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  • 1
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    PANGAEA
    In:  Supplement to: Wei, Gangjian; Deng, Wenfeng; Yu, Kefu; Li, Xian-hua; Sun, Weidong D; Zhao, Jian-Xin (2007): Sea surface temperature records in the northern South China Sea from mid-Holocene coral Sr/Ca ratios. Paleoceanography, 22(3), PA3206, https://doi.org/10.1029/2006PA001270
    Publication Date: 2023-05-12
    Description: Three mid-Holocene sea surface temperature (SST) records spanning more than 30 years were reconstructed for the northern South China Sea using Sr/Ca ratios in Porites corals. The results indicate warmer than present climates between circa 6100 yr B.P. and circa 6500 yr B.P. with the mid-Holocene average minimum monthly winter SSTs, the average maximum monthly summer SSTs, and the average annual SSTs being about 0.5°-1.4°C, 0°-2.0°C, and 0.2°-1.5°C higher, respectively, than they were during 1970-1994. Summer SSTs decrease from circa 6500 yr B.P. to circa 6100 yr B.P. with a minimum centered at circa 6300 yr B.P. The higher average summer SSTs are consistent with a stronger summer monsoon during the mid-Holocene, and the decreasing trend indicates a secular decrease of summer monsoon strength, which reflects the change in summer insolation in the Northern Hemisphere. El Niño-Southern Oscillation (ENSO) cycles were apparent in both the mid-Holocene coral and modern instrumental records. However, the ENSO variability in the mid-Holocene SSTs was weaker than that in the modern record, and the SST record with the highest summer temperatures from circa 6460 yr B.P. to 6496 yr B.P. shows no robust ENSO cycle. This agrees with other studies that indicate that stronger summer monsoon circulation may have been associated with suppressed ENSO variability during the mid-Holocene.
    Keywords: CHEM; Chemistry; Dadonghai; Hainan Island, China
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 2
    Publication Date: 2023-05-12
    Keywords: Age, dated; Age, dated standard deviation; Age, Thorium; CHEM; Chemistry; Dadonghai; Hainan Island, China; Sample code/label; Thorium-230/Thorium-232 ratio; Thorium-230/Uranium-238, error, relative; Thorium-230/Uranium-238 ratio; Thorium-232; Uranium; Uranium, standard deviation; Uranium-234/Uranium-238 activity ratio; Uranium-234/Uranium-238 activity ratio, standard deviation; δ234 Uranium; δ234 Uranium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 45 data points
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  • 3
    Publication Date: 2023-05-12
    Keywords: Calculated; CHEM; Chemistry; Dadonghai; Hainan Island, China; Porites lutea, Strontium/Calcium ratio; Sample code/label; Sea surface temperature, annual mean
    Type: Dataset
    Format: text/tab-separated-values, 7005 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Li, Xian-hua; Wei, Gangjian; Shao, Lei; Liu, Ying; Liang, Xirong; Jian, Zhimin; Sun, Min; Wang, Pinxian (2003): Geochemical and Nd isotopic variations in sediments of the South China Sea: a response to Cenozoic tectonism in SE Asia. Earth and Planetary Science Letters, 211(3-4), 207-220, https://doi.org/10.1016/S0012-821X(03)00229-2
    Publication Date: 2024-01-09
    Description: Secular variations in geochemistry and Nd isotopic data have been documented in sediment samples at ODP Site 1148 in the South China Sea. Major and trace elements show significant changes at ca. 29.5 Ma and 26-23 Ma, whereas epsilon-Nd values show a single change at ca. 26-23 Ma. Increases in Al/Ti, Al/K, Rb/Sr, and La/Lu ratios and a decrease in the Th/La ratio of the sediments beginning at 29.5 Ma are consistent with more intense chemical weathering in the source region. The abrupt change in Nd isotopes and geochemistry at ca. 26-23 Ma coincides with a major discontinuity in the sedimentology and physical properties of the sediments, implying a drastic change in sedimentary provenance and environment at the drill site. Comparison of the Nd isotopes of sediments from major rivers flowing into the South China Sea suggests that pre-27 Ma sediments were dominantly derived from a southwestern provenance (Indochina-Sunda Shelf and possibly northwestern Borneo), whereas post-23 Ma sediments were derived from a northern provenance (South China). This change in provenance from southwest to north was largely caused by ridge jumping during seafloor spreading of the South China Sea, associated with a southwestward expansion of the ocean basin crust and a global rise in sea level. Thus, the geochemical and Nd isotopic changes in the sediments at ODP Site 1148 are interpreted as a response to a major plate reorganization in SE Asia at ca. 25 Ma.
