Dianbing Liu
Biographic Data
| ID | 6370364 |
|---|---|
| NAME | Dianbing Liu |
| GIVEN NAMES | Dianbing |
| FAMILY NAME | Liu |
| SIGNATURE | LIU D |
| AFFILIATIONS | Nanjing Normal University |
| ORCID | 0000-0002-2957-8434 |
| VERIFIED | Yes |
| TOTAL WORKS | 8 |
| TOTAL CITATIONS | 22 |
| AUTHOR COUNT | 8 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2010 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 1 |
Differential responses of Asian summer monsoon circulation and local hydroclimate during the Holocene
Insolation control of millennial-scale Asian summer monsoon changes evidenced by Chinese stalagmites δ18O records
A southern and northern control on speleothem-based Asian summer monsoon variability during MIS 4
A 20-year-resolution speleothem δ 18 O record from southern China reveals a detailed Asian summer monsoon (ASM) history between 73.6 and 62.3 ka. ASM changes during Interstadial 19 and late MIS 4 matched Greenland temperature variations but were antiphased with Antarctic temperatures. However, long-term strengthening of the ASM in early MIS 4 agrees well with the gradual Antarctic warming, when Greenland remained in a stable cold state. More spec…
Remote vs. local control on the Preboreal Asian hydroclimate and soil processes recorded by an annually-laminated stalagmite from Daoguan Cave, southern China
Strong coupling of centennial-scale changes of Asian monsoon and soil processes derived from stalagmite δ 18 O and δ 13 C records, southern China
The paleoclimate application of speleothem δ 13 C is influenced by site-specific processes. Here we present four stalagmite δ 13 C records from two caves in southern China, covering early and late Marine Isotope Stage (MIS) 3 and the Holocene, to investigate the spatio-temporal pattern of calcite δ 13 C changes and the relationship with Asian monsoon (AM) variability. In each growth period, precessional- to millennial-scale changes are clear in t…
Multi-scale Holocene Asian monsoon variability deduced from a twin-stalagmite record in southwestern China
We present two isotopic (δ 18 O and δ 13 C) sequences of a twin-stalagmite from Zhuliuping Cave, southwestern China, with 230 Th dates from 14.6 to 4.6 ka. The stalagmite δ 18 O record characterizes orbital- to decadal-scale variability of Asian summer monsoon (ASM) intensity, with the Holocene optimum period (HOP) between 9.8 and 6.8 ka BP which is reinforced by its co-varying δ 13 C data. The large multi-decadal scale amplitude of the cave δ 18…
Centennial-scale Asian Monsoon variability during the mid-Younger Dryas from Qingtian Cave, central China
The regional climate correlation within the Northern Hemisphere in the cold/dry mid-Younger Dryas event (YD) remains elusive. A key to unraveling this issue is sufficient knowledge of the detailed climate variability at the low latitudes. Here we present a high-resolution (3-yr) δ 18 O record of an annually laminated stalagmite from central China that reveals a detailed Asian monsoon (AM) history from 13.36 to 10.99 ka. The YD in this record is e…
A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China
High-resolution oxygen isotope (δ 18 O) profiles of six stalagmites from Sanbao Cave in Hubei province, central China, established with 1413 oxygen isotope data and 65 230 Th ages, provide a continuous history of East Asian Summer Monsoon (EASM) intensity for the period from 13—0.2 thousand years before present (ky BP, relative to AD 1950). The δ 18 O record includes four distinct stages in the evolution of the EASM: (1) an abrupt transition (~11…
A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China
High-resolution oxygen isotope (δ 18 O) profiles of six stalagmites from Sanbao Cave in Hubei province, central China, established with 1413 oxygen isotope data and 65 230 Th ages, provide a continuous history of East Asian Summer Monsoon (EASM) intensity for the period from 13—0.2 thousand years before present (ky BP, relative to AD 1950). The δ 18 O record includes four distinct stages in the evolution of the EASM: (1) an abrupt transition (~11…
A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China
High-resolution oxygen isotope (δ 18 O) profiles of six stalagmites from Sanbao Cave in Hubei province, central China, established with 1413 oxygen isotope data and 65 230 Th ages, provide a continuous history of East Asian Summer Monsoon (EASM) intensity for the period from 13—0.2 thousand years before present (ky BP, relative to AD 1950). The δ 18 O record includes four distinct stages in the evolution of the EASM: (1) an abrupt transition (~11…
Centennial-scale Asian Monsoon variability during the mid-Younger Dryas from Qingtian Cave, central China
The regional climate correlation within the Northern Hemisphere in the cold/dry mid-Younger Dryas event (YD) remains elusive. A key to unraveling this issue is sufficient knowledge of the detailed climate variability at the low latitudes. Here we present a high-resolution (3-yr) δ 18 O record of an annually laminated stalagmite from central China that reveals a detailed Asian monsoon (AM) history from 13.36 to 10.99 ka. The YD in this record is e…
Strong coupling of centennial-scale changes of Asian monsoon and soil processes derived from stalagmite δ 18 O and δ 13 C records, southern China
The paleoclimate application of speleothem δ 13 C is influenced by site-specific processes. Here we present four stalagmite δ 13 C records from two caves in southern China, covering early and late Marine Isotope Stage (MIS) 3 and the Holocene, to investigate the spatio-temporal pattern of calcite δ 13 C changes and the relationship with Asian monsoon (AM) variability. In each growth period, precessional- to millennial-scale changes are clear in t…
Multi-scale Holocene Asian monsoon variability deduced from a twin-stalagmite record in southwestern China
We present two isotopic (δ 18 O and δ 13 C) sequences of a twin-stalagmite from Zhuliuping Cave, southwestern China, with 230 Th dates from 14.6 to 4.6 ka. The stalagmite δ 18 O record characterizes orbital- to decadal-scale variability of Asian summer monsoon (ASM) intensity, with the Holocene optimum period (HOP) between 9.8 and 6.8 ka BP which is reinforced by its co-varying δ 13 C data. The large multi-decadal scale amplitude of the cave δ 18…
Remote vs. local control on the Preboreal Asian hydroclimate and soil processes recorded by an annually-laminated stalagmite from Daoguan Cave, southern China
A southern and northern control on speleothem-based Asian summer monsoon variability during MIS 4
A 20-year-resolution speleothem δ 18 O record from southern China reveals a detailed Asian summer monsoon (ASM) history between 73.6 and 62.3 ka. ASM changes during Interstadial 19 and late MIS 4 matched Greenland temperature variations but were antiphased with Antarctic temperatures. However, long-term strengthening of the ASM in early MIS 4 agrees well with the gradual Antarctic warming, when Greenland remained in a stable cold state. More spec…
Insolation control of millennial-scale Asian summer monsoon changes evidenced by Chinese stalagmites δ18O records
Differential responses of Asian summer monsoon circulation and local hydroclimate during the Holocene
Climatology (7 works) · Geography (7 works) · Geology and Paleoclimatology Research (7 works) · Holocene (7 works) · Cave (6 works) · East Asian Monsoon (6 works) · Monsoon (6 works) · Stalagmite (6 works) · Geological formations and processes (5 works) · Physical geography (5 works)