_version_ 1867168379182252032
author Domanov, Mikhail M
Kobylyansky, V V
Svininnikov, A I
Vodyanaya, Elena G
Vladimirov, M V
Kuznetsov, Oleg L
author_facet Domanov, Mikhail M
Kobylyansky, V V
Svininnikov, A I
Vodyanaya, Elena G
Vladimirov, M V
Kuznetsov, Oleg L
collection Datos científicos de ciencias marinas y ambientales
contents Sulfide, S°, and thiosulfate were determined in waters of the Baltic Sea. Microquantities of these compounds were observed in oxic waters. Concentration levels of reduced sulfur compounds in Baltic oxic waters were very close to levels of the Black Sea oxic zone. Thiosulfate and S° were predominate compounds in oxic water whereas sulfide was a predominant compound Baltic waters high in hydrogen sulfide. Conclusion was made that during sedimentation in oxic waters anaerobic microorganisms along with aerobic bacteria take part in mineralization of organic matter. They exist on surfaces and in microniches of particles of organic detritus.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_762432
institution PANGAEA
language en
publishDate 2004
publisher PANGAEA
record_format pangaea
spellingShingle (Table 6b) 137Cs concentrations in surface layer bottom sediments of the Sea of Japan in 1994 and in 2002
Domanov, Mikhail M
Kobylyansky, V V
Svininnikov, A I
Vodyanaya, Elena G
Vladimirov, M V
Kuznetsov, Oleg L
Archive of Ocean Data; ARCOD; Caesium-137, activity per mass; Date/Time of event; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Gamma-ray spectrometry; JJKRE94-2; JJKRE94-3; JJKRE94-6; Latitude of event; Longitude of event; MULT; Multiple investigations; PGORD-03-53; PGORD-07-53; PGORD-09-53; Sea of Japan; Year of publication
Sulfide, S°, and thiosulfate were determined in waters of the Baltic Sea. Microquantities of these compounds were observed in oxic waters. Concentration levels of reduced sulfur compounds in Baltic oxic waters were very close to levels of the Black Sea oxic zone. Thiosulfate and S° were predominate compounds in oxic water whereas sulfide was a predominant compound Baltic waters high in hydrogen sulfide. Conclusion was made that during sedimentation in oxic waters anaerobic microorganisms along with aerobic bacteria take part in mineralization of organic matter. They exist on surfaces and in microniches of particles of organic detritus.
title (Table 6b) 137Cs concentrations in surface layer bottom sediments of the Sea of Japan in 1994 and in 2002
topic Archive of Ocean Data; ARCOD; Caesium-137, activity per mass; Date/Time of event; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Gamma-ray spectrometry; JJKRE94-2; JJKRE94-3; JJKRE94-6; Latitude of event; Longitude of event; MULT; Multiple investigations; PGORD-03-53; PGORD-07-53; PGORD-09-53; Sea of Japan; Year of publication
url https://doi.org/10.1594/PANGAEA.762432