    Keywords: 184-1144A; 184-1148; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg184; Ocean Drilling Program; ODP; South China Sea
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
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    PANGAEA
    In:  Supplement to: Wei, Gangjian; Li, Xian-hua; Liu, Ying; Shao, Lei; Liang, Xirong (2006): Geochemical record of chemical weathering and monsoon climate change since the early Miocene in the South China Sea. Paleoceanography, 21(4), PA4214, https://doi.org/10.1029/2006PA001300
    Publication Date: 2024-01-09
    Description: The chemical index of alteration (CIA) and elemental ratios that are sensitive to chemical weathering, such as Ca/Ti, Na/Ti, Al/Ti, Al/Na, Al/K, and La/Sm, were analyzed for detrital sediments at Ocean Drilling Program Site 1148 from the northern South China Sea to reveal information of chemical weathering in the source regions during the early Miocene. High CIA values of ~80, coupled with high Al/Ti and Al/Na and low Na/Ti and Ca/Ti, are observed for the sediments at ~23 Ma, indicating a high chemical weathering intensity in the north source region, i.e., south China. This was followed by gradual decreases in Al/Ti, Al/Na, La/Sm, and Al/K ratios, as well as the CIA values, and increases in Ca/Ti and Na/Ti ratios. These records together with other paleoclimate proxies, such as black carbon d13C and benthic foraminifer d18O, give reliable information on the climate changes in south China. Our results show that the climate in south China was warm and humid in the early Miocene (~23 Ma) according to the chemical weathering records. The humidity in south China decreased from the early Miocene to Present with several fluctuations centering at approximately 15.7 Ma, 8.4 Ma, and 2.5 Ma, coincident with the global cooling since the middle Miocene. These climate changes implied that the summer east Asian monsoon has dramatically affected south China in the early Miocene, whereas the influence of the summer monsoon on this region has decreased continuously since that time, probably because of the intensification of the winter monsoon. Such an evolution for the east Asian monsoon is different from that for the Indian monsoon.
    Keywords: 184-1148; AGE; Aluminium oxide; Calcium oxide; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Lanthanum; Leg184; Magnesium oxide; Ocean Drilling Program; ODP; Potassium oxide; Samarium; Scandium; Sodium oxide; South China Sea; Thorium; Titanium dioxide; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 946 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 184-1148; Age model; Ageprofile Datum Description; COMPCORE; Composite Core; DEPTH, sediment/rock; Joides Resolution; Leg184; Ocean Drilling Program; ODP; South China Sea
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 184-1144A; Area/locality; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Epoch; Event label; Joides Resolution; LATITUDE; Leg184; LONGITUDE; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; Ocean Drilling Program; ODP; Sample code/label; South China Sea; ε-Neodymium
    Type: Dataset
    Format: text/tab-separated-values, 150 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Wei, Gangjian; Liu, Ying; Li, Xian-hua; Shao, Lei; Fang, Dianyong (2004): Major and trace element variations of the sediments at ODP Site 1144, South China Sea, during the last 230 ka and their paleoclimate implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 212(3-4), 331-342, https://doi.org/10.1016/j.palaeo.2004.06.011
    Publication Date: 2024-04-16
    Description: We present here the major and trace element data of the sediments at ODP Site 1144 of the last 230 ka with time resolution about 1.5 kyr to investigate their relations to the climate changes. Estimated from TiO2 and CaO contents, over 70% in weight of the sediments are terrestrial materials, and CaCO3 abundance ranges between 7% and 19%. The variation patterns of some of the major elements, such as Al, Fe, K, Mg and Mn, and some of the trace elements, such as the alkali elements (such as Rb and Cs), the alkali earth elements (such as Ba) and most transition metals (such as Sc, V, Co, Cr, Zn), well match that of the oxygen isotopes of the planktonic foraminifer, after normalized with Ti, with higher values during interglacial periods and lower values during glacial periods. Whilst the Na abundance exhibits inverse variation patterns with lower values during interglacial periods and higher values during glacial periods. However, most refractory elements, such as Y, Zr, Nb, Hf, Ta, REEs, Th and U, do not show such patterns. These agree well with the behaviors of these elements during chemical weathering. Therefore, the changes of chemical weathering intensity in South China, the source area of these sediments may account for such variation patterns. During interglacials, wet and warm climate might occur at South China, which resulted in stronger chemical weathering, and dry climate might occur during glacials, which resulted in weaker chemical weathering. Such paleoclimate interpretation agrees with those from other paleoclimate proxies, such as pollen records, indicating that change of the East Asian monsoon, especially change of the winter monsoon is the key for such paleoclimate variation patterns.
