Geochemical Perspectives,
Journal Year:
2021,
Volume and Issue:
unknown, P. 145 - 307
Published: Oct. 1, 2021
Complex
interactions
between
microbial
communities
and
geochemical
processes
drive
the
major
element
cycles
control
function
of
marine
sediments
as
a
dynamic
reservoir
organic
matter.
Sulfate
reduction
is
globally
dominant
pathway
anaerobic
mineralisation
main
source
sulfide.
The
effective
re-oxidation
this
sulfide
at
direct
or
indirect
expense
oxygen
prerequisite
for
aerobic
life
on
our
planet.
Although
largely
hidden
beneath
oxic
sediment
surface,
sulfur
cycle
therefore
critical
Earth’s
redox
state.
This
Geochemical
Perspectives
begins
with
brief
primer
description
my
own
scientific
journey
through
nearly
fifty
years
studies
geochemistry
microbiology.
Among
objectives
these
were
to
quantify
identify
behind
them.
Radiotracers
in
combination
chemical
analyses
have
thereby
been
used
extensively
laboratory
experiments,
supported
by
diverse
molecular
microbiological
methods.
following
sections
discuss
sulfate
reduction,
oxidation
disproportionation
inorganic
intermediates,
especially
elemental
thiosulfate.
experimental
approaches
enable
analysis
how
environmental
factors
such
substrate
concentration
temperature
affect
process
rates
concurrent
cryptic
cycle.
energy
chemolithotrophic
bacteria,
including
fascinating
big
bacteria
cable
supports
their
dark
CO2
fixation,
which
produces
new
biomass.
During
burial
aging
sediments,
predominant
change
cascade
reactions,
rate
matter
degradation
drops
continuously
over
many
orders
magnitude.
pathways
age
turnover
are
discussed.
In
deep
methanic
zone,
only
few
percent
entire
remains,
provides
small
boost
methane
oxidation.
stable
isotopes
provide
an
additional
tool
understand
diagenetic
processes,
whereby
isotope
fractionation
open
system
diagenesis
generate
differential
diffusion
flux
isotopes.
relation
carbon
seabed
contribution
methane,
paper
discusses
global
budget
role
different
depth
regions
ocean
–
from
coast
sea.
published
estimates
parameters
evaluated
compared.
Finally,
looks
future
perspectives
respect
gaps
current
understanding
need
further
studies.
Annual Review of Marine Science,
Journal Year:
2020,
Volume and Issue:
13(1), P. 161 - 175
Published: Aug. 4, 2020
Microbes
in
marine
sediments
represent
a
large
portion
of
the
biosphere,
and
resolving
their
ecology
is
crucial
for
understanding
global
ocean
processes.
Single-gene
diversity
surveys
have
revealed
several
uncultured
lineages
that
are
widespread
whose
ecological
roles
unknown,
advancements
computational
analysis
increasingly
genomic
data
sets
made
it
possible
to
reconstruct
individual
genomes
from
complex
microbial
communities.
Using
these
metagenomic
approaches
characterize
transforming
our
view
communities
on
floor
biodiversity
planet.
In
recent
years,
been
prominent
source
new
tree
life.
The
incorporation
into
existing
phylogenies
has
many
belong
distinct
phyla,
including
archaeal
phyla
advancing
origins
cellular
complexity
eukaryotes.
Detailed
comparisons
metabolic
potentials
clear
bacteria
archaea
capable
mediating
key
previously
undescribed
steps
carbon
nutrient
cycling.
Astrobiology,
Journal Year:
2020,
Volume and Issue:
20(6), P. 785 - 814
Published: May 29, 2020
On
November
5–8,
2019,
the
"Mars
Extant
Life:
What's
Next?"
conference
was
convened
in
Carlsbad,
New
Mexico.
The
gathered
a
community
of
actively
publishing
experts
disciplines
related
to
habitability
and
astrobiology.
Primary
conclusions
are
as
follows:
A
significant
subset
attendees
concluded
that
there
is
realistic
possibility
Mars
hosts
indigenous
microbial
life.
powerful
theme
permeated
key
search
for
martian
extant
life
lies
identifying
exploring
refugia
("oases"),
where
conditions
either
permanently
or
episodically
significantly
more
hospitable
than
average.
Based
on
our
existing
knowledge
Mars,
participants
highlighted
four
potential
refugium
(not
listed
priority
order):
Caves,
Deep
Subsurface,
Ices,
Salts.
group
did
not
attempt
reach
consensus
prioritization
these
candidate
environments,
but
instead
felt
defensible
would
require
future
competitive
process.
Within
context
we
identified
variety
geological
strategies
could
narrow
space.
