Transport and depositional processes of organic matter evaluated by biomarker profiles in Miocene turbiditic sequences from Hokkaido, Japan

Extrabasinal turbidity currents, also known as hyperpycnal flows, can deposit vast amounts of organic carbon to the marine realm. On the other hand, intrabasinal turbidity currents are commonly thought to resuspend and further oxidize organic matter (OM), creating deposits with poor preservation of...

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Vydáno v:	Sedimentary geology Ročník 454; s. 106455
Hlavní autoři:	Ismail, Muhammad Adam, Asahi, Hiroyasu, Sawada, Ken
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Elsevier B.V 01.08.2023
Témata:	algae Biomarkers domain Hyperpycnal flow Japan marine environment Miocene epoch organic carbon Organic matter sediments Terrestrial environment Turbidites turbidity woody plants Terrestrial environment Biomarkers Organic matter Hyperpycnal flow Turbidites
ISSN:	0037-0738, 1879-0968
On-line přístup:	Získat plný text
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