# Environmental and Ecological Risk Assessment of Trace Metal Contamination in Mangrove Ecosystems: A Case from Zhangjiangkou Mangrove National Nature Reserve, China

Authors: Jun Wang; Huihong Du; Ye Xu; Kai Chen; Junhua Liang; Hongwei Ke; Sha-Yen Cheng; Mengyang Liu; Hengxiang Deng; Tong He; Wenqing Wang; Minggang Cai
Journal: BioMed Research International
 (2016)

---

## Abstract

Zhangjiangkou Mangrove National Nature Reserve is a subtropical wetland ecosystem in southeast coast of China, which is of dense population and rapid development. The concentrations, sources, and pollution assessment of trace metals (Cu, Cd, Pb, Cr, Zn, As, and Hg) in surface sediment from 29 sites and the biota specimen were investigated for better ecological risk assessment and environmental management. The ranges of trace metals in mg/kg sediment were as follows: Cu (10.79–26.66), Cd (0.03–0.19), Pb (36.71–59.86), Cr (9.67–134.51), Zn (119.69–157.84), As (15.65–31.60), and Hg (0.00–0.08). The sequences of the bioaccumulation of studied metals are Zn > Cu > As > Cr > Pb > Cd > Hg with few exceptions. Cluster analysis and principal component analysis revealed that the trace metals in the studied area mainly derived from anthropogenic activities, such as industrial effluents, agricultural waste, and domestic sewage. Pollution load index and geoaccumulation index were calculated for trace metals in surface sediments, which indicated unpolluted status in general except Pb, Cr, and As.


---

## Body

## 1. Introduction

Differing from the land ecosystem and marine ecosystem in the structure and function, the mangrove wetland, periodically suffering seawater immersion, locates in the dynamic ocean and land interface of tropics and subtropics and plays an extremely important role in the global ecological balance [1, 2]. In recent years, since many mangrove ecosystems are close to urban development which is tied to industrialization and human activities, the important intertidal zone is subjected to contamination from a variety of human activities [3–5], because it is always located near the coast where the wind is weak and the water movement is slow and the pollutants can directly settle in the sediments [6]. Inherent physical and chemical properties of mangrove sediments confer an extraordinary capacity to accumulate materials or pollutants discharged to the nearshore marine environment [7, 8].Because of the toxicity, broad sources, biodegradable properties, and cumulative behavior, trace metals are of special environmental concern [9]. Trace metals with low solubility in water are easily adsorbed and accumulated in sediments [10]. Therefore, coastal sediments are always regarded as the ultimate sinks for trace metals [9]. On the other hand, some trace metal elements cannot be permanently fastened by sediments and will be released back to the overlying water, when the environmental condition changes (like salinity, resuspension, pH, redox potential, and the organic matter decay rate) [11, 12].Some trace metals such as copper, zinc, cobalt, and arsenic are essential elements of marine organisms in the environment, indispensable for body for normal physiological activity [13]. Nevertheless, trace metals are such as cadmium and mercury, which have no essential biological functions and are toxic even at low concentrations [14, 15]. The organism is exposed to these pollutants from the water or the particles and then accumulates them in the body [16–18]. Humans, as a final link in the food chain, are always mostly affected, and consequently the public has become the potential risk to human health when consuming such polluted biota [19]. Conversely, benthic organisms (like gastropod, fish, and crab) can be used to monitor the quality of aquatic ecosystems with broad geographical distribution, fixed lifestyle, easiness of capture, and the promotion of bioturbation [17, 18, 20, 21].Although several studies have focused on trace metal distribution in mangrove sediments and benthic organism worldwide [22–26], little is known about mangroves in the southeast China [27–29], where high levels of trace metals were observed in the biota according to the rather limited studies [30–32]. From 1980 to 2006, some researches have been conducted to investigate the content and distribution of trace metals in the surface sediments in Dongshan Bay and Zhangjiang River Estuary mangrove zone to examine the concentrations of some selected trace metals (Cr, Cu, Zn, As, Cd, Hg, and Pb) in the surface sediment [6, 33–35]. However, no reports are available in the Zhangjiangkou Mangrove National Nature Reserve (ZMNNR) relating metals in the sediments to bioaccumulation in edible biota [27–29]. With more industry developed nearby, such as nuclear power industry, chemical industry, and power plants, it is necessary to investigate and assess the environmental risk in Zhangjiang River catchment for environment management and sustainable development [5, 36].The objectives of this study were to measure the contents and distribution of some trace metals in surface sediments and benthic animals from ZMNNR. The goals of this research were1 to evaluate the concentration level and distribution of the trace metals in the sediment and biota in the ZMNNR; 2 to accurately quantify the extent of trace metal pollution using the geoaccumulation index I
g
e
o and pollution load index (PLI); and 3 to analyze possible sources of trace metals in sediment using the Pearson correlation analysis, cluster analysis (CA), and principal component analysis (PCA).


## 2. Materials and Methods

### 2.1. Study Area

Zhangjiangkou Mangrove National Nature Reserve, covering approximately an area of 23.60 km2, is the biggest mangrove zone to the north of the Tropic of Cancer, China. ZMNNR locates at the outlet of the Zhangjiang River (23°23′–23°56′ N, 117°24′–117°30′ E), which flows into the Dongshan Bay from the northwest, and is a traditional agriculture area, which irrigates vast stretches of farmland along its course. The catchment area and total length are 855 km2 and 58 km, respectively. Dongshan Bay locates on the west coast of the south of the Taiwan Strait, covering 247.89 km2 area, with a water surface of approximately 155.5 km2, and is the largest bay in southern Fujian. The bay is a semiclosed bay, inundated by the incoming tide twice a day, with the largest tidal difference during spring at 3.15 m. The current of the bay is a reciprocating semidiurnal tidal current. The bay is a place in which the East China Sea and South China Sea cross where the fish from East China Sea and South China Sea fish can be bred.The average temperature is between 13.5°C (in January) and 28.9°C (in August) in this area. The wind direction during the dry season is prevalent from north-west to south-east while it is the opposite during the rainy season. Annual fall of rain is about 1714.5 mm and the monsoon will bring heavy rainfall during rainy season from April to September.


### 2.2. Sampling

A lot of research elaborates the method for extraction, purification, and measurement of trace metals in sediment and biota samples elsewhere, including Cai et al. [6] and Shi et al. [43], to name but a few. And we give only a concise presentation here.29 surface sediment samples and the biota specimen were carried out from the study area in August 2013 (Figure1). In this study, the sampling region included the mangrove intertidal zone (C01–C17) and the subtidal zone (DS01–DS12). Surface sediments were collected with a grab sampler and were subsampled from the center of the collected material using plastic spatula. Once removed the samples were placed into precleaned Teflon containers and stored at −20°C before undergoing analysis in a laboratory.Figure 1
The study area and sampling stations.The benthic, mussel (Siliqua minima,SM), crab (Uca maracoani,UM), and fish (Boleophthalmus pectinirostris, BP) of biota specimens were also carried out from the study area in August 2013. The two kinds of biological samples were sampled by local fisherman from northwest Zhangjiang River. The fishes were bought from the local fisherman on the same day of capture and brought to the laboratory, where they were stored at −20°C until analysis. During analysis stage, we selected the samples (Siliqua minima, n
=
25;Uca maracoani, n
=
10) in the medium body length and preferable growth situation. The samples had been dissected to separate their shell and tissue, freeze-dried, and stored at −20°C.


### 2.3. Sample Analysis

The sediment samples for trace metals analysis were freeze-dried under −80°C for 36 hours and then ground to powder using an agate mortar and pestle and passed through a 180-mesh nylon sieve to remove large particles. The screened sample was collected in acid-rinsed glass vials and stored in desiccators. 0.1000 ± 0.005 g of sediment sample (dry weight) was put into acid-washed PTFE vessel and digested with the method of HNO3 + HClO4. Sample was diluted to 50 mL with Milli-Q water (National Standard of China, GB 17378.5-1998). Sample solutions were analyzed for Zn using flame atomic absorption spectrometry (FAAS, SOLAAR M6, Thermo Electron) and for Cr, Pb, Cu, and Cd using Graphite Furnace Atomic Absorption Spectrometer (GF-AAS, SOLLAAR M6, Thermo Electron) and for Hg and As using inductively coupled plasma mass spectrometry (ICP-MS) (DRC-II, Perkin Elmer, USA). 0.200
±
0.005 g of freeze-drying of benthic animals sample was put into acid-washed PTFE vessel and digested with the method of HNO3 + H2O2 (National Standard of China, GB 17378.6-2007). Sample solutions were analyzed for Cu, Cr, and Cd, using Graphite Furnace Atomic Absorption Spectrophotometer (GF-AAS).Granulometry was analyzed using a laser particle size analyzer (Mastersizer 2000, Malvern) and pH was performed by Vario pH meter (SMCH-2V00-001V, German).


### 2.4. Quality Assurance and Quality Control (QA/QC)

All reagents were of superior grade pure and ultrapure water throughout this study using a Milli-Q water purification system (Millipore, Bedford, MA, USA) with resistivity of 18.2 Megohm-cm. A method blank, limit of detection (LOD), and precision were run to correct the measurement. Lab ware prepared for sample was soaked in nitric acid (1 : 3) for at least 48 h and then rinsed with Milli-Q water. Detection limits were 1.80μg/L for Zn, 0.03 μg/L for Cr, 0.21 μg/L for Pb, 0.009 μg/L for Cd, 0.06 μg/L for Cu, 0.04 ng/g for As, and 0.05 ng/g for Hg. All samples were analyzed in duplicate. Sediment standard reference material (GBW07314; National Research Council of China) was digested in quadruplicate and analyzed to support the QA/QC of sediment measurements, which yielded satisfactory results, with recovery ranging from 85% to 115%. Biota standard reference material (DORM-4, National Research Council of Canada; GBW10024, National Research Council of China) was digested in quadruplicate and analyzed to support the QA/QC of biota measurements, which yielded satisfactory results, with recovery ranging from 81% to 112%.


