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DOI | 10.1016/j.quascirev.2019.05.001 |
Holocene sea-level database for the Rhine-Meuse Delta; The Netherlands: Implications for the pre-8.2 ka sea-level jump | |
Hijma M.P.; Cohen K.M. | |
发表日期 | 2019 |
ISSN | 0277-3791 |
起始页码 | 68 |
结束页码 | 86 |
卷号 | 214 |
英文摘要 | This paper provides the most-accurate sea-level index points (SLIPs)for the Rhine-Meuse Delta (RMD), The Netherlands, identified amidst a wealth of data accumulated in sixty years of research. Following documented protocols, 106 selected radiocarbon dates from peat beds from transgressed valley floor, upper estuarine and back-barrier lagoonal settings were first listed individually, then screened in ensemble on quantified age-depth position and inshore palaeotidal setting. The database contains 50 SLIPs and 56 upper limiting data points spanning a depth range of −34 to −1.5 m. The dates in the database originate from dedicated sea-level research, which kept surface elevation and sampling depth uncertainty small, and sampling of basal-peat beds was favoured, keeping compaction uncertainties small too. The SLIPs cover an age-range of 8.8–3.0 ka BP and are available from Greater Rotterdam and its near offshore. For upper limiting data points, the coverage extends offshore, tracing the Rhine palaeovalley, and reaches back to 11.5 ka BP. The age-depth data density and spatial concentration of subsets of dates allow to perform Bayesian radiocarbon calibration and to reduce temporal uncertainty by 25% for the average sample (1σ age uncertainty ≈ 75 cal. yr), when depth position and rates of relative sea-level rise (RSLR)are used to assign sequence order. Between 8.0–4.5 ka BP, rates of RSLR gradually decreased from 9 to 1 mm/yr. In the millennium before, rates of RSLR were much higher, on average 10 mm/yr, and marked by a sea-level jump between 8.45–8.2 ka BP. A two-phased nature of this jump starts to be resolved, with local magnitudes of 1.7 ± 0.6 m (1σ, first phase)and 0.2 ± 0.2 m (second phase), corresponding to globally-averaged jumps of 2.5 m ± 0.9 m for the first and 0.3 ± 0.3 m for the second phase. For the pre-9 ka BP period, only offshore upper limiting data points are currently available. Until new offshore data are gathered, trends of RSLR before 9 ka BP can only be estimated, fed with global insights in post-glacial eustasy, regional estimates regarding rates of glacio-isostatic adjustments and tectonic subsidence, and sedimentary geological interpretations of scattered basal-peat presence. © 2019 Elsevier Ltd |
英文关键词 | Europe; Holocene; Netherlands; Radiogenic isotopes; Rhine-Meuse; Sea-level changes; Sea-level jump |
语种 | 英语 |
scopus关键词 | Database systems; Offshore oil well production; Peat; Europe; Holocenes; Netherlands; Radiogenic isotopes; Rhine-Meuse; Sealevel change; Sea level; calibration; coastal lagoon; concentration (composition); database; glacioeustacy; Holocene; isotopic analysis; paleoenvironment; Postglacial; radiocarbon dating; sampling; sea level change; uncertainty analysis; Netherlands; Rhine-Meuse Delta; Rotterdam; South Holland |
来源期刊 | Quaternary Science Reviews
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/151921 |
作者单位 | Deltares Research Institute, Dept. of Applied Geology and Geophysics, Utrecht, Netherlands; Utrecht University, Dept. of Physical Geography, Utrecht, Netherlands |
推荐引用方式 GB/T 7714 | Hijma M.P.,Cohen K.M.. Holocene sea-level database for the Rhine-Meuse Delta; The Netherlands: Implications for the pre-8.2 ka sea-level jump[J],2019,214. |
APA | Hijma M.P.,&Cohen K.M..(2019).Holocene sea-level database for the Rhine-Meuse Delta; The Netherlands: Implications for the pre-8.2 ka sea-level jump.Quaternary Science Reviews,214. |
MLA | Hijma M.P.,et al."Holocene sea-level database for the Rhine-Meuse Delta; The Netherlands: Implications for the pre-8.2 ka sea-level jump".Quaternary Science Reviews 214(2019). |
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