Pure siliceous ooze, a diagenetic environment for early chert formation.

Bohrmann, Gerhard, Abelmann, Andrea, Gersonde, Rainer, Hubberten, Hans and Kuhn, Gerhard (1994) Pure siliceous ooze, a diagenetic environment for early chert formation. Geology, 22 (3). p. 207. DOI 10.1130/0091-7613(1994)022<0207:PSOADE>2.3.CO;2.

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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.

Document Type: Article
Research affiliation: OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1130/0091-7613(1994)022<0207:PSOADE>2.3.CO;2
ISSN: 0091-7613
Date Deposited: 01 Jul 2019 10:49
Last Modified: 01 Jul 2019 10:49
URI: http://oceanrep.geomar.de/id/eprint/47045

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