2019
DOI: 10.1016/j.quaint.2018.03.019
|View full text |Cite
|
Sign up to set email alerts
|

Mineralogy and carbonate geochemistry of the Dali Lake sediments: Implications for paleohydrological changes in the East Asian summer monsoon margin during the Holocene

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

1
7
0

Year Published

2019
2019
2023
2023

Publication Types

Select...
9

Relationship

0
9

Authors

Journals

citations
Cited by 20 publications
(9 citation statements)
references
References 52 publications
1
7
0
Order By: Relevance
“…Given that the Greater Khingan Mountains region may have been covered by thick snow during the last deglaciation (Pang et al, 2021), the snow/ice meltwater from the surrounding mountains, generated in response to the persistent warming in the EASM margin induced by the high Northern Hemisphere summer insolation during the early Holocene, may have made an important contribution to the lake level change in Dali Lake. This inference is supported by other studies (Fan et al, 2019; Li et al, 1990; Xiao et al, 2008; Yue et al, 2021). In addition, the low lake water temperature caused by the cold meltwater influx during the early Holocene (Yue et al, 2021) may also have reduced the evaporation of the lake water.…”
Section: Discussionsupporting
confidence: 86%
See 1 more Smart Citation
“…Given that the Greater Khingan Mountains region may have been covered by thick snow during the last deglaciation (Pang et al, 2021), the snow/ice meltwater from the surrounding mountains, generated in response to the persistent warming in the EASM margin induced by the high Northern Hemisphere summer insolation during the early Holocene, may have made an important contribution to the lake level change in Dali Lake. This inference is supported by other studies (Fan et al, 2019; Li et al, 1990; Xiao et al, 2008; Yue et al, 2021). In addition, the low lake water temperature caused by the cold meltwater influx during the early Holocene (Yue et al, 2021) may also have reduced the evaporation of the lake water.…”
Section: Discussionsupporting
confidence: 86%
“…However, there is an ongoing and vigorous debate about whether the Holocene highest water level of Dali Lake, in northern China, occurred in the early Holocene (11.7-8.0 ka) or the mid-Holocene (8.0-4.0 ka) (Goldsmith et al, 2017a(Goldsmith et al, , 2017bJiang et al, 2020;Liu et al, 2017a). It is also disputed whether replenishment of the lake water by snow/ice meltwater from the Great Khingan Mountains affected the level of Dali Lake during the early Holocene (Fan et al, 2017(Fan et al, , 2019Goldsmith et al, 2017aGoldsmith et al, , 2017bJiang et al, 2020;Liu et al, 2017a;Xiao et al, 2008Xiao et al, , 2009Yue et al, 2021). Although the history and the factors driving the lake level changes of Dali Lake have been of major scientific interest for several years, the lack of a resolution of these issues has led to much controversy about whether the Holocene EASM maximum occurred in the early Holocene or the mid-Holocene (Goldsmith et al, 2017a(Goldsmith et al, , 2017bJiang et al, 2020;Liu et al, 2017a;Xiao et al, 2008).…”
Section: Introductionmentioning
confidence: 99%
“…In this study, the EASM northern boundary is defined by three metrics. The first is the 400‐mm annual isohyet (hereinafter P 400 ), which is widely accepted as the boundary both between the monsoon and non‐monsoon regions and between forest and steppe vegetation (Fan et al., 2019; Xiao et al., 2018). The second metric depicts the climatological northern boundary by using the 2 mm day −1 isohyet in summer (May‐September; MJJAS) (hereinafter P summer ) (J. Chen et al., 2018).…”
Section: Methodsmentioning
confidence: 99%
“…In Dali Lake, a significant variation of mineral content indicated dramatically decreased inflowing water and decreased lake levels from 5.9 to 4.8 ka ago. Since 4.8 ka, quartz and albite percentages recovered to higher levels compared with the preceding period of 5.9-4.8 ka, but were much lower than before 5.9 ka, which suggests that drainage losses of lake water were much less from 4.8 to 0 ka than from 5.9 to 4.8 ka [149]. Compared with Dali's relatively large-amplitude oscillation of the hydrographic environment at 5.9-4.8 ka, pollen-derived, reconstructed Pa in Hulun lake declined slightly (fluctuating at around 330 mm at 6.4-4.4 ka) compared to the last stage (around 340 mm); until the period of 4.4-3.3 ka, the lowest Pa of the entire Holocene with an average of 260 mm was registered [115].…”
Section: Asynchronous Onset Of Mid-holocene Moisture Declinementioning
confidence: 82%