<?xml version="1.0" encoding="utf-8" standalone="yes"?><rss version="2.0" xmlns:atom="http://www.w3.org/2005/Atom"><channel><title>Motoo Utsumi | Amano Lab | Hokkaido University</title><link>https://amanoresearch.com/authors/motoo-utsumi/</link><atom:link href="https://amanoresearch.com/authors/motoo-utsumi/index.xml" rel="self" type="application/rss+xml"/><description>Motoo Utsumi</description><generator>HugoBlox Kit (https://hugoblox.com)</generator><language>en-us</language><lastBuildDate>Wed, 14 Dec 2022 00:00:00 +0000</lastBuildDate><item><title>A device for assessing microbial activity under ambient hydrostatic pressure: The in situ microbial incubator (ISMI)</title><link>https://amanoresearch.com/publication/amano-202212-ismi/</link><pubDate>Wed, 14 Dec 2022 00:00:00 +0000</pubDate><guid>https://amanoresearch.com/publication/amano-202212-ismi/</guid><description>&lt;p&gt;Microbes in the dark ocean are exposed to hydrostatic pressure increasing with depth. Activity rate
measurements and biomass production of dark ocean microbes are, however, almost exclusively
performed under atmospheric pressure conditions due to technical constraints of sampling equipment
maintaining in situ pressure conditions. To evaluate the microbial activity under in situ
hydrostatic pressure, we designed and thoroughly tested an in situ microbial incubator (ISMI). The
ISMI allows autonomously collecting and incubating seawater at depth, injection of substrate and
fixation of the samples after a preprogramed incubation time. The performance of the ISMI was tested
in a high‐pressure tank and in several field campaigns under ambient hydrostatic pressure by
measuring prokaryotic bulk 3H‐leucine incorporation rates. Overall, prokaryotic leucine
incorporation rates were lower at in situ pressure conditions than under to depressurized conditions
reaching only about 50% of the heterotrophic microbial activity measured under depressurized
conditions in bathypelagic waters in the North Atlantic Ocean off the northwestern Iberian
Peninsula. Our results show that the ISMI is a valuable tool to reliably determine the metabolic
activity of deep‐sea microbes at in situ hydrostatic pressure conditions. Hence, we advocate that
deep‐sea biogeochemical and microbial rate measurements should be performed under in situ pressure
conditions to obtain a more realistic view on deep‐sea biotic processes.&lt;/p&gt;</description></item><item><title>Limited carbon cycling due to high-pressure effects on the deep-sea microbiome</title><link>https://amanoresearch.com/publication/amano-202211-pressure/</link><pubDate>Mon, 28 Nov 2022 00:00:00 +0000</pubDate><guid>https://amanoresearch.com/publication/amano-202211-pressure/</guid><description>&lt;p&gt;Deep-sea microbial communities are exposed to high-pressure conditions, which has a variable impact
on prokaryotes depending on whether they are piezophilic (that is, pressure-loving), piezotolerant
or piezosensitive. While it has been suggested that elevated pressures lead to higher
community-level metabolic rates, the response of these deep-sea microbial communities to the
high-pressure conditions of the deep sea is poorly understood. Based on microbial activity
measurements in the major oceanic basins using an in situ microbial incubator, we show that the bulk
heterotrophic activity of prokaryotic communities becomes increasingly inhibited at higher
hydrostatic pressure. At 4,000 m depth, the bulk heterotrophic prokaryotic activity under in situ
hydrostatic pressure was about one-third of that measured in the same community at atmospheric
pressure conditions. In the bathypelagic zone—between 1,000 and 4,000 m depth—~85% of the
prokaryotic community was piezotolerant and ~5% of the prokaryotic community was piezophilic.
