High-resolution stratigraphy and palaeoenvironmentsof the Volgian-Valanginian in the Olenek key section (Anabar-Lena region, Arctic East Siberia, Russia)

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High-resolution stratigraphy and palaeoenvironmentsof the Volgian-Valanginian in the Olenek key section (Anabar-Lena region, Arctic East Siberia, Russia). / Nikitenko, B. L.; Pestchevitskaya, E. B.; Khafaeva, S. N.

в: Revue de Micropaleontologie, Том 61, № 3-4, 01.12.2018, стр. 271-312.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

BibTeX

@article{9f4b31f0347a4125bafad904deac8087,

title = "High-resolution stratigraphy and palaeoenvironmentsof the Volgian-Valanginian in the Olenek key section (Anabar-Lena region, Arctic East Siberia, Russia)",

abstract = "The Volgian-Valanginian shallow-water deposits from the Olenek key section (Anabar-Lena region, Arctic Siberia) were studied by sedimentological, palaeontological and geochemical methods. High-resolution biostratigraphy of the studied interval is based on ammonites, foraminifera, and marine and terrestrial palynomorphs. An almost complete succession of ammonite zones provides biostratigraphic control for the upper part of the Buolkalakh Formation and the boundary between the Volgian and Boreal Berriasian stages. Foraminiferal and palynological zones have important regional implications providing well-constrained biostratigraphy of the Anabar-Lena region. Several levels important for interregional correlations are defined in the Volgian and Berriasian on the basis of taxonomic changes in microfossil assemblages as well as lowest and highest occurrences of indicative taxa. Combined sedimentological, geochemical studies and ecological analysis of microfossil associations (foraminifera, marine and terrestrial palynomoprhs) allowed the palaeoenvironmental reconstructions for the marginal area of the Anabar-Lena palaeosea and coastal land areas.",

keywords = "Arctic Siberia, Foraminifera, Lower Cretaceous, Palaeoenvironments, Palynomorphs, Stratigraphy, Upper Jurassic",

author = "Nikitenko, {B. L.} and Pestchevitskaya, {E. B.} and Khafaeva, {S. N.}",

note = "Publisher Copyright: {\textcopyright} 2018 Elsevier Masson SAS",

year = "2018",

month = dec,

day = "1",

doi = "10.1016/j.revmic.2018.07.001",

language = "English",

volume = "61",

pages = "271--312",

journal = "Revue de Micropaleontologie",

issn = "0035-1598",

publisher = "Elsevier Masson",

number = "3-4",

}

RIS

TY - JOUR

T1 - High-resolution stratigraphy and palaeoenvironmentsof the Volgian-Valanginian in the Olenek key section (Anabar-Lena region, Arctic East Siberia, Russia)

AU - Nikitenko, B. L.

AU - Pestchevitskaya, E. B.

AU - Khafaeva, S. N.

PY - 2018/12/1

Y1 - 2018/12/1

N2 - The Volgian-Valanginian shallow-water deposits from the Olenek key section (Anabar-Lena region, Arctic Siberia) were studied by sedimentological, palaeontological and geochemical methods. High-resolution biostratigraphy of the studied interval is based on ammonites, foraminifera, and marine and terrestrial palynomorphs. An almost complete succession of ammonite zones provides biostratigraphic control for the upper part of the Buolkalakh Formation and the boundary between the Volgian and Boreal Berriasian stages. Foraminiferal and palynological zones have important regional implications providing well-constrained biostratigraphy of the Anabar-Lena region. Several levels important for interregional correlations are defined in the Volgian and Berriasian on the basis of taxonomic changes in microfossil assemblages as well as lowest and highest occurrences of indicative taxa. Combined sedimentological, geochemical studies and ecological analysis of microfossil associations (foraminifera, marine and terrestrial palynomoprhs) allowed the palaeoenvironmental reconstructions for the marginal area of the Anabar-Lena palaeosea and coastal land areas.

AB - The Volgian-Valanginian shallow-water deposits from the Olenek key section (Anabar-Lena region, Arctic Siberia) were studied by sedimentological, palaeontological and geochemical methods. High-resolution biostratigraphy of the studied interval is based on ammonites, foraminifera, and marine and terrestrial palynomorphs. An almost complete succession of ammonite zones provides biostratigraphic control for the upper part of the Buolkalakh Formation and the boundary between the Volgian and Boreal Berriasian stages. Foraminiferal and palynological zones have important regional implications providing well-constrained biostratigraphy of the Anabar-Lena region. Several levels important for interregional correlations are defined in the Volgian and Berriasian on the basis of taxonomic changes in microfossil assemblages as well as lowest and highest occurrences of indicative taxa. Combined sedimentological, geochemical studies and ecological analysis of microfossil associations (foraminifera, marine and terrestrial palynomoprhs) allowed the palaeoenvironmental reconstructions for the marginal area of the Anabar-Lena palaeosea and coastal land areas.

KW - Arctic Siberia

KW - Foraminifera

KW - Lower Cretaceous

KW - Palaeoenvironments

KW - Palynomorphs

KW - Stratigraphy

KW - Upper Jurassic

UR - http://www.scopus.com/inward/record.url?scp=85053671757&partnerID=8YFLogxK

U2 - 10.1016/j.revmic.2018.07.001

DO - 10.1016/j.revmic.2018.07.001

M3 - Article

AN - SCOPUS:85053671757

VL - 61

SP - 271

EP - 312

JO - Revue de Micropaleontologie

JF - Revue de Micropaleontologie

SN - 0035-1598

IS - 3-4

ER -

ID: 16683021