Earth Surface Dynamics,
Год журнала:
2024,
Номер
12(5), С. 973 - 994
Опубликована: Сен. 6, 2024
Abstract.
Fluvial
drainage
patterns
in
orogenic
belts
reflect
interactions
among
tectonics,
climate,
and
lithology.
The
central
South
Tian
Shan
displays
a
complex
fluvial
pattern
that
shifts
from
longitudinal
(flowing
parallel
to
mountain
ranges)
the
west
transverse
across
east.
Whether
such
underlying
of
tectonic
deformation,
lithology,
or
influence
surface
processes
within
basin
is
often
unclear.
We
focus
here
on
large
Saryjaz
catchment
SE
Kyrgyzstan,
which
marks
transition
between
drainages.
analyse
topographic
metrics
including
slope,
river
steepness
(ksn),
integral
proxy
(χ)
along
profile,
we
map
spatial
distribution
characteristics
knickpoints
discern
possible
controls
observed
pattern.
discriminate
different
origin,
namely
tectonic,
lithologic,
glacial,
those
linked
transient
waves
incision.
find
series
tributaries
downstream
sharp
180°
bend
main
stem
river,
also
striking
increase
channel
steepness.
Both
observations
indicate
accelerated
incision
this
lower
reach
catchment.
Knickpoint
elevations
ksn
below
decrease
downstream,
whereas
χt
values
(χ
measured
tributary
junctions)
remain
near-constant
tributaries.
These
results,
together
with
comparison
other
rivers
vicinity
show
no
evidence
knickpoints,
suggest
driven
“top-down”
by
large-magnitude
capture
event
rather
than
“bottom-up”
uplift
base-level
fall.
estimate
an
erodibility
parameter
10Be-derived
catchment-average
denudation
rates
use
celerity
knickpoints.
started
retreating
at
similar
time
ca.
1.5
4.4
Myr
ago.
Considering
timing
constraints,
was
likely
overfill
Neogene
intermontane
basins,
potentially
affected
both
climate
factors.
Ecology and Evolution,
Год журнала:
2025,
Номер
15(4)
Опубликована: Апрель 1, 2025
ABSTRACT
Understanding
the
geographic
distributions
of
rare
species
can
be
crucial
for
conservation
management.
New
environmental
DNA
(eDNA)
technologies
offer
potential
to
efficiently
document
endangered
species,
but
date,
such
screening
has
focused
largely
on
vertebrate
taxa.
Here
we
use
freshwater
eDNA
assess
distribution
Maungatua
stonefly,
Zelandoperla
maungatuaensis
,
a
flightless
insect
previously
known
from
only
handful
streams
draining
4‐km
section
mountain
range
in
southern
Zealand.
We
analyzed
12
stream
localities
across
range.
Screening
with
commercial
COI
primers
failed
detect
focal
Z.
.
However,
newly
designed
species‐specific
detected
this
taxon
four
adjacent
east‐flowing
contain
and
two
which
it
had
not
been
detected.
Subsequent
manual
surveys
confirmed
presence
discovered
populations,
barcoding
revealing
that
they
together
represent
unknown,
genetically
divergent
subclade.
Our
results
illustrate
metabarcoding
help
delineate
ranges
taxa,
highlight
importance
primer
specificity
when
These
findings
also
have
considerable
implications
companies
offering
biodiversity
health
services
targeting
invertebrates.
Proceedings of the National Academy of Sciences,
Год журнала:
2025,
Номер
122(21)
Опубликована: Май 19, 2025
We
explore
how
and
when
Hells
Canyon,
North
America’s
deepest
river
gorge
(~2,400
m
deep),
formed,
addressing
these
fundamental
questions
first
posed
by
W.
Lindgren
[
The
Gold
Belt
of
the
Blue
Mountains
Oregon
(1901)].
Existing
hypotheses
about
canyon’s
formation
timing
incision
remain
speculative
due
to
a
lack
direct
constraints
geomorphic
analysis
in
canyon.
