Interrelationships between climate change and surface processes in the First Meander of the Yellow River since the Last Deglaciation

doi:10.7522/j.issn.1000-694X.2023.00148

Journal of Desert Research ›› 2024, Vol. 44 ›› Issue (2): 121-132.DOI: 10.7522/j.issn.1000-694X.2023.00148

Interrelationships between climate change and surface processes in the First Meander of the Yellow River since the Last Deglaciation

Jianhui Ge¹^,²(), Bing Liu¹(), Yujie Xu¹^,², Aijun Sun¹^,²^,³, Keqi Wang¹^,², Dongxue Li¹^,², hui Zhao¹

^1.Key Laboratory of Desert and Desertification，Northwest Institute of Eco-Environment and Resources，Chinese Academy of Sciences，Lanzhou 730000，China
^2.University of Chinese Academy of Sciences，Beijing 100049，China
^3.Ministry of Education Key Laboratory of Western China's Environmental Systems，College of Earth and Environmental Sciences，Lanzhou University，Lanzhou 730000，China

Received:2023-08-31 Revised:2023-10-21 Online:2024-03-20 Published:2024-03-19
Contact: Bing Liu

Abstract

Abstract:

The First Meander of the Yellow River， an area rich in biodiversity， is highly sensitive to ecological changes in the world's high-altitude regions， in where the environmental evolution how responds to regional climate change is of great important scientific significance. In view of the reconstructed results divergence of climate/environment since the last deglaciation， we individually synthesized the framework process of regional climatic change and the history of earth surface environmental evolution， as well as further discuss the relationship between them， with the aid of the published multi-archive records. The results indicated that the regional climate became warmer and wetter during the period of 13-6 ka， with the climatic optimum of 10-6 ka， afterwards， the regional climate tended to be cold-dry owing to the declined temperature and humidity. The regional earth surface process was dominated by the fluvio-lacustrine sediments during 18-11 ka， accompanying with the weakest aeolian activity， whereas the aeolian activity began enhanced from 11 ka to 8 ka， along with the weakened fluvio-lacustrine process. In 8-3 ka， the paleosol is unprecedentedly developed and alpine meadow is extensively formed thereafter. An asynchronous relationship was detected between regional surface environmental and climate change， in detail， climate change positively drove regional surface processes prior to 6 ka， whereas it exerted a negative influence hereafter. Additionally， we concluded that meadow soil is a product of continuous accumulation of aeolian material under the context of gradually cold and dry conditions， by comparing modern and late Holocene meadow soil particle sizes， which implying a complex relationship between regional soil development and climate change.

Key words: the Last Deglaciation, the First Meander of the Yellow River, climate change, surface processes, interrelationship

CLC Number:

P532

Jianhui Ge, Bing Liu, Yujie Xu, Aijun Sun, Keqi Wang, Dongxue Li, hui Zhao. Interrelationships between climate change and surface processes in the First Meander of the Yellow River since the Last Deglaciation[J]. Journal of Desert Research, 2024, 44(2): 121-132.

