Moisture variations in Lacustrine−eolian sequence from the Hunshandake sandy land associated with the East Asian Summer Monsoon changes since the late Pleistocene

Ming, Guodong; Zhou, Wei; Wang, Hong; Cheng, Peng; Shu, Peixian; Feng, Xinbin; Fu, Yang

doi:10.1016/j.quascirev.2020.106210

Cited by 33 publications

(7 citation statements)

References 134 publications

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“…in the Hunshandake Sandy Lands also suggested that the EASM peaked between 11.3 and 8.5 ka BP (early Holocene), after which moisture levels gradually decreased (Ming et al, 2020). That analysis also suggested that lakes expanded and deserts shrank during the early-Holocene.…”

mentioning

confidence: 89%

“…Over the past few decade, several multiproxy studies based on lake sediments (An et al., 2012; Chen et al., 2015; Ming et al., 2020; Wu & Liu, 2012; Y. Zhao et al., 2007; Zhou et al., 2016), peat (X. Liu et al., 2018; Y. Zhao et al., 2020), stalagmites (Dong et al., 2015), loess‐paleosol (Y. C. Lu et al., 2007; Yang & Ding, 2014; Zhou et al., 2014), and eolian sand‐paleosol (H. Lu et al., 2013; J. Sun et al., 1999) have shown that changes in the region are consistent with global climate change on orbital and suborbital scales (Chen et al., 2019).…”

Section: Introductionmentioning

confidence: 99%

“…(2000) showed that paleosol widely developed in the early Holocene in north central China and, as eolian activity increased in the mid‐Holocene, the dryland area expanded. A recent comprehensive analysis of high‐resolution lacustrine‐eolian sequences and multiple climate proxies in the Hunshandake Sandy Lands also suggested that the EASM peaked between 11.3 and 8.5 ka BP (early Holocene), after which moisture levels gradually decreased (Ming et al., 2020). That analysis also suggested that lakes expanded and deserts shrank during the early‐Holocene.…”

Section: Introductionmentioning

confidence: 99%

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Holocene Moisture Variability and Its Lagged Response to Summer Insolation Revealed by Eolian Deposits in the Lake Qinghai Basin, NE Tibetan Plateau

Ding

Wang

2021

Paleoceanog and Paleoclimatol

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The East Asian Summer Monsoon (EASM) drives the distribution of heat and water vapor in east Asia, and has been linked to the survival of billions of people in the region (An et al., 2012; Chen et al., 2015). Understanding the dynamics and variability of the EASM since the Holocene is crucial for understanding current global warming, and for accurate prediction of future climate change. As a transition region between monsoon and arid inland climates, the modern monsoon marginal zone has a semi-arid to semi-humid climate, which is highly sensitive to global climate change and to the EASM response to the changes. There are abundant geological archives in the monsoon marginal zone containing information about the evolution of the EASM (Figure 1a) (

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mentioning

confidence: 89%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Holocene Moisture Variability and Its Lagged Response to Summer Insolation Revealed by Eolian Deposits in the Lake Qinghai Basin, NE Tibetan Plateau

Ding

Wang

2021

Paleoceanog and Paleoclimatol

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“…In addition, Ming et al (2020) discussed the influence of reservoir age uncertainties on climate reconstructions from Lake Bayan Nuur sediments in Inner Mongolia and put forward a paleoclimatic method to determine the 14 C reservoir age. They generated different Bayesian age models based on the Bacon program, varying only the 14 C reservoir age from its possible range (0-800 cal years), then evaluated its rationality by stratigraphic alignment.…”

Section: Reservoir Correction Of Lake Sediment Samplementioning

confidence: 99%

¹⁴C GEOCHRONOLOGY AND RADIOCARBON RESERVOIR EFFECT OF REVIEWED LAKES STUDY IN CHINA

et al. 2021

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Lacustrine sediments are important archives for paleoclimate research, but there are evident carbon reservoir effects. Radiocarbon (14C) ages of lake sediments must be corrected for these effects before applying them to paleoclimate research. The authors review the lacustrine research from the last 20 years from different climatic regions in China, and systematically investigate the 14C age and correction methods used in the studies of 81 lakes. It is found that the climate-vegetation cover and distribution of carbonate around lakes are dominant factor controlling radiocarbon reservoir effects. In eastern China, the average 14C reservoir age is about 500 14C years and is associated with relatively dense vegetation. However, in northwest China and Qinghai-Tibet Plateau, widespread carbonate bedrock may markedly increase the radiocarbon reservoir age which frequently is about 1500 and 2500 14C years. A piecewise linear regression model provides more reliable 14C reservoir age correction that accounts for sedimentary facies and sedimentation rate changes. It is worth mentioning that when analyzing 14C ages deviated greatly from time sequence, the age anomalies may indicate important effects relevant to the study of climate and environmental changes.

