Tungsheng Liu

Dados Biográficos

ID	5599327
NOME	Tungsheng Liu
PRENOMES	Tungsheng
SOBRENOME	Liu
ASSINATURA	LIU T
AFILIAÇÕES	Chinese Academy of Sciences
VERIFICADO	Não
TOTAL DE OBRAS	19
TOTAL DE CITAÇÕES	7
TOTAL COMO AUTOR	19
TOTAL COMO EDITOR	0
PRIMEIRO ANO DE PUBLICAÇÃO	1981
ANO MAIS RECENTE DE PUBLICAÇÃO	2006
ÍNDICE H	2

Phytoliths as quantitative indicators for the reconstruction of past environmental conditions in China I
Open AccessHouyuan Lu, Hou-Yuan Lu et al.ARTICLEQuaternary Science Reviews2006
Evolution of megadunes and lakes in the Badain Jaran Desert, Inner Mongolia, China during the last 31,000 years
Open AccessXiaoping Yang, Tungsheng Liu et al.ARTICLEQuaternary International2003
Glacial environments on the Tibetan Plateau and global cooling
Open AccessTungsheng Liu, Xinshi Zhang et al.ARTICLEQuaternary International2002
The ‘Mediaeval Warm Period’ drought recorded in Lake Huguangyan, tropical South China
Open AccessGuoqiang Chu, Jiaqi Liu et al.ARTICLEThe Holocene2002Citada por: 3Referências: 3
The geochemistry of dated sediment cores from Lake Huguangyan (21°9′N, 110°17′E), tropical South China, reveals distinct stratigraphical patterns in total organic and inorganic carbon (TOC, TIC), biogenic silica (BS) and total nitrogen (TN) over the past 1400 years. In this hydrologically closed lake, TIC variations may re‘ ect changes in the precipitation/evaporation ratio, which controls the evaporative enrichment of carbonate. TOC, BS and TN i…
Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve
Open AccessChengde Shen, Weixi Yi et al.ARTICLERadiocarbon2001Citada por: 1Referências: 12
We report here first results on the bulk soil organic carbon (SOC), apparent radiocarbon ages and δ 13 C characteristics of the tropical and subtropical forest soil in Dinghushan Biosphere Reserve (DHSBR). The forest oxisol in Dinghushan has developed during the Holocene. The δ 13 C variation curves in all three profiles may be divided into two sections. The upper section from 0 to 40 cm has δ 13 C values varying from −27.4 to −24.1‰, −27.5 to −2…
Stratigraphic Evidence for the Uplift of the Tibetan Plateau between ∼1.1 and ∼0.9 myr Ago
Open AccessJimin Sun, Tungsheng LiuARTICLEQuaternary Research2000
Uplift of the Tibetan Plateau is manifest not only in widespread denudation, but also by an increased deposition rate of sediment, near or far from the exhumed regions. Our results indicate that the mass accumulation rate (MAR) of eolian dust increased between ∼1.1 and ∼0.9 myr ago. We associate this increase in MAR and median grain size with uplift of the Tibetan Plateau and its adjacent regions during this period. This Middle Pleistocene uplift…
Changes in Sand Content of Loess Deposits along a North–South Transect of the Chinese Loess Plateau and the Implications for Desert Variations
Open AccessZhongli Ding, Jimin Sun et al.ARTICLEQuaternary Research1999
Geological records have shown that the deserts east of the Helan Mountains in northern China were covered by grass during the Holocene Optimum, whereas during marine oxygen isotope stages 2 and 4 distribution of the deserts was almost the same as at present. The wide advance–retreat cycles of the deserts may have exerted an important control on grain-size changes in the loess of the Loess Plateau by altering the distance between the source and th…
Spectral analysis of a 1000-year stalagmite lamina-thickness record from Shihua Cavern, Beijing, China, and its climatic significance
Open AccessXiaoguang Qin, Ming Tan et al.ARTICLEThe Holocene1999Citada por: 2Referências: 1
Stalagmite laminae provide a high-resolution geological record of climate change. In this paper, moving spectral analysis is used to analyse a stalagmite lamina thickness record to study climatic variability. It was found that the dominant cycles of the lamina thickness sequence are 2, 3.3, 5–6, 10–12, 14–18, 133 and 194 years. Some of the cycles are the same as the cycles of modern climatic indices, such as the QBO (Quasi Biennial Oscillation) o…
