北大西洋45°N区氧同位素3期以来上层水体性质的变化

叶孝贤; HarunurRashid

doi:10.16562/j.cnki.0256-1492.2020073102

北大西洋45°N区氧同位素3期以来上层水体性质的变化

叶孝贤,
HarunurRashid^,

上海海洋大学海洋科学学院，上海 201306

基金项目: 国家自然科学基金项目“浮游有孔虫δ¹⁸O和Mg/Ca比值示踪过去45万年以来西北大西洋混合层和温跃层的温度和密度梯度在千年尺度上的变化”（41776064）

详细信息

作者简介: 叶孝贤（1996—），女，硕士研究生，主要从事海洋地质学及古海洋环境研究，E-mail：m180200489@st.shou.edu.cn

通讯作者: Harunur Rashid（1969—），男，教授，主要从事海洋地质学、古海洋学、低温地球化学研究，E-mail：rashid@shou.edu.cn

中图分类号: P736.4

收稿日期: 2020-07-31

修回日期: 2021-01-03

刊出日期: 2021-06-28

Changes of the upper water column at the 45°N North Atlantic since marine isotope stage 3

YE Xiaoxian,
Harunur Rashid^,

College of Marine Sciences, Shanghai Ocean University, Shanghai, CHINA 201306

More Information

Corresponding author: Harunur Rashid, rashid@shou.edu.cn

Received Date: 31 July 2020

Revised Date: 03 January 2021

Publish Date: 28 June 2021

摘要

摘要:
北大西洋45°N区是北大西洋冰筏碎屑（IRD）带的中心区，其海洋沉积物包含高分辨率沉积环境和气候变化信息，对45°N区沉积记录的研究有利于反演末次冰期以来古海洋环境的变化。通过对岩心Hu71-377中IRD含量的统计、浮游有孔虫组合及氧和碳同位素（δ¹⁸O和δ¹³C）分析，重建了北大西洋45°N上层水体水团性质演化历史。结合AMS¹⁴C数据和氧同位素地层学，在氧同位素3期（MIS3）和2期（MIS2）中识别出5个Heinrich层，其中Heinrich 1、2和4层具有明显IRD峰值、Neogloboquadrina pachyderma高丰度和轻δ¹⁸O值特征，而Heinrich 3和5层的δ¹⁸O值未明显变轻。Heinrich 3和5层与Heinrich 1、2和4层的δ¹⁸O 差异可能反映了上层水体受融水输入的影响不同。δ¹³C_N.incompta和δ¹³C_N.pachyderma差值也反映了Heinrich事件期间混合层和温跃层的变化，它们的δ¹³C差值在Heinrich 1和2期间接近零，归因于强风驱动的海水垂向混合。而δ¹³C_N.incompta和δ¹³C_N.pachyderma差值在Heinrich 4和5期间增大，反映了季节性温跃层变浅，推测与北大西洋暖流增强有关。浮游有孔虫组合进一步反映了海洋上层水团性质, 特别是N. pachyderma和Neogloboquadrina incompta的相对丰度反映了MIS3期以来海表温度（SST）变化。
- Heinrich事件 /
- 浮游有孔虫组合 /
- 碳氧同位素 /
- 上层水团变化 /
- 北大西洋
Abstract:
The 45°N of North Atlantic is located at the central zone of the ice-rafted detritus (IRD) belt of the North Atlantic, where the marine sediments contain rich environmental and climatic information of high-resolution. The sedimentary records there are used for reconstruction of the pale-oceanic environment since the last glacial in this study. IRD contents, planktonic foraminiferal assemblages and their oxygen and carbon isotopes (δ¹⁸O and δ¹³C) from the core Hu71-377, are used as major tools. Combined with AMS¹⁴C dating and oxygen isotope stratigraphy, five Heinrich layers are identified in the MIS3 and MIS2, in which the Heinrich layer 1, 2 and 4 have obvious IRD peaks, high relative abundance of Neogloboquadrina pachyderma and light δ¹⁸O values, but no obvious light δ¹⁸O are observed in the Heinrich layer 3 and 5. The difference in δ¹⁸O between the Heinrich layers 3 and 5 and the Heinrich layers 1, 2 and 4 may suggest the impacts of melt water on the upper water column. Further, the offsets between δ¹³C_N.incompta and δ¹³C_N.pachyderma may also reflect the changes in the mixed layer and thermocline during the Heinrich events. The δ¹³C offsets were close to zero during Heinrich 1 and Heinrich 2, attributing to the vertical mixing of seawater driven by strong winds. And the δ¹³C offsets became larger during Heinrich 4 and Heinrich 5, indicating that the seasonal thermocline became shallower, which supports the inference of the penetration of the North Atlantic Current. What’s more, the planktonic foraminiferal assemblages may reflect the properties of the water masses in the upper water column, especially the relative abundance of N. pachyderma and Neogloboquadrina incompta may indicate the sea surface temperature (SST) changes during MIS3.
- Heinrich events /
- planktonic foraminifera assemblages /
- carbon and oxygen isotopes /
- upper water masses variations /
- North Atlantic

