地理科学 ›› 2016, Vol. 36 ›› Issue (3): 448-457.doi: 10.13249/j.cnki.sgs.2016.03.017
舒培仙1,2(), 李保生1,2(
), 牛东风1, 王丰年3, 温小浩1, 司月君4, 陈琼1
收稿日期:
2014-12-05
修回日期:
2015-03-16
出版日期:
2016-03-20
发布日期:
2016-03-20
作者简介:
舒培仙(1990-),男,安徽宣城人,博士研究生,主要研究方向为地表过程与第四纪环境演变。E-mail:
基金资助:
Peixian Shu1,2(), Baosheng Li1,2(
), Dongfeng Niu1, Fengnian Wang3, Xiaohao Wen1, Yuejun Si4, Qiong Chen1
Received:
2014-12-05
Revised:
2015-03-16
Online:
2016-03-20
Published:
2016-03-20
Supported by:
摘要:
分析滴哨沟湾剖面全新统DGS1段的粒度数据,认为流动沙丘砂、泥炭、砂质古土壤、古固定-半固定沙丘砂到湖沼相和次生黄土的颗粒总体上变细,分选变差。结合腹足类动物化石和湖沼相地层中石英砂粒表面电镜扫描,认为DGS1粒度结果实际上是全新世以来多次冬夏季风的交互演替过程的气候-地质记录。据此,将DGS1粒度信号记录的全新世气候分为4个阶段——全新世早期好转期、全新世鼎盛期、大暖期向寒冷期转变波动期和降温不稳定的沙漠化频繁变化时期。
中图分类号:
舒培仙, 李保生, 牛东风, 王丰年, 温小浩, 司月君, 陈琼. 毛乌素沙漠东南缘滴哨沟湾剖面DGS1层段粒度特征及其指示的全新世气候变化[J]. 地理科学, 2016, 36(3): 448-457.
Peixian Shu, Baosheng Li, Dongfeng Niu, Fengnian Wang, Xiaohao Wen, Yuejun Si, Qiong Chen. Climate Variations Recorded by the Grain-size from the DGS1 Segment in the Southeast of China′s Mu Us Desert During the Holocene[J]. SCIENTIA GEOGRAPHICA SINICA, 2016, 36(3): 448-457.
表2
DGS1层段各沉积相粒度参数特征分布"
沉积相(样品数) | 特征参数 | Mz(?) | σ1(?) | SK1 | KG |
---|---|---|---|---|---|
流动沙丘砂(37) | 平均值 | 2.55 | 0.97 | 0.29 | 1.43 |
范围 | 2.21~3.36 | 0.51~1.68 | 0.01~0.45 | 0.94~1.70 | |
固定半固定沙丘砂(22) | 平均值 | 3.89 | 1.76 | 0.32 | 1.03 |
范围 | 2.27~5.12 | 0.53~2.51 | 0.02~0.51 | 0. 92~1.24 | |
古土壤(25) | 平均值 | 2.58 | 1.00 | 0.34 | 1.42 |
范围 | 2.4~2.87 | 0.81~1.25 | 0.23~0.43 | 1.28~1.61 | |
次生黄土(19) | 平均值 | 4.58 | 1.46 | 0.36 | 1.44 |
范围 | 4.25~5.27 | 1.15~2.10 | 0.22~0.38 | 1.22~1.51 | |
湖沼相(111) | 平均值 | 4.28 | 2.13 | 0.32 | 1.13 |
范围 | 2.33~6.38 | 0.81~3.25 | 0.09~0.53 | 0.65~1.80 | |
泥炭(20) | 平均值 | 2.54 | 0.71 | 0.14 | 1.07 |
范围 | 2.33~3.47 | 0.53~1.69 | 0.03~0.51 | 0.94~1.74 | |
全剖面(234) | 平均值 | 3.67 | 1.62 | 0.31 | 1.22 |
范围 | 2.21~6.38 | 0.52~3.25 | 0.01~0.53 | 0.65~1.80 |
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