Biogenic silica in ODP Hole 105-647A ...

Eocene to Holocene sediments from Ocean Drilling Program (ODP) Site 647 (Leg 105) in the southern Labrador Sea, approximately 200 km south of the Gloria Drift deposits, were investigated for their biogenic silica composition. Three sections of different diagenetic alteration products of primary sili...

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Main Authors: Bohrmann, Gerhard, Stein, Ruediger
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.744936
https://doi.pangaea.de/10.1594/PANGAEA.744936
id ftdatacite:10.1594/pangaea.744936
record_format openpolar
spelling ftdatacite:10.1594/pangaea.744936 2024-09-30T14:38:11+00:00 Biogenic silica in ODP Hole 105-647A ... Bohrmann, Gerhard Stein, Ruediger 1989 application/zip https://dx.doi.org/10.1594/pangaea.744936 https://doi.pangaea.de/10.1594/PANGAEA.744936 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.105.121.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg105 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 1989 ftdatacite https://doi.org/10.1594/pangaea.74493610.2973/odp.proc.sr.105.121.1989 2024-09-02T08:42:43Z Eocene to Holocene sediments from Ocean Drilling Program (ODP) Site 647 (Leg 105) in the southern Labrador Sea, approximately 200 km south of the Gloria Drift deposits, were investigated for their biogenic silica composition. Three sections of different diagenetic alteration products of primary siliceous components could be distinguished: (1) opal-A was recorded in the Miocene and the early Oligocene time intervals with strongly corroded siliceous skeletons in the Miocene and mostly well preserved biogenic opal in the early Oligocene; (2) opal-CT precipitation occurs between 250-440 meters below seafloor (mbsf) (earliest Oligocene to late Eocene); (3) between 620-650 mbsf (early/middle Eocene), biogenic opal was transformed to clay minerals by authigenesis of smectites. Using accumulation rates of biogenic opal, paleoproductivity was estimated for the early Oligocene to late Eocene interval. A maximum productivity of biogenic silica probably occurred between 35.5 and 34.5 Ma (early Oligocene). No evidence ... : Supplement to: Bohrmann, Gerhard; Stein, Ruediger (1989): Biogenic silica at ODP Site 647 in the southern Labrador Sea: occurrence, diagenesis, and paleoceanographic implications. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 155-170 ... Article in Journal/Newspaper Labrador Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
Bohrmann, Gerhard
Stein, Ruediger
Biogenic silica in ODP Hole 105-647A ...
topic_facet Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
description Eocene to Holocene sediments from Ocean Drilling Program (ODP) Site 647 (Leg 105) in the southern Labrador Sea, approximately 200 km south of the Gloria Drift deposits, were investigated for their biogenic silica composition. Three sections of different diagenetic alteration products of primary siliceous components could be distinguished: (1) opal-A was recorded in the Miocene and the early Oligocene time intervals with strongly corroded siliceous skeletons in the Miocene and mostly well preserved biogenic opal in the early Oligocene; (2) opal-CT precipitation occurs between 250-440 meters below seafloor (mbsf) (earliest Oligocene to late Eocene); (3) between 620-650 mbsf (early/middle Eocene), biogenic opal was transformed to clay minerals by authigenesis of smectites. Using accumulation rates of biogenic opal, paleoproductivity was estimated for the early Oligocene to late Eocene interval. A maximum productivity of biogenic silica probably occurred between 35.5 and 34.5 Ma (early Oligocene). No evidence ... : Supplement to: Bohrmann, Gerhard; Stein, Ruediger (1989): Biogenic silica at ODP Site 647 in the southern Labrador Sea: occurrence, diagenesis, and paleoceanographic implications. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 155-170 ...
format Article in Journal/Newspaper
author Bohrmann, Gerhard
Stein, Ruediger
author_facet Bohrmann, Gerhard
Stein, Ruediger
author_sort Bohrmann, Gerhard
title Biogenic silica in ODP Hole 105-647A ...
title_short Biogenic silica in ODP Hole 105-647A ...
title_full Biogenic silica in ODP Hole 105-647A ...
title_fullStr Biogenic silica in ODP Hole 105-647A ...
title_full_unstemmed Biogenic silica in ODP Hole 105-647A ...
title_sort biogenic silica in odp hole 105-647a ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.744936
https://doi.pangaea.de/10.1594/PANGAEA.744936
genre Labrador Sea
genre_facet Labrador Sea
op_relation https://dx.doi.org/10.2973/odp.proc.sr.105.121.1989
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.74493610.2973/odp.proc.sr.105.121.1989
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