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“…The spatiotemporal heterogeneity of EASM rainfall during the Holocene is also a debated issue (Shi et al, 2012;Xie et al, 2013;Chen F. et al, 2015;Jia et al, 2015;Rao et al, 2016;Zhou et al, 2016;Goldsmith et al, 2017;Zhu et al, 2017;Huang X. et al, 2018;Ming et al, 2020;Xu et al, 2020). For example, stalagmite δ 18 O records show an early Holocene EASM maximum (Dykoski et al, 2005;Wang et al, 2005;Cai et al, 2010;Dong et al, 2010;Zhang et al, 2019), which is also supported by lacustrine records from southern China (Zhou et al, 2004;Zhong et al, 2010;Wang et al, 2016;Sheng et al, 2017).…”

Section: Introductionmentioning

confidence: 97%

Holocene East Asian Summer Monsoon Rainfall Variability in Taiwan

Ding

Zheng

et al. 2020

Front. Earth Sci.

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Characterizing the spatiotemporal variability of the East Asian summer monsoon (EASM) advances our understanding of its rhythm, dynamics, and future impacts. East Asian summer monsoon variations during the Holocene have been reconstructed from a variety of geological archives and proxies. However, the spatiotemporal heterogeneity of EASM rainfall during the Holocene remains controversial. Taiwan is geographically suitable for studying the EASM history, through its geological archives. Herein, we synthesize the reported lake and peat sedimentary records of the entire Holocene, in addition to the records of mass-wasting and on-land deposition from cores collected from Taiwan to illustrate the EASM induced hydroclimate changes in Taiwan throughout the Holocene. Records from Taiwan indicate that the EASM rainfall maximum occurred during the early Holocene, concurring with other EASM records from monsoon regions in southern China. We suggest that the early Holocene EASM rainfall maximum in southern China was mainly forced by the higher Northern Hemisphere summer insolation and sea surface temperatures (SSTs) in the Western Pacific Warm Pool (WPWP). A synthesis of EASM rainfall records from across China shows that the timing of the Holocene EASM rainfall maximum occurred progressively later than that from southern to northern China. This time-transgressive EASM rainfall maximum may be due to the latitudinal shift of the westerlies and Western Pacific subtropical high (WPSH) that was induced by changes of interhemispheric temperature gradients (T N−S) and the northern high latitude ice volume. Moreover, records from Taiwan suggest a significant collapse of the EASM in Taiwan at ∼4-2 ka BP. Based on the records from Taiwan, coastal East Asia, and the Tropical Pacific, we propose that the SSTs of the WPWP and/or El Niño-Southern Oscillation activity may have exerted a strong influence on the EASM rainfall changes during the late Holocene. Moreover, increased EASM rainfall in southern China during the last 2 ka was likely caused by a southward shift of WPSH, which is associated with gradual decreases in T N−S during the late Holocene.

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Moisture variations in Lacustrine−eolian sequence from the Hunshandake sandy land associated with the East Asian Summer Monsoon changes since the late Pleistocene

Cited by 33 publications

References 134 publications

Holocene Moisture Variability and Its Lagged Response to Summer Insolation Revealed by Eolian Deposits in the Lake Qinghai Basin, NE Tibetan Plateau

Holocene Moisture Variability and Its Lagged Response to Summer Insolation Revealed by Eolian Deposits in the Lake Qinghai Basin, NE Tibetan Plateau

¹⁴C GEOCHRONOLOGY AND RADIOCARBON RESERVOIR EFFECT OF REVIEWED LAKES STUDY IN CHINA

Holocene East Asian Summer Monsoon Rainfall Variability in Taiwan

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Moisture variations in Lacustrine−eolian sequence from the Hunshandake sandy land associated with the East Asian Summer Monsoon changes since the late Pleistocene

Cited by 33 publications

References 134 publications

Holocene Moisture Variability and Its Lagged Response to Summer Insolation Revealed by Eolian Deposits in the Lake Qinghai Basin, NE Tibetan Plateau

Holocene Moisture Variability and Its Lagged Response to Summer Insolation Revealed by Eolian Deposits in the Lake Qinghai Basin, NE Tibetan Plateau

14C GEOCHRONOLOGY AND RADIOCARBON RESERVOIR EFFECT OF REVIEWED LAKES STUDY IN CHINA

Holocene East Asian Summer Monsoon Rainfall Variability in Taiwan

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¹⁴C GEOCHRONOLOGY AND RADIOCARBON RESERVOIR EFFECT OF REVIEWED LAKES STUDY IN CHINA