Time correlation between MIS5a transgression and global sea level change of the second Marine layer in the coastal lowland of Bohai Bay
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摘要:
研究目的 渤海湾地区第II海相层的形成时代仍存争议，制约着该地区海平面变化研究进展。本研究对该层进行光释光定年，以期标定准确的地层年代及对应的海侵期次。
研究方法 以渤海湾西岸CZ80、CZ85、CZ66钻孔为研究对象，在岩心沉积结构、构造及有孔虫丰度，沉积微相研究基础上，识别出了第II海相层，并建立了第II海相层对比剖面。通过光释光测年方法对该地层的形成时代进行了准确测定，进一步讨论第II海相层的发育时间与全球海平面变化关系。
研究结果 CZ80、CZ85及CZ66孔在全新统（含第I海相层）以下均钻遇到了第II海相层，海相层底板埋深在35~33 m，对应黄海高程−31.13~−28.39 m，顶板埋深32~20 m，高程−25.58~−15.39 m。光释光测年结果表明第II海相层所对应的海侵事件发育时间约为94~71 ka。
结论 光释光测年结果表明，该区第II海相层始于94 ka或更早，海水影响在距今约71 ka结束。对比全球海面曲线，第II海相层时空特征与MIS5a阶段相符，记录了MIS5a阶段海侵事件。
Abstract:This paper is the result of coastal geological survey engineering.
Objective The second marine layer in the coastal lowland of Bohai Bay remains controversial, which restricts the progress of sea level change research in this area. This study performs optically stimulated luminescence dating on this layer, expecting to calibrate the precise stratigraphic age and the corresponding marine transgression episodes.
Methods By taking the CZ80, CZ85, and CZ66 boreholes on the west coast of the Bohai Bay as the research targets, based on the examination of sedimentary structures, textures and foraminifera abundance in the cores and sedimentary microfacies, the second marine layer was identified, and a comparative profile of the second marine layer was constructed. The formation age of this layer was precisely determined through the optically stimulated luminescence dating method, and the relationship between the development duration of the second marine layer and global sea level changes was further explored.
Results The CZ80, CZ85, and CZ66 boreholes all intersected the second marine layer beneath the Holocene stratum (including the first marine layer). The base of the marine layer was embedded at a depth ranging between 35 and 33 meters, corresponding to the elevation ranging from −31.13 to −28.39 meters in the Yellow Sea. The top of the marine layer was buried within a depth range of 32 to 20 meters, with an elevation varying from −25.58 to −15.39 meters. The optically stimulated luminescence dating outcomes reveal that the occurrence time of the marine transgression event corresponding to the second marine layer was approximately 94 to 71 ka.
Conclusions The optically stimulated luminescence (OSL) dating outcomes reveal that the second marine layer in this region commenced at 94 ka or earlier, and the influence of seawater terminated approximately 71 ka ago. Through comparison with the global sea−level curve, the spatio−temporal attributes of the second marine layer are consistent with the MIS5a stage, chronicling the marine transgression event during the MIS5a stage.
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图 4 CZ80、CZ85和CZ66孔第II海相层与全球海面时空对比图（全球海面变化曲线据Waelbroeck et al., 2002; Rohling et al., 2010; Yokoyama and East, 2011; Elderfield et al., 2012; Pico et al., 2016; Dutton and Barlow, 2019）
Figure 4.
表 1 钻孔信息表
Table 1. List of boreholes CZ80, CZ85 and CZ66
钻孔编号 孔深
/m坐标 孔口黄海
高程/mCZ80 40 38°26′12″N 116°53′39″E +6.42 CZ85 40 38°28′09″N 117°01′10″E +4.61 CZ66 40 38°31′29″N 117°07′59″E +3.87 
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表 2 AMS 14C测年材料和结果
Table 2. Materials for AMS 14C dating and results
野外编号 实验室编号 深度/m 高程/m 测年材料 δ13C/‰ 惯用年龄/BP 校正年龄/(a cal BP) 2σ 概率 CZ80-14C-11 403411 13.84 −7.42 泥炭 −24.6 7300 ± 30 8175~8029 1 CZ85-14C-4 399722 12.65 −9.04 泥炭 −28 7270 ± 30 8165~8015 1 CZ66-14C-15 399718 13.63 −9.76 泥炭 −27.6 7670 ± 30 8523~8406 0.955
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表 3 钻孔沉积物样品光释光测年结果
Table 3. OSL dating results of boreholes
样品编号 深度/m 测片 U/10−6 Th/10−6 K/% 含水/% 等效剂量/Gy 剂量率/(Gy/ka) 年龄/ka CZ80-6 27.4 14/28 1.14±0.06 5.69±0.19 1.93±0.06 13 180.52±39.61 2.31 ±0.05 78.1 ±17.2 CZ80-7 32.58 12/28 1.70±0.08 8.20±0.25 1.97±0.06 16 205.40±23.97 2.56 ±0.05 80.3 ±9.5 CZ80-8 35.5 9/14 2.94±0.11 13.3±0.36 2.18±0.06 22 259.26±48.20 3.64 ±0.17 71.3 ±13.7 CZ80-10 40.35 6/14 1.91±0.08 9.01±0.26 1.84±0.06 18 224.89±26.87 2.85 ±0.12 79.0 ±10.0 CZ85-4 19.51 10/14 2.35±0.09 13.4±0.36 2.20±0.06 22 199.96±41.60 3.52 ±0.16 56.8 ±12.1 CZ85-7 25.45 18/28 2.28±0.09 11.0±0.31 1.93±0.06 17 196.55±42.82 3.22 ±0.15 61.0 ±13.6 CZ85-11 31.4 19/28 2.14±0.09 12.0±0.34 2.18±0.06 25 256.38±17.12 3.21 ±0.14 79.8 ±6.3 CZ85-15 35.4 16/28 2.82±0.11 16.6±0.45 2.25±0.07 26 320.80±49.15 3.76 ±0.18 85.2 ±13.7 CZ66-3 20.73 13/14 1.92±0.08 11.8±0.33 2.04±0.06 18 203.06±22.94 2.85 ±0.05 71.4 ±8.2 CZ66-6 27.4 11/28 2.33±0.09 12.2±0.34 2.03±0.06 25 271.19±41.19 3.17 ±0.14 85.4 ±13.5 CZ66-10 31.55 11/28 2.41±0.10 13.3±0.36 2.42±0.07 33 273.60±35.80 3.33±0.14 82.3 ±11.3 CZ66-15 37.27 11/42 2.02±0.08 9.53±0.28 1.73±0.06 19 347.29±37.59 2.81±0.13 123.6±14.5
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