压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡

夏鹏; 孟宪伟; 丰爱平; 李珍; 杨刚

doi:10.14027/j.cnki.cjxb.2015.03.013

ISSN 1000-0550 CN 62-1038/P

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压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡

夏鹏, 孟宪伟, 丰爱平, 李珍, 杨刚

文章导航 > 沉积学报 > 2015 > 33(3): 551-560

夏鹏, 孟宪伟, 丰爱平, 李珍, 杨刚. 压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡[J]. 沉积学报, 2015, 33(3): 551-560. doi: 10.14027/j.cnki.cjxb.2015.03.013

引用本文:

XIA Peng, MENG XianWei, FENG AiPing, LI Zhen, YANG Gang. Sediment Compaction Rates in Mangrove Swamps of Guangxi and Its Mangrove Migration Response to Sea-level Rise[J]. Acta Sedimentologica Sinica, 2015, 33(3): 551-560. doi: 10.14027/j.cnki.cjxb.2015.03.013

Citation:

XIA Peng, MENG XianWei, FENG AiPing, LI Zhen, YANG Gang. Sediment Compaction Rates in Mangrove Swamps of Guangxi and Its Mangrove Migration Response to Sea-level Rise[J]. Acta Sedimentologica Sinica, 2015, 33(3): 551-560. doi: 10.14027/j.cnki.cjxb.2015.03.013

引用本文:

Citation:

压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡

doi: 10.14027/j.cnki.cjxb.2015.03.013

1.
国家海洋局第一海洋研究所山东青岛 266061;
2.
华东师范大学河口海岸学国家重点实验室上海 200062

基金项目: 国家自然科学基金“广西英罗湾中全新世以来红树林演变的沉积物有机碳同位素和孢粉记录及其对气候变化的响应”(批准号:41206057)与中央级公益性科研院所基本科研业务费专项资金“近百年来人类活动影响下广西红树林生长发育的孢粉和稳定碳同位素记录”(编号:2012G18)联合资助

详细信息

通讯作者:
孟宪伟男研究员 E-mail:mxw@fio.org.cn

中图分类号: TE121.3

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Sediment Compaction Rates in Mangrove Swamps of Guangxi and Its Mangrove Migration Response to Sea-level Rise

1.
First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061;
2.
State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062

摘要

摘要: 气候变化造成的海平面上升是迫使红树林向陆迁移的主要驱动力, 而其自身通过捕沙促淤不同程度的减缓了海平面上升速率的影响。基于广西典型红树林区8根短柱的²¹⁰Pb测年和含水率分析, 以考虑/未考虑沉积物压实作用为研究情景, 通过对比研究红树林区潮滩地表高程抬升速率和相对海平面上升速率的大小关系, 揭示当前海平面上升对广西红树林向陆/向海迁移的驱动机制。研究发现:未考虑压实作用下的沉积速率约是考虑压实作用下沉积速率的1.00~1.34倍(平均1.12倍), 压实作用明显;压实沉积速率介于0.16~0.78 cm/a, 其底层压实沉积速率与潮滩地表高程抬升速率相等。压实作用下, 英罗湾和丹兜海红树林区的地表高程抬升速率小于相对海平面上升速率;与未考虑压实作用得到的结论相悖。由于广西红树林海岸大都建有防波堤, 限制了红树林向陆的迁移;表明英罗湾和丹兜海的红树林正面临海平面上升的威胁。压实作用校正与否对地表高程抬升速率与相对海平面上升速率相当的区域尤为重要。
- 红树林 /
- 沉积速率 /
- 压实作用 /
- 海平面上升 /
- 迁移
Abstract: Rising sea levels caused by climate change is the major driving force in landward migration of mangrove communities, and its overlying plants can slow down the rate of sea-level rise deriving from sediment trapping. In the paper, six sediment cores were collected from the typical mangrove swamps in Guangxi, China. Based on moisture contents and ²¹⁰Pb analysis, the average sedimentary rates were calculated using the CIC model in different cases of considering/no-considering sediment compaction. Compared between the rate of regional sea-level rise and the sedimentary rates, it reveals the relationship of landward mangrove migration in response to relative sea-level rise. The sediment compaction rates are between 0.16~0.78 cm/a, but no-considering sediment compaction rates are approximately 1.00~1.34 times (mean 1.12 times) more than the rates of sediment compaction. The sediment compaction rates are lower than the rate of regional sea-level rise in mangrove swamps of Yingluo Bay and Dandou Sea, however, the sediment compaction rates are obviously higher in the Maowei Sea. Owing to the seawall preventing the landward mangrove migration, the mangrove plants are currently under threat from sea-level rise in the Yingluo Bay and Dandou Sea. It is obviously different with previous reports. Taking no account of sediment compaction, the sediment rates were be overestimated in the recent studies.
- mangrove /
- sedimentary rate /
- sediment compaction /
- sea-level rise /
- migration

