雷州半岛南部湖相沉积揭示的全新世早中期气候环境演变

汤文坤; 王永; 董进; 田飞; 刘瑾; 江南

雷州半岛南部湖相沉积揭示的全新世早中期气候环境演变

中国地质科学院地质研究所, 北京 100037

基金项目:
中国地质调查局项目《中国东部第四纪晚期地层序列与环境演变调查》（编号：121201102000150010-07）

详细信息

作者简介: 汤文坤(1992-), 男, 在读硕士生, 第四纪地质与环境专业。E-mail:wenkuntang@foxmail.com

通讯作者: 王永(1968-), 男, 博士, 研究员, 从事第四纪地质和新构造研究。E-mail:wangyong@cags.ac.cn

中图分类号: P534.63⁺2

收稿日期: 2016-07-26

修回日期: 2017-01-24

刊出日期: 2017-09-25

Early-Middle Holocene paleoenvironmental evolution revealed by a la-custrine sediment sequence in Leizhou Peninsula

Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

More Information

Corresponding author: WANG Yong, wangyong@cags.ac.cn

Received Date: 26 July 2016

Revised Date: 24 January 2017

Publish Date: 25 September 2017

摘要

摘要:
对雷州半岛南部徐闻县九亩村一段1.54m厚的湖相沉积剖面进行粒度、磁化率、色度及有机碳氮分析，结合AMS¹⁴C测年结果，重建了该地区10.5~6.5cal ka BP的气候环境变化。共分为3个阶段：①10.5~9.5cal ka BP，湖泊水体较浅，气候较干燥；②9.5~7.2cal ka BP，湖泊水位较高，环境稳定，气候较湿润；③7.2~6.5cal ka BP，湖水相对变浅，气候相对阶段②干燥。雷州半岛地区降水变化与印度季风演变模式一致，可与北半球夏季平均太阳辐射及其影响下热带辐合带（ITCZ）的移动进行对比，指标时间序列的红外噪声谱分析结果表明，存在千年-百年的准周期，反映了研究区气候环境变化对太阳活动的响应。
- 雷州半岛 /
- 全新世早中期 /
- 环境变化
Abstract:
This study presents the record of paleoenvironmental evolution results from a radiocarbon-dated 1.54m-long lacustrine sediment sequence in south Leizhou Peninsula. Measurement of grain size, magnetic susceptibility (MS), total nitrogen (TN), total or-ganic carbon (TOC), atomic TOC/TN (C/N) and color reflectance values was carried out in order to reconstruct the climate span-ning the interval 10.5~6.5cal ka BP. Three distinct stages can be identified as follows:①10.5~6.5 cal ka BP, a shallow lake level and relatively dry climate dominated this area. ②The interval from 9.5~7.2cal ka BP was characterized by a relatively high lake level and humid climate. ③During 7.2~6.5cal ka BP, lake level was relatively shallow with a relatively dry climate. Indian monsoon was more responsible for precipitation variability in this area, which was interconnected with average monthly solar radiation in summer and ITCZ migration. Red noise spectrum analysis of proxies shows centennial to millennia time scale cycles, which suggests that the envi-ronmental evolution was probably sensitive to the secular solar activity.
- Leizhou Peninsula /
- Early-Middle Holocene /
- paleoenvironmental evolution

HTML全文

图 1 研究区位置(a)、剖面位置（b, 据参考文献[26]修改）和剖面照片（c）

Figure 1.

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图 2 徐闻月平均气温与降水图（1981—2010年）^[32]

Figure 2.

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图 3 JM剖面沉积年龄与深度对应关系

Figure 3.

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图 4 JM剖面粒度组分及粒度参数

Figure 4.

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图 5 JM剖面色度、质量磁化率、TOC、TN及粒度组分

Figure 5.

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图 6 不同区域指标综合对比图

Figure 6.

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图 7 JM剖面亮度时间序列红色噪声谱分析

Figure 7.

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表 1 JM剖面沉积物¹⁴C测年结果

Table 1. AMS radiocarbon dates for JM section

样品编号	实验室编号	深度/cm	测年材料	¹⁴C年龄/a BP	校正年龄/cal a BP
13jm-3	Beta-416459	5~6	沉积物	5730±30	6445~6633
13jm-27	Beta-434636	53~54	沉积物	5940±30	6673~6851
13jm-50	Beta-434638	99~100	沉积物	7540±40	8325~8408
13jm-66	Beta-416461	131~132	沉积物	8610±30	9526~9655

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