Contrasting intensity of aragonite dissolution and dolomite cementation in glacial versus interglacial intervals of a subtropical carbonate succession-Reference-Cited by-同舟云学术

Contrasting intensity of aragonite dissolution and dolomite cementation in glacial versus interglacial intervals of a subtropical carbonate succession

Published:2022-03-17 Issue:5 Volume:69 Page:2131-2150
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Reuning Lars¹^ORCID,Deik Hanaa²,Petrick Benjamin¹,Auer Gerald³,Takayanagi Hideko⁴,Iryu Yasufumi⁴^ORCID,Courtillat Margot⁵,Bassetti Maria‐Angela⁵

Affiliation:

1. Institute of Geosciences CAU Kiel University Ludewig‐Meyn‐Straße 10 Kiel 24118 Germany

2. Geological Institute RWTH Aachen University Wüllnerstrasse2 Aachen 52062 Germany

3. Institute of Earth Sciences (Geology and Paleontology) NAWI Graz Geocenter University of Graz Heinrichstraße 26 Graz 8010 Austria

4. Institute of Geology and Paleontology Tohoku University Aobayama Sendai 980‐8578 Japan

5. Centre de Formation et de Recherche sur les Environnements Méditerranéens Université de Perpignan Via Domitia UMR 5110 CEDEX 52 Avenue Paul Alduy Perpignan F‐66860 France

Funder

Deutsche Forschungsgemeinschaft

Studienstiftung des Deutschen Volkes

Publisher

Wiley

Subject

Stratigraphy,Geology,General Medicine

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12985

Reference81 articles.

1. Destructive diagenesis of carbonate sediments in the eastern Skagerrak, North Sea

2. Organic carbon remineralisation and complex, early diagenetic solid–aqueous solution–gas interactions: Case study ODP Leg 204, Site 1246 (Hydrate Ridge)