Herein,
we
combine
cosmogenic
nuclide
dating
cave-bound
deposits,
profile
analysis,
numerical
modeling
provide
age
systematic
processes
at
work
Canyon.
Our
study
reveals
significant
drainage
capture
triggered
rapid
~2.1
±
1.0
Ma,
establishing
Snake
River’s
modern
route
into
Columbia
River
system.
increased
area
subsequent
increase
stream
power
resulted
Canyon
tributary
knickpoints
(KPs)
that
decrease
elevation
away
from
location.
Cosmogenic
cave
deposits
indicates
rates
~0.01
~0.16
mm
y
−1
.
Numerical
supports
observations,
demonstrating
abrupt
drives
incision.
findings
well-constrained
example
can
dramatically
shape
evolution
major
gorge.
Evolution
proceeds
unevenly
across
the
tree
of
life,
with
some
lineages
accumulating
diversity
more
rapidly
than
others.
Explaining
this
disparity
is
challenging
as
similar
evolutionary
triggers
often
do
not
result
in
analogous
shifts
tree,
and
may
reflect
different
triggers.
We
used
a
combination
approaches
to
directly
consider
such
context-dependency
untangle
complex
network
processes
that
shape
macroevolutionary
dynamics,
focusing
on
Pleurodonta,
diverse
radiation
lizards.
Our
framework
shows
lineage-wide
signatures
are
lost
when
conditioned
sub-lineages:
viviparity
appears
accelerate
diversification
but
its
effect
size
overestimated
by
association
Andean
mountains.
Conversely,
signals
erode
at
broader
phylogenetic
scales
emerge
shallower
ones.
Mountains
general
affect
speciation
rates;
rather,
occurrence
mountains
specifically
promotes
diversification.
Likewise,
evolution
larger
sizes
catalyzes
rates,
only
within
certain
ecological
geographical
settings.
caution
conventional
methods
fitting
models
entire
trees
mistakenly
assign
heterogeneity
specific
factors
despite
evidence
against
their
plausibility.
study
takes
significant
stride
toward
disentangling
confounding
identifying
plausible
sources
opportunities
large
radiations.
Evolution Letters,
Год журнала:
2024,
Номер
8(5), С. 623 - 637
Опубликована: Июнь 3, 2024
Evolution
proceeds
unevenly
across
the
tree
of
life,
with
some
lineages
accumulating
diversity
more
rapidly
than
others.
Explaining
this
disparity
is
challenging
as
similar
evolutionary
triggers
often
do
not
result
in
analogous
shifts
tree,
and
may
reflect
different
triggers.
We
used
a
combination
approaches
to
directly
consider
such
context-dependency
untangle
complex
network
processes
that
shape
macroevolutionary
dynamics,
focusing
on
Pleurodonta,
diverse
radiation
lizards.
Our
approach
shows
lineage-wide
signatures
are
lost
when
conditioned
sublineages:
while
viviparity
appears
accelerate
diversification,
its
effect
size
overestimated
by
association
Andean
mountains.
Conversely,
signals
erode
at
broader
phylogenetic
scales
emerge
shallower
ones.
Mountains,
general,
affect
speciation
rates;
rather,
occurrence
mountains
specifically
promotes
diversification.
Likewise,
evolution
larger
sizes
catalyzes
diversification
rates,
but
only
within
certain
ecological
geographical
settings.
caution
conventional
methods
fitting
models
entire
trees
mistakenly
assign
heterogeneity
specific
factors
despite
evidence
against
their
plausibility.
study
takes
significant
stride
toward
disentangling
confounding
identifying
plausible
sources
opportunities
large
radiations.
Systematic Biology,
Год журнала:
2023,
Номер
73(1), С. 26 - 35
Опубликована: Окт. 16, 2023
Abstract
The
origin
and
eventual
loss
of
biogeographic
barriers
can
create
alternating
periods
allopatry
secondary
contact,
facilitating
gene
flow
among
distinct
metapopulations
generating
reticulate
evolutionary
histories
that
are
not
adequately
described
by
a
bifurcating
tree.
