Earth-Science Reviews,
Journal Year:
2024,
Volume and Issue:
254, P. 104821 - 104821
Published: May 25, 2024
Clinoforms
are
ubiquitous
depositional
surfaces
in
sedimentary
systems.
The
quintessential
shape,
with
a
flat
or
gentle
topset,
sloping
foreset,
and
to
bottomset,
is
recognizable
the
smallest
ripple
kilometer
high
edges
of
continents.
Essentially
shape
one
which
develops
differential
sedimentation
away
from
source.
Systematic
decay
transport
competence
and/or
sediment
amount
site
favouring
deposition,
generates
loading
typically
lens-shaped
body.
lithology,
grain
size,
water
depth,
hydrodynamic
factors,
mechanisms,
antecedent
topography,
relative
sea
level
rate
all
interact
create
different
sizes,
slopes
shapes.
Meanwhile
there
several
fundamental
similarities
between
clinoforms,
even
bedwave
features
(ripples
dunes),
despite
forming
under
very
conditions.
All
clinoforms
some
extent
governed
by
accommodation
energy
limiting
factors
(water
agitation
flow
regime),
controls
their
height,
proxy
influences
slope
angle.
Lithology
exerts
control,
can
build
angle
repose,
higher
for
coarser
non-cohesive
sediment,
while
cohesive
gentler
slopes,
also
fail
at
lower
angles.
Sediment
repose
steep
linear
segments,
but
conversely
on
continental
margins
extremely
low
angle,
probably
reflecting
little
along-slope
contrast
mud-dominance.
clinothems
similar
lithology
display
wide
range
foreset
angles,
indicating
numerous
additional
controls.
Sedimentation
appears
exert
significant
control
steepness,
limited
promoting
steeper
related
basinward
thinning
deposits.
observation
greater
depth
response
deepening
environments
generating
effect
comparatively
less
sedimentation.
Processes
important
controlling
as
tidal
wave
reworking,
debris
flows,
overpressure
failure,
Turbidity
currents
meanwhile
part
dynamic
system
both
steepen
slope.
There
four
basic
clinoform
shapes:
concave,
linear,
convex,
sigmoidal.
These
develop
variations
along
profile
driven
erosion/bypass/factors
deposition/accumulation/waning
supply.
Curvature
tends
be
an
indication
contrast,
such
erosional
sandier
muddier
Sigmoidal
clinothems,
associated
more
trajectories,
shorter
than
concave
clinothems.
Decaying
shear-zone
reworking
erosion
shapes
rounded
rollover.
carrying
capacity
ensuing
curvature.
Concave
lacking
topsets
sharp
rollovers
often
longer
sigmoidal
forms.
Their
formation
likely
closely
linked
increased
accumulation
through
bypass,
turbidity
currents,
suspension-dominated
deposition
smaller
clinoforms.
In
this
ripples
differ,
transition
rounding
crest,
unlike
larger
Science Advances,
Journal Year:
2024,
Volume and Issue:
10(18)
Published: May 3, 2024
Deltas
are
threatened
by
erosion
due
to
climate
change
and
reduced
sediment
supply,
but
their
response
these
changes
remains
poorly
quantified.
We
investigate
the
abandoned
Yellow
River
delta
that
has
transitioned
from
rapid
growth
ongoing
deterioration
a
river
avulsion
removing
supply.
Integrating
bathymetric
data,
process
observations,
transport
modeling,
we
find
while
subaerial
was
stabilized
engineering
measures,
subaqueous
continued
erode
intensified
storms,
losing
39%
of
its
mass
deposited
before
avulsion.
Long-term
observations
show
winter
storms
initiate
scouring
delta,
contributing
up
70%
seabed
erosion.
then
analyze
108
global
deltas
assess
risks
identify
17
facing
similar
situations
decline
storm
intensification
during
past
40
years.
Our
findings
suggest
must
be
integrated
into
sustainability
evaluations.
Geophysical Research Letters,
Journal Year:
2025,
Volume and Issue:
52(4)
Published: Feb. 22, 2025
Abstract
Nearshore
erosion
is
well‐documented
in
sediment‐deficit
river
deltas
but
remains
less
understood
beyond
their
delta
front
(DF),
particularly
its
extension
to
the
deeper
prodelta
(PD)
and
distal
mud
(DM).
This
study
investigates
response
of
Changjiang
subaqueous
DM
sediment
decline
following
2003
closure
Three
Gorges
Dam.
