δ~(13)C variation in carbonate platform sediments of the Northern Tethys in Late Jurassic

Sergey Vladimirovich Rudko; Anton Borisovich Kuznetsov; Boris Glebovich Pokrovsky

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δ~(13)C variation in carbonate platform sediments of the Northern Tethys in Late Jurassic

机译：Δ〜（13）侏罗纪北部特质碳酸盐平台沉积物的变化

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摘要

Сarbon isotopic composition of Late Jurassic sediments displays a trend of ~(13)C depletion in the World ocean. Meanwhile, depending on local paleogeographical conditions, δ~(13)C curves for different palaeoprovinces differ in inclinations and absolute values (Nunn & Price 2010). That is why a separate δ~(13)C curve needs to be developed for every specific region. After such development, the inverse problem – correlation of the sedimentary complex by comparing δ~(13)C parameters – can be solved. A comparison of δ~(13)C values in contemporaneous sediments can be also used as an instrument for testing paleogeographical and paleoecological models.

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来源
《Geology, Geophysics & Environment》 |2016年第1期|共2页
作者
Sergey Vladimirovich Rudko; Anton Borisovich Kuznetsov; Boris Glebovich Pokrovsky;
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作者单位

Geological Institute of the Russian Academy of Sciences;

Moscow Russia;

Russian Academy of Sciences Institute of Precambrian Geology and Geochronology;

St. Petersburg Russia;

Geological Institute of the Russian Academy of Sciences;

Moscow Russia;

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原文格式 PDF
正文语种 eng
中图分类地质学;
关键词
δ~(13)C variation; carbonate platform; sediments;

机译：Δ〜（13）C变异;碳酸盐平台;沉积物;

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δ~(13)C variation in carbonate platform sediments of the Northern Tethys in Late Jurassic

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