Gangjian Wei
Biographic Data
| ID | 4021556 |
|---|---|
| NAME | Gangjian Wei |
| GIVEN NAMES | Gangjian |
| FAMILY NAME | Wei |
| SIGNATURE | WEI G |
| AFFILIATIONS | State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China |
| ORCID | 0000-0002-9620-0087 |
| VERIFIED | Yes |
| TOTAL WORKS | 9 |
| TOTAL CITATIONS | 3 |
| WORKS AS AUTHOR | 9 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2009 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 1 |
Paleoceanographic records of intermediate water oxygenation variability in the northern South China Sea over the last 16,100 years
Monsoon-regulated marine carbon reservoir effect in the northern South China Sea
The ubiquitous marine radiocarbon reservoir effect (MRE) constrains the construction of reliable chronologies for marine sediments and the further comparison of paleoclimate records. Different reference values were suggested from various archives. However, it remains unclear how climate and MREs interact. Here we studied two pre-bomb corals from the Hainan Island and Xisha Island in the northern South China Sea (SCS), to examine the relationship …
A high-resolution sediment record of East Asian summer monsoon from the northern South China Sea spanning the past 7500 years
High-resolution Holocene marine sediment records are limited, which hampers our understanding of paleomonsoon evolution. Continental shelf sediment records are derived mainly from terrestrial weathering products and are thus often sensitive to paleoclimate variations. In this study, the grain size and magnetic mineral composition of a well-dated sediment core (YJ Core) from the northern inner shelf of the South China Sea (SCS) were analyzed to pr…
Northern South China Sea SST changes over the last two millennia and possible linkage with solar irradiance
El Niño–Southern Oscillation variability recorded in estuarine sediments of the Changjiang River, China
Enso variability around 2000 years ago recorded by Tridacna gigas δ 18 O from the South China Sea
The development of late Holocene coastal cooling in the northern South China Sea
Paleoenvironmental shifts and precipitation variations recorded in tropical maar lake sediments during the Holocene in Southern China
Tropical ocean–atmosphere system exerts powerful control on the precipitation variations around the Pacific Ocean area where interactions among monsoon system, Intertropical Convergence Zone (ITCZ) migration, and other tropical ocean circulations modulate the regional climate changes in centennial-scale. However, little high-resolution information is known about the paleoenvironment changes in this area during the Holocene. In this study, a compo…
Paleoprecipitation record from coral Sr/Ca and δ18O during the mid Holocene in the northern South China Sea
Coupled high-resolution Sr/Ca and δ 18 O records of a modern and a mid-Holocene coral from Sanya in the southern Hainan Island, northern South China Sea (SCS), were reported and the residual δ 18 O (Δδ 18 O) were calculated to indicate precipitation change in this region. Unlike other paleoclimate studies, this study focused on changes of precipitation time rather than precipitation amount. As negative Δδ 18 O peaks in coral generally correspond …
Paleoenvironmental shifts and precipitation variations recorded in tropical maar lake sediments during the Holocene in Southern China
Tropical ocean–atmosphere system exerts powerful control on the precipitation variations around the Pacific Ocean area where interactions among monsoon system, Intertropical Convergence Zone (ITCZ) migration, and other tropical ocean circulations modulate the regional climate changes in centennial-scale. However, little high-resolution information is known about the paleoenvironment changes in this area during the Holocene. In this study, a compo…
Paleoprecipitation record from coral Sr/Ca and δ18O during the mid Holocene in the northern South China Sea
Coupled high-resolution Sr/Ca and δ 18 O records of a modern and a mid-Holocene coral from Sanya in the southern Hainan Island, northern South China Sea (SCS), were reported and the residual δ 18 O (Δδ 18 O) were calculated to indicate precipitation change in this region. Unlike other paleoclimate studies, this study focused on changes of precipitation time rather than precipitation amount. As negative Δδ 18 O peaks in coral generally correspond …
Paleoprecipitation record from coral Sr/Ca and δ18O during the mid Holocene in the northern South China Sea
Coupled high-resolution Sr/Ca and δ 18 O records of a modern and a mid-Holocene coral from Sanya in the southern Hainan Island, northern South China Sea (SCS), were reported and the residual δ 18 O (Δδ 18 O) were calculated to indicate precipitation change in this region. Unlike other paleoclimate studies, this study focused on changes of precipitation time rather than precipitation amount. As negative Δδ 18 O peaks in coral generally correspond …
The development of late Holocene coastal cooling in the northern South China Sea
Paleoenvironmental shifts and precipitation variations recorded in tropical maar lake sediments during the Holocene in Southern China
Tropical ocean–atmosphere system exerts powerful control on the precipitation variations around the Pacific Ocean area where interactions among monsoon system, Intertropical Convergence Zone (ITCZ) migration, and other tropical ocean circulations modulate the regional climate changes in centennial-scale. However, little high-resolution information is known about the paleoenvironment changes in this area during the Holocene. In this study, a compo…
Northern South China Sea SST changes over the last two millennia and possible linkage with solar irradiance
El Niño–Southern Oscillation variability recorded in estuarine sediments of the Changjiang River, China
Enso variability around 2000 years ago recorded by Tridacna gigas δ 18 O from the South China Sea
A high-resolution sediment record of East Asian summer monsoon from the northern South China Sea spanning the past 7500 years
High-resolution Holocene marine sediment records are limited, which hampers our understanding of paleomonsoon evolution. Continental shelf sediment records are derived mainly from terrestrial weathering products and are thus often sensitive to paleoclimate variations. In this study, the grain size and magnetic mineral composition of a well-dated sediment core (YJ Core) from the northern inner shelf of the South China Sea (SCS) were analyzed to pr…
Monsoon-regulated marine carbon reservoir effect in the northern South China Sea
The ubiquitous marine radiocarbon reservoir effect (MRE) constrains the construction of reliable chronologies for marine sediments and the further comparison of paleoclimate records. Different reference values were suggested from various archives. However, it remains unclear how climate and MREs interact. Here we studied two pre-bomb corals from the Hainan Island and Xisha Island in the northern South China Sea (SCS), to examine the relationship …
Paleoceanographic records of intermediate water oxygenation variability in the northern South China Sea over the last 16,100 years
Climatology (8 works) · Geology (8 works) · Geology and Paleoclimatology Research (8 works) · Oceanography (8 works) · Sea surface temperature (6 works) · Geological formations and processes (5 works) · Holocene (5 works) · Monsoon (5 works) · Environmental Science (4 works) · Geological and Geophysical Studies (4 works)