Despite piezosensitive-like prokaryotes comprising only ~10% (mainly members of Bacteroidetes,
Alteromonas ) of the deep-sea prokaryotic community, the more than 100-fold metabolic activity
increase of these piezosensitive prokaryotes upon depressurization leads to high apparent bulk
metabolic activity. Overall, the heterotrophic prokaryotic activity in the deep sea is likely to be
substantially lower than hitherto assumed, with major impacts on the oceanic carbon cycling.&lt;/p&gt;</description></item><item><title>Impact of hydrostatic pressure on organic carbon cycling of the deep-sea microbiome</title><link>https://amanoresearch.com/publication/amano-202203-hydrostatic-pressure/</link><pubDate>Thu, 31 Mar 2022 00:00:00 +0000</pubDate><guid>https://amanoresearch.com/publication/amano-202203-hydrostatic-pressure/</guid><description>&lt;p&gt;Deep-sea microbial communities are exposed to high hydrostatic pressure. While some of these
deep-sea prokaryotes are adapted to high-pressure conditions, the contribution of piezophilic (i.e.,
pressure-loving) and piezotolerant prokaryotes to the total deep-sea prokaryotic community remains
unknown. Here we show that the metabolic activity of prokaryotic communities is increasingly
inhibited with increasing hydrostatic pressure. At 4,000 m depth, the bulk heterotrophic prokaryotic
activity under in sit u hydrostatic pressure was only about one-third of that measured on the same
community at atmospheric pressure conditions. Only ∼5% of the bathypelagic prokaryotic community are
piezophilic while ∼85% of the deep-sea prokaryotes are piezotolerant. A small fraction (∼10%) of the
deep-sea prokaryotes is piezosensitive (mainly members of Bacteroidetes, Alteromonas) exhibiting
specific survival strategies at meso- and bathypelagic depths. These piezosensitive bacteria
elevated their activity by more than 100-fold upon depressurization. Hence, the consistently higher
bulk metabolic activity of the deep-sea prokaryotic community measured upon depressurization is due
to a rather small fraction of the prokaryotic community. Overall, the heterotrophic prokaryotic
activity in the deep-sea is substantially lower than hitherto assumed with major impacts on the
oceanic carbon cycling.&lt;/p&gt;</description></item><item><title>Dynamics of the prokaryotic and eukaryotic microbial community during a cyanobacterial bloom</title><link>https://amanoresearch.com/publication/qian-202110-cyanobacterial/</link><pubDate>Mon, 18 Oct 2021 00:00:00 +0000</pubDate><guid>https://amanoresearch.com/publication/qian-202110-cyanobacterial/</guid><description>&lt;p&gt;Toxic cyanobacterial blooms frequently develop in eutrophic freshwater bodies worldwide. Microcystis
species produce microcystins (MCs) as a cyanotoxin. Certain bacteria that harbor the mlr gene
cluster, especially mlrA, are capable of degrading MCs. However, MC-degrading bacteria may possess
or lack mlr genes (mlr+ and mlr− genotypes, respectively). In this study, we investigated the
genotype that predominantly contributes to biodegradation and cyanobacterial predator community
structure with change in total MC concentration in an aquatic environment. The 2 genotypes coexisted
but mlr+ predominated, as indicated by the negative correlation between mlrA gene copy abundance and
total MC concentration. At the highest MC concentrations, predation pressure by Phyllopoda,
Copepoda, and Monogononta (rotifers) was reduced; thus, MCs may be toxic to cyanobacterial
predators. The results suggest that cooperation between MC-degrading bacteria and predators may
reduce Microcystis abundance and MC concentration.&lt;/p&gt;</description></item><item><title>Response of microcystin biosynthesis and its biosynthesis gene cluster transcription in Microcystis aeruginosa on electrochemical oxidation</title><link>https://amanoresearch.com/publication/gao-201806-microcystin/</link><pubDate>Fri, 01 Jun 2018 00:00:00 +0000</pubDate><guid>https://amanoresearch.com/publication/gao-201806-microcystin/</guid><description/></item><item><title>Musty-odor occurrence and their causative microorganisms in a water supply source</title><link>https://amanoresearch.com/publication/amano-2008-musty-odor-dam/</link><pubDate>Tue, 01 Jan 2008 00:00:00 +0000</pubDate><guid>https://amanoresearch.com/publication/amano-2008-musty-odor-dam/</guid><description/></item></channel></rss>