Cape Johnson Guyot Explained

17.1333°N -192°W

Cape Johnson Guyot is a guyot in the Pacific Ocean, more precisely in the Mid-Pacific Mountains, and the type locality of guyots. It is of middle Cretaceous age and a number of fossils have been dredged from it.

Name

Cape Johnson Guyot is also known as Cape Johnson Seamount or Cape Johnson Tablemount.[1] The guyot was named by Harry Hammond Hess, after his ship the ; Hess had also named the kind of flat-topped seamount "guyot" and another seamount was named after Hess himself.[2] The seamount was first described in a 1946 publication.[3] Both Hess and Cape Johnson were discovered during the same cruise[4] and Cape Johnson Guyot is the type locality of guyots.[5]

Geography and geology

The seamount lies in the Mid-Pacific Mountains[6] on their southern side and is a submarine mountain with a flat top that rises[7] over 10000feet[8] to a depth of [9] [10] -.[11] The flat top has an oval shape and a surface area of 6x;[12] it is characterized by a limestone dome on the summit, buried beneath sediments; in turn a volcanic hill is buried within the limestone dome.[13] The top of the seamount has a hummocky appearance which has been interpreted as a sediment cover[14] and its southeastern sector has a bank-like shape that resembles that of an atoll.[15] Cape Johnson Guyot is considered to be of Middle Cretaceous age[16] with an age of 120 million years reported[17] and shallow-water fossils were emplaced on it at that time.[18]

Apatite,[19] basaltic sandstone containing hypersthene,[20] clay,[21] limestone, manganese crusts,[22] manganese oxide, phosphorite[23] and lithified carbonates have been found on Cape Johnson Guyot;[24] some carbonates of biogenic origin have been altered by apatite.[25] Globigerina ooze is also found on the seamount[26] and can reach substantial thickness; such accumulations might be formed by ocean currents.[27] Similar rocks have been found at other guyots of the Mid-Pacific Mountains.[28]

Biology

During the Cretaceous, corals and rudists lived on Cape Johnson Guyot[29] and fossils have been dated to 91-112 million years ago;[30] some corals[31] and rudists are of Albian to Cenomanian age.[32] Fossils of anthozoa,[33] gastropods, reef-building hexacorals,[34] pelecypods, stromatoporoids[35] and Tridacna were also found.[36] The Cretaceous fossils[37] Actinostroma pacifica,[38] Astrocoenia dietzi,[39] Brachyseris montemarina,[40] the caprinid rudists Caprina mediopacifica, Caprina mulleri[41] - including a detailedly described holotype of the latter[42] - and Cardita sp.,[43] Lophosmilia fundimaritima,[44] Montastrea menardii,[45] Nerinea sp.[46] and Tiarasmilia casteri occur on Cape Johnson Guyot.[47] Caprina mulleri was also found on other Mid-Pacific Mountains.[48] About 300 species of extant foraminifera have been found on the seamount as well,[49] with additional fossil foraminifera[50] including Paleocene-Eocene specimens that were redeposited by ocean currents.[51] Finally, a cetacean bone of undetermined age has also been found on Cape Johnson Guyot.[52]

References

Sources

Notes and References

  1. Marineregions 2019
  2. BUDDINGTON, p.21
  3. Hamilton 1956, p.18
  4. Hamilton 1953, p.213
  5. Marineregions 2019
  6. Hamilton and Rex 1959, p.787
  7. Hamilton 1953, p.213
  8. Hamilton 1956, p.19
  9. Hamilton 1953, p.213
  10. Hamilton 1956, p.20
  11. Hey and Grigg 1992, p.175
  12. Hamilton 1956, p.20
  13. Winterer, Sager and Firth 1995, p.436
  14. Hamilton 1956, p.18
  15. Hamilton 1956, p.20
  16. Shields 1976, p.47
  17. Morgan 1972, p.12
  18. Winterer, Sager and Firth 1995, p.436
  19. El Wardani 1958, p.240
  20. Heezen and MacGregor 1973, p.667
  21. Hamilton 1956, p.20
  22. Hamilton 1953, p.213
  23. Hill 2005, p.682
  24. Fischer and Garrison 1967, p.489
  25. Hamilton and Rex 1959, p.787
  26. Hamilton 1953, p.213
  27. Hamilton 1953, p.219
  28. Heezen and MacGregor 1973, p.655
  29. Hamilton 1959, p.1409
  30. Hey and Grigg 1992, p.175
  31. Löser 2010, p.158
  32. Hamilton 1956, p.26
  33. Hamilton 1956, p.22
  34. Hamilton 1956, p.20
  35. Hamilton 1956, p.22
  36. UNIVERSITY OF CALIFORNIA SCRIPPS INSTITUTION OF OCEANOGRAPHY. p.5
  37. Cairns 1991, p.31
  38. Hamilton 1956, p.61
  39. Cairns 1991, p.31
  40. Cairns 1991, p.42
  41. Sano et al. 2012, p.849
  42. Masse, Sano and Skelton 2013, p.517
  43. Cairns 1991, p.66
  44. Cairns 1991, p.34
  45. Hamilton 1956, p.59
  46. Cairns 1991, p.64
  47. Löser 2010, p.161
  48. Masse, Sano and Skelton 2013, p.515
  49. Hamilton 1953, p.207
  50. Hamilton 1953, p.213
  51. Hamilton 1953, p.219
  52. Hamilton 1956, p.29

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