Phylodynamic
models
can
be
used
to
estimate
diversification
trajectories
from
time-calibrated
phylogenies.
Here
we
apply
two
such
phylogenies
of
non-avian
dinosaurs,
a
clade
whose
evolutionary
history
has
been
widely
debated.
Although
some
authors
have
suggested
that
the
experienced
decline
in
diversity,
potentially
starting
millions
years
before
end-Cretaceous
mass
extinction,
others
group
remained
highly
diverse
right
up
until
Cretaceous-Paleogene
(K-Pg)
boundary.
Our
results
show
model
assumptions,
likely
with
respect
incomplete
sampling,
large
impact
on
whether
dinosaurs
appear
long-term
or
not.
The
are
also
sensitive
topology
and
branch
lengths
phylogeny
used.
Developing
comprehensive
sampling
bias,
building
larger
more
accurate
phylogenies,
necessary
steps
for
us
determine
dinosaur
diversity
was
not
extinction.
Cambridge Prisms Extinction,
Journal Year:
2024,
Volume and Issue:
2
Published: Jan. 1, 2024
Abstract
Phylodynamic
models
can
be
used
to
estimate
diversification
trajectories
from
time-calibrated
phylogenies.
Here
we
apply
two
such
phylogenies
of
non-avian
dinosaurs,
a
clade
whose
evolutionary
history
has
been
widely
debated.
Although
some
authors
have
suggested
that
the
experienced
decline
in
diversity,
potentially
starting
millions
years
before
end-Cretaceous
mass
extinction,
others
group
remained
highly
diverse
right
up
until
Cretaceous-Paleogene
(K-Pg)
boundary.
Our
results
show
model
assumptions,
likely
with
respect
incomplete
sampling,
large
impact
on
whether
dinosaurs
appear
long-term
or
not.
The
are
also
sensitive
topology
and
branch
lengths
phylogeny
used.
Developing
comprehensive
sampling
bias,
building
larger
more
accurate
phylogenies,
necessary
steps
for
us
determine
dinosaur
diversity
was
not
extinction.
Earth-Science Reviews,
Journal Year:
2022,
Volume and Issue:
234, P. 104196 - 104196
Published: Sept. 28, 2022
The
Early
Jurassic
Jenkyns
Event
(∼183
Ma)
was
characterized
in
terrestrial
environments
by
global
warming,
perturbation
of
the
carbon
cycle,
enhanced
weathering
and
wildfires.
Heating
acid
rain
on
land
caused
a
loss
forests
affected
diversity
composition
plant
assemblages
rest
trophic
web.
We
suggest
that
Event,
triggered
activity
Karoo-Ferrar
Large
Igneous
Province,
pivotal
remodelling
ecosystems,
including
plants
dinosaurs.
Macroplant
palynological
data
show
reductions
richness
conifers,
cycadophytes,
ginkgophytes,
bennetitaleans,
ferns,
continuation
seasonally
dry
warm
conditions.
Major
changes
occurred
to
sauropodomorph
dinosaurs,
with
extinction
diverse
basal
families
formerly
called
‘prosauropods’
as
well
some
sauropods,
diversification
derived
Eusauropoda
Toarcian
South
America,
Africa,
Asia,
wider
new
families,
Mamenchisauridae,
Cetiosauridae
Neosauropoda
(Dicraeosauridae
Macronaria)
Middle
Jurassic,
showing
massive
increase
size
feeding
modes.
Ornithischian
dinosaurs
patchy
records;
heterodontosaurids
scelidosaurids
disappeared,
major
clades
(Stegosauridae,
Ankylosauridae,
Nodosauridae)
emerged
soon
after
Bajocian
Bathonian
worldwide.
Among
theropod
Coelophysidae
Dilophosauridae
died
out
during
theropods
(Megalosauroidea,
Allosauroidea,
Tyrannosauroidea)
this
event
substantial
increases
size.
then
crisis
marked
especially
floral
origins
clades,
increasing
body
Comparison
end
Triassic
Mass
Extinction
helps
understand
incidence
climatic
driven
large
igneous
provinces
ecosystems
their
great
impacts
early
dinosaur
evolution.
