BIOACCUMULATION AND CHROMIUM UPTAKE IN MANGROVE ECOSYSTEM OF SUNGAI SEPANG KECIL, SELANGOR, MALAYSIA
* School of Environmental Science and Natural Resources, Faculty of Science and Technology, Universiti Kebangsaan Malaysia. 43600 Bangi, Selangor, Malaysia. < mushrifah@yahoo.com>
** Universidade estadual de Santa Cruz, Departamento de Cijncias Biolsgicas, km16 rod. Ilhius Itabuna, Bahia Brazil CEP 45650000. paom@jacaranda.uescba.com.br
***Laboratoire de Biophysics, Faculte de Medicine, Universite Val de Marne, Creteil, France. francoise.escaig@wanadoo.fr
Chromium accumulation was studied in sediments and two mangrove species Avicenia officinalis and Rhizophora mucrotata of mangal ecosytem. The percentage of sediment with particle size < 63um increased from the river mouth upstream from 20 to 90 % respectively. The concentration of chromium increases as the percentage of particle size <63um increased. A. officinalis is a better chromium accumulant showing high concentration in roots, branches and leaves. As compared to R mucronata, low accumulation was shown in branches, leaves and roots. Initial studies using secondary ion mass spectrophotometry (SIMS) seems to show that chromium is deposited within the spongy mesophylls of the leaves. In the stem chromium was deposited within the vascular cells.
INTRODUCTION
Mangrove forest or mangal forms about 3.1% of the forest in Malaysia ( Leong,1992). Mangal is rich in biodiversity providing niche for both the flora and fauna. With growing agricultural and industrial activities, production of waste such as heavy metals has a significant effect on the environment. Effluent from treated sewerage, which is rich in chromium, can end its journey in rivers. Its existance by absorption, complexation and formation to organic and non-organic, can disturb the stability of mangal ecosystem.
This study intends to quantify the fate of chromium in the mangal ecosystem. Preliminary studies using two mangrove species were used to identify the site of chromium accummulation. It was carried out using a secondary ion mass spectrometry (SIMS). Other researches have used SIMS to study the biological systems under physiological and pathological conditions. Current data on the river ecosystem is insufficient to provide further information on biodiversity management plans for the river. Therefore, a study on heavy metals contamination in the river ecosystem is vital.
Study
area
Sungai Sepang Kecil is a
river situated in the state of Selangor, on the western coast of Malaysia. Only
the first half of the 10km long river, from the estuary is still mangal. The
rest has succumbed to agriculture, agrobase industries, human settlement and
plantation. The mangal provides the river with high nutrient, which was once a
nursery for oyster and mussel aquaculture cottage industry by the locals to
supply their local seafood restuarant in the area. Reports from the Division of Environment, Malaysia ( Jabatan Alam
Sekitar, 1995) showed that degradation in the water quality is mainly due to
waste from the domestic sewage, development such as the conversion of land to
make way for new airports and industries. Such activity too is putting a strain
to the river and the mangal ecosystem.
About 10 sampling sites were
chosen beginning from the river mouth upstream up to where the mangal ends.
Both sediment and mangrove were collected and later analysed in the laboratory.
Sediments were analysed by
sequential extraction as in Badri and Aston (1983). It has been shown that most
of the heavy metals were found in sediment with particle size <63um. Two
prominant mangrove species Rhizophora
mucronata and Avicenia officinalis
were identified at the10 sampling sites along the river. No mangal was observed after the 10th sampling
site. Sampling of the breathing roots, branches and mature leaves were carried
out within a period of one year. These samples were used for chromium analysis
and the detection of intracellular chromium. Chromium analysis was carried out
using atomic absorption and wet digestion
analysis.
Similar samples that were used for chromium analysis were fixed and dehydrated. Thin sections of 2um thick were cut and a first generation ion microprobe, SMI 300 Cameca with direct image was used in determination of chromium localisation as carried out by Casting and Slodzian (1962), Galle and Berry (1986).
|
Sampling site |
Particle size <63um |
Concentration of Cr, ug/g dry wt. |
|
1 |
19.6± 1.6 |
8.01± 3.0 |
|
2 |
57.6 ±2.3 |
8.3 ±2.9 |
|
3 |
86.5 ±1.2 |
10.1± 3.7 |
|
4 |
70.6 ±2.4 |
11.7± 4.2 |
|
5 |
84.2 ±0.8 |
10.4±3.7 |
|
6 |
88.6 ±0.4 |
9.9 ±3.6 |
|
7 |
89.4 ±0.7 |
14.1± 5.2 |
|
8 |
82.7 ±1.4 |
11.6± 3.9 |
|
9 |
74.9 ±2.2 |
12.6± 4.3 |
|
10 |
91.9± 0.3 |
13.0± 5.1 |
mangal are mainly silt/clay
and loam ( particle size 3um). Harbison (1986) has reported similar work. There
is a positive linear relationship (r=0.705), indicating that with increase in %
of particle size <63um, the concentration of chromium increased. Such
particles provide the bioavailability to sediment-bound metals.
Figs 1 and 2 showed the
accumulation of chromium by both the mangrove species. A. officinalis seems to accumulate chromium highest in roots (
range 5.3± 0.2 - 8.4± 0.7 ug/g dry wt), followed
by branches ( range 0.8± 0.4 - 2.6± 0.1 ug/g dry wt) and leaves
(range 0.5 0.1 -2.6± 0.3 ug/g dry wt
). The accumulation of chromium in R.
mucronata is highest in branches (range 0.03± 0.04 - 0.7 ±0.3 ug/g dry wt ) while in
leaves ( 0.3± 0 - 0.4± 0.1 ug/g dry wt ) and in
roots (ranged from undetectable levels - 0.1± 0.01 ug/g dry wt). Boring
et al (1981), has reported that metal accumulation also occurred in perennial
tissues. The low chromium uptake in plant showed that there was a low
availability of chromium from sediments.

The SIMS images provide a map of the distribution of Ca, Na which are the essential nutrients

for plants. Chromium signals were made in
comparison to both the Ca and Na images as a bright signal. Chromium was
detected within the phloem cells of the branch of A officinalis ( Fig. 3). In the leaves of the same species, only a
small amount of Cr was was detected within the spongy mesophyll cells ( Fig.
4). Generally translocation of Cr from the roots to the leaves are slow. Roots
act as the intermediate before Cr was transported to the xylem and the phloem
to the leaves.
Organic matter,
iron minerals and other reducing agents in sediment are know to reduce chromium
VI to chromium III under acidic conditions. This condition persists in mangal
ecosystem. Chromium accumulation in Rhizophora
and Avicenia could suggest that
mangal could be the reservoir for metal in the long term.
Chromium deposition in R. mucronata has been described elswhere
( Proc. in Symposium Biology in the Next Millenium. Kuala Lumpur, 1-3 December
1999- in press).
![]()
Fig. 3 Ion microscope images of A. officinalis showing the vascular cells in stem. A. 23Na
image B. 40 Ca image
C. 52Cr image. Xylem (X), Phloem (Ph),
Chromium (Cr). Magnification x700
![]()

A B C
Fig. 4 Ion microscope images of A. officinalis showing the cells in leaves. A. 23Na image
B. 40Ca image
C. 52Cr image.
Spongy mesophyll cells (SM), Interstitial spaces (IS),
Chromium (Cr). Magnification x700
![]()


A B C
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This project is made possible from the following funds. UNESCO Biotechnology fellowship, IRPA 08-02-02-0006 and Laboratoire de Biophysics, Faculte de Medicine, Univ. Paris Val de Marne, Creteil, France.