Use of Halimeda sp. as Liquid Organic Fertilizer Enriched with Trichoderma viride Strain TV-15 Isolated from Soil
A.B. Susanto1, Wilis Ari
Setyati1*, Juwita Lesly Senduk2, Dewi Basthika Makrima2
and Dony Bayu Putra Pamungkas2
1Department of Marine Science, Faculty of Fisheries and
Marine Science, Diponegoro University. Jl. Prof. Sudarto No. 13, Central Java,
Indonesia
2Department of Biology, Faculty
of Biology, Jenderal Soedirman University. Jl. dr. Suparno 63 Grendeng,
Purwokerto 53122, Central Java, Indonesia
*For correspondence: wilisarisetyati@yahoo.co.id
Received 29 November 2022;
Accepted 09 January 2023; Published 27 January 2023
Abstract
Halimeda
sp.
is a seaweed that is are underutilized despite being abundant in tropical areas
such as Indonesia. Seaweed has the potential to be liquid organic fertilizer
due to it containing essential nutrients, as well as plant growth substances,
including auxins, cytokinins, gibberellins, which stimulate growth and increase
crop production. On the other hand, Trichoderma sp. is a fungus that
acts as a bio-activator, decomposer of organic matter, and controller of plant
pests and diseases. The two factors combined are expected to complement each
other as raw materials for liquid organic fertilizer, which improve soil
structure and aid plant growth. This research was aimed at to determine the
composition and content of seaweed-based organic fertilizers, some of which are
enhanced with Trichoderma sp. isolated from soil. In this study Halimeda sp. was sampled from water, Trichoderma
sp. was isolated from soil followed by morphology testing both macroscopically
and microscopically and molecular testing of Trichoderma sp., and
lastly, formulating liquid organic fertilizer (LOF) and its analysis. Trichoderma
sp. was identified as T. viride strain TV-15. This species combined
with Halimeda sp. LOF showed that both control and Halimeda sp.
based LOF yielded a good level of organic carbon, iron and copper. These findings
revealed that Halimeda sp. and Trichoderma sp. showed great
potential as liquid organic fertilizers. © 2023 Friends Science Publishers
Keywords: Fertilizer; Growth; Seaweed; Soil; Trichoderma sp.; Plant growth substances
Introduction
As a maritime
country, Indonesia has an extensive marine region with high potential and
numerous biological resources such as seaweed. For example, Halimeda sp.
is a seaweed with high economic value that has the potential to be developed
further (Nazarudin et al. 2022).
Furthermore, Halimeda sp. thrives in protected environments such as bays
and grows in shallow water (Vogel et al.
2015; Ghosh et al. 2017). The thallus of Halimeda
sp. resembles tiny sheets with a rough surface, rigid, greenish-white, and
shaped like a branching kidney. Extracellular aragonite deposits were
discovered in its thallus, with the majority of them containing CaCO3,
MgCO3 and SrCO3. However, Halimeda sp. is one of
the underutilized seaweed species found in Indonesia. Seaweed has the potential
to be used as organic fertilizer due to containing Fe, B, Ca, Cu, Cl, K, Mg and
Mn, as well as plant growth substances such as auxins, cytokinins,
gibberellins, which stimulate growth and improve crop yield (Zaman et al. 2015; Taberna
et al. 2022). Study to utilize Gracilaria sp. and Sargassum
sp. as liquid organic fertilizers (LOF) revealed that the liquid organic fertilizer derived
from Gracilaria sp. and Sargassum sp. yielded 1.15% organic
carbon (OC), 0.67 nitrogen, 0.45% phosphorus, and 0.48% potassium, with a pH
level of 4.48 (Nasmia et al. 2021).
Organic fertilizers are classified as liquid or solid,
depending on their form. Primary ingredients of organic fertilizer are derived
from natural elements such as animal manure, animal body parts, and plants,
which are high in minerals and have beneficial effects on soil fertility. LOF
is a solution-based fertilizer that contains one or more soluble elements required
for plant life (Phibunwatthanawong and Riddech 2019). LOFs are an alternative
for plants to meet their macro- and micronutrient needs without producing
pollutants (Ortiz 2020; Shaji et al. 2021). In addition, these
fertilizers can deliver nutrients more quickly, allowing nutrient deficiencies
to be corrected, thereby resulting in faster nutrient absorption (Ji et al. 2017). Thus, LOF is beneficial as
it does not damage soil structure and can be used immediately without taking a
long time to be absorbed by plants (Soeparjono 2016).