Chinese Loess and the Paleomonsoon
Tungsheng Liu, Zhongli DingARTICLEAnnual Review of Earth and…1998
This paper presents a general review of the recent research advances of the East Asian paleomonsoon, based mainly on studies of the loess-soil sequences in the Chinese Loess Plateau. In the last 2.6 million years, the paleomonsoonal history may be divided into about 166 events on a time scale of the Earth's orbital variations. During the last glacial period, millenial-scale oscillations of the monsoon system were prominent, which can be fairly we…
Biogenic Silica Record in Lake Biwa of Central Japan over the Past 145,000 Years
Open AccessJule Xiao, Yoshio Inouchi et al.ARTICLEQuaternary Research1997
The record of the biogenic silica flux (BSF, g cm −2 (10 3 yr) −1 ) in Lake Biwa reflects changes in diatom productivity in the lake and provides information regarding changes in paleoclimatic conditions. The BSF record of Lake Biwa demonstrates five periods over the past ca. 145,000 yr when the BSF values were significantly greater than 7.5 g cm −2 (10 3 yr) −1 , and five intervals when they were lower. The data imply that paleoclimatic conditio…
Eolian Quartz Flux to Lake Biwa, Central Japan, over the Past 145,000 Years
Open AccessJule Xiao, Yoshio Inouchi et al.ARTICLEQuaternary Research1997
Eolian quartz flux (EQF, g cm −2 (10 3 yr) −1 ) to Lake Biwa, central Japan, provides direct information on variations of the East Asian winter monsoon. Lake Biwa sediments spanning the past ca. 145,000 yr are characterized by two main periods when EQF values were significantly greater than 5.50 g cm −2 (10 3 yr) −1 , and two main intervals during which EQF values were lower. Two periods with EQF values >5.50 g cm −2 (10 3 yr) −1 occurred from ca…
Stable isotope composition of the carbonate concretion in loess and climate change
Open AccessJiamao Han, Edward Keppens et al.ARTICLEQuaternary International1997
The onset of extensive loess deposition around the G/M boundary in China and its palaeoclimatic implications
Open AccessZhongli Ding, Nat W Rutter et al.ARTICLEQuaternary International1997
C Dating of Terrestrial Moss in Tern Lake Deposits, Antarctica
Open AccessChengde Shen, Tungsheng Liu et al.ARTICLERadiocarbon1997Citada por: 1Referências: 6
Accurate radiocarbon ages were obtained from terrestrial moss from two drill holes in Tern Lake deposits, Antarctica, using liquid scintillation counting (LSC) and accelerator mass spectrometry (AMS). The results show that the lake deposits have been accumulating since the end of the last glacial epoch ca. 12,600 cal BP at the rate of 0.13–1.1 mm a -1 . We discuss the validity of 14 C ages of Antarctic lake deposits, with respect to the latitude …
Ice-Volume Forcing of East Asian Winter Monsoon Variations in the Past 800,000 Years
Open AccessZhongli Ding, Tungsheng Liu et al.ARTICLEQuaternary Research1995
Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio of 10 μm (%) can be used as an indicator of variations in intensity of the East Asian winter monsoon winds. Grain-size curves of the Baoji and Weinan sections show that this proxy indicator is very sensitive to loess-soil alterations. Analytical results also suggest that during soil-forming…
Remanence Characteristics of Different Magnetic Grain Size Categories at Xifeng, Central Chinese Loess Plateau
Open AccessXiuming Liu, Tim Rolph et al.ARTICLEQuaternary Research1994
Utilizing the thermal unblocking of low-temperature remanent magnetization in superparamagnetic (SP) ferrimagnets and the low-temperature demagnetization of multidomain (MD) magnetite remanences, the relative proportions of SP, MD, and singledomain (SD and SD-like) ferrimagnets are estimated in the topmost part of a loess section at Xifeng, China, which covers about the past 130,000 yr. SP ferrimagnets are commonly regarded as pedogenic (authigen…
