Nicolo, Micah J. and Dickens, Gerald Roy (2007): Data report; terrigenous grain-size distributions at Sites 1263 and 1267; testing the applicability of Leg 208 sediments for eolian analysis

Leg/Site/Hole:
ODP 208
DSDP 22
DSDP 22 215
ODP 208 1263
ODP 208 1267
Identifier:
2007-087737
georefid

10.2973/odp.proc.sr.208.205.2006
doi

Creator:
Nicolo, Micah J.
Rice University, Department of Earth Science, Houston, TX, United States
author

Dickens, Gerald Roy
University of California, Santa Cruz, United States
author

Identification:
Data report; terrigenous grain-size distributions at Sites 1263 and 1267; testing the applicability of Leg 208 sediments for eolian analysis
2007
In: Kroon, Dick, Zachos, James C., Blum, Peter, Bowles, Julie, Gaillot, Philippe, Hasegawa, Takashi, Hathorne, Edmund C., Hodell, David A., Kelly, Daniel C., Jung, Ja-Hun, Keller, Susan M., Lee, Youn Soo, Leuschner, Dirk C., Liu Zhifei, Lohmann, Kyger C., Lourens, Lucas, Monechi, Simonetta, Nicolo, Micah, Raffi, Isabella, Riesselman, Christina, Roehl, Ursula, Schellenberg, Stephen A., Schmidt, Daniela, Sluijs, Appy, Thomas, Deborah, Thomas, Ellen, Vallius, Henry, Proceedings of the Ocean Drilling Program; scientific results; early Cenozoic extreme climates; the Walvis Ridge Transect; covering Leg 208 of the cruises of the drilling vessel JOIDES Resolution; Rio de Janeiro, Brazil, to Rio de Janeiro, Brazil; Sites 1262-1267; 6 March-6 May 2003
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
208
To date, the only Southern Hemisphere eolian grain-size record constructed for the early Paleogene comes from Deep Sea Drilling Project Site 215. Ten early Paleogene sediment samples from Site 215 were collected and processed to show that the existing eolian grain-size record at this site can be reproduced. Five samples each from Ocean Drilling Program Sites 1263 and 1267 were similarly examined to test the possibility of generating new Southern Hemisphere eolian grain-size records for the early Paleogene. Our results indicate that an eolian grain-size signal can be constructed at Walvis Ridge, although the record will be complicated by hemipelagic terrigenous inputs. Further, we assert that a record generated at a site located on the deep flanks of Walvis Ridge is particularly susceptible to hemipelagic influence.
English
Coverage:Geographic coordinates:
North:-8.0718
West:1.4200East: 86.4730
South:-28.3200

Stratigraphy; Atlantic Ocean; boreholes; Cenozoic; cores; Deep Sea Drilling Project; DSDP Site 215; grain size; Indian Ocean; Leg 208; Leg 22; lithostratigraphy; lower Paleogene; marine sediments; methods; Ocean Drilling Program; ODP Site 1263; ODP Site 1267; Paleogene; sample preparation; sediments; size distribution; South Atlantic; Southeast Atlantic; terrigenous materials; Tertiary; Walvis Ridge; wind transport;

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