Current Biology,
Journal Year:
2022,
Volume and Issue:
33(1), P. 206 - 214.e4
Published: Dec. 16, 2022
The
ascendancy
of
dinosaurs
to
become
dominant
components
terrestrial
ecosystems
was
a
pivotal
event
in
the
history
life,
yet
drivers
their
early
evolution
and
biodiversity
are
poorly
understood.1Brusatte
S.L.
Benton
M.J.
Ruta
M.
Lloyd
G.T.
first
50
Myr
dinosaur
evolution:
macroevolutionary
pattern
morphological
disparity.Biol.
Lett.
2008;
4:
733-736https://doi.org/10.1098/rsbl.2008.0441Crossref
PubMed
Scopus
(105)
Google
Scholar,2Irmis
R.B.
Evaluating
hypotheses
for
diversification
dinosaurs.Earth
Environ.
Sci.
Trans.
R.
Soc.
Edinb.
2010;
101:
397-426https://doi.org/10.1017/S1755691011020068Crossref
(94)
Scholar,3Benton
Forth
J.
Langer
M.C.
Models
rise
dinosaurs.Curr.
Biol.
2014;
24:
R87-R95https://doi.org/10.1016/j.cub.2013.11.063Abstract
Full
Text
PDF
(93)
Scholar
During
Late
Triassic,
were
initially
rare
geographically
restricted,
only
attaining
wider
distributions
greater
abundance
following
end-Triassic
mass
extinction
event.4Brusatte
Superiority,
competition,
opportunism
evolutionary
radiation
dinosaurs.Science.
321:
1485-1488https://doi.org/10.1126/science.1161833Crossref
(334)
Scholar,5Langer
Ezcurra
M.D.
Bittencourt
J.S.
Novas
F.E.
origin
dinosaurs.Biol.
Rev.
Camb.
Philos.
85:
55-110https://doi.org/10.1111/j.1469-185X.2009.00094.xCrossref
(212)
Scholar,6Langer
Godoy
P.L.
So
volcanoes
created
dinosaurs?
quantitative
characterization
pan-aves.Front.
Earth
2022;
10https://doi.org/10.3389/feart.2022.899562Crossref
(3)
This
is
consistent
with
an
opportunistic
expansion
model,
initiated
by
co-occurring
groups
such
as
aetosaurs,
rauisuchians,
therapsids.4Brusatte
Scholar,7Tucker
M.E.
Triassic
environments,
climates
reptile
evolution.Palaeogeogr.
Palaeoclimatol.
Palaeoecol.
1982;
40:
361-379https://doi.org/10.1016/0031-0182(82)90034-7Crossref
(89)
Scholar,8Benton
Dinosaur
success
triassic:
noncompetitive
ecological
model.Q.
1983;
58:
29-55Crossref
(170)
However,
this
could
instead
be
response
changes
global
climatic
through
Jurassic
transition,
especially
given
increasing
evidence
that
climate
played
key
role
constraining
distributions.7Tucker
Scholar,9Whiteside
J.H.
Lindström
S.
Irmis
Glasspool
I.J.
Schaller
M.F.
Dunlavey
Nesbitt
S.J.
Smith
N.D.
Turner
A.H.
Extreme
ecosystem
instability
suppressed
tropical
dominance
30
million
years.Proc.
Natl.
Acad.
USA.
2015;
112:
7909-7913https://doi.org/10.1073/pnas.1505252112Crossref
(61)
Scholar,10Bernardi
Gianolla
P.
Petti
F.M.
Mietto
linked
Carnian
pluvial
episode.Nat.
Commun.
2018;
9:
1499https://doi.org/10.1038/s41467-018-03996-1Crossref
(87)
Scholar,11Lovelace
D.M.
Hartman
S.A.
Mathewson
P.D.
Linzmeier
B.J.
Porter
W.P.
Modeling
Dragons:
using
mechanistic
physiological
microclimate
models
explore
environmental,
physiological,
constraints
on
dinosaurs.PLoS
One.
2020;
15e0223872https://doi.org/10.1371/journal.pone.0223872Crossref
(8)
Scholar,12Mancuso
A.C.
Benavente
C.A.
Mundil
Evidence
episode
Gondwana:
new
multiproxy
records
bearing
diversification.Gondwana
Res.
86:
104-125https://doi.org/10.1016/j.gr.2020.05.009Crossref
(35)
Scholar,13Mancuso
Pedernera
T.E.
Gaetano
L.C.
Breeden
III
B.T.
