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  • 124-769A; 124-769B; DRILL; Drilling/drill rig; Joides Resolution; Leg124; Ocean Drilling Program; ODP; Sulu Sea  (1)
  • Compound-specific hydrogen isotopes
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  • 1
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    PANGAEA
    In:  Supplement to: Linsley, Braddock K; Dunbar, Robert G (1994): The late Pleistocene history of surface water d13C in the Sulu Sea: Possible relationship to Pacific deepwater d13C changes. Paleoceanography, 9(2), 317-340, https://doi.org/10.1029/93PA03216
    Publication Date: 2024-01-09
    Description: A reconstruction of late Pleistocene surface water carbon isotopic (delta13C) variability is presented from Ocean Drilling Program (ODP) site 769 in the Sulu Sea in the western tropical Pacific. The Sulu Sea is a shallowly silled back arc basin with a maximum sill depth of 420 m. Site 769 was drilled on a bathymetric high in 3643 m of water and has average late Pleistocene sedimentation rates of 8.5 cm/kyr. The oxygen isotope record (delta18O) of Globigerinoides ruber at site 769 shows a strong correlation with the SPECMAP stacked delta18O record, attesting to the continuity of sediment archive at the site. Surface delta13C displays consistent glacial-interglacial variability which averages ~0.9 per mil and has varied from 0.75 to 1.1 per mil over the last 800 kyr. Comparison to surface water delta13C records in the South China Sea and western tropical Pacific suggests that the glacial-interglacial surface delta13C variability is regional in scale. Planktonic delta13C data from ODP site 677 in the eastern Pacific is also coherent with the site 769. Additionally, we have found that the site 769 surface delta13C record is coherent at periods of 100 and 41 kyr with deepwater delta13C records from the Pacific. The highest correlation occurs with the deep eastern Pacific, where benthic delta13C data from cores RC13-110 and ODP site 677 closely match the Sulu Sea surface water record. We evaluate several possible controls of surface water delta13C in the Sulu Sea that may explain the coherent timing with Pacific deepwater delta13C records. These include variations in terrestrial organic matter flux to the basin, the upwelling of subsurface water and productivity changes, and the influx of western Pacific intermediate water to the Sulu Sea. Our preferred explanation involves a region of upper intermediate water upwelling in the far western Pacific which has been shown to outgas CO2 from subsurface waters into surface waters. Upwelling also occurs in the area of Panama Basin site 677. These equatorial upwelling zones could potentially provide a route by which Pacific intermediate water can modulate the delta13C composition of certain Pacific surface water locations. Future reconstructions of late Pleistocene surface water delta13C variability in the western Pacific and Indonesian seas will be required to further evaluate the source of the glacial-interglacial surface water delta13C change.
    Keywords: 124-769A; 124-769B; DRILL; Drilling/drill rig; Joides Resolution; Leg124; Ocean Drilling Program; ODP; Sulu Sea
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 25 (2010): PA1102, doi:10.1029/2009PA001871.
    Description: Instrumental data suggest that major shifts in tropical Pacific atmospheric dynamics and hydrology have occurred within the past century, potentially in response to anthropogenic warming. To better understand these trends, we use the hydrogen isotopic ratios of terrestrial higher plant leaf waxes (δDwax) in marine sediments from southwest Sulawesi, Indonesia, to compile a detailed reconstruction of central Indo-Pacific Warm Pool (IPWP) hydrologic variability spanning most of the last two millennia. Our paleodata are highly correlated with a monsoon reconstruction from Southeast Asia, indicating that intervals of strong East Asian summer monsoon (EASM) activity are associated with a weaker Indonesian monsoon (IM). Furthermore, the centennial-scale oscillations in our data follow known changes in Northern Hemisphere climate (e.g., the Little Ice Age and Medieval Warm Period) implying a dynamic link between Northern Hemisphere temperatures and IPWP hydrology. The inverse relationship between the EASM and IM suggests that migrations of the Intertropical Convergence Zone and associated changes in monsoon strength caused synoptic hydrologic shifts in the IPWP throughout most of the past two millennia.
    Description: This research was supported by the U.S. NSF, the Ocean and Climate Change Institute at WHOI, and a National Defense Science and Engineering Graduate Fellowship to J. Tierney.
    Keywords: Tropical Pacific climate ; Compound-specific hydrogen isotopes
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/postscript
    Format: application/pdf
    Format: text/plain
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