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  • 2010-2014  (5)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Wan, Shiming; Tian, Jun; Steinke, Stephan; Li, Anchun; Li, Tiegang (2010): Evolution and variability of the East Asian summer monsoon during the Pliocene: Evidence from clay mineral records of the South China Sea. Palaeogeography, Palaeoclimatology, Palaeoecology, 293(1-2), 237-247, https://doi.org/10.1016/j.palaeo.2010.05.025
    Publication Date: 2024-01-09
    Description: The Late Pliocene is thought to be characterized by the simultaneous intensification of both the East Asian winter monsoon (EAWM) and East Asian summer monsoon (EASM). However, the evolution of the EASM during the Pliocene remains still controversial and only little is known about the dynamics of the EASM during the Pliocene on orbital time scales. Here we use clay mineral assemblages in sediments from Ocean Drilling Program (ODP) Site 1143 in the southern South China Sea (SCS) to obtain proxy records of past changes in the EASM climate during the Pliocene. Provenance analysis suggests that illite, chlorite and kaolinite originated mainly from the Mekong River drainage area. Smectite was derived mainly from the Indonesian islands. The kaolinite/illite ratio and the chemical index of alteration (CIA) of siliciclastic sediments allowed us to reconstruct the history of chemical weathering and physical erosion of the Mekong River drainage area and thus, the evolution of the EASM during the Pliocene. Our clay minerals proxy data suggests a stronger EASM during the Early Pliocene than during the Late Pliocene. We propose that the long-term evolution of the EASM has been driven by global cooling rather than the uplift of the Tibetan Plateau. Spectral analysis of kaolinite/illite ratio displays a set of strong periodicities at 100 ka, 30 ka, 28 ka, 25 ka, and 22 ka, with no clear obliquity-related signal. Our study suggests that the Pliocene EASM intensity on orbital time scales is not only controlled by the Northern Hemisphere summer insolation, but also strongly influenced by equatorial Pacific ENSO-like ocean-atmosphere dynamics.
    Keywords: 184-1143; AGE; Chlorite; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Illite; Illite, chemical index; Illite, full width at half maximum, 10Å; Joides Resolution; Kaolinite; Leg184; Ocean Drilling Program; ODP; Sample code/label; see reference(s); Smectite; South China Sea; X-ray diffraction (XRD)
    Type: Dataset
    Format: text/tab-separated-values, 4920 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-01-09
    Keywords: 184-1144; Accumulation rate, terrigenous; AGE; Calculated; Chlorite; COMPCORE; Composite Core; DEPTH, sediment/rock; Grain size, mean; Illite; Illite, chemical index; Illite, full width at half maximum, 10Å; Joides Resolution; Kaolinite; Leg184; Ocean Drilling Program; ODP; Smectite; South China Sea; X-ray diffraction, clay fraction
    Type: Dataset
    Format: text/tab-separated-values, 1192 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2024-01-09
    Keywords: 184-1146; Accumulation rate, terrigenous; AGE; Barium; Caesium; Calculated; Cerium; Chlorite; Chromium; Cobalt; COMPCORE; Composite Core; Copper; DEPTH, sediment/rock; Dysprosium; Erbium; Europium; Gadolinium; Gallium; Hafnium; Holmium; Illite; Illite, chemical index; Illite, full width at half maximum, 10Å; Inductively coupled plasma - mass spectrometry (ICP-MS); Joides Resolution; Kaolinite; Lanthanum; Lead; Leg184; Lutetium; Neodymium; Nickel; Niobium; Ocean Drilling Program; ODP; Praseodymium; Rubidium; Samarium; Scandium; Smectite; South China Sea; Strontium; Tantalum; Terbium; Thorium; Thulium; Uranium; Vanadium; X-ray diffraction, clay fraction; Ytterbium; Yttrium; Zinc; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 11255 data points
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Wan, Shiming; Li, Anchun; Clift, Peter D; Wu, Shiguo; Xu, Kehui; Li, Tiegang (2010): Increased contribution of terrigenous supply from Taiwan to the northern South China Sea since 3 Ma. Marine Geology, 278(1-4), 115-121, https://doi.org/10.1016/j.margeo.2010.09.008
    Publication Date: 2024-01-09
    Description: Seismic profiles provide evidence that there has been strong transport by deep-water bottom currents and drift deposition on the northern slope of the South China Sea. Earlier geochemical studies suggest that the drift sediments originated primarily from Taiwan. However, the transport process, history and origin of the deep-water bottom deposition in the northern South China Sea, on both glacial-interglacial and tectonic time scales, remain unclear. Here, we show new high-resolution records of clay minerals, grain size and mass accumulation rate (MAR) of terrigenous materials from Ocean Drilling Program (ODP) Site 1144, together with trace element concentrations in siliciclastic sediments from ODP Site 1146. Combined with other published data, we find that the primary source for sediments at ODP Sites 1144-1148 since 3 Ma is from Taiwan, and not from Pearl River as previously thought. Before 3 Ma, however, sediment source to ODP Sites 1146 and 1148 was mainly from the Pearl River. Increased contribution of terrigenous supply from Taiwan to the northern South China Sea since ~ 3 Ma may be related to the formation of the Taiwan orogen and strengthening of deep-water bottom current transport in the northern South China Sea. Variations in clay mineralogy and sedimentology at ODP Site 1144, located on a sediment drift, shows strong glacial-interglacial cyclicity. This suggests that bottom current deposition is highly dependent on sea-level fluctuations, which control the terrigenous supply to the deep sea.
    Keywords: 184-1144; 184-1146; COMPCORE; Composite Core; Joides Resolution; Leg184; Ocean Drilling Program; ODP; South China Sea
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 5
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    AGU (American Geophysical Union) | Wiley
    In:  Geochemistry, Geophysics, Geosystems, 14 (5). pp. 1538-1551.
    Publication Date: 2018-02-28
    Description: The radiogenic strontium (Sr) and neodymium (Nd) isotope compositions of the detrital fraction of surface and subsurface sediments have been determined to trace sediment provenance and contributions from Asian dust off the east coast of Luzon Islands in the western Philippine Sea. The Sr and Nd isotope compositions have been very homogenous near the east coast of the Luzon Islands during the latest Quaternary yielding relatively least radiogenic Sr (87Sr/86Sr = 0.70453 to 0.70491) and more radiogenic Nd isotope compositions (εNd(0) = +5.3 to +5.5). These isotope compositions are similar to Luzon rocks and show that these sediments were mainly derived from the Luzon Islands. In contrast, the Sr and Nd isotope compositions of sediments on the Benham Rise and in the Philippine Basin are markedly different in that they are characterized by overall more variable and more radiogenic Sr isotope compositions (87Sr/86Sr = 0.70452 to 0.70723) and less radiogenic Nd isotope compositions (εNd(0) = −5.3 to +2.4). The Sr isotope composition in the Huatung Basin is intermediate between those of the east coast of Luzon and Benham Rise, but shows the least radiogenic Nd isotope compositions. The data are consistent with a two end-member mixing relationship between Luzon volcanic rocks and eolian dust from the Asian continent, which is characterized by highly radiogenic Sr and unradiogenic Nd isotope compositions. The results show that Asian continental dust contributes about 10–50% of the detrital fraction of the sediments on Benham Rise in the western Philippine Sea, which offers the potentials to reconstruct the climatic evolution of eastern Asia from these sediments and compare this information to the records from the central and northern Pacific.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
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