Hasegawa, Takashi et al. (2007): Data report; stable carbon isotope fluctuation of long-chain n-alkanes from Leg 208 Hole 1263A across the Paleocene/Eocene boundary

Leg/Site/Hole:
ODP 208
ODP 208 1263
Identifier:
2007-087740
georefid

10.2973/odp.proc.sr.208.202.2006
doi

Creator:
Hasegawa, Takashi
Kanazawa University, Graduate School of Natural Science and Technology, Department of Earth Sciences, Kanazawa, Japan
author

Yamamoto, Shinya
University of California, Santa Cruz, United States
author

Pratt, Lisa M.
Ocean Drilling Program, United States
author

Identification:
Data report; stable carbon isotope fluctuation of long-chain n-alkanes from Leg 208 Hole 1263A across the Paleocene/Eocene boundary
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
Carbon isotope ratios of terrestrial biomarkers extracted from Ocean Drilling Program Hole 1263A show a prominent negative excursion across the Paleocene/Eocene boundary. The isotope profiles of the normal alkanes nonacosane (n-C29), hentriacontane (n-C31), and tritriacontane (n-C33), the first such profiles generated with samples from a pelagic section, are similar to those of carbonate carbon, though the magnitude of the excursion is larger, roughly 4 per mil-5 per mil. In addition, the n-alkane records show an inflection at 334.70 meters composite depth, which is roughly equivalent to where the inflection occurs in the carbonate record. These results suggest that the terrestrial compounds are directly recording changes in atmospheric carbon delta (super 13) C and that the actual excursion may have been larger than that recorded by marine carbonates.
English
Coverage:Geographic coordinates:
North:-28.3200
West:2.4700East: 2.4700
South:-28.3200

Stratigraphy; Isotope geochemistry; aliphatic hydrocarbons; alkanes; Atlantic Ocean; biomarkers; boreholes; C-13/C-12; carbon; carbon dioxide; Cenozoic; chemostratigraphy; cores; Eocene; gas chromatograms; geochemistry; hydrocarbons; isotope ratios; isotopes; Leg 208; marine sediments; n-alkanes; Ocean Drilling Program; ODP Site 1263; organic compounds; paleo-oceanography; Paleocene; paleoclimatology; Paleogene; sediments; South Atlantic; Southeast Atlantic; stable isotopes; stratigraphic boundary; Tertiary; Walvis Ridge;

.