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Biomass estimation and carbon sequestration potential of gymnosperms in the unique ecological milieu of Kalash valley Chitral, Pakistan

Author: Asad, Ullah
Publisher: Zenodo
DOI: 10.5281/zenodo.17317737
Source: https://zenodo.org/records/17317737/files/JBES-V26-No6-p26-33.pdf
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Biomass es ima ion and ca bon seques a ion po en ial o
gymnospe ms in he unique ecological milieu o Kalash alley
Chi al, Pakis an
Aziz U
Rahman, As
ad Ullah
*
, Sheeza Za a
Ins i u e o Plan Biodi e si y, Uni e si y o Peshawa , Pakis an
A icle published on June 04, 2025
Key wo ds:
Biomass es ima ion, Ca bon seques a ion po en ial,
Gymnospe ms, Ecological milieu,
Kalash alley,
Chi al, Pakis an
Abs ac
This s udy is o ho oughly in es iga e biomass and o gain comp ehensi e insigh s in o he ca bon
seques a ion dynamics o Gymnospe m ees in h ee sub- alleys wi hin he Kalash egion: Bumbu a e,
Rambu , and Bi i . The s udy honed in on coni e s dis ibu ed abo e an ele a ion o 1800 me e s abo e sea
le el. The species selec ed we e Ced us deoda a, Junipe us excelsa, Pinus ge a diana, and Pinus
wallichiana. Remo e sensing using NDVI indica es ha coni e s cons i u e an expanse o 11,251 hec a es
and 3.325% o he o al 1,048 squa e kilome es selec ed o his s udy. The o al biomass con ibu ion o
he ou Gymnospe m species in he a ea is eco ded a 30.22 onnes pe hec a e, seques e ing 136,171
onnes o ca bon and emi ing a ca bon dioxide equi alen o 499,297 onnes. The Shannon di e si y index
was de e mined o be 1.57, while Simpson's Di e si y Index (D) s ood a 0.78. The s udy ound no able
con ibu ion o Gymnospe ms in ca bon seques a ion and long e m sink o ca bon bo h AGB and BGB.
*
Co esponding Au ho : Asad Ullah  asa[email p o ec ed]u.pk
Jou nal o Biodi e si y and En i onmen al Sciences (JBES)
ISSN: 2220-6663 (P in ) 2222-3045 (Online)
Vol. 26, No. 6, p. 26-33, 2025
h p://www.innspub.ne
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In oduc ion
The concen a ion o CO
2
in he a mosphe e has
exponen ially isen o dange ous ange o 800 ppm
(By ne, 2023) i makes en i onmen al conce ns as a
mode n op mos issue. The pi o al ole played by
o es ege a ion in s o ing biomass and ca bon (C)
s ock and p ima y solu ion o mi iga e he impac s in
ising CO
2
Concen a ion (Haq, 2023). To coun e
his issue Fo es ecosys ems ha e he capabili y o
p o ide c ucial ca bon sinks con ibu ing o global
ca bon neu ali y (Xu e al., 2023). I is
unques ionable ha Fo es s play an impo an ole in
ca bon s o age, known as ca bon biomass. They se e
as massi e ca bon eposi o ies and and po en ial sink
o ca bon in he a mosphe e (Bae e al., 2004) by
seques e ing and emo ing ca bon om he
a mosphe e and s o es i as biomass in g een plan s
(Cha an and Rasal, 2012) and aluable and iable
solu ion o mi iga ing clima e change. They hold 92%
o all land-based biomass and s o e abou 400 billion
ons o ca bon (Pan, 2013). Ca bon Biomass is s o ed
in plan s and o he plan ma e ial (Os adhashemi,
2014). The IPCC classi ies biomass ca bon pools in o
AGB, BGB, li e , woody deb is, and soil o ganic
ma e (Nunoo e al., 2006). Assessing biomass and
ca bon budge s is essen ial o assessing p oduc i i y,
sus ainabili y, and ca bon seques a ion capaci y bu
assessmen s p ima ily ely on accu a e biomass
es ima ions (Salunkhe e al., 2023)
Biomass es ima ion is key o e alua e he s a us and
lux ca bon and dynamics o he ecosys em. Biomass
can be es ima ed in a ious ways like Des uc i e o
ha es ing me hod, emo e sensing me hod and non-
des uc i e allome ic equa ion. The equa ions
ailo ed o ind biomass o ees can p o ide mo e
accu a e es ima es o biomass pa icula ly i alida ed
wi h he help o emo e sensing (Na a , 2009). The
es ima ion o biomass and C s ock based on accu a e
local/ egional allome ic models is sui able me hod o
la ge-scale alling o o es ee (Salunkhe e al.,
2023) and be e ma hema ical app oach as
compa ed o des uc i e and manual me hods. As pe
he IPCC, e es ial ecosys ems encompass i e
ca bon pools ela ed o biomass: abo e-g ound
biomass, below-g ound biomass, li e , and woody
deb is, and soil o ganic ma e . AGB is he
p edominan componen o he ca bon pool, se ing
as he mos signi ican and conspicuous ese oi
wi hin he e es ial o es ecosys em (Haq e al.,
2023). Abo eg ound biomass (AGB) in pa icula
se es as a c ucial indica o o ecosys em s uc u e
and unc ionali y, playing a signi ican ole in he
es ima ion o o es ca bon s ocks (Fig. 1).