### 2.5. Quantification of Sediment Pollution

#### 2.5.1. Pollution Load Index (PLI)

To assess the level of trace metal pollution, an integrated pollution load index of eight metals was calculated as suggested by Suresh et al. [44]. PLI > 1 means that pollution is present; otherwise, if it is below 1, there is no metal pollution(1)
PLI
=
CF
1
∗
CF
2
∗
CF
3
∗
⋯
∗
CF
n
1
/
n
.The contaminant factor (CF) was developed by Hakanson [45] and had been widely used in trace metals studies of sediments and soils [46].


#### 2.5.2. Geoaccumulation Index (I
geo)

The geoaccumulation indexI
g
e
o was introduced by Müller [47] to quantify trace metal pollution levels in the study area. The index can be calculated by the following expression:(2)
I
geo
=
log
2
⁡
C
n
1.5
B
n
,where C
n is the measured concentration of trace metal in the mangrove sediment and B
n is the geochemical background value in average shale. Because there is no background value of metal in the sediment from the study area, the geoaccumulation index was calculated using the values of the earth’s crust [48].


#### 2.5.3. Biota-Sediment Accumulation Factor

To estimate the proportion in which metal occurs in the organism and in associated sediment, biota-sediment accumulation factors (BSAFs) were calculated for selected metal in the molluscs studied by the following expression:(3)
BSAF
=
C
x
C
s
,where C
x is the mean concentrations of metals in the organism, C
s is the mean concentrations of metals in associated sediment [49, 50].


### 2.6. Statistical Analysis

Pearson correlation analysis, cluster analysis, and principal component analysis were conducted using SPSS® for Windows Release 21.0 (SPSS Inc., US). Pearson correlation analysis and cluster analysis were applied to examine the relationship among trace metals in the surface sediment. The general characteristics of the ZMNNR sediments were further analyzed using PCA methods to determine the degree of pollution by trace metals from natural (lithogenic) action and anthropogenic sources [51–53].


## 2.1. Study Area

Zhangjiangkou Mangrove National Nature Reserve, covering approximately an area of 23.60 km2, is the biggest mangrove zone to the north of the Tropic of Cancer, China. ZMNNR locates at the outlet of the Zhangjiang River (23°23′–23°56′ N, 117°24′–117°30′ E), which flows into the Dongshan Bay from the northwest, and is a traditional agriculture area, which irrigates vast stretches of farmland along its course. The catchment area and total length are 855 km2 and 58 km, respectively. Dongshan Bay locates on the west coast of the south of the Taiwan Strait, covering 247.89 km2 area, with a water surface of approximately 155.5 km2, and is the largest bay in southern Fujian. The bay is a semiclosed bay, inundated by the incoming tide twice a day, with the largest tidal difference during spring at 3.15 m. The current of the bay is a reciprocating semidiurnal tidal current. The bay is a place in which the East China Sea and South China Sea cross where the fish from East China Sea and South China Sea fish can be bred.The average temperature is between 13.5°C (in January) and 28.9°C (in August) in this area. The wind direction during the dry season is prevalent from north-west to south-east while it is the opposite during the rainy season. Annual fall of rain is about 1714.5 mm and the monsoon will bring heavy rainfall during rainy season from April to September.


## 2.2. Sampling

A lot of research elaborates the method for extraction, purification, and measurement of trace metals in sediment and biota samples elsewhere, including Cai et al. [6] and Shi et al. [43], to name but a few. And we give only a concise presentation here.29 surface sediment samples and the biota specimen were carried out from the study area in August 2013 (Figure1). In this study, the sampling region included the mangrove intertidal zone (C01–C17) and the subtidal zone (DS01–DS12). Surface sediments were collected with a grab sampler and were subsampled from the center of the collected material using plastic spatula. Once removed the samples were placed into precleaned Teflon containers and stored at −20°C before undergoing analysis in a laboratory.Figure 1
The study area and sampling stations.The benthic, mussel (Siliqua minima,SM), crab (Uca maracoani,UM), and fish (Boleophthalmus pectinirostris, BP) of biota specimens were also carried out from the study area in August 2013. The two kinds of biological samples were sampled by local fisherman from northwest Zhangjiang River. The fishes were bought from the local fisherman on the same day of capture and brought to the laboratory, where they were stored at −20°C until analysis. During analysis stage, we selected the samples (Siliqua minima, n
=
25;Uca maracoani, n
=
10) in the medium body length and preferable growth situation. The samples had been dissected to separate their shell and tissue, freeze-dried, and stored at −20°C.


## 2.3. Sample Analysis

The sediment samples for trace metals analysis were freeze-dried under −80°C for 36 hours and then ground to powder using an agate mortar and pestle and passed through a 180-mesh nylon sieve to remove large particles. The screened sample was collected in acid-rinsed glass vials and stored in desiccators. 0.1000 ± 0.005 g of sediment sample (dry weight) was put into acid-washed PTFE vessel and digested with the method of HNO3 + HClO4. Sample was diluted to 50 mL with Milli-Q water (National Standard of China, GB 17378.5-1998). Sample solutions were analyzed for Zn using flame atomic absorption spectrometry (FAAS, SOLAAR M6, Thermo Electron) and for Cr, Pb, Cu, and Cd using Graphite Furnace Atomic Absorption Spectrometer (GF-AAS, SOLLAAR M6, Thermo Electron) and for Hg and As using inductively coupled plasma mass spectrometry (ICP-MS) (DRC-II, Perkin Elmer, USA). 0.200
±
0.005 g of freeze-drying of benthic animals sample was put into acid-washed PTFE vessel and digested with the method of HNO3 + H2O2 (National Standard of China, GB 17378.6-2007). Sample solutions were analyzed for Cu, Cr, and Cd, using Graphite Furnace Atomic Absorption Spectrophotometer (GF-AAS).Granulometry was analyzed using a laser particle size analyzer (Mastersizer 2000, Malvern) and pH was performed by Vario pH meter (SMCH-2V00-001V, German).


## 2.4. Quality Assurance and Quality Control (QA/QC)

All reagents were of superior grade pure and ultrapure water throughout this study using a Milli-Q water purification system (Millipore, Bedford, MA, USA) with resistivity of 18.2 Megohm-cm. A method blank, limit of detection (LOD), and precision were run to correct the measurement. Lab ware prepared for sample was soaked in nitric acid (1 : 3) for at least 48 h and then rinsed with Milli-Q water. Detection limits were 1.80μg/L for Zn, 0.03 μg/L for Cr, 0.21 μg/L for Pb, 0.009 μg/L for Cd, 0.06 μg/L for Cu, 0.04 ng/g for As, and 0.05 ng/g for Hg. All samples were analyzed in duplicate. Sediment standard reference material (GBW07314; National Research Council of China) was digested in quadruplicate and analyzed to support the QA/QC of sediment measurements, which yielded satisfactory results, with recovery ranging from 85% to 115%. Biota standard reference material (DORM-4, National Research Council of Canada; GBW10024, National Research Council of China) was digested in quadruplicate and analyzed to support the QA/QC of biota measurements, which yielded satisfactory results, with recovery ranging from 81% to 112%.


## 2.5. Quantification of Sediment Pollution

### 2.5.1. Pollution Load Index (PLI)

To assess the level of trace metal pollution, an integrated pollution load index of eight metals was calculated as suggested by Suresh et al. [44]. PLI > 1 means that pollution is present; otherwise, if it is below 1, there is no metal pollution(1)
PLI
=
CF
1
∗
CF
2
∗
CF
3
∗
⋯
∗
CF
n
1
/
n
.The contaminant factor (CF) was developed by Hakanson [45] and had been widely used in trace metals studies of sediments and soils [46].


### 2.5.2. Geoaccumulation Index (I
geo)

The geoaccumulation indexI
g
e
o was introduced by Müller [47] to quantify trace metal pollution levels in the study area. The index can be calculated by the following expression:(2)
I
geo
=
log
2
⁡
C
n
1.5
B
n
,where C
n is the measured concentration of trace metal in the mangrove sediment and B
n is the geochemical background value in average shale. Because there is no background value of metal in the sediment from the study area, the geoaccumulation index was calculated using the values of the earth’s crust [48].


### 2.5.3. Biota-Sediment Accumulation Factor

To estimate the proportion in which metal occurs in the organism and in associated sediment, biota-sediment accumulation factors (BSAFs) were calculated for selected metal in the molluscs studied by the following expression:(3)
BSAF
=
C
x
C
s
,where C
x is the mean concentrations of metals in the organism, C
s is the mean concentrations of metals in associated sediment [49, 50].


## 2.5.1. Pollution Load Index (PLI)

To assess the level of trace metal pollution, an integrated pollution load index of eight metals was calculated as suggested by Suresh et al. [44]. PLI > 1 means that pollution is present; otherwise, if it is below 1, there is no metal pollution(1)
PLI
=
CF
1
∗
CF
2
∗
CF
3
∗
⋯
∗
CF
n
1
/
n
.The contaminant factor (CF) was developed by Hakanson [45] and had been widely used in trace metals studies of sediments and soils [46].


## 2.5.2. Geoaccumulation Index (I
geo)

The geoaccumulation indexI
g
e
o was introduced by Müller [47] to quantify trace metal pollution levels in the study area. The index can be calculated by the following expression:(2)
I
geo
=
log
2
⁡
C
n
1.5
B
n
,where C
n is the measured concentration of trace metal in the mangrove sediment and B
n is the geochemical background value in average shale. Because there is no background value of metal in the sediment from the study area, the geoaccumulation index was calculated using the values of the earth’s crust [48].


## 2.5.3. Biota-Sediment Accumulation Factor

To estimate the proportion in which metal occurs in the organism and in associated sediment, biota-sediment accumulation factors (BSAFs) were calculated for selected metal in the molluscs studied by the following expression:(3)
BSAF
=
C
x
C
s
,where C
x is the mean concentrations of metals in the organism, C
s is the mean concentrations of metals in associated sediment [49, 50].


