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  • 1
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    Major element composition of IODP Site U1501 in the South China Sea from 5.2 to 5.8 Ma (2021)
    PANGAEA
    Details
    Publication Date: 2023-06-27
    Description: IODP Site U1501 (18°53.09′N, 115°45.95′E, water depth: 2846 m) is situated on the west side of Pearl River Canyon. The length for hole C at IODP Site U1501 is up to 461.8 m, covering the last 40 Ma (Jian et al., 2018; Ma et al., 2019). 31 samples were selected at 20 cm intervals from the interval from 92.86 to 99.29 m, which spans from 5.2-5.8 Ma (Jian et al., 2018). All 31 samples of IODP Site U1501 are analyzed by inductively coupled plasma-optical emission (ICP-OES) to acquire the major elemental contents in Peking University during June 2021. We use the major element data to calculate the provenance proxies (Hu et al., 2021), then further discuss the change of Taiwan input during the late Miocene.
    Keywords: 368-U1501C; AGE; Aluminium oxide; Calcium oxide; deep sea sediment; DEPTH, sediment/rock; Exp368; ICP-OES, Inductively coupled plasma - optical emission spectrometry; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Late Miocene; Magnesium oxide; Major element; Phosphorus pentoxide; Potassium oxide; Sodium oxide; South China Sea; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 217 data points
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  • 2
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    (Appendix 1) Stable carbon and oxygen isotope ratios of planktonic foraminifera in surface sediments of the South China Sea (2005)
    PANGAEA
    Details
    Publication Date: 2023-12-18
    Keywords: DEPTH, sediment/rock; Elevation of event; Event label; Giant box corer; GIK17920-1; GIK17921-1; GIK17924-1; GIK17925-2; GIK17926-2; GIK17927-1; GIK17928-2; GIK17929-1; GIK17930-1; GIK17931-1; GIK17932-1; GIK17933-2; GIK17934-1; GIK17935-2; GIK17937-1; GIK17938-1; GIK17939-1; GIK17940-1; GIK17941-1; GIK17942-1; GIK17943-1; GIK17944-1; GIK17945-1; GIK17946-1; GIK17947-2; GIK17948-1; GIK17949-1; GIK17950-1; GIK17951-1; GIK17952-2; GIK17954-1; GIK17955-1; GIK17956-1; GIK17957-1; GIK17958-1; GIK17959-1; GIK17960-1; GIK17961-1; GIK17962-1; GIK17963-2; GIK17964-1; GIK17965-1; GIK18267-1; GIK18268-1; GIK18284-2; GIK18285-1; GIK18286-1; GIK18287-1; GIK18288-1; GIK18289-1; GIK18290-1; GIK18291-1; GIK18292-1; GIK18293-1; GIK18294-1; GKG; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Globigerinoides sacculifer, δ13C; Globigerinoides sacculifer, δ18O; Latitude of event; Longitude of event; Mass spectrometer Finnigan MAT 252; MONITOR MONSUN; MUC; MultiCorer; Pulleniatina obliquiloculata, δ13C; Pulleniatina obliquiloculata, δ18O; SO115; SO115_20; SO115_21; SO115_37; SO115_38; SO115_39; SO115_40; SO115_41; SO115_42; SO115_43; SO115_44; SO115_45; SO115_46; SO115_47; SO95; Sonne; South China Sea; SUNDAFLUT; Sunda Shelf
    Type: Dataset
    Format: text/tab-separated-values, 606 data points
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  • 3
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    Age models, clay minerals and major element concentrations of sediment cores DLW3101, MD12-3429 and MD12-3432 in the South China Sea since 150 ka (2020)
    PANGAEA
    Details
    Publication Date: 2023-12-15
    Description: The source-to-sink system of the northern South China Sea (SCS) has been widely discussed during the past few decades, but little is known about the transport processes and the controlling mechanisms on different spatiotemporal scales. Here, we study the spatiotemporal changes in sediment depositional patterns on the northern SCS continental slope since 150 ka using major element, clay mineralogy and grain size data from four sediment sites. Although the changes in major element composition are strongly related to mineral content variations, few studies have focused on the relationship between element compositions and provenance changes. We presents the major element compositions from three sites that cover the full depth range of the northern South China Sea slope. The results indicate that the most significant control on element composition is provenance change. Elemental and mineral contents are used to reconstruct the spatiotemporal patterns of sediment deposition over the last 150 kyr. And we infer that the ocean currents, bathymetry, sea level and monsoon control sediment depositional processes here on different spatiotemporal scales.
