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.
Proceedings of the National Academy of Sciences,
Journal Year:
2018,
Volume and Issue:
115(25), P. 6506 - 6511
Published: May 21, 2018
Significance
The
composition
of
the
biosphere
is
a
fundamental
question
in
biology,
yet
global
quantitative
account
biomass
each
taxon
still
lacking.
We
assemble
census
all
kingdoms
life.
This
analysis
provides
holistic
view
and
allows
us
to
observe
broad
patterns
over
taxonomic
categories,
geographic
locations,
trophic
modes.
Frontiers in Microbiology,
Journal Year:
2019,
Volume and Issue:
10
Published: April 24, 2019
Microbial
dissimilatory
sulfate
reduction
to
sulfide
is
a
predominant
terminal
pathway
of
organic
matter
mineralization
in
the
anoxic
seabed.
Chemical
or
microbial
oxidation
produced
establishes
complex
network
pathways
sulfur
cycle,
leading
intermediate
species
and
partly
back
sulfate.
The
intermediates
include
elemental
sulfur,
polysulfides,
thiosulfate,
sulfite,
which
are
all
substrates
for
further
oxidation,
disproportionation.
New
microbiological
discoveries,
such
as
long-distance
electron
transfer
through
oxidizing
cable
bacteria,
add
complexity.
Isotope
exchange
reactions
play
an
important
role
stable
isotope
geochemistry
experimental
study
transformations
using
radiotracers.
Microbially
catalyzed
processes
reversible
whereby
back-reaction
affects
our
interpretation
radiotracer
experiments
provides
mechanism
fractionation.
We
here
review
progress
current
status
understanding
cycle
seabed
with
respect
its
ecology,
biogeochemistry,
geochemistry.
Marine Genomics,
Journal Year:
2015,
Volume and Issue:
24, P. 185 - 196
Published: Dec. 1, 2015
In
marine
sediments,
DNA
occurs
both
inside
and
outside
living
organisms.
not
enclosed
in
cells
may
account
for
the
largest
fraction
of
total
DNA,
include
molecules
locked
within
dead
cells,
organic
inorganic
aggregates,
adsorbed
onto
mineral
matrices,
viral
DNA.
This
comprises
genetic
material
released
situ
from
sediment
microbial
communities,
as
well
pelagic
terrestrial
origin
deposited
to
seafloor.
undermines
assumption
a
direct
link
between
overall
pool
local,
currently
assemblages,
terms
cell
abundance
diversity.
At
same
time,
extracellular
provide
an
integrated
view
biodiversity
ecological
processes
occurring
on
land,
water
columns,
sediments
themselves,
thereby
acting
archive
information
which
can
be
used
reconstruct
past
changes
source
environments.
this
review,
we
identify
discuss
pools
with
special
focus
its
origin,
dynamics,
methodological
implications.
Achievements
deciphering
held
each
are
presented
along
still-standing
challenges
major
gaps
current
knowledge.
Proceedings of the National Academy of Sciences,
Journal Year:
2020,
Volume and Issue:
117(44), P. 27587 - 27597
Published: Oct. 19, 2020
Significance
Marine
sediment
covers
70%
of
Earth’s
surface
and
harbors
as
much
biomass
seawater.
However,
the
global
taxonomic
diversity
marine
sedimentary
communities,
spatial
distribution
that
remain
unclear.
We
investigated
microbial
composition
from
40
globally
distributed
sampling
locations,
spanning
depths
0.1
to
678
m.
Statistical
analysis
reveals
oxygen
presence
or
absence
organic
carbon
concentration
are
key
environmental
factors
for
defining
communities.
Global
richness
predicted
by
species–area
relationship
models
is
7.85
×
10
3
6.10
5
Archaea
3.28
4
2.46
6
Bacteria
amplicon
sequence
variants,
which
comparable
in
seawater
topsoil.
Nature Communications,
Journal Year:
2018,
Volume and Issue:
9(1)
Published: Nov. 21, 2018
Microbes
in
Guaymas
Basin
(Gulf
of
California)
hydrothermal
sediments
thrive
on
hydrocarbons
and
sulfur
experience
steep,
fluctuating
temperature
chemical
gradients.
The
functional
capacities
communities
inhabiting
this
dynamic
habitat
are
largely
unknown.
Here,
we
reconstructed
551
genomes
from
hydrothermally
influenced,
nearby
cold
belonging
to
56
phyla
(40
uncultured).
These
comprise
22
unique
lineages,
including
five
new
candidate
phyla.
In
contrast
findings
hydrocarbon
seeps,
hydrothermal-associated
more
diverse
archaea
dominate
over
bacteria.
Genome-based
metabolic
inferences
provide
first
insights
into
the
ecological
niches
these
uncultured
microbes,
methane
cycling
Crenarchaeota
alkane
utilization
ANME-1.
shaped
by
a
high
biodiversity,
partitioning
among
nitrogen
pathways
redundancy
core
carbon-processing
pathways.
select
for
distinctive
microbial
that
stand
out
expansive
open
up
physiological
perspectives
ecosystem
function.
Proceedings of the National Academy of Sciences,
Journal Year:
2017,
Volume and Issue:
114(11), P. 2940 - 2945
Published: Feb. 27, 2017
Significance
Our
study
shows
that
deep
subseafloor
sediments
are
populated
by
descendants
of
rare
members
surface
sediment
microbial
communities
become
predominant
during
burial
over
thousands
years.
We
provide
estimates
mutation
rates
and
strength
purifying
selection
in
a
set
taxonomically
diverse
populations
marine
show
their
genetic
diversification
is
minimal
burial.
data
suggest
the
ability
microbes
to
subsist
energy-deprived
biosphere
not
acquired
but
these
were
already
capable
living
this
unique
environment.
These
findings
represent
significant
step
toward
understanding
bounds
for
life
its
connection
world.