Fig.
1.
Land co e o Kalash
alley
2022 (Landsa
-
8
image)
Pakis an no dissimila om he wo ld, is acing an
imminen isk o inc eased de o es a ion and o es
deg ada ion by an h opogenic ac i i ies and
exace ba ed by he ad e se e ec s o clima e change
(Hussain and Fa ima, 2015). Luckily Pakis an has
signi ican po en ial o ca bon seques a ion, i.e.,
o es s, ang elands, and ag icul u al lands seques e
up o 225 million ons o CO
2
pe yea (Khila a ,
2022). Acco ding o FAO 2020, Biomass ese oi o
Pakis an is app oxima ely 213 million onnes o
ca bon including o al o es a ea o 4.2 million
hec a es (Mahmood, 2011) 4.57 million ha acco ding
o Bha i, 2011. Nume ous s udies in Pakis an, such as
Nizami e al. (2009) on sub opical pine o es s in
Mu ee hills, Shaheen e al. (2016) on sub opical
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Himalayan o es s (Gha oo , 2020; Nizami e al.,
2009; Shaheen e al., 2016; Khan e al., 2021;
Hamayoon Jalla ; Ami e al., 2018; Ali e al., 2020a;
Sheikh e al., 2012; Nizami, 2012; Ali and Anwa ,
2020; Ma in e al., 2013; A i e al., 2017; Akba e
al., 2023; Raqeeb, 2020) help us o unde s and
Ca bon seques a ion in Pakis an.
Ma e ials and me hods
S udy a ea
The a ea cen ed Fo Biomass s udy was Kalash
Valley was on h ee esea ch si es, i.e., Bumbu e ,
Rambu and Bi i , whe ein he in es iga ion del ed
in o he biomass and ca bon s ock speci ically
pe aining o Gymnospe ms, aiming o
unde s anding o Ca bon seques a ion o he A ea.
Ced us deoda a, Junipe us exelsa, Pinus
ge a diana and Pinus wallichiana we e
Gymnospe m ees o he a ea.
Chi al, a moun ain locked land, si ua ed be ween 35
0
15
/
o 36
0
55
/
No h la i udes and 71
0
11
/
o 73
0
51
/
Eas
longi udes. I co e s an a ea o 14,850 km² (DCR,
1998) (Ali and Qaise , 2009) while Lowe Chi al
(es ablished in 2018) is a dis ic in he Malakand
di ision co e ing 6,458 km² and loca ed be ween 35°
and 37° N la i udes and 71° and 22° o 74° E
longi udes (GoP). 40 km downs eam om Chi al
ci y lies Kalash Valley, posi ioned wi hin 35° 70
/
o
35°42
/
No h La i ude and 71°69
/
o 71°41
/
Eas
Longi ude. The ele a ion anges om 1900 o 2200
(DCR, 1998), (Open Loca ion Code 8J7 HPM6H). The
alley comp ises h ee sub- alleys and esea ch si e in
his s udy a e Bumbu e , Rumbo , and Bi i . They a e
bblessed wi h di e se lo a, o oak and coni e ous
o es s, ich biodi e si y and indigenous cul u e.
Kalash a e belie ed o be descended om Alexande
he G ea 's a my (Hadi and Ib a , 2015; Ullah e al.,
2014; Zeb, 2019). Rambu , posi ioned a a highe
ele a ion han Bumbu e , is enowned o i s eeding
glacie s and alpine meadows. Bumbu e , he la ges
alley among he Kalash alley is si ua ed a
coo dina es 35º 41' N and 71º 38' E. The a ea is
cha ac e ized by ugged opog aphy and s eep slopes.
