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- Chapter contents
- Abstract
- Introduction
- Material and methods
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Results and discussion
- Summary
- Acknowledgments
- References
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Figures
- F1. Location map.
- F2. Site U1331 paleomagnetic and physical property data.
- F3. Digital line scan images, Site U1331.
- F4. Growth factor, Site U1331.
- F5. Site U1332 paleomagnetic and physical property data.
- F6. Digital line scan images, Site U1332.
- F7. Growth factor, Site U1332.
- F8. Site U1333 paleomagnetic and physical property data.
- F9. Digital line scan images, Site U1333.
- F10. Growth factor, Site U1333.
- F11. Site U1334 paleomagnetic and physical property data.
- F12. Digital line scan images, Site U1334.
- F13. Growth factor, Site U1334.
- F14. Site 1218 paleomagnetic and physical property data.
- F15. Digital line scan images, Site 1218.
- F16. Growth factor, Site 1218.
- F17. Site 1219 paleomagnetic and physical property data.
- F18. Digital line scan images, Site 1219.
- F19. Site 1220 paleomagnetic and physical property data.
- F20. Digital line scan images, Site 1220.
- F21. Growth factor, Site 1220.
- F22. Site-to-site correlation on Site 1218 scale.
- F23. Site-to-site correlation on Site 1220 scale.
- F24. Linear sedimentation rates.
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Tables
- T1. Revised splice tie points, Site U1331.
- T2. Revised composite depths, Site U1331.
- T3. Mapping pairs, Site U1331.
- T4. Turbidites, Site U1331.
- T5. Revised composite depths, Site U1332.
- T6. Revised splice tie points, Site U1332.
- T7. Mapping pairs, Site U1332.
- T8. Revised composite depths, Site U1333.
- T9. Revised splice tie points, Site U1333.
- T10. Mapping pairs, Site U1333.
- T11. Revised composite depths, Site U1334.
- T12. Revised splice tie points, Site U1334.
- T13. Mapping pairs, Site U1334.
- T14. Revised offset, Site 1218.
- T15. Tie points, Site 1218.
- T16. Mapping pairs, Site 1218.
- T17. Tie points, Site 1219.
- T18. Revised offset, Site 1219.
- T19. Revised offset, Site 1220.
- T20. Tie points, Site 1220.
- T21. Mapping pairs, Site 1220.
- T22. Cleaned magnetic susceptibility and GRA, Site U1331.
- T23. Cleaned magnetic susceptibility and GRA, Site U1332.
- T24. Cleaned magnetic susceptibility and GRA, Site U1333.
- T25. Cleaned magnetic susceptibility and GRA, Site U1334.
- T26. Cleaned magnetic susceptibility and GRA, Site 1218.
- T27. Cleaned magnetic susceptibility and GRA, Site 1219.
- T28. Cleaned magnetic susceptibility and GRA, Site 1220.
- T29. Correlation of sites to Site 1218.
- T30. Correlation of sites to Site 1220.
- T31. Revised magnetochrons.
- T32. Site U1331 radiolarian datums.
- T33. Site U1332 radiolarian datums.
- T34. Site U1333 radiolarian datums.
- T35. Site U1334 radiolarian datums.
- T36. Site 1218 radiolarian datums.
- T37. Site 1219 radiolarian datums.
- T38. Site 1220 radiolarian datums.
- T39. Site U1331 calcareous nannofossil datums.
- T40. Site U1332 calcareous nannofossil datums.
- T41. Site U1333 calcareous nannofossil datums.
- T42. Site U1334 calcareous nannofossil datums.
- T43. Site 1218 calcareous nannofossil datums.
- T44. Site 1219 calcareous nannofossil datums.
- T45. Site 1220 calcareous nannofossil datums.
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doi:10.2204/iodp.proc.320321.201.2012
Revised composite depth scales and integration of IODP Sites U1331–U1334 and ODP Sites 1218–12201
Thomas Westerhold,2 Ursula Röhl,2 Roy Wilkens,3 Heiko Pälike,4 Mitch Lyle,5 Tom Dunkley Jones,6 Paul Bown,7 Ted Moore,8 Shin-ichi Kamikuri,9 Gary Acton,10 Christian Ohneiser,11 Yuhji Yamamoto,12 Carl Richter,13 Peter Fitch,6 Howie Scher,14 Diederik Liebrand,4 and the Expedition 320/321 Scientists15
Abstract
To reconstruct the climate history of the equatorial Pacific, one major objective of the Pacific Equatorial Age Transect (PEAT) program is to compile a Cenozoic megasplice that integrates all available bio-, chemo-, and magnetostratigraphic data including key records from Ocean Drilling Program (ODP) Leg 199. In order to do so, extended postcruise refinements of the shipboard composite depth scales and composite records are required. Here, we present a revised depth scale of Integrated Ocean Drilling Program (IODP) Expedition 320 Sites U1331, U1332, U1333, and U1334 as well as Leg 199 Sites 1218, 1219, and 1220. The revised composite records were used to perform site-to-site correlation and integration of Leg 199 and Expedition 320 sites. Based on this decimeter-scale correlation, a high-resolution integrated paleomagnetic, calcareous nannofossil, and radiolarian stratigraphy for the equatorial Pacific is established that covers the time from 20 to 40 Ma. This sedimentary compendium from the equatorial Pacific will be the backbone for paleoceanographic reconstructions for the late Paleogene.
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