By
analyzing
temporal
spatial
variations
210
Pb
ex
profile
styles,
discrepancies
between
137
Cs
accumulation
rates,
surface
grain
sizes,
we
identified
onset
at
DF
shortly
after
2003,
which
spread
PD
by
2009
reached
northern
2015.
tracking
burial
depths
1963
peak,
found
progressively
lower
rates
newly
eroded
subzones
primarily
due
redistribution.
study,
leveraging
historical
radionuclides
data,
offers
a
valuable
approach
for
monitoring
areas
lacking
remote
sensing
detection
bathymetric
data.
Abstract
We
review
impacts
of
climate
change,
energy
scarcity,
and
economic
frameworks
on
sustainability
natural
human
systems
in
coastal
zones,
areas
high
biodiversity,
productivity,
population
density,
activity.
More
than
50%
the
global
lives
within
200
km
a
coast,
mostly
tropical
developing
countries.
These
developed
during
stable
Holocene
conditions.
Changes
forcings
are
threatening
ecosystems
populations.
During
Holocene,
earth
warmed
became
wetter
more
productive.
Climate
changes
impacting
via
sea
level
rise,
stronger
cyclones,
basin
inputs,
extreme
weather
events.
passing
tipping
points
as
fossil
fuel-powered
industrial-technological-agricultural
revolution
has
overwhelmed
source–sink
functions
biosphere
degraded
systems.
The
current
status
industrialized
society
is
primarily
result
fuel
(FF)
use.
FFs
provided
80%
primary
projected
to
decline
by
mid-century.
This
profound
implications
for
societal
requirements,
including
transition
renewable
economy.
development
industrial
economy
allowed
social
become
spatially
separated
from
their
dominant
food
sources.
will
difficult
maintain
with
fading
cheap
energy.
It
seems
inevitable
that
past
growth
use,
resource
consumption,
cannot
be
sustained,
forefront
these
challenges.
Rapid
planning
cooperation
necessary
minimize
associated
coming
transition.
There
an
urgent
need
new
framework
guide
through
mainstream
neoclassical
economics
not
based
sciences
does
adequately
consider
either
importance
or
work
nature.
Annual Review of Environment and Resources,
Journal Year:
2024,
Volume and Issue:
49(1), P. 105 - 135
Published: Sept. 4, 2024
We
review
the
functioning
and
sustainability
of
coastal
marshes
mangroves.
Urbanized
humans
have
a
7,000-year-old
enduring
relationship
to
wetlands.
Wetlands
include
marshes,
salt
flats,
saline
freshwater
forests.
Coastal
wetlands
occur
in
all
climate
zones
but
are
most
abundant
deltas.
Mangroves
tropical,
whereas
from
tropical
boreal
areas.
Quantification
wetland
areas
has
advanced
recent
years
is
still
insufficiently
accurate.
Climate
change
sea-level
rise
predicted
lead
significant
losses
other
impacts
on
associated
with
them.
Landward
migration
retreat
not
expected
significantly
reduce
losses.
Nitrogen
watershed
inputs
unlikely
alter
marsh
stability
because
loadings
mostly
lower
than
those
fertilization
studies
that
show
decreased
belowground
biomass
increased
decomposition
soil
organic
matter.
Blue
carbon
impacts.
The
high
values
ecosystem
goods
services
be
reduced
by
area
Humans
had
strong
Holocene,
these
increase
Anthropocene.
Earth s Future,
Journal Year:
2024,
Volume and Issue:
12(4)
Published: April 1, 2024
Abstract
Estuaries
have
great
ecological
and
economic
value
sustain
both
population
growth.
Global‐scale
analyses
suggest
that
human
activities
drive
estuarine
area
change
but
these
projections
neglect
direct
human‐estuary
interactions
socio‐economic
feedbacks.
Here,
we
quantified
changes
of
2,396
estuaries
in
response
to
recent
impacts
(e.g.,
land
reclamation,
dam
construction)
development
between
1984
2019,
find
shrank
by
5,372
km
2
whereas
upland
submergence
created
5,015
elsewhere.
Approximately
44%
(
n
=
1,046)
today's
been
directly
altered
through
construction,
or
a
combination
both,
∼250,000
acres
(1,027
)
converted
urban
agricultural
fields.
Nearly
90%
(923
reclamation
occurred
Asia
linked
advances
during
the
middle‐income
stage.
Additional
historical
mapping
5‐year
interval
revealed
while
alterations
were
insignificant
low‐income
stages,
predominantly
their
where
degradation
is
common
consequence
However,
this
trend
stabilizes
high‐income
countries
with
adaption
conservation
laws
policies.
Together,
our
results
indicate
large‐scale
loss
can
be
avoided
preserving
low‐
mid‐income
early
stages
development.