## 2.6. Statistical Analysis

Pearson correlation analysis, cluster analysis, and principal component analysis were conducted using SPSS® for Windows Release 21.0 (SPSS Inc., US). Pearson correlation analysis and cluster analysis were applied to examine the relationship among trace metals in the surface sediment. The general characteristics of the ZMNNR sediments were further analyzed using PCA methods to determine the degree of pollution by trace metals from natural (lithogenic) action and anthropogenic sources [51–53].


## 3. Results

### 3.1. Trace Metals in the Surface Sediments

Major sediment characteristics are shown in Table1, which presents the granulometry, the content of water (CW), and pH in surface sediments from ZMNNR. The result indicated that the sediment mainly consists of silt and clay-type soil, which account for an average 29.77% and 58.18%, respectively. Sand contents were low (average is 11.84%) except in DS03 and DS07 (74.78% and 45.8%, resp.). Water content in sediments varied from 33.05% to 52.2%, with a mean of 42.92%, and pH ranged from 5.99 to 8.26, with a mean of 7.53.Table 1
Physicochemical parameters and trace metals concentrations (mg/kg) in surface sediments from ZMNNR.
Stat.
Clay (%)
Silt (%)
Sand (%)
pH
CW (%)
Trace metals (mg/kg)
Cu
Cd
Pb
Cr
Zn
As
Hg
C01
—
—
—
7.93
—
24.96
0.09
36.98
27.53
135.18
26.32
0.02
C02
31.48
63.30
5.22
7.86
44.28
22.78
0.08
42.32
134.51
157.84
24.03
0.02
C03
32.52
63.13
4.35
7.77
40.86
21.44
0.09
47.93
42.30
155.98
24.43
0.03
C04
31.14
66.18
2.68
6.98
40.17
23.13
0.05
42.49
45.03
145.79
24.89
0.01
C05
30.63
66.57
2.80
7.48
39.53
22.85
0.04
50.22
52.55
149.81
25.25
0.04
C06
28.54
67.57
3.89
7.69
42.79
19.68
0.05
36.80
22.07
120.55
22.99
0.00
C07
32.17
64.30
3.53
7.02
41.33
21.86
0.06
36.71
32.39
134.18
23.74
0.02
C08
31.92
65.27
2.81
7.97
39.21
22.43
0.05
41.32
39.13
139.20
28.17
0.02
C09
30.71
65.22
4.07
7.12
44.76
21.30
0.05
39.49
34.25
144.36
22.16
0.01
C10
31.66
63.02
5.32
7.08
41.07
24.54
0.06
48.11
27.73
141.06
23.24
0.01
C11
31.94
63.98
4.08
6.95
44.96
23.84
0.04
39.66
26.72
136.33
25.47
0.00
C12
32.04
63.23
4.73
7.23
41.03
24.68
0.05
41.96
23.12
129.73
22.91
0.02
C13
33.67
62.90
3.43
7.68
49.53
17.14
0.04
46.61
22.93
140.63
27.17
0.00
C14
31.67
65.00
3.33
7.72
39.94
22.57
0.05
38.79
30.98
127.58
24.53
0.03
C15
36.33
63.49
0.18
7.23
40.75
21.02
0.18
41.25
25.60
134.03
25.99
0.08
C16
31.48
63.30
5.22
5.99
49.40
21.02
0.06
42.32
26.59
150.81
23.01
0.01
C17
32.52
63.13
4.35
6.97
—
26.73
0.04
40.48
34.44
150.24
26.16
0.01
DS01
32.75
66.87
0.38
7.45
52.20
21.72
0.09
46.27
27.81
146.22
26.88
0.02
DS02
35.29
59.31
5.40
7.31
41.77
26.66
0.11
59.86
14.42
141.49
26.15
0.07
DS03
8.98
16.24
74.78
7.88
33.05
19.68
0.06
55.31
19.63
119.69
29.27
0.02
DS04
28.31
61.37
10.32
8.22
46.84
10.79
0.11
40.84
29.83
136.76
15.65
0.01
DS05
26.32
49.58
24.10
8.11
44.61
16.64
0.08
36.86
16.61
124.14
19.76
0.01
DS06
21.57
50.03
28.40
8.26
40.12
18.19
0.03
40.84
18.52
124.71
22.51
0.04
DS07
18.79
15.41
45.80
7.97
36.39
21.37
0.19
43.97
9.67
139.77
31.60
0.01
DS08
32.63
59.16
8.21
7.81
44.96
18.48
0.03
56.17
26.60
133.46
24.39
0.05
DS09
26.02
46.93
26.95
7.80
44.46
19.96
0.07
45.38
13.00
122.27
28.72
0.02
DS10
28.18
50.07
21.75
8.11
38.98
18.05
0.04
40.66
13.01
141.20
25.78
0.02
DS11
32.08
61.98
5.94
—
48.61
19.96
0.04
48.51
12.88
133.89
27.83
0.03
DS12
32.20
62.53
5.27
7.12
47.38
21.44
0.06
48.47
32.66
134.32
28.09
0.01
Mean
29.77
58.18
11.33
7.53
42.93
21.20
0.07
44.02
30.43
137.63
25.07
0.02
“—”: no detected.The concentrations of seven common trace metals (Cu, Cd, Pb, Cr, Zn, As, and Hg) in the sediments from ZMNNR are listed in Table1. The ranges of Cu, Cd, Pb, Cr, Zn, As, and Hg were 10.79–26.66 mg/kg (21.20 mg/kg in avg.), 0.03–0.19 mg/kg (0.07 mg/kg in avg.), 36.71–59.86 mg/kg (44.02 mg/kg in avg.), 9.67–134.51 mg/kg (30.43 mg/kg in avg.), 119.69–157.84 mg/kg (137.63 mg/kg in avg.), 15.65–31.60 mg/kg (25.07 mg/kg in avg.), and 0.00–0.08 mg/kg (0.02 mg/kg in avg.). The mean concentrations of all trace metals in the surface sediments of the ZMNNR were much higher than their respective background levels (Table 2), and in particular those of Cu and Zn were four times higher than the background levels. This exceeding of trace metals in the sediments from Zhangjiang River Estuary was also reported by Xie et al. [33].Table 2
Summary of trace metals concentrations in surface sediments of the ZMNNR.
Time of sampling
Number of samplings
Concentrations (mg/kg)
Cu
Cd
Pb
Cr
Zn
As
Hg
This study
2013
17a
21.47 ± 2.23
0.064 ± 0.034
41.97 ± 4.09
38.11 ± 26.26
140.78 ± 10.25
24.73 ± 1.67
0.019 ± 0.019
12b
19.41 ± 3.73
0.076 ± 0.046
46.93 ± 7.10
19.55 ± 7.74
133.16 ± 8.61
25.55 ± 4.44
0.026 ± 0.019
Previous survey
2007
17
21.04 ± 6.13
0.336 ± 0.055
63.20 ± 3.04
61.50 ± 18.03
127.65 ± 4.74
14.29 ± 1.00
0.034 ± 0.026
Jingchun  et al., 2010 [35]
2004
7c
30.28 ± 4.70
0.21 ± 0.03
53.91 ± 4.83
—
127.51 ± 13.92
—
—
7d
28.79 ± 5.59
0.30 ± 0.01
62.81 ± 9.44
—
143.96 ± 12.37
—
—
7e
36.42 ± 5.74
0.36 ± 0.08
70.09 ± 3.96
—
159.56 ± 9.88
—
—
Backgroundf
5.40
0.03
16.20
—
33.90
—
—
ISQG low
65
1.5
50
80
200
20
21
ISQG high
270
10
218
370
410
70
100
Data are means ± standard deviation of sites.
ISQG, Interim Sediment Quality Guidelines. The guidelines define the ISQG-high and ISQG-low values, which represent the lower 10th percentile and 50th percentile of chemical concentrations associated with adverse biological effects, based on the results of sediment toxicity testing [37].
aThe sampling sites in the intertidal zone.
bThe sampling sites in the subtidal zone.
cThe sampling sites in the mudflat.
dThe sampling sites in the forest edge.
eThe sampling sites in the forest.
fThe background levels of trace metals obtained from a subsample of 41 surface sediments in a location in continental shelf area of south Taiwan Strait.Furthermore, spatial distributions of trace metals are shown in Figures2 and 3. Higher concentrations of trace metals are generally found in the fine-grained sediments in the western coastal region of Zhangjiang River Estuary.Figure 2
Spatial distributions of trace metals (mg/kg) in the mangrove intertidal zone of the ZMNNR.Figure 3
Spatial distributions of trace metals (mg/kg) in the subtidal zone of the ZMNNR.


### 3.2. Trace Metals Concentrations in Biota

The concentration ranges of different metals in the organism were various. The overall trend of the accumulated degree of trace metals in the samples was as follows: Zn > Cu > As > Cr > Pb > Cd > Hg. Concentrations of four trace metals in the organisms from the study area (Table3) varied within 1.69~155.99 mg/kg for Cu, 17.88–105.34 mg/kg for Zn, 0.45–1.59 mg/kg for Pb, 0.23–12.35 mg/kg for Cr, 2.20–53.98 mg/kg for As, and 0.01–0.02 mg/kg for Hg. For Cu and Cd, the content of theUM sample is far higher than other creatures. For Pb, the concentration of the shell sample is more than the muscle sample. For Cr, the concentration in theBP shows the highest value of 12.35 mg/kg inBP liver.Table 3
Trace metals concentrations (mg/kg) inBoleophthalmus pectinirostris (BP), Siliqua minima (SM), and Uca maracoani (UM).
Biota
Cu
Zn
Pb
Cr
Cd
As
Hg
BP (muscle)
1.69
36.88
0.45
10.68
0.02
2.29
0.02
BP (liver)
7.34
105.34
0.95
12.35
0.14
2.40
0.02
SM (shell)
5.72
17.88
1.59
0.23
—
53.98
0.02
SM (muscle)
9.56
101.45
0.45
1.14
0.29
43.98
0.02
UM
115.99
87.50
1.50
0.72
0.62
17.65
0.01
Sediment
21.20
137.63
44.02
30.43
0.07
25.07
0.02
“—”: no detected.


