 |
The
rata
trees
are
flowering
again,
now
that
possums
have
been
controlled
in
Pukaha
Mount
Bruce
|
The
Pukaha
Mount
Bruce
Forest
is
one
of
the
largest
and
most
accessible
remnants
of
the
"Seventy
Mile
Bush",
an
almost
unbroken
tract
of
forest
that
stretched
from
Opaki
to
Norsewood,
before
being
largely
cleared
and
the
land
converted
to
agriculture.
Generally,
the
forest
is
in
good
heart,
with
extensive
regeneration
of
emergent
and
canopy
trees
and
a
vigorous
and
diverse
shrub
and
ground
flora.
Animal
control
efforts
already
in
place
have
halted
any
extensive
damage
and
a
continuation
of
these
will
aid
the
regenerative
process.
It
is
one
of
New
Zealand's
great
"vanished
forests".
Early
accounts
of
the
forest
all
mention
the
size
of
the
trees
and
the
luxuriance
of
the
growth.
One
has
it
"so
dark
that
you
need
to
light
a
torch
during
the
day
to
see
the
way
ahead."
These,
along
with
the
abundance
of
birdlife
and
the
sheer
immensity
of
the
area
covered
are
common
and
recurring
themes.
In
"A
History
of
the
Birds
of
New
Zealand"
W.L.
Buller
gives
a
description
of
the
forest
as
seen
from
the
road,
and
though
he
mentions
kohekohe,
which
almost
certainly
was
not
present,
the
narrative
serves
as
a
good
description
of
the
type
of
forest
that
was
the
typical
cover
of
this
area.
Rimu
is
a
dominant
tree,
with
"just
a
sufficient
admixture
of
kahikatea
and
rata
to
set
off
the
peculiar
softness
of
the
former",
while
tree
ferns,
Cyathea
dealbata
and
C.
medullaris,
along
with
Dicksonia
fibrosa
(as
D.
antarctica)
are
always
present
and
the
ground
is
"covered
with
ferns
and
mosses
and
cryptogams
in
amazing
variety."
His
description
of
the
seasonal
changes
in
the
forest
is
by
no
means
confined
to
the
variation
in
birdlife.
Rather,
it
is
the
changes
in
the
plants
as
well
which
took
his
imagination,
from
the
spring
time
sight
of
the
Clematis
"hanging
in
garlands
round
the
trees,
festooned
in
clumps
among
the
lower
vegetation
on
the
roadside,
and
displaying
its
petals
of
snowy
white
in
great
profusion
"
and
later,
in
the
summer,
having
shed
its
flowers,
"bunches
of
silky
green
tassels,
containing
the
seed
vessels
of
this
plant
and
possessing
a
characteristic
beauty
of
their
own."
Kohia
(Passiflora
tetrandra)
is
mentioned
as
characteristic,
"hanging
from
almost
every
branch",
though,
as
yet,
it
has
only
recently
been
found
in
the
Pukaha
Mount
Bruce
forest.
Of
more
interest
is
the
mention
of
"a
bunch
of
Loranthus
ablaze
with
its
crimson
flowers
and
forming
a
picturesque
object
amidst
its
green
surroundings."
The
crimson
mistletoe,
now
Peraxilla
colensoi,
but
formerly
included
in
the
genus
Loranthus,
has
only
recently
been
rediscovered
in
the
Tararua
Range,
having
not
been
seen
for
a
number
of
years.
Its
inclusion
as
a
plant
of
the
70-mile
bush
provides
an
interesting
and
somewhat
enigmatic
addition
to
the
flora,
given
that
its
usual
hosts
are
beech
trees,
and
that
these
were
hardly
the
dominant
feature
of
this
forest,
though
they
were
present.
Other
early
accounts
of
the
70-mile
bush
are
as
much
concerned
with
its
felling
and
conversion
to
agricultural
land
as
they
are
with
its
composition,
but
all
are
united
by
reference
to
both
the
size
and
density
of
the
trees
and
the
abundance
of
the
birdlife.
