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The silicoflagellate genus Distephanus ( Distephanopsis )

The silicoflagellate genus Distephanus ( Distephanopsis ). Robert Baldwin University Day April 14, 2010. What is a silicoflagellate ?.

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The silicoflagellate genus Distephanus ( Distephanopsis )

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  1. The silicoflagellategenus Distephanus (Distephanopsis) Robert Baldwin University Day April 14, 2010

  2. What is a silicoflagellate? “Silicoflagellates are protists and claimed both by zoologists (as protozoans) and botanists (as algae). However, due to their autotrophic phytoplanktonic nature it is more logical to regard them as planktonic algae.” “The silicoflagellates are minute (20−50 µm, rarely up to 100 µm), unicellar, marine flagellates with a siliceous skeleton.” Bilal U. Haq et al., 1978 “The silicoflagellates are a group of planktonicprotists, exclusively marine, that contain chromatophores for photosynthesis. In that respect they are like other ‘algae’. They possess a single flagellum, presumably to maintain proper orientation to the sun for maximum efficiency in photosynthetic production. Unlike other “algae”, however, they also possess pseudopodia – a fact that led several early scholars to classify them as ‘animals’.” Richard T. Carter, 2008

  3. How silicoflagellates are used Silicoflagellates are silica-secreting marine microplankton. “Recent revival of interest in the history of ocean basins and paleoclimates has enhanced their importance in paleooceanographic interpretations, especially in those areas where calcareous microfossils are either relatively scarce or completely lacking (e.g., in higher latitudes and deeper waters).” Bilal U. Haq et al., 1978 The carbonate compensation depth The reason why silica fossils are useful in deeper waters is because calcareous fossils dissolve below the calcite compensation depth. The calcite compensation depth (CCD), at the present time, is about 4200 to 4500 meters and can be 5000 meters deep in some places at the present time. It has not always been the same in the past. (Wikipedia)

  4. Skeletal Terminology Figure 1. Maximum length = 65 microns. Richard T. Carter, 2007

  5. Richard T. Carter, 2007

  6. Silicoflagellate descriptive terminology McCartney et al., 1990

  7. Distephanus speculum has a hollow skeleton Y. T. Mandra

  8. Distephanusspeculum with a double skeleton J. A. Barron

  9. McCartney et al., 1990

  10. McCartney et al., 1990

  11. McCartney et al., 1990

  12. Pseudofibula Plexus map McCartney et al., 1993

  13. pseudofibulid morphologies McCartney et al., 1990

  14. The second column shows the minimum-distance configuration that connects all points (from Almgren and Taylor, 1976; Isenberg, 1976). McCartney et al., 1990

  15. Scanning electron micrographs of specimens of the pseddofibula plexus from Leg 113, 100x. McCartney et al., 1990

  16. Pseudofibula Plexusof Distephanus speculum speculum from ODP Leg 113 McCartney et al., 1990

  17. Richard T. Carter, 2008

  18. Richard T. Carter, 2008

  19. Distribution of Dictyocha and Distephanus Dictyocha McCartney, 1995 Distephanus

  20. Multiwindowed morphologies and some many sided types from ODP Leg 113 McCartney et al., 1990

  21. Cretaceousgenera McCartney et al., 1990

  22. Wide band indicates relative abundance > 50 %. • Narrow band denotes relative abundance = 10 %. • Line indicates a regular presence. • Small numbers refer to DSDP Leg. McCartney, 1987

  23. Richard T. Carter, 2008

  24. Richard T. Carter, 2007

  25. Corbisematriacantha(Ehrenberg) McCartney et al., 1990

  26. Richard T. Carter, 2007

  27. Richard T. Carter, 2008

  28. Richard T. Carter, 2007

  29. Richard T. Carter, 2008

  30. Richard T. Carter, 2007

  31. Richard T. Carter, 2008

  32. Richard T. Carter, 2007

  33. DictyochacalidaPoelchau, abapical view McCartney et al., 1990

  34. Richard T. Carter, 2008

  35. Richard T. Carter, 2007

  36. Richard T. Carter, 2008

  37. Richard T. Carter, 2007

  38. Richard T. Carter, 2007

  39. Richard T. Carter, 2007

  40. Distephanusbolivensis McCartney et al., 1990

  41. Distephanuspolyactis 1973

  42. Cannopilushemisphaericus A Bachmann et al., 1963

  43. Cannopilushemisphaericus A Bachmann et al., 1963

  44. Richard T. Carter, 2008

  45. Cannopilussphaericus A Bachmann et al, 1963

  46. Cannopiluspicassori A Bachmann et al., 1963

  47. Cannopiluspicassori A Bachmann et al., 1963

  48. References: Silicoflagellate: Distephanus speculum, showing hollow skeleton. Upper Miocene near San Felipe, Baja California. Upper specimen is about 60 microns from spine tip to tip. Scanning electron micrograph. From Y. T. Mandra and H. Mandra, Occasional Papers of the California Academy of Sciences, no. 99. Used with the permission of Y. T. Mandra, San Francisco State University. Silicoflagellate: Distephanus speculum with a double skeleton. Late Miocene. Lompoc, California. Length is 45 microns. Courtesy of J. A. Barron, U. S. G. S. http://www.cushmanfoundation.org/resources/slides/silmicros.html • Carbonate compensation depth (Wikipedia) • This page was last modified on 21 February 2010 • http://en.wikipedia.org/wiki/Carbonate_compensation_depth

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