Ubiquitous 13C-depleted secondary calcite within the Zaonega Formation, Russia: insights into the Paleoproterozoic global carbon cycle

A.E. Črne; V.A. Melezhik; A. Lepland; A.E. Fallick; A.R. Prave; A.T. Brasier

doi:10.1016/j.precamres.2013.10.005

Ubiquitous 13C-depleted secondary calcite within the Zaonega Formation, Russia: insights into the Paleoproterozoic global carbon cycle

A.E. Črne, V.A. Melezhik, A. Lepland, A.E. Fallick, A.R. Prave, A.T. Brasier

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

The ca. 2.0 Ga Zaonega Formation in the Onega Basin of NW Russia represents a deep-water, mixed siliciclastic-carbonate depositional system with voluminous mafic volcanism. It is typified by extremely organic-rich rocks (TOC>40 wt%) and represents one of the earliest known episodes of oil/asphalt generation. These rocks have been inferred to archive one of the largest negative δ

Original language	English
Journal	Precambrian Research
Volume	2013
Issue number	01
DOIs	https://doi.org/10.1016/j.precamres.2013.10.005
Publication status	Accepted/In press - 2013

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10.1016/j.precamres.2013.10.005

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title = "Ubiquitous 13C-depleted secondary calcite within the Zaonega Formation, Russia: insights into the Paleoproterozoic global carbon cycle",

abstract = "The ca. 2.0 Ga Zaonega Formation in the Onega Basin of NW Russia represents a deep-water, mixed siliciclastic-carbonate depositional system with voluminous mafic volcanism. It is typified by extremely organic-rich rocks (TOC>40 wt%) and represents one of the earliest known episodes of oil/asphalt generation. These rocks have been inferred to archive one of the largest negative δ",

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AU - Črne, A.E.

AU - Melezhik, V.A.

AU - Lepland, A.

AU - Fallick, A.E.

AU - Prave, A.R.

AU - Brasier, A.T.

PY - 2013

Y1 - 2013

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AB - The ca. 2.0 Ga Zaonega Formation in the Onega Basin of NW Russia represents a deep-water, mixed siliciclastic-carbonate depositional system with voluminous mafic volcanism. It is typified by extremely organic-rich rocks (TOC>40 wt%) and represents one of the earliest known episodes of oil/asphalt generation. These rocks have been inferred to archive one of the largest negative δ

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DO - 10.1016/j.precamres.2013.10.005

M3 - Article

SN - 0301-9268

VL - 2013

JO - Precambrian Research

JF - Precambrian Research

IS - 01

ER -

Ubiquitous 13C-depleted secondary calcite within the Zaonega Formation, Russia: insights into the Paleoproterozoic global carbon cycle

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