A
northern
rata
(Metrosideros
robusta)
in
the
Mangatainoka
area
was
said
to
be
66
feet
(31
metres)
in
circumference.
By
contrast
large
measured
rata
currently
alive,
including
some
at
Mount
Bruce,
are
between
9
and
12
metres
in
circumference.
The
soil
fertility
and
"magnificent
stands
of
matai,
rimu,
tawa
and
maire"
are
everywhere
stressed.
Geology
Mount
Bruce
is
an
isolated
elongated
massif
tending
NNE
to
SSW.
The
forest
occupies
an
outlier
of
greywacke
emergent
through
beds
of
tertiary
mudstone.
The
soils
are
skeletal
and
rubbly
on
the
upper
slopes,
deeper
on
the
lower
slopes.
When
viewed
from
a
distance
the
high
point
(Bruce's
Hill)
and
the
associated
ridge
and
gully
system
stand
out
distinctly
from
the
nearby
Tararua
foothills
and
the
low
rounded
hills
of
the
northern
Wairarapa.
Little,
if
any,
geological
work
has
been
undertaken
on
Pukaha
Mount
Bruce
itself,
though
there
has
been
work
done
in
the
vicinity.
Rocks
and
geological
formations
in
the
wider
area
span
Jurassic
(190
-
135
MY)
to
Holocene
(10,000
yr.
before
present),
and
cover
a
range
of
rock
types
including
greywackes,
limestones,
sandstones
and
mudstones
(papa).
Limestone
occurs
on
both
sides
of
Pukaha
Mount
Bruce,
literally
over
the
road
to
the
west.
Limestone
is
also
common
to
the
north.
The
recent
geology
in
the
area
to
the
south
of
Pukaha
Mount
Bruce
is
strongly
influenced
by
the
Ruamahanga
River.
The
rock
type
on
Pukaha
Mount
Bruce
itself
is
described
as
a
part
of
the
Tararua
formation
of
the
Torlesse
supergroup.
This
rock
is
a
greywacke,
which
dates
from
the
Jurassic
age
and
was
deposited
when
New
Zealand
was
situated
near
Antarctica.
Most
of
the
forested
area
remaining
on
Pukaha
Mount
Bruce
grows
on
this
rock,
the
only
major
exception
being
a
small
area
near
Bruce
Stream
which
grows
on
the
recently
deposited
alluvium
associated
with
the
stream
itself.
Near
the
Ruamahanga
River
is
the
Mangaoranga
formation
which
accumulated
during
the
Miocene
(25
-
7
MY)
as
a
result
of
marine
transgression.
This
formation
contains
both
marine
and
terrestrial
fossils
dating
back
to
the
upper
Miocene.
The
transgression,
which
was
at
its
peak
in
the
early
Pliocene
(7
-
2
MY),
was
the
last
major
marine
transgression
to
occur
in
the
New
Zealand
region,
inundating
much
of
the
present
lowlands.
Fossils
found
in
the
Mangaorangan
formation
comprise
a
wide
range
of
plants
from
estuarine
species
and
those
of
warm
temperate
forests,
including
some
which
failed
to
survive
colder
times
during
more
recent
glacial
episodes,
to
an
assemblage
typical
of
cool
upland
vegetation.
Included
in
these
were
the
now
extinct
beeches
of
the
"brassi"
group.
The
relatively
poor
dispersal
ability
of
these
trees
and
their
inability
to
disperse
even
relatively
short
distances
over
salt
water
would
indicate
that
the
forest
from
which
they
were
derived
was
long
established
and
not
of
recent
origin,
as
would
be
expected
had
the
forest
colonised
a
landmass
recently
exposed
by
a
falling
sea
level.
Rocks
near
Mauriceville,
to
the
northeast
of
the
Mangaorangan
site,
also
contain
a
diverse
fossil
flora
derived
from
both
a
coastal
area
and
an
elevated
landmass.
Fossils
from
these
sites
date
from
a
time
long
before
the
Tararua
Ranges
began
their
recent
and
rapid
uplift
and
indicate
that
in
the
area
of
Mount
Bruce
there
existed
an
extensive
series
of
plant
associations,
covering
a
wide
altitudinal
band.
