Standard

Stratigraphy of Late Cenozoic sediments of the western Chukchi Sea: New results from shallow drilling and seismic-reflection profiling. / Gusev, E.A.; Andreeva, I.A.; Anikina, N.Y.; Bondarenko, S.A.; Derevyanko, L.G.; Iosifidi, A.G.; Klyuvitkina, T.S.; Litvinenko, I.V.; Petrova, V.I.; Polyakova, E.I.; Popov, V.V.; Stepanova, A.Y.

In: Global and Planetary Change, Vol. 68, No. 1-2, 2009, p. 115-131.

Research output: Contribution to journal › Article › peer-review

Harvard

Gusev, EA, Andreeva, IA, Anikina, NY, Bondarenko, SA, Derevyanko, LG, Iosifidi, AG, Klyuvitkina, TS, Litvinenko, IV, Petrova, VI, Polyakova, EI, Popov, VV & Stepanova, AY 2009, 'Stratigraphy of Late Cenozoic sediments of the western Chukchi Sea: New results from shallow drilling and seismic-reflection profiling', Global and Planetary Change, vol. 68, no. 1-2, pp. 115-131. https://doi.org/10.1016/j.gloplacha.2009.03.025

APA

Gusev, E. A., Andreeva, I. A., Anikina, N. Y., Bondarenko, S. A., Derevyanko, L. G., Iosifidi, A. G., Klyuvitkina, T. S., Litvinenko, I. V., Petrova, V. I., Polyakova, E. I., Popov, V. V., & Stepanova, A. Y. (2009). Stratigraphy of Late Cenozoic sediments of the western Chukchi Sea: New results from shallow drilling and seismic-reflection profiling. Global and Planetary Change, 68(1-2), 115-131. https://doi.org/10.1016/j.gloplacha.2009.03.025

Vancouver

Gusev EA, Andreeva IA, Anikina NY, Bondarenko SA, Derevyanko LG, Iosifidi AG et al. Stratigraphy of Late Cenozoic sediments of the western Chukchi Sea: New results from shallow drilling and seismic-reflection profiling. Global and Planetary Change. 2009;68(1-2):115-131. https://doi.org/10.1016/j.gloplacha.2009.03.025

Author

Gusev, E.A. ; Andreeva, I.A. ; Anikina, N.Y. ; Bondarenko, S.A. ; Derevyanko, L.G. ; Iosifidi, A.G. ; Klyuvitkina, T.S. ; Litvinenko, I.V. ; Petrova, V.I. ; Polyakova, E.I. ; Popov, V.V. ; Stepanova, A.Y. / Stratigraphy of Late Cenozoic sediments of the western Chukchi Sea: New results from shallow drilling and seismic-reflection profiling. In: Global and Planetary Change. 2009 ; Vol. 68, No. 1-2. pp. 115-131.

BibTeX

@article{b2551c0fecc341ffa916e21c38a2325e,
title = "Stratigraphy of Late Cenozoic sediments of the western Chukchi Sea: New results from shallow drilling and seismic-reflection profiling",
abstract = "The Quaternary history of Beringia and of the Arctic–Pacific marine connection via the Bering Strait is poorly understood because of the fragmentary stratigraphic record from this region. We report new borehole and seismic-reflection data collected in 2006 in the southwestern Chukchi Sea. Sediment samples were analyzed for magnetic properties, grain size, heavy minerals, and biostratigraphic proxies (spores and pollen, foraminifers, ostracodes, diatoms, and aquatic palynomorphs). Two shallow boreholes drilled between the Chukotka Peninsula and the Wrangel Island recovered sediments of two principal stratigraphic units with a distinct unconformity between them. Based on predominantly reverse paleomagnetic polarity of the lower unit and pollen spectra indicative of forested coasts and climate warmer than present, the age of this unit is estimated as Pliocene to early Pleistocene (broadly between ca. 5 and 2 Ma). Attendant sedimentary environments were likely alluvial to nearshore marine. These deposits can be c",
keywords = "Chukchi Sea, Beringia, sediment stratigraphy, seismic stratigraphy, Pliocene, Quaternary",
author = "E.A. Gusev and I.A. Andreeva and N.Y. Anikina and S.A. Bondarenko and L.G. Derevyanko and A.G. Iosifidi and T.S. Klyuvitkina and I.V. Litvinenko and V.I. Petrova and E.I. Polyakova and V.V. Popov and A.Y. Stepanova",
year = "2009",
doi = "10.1016/j.gloplacha.2009.03.025",
language = "English",
volume = "68",
pages = "115--131",
journal = "Global and Planetary Change",
issn = "0921-8181",
publisher = "Elsevier",
number = "1-2",

}

RIS

TY - JOUR

T1 - Stratigraphy of Late Cenozoic sediments of the western Chukchi Sea: New results from shallow drilling and seismic-reflection profiling

AU - Gusev, E.A.

AU - Andreeva, I.A.

AU - Anikina, N.Y.

AU - Bondarenko, S.A.

AU - Derevyanko, L.G.

AU - Iosifidi, A.G.

AU - Klyuvitkina, T.S.

AU - Litvinenko, I.V.

AU - Petrova, V.I.

AU - Polyakova, E.I.

AU - Popov, V.V.

AU - Stepanova, A.Y.

PY - 2009

Y1 - 2009

N2 - The Quaternary history of Beringia and of the Arctic–Pacific marine connection via the Bering Strait is poorly understood because of the fragmentary stratigraphic record from this region. We report new borehole and seismic-reflection data collected in 2006 in the southwestern Chukchi Sea. Sediment samples were analyzed for magnetic properties, grain size, heavy minerals, and biostratigraphic proxies (spores and pollen, foraminifers, ostracodes, diatoms, and aquatic palynomorphs). Two shallow boreholes drilled between the Chukotka Peninsula and the Wrangel Island recovered sediments of two principal stratigraphic units with a distinct unconformity between them. Based on predominantly reverse paleomagnetic polarity of the lower unit and pollen spectra indicative of forested coasts and climate warmer than present, the age of this unit is estimated as Pliocene to early Pleistocene (broadly between ca. 5 and 2 Ma). Attendant sedimentary environments were likely alluvial to nearshore marine. These deposits can be c

AB - The Quaternary history of Beringia and of the Arctic–Pacific marine connection via the Bering Strait is poorly understood because of the fragmentary stratigraphic record from this region. We report new borehole and seismic-reflection data collected in 2006 in the southwestern Chukchi Sea. Sediment samples were analyzed for magnetic properties, grain size, heavy minerals, and biostratigraphic proxies (spores and pollen, foraminifers, ostracodes, diatoms, and aquatic palynomorphs). Two shallow boreholes drilled between the Chukotka Peninsula and the Wrangel Island recovered sediments of two principal stratigraphic units with a distinct unconformity between them. Based on predominantly reverse paleomagnetic polarity of the lower unit and pollen spectra indicative of forested coasts and climate warmer than present, the age of this unit is estimated as Pliocene to early Pleistocene (broadly between ca. 5 and 2 Ma). Attendant sedimentary environments were likely alluvial to nearshore marine. These deposits can be c

KW - Chukchi Sea

KW - Beringia

KW - sediment stratigraphy

KW - seismic stratigraphy

KW - Pliocene

KW - Quaternary

U2 - 10.1016/j.gloplacha.2009.03.025

DO - 10.1016/j.gloplacha.2009.03.025

M3 - Article

VL - 68

SP - 115

EP - 131

JO - Global and Planetary Change

JF - Global and Planetary Change

SN - 0921-8181

IS - 1-2

ER -

ID: 5313914