    Keywords: Age model; Clay mineral; Element concentration; South China Sea
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 4
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    Clay mineral composition of sediment core DLW3101 in the South China Sea since 150 ka (2020)
    PANGAEA
    Details
    Publication Date: 2023-12-15
    Keywords: AGE; Age model; Chlorite; Clay mineral; Core; CORE; DEPTH, sediment/rock; DLW3101; Element concentration; Illite; Illite chemistry index; Illite crystallinity; Kaolinite; Smectite; South China Sea
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 5
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    Age model of sediment core DLW3101 in the South China Sea since 150 ka (2020)
    PANGAEA
    Details
    Publication Date: 2023-12-15
    Keywords: Age model; Clay mineral; Core; CORE; DEPTH, sediment/rock; DLW3101; Element concentration; Sedimentation rate; South China Sea
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 6
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    Age model of sediment core MD12-3429 in the Sourh China Sea since 150 ka (2020)
    PANGAEA
    Details
    Publication Date: 2023-12-15
    Keywords: Age model; CIRCEA; Clay mineral; Core; CORE; DEPTH, sediment/rock; Element concentration; Marion Dufresne (1995); MD12-3429; MD190; Sedimentation rate; South China Sea
    Type: Dataset
    Format: text/tab-separated-values, 19 data points
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  • 7
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    Major element composition of sediment core MD12-3429 in the Sourh China Sea since 150 ka (2020)
    PANGAEA
    Details
    Publication Date: 2023-12-15
    Keywords: AGE; Age model; Aluminium oxide; Calcium oxide; CIRCEA; Clay mineral; Core; CORE; DEPTH, sediment/rock; Element concentration; Magnesium oxide; Marion Dufresne (1995); MD12-3429; MD190; Phosphorus pentoxide; Potassium oxide; Sodium oxide; South China Sea; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 350 data points
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  • 8
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    Major element composition of sediment core DLW3101 in the South China Sea since 150 ka (2020)
    PANGAEA
    Details
    Publication Date: 2023-12-15
    Keywords: AGE; Age model; Aluminium oxide; Calcium oxide; Clay mineral; Core; CORE; DEPTH, sediment/rock; DLW3101; Element concentration; Magnesium oxide; Phosphorus pentoxide; Potassium oxide; Sodium oxide; South China Sea; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 854 data points
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  • 9
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    Major element composition of sediment core MD12-3432 in the Sourh China Sea since 150 ka (2020)
    PANGAEA
    Details
    Publication Date: 2023-12-15
    Keywords: AGE; Age model; Aluminium oxide; Calcium oxide; CALYPSO; Calypso Corer; CIRCEA; Clay mineral; DEPTH, sediment/rock; Element concentration; Magnesium oxide; Marion Dufresne (1995); MD12-3432; MD190; Phosphorus pentoxide; Potassium oxide; Sodium oxide; South China Sea; Titanium dioxide
    Type: Dataset
    Format: text/tab-separated-values, 700 data points
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  • 10
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    Stable carbon and oxygen isotope ratios of foraminifera in surface sediments of the South China Sea (2005)
    PANGAEA
    In:  Supplement to: Cheng, Xinrong; Huang, Baoqi; Jian, Zhimin; Zhao, Quanhong; Tian, Jun; Li, Jianru (2005): Foraminiferal isotopic evidence for monsoonal activity in the South China Sea: a present-LGM comparison. Marine Micropaleontology, 54(1-2), 125-139, https://doi.org/10.1016/j.marmicro.2004.09.007
    Details
    Publication Date: 2024-01-09
    Description: The relationship between planktonic and benthic foraminiferal stable-isotope values and oceanographic conditions and factors controlling isotopic variations are discussed on the basis of oxygen and carbon isotopic analyses of 192 modern surface and Last Glacial Maximum (LGM) samples from the South China Sea (SCS). The harmonic variation of benthic delta18O in surface sediments with water depth and temperature implies that the temperature is the main factor influencing benthic delta18O variations. Planktonic delta18O fluctuates with sea surface temperature (SST) and salinity (SSS). The N-S temperature gradient results in planktonic delta18O decreasing from the northeast to the south. Cool, saline waters driven by the winter monsoon are interpreted to have been responsible for the high delta18O values in the northeast SCS. The East Asian monsoons not only bring nutrients into the South China Sea and maintain high nutrient concentration levels at the southwestern and northeastern ends, which cause depleted delta13C both in planktonic (surface) and benthic (bottom) samples but also reduce planktonic/benthic delta18O differences. The distribution of delta18O and delta13C in the surface and LGM samples are strikingly similar, indicating that the impact of SST and SSS has been maintained, and nutrient inputs, mainly from the northeastern and southwestern ends, have been controlled by monsoons since the LGM. Comparisons of the modern and LGM delta18O indicate a difference of about 3.6 °C in bottom-water temperature and a large surface-to-bottom temperature gradient during the LGM as compared to today.
    Keywords: 184-1143; COMPCORE; Composite Core; Giant box corer; GIK17920-1; GIK17921-1; GIK17924-1; GIK17925-2; GIK17926-2; GIK17927-1; GIK17928-2; GIK17929-1; GIK17930-1; GIK17931-1; GIK17932-1; GIK17933-2; GIK17934-1; GIK17935-2; GIK17937-1; GIK17938-1; GIK17939-1; GIK17940-1; GIK17941-1; GIK17942-1; GIK17943-1; GIK17944-1; GIK17945-1; GIK17946-1; GIK17947-2; GIK17948-1; GIK17949-1; GIK17950-1; GIK17951-1; GIK17952-2; GIK17954-1; GIK17955-1; GIK17956-1; GIK17957-1; GIK17958-1; GIK17959-1; GIK17960-1; GIK17961-1; GIK17962-1; GIK17963-2; GIK17964-1; GIK17965-1; GIK18267-1; GIK18268-1; GIK18284-2; GIK18285-1; GIK18286-1; GIK18287-1; GIK18288-1; GIK18289-1; GIK18290-1; GIK18291-1; GIK18292-1; GIK18293-1; GIK18294-1; GKG; Joides Resolution; Leg184; MONITOR MONSUN; MUC; MultiCorer; Ocean Drilling Program; ODP; SO115; SO115_20; SO115_21; SO115_37; SO115_38; SO115_39; SO115_40; SO115_41; SO115_42; SO115_43; SO115_44; SO115_45; SO115_46; SO115_47; SO95; Sonne; South China Sea; SUNDAFLUT; Sunda Shelf
    Type: Dataset
    Format: application/zip, 2 datasets
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