The former presence of organic matter caused its later absence: Burn‐down of organic matter in oceanic red beds enhanced by bioturbation (Eocene Variegated Shale, Carpathians)-Reference-Cited by-同舟云学术

The former presence of organic matter caused its later absence: Burn‐down of organic matter in oceanic red beds enhanced by bioturbation (Eocene Variegated Shale, Carpathians)

Published:2017-12-26 Issue:5 Volume:65 Page:1504-1519
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Wetzel Andreas¹,Uchman Alfred²

Affiliation:

1. Geologisches Institut der Universität Basel Bernoullistrasse 32 CH‐4056 Basel Switzerland

2. Institute of Geological Sciences Jagiellonian University Gronostajowa 3a PL 30‐387 Kraków Poland

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12436

Reference82 articles.

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5. On the use and abuse of N2 physisorption for the characterization of the pore structure of shales

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