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Yen HPH, Nhan TTT, Nghi T, Toan NQ, Khien HA, Lam DD, Van Long H, Thanh DX, Hung NT, Trang NTH, Dien TN, Tuyen NT, Truong TX, Dung TT, Thao NTP, Lan VQ. Late Pleistocene-Holocene sedimentary evolution in the coastal zone of the Red River Delta. Heliyon 2021; 7:e05872. [PMID: 33521345 PMCID: PMC7820486 DOI: 10.1016/j.heliyon.2020.e05872] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/19/2019] [Revised: 05/15/2020] [Accepted: 12/24/2020] [Indexed: 11/26/2022] Open
Abstract
The Red River Delta is considered one of the largest megadelta systems in Asia. The formation of this delta has been controlled by the continent-ocean interaction and sea-level fluctuation during the Cenozoic. In this study, we present a new sequence stratigraphic framework of the Red River Delta based on borehole lithofacies analysis and high resolution seismic data. The Late Pleistocene–Holocene sediments in the coastal zone of the Red River Delta were subdivided into three systems tracts: (1) the lowstand systems tract (LST) is characterized by a Late Pleistocene alluvial silty sand facies complex (arLSTQ13b); (2) the transgressive systems tract (TST) is illustrated by the coastal marsh facies complex and the lagoonal greenish-gray clay facies of Early-Middle Holocene (amt, mtTSTQ21−2); and (3) the highstand systems tract (HST) is composed of the Middle-Late Holocene deltaic clayish silt facies complex (amhHSTQ22−3). The boundaries between these three systems tracts are not isochronous, namely: (1) The LST-HST boundary has been associated with the Würm 2 Glaciation, which occurred at ~40-18 Ka.; (2) The TST-LST boundary is identified by a transgressive erosion surface, whose age ranges from ~12-5 Ka.; and (3) the HST-TST boundary is an unconformity between the submarine deltaic facies complex and the Middle Holocene marine flooding plain.
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Affiliation(s)
- Hoang Phan Hải Yen
- School of Social Sciences Education, Vinh University, 182 Le Duan, Vinh, Nghe An, Viet Nam
| | - Tran Thị Thanh Nhan
- University of Science, Vietnam National University, Hanoi (VNU), 334, Nguyen Trai, Thanh Xuan, Hanoi, Viet Nam
| | - Tran Nghi
- University of Science, Vietnam National University, Hanoi (VNU), 334, Nguyen Trai, Thanh Xuan, Hanoi, Viet Nam
| | - Ngo Quang Toan
- Vietnam Association of Geology, 6, Pham Ngu Lao, Hanoi, Viet Namw
| | - Hoang Anh Khien
- Vietnam Association of Geology, 6, Pham Ngu Lao, Hanoi, Viet Namw
| | - Doan Dinh Lam
- Institute of Geology, 84, Chua Lang, Dong Da, Hanoi, Viet Nam
| | - Hoang Van Long
- Vietnam Petroleum Institute, 167, Trung Kinh, Yen Hoa, Cau Giay, Hanoi, Viet Nam
| | - Dinh Xuân Thanh
- University of Science, Vietnam National University, Hanoi (VNU), 334, Nguyen Trai, Thanh Xuan, Hanoi, Viet Nam
| | - Nguyen The Hung
- University of Science, Vietnam National University, Hanoi (VNU), 334, Nguyen Trai, Thanh Xuan, Hanoi, Viet Nam
| | - Nguyen Thị Huyen Trang
- University of Science, Vietnam National University, Hanoi (VNU), 334, Nguyen Trai, Thanh Xuan, Hanoi, Viet Nam
| | - Tran Ngọc Dien
- Vietnam Association of Geology, 6, Pham Ngu Lao, Hanoi, Viet Namw
| | - Nguyen Thị Tuyen
- University of Science, Vietnam National University, Hanoi (VNU), 334, Nguyen Trai, Thanh Xuan, Hanoi, Viet Nam
| | - Tran Xuan Truong
- Hanoi University of Natural Resources and Environment, 41A, Phu Dien str. Hanoi, Viet Nam
| | - Tran Thị Dung
- University of Science, Vietnam National University, Hanoi (VNU), 334, Nguyen Trai, Thanh Xuan, Hanoi, Viet Nam
| | - Nguyen Thi Phuong Thao
- University of Science, Vietnam National University, Hanoi (VNU), 334, Nguyen Trai, Thanh Xuan, Hanoi, Viet Nam
| | - Vu Quang Lan
- North Vietnam Geological Mapping Division, DGMV, Ai Mo, Gia Lam, Hanoi, Viet Nam
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Chang CC, Burr GS, Jull AJT, Russell JL, Biddulph D, White L, Prouty NG, Chen YG, Shen CC, Zhou W, Lam DD. Reconstructing surface ocean circulation with 129I time series records from corals. J Environ Radioact 2016; 165:144-150. [PMID: 27721136 DOI: 10.1016/j.jenvrad.2016.09.016] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/02/2016] [Revised: 09/28/2016] [Accepted: 09/28/2016] [Indexed: 06/06/2023]
Abstract