Trichoderma spp. are a group of rhizorferous
fungi that live in the soil and act as organic matter decomposers, as well as
plant pests and disease controllers (Tyśkiewicz et al. 2022). They
are prevalent practically in all types of soils and ecosystems (Thapa et al.
2020). This fungus reproduces rapidly in plant roots. Many nutrients in the
soil are soluble in small amounts or even insoluble, limiting nutrient cycling
in the soil. Trichoderma has the ability to secrete organic acids that break
down minerals and release nutrients into the rhizosphere (Abirami et al.
2022). Moreover, Trichoderma can degrade nitrogen molecules into simple
nitrogen compounds such as NO2. The presence of this fungus may
allow the use of nitrogen-based fertilizers to be reduced.
Seaweed fertilizers are non-toxic and naturally decompose,
especially making them environmentally benign (Prasedya et al. 2022). Several studies on seaweed fertilizer have been conducted
(Soeparjono 2016; Ji et al. 2017).
However, minimum levels of macro- and micronutrients from the liquid fertilizer
have yet to be met because the levels are still relatively lower. Furthermore,
the addition of EM4 as a bio-activator in seaweed fermentation is known to be
unsatisfactory since various macro- and micro-elements in liquid fertilizer
made from seaweed do not match the standards required by the Indonesian
Ministry of Agriculture. Mold is known for being a significant producer of
enzymes, which are expected to breakdown seaweed cell walls and release minerals
for incorporation into liquid fertilizers (Baroud et al. 2021; Ammar et al.
2022). In addition,
the bio-activator produced by Trichoderma sp. can accelerate the
fermentation process and produce LOF (Raden et al. 2017).
Previous research has never utilized Halimeda sp.
as a raw material for liquid organic fertilizer. The goal of this study was to
create several liquid organic fertilizer formulations based on Halimeda sp.
with Trichoderma sp. enrichment, with a control and three formulations.
The preparation of LOF was achieved through experiments with various
formulations, followed by testing based on numerous parameters to identify
their contents. LOF from Halimeda sp. enriched with Trichoderma sp.,
being environment-friendly, is expected to promote plant growth and resistance.
Materials and Methods
Study area and species sampling
This study was carried out at Diponegoro University's Faculty of
Agriculture and Animal Husbandry in Semarang, Indonesia. Halimeda sp., was collected in August 2022 from Jepara, Central
Java, Indonesia (Fig. 1–2). Dry and aerated
samples of Halimeda sp. were pulverized in a blender and sifted into
flour. The fungal species Trichoderma
viride strain TV-15 was isolated from the soil collected
from tree root area at a depth of 10 cm. Soil sample (1 g) was weighed and
transferred to a test tube with 10 mL of sterile distilled water and
homogenized with a vortex for a few seconds. Next, the soil suspension was
diluted up to 10-5 using the serial dilution method. A 0.1 mL of the
last dilution was inoculated on Potato Dextrose Agar (PDA) medium. For this, 39
g PDA medium was dissolved in distilled water in a glass beaker filled up to
the line of 1000 mL. Next, PDA medium solution was homogenized before heated to
boiled. The mixture was then poured into six Erlenmeyer flasks of 250 mL and
firmly closed using gauze. After that, the medium was sterilized in an
autoclave for 15 min at 121ºC and 1 atm. The scatter plate method was used to
inoculate the soil suspension with PDA that was put into a petri dish and
solidified. The isolates were then cultured for 3×24 at 30ºC. During
incubation, the observations were conducted every day at 1×24 h. Isolates
exhibiting Trichoderma sp. features, such as light green to dark green
colony color, hyphae reproduced quickly and evenly, and round-shaped colonies
were purified and sub-cultured on a new PDA medium. Next, Trichoderma sp.
fungus was purified and cultured on new PDA media, followed by incubation for
3×24 h at 30ºC. The pure colonies of Trichoderma sp. were obtained by
isolating from other fungi (Fig. 3).
Trichoderma sp. identification
Morphological
identification: Fungi were identified based on morphological characteristics and observed
macroscopically and microscopically. Identification of Trichoderma sp.
at the macroscopic level was done by determining colony color and growth rate.