It
could
well
be
that
Pukaha
Mount
Bruce
is
not
only
one
of
the
remnants
of
the
70-mile
bush,
but
is
also
one
of
its
parents.
The
present
vegetation
and
forest
types
The
vegetation
on
Pukaha
Mount
Bruce
today
is
a
mosaic
influenced
by
a
number
of
disruptive
events,
while
still
retaining
at
least
some
of
the
character
and
trees
of
the
original
forest.
Fires
burned
unchecked
in
the
early
part
of
this
century,
and
trees
were
felled
for
firewood,
fencing
and
timber.
Farm
stock
and,
until
recently,
feral
goats
have
all
affected
the
composition
and
regeration
of
the
forest.
Forest
plants
represent
a
remarkably
homogenous
group
of
species
within
broad
forest
types,
and,
as
would
be
expected,
most
of
the
species
present
on
Pukaha
Mount
Bruce
are
also
found
in
nearby
remnants
and
in
the
Tararua
Ranges.
The
major
exceptions
appear
to
be
those
species
which
prefer
dry
conditions,
e.g.,
the
small
herb
Acaena
juvenca,
which
grows
nearby
in
forest
associated
with
the
Ruamahanga
River,
and
shrubs
such
as
the
matagouri
(Discaria
toumatou).
Also
absent
are
some
species
characteristic
of
lowland
forest,
such
as
the
liana
Fuchsia
perscandens.
Forest
typing
maps
show
9
broad
vegetation
types
for
the
Pukaha
Mount
Bruce
forest.
These
are:
-
F3
(rimu/kamahi)
F6
(rimu/kamahi)
I
16
(podocarp/red
beech/kamahi)
N2,
ND15
(logged
rata-rimu/tawa/kamahi)
PF3
(logged
rimu/tawa)
PF6
(logged
rimu/tawa)
RF
(regenerating
forest)
R2
(mahoe
shrubland,
shrub
hardwoods,
general
scrubland)
TI
16
(logged
podocarp/red
beech/kamahi)
Along
with
these,
there
is
another
comprised
of
red
beech
(Nothofagus
fusca)
over
a
well
lit
understorey
containing
Leucopogon
fasciculatus
and
Metrosideros
fulgens,
along
with
terrestrial
growth
of
normally
epiphytic
plants,
particularly
the
orchids
Earina
mucronata,
and
Earina
autumnalis,
along
with
the
kidney
fern
(Cardiomanes
reniforme).
This
type
has
so
far
been
seen
in
two
small
stands
on
the
tops
of
leading
ridges
rising
from
the
valley
to
the
east
of
the
National
Wildlife
Centre.
Weeds
Weeds
do
not
appear
to
have
major
footholds
in
the
Pukaha
Mount
Bruce
forest.
Some
plants
of
old
man's
beard
(Clematis
vitalba)
are
encountered
from
time
to
time
and
the
species
does
persist
in
a
clearing
in
the
valley
running
north
from
Bruce's
Hill.
Japanese
honeysuckle
(Lonicera
japonica)
is
present
in
low
numbers
near
the
western
entrance
to
the
Pukaha
Mount
Bruce
track.
Most
of
these
plants
have
been
hand
pulled
and
regeneration
from
fallen
vines
is
being
dealt
with
as
it
is
encountered
Apart
from
that,
most
weed
species
are
those
to
be
expected
on
and
near
a
disturbed
forest
margin.
Gorse
(Ulex
europaeus)
has
been
reported
from
the
vicinity
of
oneold
logging
track
and
though
Himalayan
honeysuckle
(Leycesteria
formosana)
is
prominent
along
some
tracksides,
it
is
only
the
continual
disturbance
involved
with
keeping
the
tracks
open
that
allows
it
to
persist.
A
shrubby
Cotoneaster
(C.
franchetii)
is
present
on
the
western
side,
near
the
logging
site.
Pasture
grasses
and
low
herbaceous
plants
will
all
be
displaced
by
the
gradual
return
of
their
favoured
open
sites
to
shrubs,
then
forest.
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