## 3.1. Trace Metals in the Surface Sediments

Major sediment characteristics are shown in Table1, which presents the granulometry, the content of water (CW), and pH in surface sediments from ZMNNR. The result indicated that the sediment mainly consists of silt and clay-type soil, which account for an average 29.77% and 58.18%, respectively. Sand contents were low (average is 11.84%) except in DS03 and DS07 (74.78% and 45.8%, resp.). Water content in sediments varied from 33.05% to 52.2%, with a mean of 42.92%, and pH ranged from 5.99 to 8.26, with a mean of 7.53.Table 1
Physicochemical parameters and trace metals concentrations (mg/kg) in surface sediments from ZMNNR.
Stat.
Clay (%)
Silt (%)
Sand (%)
pH
CW (%)
Trace metals (mg/kg)
Cu
Cd
Pb
Cr
Zn
As
Hg
C01
—
—
—
7.93
—
24.96
0.09
36.98
27.53
135.18
26.32
0.02
C02
31.48
63.30
5.22
7.86
44.28
22.78
0.08
42.32
134.51
157.84
24.03
0.02
C03
32.52
63.13
4.35
7.77
40.86
21.44
0.09
47.93
42.30
155.98
24.43
0.03
C04
31.14
66.18
2.68
6.98
40.17
23.13
0.05
42.49
45.03
145.79
24.89
0.01
C05
30.63
66.57
2.80
7.48
39.53
22.85
0.04
50.22
52.55
149.81
25.25
0.04
C06
28.54
67.57
3.89
7.69
42.79
19.68
0.05
36.80
22.07
120.55
22.99
0.00
C07
32.17
64.30
3.53
7.02
41.33
21.86
0.06
36.71
32.39
134.18
23.74
0.02
C08
31.92
65.27
2.81
7.97
39.21
22.43
0.05
41.32
39.13
139.20
28.17
0.02
C09
30.71
65.22
4.07
7.12
44.76
21.30
0.05
39.49
34.25
144.36
22.16
0.01
C10
31.66
63.02
5.32
7.08
41.07
24.54
0.06
48.11
27.73
141.06
23.24
0.01
C11
31.94
63.98
4.08
6.95
44.96
23.84
0.04
39.66
26.72
136.33
25.47
0.00
C12
32.04
63.23
4.73
7.23
41.03
24.68
0.05
41.96
23.12
129.73
22.91
0.02
C13
33.67
62.90
3.43
7.68
49.53
17.14
0.04
46.61
22.93
140.63
27.17
0.00
C14
31.67
65.00
3.33
7.72
39.94
22.57
0.05
38.79
30.98
127.58
24.53
0.03
C15
36.33
63.49
0.18
7.23
40.75
21.02
0.18
41.25
25.60
134.03
25.99
0.08
C16
31.48
63.30
5.22
5.99
49.40
21.02
0.06
42.32
26.59
150.81
23.01
0.01
C17
32.52
63.13
4.35
6.97
—
26.73
0.04
40.48
34.44
150.24
26.16
0.01
DS01
32.75
66.87
0.38
7.45
52.20
21.72
0.09
46.27
27.81
146.22
26.88
0.02
DS02
35.29
59.31
5.40
7.31
41.77
26.66
0.11
59.86
14.42
141.49
26.15
0.07
DS03
8.98
16.24
74.78
7.88
33.05
19.68
0.06
55.31
19.63
119.69
29.27
0.02
DS04
28.31
61.37
10.32
8.22
46.84
10.79
0.11
40.84
29.83
136.76
15.65
0.01
DS05
26.32
49.58
24.10
8.11
44.61
16.64
0.08
36.86
16.61
124.14
19.76
0.01
DS06
21.57
50.03
28.40
8.26
40.12
18.19
0.03
40.84
18.52
124.71
22.51
0.04
DS07
18.79
15.41
45.80
7.97
36.39
21.37
0.19
43.97
9.67
139.77
31.60
0.01
DS08
32.63
59.16
8.21
7.81
44.96
18.48
0.03
56.17
26.60
133.46
24.39
0.05
DS09
26.02
46.93
26.95
7.80
44.46
19.96
0.07
45.38
13.00
122.27
28.72
0.02
DS10
28.18
50.07
21.75
8.11
38.98
18.05
0.04
40.66
13.01
141.20
25.78
0.02
DS11
32.08
61.98
5.94
—
48.61
19.96
0.04
48.51
12.88
133.89
27.83
0.03
DS12
32.20
62.53
5.27
7.12
47.38
21.44
0.06
48.47
32.66
134.32
28.09
0.01
Mean
29.77
58.18
11.33
7.53
42.93
21.20
0.07
44.02
30.43
137.63
25.07
0.02
“—”: no detected.The concentrations of seven common trace metals (Cu, Cd, Pb, Cr, Zn, As, and Hg) in the sediments from ZMNNR are listed in Table1. The ranges of Cu, Cd, Pb, Cr, Zn, As, and Hg were 10.79–26.66 mg/kg (21.20 mg/kg in avg.), 0.03–0.19 mg/kg (0.07 mg/kg in avg.), 36.71–59.86 mg/kg (44.02 mg/kg in avg.), 9.67–134.51 mg/kg (30.43 mg/kg in avg.), 119.69–157.84 mg/kg (137.63 mg/kg in avg.), 15.65–31.60 mg/kg (25.07 mg/kg in avg.), and 0.00–0.08 mg/kg (0.02 mg/kg in avg.). The mean concentrations of all trace metals in the surface sediments of the ZMNNR were much higher than their respective background levels (Table 2), and in particular those of Cu and Zn were four times higher than the background levels. This exceeding of trace metals in the sediments from Zhangjiang River Estuary was also reported by Xie et al. [33].Table 2
Summary of trace metals concentrations in surface sediments of the ZMNNR.
Time of sampling
Number of samplings
Concentrations (mg/kg)
Cu
Cd
Pb
Cr
Zn
As
Hg
This study
2013
17a
21.47 ± 2.23
0.064 ± 0.034
41.97 ± 4.09
38.11 ± 26.26
140.78 ± 10.25
24.73 ± 1.67
0.019 ± 0.019
12b
19.41 ± 3.73
0.076 ± 0.046
46.93 ± 7.10
19.55 ± 7.74
133.16 ± 8.61
25.55 ± 4.44
0.026 ± 0.019
Previous survey
2007
17
21.04 ± 6.13
0.336 ± 0.055
63.20 ± 3.04
61.50 ± 18.03
127.65 ± 4.74
14.29 ± 1.00
0.034 ± 0.026
Jingchun  et al., 2010 [35]
2004
7c
30.28 ± 4.70
0.21 ± 0.03
53.91 ± 4.83
—
127.51 ± 13.92
—
—
7d
28.79 ± 5.59
0.30 ± 0.01
62.81 ± 9.44
—
143.96 ± 12.37
—
—
7e
36.42 ± 5.74
0.36 ± 0.08
70.09 ± 3.96
—
159.56 ± 9.88
—
—
Backgroundf
5.40
0.03
16.20
—
33.90
—
—
ISQG low
65
1.5
50
80
200
20
21
ISQG high
270
10
218
370
410
70
100
Data are means ± standard deviation of sites.
ISQG, Interim Sediment Quality Guidelines. The guidelines define the ISQG-high and ISQG-low values, which represent the lower 10th percentile and 50th percentile of chemical concentrations associated with adverse biological effects, based on the results of sediment toxicity testing [37].
aThe sampling sites in the intertidal zone.
bThe sampling sites in the subtidal zone.
cThe sampling sites in the mudflat.
dThe sampling sites in the forest edge.
eThe sampling sites in the forest.
fThe background levels of trace metals obtained from a subsample of 41 surface sediments in a location in continental shelf area of south Taiwan Strait.Furthermore, spatial distributions of trace metals are shown in Figures2 and 3. Higher concentrations of trace metals are generally found in the fine-grained sediments in the western coastal region of Zhangjiang River Estuary.Figure 2
Spatial distributions of trace metals (mg/kg) in the mangrove intertidal zone of the ZMNNR.Figure 3
Spatial distributions of trace metals (mg/kg) in the subtidal zone of the ZMNNR.


## 3.2. Trace Metals Concentrations in Biota

The concentration ranges of different metals in the organism were various. The overall trend of the accumulated degree of trace metals in the samples was as follows: Zn > Cu > As > Cr > Pb > Cd > Hg. Concentrations of four trace metals in the organisms from the study area (Table3) varied within 1.69~155.99 mg/kg for Cu, 17.88–105.34 mg/kg for Zn, 0.45–1.59 mg/kg for Pb, 0.23–12.35 mg/kg for Cr, 2.20–53.98 mg/kg for As, and 0.01–0.02 mg/kg for Hg. For Cu and Cd, the content of theUM sample is far higher than other creatures. For Pb, the concentration of the shell sample is more than the muscle sample. For Cr, the concentration in theBP shows the highest value of 12.35 mg/kg inBP liver.Table 3
Trace metals concentrations (mg/kg) inBoleophthalmus pectinirostris (BP), Siliqua minima (SM), and Uca maracoani (UM).
Biota
Cu
Zn
Pb
Cr
Cd
As
Hg
BP (muscle)
1.69
36.88
0.45
10.68
0.02
2.29
0.02
BP (liver)
7.34
105.34
0.95
12.35
0.14
2.40
0.02
SM (shell)
5.72
17.88
1.59
0.23
—
53.98
0.02
SM (muscle)
9.56
101.45
0.45
1.14
0.29
43.98
0.02
UM
115.99
87.50
1.50
0.72
0.62
17.65
0.01
Sediment
21.20
137.63
44.02
30.43
0.07
25.07
0.02
“—”: no detected.