    Keywords: 184-1144A; Barium; Caesium; Calcium oxide; Cerium; Chromium; Cobalt; Copper; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Dysprosium; Erbium; Europium; Gadolinium; Gallium; Germanium; Hafnium; Holmium; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Inductively coupled plasma - mass spectrometry (ICP-MS); Iron oxide, FeO; Joides Resolution; Lanthanum; Lead; Leg184; Lutetium; Magnesium oxide; Manganese oxide; Neodymium; Niobium; Ocean Drilling Program; ODP; Phosphorus pentoxide; Praseodymium; Rubidium; Samarium; Sodium oxide; South China Sea; Strontium; Tantalum; Terbium; Thorium; Thulium; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 4719 data points
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  • 9
    Publication Date: 2024-04-16
    Keywords: 184-1148; AGE; Aluminium oxide; Barium; Caesium; Calcium oxide; Cerium; Chromium; Cobalt; COMPCORE; Composite Core; Copper; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Dysprosium; Erbium; Europium; Gadolinium; Gallium; Hafnium; Holmium; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Iron oxide, FeO; Isotope ratio mass spectrometry; Joides Resolution; Lanthanum; Lead; Leg184; Lutetium; Magnesium oxide; Neodymium; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; Nickel; Niobium; Ocean Drilling Program; ODP; Phosphorus pentoxide; Potassium oxide; Praseodymium; Rubidium; Samarium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; South China Sea; Strontium; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Uranium; Vanadium; Ytterbium; Yttrium; Zinc; Zirconium; ε-Neodymium
    Type: Dataset
    Format: text/tab-separated-values, 7837 data points
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  • 10
    Publication Date: 2022-10-26
    Description: Author Posting. © American Geophysical Union, 2020. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Solid Earth 125(9),(2020): e2020JB020393, doi:10.1029/2020JB020393.
    Description: Fast diffusing Li isotopes provide important insights into the “recent” transient events or processes for both modern and ancient times, but questions remain concerning the large Li isotopic variations of mantle peridotites, which greatly hampers their usage as a geochemical tracer. This study investigates in situ Li content and isotopic profiles of the constituent minerals of abyssal peridotites from the Gakkel Ridge and Southwest Indian Ridge. The complicated and large variations of Li isotopic profiles in Clinopyroxene (Cpx) and Orthopyroxene (Opx) indicate Li isotopic disequilibrium at millimeter scale. The negative correlations of a wide range of Li contents (0.5 to 6.5 ppm) and δ7Li values (−10 to +20‰) of olivine, Opx and Cpx grains/relicts, trace element zoning of Cpx, the occurrence of plagioclase, olivine serpentinization along cracks, together with numerical modeling demonstrate the observed Li characteristics to be a manifestation of high‐temperature mineral‐melt Li diffusion during melt impregnation overprinted by low‐temperature mineral‐fluid Li diffusion during dissolution and serpentinization. The preservation of the Li isotopic diffusion profiles requires rapid cooling of 0.3–5°C/year after final‐stage melt impregnation at the Moho boundary, which is consistent with the low temperature at very slow spreadin g ridges caused by conductive cooling. Compared with the well‐studied melt‐rock interaction process, our study indicates that low‐temperature fluid‐rock interaction can induce Li diffusion even in the visibly unaltered mineral relicts of partially altered rocks.
    Description: This study was financially supported by the National Science Foundation of China (grant no. 41872058) and the U.S. National Science Foundation grant.
    Description: 2021-03-07
    Keywords: Li isotope ; Abyssal peridotite ; Isotope diffusion ; Melt‐rock interaction ; Fluid‐rock interaction
    Repository Name: Woods Hole Open Access Server
    Type: Article
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