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  • 160-963A; AGE; Counting 〉125 µm fraction; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Globigerina bulloides; Globigerinita glutinata; Globigerinoides ruber; Globorotalia inflata; Globorotalia scitula dextral; Globorotalia scitula sinistral; Globorotalia truncatulinoides; Globoturborotalita tenella; Hastigerina siphonifera; Joides Resolution; Leg160; Neogloboquadrina dutertrei; Neogloboquadrina pachyderma dextral; Neogloboquadrina pachyderma sinistral; Ocean Drilling Program; ODP; Orbulina spp.; Sample code/label; Stainforthia davisi; Strait of Sicilia; Turborotalia quinqueloba  (1)
  • Elemental ratios
  • 2005-2009  (2)
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  • 2005-2009  (2)
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  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © Elsevier B.V., 2008. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Chemical Geology 257 (2008): 240-246, doi:10.1016/j.chemgeo.2008.10.002.
    Description: Sediments of the upper 28.2 meters of Ocean Drilling Program (ODP) Site 1145 from the northern South China Sea (SCS) were analyzed for their geochemical composition. Most of the major and trace elements exhibit significant fluctuations at glacial-interglacial scales, implying a close relation with regional and global climate change. Al-normalized elemental ratios can be subdivided into three principal components (PC). PC1 (e.g., Ca/Al, Ba/Al, Sr/Al) displays significant glacial-interglacial variation and is related to paleoproductivity in the northern SCS. PC2 (e.g., K/Al, Mg/Al, Rb/Al) is associated with the degree of chemical weathering in the source regions and shows little glacial-interglacial variation. PC3 (e.g., Ti/Al, Zr/Al) reflects the relative contribution of coarse- and fine-grained materials in the terrigenous components of the SCS sediments, likely associated with changes in sea level and monsoon-induced fluvial input. Spectral analyses indicate that paleoproductivity (i.e., Ba/Al) in the South China Sea lags Hulu/Sanbao speleothem δ18O record (a indicator of annual average meteoric precipitation) by 102° and Indian summer monsoon (multi-proxy stack) by 23° at the precession band, indicating a close relationship with the Indian summer monsoon. However, the chemical weathering degree in the source area (PC2) is not sensitive to monsoon-related changes at the precession band during the last climatic cycle.
    Description: This study was supported by the NSFC to Y.B. Sun and the US NSF to D.W. Oppo (OCE 0502960) and S.C. Clemens (OCE 0352215).
    Keywords: South China Sea ; Major and trace elements ; Elemental ratios ; East Asian monsoon
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
    Location Call Number Expected Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Sprovieri, Rodolfo; Di Stefano, Enrico; Incarbona, Alessandro; Oppo, Delia W (2006): Suborbital climate variability during Marine Isotopic Stage 5 in the central Mediterranean basin: evidence from calcareous plankton record. Quaternary Science Reviews, 25(17-18), 2332-2342, https://doi.org/10.1016/j.quascirev.2006.01.035
    Publication Date: 2024-01-09
    Description: New faunal and floral records from Ocean Drilling Project Hole 963A, resolved at ?80-year spacing, provide evidence of suborbital scale climate variability in the central Mediterranean Sea throughout Marine Isotope Stage (MIS) 5. Cold events in the central Mediterranean Sea, indicated by low abundances of warm species and high abundances of cold species, are also evident in a planktonic foraminifera paleoclimatic curve. They have been linked to NGRIP Greenland ice core “C” events and appear correlative with similar sub-millennial climate fluctuations identified in the North Atlantic region and in the Alboran Basin (Westernmost Mediterranean). Low-resolution benthic and planktonic Oxygen Isotope fluctuations parallel trends in the surface records evidenced by planktonic assemblage fluctuations, bolstering their interpretation as climate proxies. Climate events also occur in the Mediterranean between named “C” events, and may be coeval with additional climate events identified recently in the western subtropical Atlantic. Hence, we propose that frequent climate oscillations during MIS 5 characterize both sides of the mid-latitude North Atlantic, perhaps indicating millennial scale variations in mid-latitude atmospheric patterns.
    Keywords: 160-963A; AGE; Counting 〉125 µm fraction; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Globigerina bulloides; Globigerinita glutinata; Globigerinoides ruber; Globorotalia inflata; Globorotalia scitula dextral; Globorotalia scitula sinistral; Globorotalia truncatulinoides; Globoturborotalita tenella; Hastigerina siphonifera; Joides Resolution; Leg160; Neogloboquadrina dutertrei; Neogloboquadrina pachyderma dextral; Neogloboquadrina pachyderma sinistral; Ocean Drilling Program; ODP; Orbulina spp.; Sample code/label; Stainforthia davisi; Strait of Sicilia; Turborotalia quinqueloba
    Type: Dataset
    Format: text/tab-separated-values, 12896 data points
    Location Call Number Expected Availability
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