## 4. Discussion

### 4.1. Influencing Factors on Trace Metals in Sediment

Grain size, CW, and pH are the most important factors which control the distribution of trace metals in sediments. Significant spatial variation was observed, with increased clay content in sediments of the mangrove intertidal zone and the Zhangjiang River areas. Clay mineral and organic matter are the active components in the adsorption process, which is an important way for trace metals to enter into the sediment. Most of trace metals (Cu, Cd, Zn, and Hg) showed an obviously positive correlation with clay and silt contents with the correlation coefficients of 0.22–0.46 and 0.20–0.36 and negative correlation with sand content with the correlation coefficients from 0.08 for Hg to 0.45 for Zn. They indicated that Cu, Zn, Cd, and Hg tended to accumulate in fine particles which might be a major carrier for transporting these metals from rivers to Zhangjiang River Estuary. On the other hand, as for pH, they were higher in the mudflat > forest, but no significant difference was found among different stations. DS06 in Zhangjiang River had the highest pH, while station C16 in the mangrove intertidal zone had the lowest pH. Low pH values are frequently observed in mangrove forest sediments compared to the vegetated mudflat sediments [54]. This is attributed to the microbial decomposition of mangrove litter and hydrolysis of tannin in mangrove plants which releases organic acids [55]. In addition, anthropogenic turbulence would influence the distribution pattern, especially in the southwestern and northwestern coastal region upstream of mangrove, which seems to be the contribution of metals from Zhangjiang River and wastewater discharge of Yunxiao County. Since the mangrove is located near the Zhangjiang River Estuary, trace metals are highly concentrated due to the convergence of several sewage-polluted tributaries.When compared with historical records in the document published, the mean concentration of Cu, Cd, Pb, Cr, Hg, and Zn in the ZMNNR surface sediments decreased over the last decade, but the mean concentration of As increased (Table2). High As concentration might be attributed to the anthropogenic activities such as treatment of agricultural land with fertilizers and arsenical pesticides [56]. Attention should be paid when comparing the historical data on the concentrations of metal pollutants in sediments, because the differences in the pretreatment and analytical methods could cause errors. The same sampling and analytical methods were used in 2007 and 2013 surveys (Table 2). The results showed a decrease in the concentration of Pb, Cr, Cd, and Hg in the ZMNNR sediments. The concentrations of As, Cu, and Zn in the ZMNNR surface sediments decreased from 2007 to 2013.


### 4.2. Assessment of Sediment Quality

Compared with the Interim Sediment Quality Guidelines (ISQG), the average concentrations of these trace metals were over the ISQG-low value, but below the ISQG-high value [37]. The extent of metal pollution was accurately quantified using the pollution load index (PLI) and geoaccumulation index I
g
e
o. The pollution load index values of Cr, Cd, Zn, Cu, Pb, As, and Hg in all sediment samples are summarized in Table 4. The pollution load index values of all sites range from 0.38 to 1.10. According to the mean PLI value (0.77), the sediments of Zhangjiang River Estuary are unpolluted. But in C15 and DS02 the PLI value is above 1, indicating there may be some transportation and industrial and human activities in these locations.Table 4
Contaminant factor (CF) and pollution load index (PLI) values of trace metals in sediments from Zhangjiang River Estuary mangrove zone.
Station
CF (Cu)
CF (Cd)
CF (Pb)
CF (Cr)
CF (Zn)
CF (As)
CF (Hg)
PLI
C01
0.78
0.45
2.31
0.39
1.06
3.33
0.25
0.83
C02
0.71
0.40
2.65
—
1.24
3.04
0.25
0.94
C03
0.67
0.45
3.00
0.60
1.23
3.09
0.38
0.96
C04
0.72
0.25
2.66
0.63
1.15
3.15
0.13
0.75
C05
0.71
0.20
3.14
0.74
1.18
3.20
0.50
0.94
C06
0.62
0.25
2.30
0.31
0.95
2.91
0.00
0.38
C07
0.68
0.30
2.29
0.46
1.06
3.01
0.25
0.78
C08
0.70
0.25
2.58
0.55
1.10
3.57
0.25
0.82
C09
0.67
0.25
2.47
0.48
1.14
2.81
0.13
0.70
C10
0.77
0.30
3.01
0.39
1.11
2.94
0.13
0.73
C11
0.75
0.20
2.48
0.38
1.07
3.22
0.00
0.72
C12
0.77
0.25
2.62
0.33
1.02
2.90
0.25
0.74
C13
0.54
0.20
2.91
0.32
1.11
3.44
0.00
0.85
C14
0.71
0.25
2.42
0.44
1.00
3.11
0.38
0.80
C15
0.66
0.90
2.58
0.36
1.06
3.29
1.00
1.10
C16
0.66
0.30
2.65
0.37
1.19
2.91
0.13
0.70
C17
0.84
0.20
2.53
0.49
1.18
3.31
0.13
0.72
DS01
0.68
0.45
2.89
0.39
1.15
3.40
0.25
0.86
DS02
0.83
0.55
3.74
0.20
1.11
3.31
0.88
1.02
DS03
0.62
0.30
3.46
0.28
0.94
3.71
0.25
0.77
DS04
0.34
0.55
2.55
0.42
1.08
1.98
0.13
0.66
DS05
0.52
0.40
2.30
0.23
0.98
2.50
0.13
0.62
DS06
0.57
0.15
2.55
0.26
0.98
2.85
0.50
0.70
DS07
0.67
0.95
2.75
0.14
1.10
4.00
0.13
0.75
DS08
0.58
0.15
3.51
0.37
1.05
3.09
0.63
0.81
DS09
0.62
0.35
2.84
0.18
0.96
3.64
0.25
0.72
DS10
0.56
0.20
2.54
0.18
1.11
3.26
0.25
0.65
DS11
0.62
0.20
3.03
0.18
1.05
3.52
0.38
0.72
DS12
0.67
0.30
3.03
0.46
1.06
3.56
0.13
0.75TheI
g
e
o values were listed in Table 5. Among the studied metals, the I
g
e
o values showed the decreasing order As > Pb > Zn > Cu > Cr > Cd > Hg. Owing to the Müller scale, the results of I
g
e
o values indicated that Cd, Cu, Zn, and Hg showed an unpolluted situation at all stations (
I
g
e
o
<
0
). Cr showed less extent of pollution at stations C02 (I
g
e
o, 0.29), and other stations showed an unpolluted situation (
I
g
e
o
<
0
). For Pb, stations C07 and DS02 showed values falling into the uncontaminated to moderately contaminated classes (I
g
e
o, 0.61–1.32). For As, uncontaminated to moderately contaminated classes were showed at stations DS04 and DS07 (I
g
e
o, 0.4–1.42). The results suggested that station C02 was polluted by more trace metals than other stations.Table 5
Geoaccumulation index (I
g
e
o) values of trace metals in sediments from Zhangjiangkou Mangrove National Nature Reserve.
Station
Cu
Cd
Pb
Cr
Zn
As
Hg
C01
−0.94
−1.74
0.62
−1.95
−0.49
1.15
−2.58
C02
−1.08
−1.91
0.82
0.29
−0.27
1.02
−2.58
C03
−1.16
−1.74
1.00
−1.33
−0.29
1.04
−2.00
C04
−1.05
−2.58
0.82
−1.24
−0.39
1.07
−3.58
C05
−1.07
−2.91
1.07
−1.02
−0.35
1.09
−1.58
C06
−1.29
−2.58
0.62
−2.27
−0.66
0.96
/
C07
−1.13
−2.32
0.61
−1.72
−0.51
1.00
−2.58
C08
−1.10
−2.58
0.78
−1.44
−0.45
1.25
−2.58
C09
−1.17
−2.58
0.72
−1.64
−0.40
0.90
−3.58
C10
−0.97
−2.32
1.00
−1.94
−0.43
0.97
−3.58
C11
−1.01
−2.91
0.72
−1.99
−0.48
1.10
/
C12
−0.96
−2.58
0.81
−2.20
−0.55
0.95
−2.58
C13
−1.49
−2.91
0.96
−2.22
−0.44
1.20
/
C14
−1.09
−2.58
0.69
−1.78
−0.58
1.05
−2.00
C15
−1.19
−0.74
0.78
−2.06
−0.51
1.13
−0.58
C16
−1.19
−2.32
0.82
−2.00
−0.34
0.96
−3.58
C17
−0.84
−2.91
0.75
−1.63
−0.34
1.14
−3.58
DS01
−1.14
−1.74
0.95
−1.94
−0.38
1.18
−2.58
DS02
−0.85
−1.45
1.32
−2.88
−0.43
1.14
−0.78
DS03
−1.29
−2.32
1.20
−2.44
−0.67
1.30
−2.58
DS04
−2.15
−1.45
0.77
−1.84
−0.48
0.40
−3.58
DS05
−1.53
−1.91
0.62
−2.68
−0.62
0.74
−3.58
DS06
−1.40
−3.32
0.77
−2.52
−0.61
0.93
−1.58
DS07
−1.17
−0.66
0.87
−3.46
−0.45
1.42
−3.58
DS08
−1.38
−3.32
1.23
−2.00
−0.51
1.04
−1.26
DS09
−1.27
−2.10
0.92
−3.03
−0.64
1.28
−2.58
DS10
−1.41
−2.91
0.76
−3.03
−0.43
1.12
−2.58
DS11
−1.27
−2.91
1.02
−3.05
−0.51
1.23
−2.00
DS12
−1.16
−2.32
1.01
−1.71
−0.50
1.25
−3.58
Mean
−1.20
−2.30
0.86
−2.03
−0.47
1.07
−2.49
I
g
e
o class: 0: none, 1: none to medium, 2: moderate, 3: moderate to strong, 4: strongly polluted, 5: strong to very strong, and 6: very strong.
“/”: no data.The ecosystem in this study, which covered a wide range of perturbations, from industrial activities to agriculture, fisheries, and transport, held higher Pb, Zn, and As content than other mangrove sediments (Table6). It is noted that the concentration of Cu and Zn in Australia is very high in the mangroves and I
g
e
o values must also be high. In contrast, the mangroves in Singapore and France are much less contaminated with trace metals, probably because of better management of anthropogenic sources. Within Asia, the sediment in Zhangjiang mangrove zone is more contaminated with Pb and As than the other cities in China like Pearl River, Hong Kong, and Zhanjiang, likely owing to the rapid socioeconomic development in the region of the ZMNNR.Table 6
Mean concentrations of trace metals in the sediment of the mangroves worldwide.
Location
Cr (mg/kg)
Cu (mg/kg)
Zn (mg/kg)
As (mg/kg)
Cd (mg/kg)
Hg (mg/kg)
Pb (mg/kg)
Reference
Zhangjiang River Estuary, China
30.43
21.20
133.16
25.07
0.07
0.02
125.65
This study
Pearl River Estuary, China
51.52
1.18
32.23
104.68
127.41
/
/
Bai et al., 2011 [38]
Yingluo Bay, China
16.9
0.16
32.8
5.12
49
/
/
Li et al., 2008 [39]
Mai Po mangrove swamp, HK
42.8
1.05
52.6
22.4
149
/
/
Liang and Wong, 2003 [40]
Vellar Estuary, India
16.28
9.15
0.98
9.44
39.28
/
/
Palpandi and Kesavan, 2012 [22]
Sungei Buloh Wetland, Singapore
7.06
0.18
12.3
16.6
51.2
/
/
Cuong and Obbard, 2006 [41]
Port Klang, Malaysia
24.89
1.46
96.02
60.19
72.2
63.2
/
Sany et al., 2013 [42]
Mangrove zone, French Guiana
0.28
/
0.13
1.15
2.51
/
0.41
Marchand et al., 2006 [28]
Sydney Estuary, Australia
42
0.59
95
31
156
8.1
/
Nath et al., 2014 [25]
Estero Salado mangrove, Ecuador
161.69
0.97
45.24
54.4
390.19
4.37
/
Fernández-Cadena et al., 2014 [24]
“/”: no data.