One
such
example
may
exist
in
the
two-lined
salamander
(Eurycea
bislineata)
species
complex,
where
discordance
morphological
molecular
datasets
has
created
“vexing
taxonomic
challenge.”
Previous
phylogeographic
analyses
mitochondrial
DNA
(mtDNA)
suggested
reorganization
Miocene
paleodrainages
drove
vicariance
dispersal,
but
inherent
limitations
single-locus
dataset
precluded
evaluation
subsequent
flow.
Here,
we
generate
triple-enzyme
restriction
site-associated
sequencing
(3RAD)
data
for
>
100
individuals
representing
all
major
mtDNA
lineages
use
suite
complementary
methods
to
demonstrate
earlier
is
best
explained
history
influenced
river
drainage
reorganization.
Systematics
groups
should
acknowledge
these
complex
relationships
strictly
hierarchical.
[Amphibian;
hybridization;
introgression;
Plethodontidae;
stream
capture.]
Genes,
Год журнала:
2023,
Номер
14(12), С. 2146 - 2146
Опубликована: Ноя. 27, 2023
Understanding
historical
processes
underlying
lineage
distribution
patterns
is
a
primary
goal
of
phylogeography.
We
selected
Gobio
rivuloides
(Cypriniformes:
Gobionidae)
as
model
to
improve
our
knowledge
about
how
intraspecific
genetic
divergence
freshwater
fishes
arises
in
coastal
drainages
northern
China
via
statistical
analysis
using
cytochrome
b
gene.
The
time-calibrated
phylogeny
G.
showed
the
two
major
lineages
(I
and
II)
at
~0.98
Ma
(million
years
ago).
Lineage
I
can
be
divided
into
sub-lineages
(I-A
I-B)
with
time
~0.83
Ma.
Sub-lineage
I-A
inhabits
Amur
River,
sub-lineage
I-B
lives
Luan
River
Liao
River.
II
distributed
Yellow
Hai
close
relationships
between
drainages,
split
(II-C
II-D)
~0.60
Our
findings
indicate
that
splitting
could
attributed
geographic
isolation
caused
by
formation
Bohai
Sea,
river
capture,
episodic
hydrologic
closing
paleolake
during
late
Lower-Middle
Pleistocene.
It
also
first
report
we
know
displaying
clear
phylogeographic
break
for
across
China.
Abstract.
Fluvial
drainage
patterns
in
orogenic
belts
reflect
the
interaction
between
tectonics,
climate,
and
lithology.
The
central
South
Tian
Shan
displays
a
complex
fluvial
pattern
that
shifts
from
longitudinal
(flowing
parallel
to
mountain
ranges)
west
transverse
across
east.
Whether
such
underlying
of
tectonic
deformation,
lithology,
climatic
changes,
or
influence
surface
processes
within
basin
is
often
unclear.
We
focus
here
on
anomalously
large
Saryjaz
catchment
SE
Kyrgyzstan,
which
marks
transition
drainage.
analyse
topographic
metrics
including
slope,
river
steepness
(ksn)
integral
proxy
χ
along
profile,
map
spatial
distribution
characteristics
knickpoints
discern
possible
controls
observed
pattern.
discriminate
different
origin:
tectonic,
lithologic,
glacial,
those
linked
transient
waves
incision.
find
series
tributaries
downstream
sharp
180ᵒ
bend
main
stem
River,
also
striking
increase
channel
steepness.
Both
observations
indicate
accelerated
incision
this
lower
reach
catchment.
Knickpoint
elevations
decrease
downstream,
whereas
depth,
values
(measured
tributary
junctions)
ksn
ratios
are
constant
among
tributaries.
