地理学报 ›› 2019, Vol. 74 ›› Issue (7): 1345-1362.doi: 10.11821/dlxb201907006
郭超1,2,蒙红卫3,马玉贞1(),李丹丹1,胡彩莉1,刘杰瑞1,雒聪文1,王凯1
收稿日期:
2018-01-24
修回日期:
2019-03-11
出版日期:
2019-07-25
发布日期:
2019-07-23
作者简介:
郭超(1988-), 男, 陕西人, 博士, 主要从事环境演变、孢粉学、元素地球化学等方面研究。E-mail: gc@mail.bnu.edu.cn
基金资助:
GUO Chao1,2,MENG Hongwei3,MA Yuzhen1(),LI Dandan1,HU Caili1,LIU Jierui1,LUO Congwen1,WANG Kai1
Received:
2018-01-24
Revised:
2019-03-11
Published:
2019-07-25
Online:
2019-07-23
Supported by:
摘要:
以青藏高原南部的羊卓雍错(简称羊湖)沉积岩芯为研究对象,以较可靠的年代数据( 210Pb和AMS 14C交叉定年)为框架,基于高分辨率的元素地球化学记录,通过数理统计分析方法提取环境信息,结合粒度和磁化率,重建该地区过去2000年来的环境变化。结果显示,该区黑暗时代冷期(DCAP)和小冰期(LIA)气候较为寒冷,降水量较高;而中世纪暖期(MWP)和现代暖期(CWP)气候较为温暖,降水量较低,气候具有冷湿—暖干的特征。其中,重建的温度显示,中世纪暖期的温暖程度似乎持平甚至超过20世纪暖期;小冰期期间可能存在一次百年尺度的温暖事件,而17世纪和18世纪可能是过去2000中最寒冷的一段时期。分析发现,过去2000年以来青藏高原南部存在着冷湿—暖干的气候模式;过去2000年青藏高原南部地区温度的变化可能主要受到太阳辐射的影响,而小冰期期间西风环流的南移和增强可能是导致区域降水增加的重要因素。另外,该时期羊湖的湖泊水位的变化受温度和降水共同控制:当温度降低,降水增加时,湖泊水位上升,反之亦然。
郭超,蒙红卫,马玉贞,李丹丹,胡彩莉,刘杰瑞,雒聪文,王凯. 藏南羊卓雍错沉积物元素地球化学记录的过去2000年环境变化[J]. 地理学报, 2019, 74(7): 1345-1362.
GUO Chao,MENG Hongwei,MA Yuzhen,LI Dandan,HU Caili,LIU Jierui,LUO Congwen,WANG Kai. Environmental variations recorded by chemical element in the sediments of Lake Yamzhog Yumco on the southern Tibetan Plateau over the past 2000 years[J]. Acta Geographica Sinica, 2019, 74(7): 1345-1362.
表2
羊湖岩芯主要元素的相关性分析结果
Al | Si | K | Ti | Rb | Fe | Cu | Zn | Pb | Br | Ca | Sr | |
---|---|---|---|---|---|---|---|---|---|---|---|---|
Si | 0.69** | |||||||||||
K | 0.68** | 0.91** | ||||||||||
Ti | 0.71** | 0.89** | 0.97** | |||||||||
Rb | 0.70** | 0.73** | 0.85** | 0.89** | ||||||||
Fe | 0.47** | 0.37** | 0.59** | 0.62** | 0.81** | |||||||
Cu | 0.40** | 0.22* | 0.32** | 0.42** | 0.66** | 0.74** | ||||||
Zn | 0.54** | 0.49** | 0.68** | 0.70** | 0.82** | 0.83** | 0.70** | |||||
Pb | 0.09 | -0.17 | 0.01 | 0.04 | 0.35** | 0.76** | 0.67** | 0.45** | ||||
Br | 0.04 | -0.29** | -0.1 | -0.06 | 0.18 | 0.59** | 0.56** | 0.33** | 0.86** | |||
Ca | -0.35** | -0.09 | -0.12 | -0.28** | -0.52** | -0.43** | -0.72** | -0.43** | -0.38** | -0.33** | ||
Sr | -0.29** | -0.04 | -0.08 | -0.24* | -0.45** | -0.39** | -0.64** | -0.36** | -0.36** | -0.33** | 0.95** | |
Y | 0.50** | 0.64** | 0.54** | 0.56** | 0.47** | 0.09 | 0.23* | 0.31** | -0.28** | -0.38** | -0.29** | -0.23* |
表3
羊湖岩芯主要元素的主成分得分
元素 | 主成分 | ||
---|---|---|---|
1 | 2 | 3 | |
Al | 0.747 | 0.122 | -0.223 |
Si | 0.948 | -0.101 | 0.052 |
K | 0.949 | 0.160 | 0.133 |
Ti | 0.947 | 0.172 | -0.038 |
Rb | 0.838 | 0.435 | -0.224 |
Y | 0.706 | -0.346 | -0.325 |
Fe | 0.485 | 0.838 | -0.098 |
Cu | 0.335 | 0.653 | -0.549 |
Zn | 0.643 | 0.604 | -0.130 |
Pb | -0.100 | 0.925 | -0.168 |
Br | -0.238 | 0.866 | -0.165 |
Ca | -0.196 | -0.305 | 0.898 |
Sr | -0.138 | -0.292 | 0.870 |
方差贡献(%) | 47.301 | 23.763 | 11.850 |
累积方差贡献(%) | 47.301 | 71.064 | 82.914 |
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