### 4.3. Sources of Trace Metals in Mangrove Sediment

In order to obtain the possible metal sources of ZMNNR sediment, multivariate statistical analyses were carried out. According to the values of the Pearson correlation coefficients (Table7), many trace metals are significantly correlated (p
<
0.05). In this study, the Pearson matrix shows the significantly positive correlation of Pb with Cu (r
=
0.620) and indicates that these elements have the same source, most likely related to the anthropogenic activities in such a densely populated and agricultural area. Anthropogenic activities such as agricultures are the possible causes; for example, manufacturing fertilizers bring about metals and improve the accumulation and capacity of holding them [57]. Significant correlations between Cr and Zn (r
=
0.565) indicate that these elements are also derived from the same source.Table 7
Pearson correlation coefficient matrix between the trace metals and major elements and fine particles in surface sediments of the ZMNNR (n
=
29).
Cu
Cd
Pb
Cr
Zn
As
Hg
Clay
Silt
Cd
−0.055
Pb
0.620
0.313
Cr
0.203
−0.060
0.040
Zn
0.339
0.085
0.396
0.565
As
0.410
0.149
0.402
−0.146
−0.001
Hg
0.155
0.327
0.223
−0.042
−0.022
0.098
Clay
0.313
−0.078
0.150
0.221
0.463
−0.199
0.219
Silt
0.203
−0.363
−0.064
0.317
0.362
−0.424
0.046
0.882
Sand
−0.273
0.178
−0.064
−0.289
−0.457
0.314
−0.082
−0.959
−0.957
The bold numbers represent the significant coefficients at the level ofp
<
0.05.Cluster analysis (CA) is a method that is used to provide important information about the grouping of variables on the basis of similarity [58]. It was performed on the data using the Ward method and squared Euclidean distance and grouped into two clusters. It produced a dendrogram as shown in Figure 4. Cluster 1 includes Cd and Hg, which are supposed as contaminants derived from industrial sources. Cluster 2 contains Cu, As, Cr, and Pb which are identified as intensive agricultural activities.Figure 4
Dendrogram of trace metals concentrations of sediment samples.To further explore the extent of metal pollution and for source identification, principal component analysis (PCA) was performed for the studied sediments. And varimax rotation method was used to maximize the sum of the variances of the factor coefficients which better explained the possible sources. The results of PCA for trace metals contents are listed in Table8. According to these results, Hg, Cd, Pb, Cr, Cu, Zn, and As concentrations could be grouped into a three-component model, which accounted for 72.61% of all of the data variation.Table 8
Total variance explained and component matrices for the trace metals in surface sediments from the ZMNNR.
Component
⁢Initial eigenvalues
Extraction sums of squared loading
Rotation sums of squared loading
Total
% of variance
Cumulative%
Total
% of variance
Cumulative%
Total
% of variance
Cumulative%
1
2.33
33.27
33.27
2.33
33.27
33.27
1.98
28.27
28.27
2
1.60
22.89
56.15
1.60
22.89
56.15
1.70
24.23
52.50
3
1.15
16.45
72.61
1.15
16.45
72.61
1.41
20.11
72.61
4
0.76
10.80
83.40
5
0.56
7.97
91.37
6
0.38
5.38
96.75
7
0.23
3.26
100.00
Elements
⁢Component matrix
⁢Rotated component matrixa
F1
F2
F3
F1
F2
F3
Cu
0.79
0.06
−0.38
0.84
0.28
−0.04
Cd
0.36
−0.41
0.65
0.06
0.00
0.85
Pb
0.86
−0.15
−0.07
0.78
0.22
0.33
Cr
0.29
0.80
0.24
−0.07
0.87
−0.08
Zn
0.57
0.65
0.19
0.22
0.86
0.06
As
0.55
−0.43
−0.44
0.78
−0.27
0.05
Hg
0.33
−0.41
0.55
0.09
−0.03
0.75
Extraction method: principal component analysis.
Rotation method: varimax with Kaiser normalization.
aRotation converged in 4 iterations.In detail, the principal component 1 (PC1) which has high loading of Cu (0.84), Pb (0.78), and As (0.78) accounts for 28.27% of variance (Table8) and is the most important component. PC1 could be better explained as the agriculture factor. For irrigation purpose, the farmers often use the mine drainage water and chemical fertilizer that often release some ions in the soil [59]. PC2, which has high loading of Cr (0.87) and Zn (0.86) accounts for 24.23% of the variance. It was in accordance with the results of the correlation analysis (Table 8). These results implied that these metals could be originated from natural source. Xie et al. [33] found that the concentrations of Zn and Cr in ZMNNR sediment were not in evidence with the surrounding human activities. Zn and Cr mainly derived from parent rocks and their distribution patterns may depend on local hydrodynamic conditions [60]. The loading of Cd (0.85) and Hg (0.75) accounts for 20.11% of the variance, where PC3 can be considered as industry component. Pigments, electroplating, and metal industries were probably the major sources of these elements [61].


### 4.4. Comparison of Trace Metals Levels in Tissues

In order to evaluate the efficiency of trace metals bioaccumulation bySiliqua minima(SM), the biota-sediment factor, defined as the ratio between metals degrees in molluscs and sediment, respectively [49], has been computed for both species (Figure 5). Cd is the metal which records the highest BSAF values and Pb is the metal with the lowest one.Uca maracoani (UM) has the highest BSAF mean for all metals except Cr, As, and Hg (Figure 5).Figure 5
Mean biosediment accumulation factor values (BSAF) inBoleophthalmus pectinirostris(BP), Siliqua minima(SM), andUca maracoani(UM).Relative differences in the concentrations of the metals between muscle and liver are apparent, where metal concentrations were between 1 and 5 times higher inBoleophthalmus pectinirostris. The reason may be their physiological roles in fish metabolism. As shown in Table 3, the target tissues of trace metals are metabolically active ones, like the liver, kidney, and gill. Therefore, in contrast to some other tissues like the muscle, where metabolic activity is relatively low, metal accumulation in these tissues records higher level [62–64].SM, a kind of mussel, is considered as excellent indicators of metal bioavailability in the environment, as the concentrations in its tissues were related to the Bakun upwelling index [65].Concentrations of Zn and Cu in the tissue of the benthos were higher than those of other metals. The reason may be that Zn and Cu are essential metals for aquatic organisms and thus subject to active absorption in marine organisms [66]. Variations in the concentration of Cu showed a highest level of accumulation inUM, whereas concentrations of other metals are appreciably low. Cu is essential for crustaceans, because it can participate in the respiratory pigment hemocyanin [67]. The concentrations of As are of great concern with regard to its richness in the organisms. Cr is an essential trace element in organisms and plays a very important role (in its biologically usable form) during the metabolic processing of glucose [68]. Compared with Zn and Cu, the quantity of Cr demanded for the organisms is low, and thus the levels of Cr in the organisms are relatively lower than those of Zn and Cu. Cd, Hg, and Pb are not essential for organisms and have toxic effects at low concentration [69, 70].Zn and Cd are the elements that have previously attracted much attention in the ZMNNR, because the concentration often can be related to the intense upwelling of sea water characteristic of the area [20, 71]. The cadmium represents concentrations constantly higher (around 0.29 mg/kg, dry weight) than expected or observed at comparable locations. The highest concentration of Zn was measured in muscle ofSM. It is worth studying the source of the Cd and Zn enrichment in fish and mussels, respectively. Although industrial pollution, like lead-acid battery factory and chemical industry effluents, can increase the level of contaminant, the possibility of the strong upwelling bringing high levels of Cd and Zn cannot be excluded. Indeed, such a phenomenon has been explicated in the previous study [72].