Furthermore, its characteristic was observed by looking at colony shape,
margin, tip and color. Microscopic examination of was done by observing its
hyphae, spores, sporangium, conidia and conidiophores under a microscope at
10×100 magnification. The hyphae were identified microscopically using Pitt and Hocking (2012) fungi identification
key, as well as fungal identification guidebooks (Gadjar et al. 2000; Sastrahidayat and Rochjatun 2011).
Molecular
identification: Molecular testing was done by transferring
purified isolates (single colony) on slanted media in test tubes to the
Genetics Science Lab in Tangerang, Banten, Indonesia. The molecular analysis
began with fungal DNA isolation, amplification using an ITS1/4 universal
primer, sequencing, and data interpretation (Martin
and Rygiewicz 2005). Base sequences from sequencing findings were
blasted or data matched with the NCBI database (Alshammari
et al. 2021). Finally, the
relationship of discovered fungal species was determined using NCBI data taking
the highest similarity value, closest to 100% (Pearson
2013).
Formation of
liquid organic fertilizer Halimeda sp. and T. viride
LOF by Halimeda sp. enriched with T. viride strain TV-15
were made using the following formulation:
H0 = Halimeda sp. + Aquades + Sugar + EM 4 (Control)
H1 = Halimeda sp. + Aquades + Sugar + EM 4 + H2SO4
H2 = Halimeda sp. + Aquades + Sugar + EM 4 + T. viride strain
TV-15
H3 = Halimeda sp. + Aquades + Sugar + EM 4 + H 2SO4
+ T. viride strain TV-15.
Fig. 1: Location of Awur Bay, Jepara,
Indonesia; sampling location for seaweed Halimeda sp; (6º36’17”S, 110º40’16”E)
Fig. 2: Halimeda sp. seaweed
samples
Fig. 3: Trichoderma sp. isolated
from soil samples
Halimeda sp. flour
was placed in a composter drum at a concentration of 250 g, and 0.2 M of H2SO4
1000 mL was added to hydrolyze the seaweed for 2 h before adding 25 mL of
sugar, 500 mL of distilled water and 2.5 mL of EM4 to speed up the
decomposition process. Next, the concoction was mixed until the mixture was
equally distributed. The mixture was enriched with one cup of T. viride strain
TV-15. Finally, the composter was completely sealed and left for 14 days (Tsaniya et al. 2021).
Analysis of
liquid organic fertilizer using Halimeda sp. and T. viride
The LOF samples made
by Halimeda sp. enriched with T. viride strain TV-15 were then tested
at BBTPPI Laboratory (Central Center for Industrial Pollution Prevention
Technology) Semarang, Central Java, to determine its concentration and
composition. Several parameters of Halimeda sp. and T. viride strain TV-15 based LOF were tested,
namely levels of OC (Walkey-Black method), pH levels (SNI 6989.11:2019), nitrogen (N) (SNI 2803: 2012
point 6.2), phosphorus (P) (SNI 2803.: 2012 point 6.3), potassium (K) as K2O (SNI 2803: 2012 point 6.4.2), ferric (Fe) (AOAC 19th,
980.01, 2021, Ch.2, p.35), manganese (Mn) (AOAC 19th, 972.03, 2012, Ch.2, p.39)
and copper (Cu) (AOAC 19th,
975.01, 2012, Ch.2, p.34). In addition, the populations of Escherichia coli (SNI ISO
7251: 2012), Salmonella sp. (SNI ISO 6579.: 2015) were also determined. The values of the
above parameters in various treatments were compared with minimum
technical requirements for LOF notified (No. 261/KPTS/SR.310/M/4/2019) by the Indonesian Ministry of Agriculture.
Results
Identification
of T. viride
Macroscopic observations revealed that isolates recovered from soil
samples had a dark green color, while hyphae were thick with a slightly
yellowish dark green, light green, and white tint. The isolates exhibited T. viride
features from this observation (Fig. 4). Observation showed that colony isolates
had green hyphae, short phialides stalks, and round greenish conidia/spores
developing at the ends. Conidia were growing in light green clusters. In
addition, observations further revealed that the colonies had many conidiophore
branches with longer branches underneath, and phialides were distinctly
grouped, with 2-3 phialides in each group. This isolate had the morphological
characteristics of T. viride (Fig. 4). The molecular test using ITS 1/4 primer identified the species
as T. viride strain TV-15, with the identity of 97.57% (Fig. 5).