HTML全文

图 1 北大西洋Hu71-377与相关岩心^[8,28-29]的位置以及洋流和SST分布

Figure 1.

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图 2 岩心Hu71-377深度-年龄模型（a）和沉积速率（b）

Figure 2.

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图 3 北大西洋Hu71-377岩心IRD、N. pachyderma相对丰度和δ¹⁸O指标与DSDP609岩心^[36]和NGRIP冰芯^[35]地层学对比以及SU9008岩心^[28]相关指标

Figure 3.

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图 4 北大西洋Hu71-377岩心IRD、有孔虫相对丰度、δ¹⁸O和δ¹³C、壳体质量等指标与岩心SO82_5-2^[29] 和DSDP609^[37]的δ¹⁸O和δ¹³C指标

Figure 4.

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表 1 岩心Hu71-377 ¹⁴C年龄及日历年龄

Table 1. ¹⁴C Age and Calendar Age of the core Hu71-377

深度/cm	实验ID	¹⁴C年龄/a	测试材料	日历年龄/ka
0 ～ 2	UCI-212015	1930±15	G. inflata	1.333
68.5 ～ 69.5	UCI-214037	11545±25	G. inflata	12.860
115 ～ 116	UCI-23843	15840±60	N. pachyderma	18.174
256 ～ 257	UCI-212021	25610±80	G. inflata	28.887
389 ～ 390	UCI-214039	37120±230	G. bulloides	40.920

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表 2 NGRIP冰芯、DSDP609岩心和Hu71-377岩心的Heinrich事件相关控制点

Table 2. Heinrich events in the ice core NGRIP, core DSDP609 and core Hu71-377

控制点	NGRIP^[36]		DSDP609^[35]		Hu71-377^[27]
控制点	年龄/ka	δ¹⁸O/‰	深度/cm	δ¹⁸O/‰	深度/cm	δ¹⁸O/‰
Heinrich 1	15.58	−44.56	88	4.25	110.5	4.30
Heinrich 2	23.72	−45.29	120	3.89	178	4.14
Heinrich 3	29.70	−46.45	158	3.93	273.5	3.54
Heinrich 4	38.72	−44.41	248	3.88	405.5	3.34
Heinrich 5	48.16	−45.08	305	3.67	562.5	3.46

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北大西洋45°N区氧同位素3期以来上层水体性质的变化

上海海洋大学海洋科学学院，上海 201306

作者简介: 叶孝贤（1996—），女，硕士研究生，主要从事海洋地质学及古海洋环境研究，E-mail：m180200489@st.shou.edu.cn

通讯作者: Harunur Rashid（1969—），男，教授，主要从事海洋地质学、古海洋学、低温地球化学研究，E-mail：rashid@shou.edu.cn

Changes of the upper water column at the 45°N North Atlantic since marine isotope stage 3

College of Marine Sciences, Shanghai Ocean University, Shanghai, CHINA 201306

Corresponding author: Harunur Rashid, rashid@shou.edu.cn

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