Mineralogical and chemical investigation of biogenic siliceous Antarctic deep-ses sediments
The formation of marine opal-CT nodules or layers as early diagenetic deposits has been documented only in Antarctic deep-sea sediments. In contrast, porcellanites and cherts in land sections and Deep Sea Drilling Project and Ocean Drilling Program drill sites are usually found in sediment sections...
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1994
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.735716 2023-05-15T13:42:10+02:00 Mineralogical and chemical investigation of biogenic siliceous Antarctic deep-ses sediments Bohrmann, Gerhard Abelmann, Andrea Gersonde, Rainer Kuhn, Gerhard LATITUDE: -53.188330 * LONGITUDE: 5.330330 * DATE/TIME START: 1991-04-08T14:59:00 * DATE/TIME END: 1991-04-08T14:59:00 1994-03-25 application/zip, 4 datasets https://doi.pangaea.de/10.1594/PANGAEA.735716 https://doi.org/10.1594/PANGAEA.735716 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.735716 https://doi.org/10.1594/PANGAEA.735716 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Bohrmann, Gerhard; Abelmann, Andrea; Gersonde, Rainer; Kuhn, Gerhard (1994): Pure siliceous ooze, a diagenetic environment for early chert formation. Geology, 22(3), 207-210, https://doi.org/10.1130/0091-7613(1994)022%3C0207:PSOADE%3E2.3.CO;2 ANT-IX/4 AWI_Paleo gcmd1 KL Meteor Rise Paleoenvironmental Reconstructions from Marine Sediments @ AWI Piston corer (BGR type) Polarstern PS18 PS18/247 PS2089-2 Silicon Cycling in the World Ocean SINOPS Dataset 1994 ftpangaea https://doi.org/10.1594/PANGAEA.735716 https://doi.org/10.1130/0091-7613(1994)022%3C0207:PSOADE%3E2.3.CO;2 2023-01-20T07:31:42Z The formation of marine opal-CT nodules or layers as early diagenetic deposits has been documented only in Antarctic deep-sea sediments. In contrast, porcellanites and cherts in land sections and Deep Sea Drilling Project and Ocean Drilling Program drill sites are usually found in sediment sections of Miocene age and older. During R.V. Polarstem cruises ANT-IX/3 and 4, young porcellanites were recovered for the first time in contact with their host sediment in two cores from the Atlantic sector of the southern ocean. Chemical and mineralogical studies of these deposits and their surrounding sediments have increased knowledge about very early chert formation. In both cores the porcellanites are embedded in sediments rich in opal-A with extremely low levels of detrital minerals, an environment that seems conducive to a rapid transformation of biogenic silica into porcellanites. Dataset Antarc* Antarctic Southern Ocean PANGAEA - Data Publisher for Earth & Environmental Science Antarctic Southern Ocean ENVELOPE(5.330330,5.330330,-53.188330,-53.188330) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
ANT-IX/4 AWI_Paleo gcmd1 KL Meteor Rise Paleoenvironmental Reconstructions from Marine Sediments @ AWI Piston corer (BGR type) Polarstern PS18 PS18/247 PS2089-2 Silicon Cycling in the World Ocean SINOPS |
spellingShingle |
ANT-IX/4 AWI_Paleo gcmd1 KL Meteor Rise Paleoenvironmental Reconstructions from Marine Sediments @ AWI Piston corer (BGR type) Polarstern PS18 PS18/247 PS2089-2 Silicon Cycling in the World Ocean SINOPS Bohrmann, Gerhard Abelmann, Andrea Gersonde, Rainer Kuhn, Gerhard Mineralogical and chemical investigation of biogenic siliceous Antarctic deep-ses sediments |
topic_facet |
ANT-IX/4 AWI_Paleo gcmd1 KL Meteor Rise Paleoenvironmental Reconstructions from Marine Sediments @ AWI Piston corer (BGR type) Polarstern PS18 PS18/247 PS2089-2 Silicon Cycling in the World Ocean SINOPS |
description |
The formation of marine opal-CT nodules or layers as early diagenetic deposits has been documented only in Antarctic deep-sea sediments. In contrast, porcellanites and cherts in land sections and Deep Sea Drilling Project and Ocean Drilling Program drill sites are usually found in sediment sections of Miocene age and older. During R.V. Polarstem cruises ANT-IX/3 and 4, young porcellanites were recovered for the first time in contact with their host sediment in two cores from the Atlantic sector of the southern ocean. Chemical and mineralogical studies of these deposits and their surrounding sediments have increased knowledge about very early chert formation. In both cores the porcellanites are embedded in sediments rich in opal-A with extremely low levels of detrital minerals, an environment that seems conducive to a rapid transformation of biogenic silica into porcellanites. |
format |
Dataset |
author |
Bohrmann, Gerhard Abelmann, Andrea Gersonde, Rainer Kuhn, Gerhard |
author_facet |
Bohrmann, Gerhard Abelmann, Andrea Gersonde, Rainer Kuhn, Gerhard |
author_sort |
Bohrmann, Gerhard |
title |
Mineralogical and chemical investigation of biogenic siliceous Antarctic deep-ses sediments |
title_short |
Mineralogical and chemical investigation of biogenic siliceous Antarctic deep-ses sediments |
title_full |
Mineralogical and chemical investigation of biogenic siliceous Antarctic deep-ses sediments |
title_fullStr |
Mineralogical and chemical investigation of biogenic siliceous Antarctic deep-ses sediments |
title_full_unstemmed |
Mineralogical and chemical investigation of biogenic siliceous Antarctic deep-ses sediments |
title_sort |
mineralogical and chemical investigation of biogenic siliceous antarctic deep-ses sediments |
publisher |
PANGAEA |
publishDate |
1994 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.735716 https://doi.org/10.1594/PANGAEA.735716 |
op_coverage |
LATITUDE: -53.188330 * LONGITUDE: 5.330330 * DATE/TIME START: 1991-04-08T14:59:00 * DATE/TIME END: 1991-04-08T14:59:00 |
long_lat |
ENVELOPE(5.330330,5.330330,-53.188330,-53.188330) |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic Southern Ocean |
genre_facet |
Antarc* Antarctic Southern Ocean |
op_source |
Supplement to: Bohrmann, Gerhard; Abelmann, Andrea; Gersonde, Rainer; Kuhn, Gerhard (1994): Pure siliceous ooze, a diagenetic environment for early chert formation. Geology, 22(3), 207-210, https://doi.org/10.1130/0091-7613(1994)022%3C0207:PSOADE%3E2.3.CO;2 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.735716 https://doi.org/10.1594/PANGAEA.735716 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.735716 https://doi.org/10.1130/0091-7613(1994)022%3C0207:PSOADE%3E2.3.CO;2 |
_version_ |
1766163748485070848 |