Analysis of LOF
Results of heavy metal testing on Halimeda
sp. flour are shown in Tables 1–2. The amount of As in Halimeda sp. was relatively higher
(4.970 mg/kg), closer to the Ministry of Agriculture's minimum technical
standard for organic fertilizer (5.0 mg/kg). Hg levels was 0.152 mg/kg, which
was lower than the highest quality limit for gum (0.2 mg/kg). Pb level was
0.020 mg/kg, much below the gum quality limit (5.0 mg/kg). Cd level as 0.005
mg/kg, which was also lower than the quality standard for gum (1 mg/kg). Cr was
0.074 mg/kg, but lower than the quality level for gum (40 mg/kg).
The analysis results showed that in treatments
H0, H1, H2, and H3 the OC content was higher as compared to Commercial Seaweed
Organic Fertilizer (CSOF) (Fig. 6). When compared with the minimum technical
requirements for organic fertilizers, biological fertilizers or soil
conditioners laid down by the Indonesian Ministry of Agriculture, LOF was still below the OC quality standard, namely
at least 10%, so that the OC content in all treatments and CSOF was classified
as very low and far from the quality standard of liquid organic fertilizer. The
pH data in several treatments H0, H1, H2 and H3 obtained the same results (pH
7), while CSOF had pH of 8 (Fig. 6). Based on the minimum technical
requirements of the Indonesian Ministry of Agriculture the pH values for all treatments for CSOF met
quality standards i.e., 4–9. The N content in several treatments H0, H1, H2,
and H3 showed lower results compared to CSOF, which was 0.78. Among the
treatments, H0 and H1 obtained the highest results of 0.041 compared to the
other treatments, namely H2 of 0.026, and H3 of 0.040. Based on the minimum
technical requirements for LOF by the Indonesian Ministry of Agriculture, the quality standard for N content was 2-6%.
Hence, all treatments and CSOF did not meet quality standards.
The results of the analysis of P content in
treatments H0, H1, H2, and H3 showed lower results compared to CSOF, which was
0.04 (Fig. 6). However, in the H2 treatment the highest value was obtained,
namely 0.008 compared to H0, H1, and H3. Based on the minimum technical requirements
for LOF, laid down by the Indonesian Ministry of Agriculture, the quality standard for P content is 2–6%. So
that all treatments and CSOF did not meet quality standards. The K (as K2O)
content in the treatments H0, H1, H2, and H3 showed lower results compared to
CSOF, which was 0.41 (Fig. 6). However, among the treatments H0 obtained the
highest value of 0.042 compared to H1, H2, and H3. Based on the minimum
technical requirements for LOF laid down by the Indonesian Ministry of
Agriculture, the quality standard for K
content is 2–6%. So all treatments and CSOF did not meet quality standards.
The analysis of Fe content in treatments H0,
H1, H2, and H3 showed higher results compared to CSOF. The treatment H3
obtained the highest value of 25.90 compared to H0, H1, and H2. Meanwhile, in
CSOF, the Fe was not detected. The quality standard for Fe laid down by the Indonesian Ministry of
Agriculture is 90-900 mg/kg. So all treatments
and CSOF did not meet quality standards (Fig. 6). The Mn content in treatments
H0, H1, H2 and H3 was higher as compared to CSOF. Among the treatments, H1
obtained the highest value of 22.4 compared to H0, H2, and H3, while in CSOF
the Mn content was 0.40. Based on the minimum technical requirements for LOF,
the quality standard for Mn content was 25-500 mg/kg. Hence, all treatments and
CSOF did not meet quality standards (Fig. 6). The Cu content in treatments H0,
H1, H2, and H3 were higher as compared to CSOF. In the treatment, H0 obtained
the highest value of 0.497 as compared to H1, H2, and H3. In CSOF, the Cu
content was 0.241. Based on the minimum technical requirements for LOF, the quality
standard for Mn is 25-500 mg/kg. So that all treatments and CSOF did not meet
quality standards for Mn (Fig. 6).
