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Data

 
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Windrose

263 datasets found! (Query time: 3 ms)

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  1. Sluijs, A; Schouten, S; Donders, TH et al. (2010): Branched and isoprenoid tetraether (BIT) index, TEX86 and sea surface temperatures of IODP Hole 302-M0004A
    Related to:  Sluijs, A; Schouten, S; Donders, TH et al. (2009): Warm and wet conditions in the Arctic region during Eocene Thermal Maximum 2. Nature Geosciences
    Size:  1841 data points
    https://doi.org/10.1594/PANGAEA.735737 - Score: 15.312

  2. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 3) Tie points of Hole 302-M0003A
    Related to:  O'Regan, M; Sakamoto, T; King, JW (2008): Data report: Regional stratigraphic correlation and a revised composite depth scale for IODP Expedition 302. In: Backman, J., Moran, K., McInroy, D.B., Mayer, L.A., and the Expedition 302 Scientists, Proc. IODP, 302: Edinburgh (Integrated Ocean Drilling Program Management International, Inc.).
    Size:  87 data points
    https://doi.org/10.1594/PANGAEA.707035 - Score: 15.312

  3. Sluijs, A; Schouten, S; Donders, TH et al. (2010): X-ray fluorescence data of IODP Hole 302-M0004A
    Related to:  Sluijs, A; Schouten, S; Donders, TH et al. (2009): Warm and wet conditions in the Arctic region during Eocene Thermal Maximum 2. Nature Geosciences
    Size:  5531 data points
    https://doi.org/10.1594/PANGAEA.735713 - Score: 15.312

  4. Onodera, J; Takahashi, K (2012): (Appendix 1) Ebridian skeleton contents from IODP Exp302
    Related to:  Onodera, J; Takahashi, K (2009): Middle Eocene ebridians from the central Arctic Basin. Micropaleontology
    Size:  4970 data points
    https://doi.org/10.1594/PANGAEA.787376 - Score: 15.312

  5. Vogt, C (2008): Relative mineral abundances from bulk fraction X-ray diffraction data of Hole 302-M0004C
    Related to:  Vogt, C (2009): Data report: semiquantitative determination of detrital input to ACEX sites based on bulk sample X-ray diffraction data. In: Backman, J., Moran, K., McInroy, D.B., Mayer, L.A., and the Expedition 302 Scientists, Proc. IODP: Edinburgh (Integrated Ocean Drilling Program Management International, Inc.)
    Size:  13327 data points
    https://doi.org/10.1594/PANGAEA.704660 - Score: 15.312

  6. Stein, R (2007): Analysis of organic carbon from Hole 302-M0002A
    Related to:  Stein, R (2007): Upper Cretaceous/Lower Tertiary black shales near the North Pole: Organic-carbon origin and source-rock potential. Marine and Petroleum Geology
    Size:  2445 data points
    https://doi.org/10.1594/PANGAEA.548674 - Score: 15.312

  7. Sluijs, A; Schouten, S; Donders, TH et al. (2010): Palynological analyses of IODP Hole 302-M0004A
    Related to:  Sluijs, A; Schouten, S; Donders, TH et al. (2009): Warm and wet conditions in the Arctic region during Eocene Thermal Maximum 2. Nature Geosciences
    Size:  595 data points
    https://doi.org/10.1594/PANGAEA.735707 - Score: 15.312

  8. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 4) Correlation tie points of Exp302 (ACEX) composite depth scale and cores 96/12-1PC and PS2185-6
    Related to:  O'Regan, M; Sakamoto, T; King, JW (2008): Data report: Regional stratigraphic correlation and a revised composite depth scale for IODP Expedition 302. In: Backman, J., Moran, K., McInroy, D.B., Mayer, L.A., and the Expedition 302 Scientists, Proc. IODP, 302: Edinburgh (Integrated Ocean Drilling Program Management International, Inc.).
    Size:  60 data points
    https://doi.org/10.1594/PANGAEA.707039 - Score: 15.229

  9. Haley, BA; Frank, M; Spielhagen, RF et al. (2008): Neodymium and Strontium chemistry of IODP Exp302-Composite Site
    Related to:  Haley, BA; Frank, M; Spielhagen, RF et al. (2008): Influence of brine formation on Arctic Ocean circulation over the past 15 million years. Nature Geoscience
    Size:  138 data points
    https://doi.org/10.1594/PANGAEA.769603 - Score: 15.229

  10. O'Regan, M; King, JW; Backman, J et al. (2008): (Table S3) Possible ties beyond 1215 ka in the slower sedimentation rate age model of IODP Exp302 composite core
    Related to:  O'Regan, M; King, JW; Backman, J et al. (2008): Constraints on the Pleistocene chronology of sediments from the Lomonosov Ridge. Paleoceanography
    Size:  28 data points
    https://doi.org/10.1594/PANGAEA.832425 - Score: 15.229

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