Rambu is posi ioned be ween coo dina es 35º 46' N
and 71º 40' E, si ua ed o he no h o Bumbu e in
p oximi y o abou 8 kilome es. Bi i alley is loca ed
a he sou he nmos end o Chi al ci y. In con as o
he o he wo alleys, i has na owe wid h, a
coo dina es 35º 40' N and 71º 45' E and an ele a ion
o 1360 me e s (Zeb, 2019). Inhabi an s o he a ea
ely hugely on o es and o es y p oduc s o hei
li elihood. Acco ding o Aziz and Nadi a (2003),
app oxima ely 25 housand me ic ons o o es wood
is used as a sou ce o uel o 13% o he popula ion
(I um e al., 2014).
The alley expe iences ha sh and snowy win e s,
some ime as low as -20°C in ce ain a eas and
summe anging om 15 o 25°C. The monsoon
season con ibu ing signi ican ly o annual
p ecipi a ion om 1500 o 2500 mm pe yea (Ali,
2010). In Gymnospe ms Ced us deoda a, Junipe us
sp., Pinus ge a diana and Pinus wallichiana along
wi h Que cus spp. domina e he na u al o es o he
a ea (Hadi e al., 2014; She e al., 2003; FAO, 2010).
Sampling and ield campaign
Ci cula plo s, wi h a adius o 17.84 me e s
(equi alen o 0.1 hec a es), we e deployed wi hin he
expanse o gymnospe m o es o Kalash alley using
geog aphic coo dina es ob ained h ough andom
sampling as used by Ismail e al., 2017. The
e inemen o plo adius was achie ed by applying
slope co ec ion ac o s. Fo measu emen o
Diame e a B eas Heigh (DBH), ees wi h
diame e s exceeding 5 cen ime es and heigh
su passing 2 me e s we e eco ded wi hin he
con ines o each designa ed plo . Fo his pu pose
Diame e Tape (D-Tape) was used. Fo ee heigh
Haga Al ime e was used. Reading was penned down
along wi h Coo dina es eco ded by GPS. Fo es
image y was cap u ed using a digi al came a. Fo
be e compa ison Image o SAT 8 we e also aken.
Occu ence and dis ibu ion o ee species/ T ee
e enness and di e si y index
T ees and communi y we e iden i ied ollowed by
Vege a ion analysis i.e., T ee heigh , DBH, Basal A ea
(BA), Rela i e F equency (RF), Rela i e Densi y (RD),
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Rela i e Abundance (RA), Rela i e Co e , and
Impo ance Value Index (IVI) using he o mulae
used by Ismail e al., 2017. Reg ession model o
Heigh s and DBH we e calcula ed o each ee and
si es. T ee species di e si y index, i.e., Shannon
Di e si y Index (H') (Equa ion 1) and Simpson
Di e si y Index (Equa ion 2).
H=−(Pi×lnPi)

 Eq.1
Whe e H/ is Shanon Di e si y Index, Pi is F ac ion o
en i e popula ion made up o species i, and s is
numbe o species encoun e ed and ln is na u al
algo a hm.
D=∑(n/N)2 Eq. 2
Whe e D is Simpson Di e si y Index, n is o al
numbe o pa icula species and N is numbe o o al
ees. The alue o D anges om 0- 1. 0 means
in ini e di e si y and 1 means no di e si y.
T ee allome ic equa ions o biomass es ima ion
To es ima e he abo e-g ound ee biomass (AGTB),
T ee allome ic equa ions speci ic o he selec ed
species, de eloped by p e ious esea che s we e
employed. These equa ions a e, i.e., M= Ln (D
2
H)
n
Ced us deoda a = 0.0491(D
2
H)
0.9167
Eq. 3
Pinus oxbu ghii =0.0224(D
2
H
)0.9767
Eq. 4
Pinus ge a diana = 0.0253D
2.6077
Eq. 5
Junipe us exelsa = 0.1645 × (p × Dˆ2 × H)ˆ0.8586
Eq. 6 (Ali e al., 2015)
Whe e M is D y biomass o he ee in kilog am; D is
Diame e a B eas Heigh in cen ime e; H is To al
heigh o ee in m; Ln is Na u al Loga i hm and p is
wood densi y. Used by Ali (2020).
Below G ound Biomass, abo e g ound Ca bon, below
g ound ca bon andCO2 equi alen we e calcula ed
using exi ing li e a u e as ollowing.