Paleoenvironmental
biotic
late
triassic
Argentina:
testing
abiotic
forcing
at
basin
scale.Front.
10https://doi.org/10.3389/feart.2022.883788Crossref
(4)
Scholar,14Kent
D.V.
Clemmensen
L.B.
Northward
dispersal
from
Gondwana
Greenland
mid-Norian
(215–212
Ma,
Triassic)
dip
atmospheric
pCO2.Proc.
2021;
118e2020778118https://doi.org/10.1073/pnas.2020778118Crossref
(16)
Scholar,15Griffin
C.T.
Wynd
B.M.
Munyikwa
D.
Broderick
T.J.
Zondo
Tolan
Taruvinga
H.R.
Africa's
oldest
reveal
suppression
distribution.Nature.
609:
313-319https://doi.org/10.1038/s41586-022-05133-xCrossref
Scholar,16Olsen
Sha
Fang
Y.
Chang
C.
Whiteside
Kinney
Sues
H.-D.
Kent
Vajda
V.
Arctic
ice
dinosaurs.Sci.
Adv.
8eabo6342https://doi.org/10.1126/sciadv.abo6342Crossref
(5)
Here,
we
test
hypothesis
elucidate
how
influenced
distribution
quantitatively
examining
tetrapod
"climatic
niche
space"
across
Triassic-Jurassic
boundary.
Statistical
analyses
show
sauropodomorph
occupied
more
restricted
space
than
other
tetrapods
dinosaurs,
being
excluded
hottest,
low-latitude
zones.
A
subsequent,
earliest
geographic
preferred
conditions.
Evolutionary
model-fitting
provide
important
shift
cooler
warmer
niches
during
Sauropoda.
These
results
facilitated
change
support
dinosaurs.
Nature,
Journal Year:
2024,
Volume and Issue:
unknown
Published: Nov. 27, 2024
Abstract
The
early
radiation
of
dinosaurs
remains
a
complex
and
poorly
understood
evolutionary
event
1–4
.
Here
we
use
hundreds
fossils
with
direct
evidence
feeding
to
compare
trophic
dynamics
across
five
vertebrate
assemblages
that
record
this
in
the
Triassic–Jurassic
succession
Polish
Basin
(central
Europe).
Bromalites,
fossil
digestive
products,
increase
size
diversity
interval,
indicating
emergence
larger
dinosaur
faunas
new
patterns.
Well-preserved
food
residues
bromalite-taxon
associations
enable
broad
inferences
interactions.
Our
results,
integrated
climate
plant
data,
indicate
stepwise
ecospace
occupancy
area.
This
involved
(1)
replacement
non-dinosaur
guild
members
by
opportunistic
omnivorous
precursors,
followed
(2)
insect
fish-eating
theropods
small
dinosaurs.
Climate
change
latest
Triassic
5–7
resulted
substantial
vegetation
changes
paved
way
for
((3)
(4))
an
expansion
herbivore
pseudosuchian
therapsid
herbivores
large
sauropodomorphs
ornithischians
ingested
broader
range,
even
including
burnt
plants.
Finally,
(5)
rapidly
evolved
developed
enormous
sizes
response
appearance
guild.
We
suggest
processes
shown
data
may
explain
global
patterns,
shedding
light
on
environmentally
governed
dominance
gigantism
endured
until
end-Cretaceous
mass
extinction.
Biology Letters,
Journal Year:
2024,
Volume and Issue:
20(12)
Published: Dec. 1, 2024
Much
of
our
view
on
Mesozoic
dinosaur
diversity
is
obscured
by
biases
in
the
fossil
record.
In
particular,
spatiotemporal
sampling
heterogeneity
affects
identification
timing
and
geographical
location
radiations,
recognition
latitudinal
gradient,
as
well
interpretation
purported
extinctions,
faunal
turnovers
their
drivers,
including
Early
Jurassic
Jenkyns
Event
across
Jurassic/Cretaceous
boundary.
The
current
distribution
means
it
impossible
to
robustly
determine
whether
these
'events'
were
globally
synchronous
geologically
instantaneous
or
spatiotemporally
staggered.
Accounting
for
also
paramount
reconciling
notable
differences
results
based
sampling-standardized
species
richness
versus
reconstructions
diversification
rates,
particularly
with
regards
lead-up
Cretaceous/Paleogene
mass
extinction.
