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Main Authors: Kouchinsky, Artem, Bengtson, Stefan, Pavlov, Vladimir, Runnegar, Bruce, Val'kov, Anatolij K, Young, Edward
Format: Dataset Open Access
Language:en
Published: PANGAEA 2005
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.688263
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author Kouchinsky, Artem
Bengtson, Stefan
Pavlov, Vladimir
Runnegar, Bruce
Val'kov, Anatolij K
Young, Edward
author_facet Kouchinsky, Artem
Bengtson, Stefan
Pavlov, Vladimir
Runnegar, Bruce
Val'kov, Anatolij K
Young, Edward
collection Datos científicos de ciencias marinas y ambientales
contents Carbon isotopic data from the Selinde section in the southeastern part of the Siberian platform area are correlated with the reference isotopic profile from the Lower Cambrian stratotype sections of the Lena Aldan region, but also show additional d13C excursions unrecognized there. The chemostratigraphic correlation suggests that the geological and fossil record of the lower Pestrotsvet Formation in the Selinde section has a deeper history than the stratotype region. This conclusion is important for both constraining the age of the earliest Cambrian marine transgression on the Siberian platform and providing a clearer understanding of the pace and order of early Cambrian geochemical and biological events.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_688263
institution PANGAEA
language en
publishDate 2005
publisher PANGAEA
record_format pangaea
spellingShingle Carbon and oxygen isotope ratios of Selinde River, southeastern Siberian platform
Kouchinsky, Artem
Bengtson, Stefan
Pavlov, Vladimir
Runnegar, Bruce
Val'kov, Anatolij K
Young, Edward
Isotope ratio mass spectrometry; OUTCROP; Outcrop sample; POINT DISTANCE from start; Sample code/label; Selinde; Siberia, Russia; δ13C, carbonate; δ18O, carbonate
Carbon isotopic data from the Selinde section in the southeastern part of the Siberian platform area are correlated with the reference isotopic profile from the Lower Cambrian stratotype sections of the Lena Aldan region, but also show additional d13C excursions unrecognized there. The chemostratigraphic correlation suggests that the geological and fossil record of the lower Pestrotsvet Formation in the Selinde section has a deeper history than the stratotype region. This conclusion is important for both constraining the age of the earliest Cambrian marine transgression on the Siberian platform and providing a clearer understanding of the pace and order of early Cambrian geochemical and biological events.
title Carbon and oxygen isotope ratios of Selinde River, southeastern Siberian platform
topic Isotope ratio mass spectrometry; OUTCROP; Outcrop sample; POINT DISTANCE from start; Sample code/label; Selinde; Siberia, Russia; δ13C, carbonate; δ18O, carbonate
url https://doi.org/10.1594/PANGAEA.688263