## 4.1. Influencing Factors on Trace Metals in Sediment

Grain size, CW, and pH are the most important factors which control the distribution of trace metals in sediments. Significant spatial variation was observed, with increased clay content in sediments of the mangrove intertidal zone and the Zhangjiang River areas. Clay mineral and organic matter are the active components in the adsorption process, which is an important way for trace metals to enter into the sediment. Most of trace metals (Cu, Cd, Zn, and Hg) showed an obviously positive correlation with clay and silt contents with the correlation coefficients of 0.22–0.46 and 0.20–0.36 and negative correlation with sand content with the correlation coefficients from 0.08 for Hg to 0.45 for Zn. They indicated that Cu, Zn, Cd, and Hg tended to accumulate in fine particles which might be a major carrier for transporting these metals from rivers to Zhangjiang River Estuary. On the other hand, as for pH, they were higher in the mudflat > forest, but no significant difference was found among different stations. DS06 in Zhangjiang River had the highest pH, while station C16 in the mangrove intertidal zone had the lowest pH. Low pH values are frequently observed in mangrove forest sediments compared to the vegetated mudflat sediments [54]. This is attributed to the microbial decomposition of mangrove litter and hydrolysis of tannin in mangrove plants which releases organic acids [55]. In addition, anthropogenic turbulence would influence the distribution pattern, especially in the southwestern and northwestern coastal region upstream of mangrove, which seems to be the contribution of metals from Zhangjiang River and wastewater discharge of Yunxiao County. Since the mangrove is located near the Zhangjiang River Estuary, trace metals are highly concentrated due to the convergence of several sewage-polluted tributaries.When compared with historical records in the document published, the mean concentration of Cu, Cd, Pb, Cr, Hg, and Zn in the ZMNNR surface sediments decreased over the last decade, but the mean concentration of As increased (Table2). High As concentration might be attributed to the anthropogenic activities such as treatment of agricultural land with fertilizers and arsenical pesticides [56]. Attention should be paid when comparing the historical data on the concentrations of metal pollutants in sediments, because the differences in the pretreatment and analytical methods could cause errors. The same sampling and analytical methods were used in 2007 and 2013 surveys (Table 2). The results showed a decrease in the concentration of Pb, Cr, Cd, and Hg in the ZMNNR sediments. The concentrations of As, Cu, and Zn in the ZMNNR surface sediments decreased from 2007 to 2013.


## 4.2. Assessment of Sediment Quality

Compared with the Interim Sediment Quality Guidelines (ISQG), the average concentrations of these trace metals were over the ISQG-low value, but below the ISQG-high value [37]. The extent of metal pollution was accurately quantified using the pollution load index (PLI) and geoaccumulation index I
g
e
o. The pollution load index values of Cr, Cd, Zn, Cu, Pb, As, and Hg in all sediment samples are summarized in Table 4. The pollution load index values of all sites range from 0.38 to 1.10. According to the mean PLI value (0.77), the sediments of Zhangjiang River Estuary are unpolluted. But in C15 and DS02 the PLI value is above 1, indicating there may be some transportation and industrial and human activities in these locations.Table 4
Contaminant factor (CF) and pollution load index (PLI) values of trace metals in sediments from Zhangjiang River Estuary mangrove zone.
Station
CF (Cu)
CF (Cd)
CF (Pb)
CF (Cr)
CF (Zn)
CF (As)
CF (Hg)
PLI
C01
0.78
0.45
2.31
0.39
1.06
3.33
0.25
0.83
C02
0.71
0.40
2.65
—
1.24
3.04
0.25
0.94
C03
0.67
0.45
3.00
0.60
1.23
3.09
0.38
0.96
C04
0.72
0.25
2.66
0.63
1.15
3.15
0.13
0.75
C05
0.71
0.20
3.14
0.74
1.18
3.20
0.50
0.94
C06
0.62
0.25
2.30
0.31
0.95
2.91
0.00
0.38
C07
0.68
0.30
2.29
0.46
1.06
3.01
0.25
0.78
C08
0.70
0.25
2.58
0.55
1.10
3.57
0.25
0.82
C09
0.67
0.25
2.47
0.48
1.14
2.81
0.13
0.70
C10
0.77
0.30
3.01
0.39
1.11
2.94
0.13
0.73
C11
0.75
0.20
2.48
0.38
1.07
3.22
0.00
0.72
C12
0.77
0.25
2.62
0.33
1.02
2.90
0.25
0.74
C13
0.54
0.20
2.91
0.32
1.11
3.44
0.00
0.85
C14
0.71
0.25
2.42
0.44
1.00
3.11
0.38
0.80
C15
0.66
0.90
2.58
0.36
1.06
3.29
1.00
1.10
C16
0.66
0.30
2.65
0.37
1.19
2.91
0.13
0.70
C17
0.84
0.20
2.53
0.49
1.18
3.31
0.13
0.72
DS01
0.68
0.45
2.89
0.39
1.15
3.40
0.25
0.86
DS02
0.83
0.55
3.74
0.20
1.11
3.31
0.88
1.02
DS03
0.62
0.30
3.46
0.28
0.94
3.71
0.25
0.77
DS04
0.34
0.55
2.55
0.42
1.08
1.98
0.13
0.66
DS05
0.52
0.40
2.30
0.23
0.98
2.50
0.13
0.62
DS06
0.57
0.15
2.55
0.26
0.98
2.85
0.50
0.70
DS07
0.67
0.95
2.75
0.14
1.10
4.00
0.13
0.75
DS08
0.58
0.15
3.51
0.37
1.05
3.09
0.63
0.81
DS09
0.62
0.35
2.84
0.18
0.96
3.64
0.25
0.72
DS10
0.56
0.20
2.54
0.18
1.11
3.26
0.25
0.65
DS11
0.62
0.20
3.03
0.18
1.05
3.52
0.38
0.72
DS12
0.67
0.30
3.03
0.46
1.06
3.56
0.13
0.75TheI
g
e
o values were listed in Table 5. Among the studied metals, the I
g
e
o values showed the decreasing order As > Pb > Zn > Cu > Cr > Cd > Hg. Owing to the Müller scale, the results of I
g
e
o values indicated that Cd, Cu, Zn, and Hg showed an unpolluted situation at all stations (
I
g
e
o
<
0
). Cr showed less extent of pollution at stations C02 (I
g
e
o, 0.29), and other stations showed an unpolluted situation (
I
g
e
o
<
0
). For Pb, stations C07 and DS02 showed values falling into the uncontaminated to moderately contaminated classes (I
g
e
o, 0.61–1.32). For As, uncontaminated to moderately contaminated classes were showed at stations DS04 and DS07 (I
g
e
o, 0.4–1.42). The results suggested that station C02 was polluted by more trace metals than other stations.Table 5
Geoaccumulation index (I
g
e
o) values of trace metals in sediments from Zhangjiangkou Mangrove National Nature Reserve.
Station
Cu
Cd
Pb
Cr
Zn
As
Hg
C01
−0.94
−1.74
0.62
−1.95
−0.49
1.15
−2.58
C02
−1.08
−1.91
0.82
0.29
−0.27
1.02
−2.58
C03
−1.16
−1.74
1.00
−1.33
−0.29
1.04
−2.00
C04
−1.05
−2.58
0.82
−1.24
−0.39
1.07
−3.58
C05
−1.07
−2.91
1.07
−1.02
−0.35
1.09
−1.58
C06
−1.29
−2.58
0.62
−2.27
−0.66
0.96
/
C07
−1.13
−2.32
0.61
−1.72
−0.51
1.00
−2.58
C08
−1.10
−2.58
0.78
−1.44
−0.45
1.25
−2.58
C09
−1.17
−2.58
0.72
−1.64
−0.40
0.90
−3.58
C10
−0.97
−2.32
1.00
−1.94
−0.43
0.97
−3.58
C11
−1.01
−2.91
0.72
−1.99
−0.48
1.10
/
C12
−0.96
−2.58
0.81
−2.20
−0.55
0.95
−2.58
C13
−1.49
−2.91
0.96
−2.22
−0.44
1.20
/
C14
−1.09
−2.58
0.69
−1.78
−0.58
1.05
−2.00
C15
−1.19
−0.74
0.78
−2.06
−0.51
1.13
−0.58
C16
−1.19
−2.32
0.82
−2.00
−0.34
0.96
−3.58
C17
−0.84
−2.91
0.75
−1.63
−0.34
1.14
−3.58
DS01
−1.14
−1.74
0.95
−1.94
−0.38
1.18
−2.58
DS02
−0.85
−1.45
1.32
−2.88
−0.43
1.14
−0.78
DS03
−1.29
−2.32
1.20
−2.44
−0.67
1.30
−2.58
DS04
−2.15
−1.45
0.77
−1.84
−0.48
0.40
−3.58
DS05
−1.53
−1.91
0.62
−2.68
−0.62
0.74
−3.58
DS06
−1.40
−3.32
0.77
−2.52
−0.61
0.93
−1.58
DS07
−1.17
−0.66
0.87
−3.46
−0.45
1.42
−3.58
DS08
−1.38
−3.32
1.23
−2.00
−0.51
1.04
−1.26
DS09
−1.27
−2.10
0.92
−3.03
−0.64
1.28
−2.58
DS10
−1.41
−2.91
0.76
−3.03
−0.43
1.12
−2.58
DS11
−1.27
−2.91
1.02
−3.05
−0.51
1.23
−2.00
DS12
−1.16
−2.32
1.01
−1.71
−0.50
1.25
−3.58
Mean
−1.20
−2.30
0.86
−2.03
−0.47
1.07
−2.49
I
g
e
o class: 0: none, 1: none to medium, 2: moderate, 3: moderate to strong, 4: strongly polluted, 5: strong to very strong, and 6: very strong.
“/”: no data.The ecosystem in this study, which covered a wide range of perturbations, from industrial activities to agriculture, fisheries, and transport, held higher Pb, Zn, and As content than other mangrove sediments (Table6). It is noted that the concentration of Cu and Zn in Australia is very high in the mangroves and I
g
e
o values must also be high. In contrast, the mangroves in Singapore and France are much less contaminated with trace metals, probably because of better management of anthropogenic sources. Within Asia, the sediment in Zhangjiang mangrove zone is more contaminated with Pb and As than the other cities in China like Pearl River, Hong Kong, and Zhanjiang, likely owing to the rapid socioeconomic development in the region of the ZMNNR.Table 6
Mean concentrations of trace metals in the sediment of the mangroves worldwide.
Location
Cr (mg/kg)
Cu (mg/kg)
Zn (mg/kg)
As (mg/kg)
Cd (mg/kg)
Hg (mg/kg)
Pb (mg/kg)
Reference
Zhangjiang River Estuary, China
30.43
21.20
133.16
25.07
0.07
0.02
125.65
This study
Pearl River Estuary, China
51.52
1.18
32.23
104.68
127.41
/
/
Bai et al., 2011 [38]
Yingluo Bay, China
16.9
0.16
32.8
5.12
49
/
/
Li et al., 2008 [39]
Mai Po mangrove swamp, HK
42.8
1.05
52.6
22.4
149
/
/
Liang and Wong, 2003 [40]
Vellar Estuary, India
16.28
9.15
0.98
9.44
39.28
/
/
Palpandi and Kesavan, 2012 [22]
Sungei Buloh Wetland, Singapore
7.06
0.18
12.3
16.6
51.2
/
/
Cuong and Obbard, 2006 [41]
Port Klang, Malaysia
24.89
1.46
96.02
60.19
72.2
63.2
/
Sany et al., 2013 [42]
Mangrove zone, French Guiana
0.28
/
0.13
1.15
2.51
/
0.41
Marchand et al., 2006 [28]
Sydney Estuary, Australia
42
0.59
95
31
156
8.1
/
Nath et al., 2014 [25]
Estero Salado mangrove, Ecuador
161.69
0.97
45.24
54.4
390.19
4.37
/
Fernández-Cadena et al., 2014 [24]
“/”: no data.