The paleosol complex S5 in the China Loess Plateau ? A record of climatic optimum during the last 1.2 Ma
Open AccessZhaolong An, An Zhisheng et al.ARTICLEGeoJournal1987
Magnetostratigraphical dating of loess deposits in China
Open AccessFriedrich Heller, Tungsheng Liu et al.ARTICLENature1982
A Review of the Multi-Disciplinary Scientific Research on the Qinghai-Xizang Plateau by Chinese Scientists in Recent Years
Tungsheng Liu, Liu Tung-Sheng et al.ARTICLEGeographical Journal1981
Liu Tung-Sheng, Sun Hung-Lieh, A Review of the Multi-Disciplinary Scientific Research on the Qinghai-Xizang Plateau by Chinese Scientists in Recent Years, The Geographical Journal, Vol. 147, No. 1 (Mar., 1981), pp. 23-26

The ‘Mediaeval Warm Period’ drought recorded in Lake Huguangyan, tropical South China
Open AccessGuoqiang Chu, Jiaqi Liu et al.ARTICLEThe Holocene2002Citada por: 3Referências: 3
The geochemistry of dated sediment cores from Lake Huguangyan (21°9′N, 110°17′E), tropical South China, reveals distinct stratigraphical patterns in total organic and inorganic carbon (TOC, TIC), biogenic silica (BS) and total nitrogen (TN) over the past 1400 years. In this hydrologically closed lake, TIC variations may re‘ ect changes in the precipitation/evaporation ratio, which controls the evaporative enrichment of carbonate. TOC, BS and TN i…
Spectral analysis of a 1000-year stalagmite lamina-thickness record from Shihua Cavern, Beijing, China, and its climatic significance
Open AccessXiaoguang Qin, Ming Tan et al.ARTICLEThe Holocene1999Citada por: 2Referências: 1
Stalagmite laminae provide a high-resolution geological record of climate change. In this paper, moving spectral analysis is used to analyse a stalagmite lamina thickness record to study climatic variability. It was found that the dominant cycles of the lamina thickness sequence are 2, 3.3, 5–6, 10–12, 14–18, 133 and 194 years. Some of the cycles are the same as the cycles of modern climatic indices, such as the QBO (Quasi Biennial Oscillation) o…
Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve
Open AccessChengde Shen, Weixi Yi et al.ARTICLERadiocarbon2001Citada por: 1Referências: 12
We report here first results on the bulk soil organic carbon (SOC), apparent radiocarbon ages and δ 13 C characteristics of the tropical and subtropical forest soil in Dinghushan Biosphere Reserve (DHSBR). The forest oxisol in Dinghushan has developed during the Holocene. The δ 13 C variation curves in all three profiles may be divided into two sections. The upper section from 0 to 40 cm has δ 13 C values varying from −27.4 to −24.1‰, −27.5 to −2…
C Dating of Terrestrial Moss in Tern Lake Deposits, Antarctica
Open AccessChengde Shen, Tungsheng Liu et al.ARTICLERadiocarbon1997Citada por: 1Referências: 6
Accurate radiocarbon ages were obtained from terrestrial moss from two drill holes in Tern Lake deposits, Antarctica, using liquid scintillation counting (LSC) and accelerator mass spectrometry (AMS). The results show that the lake deposits have been accumulating since the end of the last glacial epoch ca. 12,600 cal BP at the rate of 0.13–1.1 mm a -1 . We discuss the validity of 14 C ages of Antarctic lake deposits, with respect to the latitude …

A Review of the Multi-Disciplinary Scientific Research on the Qinghai-Xizang Plateau by Chinese Scientists in Recent Years
Tungsheng Liu, Liu Tung-Sheng et al.ARTICLEGeographical Journal1981
Liu Tung-Sheng, Sun Hung-Lieh, A Review of the Multi-Disciplinary Scientific Research on the Qinghai-Xizang Plateau by Chinese Scientists in Recent Years, The Geographical Journal, Vol. 147, No. 1 (Mar., 1981), pp. 23-26
Magnetostratigraphical dating of loess deposits in China
Open AccessFriedrich Heller, Tungsheng Liu et al.ARTICLENature1982
