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Windrose

8 datasets found! (Query time: 17 ms)

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  1. Expedition 302 Scientists (2006): Results of foraminifer and ostracode analyses of the Neogene of Hole 302-M0001A
    Size:  14 data points
    https://doi.org/10.1594/PANGAEA.356558 - Score: 20.058
  2. Expedition 302 Scientists (2006): Results of foraminifer and ostracode analyses of the Neogene of Hole 302-M0003A
    Size:  26 data points
    https://doi.org/10.1594/PANGAEA.356560 - Score: 20.058
  3. Expedition 302 Scientists (2006): Results of foraminifer and ostracode analyses of the Neogene of Hole 302-M0002A
    Size:  19 data points
    https://doi.org/10.1594/PANGAEA.356559 - Score: 20.058
  4. Expedition 302 Scientists (2006): Results of foraminifer and ostracode analyses of Hole 302-M0002A
    Size:  154 data points
    https://doi.org/10.1594/PANGAEA.354722 - Score: 20.058
  5. Expedition 302 Scientists (2006): Results of foraminifer and ostracode analyses of Hole 302-M0004A
    Size:  218 data points
    https://doi.org/10.1594/PANGAEA.356557 - Score: 19.879
  6. Expedition 302 Scientists (2006): Results of foraminifer and ostracode analyses of the Neogene of Hole 302-M0004B
    Size:  4 data points
    https://doi.org/10.1594/PANGAEA.356561 - Score: 19.563
  7. Expedition 302 Scientists (2006): Results of foraminifer and ostracode analyses of the Neogene of Hole 302-M0004C
    Size:  25 data points
    https://doi.org/10.1594/PANGAEA.356562 - Score: 19.563
  8. Eynaud, F; Cronin, TM; Smith, SA et al. (2009): (Table 1) Late Pleistocene planktonic foraminifera of Hole 302-M0004C
    Abstract:  Planktonic foraminifera populations were studied throughout the top 25 meters of the IODP ACEX 302 Hole 4C from the central Arctic Ocean at a resolution varying from 5cm (at the top of the record) to 10cm. Planktonic foraminifera occur in high absolute abundances only in the uppermost fifty centimetres and are dominated by the taxa Neogloboquadrina pachyderma. Except for a few intermittent layers below this level,most samples are barren of calcareous microfossils.Within the topmost sediments, Neogloboquadrina pachyderma specimens present large morphological variability in the shape and number of chambers in the finalwhorl, chamber sphericity, size, and coiling direction. Five morphotypeswere identified among the sinistral (sin.) population (Nps-1 to Nps-5), including a small form (Nps-5) that is similar to a non-encrusted normal form also previously identified in the modern Arctic Ocean watermasses. […]
    Size:  943 data points
    https://doi.org/10.1594/PANGAEA.672078 - Score: 15.918

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