Figures/Tables 9

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编号	剖面名称	纬度（°N）	经度（°E）	测年方式	时间范围 /ka BP	年代数	分辨率 /a	代用指标	指标意义	参考文献
Tw1	ZB08-C1	33.45	102.63	AMS¹⁴C	11.0~0	8	~60	孢粉	MTwa	Liang等^[7]
Tw2	ZB10-C9	32.78	102.52	AMS¹⁴C	11.0~0	15	~60	孢粉	MTwa	Liang等^[7]
Tw3	ZB10-C14	33.10	102.67	AMS¹⁴C	11.0~0	18	~60	孢粉	MTwa	Liang等^[7]
T1	ZB08-C1	33.45	102.63	AMS¹⁴C	11.0~0	8	~60	孢粉	MAT	Liang等^[7]
T2	ZB10-C9	32.78	102.52	AMS¹⁴C	11.0~0	15	~60	孢粉	MAT	Liang等^[7]
T3	ZB10-C14	33.10	102.67	AMS¹⁴C	11.0~0	18	~60	孢粉	MAT	Liang等^[7]
T4	HY4	32.78	102.52	AMS¹⁴C	13.0~0	8	~100	BrGDGTs	MAT	Yan等^[22]
T5	Hongyuan Peats	32.77	102.52	AMS¹⁴C	13.0~0	11	~100	GDGTs	MAT	Zheng等^[25]
P1	Hongyuan peat	32.77	102.05	AMS¹⁴C	12.0~0	15	~30	木里苔草碳同位素	夏季风	Hong等^[23]
P2	Hongyuan peatland	32.78	102.52	AMS¹⁴C	13.5~0	32	~25	冷杉花粉	夏季风	Zhou等^[9]
P3	红原泥炭剖面1	32.77	102.50	AMS¹⁴C	12.0~0	15	~30	腐殖化度	湿度	王华等^[24]
P4	红原泥炭剖面2	32.78	102.52	AMS¹⁴C	11.5~0	11	~15-20	灰度	夏季风	于学峰等^[26]
P5	ZB10-C14	33.10	102.67	AMS¹⁴C	10.5~0	18	~60	针叶林相似性得分	湿度	孙晓红等^[6]

编号	剖面名称	纬度（°N）	经度（°E）	测年方式	时间范围 /ka BP	年代数	分辨率 /a	代用指标	指标意义	参考文献
Tw1	ZB08-C1	33.45	102.63	AMS¹⁴C	11.0~0	8	~60	孢粉	MTwa	Liang等^[7]
Tw2	ZB10-C9	32.78	102.52	AMS¹⁴C	11.0~0	15	~60	孢粉	MTwa	Liang等^[7]
Tw3	ZB10-C14	33.10	102.67	AMS¹⁴C	11.0~0	18	~60	孢粉	MTwa	Liang等^[7]
T1	ZB08-C1	33.45	102.63	AMS¹⁴C	11.0~0	8	~60	孢粉	MAT	Liang等^[7]
T2	ZB10-C9	32.78	102.52	AMS¹⁴C	11.0~0	15	~60	孢粉	MAT	Liang等^[7]
T3	ZB10-C14	33.10	102.67	AMS¹⁴C	11.0~0	18	~60	孢粉	MAT	Liang等^[7]
T4	HY4	32.78	102.52	AMS¹⁴C	13.0~0	8	~100	BrGDGTs	MAT	Yan等^[22]
T5	Hongyuan Peats	32.77	102.52	AMS¹⁴C	13.0~0	11	~100	GDGTs	MAT	Zheng等^[25]
P1	Hongyuan peat	32.77	102.05	AMS¹⁴C	12.0~0	15	~30	木里苔草碳同位素	夏季风	Hong等^[23]
P2	Hongyuan peatland	32.78	102.52	AMS¹⁴C	13.5~0	32	~25	冷杉花粉	夏季风	Zhou等^[9]
P3	红原泥炭剖面1	32.77	102.50	AMS¹⁴C	12.0~0	15	~30	腐殖化度	湿度	王华等^[24]
P4	红原泥炭剖面2	32.78	102.52	AMS¹⁴C	11.5~0	11	~15-20	灰度	夏季风	于学峰等^[26]
P5	ZB10-C14	33.10	102.67	AMS¹⁴C	10.5~0	18	~60	针叶林相似性得分	湿度	孙晓红等^[6]