The paleosol complex S5 in the China Loess Plateau ? A record of climatic optimum during the last 1.2 Ma
Open AccessZhaolong An, An Zhisheng et al.ARTICLEGeoJournal1987
Remanence Characteristics of Different Magnetic Grain Size Categories at Xifeng, Central Chinese Loess Plateau
Open AccessXiuming Liu, Tim Rolph et al.ARTICLEQuaternary Research1994
Utilizing the thermal unblocking of low-temperature remanent magnetization in superparamagnetic (SP) ferrimagnets and the low-temperature demagnetization of multidomain (MD) magnetite remanences, the relative proportions of SP, MD, and singledomain (SD and SD-like) ferrimagnets are estimated in the topmost part of a loess section at Xifeng, China, which covers about the past 130,000 yr. SP ferrimagnets are commonly regarded as pedogenic (authigen…
Ice-Volume Forcing of East Asian Winter Monsoon Variations in the Past 800,000 Years
Open AccessZhongli Ding, Tungsheng Liu et al.ARTICLEQuaternary Research1995
Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio of 10 μm (%) can be used as an indicator of variations in intensity of the East Asian winter monsoon winds. Grain-size curves of the Baoji and Weinan sections show that this proxy indicator is very sensitive to loess-soil alterations. Analytical results also suggest that during soil-forming…
Biogenic Silica Record in Lake Biwa of Central Japan over the Past 145,000 Years
Open AccessJule Xiao, Yoshio Inouchi et al.ARTICLEQuaternary Research1997
The record of the biogenic silica flux (BSF, g cm −2 (10 3 yr) −1 ) in Lake Biwa reflects changes in diatom productivity in the lake and provides information regarding changes in paleoclimatic conditions. The BSF record of Lake Biwa demonstrates five periods over the past ca. 145,000 yr when the BSF values were significantly greater than 7.5 g cm −2 (10 3 yr) −1 , and five intervals when they were lower. The data imply that paleoclimatic conditio…
Eolian Quartz Flux to Lake Biwa, Central Japan, over the Past 145,000 Years
Open AccessJule Xiao, Yoshio Inouchi et al.ARTICLEQuaternary Research1997
Eolian quartz flux (EQF, g cm −2 (10 3 yr) −1 ) to Lake Biwa, central Japan, provides direct information on variations of the East Asian winter monsoon. Lake Biwa sediments spanning the past ca. 145,000 yr are characterized by two main periods when EQF values were significantly greater than 5.50 g cm −2 (10 3 yr) −1 , and two main intervals during which EQF values were lower. Two periods with EQF values >5.50 g cm −2 (10 3 yr) −1 occurred from ca…
Stable isotope composition of the carbonate concretion in loess and climate change
Open AccessJiamao Han, Edward Keppens et al.ARTICLEQuaternary International1997
The onset of extensive loess deposition around the G/M boundary in China and its palaeoclimatic implications
Open AccessZhongli Ding, Nat W Rutter et al.ARTICLEQuaternary International1997
C Dating of Terrestrial Moss in Tern Lake Deposits, Antarctica
Open AccessChengde Shen, Tungsheng Liu et al.ARTICLERadiocarbon1997Citada por: 1Referências: 6
Accurate radiocarbon ages were obtained from terrestrial moss from two drill holes in Tern Lake deposits, Antarctica, using liquid scintillation counting (LSC) and accelerator mass spectrometry (AMS). The results show that the lake deposits have been accumulating since the end of the last glacial epoch ca. 12,600 cal BP at the rate of 0.13–1.1 mm a -1 . We discuss the validity of 14 C ages of Antarctic lake deposits, with respect to the latitude …
Chinese Loess and the Paleomonsoon
Tungsheng Liu, Zhongli DingARTICLEAnnual Review of Earth and…1998
This paper presents a general review of the recent research advances of the East Asian paleomonsoon, based mainly on studies of the loess-soil sequences in the Chinese Loess Plateau. In the last 2.6 million years, the paleomonsoonal history may be divided into about 166 events on a time scale of the Earth's orbital variations. During the last glacial period, millenial-scale oscillations of the monsoon system were prominent, which can be fairly we…
