Geochemical and clay mineral characteristics of the Holocene sediments on the west coast of Bohai Bay and their implications for environmental and climatic changes
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摘要:
通过对渤海湾西岸BXZK11孔沉积物黏土矿物、地球化学元素组分、粒度分析以及AMS14C年代测定并与研究区周边6个具有较好年龄控制的钻孔剖面对比，结合黏土矿物蒙脱石/（伊利石+绿泥石）比值以及元素Al/Si和Al/Na比值对气候变化的响应，探讨了渤海湾西岸地区全新世以来沉积环境以及气候变化过程。结果表明，末次盛冰期到8830 cal. aBP，海平面快速上升，海水临近研究区，沉积物以黄河古河道沉积为主，气候温凉略湿；8830～6255 cal. aBP，海侵范围达到最大，研究区主要为潮坪-浅海环境，气候温暖湿润；6255～3650 cal. aBP，海平面逐渐降低，沉积环境为前三角洲沉积，沉积物为黄河三角洲的一期超级叶瓣，气候转为温凉稍湿；3650～2780 cal. aBP，海平面趋于稳定，三角洲不断进积，为三角洲前缘环境，气候向凉干方向变化；2780 cal. aBP至今，古黄河三角洲不断进积，该区变成三角洲平原环境，气候凉干与现今相似。
Abstract:Based on the data of clay mineralogy, element geochemistry, grain size and AMS14C dating from the core of BXZK11 collected from the west coast of Bohai Bay and the correlation made with six well dated core profiles surrounding the study area, in addition to the smectite/(illite+chlorite) ratio, Al/Si ratio and Al/Na ratio analysis results, the sedimentary environmental and climatic changes since the beginning of Holocene are discussed for the region in this paper. The results suggest that owing to the rapid sea level rising during the period from the Last Glacial Maximun to 8830 cal. aBP, the sea water was quite close to the study area, the sedimentary environment had been dominated by the paleo-channel of the Yellow River, and a cool and slightly humid climate. During the period of 8830 to 6255 cal. aBP when the transgression reached its peak, the study area had been dominated by tidal flat and shallow sea and a warm and humid climate. From 6255 cal. aBP to 3650 cal. aBP, as the sea level was gradually dropping, this area had been occupied by a prodelta deposit, as one of the super lobes of the Yellow River Delta, under a cool and slightly humid climate. In the period from 3650 to 2780 cal. aBP, the sea level had remained stable to keep the delta continuously progradating as a delta front, while the climate changed to cool and dry. Since 2780 cal. aBP, the ancient Yellow River Delta has been continuously expanding, and the study area become a wide deltaic plain and the climate is cool and dry, similar to that of the present.
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Key words:
- clay minerals /
- geochemistry /
- sedimentary environment /
- Holocene /
- the west coast of Bohai Bay
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表 1 BXZK11孔14C年代测试数据
Table 1. AMS 14C dating of core BXZK11
样品编号 实验室编号 深度/m 材料 δ13C/‰ 惯用年龄/aBP 校正年龄/cal. aBP 中值 范围（1σ） BXZK11S1 462377 6.1 Potamocorbula laevis −2 2700±30 2640 2568～2730 BXZK11S5 485924 6.58 Potamocorbula ustulata −1.5 3400±30 3475 3400～3543 BXZK11S6 485925 7.76 Estellarca olivacea −1.7 3540±30 3640 3555～3716 BXZK11S4 470414 10.3 Nassarius sp. −2.5 3580±30 3695 3609～3776 BXZK11S2 462378 14.95 Anomia sp. 0.7 5660±30 6255 6190～6306 BXZK11S3 462379 16.6 植物碎屑 −27.9 7950±30 8830 8717～8975 
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