BGB=AGB*R/S (BGB is below g ound Biomass R is
oo and S is shoo . R/ S= 0.27 Eq. 7 (Ali e al., 2017)
AGC=0.47*AGB (AGC is Abo e G ound Ca bon) Eq. 8
(Ali e al., 2020a)
BGC=0.26*AGB (BGC is below g ound ca bon) Eq. 9
(IPCC, 2008)
e Value=CS ock*44/12 (CO
2
equi alen ) Eq. 10
(Pea son e al., 2007)
Valida ion o coni e o es by h ough emo e
sensing and image y
To alida e ield s udies sa elli e image y o
gymnospe ms o Augus 2023 o Kalash Valley was
aken om om he Land-sa 8 Ope a ional Land
Image (OLI) on 08-12-2023. Bounda ies d awn
based on GPS USGS Ea h Explo e . Mul i empo al
sa elli e images 2023 we e downloaded om Uni ed
S a e o Geological Su ey websi e
h p://glo is.usgs.go /). Remo e sensing so wa e,
such as ENVI o QGIS, we e used o isualize he
sa elli e. The LULC classi ica ion is a clus e ing
algo i hm known as ISO Da a Analysis Techniques;
sel -o ganizing (ISO) A (ISODATA), which was used
o he pu pose as used by Khan e al., 2016. The
me hodology used by Tau ik 2016; Huang, 2021 and
Ha oyo, 2022. The da a was p io con i med by
Ques ionnai e me hod and hec ic ield su ey om
2021-2023 in a ious season.
Resul s
Gymnospe ms ees Ced us deoda a, Junipe us
excelsa, Pinus ge a diana, and Pinus wallichiana,
ocused in his s udy, we e obse ed o play a
subs an ial ole in ca bon seques a ion wi h
ecological con ibu ion encompassing 11,251 hec a es
ou o he o al 104,800 hec a es (Fig. 2). The
ele a ion o hese ees a e 1,830 - 2,745 masl, 2,700
masl, 2,000 - 3,500 masl and abo e 2, 900 masl
espec i ely. Que cus dila a and Qe cs baloo we e
ound o o e lap in lowe al i ude and domina e
below 1,800 masl in he a ea as s udied by (Khan e
al., 2010). Da a o FAO shows coni e o es sp ead in
he a ea o 11251 hac e s while emo e sensing shows
3.325% o 1048 km
2
o al a ea selec ed o his s udy.
O e all he a ea is ba en and ege a ion is chie ly
domina ed by Que cus dila a and Qe cus baloo .
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Fig. 2.
Ca bon s ocking by coni e ees
Fig. 3.
Reg essional model DBH o
heigh
o
C.
deoda a
Fig. 4.
Reg essional model
D
BH o heigh o
J. exelsa
Fig. 5.
Reg essional Model DBH o
heigh
o
P.
ge a diana
Ced us deoda a, o alling 126,845 onne in biomass
o he a eas and con ibu ing o a ca bon s ock o
59,617 onnes and seques e ing app oxima ely
218,596 onnes o equi alen ca bon dioxide (e-CO
2
).
I also s ands all wi h an a e age diame e a b eas
heigh (DBH) o 20.25 cm and heigh o 26.95 m, BA
o 2.45 m², RA a 28.63%, RF o 50% and RD o
29.57%, signi ying i s ecological p ominence.
Reg ession o DBH and heigh o Ced us deoda a
was 0.4561 (Fig. 3). While Junipe us excelsa
exhibi ed o al biomass 75,171 onnes and lowe in
p opo ion (Fig. 4). I p esen s a compa a i ely
smalle p o ile wi h a e age DBH o 19.64 cm and a
sho e a e age heigh o 11.22 and eg ession
ajec o y o R
2
equal o 0.0205 i showed BA o 2.29
m², RA o 21.89%, RF o 47.5%, and RD o 22.61%.
Pinus ge a diana, cha ac e ized by an a e age DBH
o 21.64 cm and an a e age heigh o 18.88 m and
linea eg ession o 0.4732, BA o 2.74 m², RA o
36.74%, RF o 54%, and RD o 37.93%, unde lining i s
ecological signi icance and dominance wi h an
a e age AGB o 88.99 kg pe ee, con ibu ed a o al
AGB o 37,982 onnes (Fig. 5).
Fig. 6.
Reg essional Model DBH o
heigh
o
P.
walli ana
Fig. 7.
No. o c
oni e s
in compa ison
The biomass pe hec a e o Pinus ge a diana was
3.38 onnes, con ibu ing o a ca bon s ock o 17,851
onnes and seques e ing app oxima ely 65,456 onnes
o e-CO
2
. Pinus wallichiana, al hough small in
numbe exhibi ed he highes a e age AGB, wi h
444.07 kg pe ee (Fig. 6). The biomass pe hec a e
o Pinus wallichiana was 5.84 onnes, con ibu ing
o a ca bon s ock o 30,884 onnes and seques e ing
a ound 113,242 onnes o e-CO
2
. The DBH was 26.61

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cm and o 30.94 m in a e age, and R
2
equal o 0.4561.
