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Foraminifera from the carbonate cobbles and pebbles of Early Jurassic conglomerates of Franz Joseph Land as direct evidence of the existence of a Late Palaeozoic carbonate succession in the northeastern Barents Sea. / Ershova, V.B.; Leven, E.; Prokopiev, A.V.

In: Norsk Geologisk Tiddsskrift, Vol. 97, No. 4, 2017, p. 161-167.

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

Harvard

Ershova, VB, Leven, E & Prokopiev, AV 2017, 'Foraminifera from the carbonate cobbles and pebbles of Early Jurassic conglomerates of Franz Joseph Land as direct evidence of the existence of a Late Palaeozoic carbonate succession in the northeastern Barents Sea', Norsk Geologisk Tiddsskrift, vol. 97, no. 4, pp. 161-167.

APA

Ershova, V. B., Leven, E., & Prokopiev, A. V. (2017). Foraminifera from the carbonate cobbles and pebbles of Early Jurassic conglomerates of Franz Joseph Land as direct evidence of the existence of a Late Palaeozoic carbonate succession in the northeastern Barents Sea. Norsk Geologisk Tiddsskrift, 97(4), 161-167.

Vancouver

Ershova VB, Leven E, Prokopiev AV. Foraminifera from the carbonate cobbles and pebbles of Early Jurassic conglomerates of Franz Joseph Land as direct evidence of the existence of a Late Palaeozoic carbonate succession in the northeastern Barents Sea. Norsk Geologisk Tiddsskrift. 2017;97(4):161-167.

Author

Ershova, V.B. ; Leven, E. ; Prokopiev, A.V. / Foraminifera from the carbonate cobbles and pebbles of Early Jurassic conglomerates of Franz Joseph Land as direct evidence of the existence of a Late Palaeozoic carbonate succession in the northeastern Barents Sea. In: Norsk Geologisk Tiddsskrift. 2017 ; Vol. 97, No. 4. pp. 161-167.

BibTeX

@article{7c7bcb80f8074c8fb82462231c316b38,
title = "Foraminifera from the carbonate cobbles and pebbles of Early Jurassic conglomerates of Franz Joseph Land as direct evidence of the existence of a Late Palaeozoic carbonate succession in the northeastern Barents Sea",
abstract = "Here we present the first description and images of foraminiferal fauna from the carbonate cobbles and pebbles of Early Jurassic polymicticconglomerates from Graham Bell Island, in the easternmost part of the Franz Joseph Land archipelago. The composition of the conglomeratessuggests a proximal provenance area. The identified foraminiferal genera and species suggest a Serpukhovian–Late Carboniferous age for theprimary carbonates from which the conglomerate clasts were derived, and which can be correlated with coeval carbonate strata of Svalbard, theVolga–Urals and the Pechora region. Combined with previous studies, our new data lead us to assert that a shallow-marine carbonate platformoccupied the entire Barents shelf, including its northeasternmost part, during Carboniferous–Early(?) Permian time. This study improves ourunderstanding of the composition and age of pre-Mesozoic successions of Franz Joseph Land and surrounding parts of the Barents Sea.",
author = "V.B. Ershova and E. Leven and A.V. Prokopiev",
year = "2017",
language = "English",
volume = "97",
pages = "161--167",
journal = "NORWEGIAN JOURNAL OF GEOLOGY",
issn = "0801-4736",
publisher = "Geological Society of Norway",
number = "4",

}

RIS

TY - JOUR

T1 - Foraminifera from the carbonate cobbles and pebbles of Early Jurassic conglomerates of Franz Joseph Land as direct evidence of the existence of a Late Palaeozoic carbonate succession in the northeastern Barents Sea

AU - Ershova, V.B.

AU - Leven, E.

AU - Prokopiev, A.V.

PY - 2017

Y1 - 2017

N2 - Here we present the first description and images of foraminiferal fauna from the carbonate cobbles and pebbles of Early Jurassic polymicticconglomerates from Graham Bell Island, in the easternmost part of the Franz Joseph Land archipelago. The composition of the conglomeratessuggests a proximal provenance area. The identified foraminiferal genera and species suggest a Serpukhovian–Late Carboniferous age for theprimary carbonates from which the conglomerate clasts were derived, and which can be correlated with coeval carbonate strata of Svalbard, theVolga–Urals and the Pechora region. Combined with previous studies, our new data lead us to assert that a shallow-marine carbonate platformoccupied the entire Barents shelf, including its northeasternmost part, during Carboniferous–Early(?) Permian time. This study improves ourunderstanding of the composition and age of pre-Mesozoic successions of Franz Joseph Land and surrounding parts of the Barents Sea.

AB - Here we present the first description and images of foraminiferal fauna from the carbonate cobbles and pebbles of Early Jurassic polymicticconglomerates from Graham Bell Island, in the easternmost part of the Franz Joseph Land archipelago. The composition of the conglomeratessuggests a proximal provenance area. The identified foraminiferal genera and species suggest a Serpukhovian–Late Carboniferous age for theprimary carbonates from which the conglomerate clasts were derived, and which can be correlated with coeval carbonate strata of Svalbard, theVolga–Urals and the Pechora region. Combined with previous studies, our new data lead us to assert that a shallow-marine carbonate platformoccupied the entire Barents shelf, including its northeasternmost part, during Carboniferous–Early(?) Permian time. This study improves ourunderstanding of the composition and age of pre-Mesozoic successions of Franz Joseph Land and surrounding parts of the Barents Sea.

M3 - Article

VL - 97

SP - 161

EP - 167

JO - NORWEGIAN JOURNAL OF GEOLOGY

JF - NORWEGIAN JOURNAL OF GEOLOGY

SN - 0801-4736

IS - 4

ER -

ID: 36003426