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...
Main Authors: | , |
---|---|
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 |
_version_ |
1811640893355065344 |