I has BA/Hac o 0.40 m² and highes among o he
coni e s (Fig. 7).
Fig. 8.
LULC Map o
coni e and non coni e
in
Kalash alley using NDVI 2023
Da a ob ained om Land-sa 8, de ailing land co e
and land use change (LCLUC) (Fig. 8) in he Kalash
Valley o alida e g ound s udies, p esen s an analysis
o he dis ibu ion o o he ege a ion ca ego ies,
e ealing a nuanced landscape composi ion.
Gymnospe ms, speci ically coni e s, al hough lowe in
composi ion in niche co e ing 3.23% o he Kalash
Valley bu o signi ican impo an mos ly domina ing
High ele a ion. Among o he ca ego ies, wa e bodies
accoun o 14.26% o he o al a ea, ba en land
comp ises a 22.5% o he landscape, a subs an ial
p esence o he baceous ege a ion in 24.86% o he
a ea. Sh ubs con ibu e o 22.02% o he a ea, a
di e se g oup o lowe ing plan s, occupying 13.1% o
he landscape.
Discussion
UN -FAO es ima e ha he wo ld has los one- hi d o
i s o es and 10 million hec a es o o es a e being
clea ed pe yea which is damaging na u al balance
i epa ably. Fo es s, in eg al in he clima e change
landscape, se e as long e m ca bon sinks (Ali e al.,
2023). To undo such ca as ophic loss scien i ic
e alua ion o cha coun e measu e is c ucial. As
hey a e la ges ese oi o Ca bon so necessi a e
accu a e biomass assessmen s o ack empo al
changes ca bon cycle. The es ima ion o o es
biomass in ol es g ound su eys o emo e sensing,
wi h ield su ey wi h des uc i e and non-des uc i e
sampling. The o me , as elucida ed by Gibbis (2007),
includes ha es ing all ees and measu ing a ious
pa s' biomass. On he o he hand Allome ic,
explained by Gha oo (2020), p o ides a
ma hema ical and s a is ical unde s anding in
ela ion o biomass.
Va ious esea che s in Pakis an ha e con ibu ed o
Biomass es ima ion o he coun y. Sa angzai e al., 2012
s udied aboiu Junipe in Balochis an and e ealed 278
ees wi h an es ima ed a e age ca bon con en o 1.96
ons pe hec a e. Ami e al. (2018) e ealed abou he
abo eg ound biomass o Pinus oxbu ghii and ound
weak co ela ions be ween ee cha ac e is ics and
biomass. Ali e al. (2020) epo ed a ia ions in ee
dimensions, while Sheikh e al. (2012) p o ided
es ima es o diame e a b eas heigh (DBH), heigh ,
and s and densi y. Ali and Anwa 's (2020) esea ch in
Khybe Pakh unkhwa highligh ed di e se soil ca bon
densi ies ac oss di e en o es ypes. Ma in e al.
(2013) ound he subs an ial ole o opical o es s in he
e es ial ca bon balance. A i e al. (2017) conduc ed
a ho ough assessmen o ca bon seques a ion in he
Chichawa ni I iga ed Plan a ion in Pakis an. Akba
e al. (2023) epo ed on he o es s uc u e in
Ska du, while Ali e al. (2023) de eloped an
allome ic equa ion o Ced us deoda a in no he n
a eas. Raqeeb (2020) conduc ed a comp ehensi e
o es in en o y in Gilgi Bal is an, es ima ing abo e-
g ound biomass. Simila ly, a s udy in Malakand,
Khybe Pakh unkhwa, p o ided es ima es o
abo eg ound and belowg ound ca bon, as well as he
o al ee ca bon s ock. Ahmad e al. (2014)
conduc ed a s udy on biomass and ca bon s ocks in
coni e ous o es s o Di Kohis an, KPK. They
epo ed an a e age biomass o 264.53 Mg ha
-1
ac oss
all o es s ands, wi h mean ca bon s ocks we e
J. Bio. &
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32 | Rahman e al.
140.37 Mg ha
-1
o deoda o es , 134.60 Mg ha
-1
o
deoda kail o es , 142.40 Mg ha
-1
o mixed
coni e ous o es , and 111.68 Mg ha
-1
o mixed i -
sp uce o es .
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