Integrated stratigraphy of the Eocene Wilkes Land Margin, Antarctica; preliminary results from IODP Expedition 318: dinoflagellate cyst and TEX86 results.

P.K. Bijl; J.A. Bendle; J. Pross; S. Schouten; U. Röhl; C.E. Stickley; M. Olney; L. Tauxe; S.M. Bohaty; H. Brinkhuis; C. Escutia

Integrated stratigraphy of the Eocene Wilkes Land Margin, Antarctica; preliminary results from IODP Expedition 318: dinoflagellate cyst and TEX86 results.

P.K. Bijl, J.A. Bendle, J. Pross, S. Schouten, U. Röhl, C.E. Stickley, M. Olney, L. Tauxe, S.M. Bohaty, H. Brinkhuis, C. Escutia

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Research output: Contribution to conference › Abstract › Other research output

Abstract

IODP Leg 318 recovered sediment cores from the Antarctic Wilkes Land Margin dating back into the early Eocene, the warmest time interval of the Cenozoic era. These cores provide a first insight into environmental dynamics of an ice-free Antarctica. The onboard and postcruise studies have resulted in a well-constrained age model, and the multidisciplinary biogeochemical and micropaleontological data allows detailed paleoecological interpretations. Here we present the results of a high-resolution dinocyst study on the Eocene recovered at IODP Site U1356. We evaluate relative sea level and productivity fluctuations and put the record of dinocyst endemism in the context of the regional tectonic evolution of the Australo-Antarctic continental breakup

Original language	English
Publication status	Published - 5 Jun 2011
Event	CBEP 2011 - Duration: 5 Jun 2011 → 8 Jun 2011

Conference

Conference	CBEP 2011
Period	5/06/11 → 8/06/11

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@conference{f215c843c9904d67a91ad0c069dd3853,

title = "Integrated stratigraphy of the Eocene Wilkes Land Margin, Antarctica; preliminary results from IODP Expedition 318: dinoflagellate cyst and TEX86 results.",

abstract = "IODP Leg 318 recovered sediment cores from the Antarctic Wilkes Land Margin dating back into the early Eocene, the warmest time interval of the Cenozoic era. These cores provide a first insight into environmental dynamics of an ice-free Antarctica. The onboard and postcruise studies have resulted in a well-constrained age model, and the multidisciplinary biogeochemical and micropaleontological data allows detailed paleoecological interpretations. Here we present the results of a high-resolution dinocyst study on the Eocene recovered at IODP Site U1356. We evaluate relative sea level and productivity fluctuations and put the record of dinocyst endemism in the context of the regional tectonic evolution of the Australo-Antarctic continental breakup",

author = "P.K. Bijl and J.A. Bendle and J. Pross and S. Schouten and U. R{\"o}hl and C.E. Stickley and M. Olney and L. Tauxe and S.M. Bohaty and H. Brinkhuis and C. Escutia",

note = "CBEP 2011; CBEP 2011 ; Conference date: 05-06-2011 Through 08-06-2011",

year = "2011",

month = jun,

day = "5",

language = "English",

}

TY - CONF

T1 - Integrated stratigraphy of the Eocene Wilkes Land Margin, Antarctica; preliminary results from IODP Expedition 318: dinoflagellate cyst and TEX86 results.

AU - Bijl, P.K.

AU - Bendle, J.A.

AU - Pross, J.

AU - Schouten, S.

AU - Röhl, U.

AU - Stickley, C.E.

AU - Olney, M.

AU - Tauxe, L.

AU - Bohaty, S.M.

AU - Brinkhuis, H.

AU - Escutia, C.

N1 - CBEP 2011

PY - 2011/6/5

Y1 - 2011/6/5

N2 - IODP Leg 318 recovered sediment cores from the Antarctic Wilkes Land Margin dating back into the early Eocene, the warmest time interval of the Cenozoic era. These cores provide a first insight into environmental dynamics of an ice-free Antarctica. The onboard and postcruise studies have resulted in a well-constrained age model, and the multidisciplinary biogeochemical and micropaleontological data allows detailed paleoecological interpretations. Here we present the results of a high-resolution dinocyst study on the Eocene recovered at IODP Site U1356. We evaluate relative sea level and productivity fluctuations and put the record of dinocyst endemism in the context of the regional tectonic evolution of the Australo-Antarctic continental breakup

AB - IODP Leg 318 recovered sediment cores from the Antarctic Wilkes Land Margin dating back into the early Eocene, the warmest time interval of the Cenozoic era. These cores provide a first insight into environmental dynamics of an ice-free Antarctica. The onboard and postcruise studies have resulted in a well-constrained age model, and the multidisciplinary biogeochemical and micropaleontological data allows detailed paleoecological interpretations. Here we present the results of a high-resolution dinocyst study on the Eocene recovered at IODP Site U1356. We evaluate relative sea level and productivity fluctuations and put the record of dinocyst endemism in the context of the regional tectonic evolution of the Australo-Antarctic continental breakup

M3 - Abstract

T2 - CBEP 2011

Y2 - 5 June 2011 through 8 June 2011

ER -

Integrated stratigraphy of the Eocene Wilkes Land Margin, Antarctica; preliminary results from IODP Expedition 318: dinoflagellate cyst and TEX86 results.

Abstract

Conference

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