Fig. 4: Microscopical observations
of Trichoderma sp. at a magnification of 10x100
Fig. 5:
PCR Products (1 µL) Were assessed by electrophoresis with 0.8% TBE
agarose; M, 1 00 bp DNA ladder (loaded 2.5 µL)
Fig. 6: Analysis result of liquid organic fertilizer Halimeda sp. and T.
viride strain TV-15
Table 1: Results of heavy metal testing on Halimeda
sp. flour
Heavy wetal |
Halimeda sp. |
Quality standard |
Arsenic (As) |
4.970 mg/kg |
Max. 5.0 mg/kg |
Mercury (Hg) |
0.152 mg/kg |
Max. 0.2 mg/kg |
Timbal (Pb) |
< 0.020 mg/kg |
Max. 5.0 mg/kg |
Cadmium (Cd) |
< 0.005 mg/kg |
Max. 1.0 mg/kg |
Chromium (Cr) |
0.074 mg/kg |
Max. 40 mg/kg |
Standard deviation |
2.456 |
2.561 |
Table 2: Analysis result of liquid organic fertilizer Halimeda
sp. and T. viride strain TV-15
Parameters |
Unit |
H0 |
H1 |
H2 |
H3 |
CSOF |
OC |
- |
0.550 |
0.404 |
0.296 |
0.311 |
0.25 |
pH |
- |
7 |
7 |
7 |
7 |
8 |
N |
% |
0.041 |
0.041 |
0.026 |
0.040 |
0,78 |
P |
- |
0.004 |
0.002 |
0.008 |
0.003 |
0,04 |
K |
mg/kg |
0.042 |
0.029 |
0.029 |
0.028 |
0,41 |
Fe |
mg/kg |
19.76 |
16.53 |
14.83 |
25.90 |
Not detect |
Mn |
mg/kg |
10.58 |
22.4 |
3.501 |
5.524 |
0.40 |
Cu |
mg/kg |
0.497 |
0.246 |
0.270 |
0.241 |
0.10 |
E. coli |
APM/100 mL |
< 0.30 |
< 0.30 |
3.8 |
12 |
- |
Salmonella |
Colony/ |
Negative/25 mL |
Negative/25 mL |
Negative/25 mL |
Negative/25 mL |
- |
Note : H0 (control), H1 (Halimeda sp. + H2SO4), H2 (Halimeda sp. + T. viride strain TV-15), H3 (Halimeda sp. + H2SO4 + T. viride
strain TV-15), OC (organic
carbon), CSOF (Commercial Seaweed Organic
Fertilizer)
The E. coli population in treatments
(H0, H1, H2 and H3) was higher; namely H0 (< 0.30), H1 (< 0.30), H2
(3.8), H3 (12) as compared to CSOF, in which E. coli was not detected.
Based on the minimum technical requirements for LOF, the quality standard for E.
coli was <1 × 102 cfu/mL. Hence, all treatments and CSOF met
quality standards (Fig. 6). The analysis of Salmonella population in several treatments
H0, H1, H2, and H3 obtained negative results and CSOF was not detected (Fig.
6). Based on the minimum technical requirements for LOF, laid down by the Indonesian Ministry of
Agriculture, the quality standard for
Salmonella was <1 × 102 cfu/mL. that all treatments and CSOF met
quality standards.
Out of several treatments, results showed that the measured parameters
were not significantly different from each other. Based on a comparison of
criteria with commercial organic fertilizers derived from other seaweeds, LOF derived from Halimeda sp. produced better results in terms of OC content, as well as Fe and Cu.
Discussion
Fertilizers made from natural materials, such as Halimeda
sp., offered a significant possibility to mitigate the harmful impact of inorganic
fertilizer overuse (Nasmia et al. 2021).
Inorganic fertilizer use has resulted in groundwater pollution, soil
degradation, and changes in soil microbial communities (Lin et al.
2019). One method that can be used as sustainable organic fertilizers is to use
Halimeda sp. as a substitute for inorganic fertilizers (Muarif et al. 2022).
This is because the components utilized to make this LOF are produced from
organic materials, specifically Halimeda sp. In addition, Halimeda
sp. contains carbohydrate molecule that affects the amount of organic matter in
fertilizers. Organic matter is required to maintain soil fertility and pH
through increasing aggregation and structure. In addition, organic matter can
boost cation exchange capacity and water retention in the soil.
This study used the
enrichment of the fungus T. viride has an important role in the decomposition process which can produce
enzymes for biodegradation and become biocontrol agents. In this case the pH
becomes an important factor affecting the activity of this fungus. An
unsuitable pH can affect the synthesis of enzymes that are useful in the
hardening process. The pH mismatch can prevent microorganisms from growing
optimally and affect the calming results. In the research, fertilizer formulations
were made to produce a pH that was in accordance with existing quality
standards.