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参考文献(0)

[1]	刘涛, 褚冠宇, 徐慧鹏. 基于风暴潮记录研究红树林淤积速率时间变化 . 沉积学报, 2022, 40(5): 1346-1354. doi: 10.14027/j.issn.1000-0550.2021.042
[2]	林承焰, 王文广, 董春梅, 张宪国, 任丽华, 林建力. 砂岩压实作用研究现状及进展 . 沉积学报, 2020, 38(3): 538-553. doi: 10.14027/j.issn.1000-0550.2019.055
[3]	陈亮, 赵千慧, 王英民, 孙红军, 万琼华, 唐武, 赵鹏. 盐构造与深水水道的交互作用——以下刚果盆地为例 . 沉积学报, 2017, 35(6): 1197-1204. doi: 10.14027/j.cnki.cjxb.2017.06.011
[4]	宗娴, 石学法, 葛晨东, 邹建军, Sergey Gorbarenko, 乔淑卿, 董智. 日本海百年来沉积速率及粒度指示意义 . 沉积学报, 2016, 34(3): 516-522. doi: 10.14027/j.cnki.cjxb.2016.03.009
[5]	. 柴达木盆地西部北区新近系非常规低渗储集层特征及控制因素分析 . 沉积学报, 2013, 31(1): 157-166.
[6]	张瑞. 长江河口水下三角洲210Pb分布特征及其沉积速率 . 沉积学报, 2009, 27(4): 704-713.
[7]	薛春汀. 西汉末—北宋黄河三角洲（公元11～1099年）的沉积记录 . 沉积学报, 2008, 26(5): 804-812.
[8]	. 库车坳陷北部白垩系沉积速率分析 . 沉积学报, 2006, 24(05): 641-649.
[9]	刘国勇. 碎屑岩成岩压实作用模拟实验研究 . 沉积学报, 2006, 24(3): 407-413.
[10]	章伟艳, 张富元, 陈荣华, 张霄宇. 南海深水区晚更新世以来沉积速率、沉积通量与物质组成 . 沉积学报, 2002, 20(4): 668-674.
[11]	邓云山, 孟自芳, 郑彦鹏. 压实作用与磁倾角变化的实验研究 . 沉积学报, 2001, 19(2): 306-308.
[12]	吴智平, 周瑶琪. 一种计算沉积速率的新方法——宇宙尘埃特征元素法 . 沉积学报, 2000, 18(3): 395-399.
[13]	潘少明, 施晓冬, 王建业, PeterTanner, LaiShingLeong. 围海造地工程对香港维多利亚港现代沉积作用的影响 . 沉积学报, 2000, 18(1): 22-28.
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压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡

doi: 10.14027/j.cnki.cjxb.2015.03.013

1. 国家海洋局第一海洋研究所山东青岛 266061;

2. 华东师范大学河口海岸学国家重点实验室上海 200062

通讯作者: 孟宪伟男研究员 E-mail:mxw@fio.org.cn

收稿日期: 2014-01-09
修回日期: 2014-08-12
刊出日期: 2015-06-10

中图分类号: TE121.3

关键词:

红树林 /

摘要: 气候变化造成的海平面上升是迫使红树林向陆迁移的主要驱动力, 而其自身通过捕沙促淤不同程度的减缓了海平面上升速率的影响。基于广西典型红树林区8根短柱的²¹⁰Pb测年和含水率分析, 以考虑/未考虑沉积物压实作用为研究情景, 通过对比研究红树林区潮滩地表高程抬升速率和相对海平面上升速率的大小关系, 揭示当前海平面上升对广西红树林向陆/向海迁移的驱动机制。研究发现:未考虑压实作用下的沉积速率约是考虑压实作用下沉积速率的1.00~1.34倍(平均1.12倍), 压实作用明显;压实沉积速率介于0.16~0.78 cm/a, 其底层压实沉积速率与潮滩地表高程抬升速率相等。压实作用下, 英罗湾和丹兜海红树林区的地表高程抬升速率小于相对海平面上升速率;与未考虑压实作用得到的结论相悖。由于广西红树林海岸大都建有防波堤, 限制了红树林向陆的迁移;表明英罗湾和丹兜海的红树林正面临海平面上升的威胁。压实作用校正与否对地表高程抬升速率与相对海平面上升速率相当的区域尤为重要。

English Abstract

Sediment Compaction Rates in Mangrove Swamps of Guangxi and Its Mangrove Migration Response to Sea-level Rise

1. First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061;

2. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062

Received Date: 2014-01-09
Rev Recd Date: 2014-08-12
Publish Date: 2015-06-10

Keywords:

Abstract: Rising sea levels caused by climate change is the major driving force in landward migration of mangrove communities, and its overlying plants can slow down the rate of sea-level rise deriving from sediment trapping. In the paper, six sediment cores were collected from the typical mangrove swamps in Guangxi, China. Based on moisture contents and ²¹⁰Pb analysis, the average sedimentary rates were calculated using the CIC model in different cases of considering/no-considering sediment compaction. Compared between the rate of regional sea-level rise and the sedimentary rates, it reveals the relationship of landward mangrove migration in response to relative sea-level rise. The sediment compaction rates are between 0.16~0.78 cm/a, but no-considering sediment compaction rates are approximately 1.00~1.34 times (mean 1.12 times) more than the rates of sediment compaction. The sediment compaction rates are lower than the rate of regional sea-level rise in mangrove swamps of Yingluo Bay and Dandou Sea, however, the sediment compaction rates are obviously higher in the Maowei Sea. Owing to the seawall preventing the landward mangrove migration, the mangrove plants are currently under threat from sea-level rise in the Yingluo Bay and Dandou Sea. It is obviously different with previous reports. Taking no account of sediment compaction, the sediment rates were be overestimated in the recent studies.

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压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡

doi: 10.14027/j.cnki.cjxb.2015.03.013

通讯作者:
孟宪伟男研究员 E-mail:mxw@fio.org.cn

计量

Sediment Compaction Rates in Mangrove Swamps of Guangxi and Its Mangrove Migration Response to Sea-level Rise

计量

目录

压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡

doi: 10.14027/j.cnki.cjxb.2015.03.013

1. 国家海洋局第一海洋研究所山东青岛 266061;

2. 华东师范大学河口海岸学国家重点实验室上海 200062

通讯作者: 孟宪伟男研究员 E-mail:mxw@fio.org.cn

English Abstract

Sediment Compaction Rates in Mangrove Swamps of Guangxi and Its Mangrove Migration Response to Sea-level Rise

1. First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061;

2. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062

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压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡

doi: 10.14027/j.cnki.cjxb.2015.03.013

通讯作者: 孟宪伟 男 研究员 E-mail:mxw@fio.org.cn

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Sediment Compaction Rates in Mangrove Swamps of Guangxi and Its Mangrove Migration Response to Sea-level Rise

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压实作用下广西典型红树林区沉积速率及海平面上升对红树林迁移效应的制衡

doi: 10.14027/j.cnki.cjxb.2015.03.013

1. 国家海洋局第一海洋研究所 山东青岛 266061; 2. 华东师范大学河口海岸学国家重点实验室 上海 200062

通讯作者: 孟宪伟 男 研究员 E-mail:mxw@fio.org.cn

English Abstract

Sediment Compaction Rates in Mangrove Swamps of Guangxi and Its Mangrove Migration Response to Sea-level Rise

1. First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061; 2. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062

全文HTML

目录

友情链接

期刊在线

联系我们

通讯作者:
孟宪伟男研究员 E-mail:mxw@fio.org.cn

1. 国家海洋局第一海洋研究所山东青岛 266061;

2. 华东师范大学河口海岸学国家重点实验室上海 200062

通讯作者: 孟宪伟男研究员 E-mail:mxw@fio.org.cn

1. First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061;

2. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062