Jurassic and Cretaceous biostratigraphy and organic matter geochemistry of the New Siberian Islands (Russian Arctic)

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Jurassic and Cretaceous biostratigraphy and organic matter geochemistry of the New Siberian Islands (Russian Arctic). / Nikitenko, B. L.; Devyatov, V. P.; Lebedeva, N. K. et al.

In: Russian Geology and Geophysics, Vol. 59, No. 2, 01.02.2018, p. 168-185.

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

BibTeX

@article{3598ce4fa1884d1186d8f529ed58723c,

title = "Jurassic and Cretaceous biostratigraphy and organic matter geochemistry of the New Siberian Islands (Russian Arctic)",

abstract = "The Jurassic-Cretaceous terrigenous complex of the Laptev and East Siberian Seas is of considerable interest as a potential exploration target. However, the key Jurassic and Cretaceous sections of the New Siberian Islands have been poorly studied. The results of this study were used to provide a detailed micropaleontological description of these sections and substantiation of the previous lithostratigraphic subdivision. We first identified a series of Boreal standard zones in the Jurassic and Cretaceous sections, based on the foraminifers, ostracods, dinocysts, and terrestrial palynomorphs. Our results, along with the published data on ammonites, bivalves, and terrestrial palynomorphs and the results of radiometric dating, provide more precise constraints on the stratigraphic position of the identified lithostratigraphic units. The results of this study can be corroborated by seismic data to explore offshore areas of the Laptev and East Siberian Seas. We also present detailed data on the geochemistry of organic matter from the Pestsovaya Formation (Hettangian-lowermost Upper Pliensbachian).",

keywords = "Arctic, biomarker molecules, Cretaceous, dinocysts, foraminifers, Jurassic, New Siberian Islands, organic geochemistry, ostracods, spores and pollen, stratigraphy, SEDIMENTS, STRATIGRAPHY, STOLBOVOI-ISLAND",

author = "Nikitenko, {B. L.} and Devyatov, {V. P.} and Lebedeva, {N. K.} and Basov, {V. A.} and Fursenko, {E. A.} and Goryacheva, {A. A.} and Peshchevitskaya, {E. B.} and Glinskikh, {L. A.} and Khafaeva, {S. N.}",

year = "2018",

month = feb,

day = "1",

doi = "10.1016/j.rgg.2018.01.014",

language = "English",

volume = "59",

pages = "168--185",

journal = "Russian Geology and Geophysics",

issn = "1068-7971",

publisher = "Elsevier Science B.V.",

number = "2",

}

RIS

TY - JOUR

T1 - Jurassic and Cretaceous biostratigraphy and organic matter geochemistry of the New Siberian Islands (Russian Arctic)

AU - Nikitenko, B. L.

AU - Devyatov, V. P.

AU - Lebedeva, N. K.

AU - Basov, V. A.

AU - Fursenko, E. A.

AU - Goryacheva, A. A.

AU - Peshchevitskaya, E. B.

AU - Glinskikh, L. A.

AU - Khafaeva, S. N.

PY - 2018/2/1

Y1 - 2018/2/1

N2 - The Jurassic-Cretaceous terrigenous complex of the Laptev and East Siberian Seas is of considerable interest as a potential exploration target. However, the key Jurassic and Cretaceous sections of the New Siberian Islands have been poorly studied. The results of this study were used to provide a detailed micropaleontological description of these sections and substantiation of the previous lithostratigraphic subdivision. We first identified a series of Boreal standard zones in the Jurassic and Cretaceous sections, based on the foraminifers, ostracods, dinocysts, and terrestrial palynomorphs. Our results, along with the published data on ammonites, bivalves, and terrestrial palynomorphs and the results of radiometric dating, provide more precise constraints on the stratigraphic position of the identified lithostratigraphic units. The results of this study can be corroborated by seismic data to explore offshore areas of the Laptev and East Siberian Seas. We also present detailed data on the geochemistry of organic matter from the Pestsovaya Formation (Hettangian-lowermost Upper Pliensbachian).

AB - The Jurassic-Cretaceous terrigenous complex of the Laptev and East Siberian Seas is of considerable interest as a potential exploration target. However, the key Jurassic and Cretaceous sections of the New Siberian Islands have been poorly studied. The results of this study were used to provide a detailed micropaleontological description of these sections and substantiation of the previous lithostratigraphic subdivision. We first identified a series of Boreal standard zones in the Jurassic and Cretaceous sections, based on the foraminifers, ostracods, dinocysts, and terrestrial palynomorphs. Our results, along with the published data on ammonites, bivalves, and terrestrial palynomorphs and the results of radiometric dating, provide more precise constraints on the stratigraphic position of the identified lithostratigraphic units. The results of this study can be corroborated by seismic data to explore offshore areas of the Laptev and East Siberian Seas. We also present detailed data on the geochemistry of organic matter from the Pestsovaya Formation (Hettangian-lowermost Upper Pliensbachian).

KW - Arctic

KW - biomarker molecules

KW - Cretaceous

KW - dinocysts

KW - foraminifers

KW - Jurassic

KW - New Siberian Islands

KW - organic geochemistry

KW - ostracods

KW - spores and pollen

KW - stratigraphy

KW - SEDIMENTS

KW - STRATIGRAPHY

KW - STOLBOVOI-ISLAND

UR - http://www.scopus.com/inward/record.url?scp=85044849677&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.01.014

DO - 10.1016/j.rgg.2018.01.014

M3 - Article

AN - SCOPUS:85044849677

VL - 59

SP - 168

EP - 185

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 2

ER -

ID: 12416938