The OC content in
liquid organic fertilizer produced was higher than commercial liquid fertilizer
due to the addition of seaweed to the LOF produced. The addition of seaweed as
a basic ingredient of OC adds nutrients containing amino acids so that the OC
content in LOF will increase (Sundari et
al. 2014). The results of helping the bacteria in LOF show that the content
of bacteria such as E. coli and Salmonella is at a predetermined
standard, so that the combustion process occuring in the fertilizer is not
disturbed and later LOF is safe to use for plants because there are no
bacterial pathogens that can cause harm to humans (Sundari et al. 2014).
Among other, N, P
and K are indicators of limiting variables for tropical lowland forest plants
growing on relatively fertile soils. N is abundant in the atmosphere and
constantly circulates among plants, soil, water and air, requiring rapid plant
growth and development. P is used for root development, seed formation, and
disease resistance. and K promotes cell division in immature meristematic
tissues of plants (Taiz et al. 2015). Soil pH is a critical feature that
indicates the acidity and alkalinity of a soil solution, and it can forecast
the availability of plant nutrients, toxins, and the activity of many key
microorganisms (Pandey et al. 2020).
Mn is essential in
Krebs cycle. It stimulates the activity of various enzymes, including
oxidoreductase, hydrolase and lyase. Furthermore, isocitrate dehydrogenase,
malate dehydrogenase, glycocyaminase, and D-alanyl synthetase are also produced
from these processes. Mn is an essential component of water-splitting enzymes
linked to photosystem II. Fe is a necessary and beneficial element (Taiz et
al. 2015). In plants, Fe-containing protein is vital for cellular
respiration, intermediate metabolism, oxygen transport, DNA stability and
repair, and photosynthesis. Cu is a micronutrient required for growth and
development. Though potentially toxic, it is also essential for electron
transport chain respiration and photosynthesis, cell wall metabolism, ethylene
synthesis, molybdenum cofactor biogenesis, and oxidative stress resistance.
Furthermore, copper has antifungal qualities and has long been utilized in
agriculture.
The LOF formulated
here has various benefits for both plants and the environment. The benefits for
plants are due to the OC content, and Fe and Cu are in accordance with the
needs of plants for growth and development. For the environment, LOF are more
environmentally friendly due to organic in nature and are not likely to change
the order of ecosystems in the soil (Nasmia et
al. 2021). Among the raw materials used for LOF, some are wastes,
and can reduce the presence of waste so that the environment is cleaner,
healthier and more balanced (Fernández-Delgado et al. 2022). This LOF
uses raw materials that can be the best alternative in an effort to overcome
the limitations of inorganic fertilizers. This is expected to reduce the use of
chemical fertilizers, which may not be good for the environment and surrounding
organisms. The LOF also contains T. viride, can maintain soil fertility due to its role as a
decomposer, and thereby has a good impact on plants.
Conclusion
This study demonstrates that the use of Halimeda sp.
as a primary ingredient with the enrichment of T. viride as a liquid organic
fertilizer has promising agricultural applications. The OC content and the
minerals Fe and Cu make liquid organic fertilizer based on Halimeda sp.
advantageous compared to other commercial seaweed fertilizers. Based on several
studies, seaweed contains minerals and contains growth regulators which are
beneficial for plants and soil. This fertilizer when applied to plants, is expected
to positively impact plant growth and yield. Use of Halimeda sp. can be as a base material for LOF and should be
followed by additional research, due to its heavy metal content being below the
highest limit of the standard set by the Decree of the Minister of Agriculture
of the Republic of Indonesia No. 261/KPTS/SR.310/M/4/2019 on the minimum
technical requirements for LOF.
Acknowledgments
This research was funded by Riset Publikasi Internasional (RPI) funding
sources other than the State Budget for Diponegoro University for the 2022
fiscal year number 569-63/UN7.D2/PP/VII/2022.
Author Contributions
AB Susanto and Wilis Ari Setyati proposed the research plan, processed
the laboratory and field experiments and shared in writing the manuscript. Juwita
Lesly Senduk, Dewi Basthika Makrima, and Dony Bayu Putra Pamungkas contributed
field and laboratory assistants involved in this research.
Conflicts of Interest
The authors declare that they have no competing
interests.
Data Availability
All new research results were presented in this article.
Ethics Approval
Not applicable
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