/early Holocene sea-level changes. The lake outlet, now 8.2 m above sea level, has been lowered 1-1.5 m by postglacial erosion. The lithology and pollen record suggest that no lengthy hiatuses in sedimentation have occurred. The basal sediments are glacialmarine and contain shell fragments and brackish/marine diatoms. Freshwater sediments above the basal section are interrupted only by a short section containing few fossils, most of which are brackish to marine indicators, and by the Mazama tephra at 9.5 m. The pollen record in the basal 4 m reveals a Pinus zone (ca. 13,850-11,000 yr B.P.) with a brief peak of Picea at ca. 13,700 yr B.P., and an Alnus/Pseudotsuga zone (ca. 11,000-6500 yr B.P.). The chronology is based on nine radiocarbon ages. A relative lowering of sea level below the 9.5-m threshold is recorded in the core at 12.41 m and dates 13,850 to 13,700 yr B.P. A marine episode occurred about 13,600 yr B.P., implying that relative sea-level temporarily rose above 9.5 m. No subsequent transgressions above the 9.5-m level have been recorded. Comparison of six radiocarbon dates ≥13,600 yr B.P. suggest that the marine reservoir correction of 760 yr currently used for this area may be too high for this time period.


2020 ◽  
Vol 12 (24) ◽  
pp. 10356
Author(s):  
Pham Thi Oanh ◽  
Makoto Tamura ◽  
Naoko Kumano ◽  
Quang Van Nguyen

This study evaluated inundation impacts and the economic damage resulting from sea level rise (SLR) in the Vietnamese Mekong River Delta (VMRD), and identified the effectiveness of mixing gray and green infrastructures using cost-benefit analysis. The results showed that the VMRD could potentially be heavily affected by SLR. Without the implementation of proper adaptations, more than 90% of this area could be below sea level and nearly 20 million people could be affected by inundation by the end of the 21st century. The total economic damage could reach more than 22,000 billion US$ (2010 real value) by 2100 with no discount rate. These threats may increase the pressure on the region to ensure well-being, equity, and progress towards achieving sustainable development goals. However, achieving these goals will require the implementation of adaptations for upgrading and restoring in the region. This study assessed the effectiveness of adaptations and demonstrated that mixing gray and green infrastructures could benefit coastal inhabitants at a cost of 12 to 19 billion US$.


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