These
results
suggest
driven
“top-down”
by
large-magnitude
river-capture
event
rather
than
“bottom-up”
base-level
fall.
estimate
an
erodibility
parameter
10Be
derived
catchment-average
denudation
rates
use
celerity
knickpoints.
started
retreating
at
similar
time,
ca.
1.5
4.4
Myr
ago.
Considering
timing
constraints,
we
capture
was
likely
overfill
Neogene
intermontane
basins,
potentially
affected
both
climate
factors.
Abstract.
Fluvial
drainage
patterns
in
orogenic
belts
reflect
the
interaction
between
tectonics,
climate,
and
lithology.
The
central
South
Tian
Shan
displays
a
complex
fluvial
pattern
that
shifts
from
longitudinal
(flowing
parallel
to
mountain
ranges)
west
transverse
across
east.
Whether
such
underlying
of
tectonic
deformation,
lithology,
climatic
changes,
or
influence
surface
processes
within
basin
is
often
unclear.
We
focus
here
on
anomalously
large
Saryjaz
catchment
SE
Kyrgyzstan,
which
marks
transition
drainage.
analyse
topographic
metrics
including
slope,
river
steepness
(ksn)
integral
proxy
χ
along
profile,
map
spatial
distribution
characteristics
knickpoints
discern
possible
controls
observed
pattern.
discriminate
different
origin:
tectonic,
lithologic,
glacial,
those
linked
transient
waves
incision.
find
series
tributaries
downstream
sharp
180ᵒ
bend
main
stem
River,
also
striking
increase
channel
steepness.
Both
observations
indicate
accelerated
incision
this
lower
reach
catchment.
Knickpoint
elevations
decrease
downstream,
whereas
depth,
values
(measured
tributary
junctions)
ksn
ratios
are
constant
among
tributaries.
These
results
suggest
driven
“top-down”
by
large-magnitude
river-capture
event
rather
than
“bottom-up”
base-level
fall.
estimate
an
erodibility
parameter
10Be
derived
catchment-average
denudation
rates
use
celerity
knickpoints.
started
retreating
at
similar
time,
ca.
1.5
4.4
Myr
ago.
Considering
timing
constraints,
we
capture
was
likely
overfill
Neogene
intermontane
basins,
potentially
affected
both
climate
factors.
Abstract.
Fluvial
drainage
patterns
in
orogenic
belts
reflect
the
interaction
between
tectonics,
climate,
and
lithology.
The
central
South
Tian
Shan
displays
a
complex
fluvial
pattern
that
shifts
from
longitudinal
(flowing
parallel
to
mountain
ranges)
west
transverse
across
east.
Whether
such
underlying
of
tectonic
deformation,
lithology,
climatic
changes,
or
influence
surface
processes
within
basin
is
often
unclear.
We
focus
here
on
anomalously
large
Saryjaz
catchment
SE
Kyrgyzstan,
which
marks
transition
drainage.
analyse
topographic
metrics
including
slope,
river
steepness
(ksn)
integral
proxy
χ
along
profile,
map
spatial
distribution
characteristics
knickpoints
discern
possible
controls
observed
pattern.
discriminate
different
origin:
tectonic,
lithologic,
glacial,
those
linked
transient
waves
incision.
find
series
tributaries
downstream
sharp
180ᵒ
bend
main
stem
River,
also
striking
increase
channel
steepness.
Both
observations
indicate
accelerated
incision
this
lower
reach
catchment.
Knickpoint
elevations
decrease
downstream,
whereas
depth,
values
(measured
tributary
junctions)
ksn
ratios
are
constant
among
tributaries.
These
results
suggest
driven
“top-down”
by
large-magnitude
river-capture
event
rather
than
“bottom-up”
base-level
fall.
estimate
an
erodibility
parameter
10Be
derived
catchment-average
denudation
rates
use
celerity
knickpoints.
started
retreating
at
similar
time,
ca.
1.5
4.4
Myr
ago.
Considering
timing
constraints,
we
capture
was
likely
overfill
Neogene
intermontane
basins,
potentially
affected
both
climate
factors.