Deul
ajh
ari hot spring h
as diverse temper
ature
and pH r
ange v
arying from 43 °C to 65 °C
and 7.83 to 8.10 respectively. Dense foli
age
around Deul
ajh
ari hot spring contributes to the high tot
al org
anic c
arbon content (TOC). In our experiment we took sediment s
amples from the two Deul
ajh
ari hot springs (S1
and S2) out of the cluster h
aving temper
ature of 43 °C
and 55 °C
and pH of 7.83
and 7.14 respectively. Sediment s
amples were
an
alysed using 16S rRNA of V3‐V4 region by
amplicon met
agenome sequencing. Over 34 phyl
a were detected in cluster S1
and 32 phyl
a in cluster S2
at the existing physiochemic
al p
ar
ameters temper
ature 43 °C, pH 7.83, electroconductivity 0.019 dSm
− 1,
and tot
al org
anic c
arbon (TOC) 3.80% for S1
and temper
ature 55 °C, pH 7.14, electroconductivity 0.019 dSm
− 1,
and tot
al org
anic c
arbon (TOC) 0.97% for S2. Existence of
a v
ast number of unresolved sequences 179 out of 292 in S1
and 186 out of 314 in S2
at the genus level emph
asizes the signific
ance of our study. Met
agenome sequence inform
ation for the both clusters S1
and S2 of Deul
ajh
ari is
av
ail
able
at
NCBI, SRA d
at
ab
ase with
accession number SRX1459732
and SRX1459733 respectively.
Direct link to the deposited data:
an id="ir0005" class="interref" data-locatorType="url" data-locatorKey="http://www-ncbi-nlm-nih-gov.library.gcu.edu:2048/sra/SRX1459732">www.ncbi.nlm.nih.gov/sra/SRX1459732a>an>
an id="ir0010" class="interref" data-locatorType="url" data-locatorKey="http://www-ncbi-nlm-nih-gov.library.gcu.edu:2048/sra/SRX1459733">www.ncbi.nlm.nih.gov/sra/SRX1459733a>an>