Additionally,
summarized
number
measurement
techniques
be
used
detect
evidence
(if
present).
Again,
it
within
scope
prioritize
techniques—that
best
left
We
specifically
note
sensitivity
detection
methods
implemented
if
samples
were
returned
Earth
greatly
exceed
methodologies
at
Mars.
Finally,
important
lessons
guide
processes
can
derived
both
from
experiments
carried
out
terrestrial
laboratories
analog
field
sites
theoretical
modeling.
Microorganisms,
Journal Year:
2021,
Volume and Issue:
9(11), P. 2362 - 2362
Published: Nov. 15, 2021
A
combination
of
physicochemical
and
radiotracer
analysis,
high-throughput
sequencing
the
16S
rRNA,
particulate
methane
monooxygenase
subunit
(pmoA)
genes
was
used
to
link
a
microbial
community
profile
with
methane,
sulfur,
nitrogen
cycling
processes.
The
objects
study
were
surface
sediments
sampled
at
five
stations
in
northern
part
Barents
Sea.
content
upper
layers
(0–5
cm)
ranged
from
0.2
2.4
µM
increased
depth
(16–19
9.5
µM.
rate
oxidation
oxic
varied
2
23
nmol
CH4
L−1
day−1
decreased
0.3
anoxic
zone
16–19
cm.
Sulfate
reduction
rates
much
higher,
2.8
µmol
day−1.
In
sediments,
ammonia-oxidizing
Nitrosopumilaceae
abundant;
subsequent
nitrite
nitrate
can
be
carried
out
by
Nitrospira
sp.
Aerobic
could
performed
uncultured
deep-sea
cluster
3
gamma-proteobacterial
methanotrophs.
Undetectable
low
levels
methanogenesis
consistent
near
complete
absence
methanogens.
Anaerobic
deeper
likely
ANME-2a-2b
ANME-2c
archaea
consortium
sulfate-reducing
Desulfobacterota.
Sulfide
oxidized
nitrate-reducing
Sulfurovum
Thus,
sulfur
cycle
linked
anaerobic
cycle,
which
included
ammonium
denitrification
coupled
sulfide
sediments.
Methane
concentrations
biogeochemical
processes
Sea
noticeably
higher
than
oligotrophic
areas
Arctic
Ocean,
indicating
that
an
increase
concentration
significantly
activates
Geochemical Perspectives,
Journal Year:
2021,
Volume and Issue:
unknown, P. 145 - 307
Published: Oct. 1, 2021
Complex
interactions
between
microbial
communities
and
geochemical
processes
drive
the
major
element
cycles
control
function
of
marine
sediments
as
a
dynamic
reservoir
organic
matter.
Sulfate
reduction
is
globally
dominant
pathway
anaerobic
mineralisation
main
source
sulfide.
The
effective
re-oxidation
this
sulfide
at
direct
or
indirect
expense
oxygen
prerequisite
for
aerobic
life
on
our
planet.
Although
largely
hidden
beneath
oxic
sediment
surface,
sulfur
cycle
therefore
critical
Earth’s
redox
state.
This
Geochemical
Perspectives
begins
with
brief
primer
description
my
own
scientific
journey
through
nearly
fifty
years
studies
geochemistry
microbiology.
Among
objectives
these
were
to
quantify
identify
behind
them.
Radiotracers
in
combination
chemical
analyses
have
thereby
been
used
extensively
laboratory
experiments,
supported
by
diverse
molecular
microbiological
methods.
following
sections
discuss
sulfate
reduction,
oxidation
disproportionation
inorganic
intermediates,
especially
elemental
thiosulfate.
experimental
approaches
enable
analysis
how
environmental
factors
such
substrate
concentration
temperature
affect
process
rates
concurrent
cryptic
cycle.
energy
chemolithotrophic
bacteria,
including
fascinating
big
bacteria
cable
supports
their
dark
CO2
fixation,
which
produces
new
biomass.
During
burial
aging
sediments,
predominant
change
cascade
reactions,
rate
matter
degradation
drops
continuously
over
many
orders
magnitude.
pathways
age
turnover
are
discussed.
In
deep
methanic
zone,
only
few
percent
entire
remains,
provides
small
boost
methane
oxidation.
stable
isotopes
provide
an
additional
tool
understand
diagenetic
processes,
whereby
isotope
fractionation
open
system
diagenesis
generate
differential
diffusion
flux
isotopes.
relation
carbon
seabed
contribution
methane,
paper
discusses
global
budget
role
different
depth
regions
ocean
–
from
coast
sea.
published
estimates
parameters
evaluated
compared.
Finally,
looks
future
perspectives
respect
gaps
current
understanding
need
further
studies.