Lund, Steven P. et al. (2006): Late Quaternary paleomagnetic secular variation and chronostratigraphy from ODP Sites 1233 and 1234

Leg/Site/Hole:
ODP 202
ODP 202 1233
ODP 202 1234
Identifier:
2007-051085
georefid

10.2973/odp.proc.sr.202.208.2006
doi

Creator:
Lund, Steven P.
University of Southern California, Department of Earth Sciences, Los Angeles, CA, United States
author

Stoner, Joseph S.
Oregon State University, United States
author

Lamy, Frank
Texas A&M University, United States
author

Identification:
Late Quaternary paleomagnetic secular variation and chronostratigraphy from ODP Sites 1233 and 1234
2006
In: Tiedemann, Ralf, Mix, Alan C., Blum, Peter, Abrantes, Fatima F., Benway, Heather, Cacho-Lascorz, Isabel, Chen, Min-Te, Delaney, Margaret L., Flores, Jose-Abel, Giosan, Liviu, Holbourn, Ann E., Irino, Tomohisa, Iwai, Masao, Joseph, Leah H., Kleiven, Helga F., Lamy, Frank, Lund, Steven P., Martinez, Philippe, McManus, Jerry F., Ninnemann, Ulysses S., Pisias, Nicklas G., Robinson, Rebecca S., Stoner, Joseph S., Sturm, Arne, Wara, Michael W., Wei, Wuchang, Proceedings of the Ocean Drilling Program; scientific results; Southeast Pacific paleoceanographic transects; covering Leg 202 of the cruises of the drilling vessel JOIDES Resolution; Valparaiso, Chile, to Balboa, Panama; Sites 1232-1242; 29 March-30 May 2002
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
202
During Ocean Drilling Program Leg 202, detailed shipboard paleomagnetic measurements at Sites 1233 and 1234 identified a reproducible high-resolution record of paleomagnetic secular variation (PSV) at each site. These records also contained evidence for three magnetic field excursions. This paper summarizes the complete paleomagnetic record from Site 1233 and the paleomagnetic record for the uppermost 30 meters from Site 1234. We also establish a detailed PSV correlation between the two sites, located approximately 500 km apart. Twenty-seven accelerator mass spectrometry radiocarbon dates permit us to develop time-depth plots and detailed PSV time series for the last approximately 50,000 yr at both sites. Based on our chronostratigraphy, the most recent excursions occur at approximately 35,000 cal. yr before present (BP) (Excursion 3alpha ) and approximately 41,000 cal. yr BP (Excursion 3beta ). The excursions were named for the oxygen isotope stages within which they occur. These two excursions are not significantly different in age from the Mono Lake Excursion and Laschamp Excursion. A third, older excursion, which has not yet been adequately dated, also occurs at Site 1233.
English
Coverage:Geographic coordinates:
North:-36.1300
West:-74.2700East: -73.4100
South:-41.0000

Quaternary geology; absolute age; alternating field demagnetization; C-14; carbon; Cenozoic; chronostratigraphy; cores; correlation; dates; demagnetization; East Pacific; isotopes; Leg 202; magnetic excursions; magnetic field; magnetization; magnetostratigraphy; natural remanent magnetization; Ocean Drilling Program; ODP Site 1233; ODP Site 1234; oxygen; Pacific Ocean; paleomagnetism; Quaternary; radioactive isotopes; remanent magnetization; secular variations; South Pacific; Southeast Pacific; upper Quaternary;

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