引用本文:	郭若舜,叶思源,何磊,赵俐红.全新世以来辽河三角洲地区的化学风化及其对气候变化的响应[J].海洋科学,2018,42(9):38-50.

【打印本页】【HTML】【下载PDF全文】【查看/发表评论】【下载PDF阅读器】【关闭】

过刊浏览高级检索

本文已被：浏览 1056次下载 768次	码上扫一扫！
分享到：微信更多字体:加大+\|默认\|缩小-
全新世以来辽河三角洲地区的化学风化及其对气候变化的响应
郭若舜^1,2, 叶思源^2,3, 何磊^2,3, 赵俐红¹
1.山东科技大学地球科学与工程学院, 山东青岛 266590;2.中国地质调查局滨海湿地生物地质重点实验室, 山东青岛 266071;3.青岛海洋地质研究所, 山东青岛 266071

摘要:

以辽河三角洲ZK2孔为研究对象，对其57件沉积物样品进行常量元素测试和分析。研究表明，该地区总体遭受的化学风化作用较弱，基本处于化学风化的初期阶段，与所处纬度整体化学风化特征类似。将该区全新世以来的气候变化过程分为如下5个阶段：全新世早期（11.0—8.8 cal ka BP）：化学风化程度逐渐增强，气候逐步向温湿方向发展；全新世早中期（8.8—6.9 cal ka BP）：化学风化程度最强，气候暖湿；全新世中期（6.9—4.6 cal ka BP）：风化强度较强，但有减弱的趋势，气候温湿；全新世中晚期（4.6—1.3 cal ka BP）：化学风化程度在该时期属于最弱阶段，气候冷干；全新世晚期（1.3 cal ka BP—至今）：气候温干，风化程度有所增强。总体来说，该区常量元素反映的气候变化过程与石笋δ¹⁸O曲线基本一致，揭示了常量元素在反演气候变化过程中有一定的作用。

关键词: 辽河三角洲常量元素风化指数化学风化气候变化

DOI：10.11759/hykx20180209002

分类号:P736.2

基金项目:科技部政府间科技创新合作重点专项（2016YFE0109600）；国家自然科学基金（41706057）

Chemical weathering and its implications regarding climate changes in the Liaohe Delta since the Holocene

GUO Ruo-shun^1,2, YE Si-yuan^2,3, HE Lei^2,3, ZHAO Li-hong¹

1.School of Earth Sciences and Engineering, Shandong University of Science and Technology, Qingdao 266590, China;2.Key Laboratory of Coastal Wetlands Biogeosciences, China Geological Survey, Qingdao 266071, China;3.Qingdao Institute of Marine Geology, Qingdao 266071, China

Abstract:

In this study, we analyzed a total of 57 samples with respect to the major elements in core ZK2 in the Liaohe Delta. The results of the research reveal that the chemical weathering of the region has been generally weak and remains in the early stage, which is similar to the overall chemical weathering characteristics observed at this latitude. We categorized the paleoclimate changes of this area into five stages since the Holocene as follows: (1) the Early Holocene (11.0–8.8 cal ka BP) during which the intensity of the chemical weathering was gradually enhanced and the climate gradually transformed into warm-wet conditions; (2) the Early and Mid-Holocene (8.8–6.9 cal ka BP) during which the intensity of the chemical weathering was strongest and the climate was hot and wet; (3) the Mid-Holocene (6.9–4.6 cal ka BP) during which the intensity of the chemical weathering was strong but exhibited a weakening trend, and the climate was warm and wet; (4) the Middle and Late Holocene (4.6–1.3 cal ka BP) during which the intensity of the chemical weathering was weakest and the climate turned cold and dry; and (5) the Late Holocene (1.3 cal ka BP–present) during which the climate was warm and dry with an enhancing intensity of the chemical weathering. In general, the climate change process reflected by the major elements in this area is consistent with the stalagmite δ¹⁸O curve, which indicates that the major elements have a certain role in the inversion process of climate change.

Key words: the Liaohe Delta major element weathering parameters chemical weathering characteristics climate change