序号	类型	剖面名称	纬度（°N）	经度（°E）	时间范围 /ka BP	测年手段	年代数	代用指标	参考文献
1	风成砂-古土壤序列	section1	33.85	102.57	10~3.5	OSL	2	粒度、总有机碳	Hu等^[10]
2	风成砂-古土壤序列	section2	33.93	102.13	3~0.5	OSL	5	粒度、总有机碳	Hu等^[10]
3	风成砂-古土壤序列	section3	33.78	102.18	1~0	OSL	3	粒度、总有机碳	Hu等^[10]
4	风成砂-古土壤序列	MQQ	33.96	102.08	10~0	AMS¹⁴C	6	粒度、磁化率	Yang等^[27]
5	风成砂-古土壤序列	剖面P.5	—	—	—	¹⁴C	1	—	徐先英等^[20]
6	风成砂-古土壤序列	剖面P.6	—	—	3.5~0.5	¹⁴C	2	—	徐先英等^[20]
7	风成砂-古土壤序列	剖面P.9	—	—	—	¹⁴C	1	—	徐先英等^[20]
8	风成砂-古土壤序列	剖面P.10	—	—	1.5~0.5	¹⁴C	2	—	徐先英等^[20]
9	风成砂-古土壤序列	剖面P.21	—	—	1.5~0	¹⁴C	2	—	徐先英等^[20]
10	风成砂-古土壤序列	MO	33.90	102.16	6~0	¹⁴C	5	地化元素	胡梦珺等^[28]
11	风成砂-古土壤序列	OL	33.94	102.02	5.5~0	¹⁴C	5	地化元素	杨爱丽^[29]
12	风成砂-古土壤序列	LQXR	33.95	102.07	7.5~1	OSL	4	粒度	周家和等^[11]
13	风成砂-古土壤序列	LQXA	33.77	102.21	4~0.5	OSL	7	粒度	周家和等^[11]
14	风成砂-古土壤序列	XCC	34.08	102.58	4.5~1.5	OSL	5	粒度、磁化率、地化元素	柴佳楠等^[17-18]
15	风成砂-古土壤序列	XM	33.7	102.53	16~1	AMS¹⁴C	5	粒度、磁化率	綦琳等^[30]
16	风成砂-古土壤序列	OQC	—	—	18~0	OSL	5	粒度	王娜等^[3]
17	风成砂-古土壤序列	WQD	—	—	18~0	OSL， AMS¹⁴C	6	粒度	周家和等^[31]
18	风成砂-古土壤序列	AB	—	—	1.5~0.5	AMS¹⁴C	2	粒度、重矿物	邹学勇等^[32]
19	风成砂-古土壤序列	EF	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
20	风成砂-古土壤序列	MN	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
21	风成砂-古土壤序列	GH	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
22	风成砂-古土壤序列	IJ	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
23	风成砂-古土壤序列	PQ	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
24	黄土-古土壤序列	TWR	33.99	101.92	13.5~8.5	OSL	4	粒度、磁化率、地化元素等	陈莹璐等^[33-34]
25	黄土-古土壤序列	DEQ-E	34.00	101.90	18~1	OSL	7	粒度、磁化率	肖奇立等^[21]
26	黄土-古土壤序列	ZHK	34.02	101.89	14~0	OSL， AMS¹⁴C	5	粒度、磁化率	Jia等^[15]
27	河湖相沉积	WDT	33.45	102.45	5~0	OSL	3	粒度、磁化率、地化元素	柴佳楠等^[17-18]
28	河湖相沉积	LQ	33.76	102.24	9.5~0	OSL， ¹⁴C	6	粒度、磁化率、地化元素等	左海玲^[13]
29	河湖相沉积	DEQ	34.01	101.88	18~0	OSL	4	粒度、磁化率、地化元素等	戎晓庆^[14]
30	河湖相沉积	JYM	33.53	102.48	18~0	OSL	14	粒度、磁化率、地化元素等	戎晓庆^[14]
31	河湖相沉积	剖面P.7	—	—	12~2	AMS¹⁴C	3	—	徐先英等^[20]

