| 渤海湾全新世贝壳堤与牡蛎礁:古气候与海面变化 |
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| 引用本文： | 王 宏,陈永胜,田立柱,李建芬,裴艳东,王 福,商志文,范昌福,姜兴钰,苏盛伟,王海峰.渤海湾全新世贝壳堤与牡蛎礁:古气候与海面变化[J].地质通报,2011,30(9):1405-1411. |
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| 作者姓名： | 王 宏 陈永胜 田立柱 李建芬 裴艳东 王 福 商志文 范昌福 姜兴钰 苏盛伟 王海峰 |
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| 作者单位： | 1. 中国地质调查局天津地质调查中心,天津 300170; 2. 吉林大学地球科学学院,吉林 长春 130061;
3. 中国地质科学院矿产资源研究所,北京 100037; 4. 中国地质大学海洋学院,北京 100083 |
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| 基金项目： | 国家自然科学基金项目《海面升高与气温上升的耦合与非耦合关系》(批准号:40742011);《渤海湾西北岸埋藏牡蛎礁记录的中全新世古环境变化》(批准号:40872106); 中国地质调查局项目《泥质海岸带对全球变化的响应与趋势预测》(编号:1212010911069) |
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| 摘 要： | 讨论了早全新世晚期以来渤海湾西岸贝壳堤平原成堤、西北岸牡蛎礁平原(及毗邻浅海区)建礁过程的同时性特征和气候变化与这一特征之间的关系,以及堤、礁记录的相对海面变化。堤、礁大致同时发育,可分为6期,依次分别被寒冷事件5、4、3、2和1分隔。堤底板前、后缘高差大致对应3m的大潮差、礁顶板大致对应海平面。据二者分别重建了南部贝壳堤平原、北部牡蛎礁平原的相对海面变化:南部自7ka cal BP以来基本与现代海平面等高,小的波动在±1m之间,压实固结作用抵消了中全新世的相对高海面;北部中全新世的相对海平面位置因新构造和固结压实双重下沉作用的影响,已位于现代海平面2~3m以下。
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| 关 键 词： | 贝壳堤 牡蛎礁 气候变化 相对海面变化 渤海湾 |
Holocene cheniers and oyster reefs in Bohai Bay: palaeoclimate and sea level changes |
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| WANG Hong,CHEN Yong-sheng,TIAN Li-zhu,LI Jian-fen,PEI Yan-dong,WANG Fu,SHANG Zhi-wen,FAN Chang-fu,JIANG Xing-yu,SU Sheng-wei,WANG Hai-feng.Holocene cheniers and oyster reefs in Bohai Bay: palaeoclimate and sea level changes[J].Geologcal Bulletin OF China,2011,30(9):1405-1411. |
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| Authors: | WANG Hong CHEN Yong-sheng TIAN Li-zhu LI Jian-fen PEI Yan-dong WANG Fu SHANG Zhi-wen FAN Chang-fu JIANG Xing-yu SU Sheng-wei WANG Hai-feng |
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| Institution: | 1. Tianjin Center of China Geological Survey (CGS), Tianjin 300170, China;
2. College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China;
3. Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;
4. School of Marine Sciences, China University of Geosciences, Beijing 100083, China |
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| Abstract: | This paper deals with the synchronous characteristics of cheniers existing on the Chenier Plain along the west coast of Bohai Bay and oyster reefs existing on the Oyster Reef Plain of northwest Bohai Bay and its adjacent shallow sea. Approximately, such synchronous processes can be separated into six periods, alternately intercalated with the Holocene cold events of 5, 4, 3, 2 and 1. The vertical range between front-foot and rear-base of the chenier-bottom corresponds to the vertical 3m contemporaneous high tidal range, and the reef top approximately reflects the MSL (mean sea level). Since 7ka cal BP, the relative sea level trend in the Chenier Plain has been quite similar to the present situation, with possible small fluctuations being less than ±1m. The Mid-Holocene high stand of the relative sea level was offset by sedimentary consolidation. However, under the joint influences of neotectonic subsidence and consolidation, the relative MSL was 2~3m below the present sea level on the Oyster Reef Plain. |
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| Keywords: | cheniers oyster reefs climate change relative sea level change Bohai Bay |
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