Authigenic carbonate of ODP SIte 104-643 ...

Different generations of complex authigenic carbonates formed in siliceous muds (lithologic Unit IV) and hemipelagic clays (lithologic Unit V) of ODP Site 643, Leg 104 Norwegian Sea. The dominant phase in Unit IV is an early diagenetic Mn, Fe-calcite with a strong negative d13C ( -14 to -16 per mil)...

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Main Author: Henrich, Rüdiger
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.742922
https://doi.pangaea.de/10.1594/PANGAEA.742922
id ftdatacite:10.1594/pangaea.742922
record_format openpolar
spelling ftdatacite:10.1594/pangaea.742922 2024-09-15T18:26:47+00:00 Authigenic carbonate of ODP SIte 104-643 ... Henrich, Rüdiger 1989 application/zip https://dx.doi.org/10.1594/pangaea.742922 https://doi.pangaea.de/10.1594/PANGAEA.742922 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.104.119.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Drilling/drill rig Leg104 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1989 ftdatacite https://doi.org/10.1594/pangaea.74292210.2973/odp.proc.sr.104.119.1989 2024-08-01T10:52:43Z Different generations of complex authigenic carbonates formed in siliceous muds (lithologic Unit IV) and hemipelagic clays (lithologic Unit V) of ODP Site 643, Leg 104 Norwegian Sea. The dominant phase in Unit IV is an early diagenetic Mn, Fe-calcite with a strong negative d13C ( -14 to -16 per mil) signature, and slightly negative d180 values. The strong negative d13C results from extensive incorporation of 12C-enriched CO2 derived from bacterial degradation of marine organic matter into early Mn, Fe - calcite cements. Concomitant framboidal pyrite precipitation and abundant SEM microtextures showing excellent preservation of delicate structures of fragile diatom valves by outpourings with early Mn-calcites strongly support their shallow burial formation before the onset of compaction. Later generations of authigenic mineralizations in lithologic Unit IV include minor amounts of a second generation of calcite with platy crystals, possibly precipitated along with opal-A dissolution, and finally opal-CT ... : Supplement to: Henrich, Rüdiger (1989): Diagenetic environments of authigenic carbonates and opal-CT crystallization in lower Miocene to upper Oligocene deposits of the Norwegian Sea (ODP Site 643, Leg 104). In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 233-247 ... Article in Journal/Newspaper Norwegian Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Drilling/drill rig
Leg104
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Composite Core
Drilling/drill rig
Leg104
Joides Resolution
Ocean Drilling Program ODP
Henrich, Rüdiger
Authigenic carbonate of ODP SIte 104-643 ...
topic_facet Composite Core
Drilling/drill rig
Leg104
Joides Resolution
Ocean Drilling Program ODP
description Different generations of complex authigenic carbonates formed in siliceous muds (lithologic Unit IV) and hemipelagic clays (lithologic Unit V) of ODP Site 643, Leg 104 Norwegian Sea. The dominant phase in Unit IV is an early diagenetic Mn, Fe-calcite with a strong negative d13C ( -14 to -16 per mil) signature, and slightly negative d180 values. The strong negative d13C results from extensive incorporation of 12C-enriched CO2 derived from bacterial degradation of marine organic matter into early Mn, Fe - calcite cements. Concomitant framboidal pyrite precipitation and abundant SEM microtextures showing excellent preservation of delicate structures of fragile diatom valves by outpourings with early Mn-calcites strongly support their shallow burial formation before the onset of compaction. Later generations of authigenic mineralizations in lithologic Unit IV include minor amounts of a second generation of calcite with platy crystals, possibly precipitated along with opal-A dissolution, and finally opal-CT ... : Supplement to: Henrich, Rüdiger (1989): Diagenetic environments of authigenic carbonates and opal-CT crystallization in lower Miocene to upper Oligocene deposits of the Norwegian Sea (ODP Site 643, Leg 104). In: Eldholm, O; Thiede, J; Taylor, E; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 104, 233-247 ...
format Article in Journal/Newspaper
author Henrich, Rüdiger
author_facet Henrich, Rüdiger
author_sort Henrich, Rüdiger
title Authigenic carbonate of ODP SIte 104-643 ...
title_short Authigenic carbonate of ODP SIte 104-643 ...
title_full Authigenic carbonate of ODP SIte 104-643 ...
title_fullStr Authigenic carbonate of ODP SIte 104-643 ...
title_full_unstemmed Authigenic carbonate of ODP SIte 104-643 ...
title_sort authigenic carbonate of odp site 104-643 ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.742922
https://doi.pangaea.de/10.1594/PANGAEA.742922
genre Norwegian Sea
genre_facet Norwegian Sea
op_relation https://dx.doi.org/10.2973/odp.proc.sr.104.119.1989
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.74292210.2973/odp.proc.sr.104.119.1989
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