Incorporation
a
greater
proportion
stratigraphically
well-resolved
dinosaurs
into
analyses
imperative
must
include
substantial
radiation
birds.
Given
relative
rarity
temporally
successive,
well-sampled
spatial
windows,
remains
possible
that
rate
showed
little
change
after
clade's
initial
until
However,
better
understanding
underlying
sampling,
combined
holistic
approach
reconstructing
diversification,
an
important
step
testing
this
hypothesis.
Phylodynamic
models
can
be
used
to
estimate
diversification
trajectories
from
time-calibrated
phylogenies.
Here
we
apply
two
such
phylogenies
of
non-avian
dinosaurs,
a
clade
whose
evolutionary
history
has
been
widely
debated.
Although
some
authors
have
suggested
that
the
experienced
decline
in
diversity,
potentially
starting
millions
years
before
end-Cretaceous
mass
extinction,
others
group
remained
highly
diverse
right
up
until
Cretaceous-Paleogene
(K-Pg)
boundary.
Our
results
show
model
assumptions,
likely
with
respect
incomplete
sampling,
large
impact
on
whether
dinosaurs
appear
long-term
or
not.
The
are
also
sensitive
topology
and
branch
lengths
phylogeny
used.
Developing
comprehensive
sampling
bias,
building
larger
more
accurate
phylogenies,
necessary
steps
for
us
determine
dinosaur
diversity
was
not
extinction.
Phylodynamic
models
can
be
used
to
estimate
diversification
trajectories
from
time-calibrated
phylogenies.
Here
we
apply
two
such
phylogenies
of
non-avian
dinosaurs,
a
clade
whose
evolutionary
history
has
been
widely
debated.
Although
some
authors
have
suggested
that
the
experienced
decline
in
diversity,
potentially
starting
millions
years
before
end-Cretaceous
mass
extinction,
others
group
remained
highly
diverse
right
up
until
Cretaceous-Paleogene
(K-Pg)
boundary.
Our
results
show
model
assumptions,
likely
with
respect
incomplete
sampling,
large
impact
on
whether
dinosaurs
appear
long-term
or
not.
The
are
also
sensitive
topology
and
branch
lengths
phylogeny
used.
Developing
comprehensive
sampling
bias,
building
larger
more
accurate
phylogenies,
necessary
steps
for
us
determine
dinosaur
diversity
was
not
extinction.
Phylodynamic
models
can
be
used
to
estimate
diversification
trajectories
from
time-calibrated
phylogenies.
Here
we
apply
two
such
phylogenies
of
non-avian
dinosaurs,
a
clade
whose
evolutionary
history
has
been
widely
debated.
Although
some
authors
have
suggested
that
the
experienced
decline
in
diversity,
potentially
starting
millions
years
before
end-Cretaceous
mass
extinction,
others
group
remained
highly
diverse
right
up
until
Cretaceous-Paleogene
(K-Pg)
boundary.
Our
results
show
model
assumptions,
likely
with
respect
incomplete
sampling,
large
impact
on
whether
dinosaurs
appear
long-term
or
not.
The
are
also
sensitive
topology
and
branch
lengths
phylogeny
used.
Developing
comprehensive
sampling
bias,
building
larger
more
accurate
phylogenies,
necessary
steps
for
us
determine
dinosaur
diversity
was
not
extinction.
Phylodynamic
models
can
be
used
to
estimate
diversification
trajectories
from
time-calibrated
phylogenies.
Here
we
apply
two
such
phylogenies
of
non-avian
dinosaurs,
a
clade
whose
evolutionary
history
has
been
widely
debated.
Although
some
authors
have
suggested
that
the
experienced
decline
in
diversity,
potentially
starting
millions
years
before
end-Cretaceous
mass
extinction,
others
group
remained
highly
diverse
right
up
until
Cretaceous-Paleogene
(K-Pg)
boundary.
Our
results
show
model
assumptions,
likely
with
respect
incomplete
sampling,
large
impact
on
whether
dinosaurs
appear
long-term
or
not.
The
are
also
sensitive
topology
and
branch
lengths
phylogeny
used.
Developing
comprehensive
sampling
bias,
building
larger
more
accurate
phylogenies,
necessary
steps
for
us
determine
dinosaur
diversity
was
not
extinction.