The long-lived radionuclide 129I (half-life: 15.7 × 106 yr) is well-known as a useful environmental tracer. At present, the global 129I in surface water is about 1-2 orders of magnitude higher than pre-1960 levels. Since the 1990s, anthropogenic 129I produced from industrial nuclear fuels reprocessing plants has been the primary source of 129I in marine surface waters of the Atlantic and around the globe. Here we present four coral 129I time series records from: 1) Con Dao and 2) Xisha Islands, the South China Sea, 3) Rabaul, Papua New Guinea and 4) Guam. The Con Dao coral 129I record features a sudden increase in 129I in 1959. The Xisha coral shows similar peak values for 129I as the Con Dao coral, punctuated by distinct low values, likely due to the upwelling in the central South China Sea. The Rabaul coral features much more gradual 129I increases in the 1970s, similar to a published record from the Solomon Islands. The Guam coral 129I record contains the largest measured values for any site, with two large peaks, in 1955 and 1959. Nuclear weapons testing was the primary 129I source in the Western Pacific in the latter part of the 20th Century, notably from testing in the Marshall Islands. The Guam 1955 peak and Con Dao 1959 increases are likely from the 1954 Castle Bravo test, and the Operation Hardtack I test is the most likely source of the 1959 peak observed at Guam. Radiogenic iodine found in coral was carried primarily through surface ocean currents. The coral 129I time series data provide a broad picture of the surface distribution and depth penetration of 129I in the Pacific Ocean over the past 60 years.
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Affiliation(s)
- Ching-Chih Chang
- NSF-Arizona AMS Laboratory, University of Arizona, Tucson, AZ 85721, USA; Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA.
| | - George S Burr
- NSF-Arizona AMS Laboratory, University of Arizona, Tucson, AZ 85721, USA; Department of Oceanography, National Sun Yat-Sen University, Kaohsiung, Taiwan
| | - A J Timothy Jull
- NSF-Arizona AMS Laboratory, University of Arizona, Tucson, AZ 85721, USA; Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA
| | - Joellen L Russell
- Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA
| | - Dana Biddulph
- NSF-Arizona AMS Laboratory, University of Arizona, Tucson, AZ 85721, USA
| | - Lara White
- NSF-Arizona AMS Laboratory, University of Arizona, Tucson, AZ 85721, USA
| | - Nancy G Prouty
- US Geological Survey Pacific Coastal & Marine Science Center, Santa Cruz, CA 95060, USA
| | - Yue-Gau Chen
- Department of Geosciences, National Taiwan University, Taipei, Taiwan
| | - Chuan-Chou Shen
- Department of Geosciences, National Taiwan University, Taipei, Taiwan
| | - Weijian Zhou
- Shaanxi Province Key Laboratory of Accelerator Mass Spectrometry Technology and Application, Institute of Earth Environment, CAS, Xi'an 710043, China
| | - Doan Dinh Lam
- Institute of Geology, Vietnamese Academy of Science and Technology, Hanoi, Viet Nam
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Shen CC, Wu CC, Liu Y, Yu J, Chang CC, Lam DD, Chou CJ, Lo L, Wei KY. Measurements of natural carbonate rare earth elements in femtogram quantities by inductive coupled plasma sector field mass spectrometry. Anal Chem 2011; 83:6842-8. [PMID: 21774547 DOI: 10.1021/ac201736w] [Citation(s) in RCA: 11] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Abstract
A rapid and precise standard-bracketing method has been developed for measuring femtogram quantity rare earth element (REE) levels in natural carbonate samples by inductively coupled plasma sector field mass spectrometry that does not require chemical separation steps. A desolvation nebulization system was used to effectively reduce polyatomic interference and enhance sensitivity. REE/Ca ratios are calculated directly from the intensities of the ion beams of (46)Ca, (139)La, (140)Ce, (141)Pr, (146)Nd, (147)Sm, (153)Eu, (160)Gd, (159)Tb, (163)Dy, (165)Ho, (166)Er, (169)Tm, (172)Yb, and (175)Lu using external matrix-matched synthetic standards to correct for instrumental ratio drifting and mass discrimination. A routine measurement time of 3 min is typical for one sample containing 20-40 ppm Ca. Replicate measurements made on natural coral and foraminiferal samples with REE/Ca ratios of 2-242 nmol/mol show that external precisions of 1.9-6.5% (2 RSD) can be achieved with only 10-1000 fg of REEs in 10-20 μg of carbonate. We show that different sources for monthly resolved coral ultratrace REE variability can be distinguished using this method. For natural slow growth-rate carbonate materials, such as sclerosponges, tufa, and speleothems, the high sample throughput, high precision, and high temporal resolution REE records that can be produced with this procedure have the potential to provide valuable time-series records to advance our understanding of paleoclimatic and paleoenvironmental dynamics on different time scales.
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Affiliation(s)
- Chuan-Chou Shen
- High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei, Taiwan 106, R.O.C.
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