Changes in Sand Content of Loess Deposits along a North–South Transect of the Chinese Loess Plateau and the Implications for Desert Variations
Open AccessZhongli Ding, Jimin Sun et al.ARTICLEQuaternary Research1999
Geological records have shown that the deserts east of the Helan Mountains in northern China were covered by grass during the Holocene Optimum, whereas during marine oxygen isotope stages 2 and 4 distribution of the deserts was almost the same as at present. The wide advance–retreat cycles of the deserts may have exerted an important control on grain-size changes in the loess of the Loess Plateau by altering the distance between the source and th…
Spectral analysis of a 1000-year stalagmite lamina-thickness record from Shihua Cavern, Beijing, China, and its climatic significance
Open AccessXiaoguang Qin, Ming Tan et al.ARTICLEThe Holocene1999Citada por: 2Referências: 1
Stalagmite laminae provide a high-resolution geological record of climate change. In this paper, moving spectral analysis is used to analyse a stalagmite lamina thickness record to study climatic variability. It was found that the dominant cycles of the lamina thickness sequence are 2, 3.3, 5–6, 10–12, 14–18, 133 and 194 years. Some of the cycles are the same as the cycles of modern climatic indices, such as the QBO (Quasi Biennial Oscillation) o…
Stratigraphic Evidence for the Uplift of the Tibetan Plateau between ∼1.1 and ∼0.9 myr Ago
Open AccessJimin Sun, Tungsheng LiuARTICLEQuaternary Research2000
Uplift of the Tibetan Plateau is manifest not only in widespread denudation, but also by an increased deposition rate of sediment, near or far from the exhumed regions. Our results indicate that the mass accumulation rate (MAR) of eolian dust increased between ∼1.1 and ∼0.9 myr ago. We associate this increase in MAR and median grain size with uplift of the Tibetan Plateau and its adjacent regions during this period. This Middle Pleistocene uplift…
Distribution of 14 C and 13 C in Forest Soils of the Dinghushan Biosphere Reserve
Open AccessChengde Shen, Weixi Yi et al.ARTICLERadiocarbon2001Citada por: 1Referências: 12
We report here first results on the bulk soil organic carbon (SOC), apparent radiocarbon ages and δ 13 C characteristics of the tropical and subtropical forest soil in Dinghushan Biosphere Reserve (DHSBR). The forest oxisol in Dinghushan has developed during the Holocene. The δ 13 C variation curves in all three profiles may be divided into two sections. The upper section from 0 to 40 cm has δ 13 C values varying from −27.4 to −24.1‰, −27.5 to −2…
Glacial environments on the Tibetan Plateau and global cooling
Open AccessTungsheng Liu, Xinshi Zhang et al.ARTICLEQuaternary International2002
The ‘Mediaeval Warm Period’ drought recorded in Lake Huguangyan, tropical South China
Open AccessGuoqiang Chu, Jiaqi Liu et al.ARTICLEThe Holocene2002Citada por: 3Referências: 3
The geochemistry of dated sediment cores from Lake Huguangyan (21°9′N, 110°17′E), tropical South China, reveals distinct stratigraphical patterns in total organic and inorganic carbon (TOC, TIC), biogenic silica (BS) and total nitrogen (TN) over the past 1400 years. In this hydrologically closed lake, TIC variations may re‘ ect changes in the precipitation/evaporation ratio, which controls the evaporative enrichment of carbonate. TOC, BS and TN i…
Evolution of megadunes and lakes in the Badain Jaran Desert, Inner Mongolia, China during the last 31,000 years
Open AccessXiaoping Yang, Tungsheng Liu et al.ARTICLEQuaternary International2003
Phytoliths as quantitative indicators for the reconstruction of past environmental conditions in China I
Open AccessHouyuan Lu, Hou-Yuan Lu et al.ARTICLEQuaternary Science Reviews2006