Sedimentary Evolution and Transgressions of the Western Subei Basin in Eastern China since the Late Pliocene
Sedimentary Evolution and Transgressions of the Western Subei Basin in Eastern China since the Late Pliocene
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中国东部苏北盆地西部晚上新世以来沉积演化与海侵
DOI：
10.1111/1755-6724.13774
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发表时间：
2019-02
期刊：
影响因子：
--
通讯作者：
LIN Jingxing
中科院分区：
文献类型：
--
作者：
CHENG Yu;LI Xiangqian;SHU Junwu;BAI Shibiao;ZHAO Zengyu;ZHANG Xiangyun;GUO Gang;ZHANG Ping;LIN Jingxing
苏北盆地沉积序列复杂，自晚上新世以来受到黄河、淮河、长江等海洋与河流相互作用的影响。这种沉积演化，特别是更新世海侵的时间，由于缺乏精确的年代证据，长期以来一直是一个有争议的问题。通过对苏北盆地TZK9岩心中有孔虫和介形虫的粒度、粒度综合分析，结合磁地层学、AMS14C和光致发光（OSL）的年代学研究，探讨该地区过去3.00 Ma沉积环境的演化。结果表明：该区沉积环境为3.00 ~ 1.01 Ma的河流相。在1.01 ~ 0.25 Ma期间有6个海平面高林分。研究区自0.25 Ma以来受4次大规模海侵的影响。在MIS7 （210 ~ 250 ka）、MIS5、MIS3和全新世分别记录了4个海相沉积层DU7（埋藏深度48 ~ 52 m）、DU5（埋藏深度35 ~ 41 m）、DU3（埋藏深度16 ~ 23 m）和DU1（埋藏深度2 ~ 4 m）。DU5海侵的强度与DU3海侵相同，均大于DU7海侵，其中DU1海侵最弱。海侵强度的变化反映了全球海平面变化、构造沉降、壳脊和沙坝的影响。在TZK9岩心中，我们发现了早-中更新世的7个海平面高林的证据，第一个海平面高林是由区域快速沉降引起的，可以追溯到0.83 ~ 0.84 Ma。上述第一次记录的海平面高度和年龄与中国东部其他岩心不同，这是由于缺乏绝对的年龄控制和古地形的差异造成的。该研究重建了沉积演化，确定了海侵及其年代，建立了晚上新世以来的年代学，为进一步的古环境和构造研究提供了科学框架。研究结果强调了局部构造和全球海平面在苏北盆地西部沉积演化和海侵过程中的重要作用。
Sedimentary sequences in the Subei Basin are complex and have been affected by interactions between the ocean and rivers since the Late Pliocene, including the Yellow River, Huaihe River, and the Yangtze River. This sedimentary evolution, in particular the timing of Pleistocene transgressions, has long been a matter of controversy owing to the lack of precise chronological evidence. The aim of this study is to explore the evolution of the sedimentary environment throughout the past 3.00 Ma in this region on the basis of a comprehensive analysis of particle size and foraminifera and ostracods collected in the TZK9 core from the Subei Basin combined with geochronological studies of magnetostratigraphy, AMS14C and optically stimulated luminescence (OSL). The results show that fluvial facies in the sedimentary environment from 3.00 to 1.01 Ma. There were fluvial facies and reflects six sea‐level high stands from 1.01 to 0.25 Ma. The study area was affected by four large‐scale transgressions since 0.25 Ma. The four marine sedimentary layers known as DU7 (buried at 48–52 m), DU5 (buried at 35–41 m), DU3 (buried at 16–23 m), and DU1 (buried at 2–4 m) are recorded in the MIS7 (210–250 ka), MIS5, MIS3, and Holocene, respectively. The magnitude of the DU5 transgression was identical to that of the DU3 transgression, both were larger than the DU7 transgression, and the DU1 transgression was the weakest. The variation of transgression strength reflects the influence of global changes in sea level, tectonic subsidence, shell ridges, and sand dams. In the TZK9 core, we found evidence of seven sea‐level high stands from the Early–Middle Pleistocene, and the first one caused by regional rapid subsidence and could be traced back to 0.83‐0.84 Ma. The sea‐level high stands and the age of the first one recorded above was different from other cores in eastern China, this was caused by the lack of absolute age control and the differences in paleotopography during this period. This study reconstructs sedimentary evolution, determines the transgression and its age, establishes the chronology since the Late Pliocene, and provides a scientific framework for further paleoenvironmental and tectonic studies. The results of this study highlight the important role that local tectonics and global sea level play in the sedimentary evolution and transgressions that have occurred in the western Subei Basin.
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影响因子：
1.4
作者：
Wang Qian;L. Fenglin;Liu Yude;Gao Xiulin
通讯作者：
Wang Qian;L. Fenglin;Liu Yude;Gao Xiulin
DOI：
--
发表时间：
2004
期刊：
Marine Geology & Quaternary Geology
影响因子：
--
作者：
Wang Zhang-hua;M. Key
通讯作者：
Wang Zhang-hua;M. Key
DOI：
10.1111/1755-6724.13319
发表时间：
2017-06
期刊：
Acta Geologica Sinica ‐ English Edition
影响因子：
--
作者：
Yumao Pang;Xun-hua Zhang;Guolin Xiao;Xing-Wei Guo;Zhenhe Wen;Zhiqiang Wu;Xiaoqing Zhu
通讯作者：
Yumao Pang;Xun-hua Zhang;Guolin Xiao;Xing-Wei Guo;Zhenhe Wen;Zhiqiang Wu;Xiaoqing Zhu
中更新世以来黄海暖流和黄海冷水团的演化
DOI：
10.1016/j.palaeo.2015.11.018
发表时间：
2016-01
期刊：
Palaeogeography, Palaeoclimatology, Palaeoecology
影响因子：
--
作者：
Mei Xi;Li Rihui;Zhang Xunhua;Liu Qingsong;Liu Jianxing;Wang Zhongbo;Lan Xianhong;Liu Jian;Sun Rongtao
通讯作者：
Sun Rongtao
中国长江三角洲平原南部沿海沉积物记录的 OIS 3 海平面上升
影响因子：
2.3
作者：
Jones, Brian G.;Chen, Ting;Zhao, Baocheng;Zhan, Qing
通讯作者：
Zhan, Qing