PHOSPHATASE AND MICROBIAL ACTIVITY WITH BIOCHEMICAL INDICATORS IN SEMI-PERMAFROST ACTIVE LAYER SEDIMENTS OVER THE PAST 10,000 YEARS

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dc.contributor.author Takano Y.
dc.contributor.author Marumo K.
dc.contributor.author Mori H.
dc.contributor.author Kaneko T.
dc.contributor.author Kobayashi K.
dc.contributor.author Ishikawa Y.
dc.date.accessioned 2024-11-17T03:30:12Z
dc.date.available 2024-11-17T03:30:12Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13994165
dc.identifier.citation Applied Geochemistry, 2006, 21, 1, 48-57
dc.identifier.issn 0883-2927
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46529
dc.description.abstract Core samples of boreal terrestrial sediments from depths of 0-300 cm at Rikubetsu, Hokkaido, Japan were analyzed for alkaline and acid phosphatase enzymatic activities. Enzymatic activities of alkaline phosphatase (ALP) and acid phosphatase (ACP) were greatest at the surface and decreased with depth; ALP and ACP activities were 25.5 and 22.0 nmol min-1 g-1, respectively, within the top 5 cm. These biological indicators were compared with measurements of microbial cell density and chemical indicators, including total organic C (TOC) and total hydrolyzed amino acids (THAA). The product-moment correlation coefficients (r) for ALP and ACP versus microbial cell density were 0.949 and 0.810, respectively. The coefficients for THAA and TOC versus ALP were 0.997 and 0.995, respectively. Vertical distributions of enzymatic activity are highly consistent with the observed microbial biomass profile and diagenetic organic matter in the sediment. However, the vertical profile of PO4 concentration shows a negative correlation coefficient for ALP and ACP of -0.937 and -0.855, respectively. Consequently, ALP and ACP were shown to be useful biomarkers of microbial activities in the terrestrial sediment over the past 10 ka at Rikubetsu, Hokkaido, Japan. © 2005 Elsevier Ltd. All rights reserved.
dc.title PHOSPHATASE AND MICROBIAL ACTIVITY WITH BIOCHEMICAL INDICATORS IN SEMI-PERMAFROST ACTIVE LAYER SEDIMENTS OVER THE PAST 10,000 YEARS
dc.type Статья
dc.identifier.doi 10.1016/j.apgeochem.2005.08.003


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