序号	类型	剖面名称	纬度（°N）	经度（°E）	时间范围 /ka BP	测年手段	年代数	代用指标	参考文献
1	风成砂-古土壤序列	section1	33.85	102.57	10~3.5	OSL	2	粒度、总有机碳	Hu等^[10]
2	风成砂-古土壤序列	section2	33.93	102.13	3~0.5	OSL	5	粒度、总有机碳	Hu等^[10]
3	风成砂-古土壤序列	section3	33.78	102.18	1~0	OSL	3	粒度、总有机碳	Hu等^[10]
4	风成砂-古土壤序列	MQQ	33.96	102.08	10~0	AMS¹⁴C	6	粒度、磁化率	Yang等^[27]
5	风成砂-古土壤序列	剖面P.5	—	—	—	¹⁴C	1	—	徐先英等^[20]
6	风成砂-古土壤序列	剖面P.6	—	—	3.5~0.5	¹⁴C	2	—	徐先英等^[20]
7	风成砂-古土壤序列	剖面P.9	—	—	—	¹⁴C	1	—	徐先英等^[20]
8	风成砂-古土壤序列	剖面P.10	—	—	1.5~0.5	¹⁴C	2	—	徐先英等^[20]
9	风成砂-古土壤序列	剖面P.21	—	—	1.5~0	¹⁴C	2	—	徐先英等^[20]
10	风成砂-古土壤序列	MO	33.90	102.16	6~0	¹⁴C	5	地化元素	胡梦珺等^[28]
11	风成砂-古土壤序列	OL	33.94	102.02	5.5~0	¹⁴C	5	地化元素	杨爱丽^[29]
12	风成砂-古土壤序列	LQXR	33.95	102.07	7.5~1	OSL	4	粒度	周家和等^[11]
13	风成砂-古土壤序列	LQXA	33.77	102.21	4~0.5	OSL	7	粒度	周家和等^[11]
14	风成砂-古土壤序列	XCC	34.08	102.58	4.5~1.5	OSL	5	粒度、磁化率、地化元素	柴佳楠等^[17-18]
15	风成砂-古土壤序列	XM	33.7	102.53	16~1	AMS¹⁴C	5	粒度、磁化率	綦琳等^[30]
16	风成砂-古土壤序列	OQC	—	—	18~0	OSL	5	粒度	王娜等^[3]
17	风成砂-古土壤序列	WQD	—	—	18~0	OSL， AMS¹⁴C	6	粒度	周家和等^[31]
18	风成砂-古土壤序列	AB	—	—	1.5~0.5	AMS¹⁴C	2	粒度、重矿物	邹学勇等^[32]
19	风成砂-古土壤序列	EF	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
20	风成砂-古土壤序列	MN	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
21	风成砂-古土壤序列	GH	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
22	风成砂-古土壤序列	IJ	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
23	风成砂-古土壤序列	PQ	—	—	—	AMS¹⁴C	1	粒度、重矿物	邹学勇等^[32]
24	黄土-古土壤序列	TWR	33.99	101.92	13.5~8.5	OSL	4	粒度、磁化率、地化元素等	陈莹璐等^[33-34]
25	黄土-古土壤序列	DEQ-E	34.00	101.90	18~1	OSL	7	粒度、磁化率	肖奇立等^[21]
26	黄土-古土壤序列	ZHK	34.02	101.89	14~0	OSL， AMS¹⁴C	5	粒度、磁化率	Jia等^[15]
27	河湖相沉积	WDT	33.45	102.45	5~0	OSL	3	粒度、磁化率、地化元素	柴佳楠等^[17-18]
28	河湖相沉积	LQ	33.76	102.24	9.5~0	OSL， ¹⁴C	6	粒度、磁化率、地化元素等	左海玲^[13]
29	河湖相沉积	DEQ	34.01	101.88	18~0	OSL	4	粒度、磁化率、地化元素等	戎晓庆^[14]
30	河湖相沉积	JYM	33.53	102.48	18~0	OSL	14	粒度、磁化率、地化元素等	戎晓庆^[14]
31	河湖相沉积	剖面P.7	—	—	12~2	AMS¹⁴C	3	—	徐先英等^[20]

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Interrelationships between climate change and surface processes in the First Meander of the Yellow River since the Last Deglaciation

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