Mangrove development and its response to environmental change in Yingluo Bay (SW China) during the last 150years: Stable carbon isotopes and mangrove pollen | |
Xia, Peng1; Meng, Xianwei1,2; Li, Zhen3; Feng, Aiping1; Yin, Ping4; Zhang, Yongqiang1 | |
刊名 | Organic Geochemistry
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2015 | |
卷号 | 85页码:32-41 |
关键词 | Barium compounds Biogeochemistry Biological materials Carbon Correlation methods Ecosystems Forestry Isotopes Organic carbon Sea level |
ISSN号 | 01466380 |
DOI | 10.1016/j.orggeochem.2015.04.003 |
英文摘要 | Located at the interface of terrestrial and marine ecosystems, mangroves are particularly sensitive to environmental change. They provide a sedimentary sink for organic carbon, whereby cores can provide detailed records of mangrove species. We aimed to trace the history of mangrove development over the past 150years in Yingluo Bay, SW China. Sedimentation rates (avg. 0.32 and 0.37cm/year) were calculated on the basis of ln(210Pbex) vs. mass depth, and offset the rate of relative sea level rise (0.22-0.24cm/year), leading to a seaward expansion of new mangrove habitats. Chemical tracers (δ13Corgand C:N) and an isotope mixing model were utilized to trace the contribution of mangrove-derived organic matter (MOM). Changes in the relative abundance of pollen from mangrove plants was used to compensate for diagenetic alteration of the stable isotope values and potential overlaps in isotope values for different sources of organic matter. The result of Pearson correlation analysis showed that the MOM was moderately positive correlated with total mangrove pollen, indicating that stable carbon isotopes and mangrove pollen provide similar information for tracing mangrove ecosystems. Based on results from this study, compositional changes in mangrove communities could be divided into two main stages: a degradation period (1870-1930 AD) and a flourishing period (1930-2011 AD), corresponding to colder temperature and warmer temperature, respectively. Owing to the location being far away from any industrial area and human activity, temperature may be a key factor for mangrove development. © 2015 Elsevier Ltd. |
资助项目 | National Program on Key Basic Research Project of China (973 Program)[2010CB951203] |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | Elsevier Ltd |
WOS记录号 | WOS:000356617000004 |
内容类型 | 期刊论文 |
源URL | [http://ir.fio.com.cn/handle/2SI8HI0U/6682] ![]() |
专题 | 业务部门_海洋地质与地球物理研究室 |
作者单位 | 1.First Institute of Oceanography, State Oceanic Administration, Qingdao; 266061, China;; 2.Function Laboratory for Marine Geology, National Oceanography Laboratory, Qingdao; 266061, China;; 3.State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai; 200062, China;; 4.Qingdao Institute of Marine Geology, China Geological Survey, Qingdao; 266071, China |
推荐引用方式 GB/T 7714 | Xia, Peng,Meng, Xianwei,Li, Zhen,et al. Mangrove development and its response to environmental change in Yingluo Bay (SW China) during the last 150years: Stable carbon isotopes and mangrove pollen[J]. Organic Geochemistry,2015,85:32-41. |
APA | Xia, Peng,Meng, Xianwei,Li, Zhen,Feng, Aiping,Yin, Ping,&Zhang, Yongqiang.(2015).Mangrove development and its response to environmental change in Yingluo Bay (SW China) during the last 150years: Stable carbon isotopes and mangrove pollen.Organic Geochemistry,85,32-41. |
MLA | Xia, Peng,et al."Mangrove development and its response to environmental change in Yingluo Bay (SW China) during the last 150years: Stable carbon isotopes and mangrove pollen".Organic Geochemistry 85(2015):32-41. |
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