## 4.3. Sources of Trace Metals in Mangrove Sediment

In order to obtain the possible metal sources of ZMNNR sediment, multivariate statistical analyses were carried out. According to the values of the Pearson correlation coefficients (Table7), many trace metals are significantly correlated (p
<
0.05). In this study, the Pearson matrix shows the significantly positive correlation of Pb with Cu (r
=
0.620) and indicates that these elements have the same source, most likely related to the anthropogenic activities in such a densely populated and agricultural area. Anthropogenic activities such as agricultures are the possible causes; for example, manufacturing fertilizers bring about metals and improve the accumulation and capacity of holding them [57]. Significant correlations between Cr and Zn (r
=
0.565) indicate that these elements are also derived from the same source.Table 7
Pearson correlation coefficient matrix between the trace metals and major elements and fine particles in surface sediments of the ZMNNR (n
=
29).
Cu
Cd
Pb
Cr
Zn
As
Hg
Clay
Silt
Cd
−0.055
Pb
0.620
0.313
Cr
0.203
−0.060
0.040
Zn
0.339
0.085
0.396
0.565
As
0.410
0.149
0.402
−0.146
−0.001
Hg
0.155
0.327
0.223
−0.042
−0.022
0.098
Clay
0.313
−0.078
0.150
0.221
0.463
−0.199
0.219
Silt
0.203
−0.363
−0.064
0.317
0.362
−0.424
0.046
0.882
Sand
−0.273
0.178
−0.064
−0.289
−0.457
0.314
−0.082
−0.959
−0.957
The bold numbers represent the significant coefficients at the level ofp
<
0.05.Cluster analysis (CA) is a method that is used to provide important information about the grouping of variables on the basis of similarity [58]. It was performed on the data using the Ward method and squared Euclidean distance and grouped into two clusters. It produced a dendrogram as shown in Figure 4. Cluster 1 includes Cd and Hg, which are supposed as contaminants derived from industrial sources. Cluster 2 contains Cu, As, Cr, and Pb which are identified as intensive agricultural activities.Figure 4
Dendrogram of trace metals concentrations of sediment samples.To further explore the extent of metal pollution and for source identification, principal component analysis (PCA) was performed for the studied sediments. And varimax rotation method was used to maximize the sum of the variances of the factor coefficients which better explained the possible sources. The results of PCA for trace metals contents are listed in Table8. According to these results, Hg, Cd, Pb, Cr, Cu, Zn, and As concentrations could be grouped into a three-component model, which accounted for 72.61% of all of the data variation.Table 8
Total variance explained and component matrices for the trace metals in surface sediments from the ZMNNR.
Component
⁢Initial eigenvalues
Extraction sums of squared loading
Rotation sums of squared loading
Total
% of variance
Cumulative%
Total
% of variance
Cumulative%
Total
% of variance
Cumulative%
1
2.33
33.27
33.27
2.33
33.27
33.27
1.98
28.27
28.27
2
1.60
22.89
56.15
1.60
22.89
56.15
1.70
24.23
52.50
3
1.15
16.45
72.61
1.15
16.45
72.61
1.41
20.11
72.61
4
0.76
10.80
83.40
5
0.56
7.97
91.37
6
0.38
5.38
96.75
7
0.23
3.26
100.00
Elements
⁢Component matrix
⁢Rotated component matrixa
F1
F2
F3
F1
F2
F3
Cu
0.79
0.06
−0.38
0.84
0.28
−0.04
Cd
0.36
−0.41
0.65
0.06
0.00
0.85
Pb
0.86
−0.15
−0.07
0.78
0.22
0.33
Cr
0.29
0.80
0.24
−0.07
0.87
−0.08
Zn
0.57
0.65
0.19
0.22
0.86
0.06
As
0.55
−0.43
−0.44
0.78
−0.27
0.05
Hg
0.33
−0.41
0.55
0.09
−0.03
0.75
Extraction method: principal component analysis.
Rotation method: varimax with Kaiser normalization.
aRotation converged in 4 iterations.In detail, the principal component 1 (PC1) which has high loading of Cu (0.84), Pb (0.78), and As (0.78) accounts for 28.27% of variance (Table8) and is the most important component. PC1 could be better explained as the agriculture factor. For irrigation purpose, the farmers often use the mine drainage water and chemical fertilizer that often release some ions in the soil [59]. PC2, which has high loading of Cr (0.87) and Zn (0.86) accounts for 24.23% of the variance. It was in accordance with the results of the correlation analysis (Table 8). These results implied that these metals could be originated from natural source. Xie et al. [33] found that the concentrations of Zn and Cr in ZMNNR sediment were not in evidence with the surrounding human activities. Zn and Cr mainly derived from parent rocks and their distribution patterns may depend on local hydrodynamic conditions [60]. The loading of Cd (0.85) and Hg (0.75) accounts for 20.11% of the variance, where PC3 can be considered as industry component. Pigments, electroplating, and metal industries were probably the major sources of these elements [61].


## 4.4. Comparison of Trace Metals Levels in Tissues

In order to evaluate the efficiency of trace metals bioaccumulation bySiliqua minima(SM), the biota-sediment factor, defined as the ratio between metals degrees in molluscs and sediment, respectively [49], has been computed for both species (Figure 5). Cd is the metal which records the highest BSAF values and Pb is the metal with the lowest one.Uca maracoani (UM) has the highest BSAF mean for all metals except Cr, As, and Hg (Figure 5).Figure 5
Mean biosediment accumulation factor values (BSAF) inBoleophthalmus pectinirostris(BP), Siliqua minima(SM), andUca maracoani(UM).Relative differences in the concentrations of the metals between muscle and liver are apparent, where metal concentrations were between 1 and 5 times higher inBoleophthalmus pectinirostris. The reason may be their physiological roles in fish metabolism. As shown in Table 3, the target tissues of trace metals are metabolically active ones, like the liver, kidney, and gill. Therefore, in contrast to some other tissues like the muscle, where metabolic activity is relatively low, metal accumulation in these tissues records higher level [62–64].SM, a kind of mussel, is considered as excellent indicators of metal bioavailability in the environment, as the concentrations in its tissues were related to the Bakun upwelling index [65].Concentrations of Zn and Cu in the tissue of the benthos were higher than those of other metals. The reason may be that Zn and Cu are essential metals for aquatic organisms and thus subject to active absorption in marine organisms [66]. Variations in the concentration of Cu showed a highest level of accumulation inUM, whereas concentrations of other metals are appreciably low. Cu is essential for crustaceans, because it can participate in the respiratory pigment hemocyanin [67]. The concentrations of As are of great concern with regard to its richness in the organisms. Cr is an essential trace element in organisms and plays a very important role (in its biologically usable form) during the metabolic processing of glucose [68]. Compared with Zn and Cu, the quantity of Cr demanded for the organisms is low, and thus the levels of Cr in the organisms are relatively lower than those of Zn and Cu. Cd, Hg, and Pb are not essential for organisms and have toxic effects at low concentration [69, 70].Zn and Cd are the elements that have previously attracted much attention in the ZMNNR, because the concentration often can be related to the intense upwelling of sea water characteristic of the area [20, 71]. The cadmium represents concentrations constantly higher (around 0.29 mg/kg, dry weight) than expected or observed at comparable locations. The highest concentration of Zn was measured in muscle ofSM. It is worth studying the source of the Cd and Zn enrichment in fish and mussels, respectively. Although industrial pollution, like lead-acid battery factory and chemical industry effluents, can increase the level of contaminant, the possibility of the strong upwelling bringing high levels of Cd and Zn cannot be excluded. Indeed, such a phenomenon has been explicated in the previous study [72].


## 5. Conclusions

We collected the sediment and biota samples in Zhangjiangkou Mangrove National Nature Reserve and conducted the experiment in Marine Organic Chemistry Lab in Xiamen University, Xiamen. The ranges of measured concentrations expressed in mg/kg were the following: 10.79–26.66 mg/kg for Cu, 0.03–0.19 mg/kg for Cd, 36.71–59.86 mg/kg for Pb, 9.67–134.51 mg/kg for Cr, 119.69–157.84 mg/kg for Zn, 15.65–31.6 mg/kg for As, and 0.00–0.08 mg/kg for Hg. Higher concentrations of trace metals are generally found in the fine-grained sediments in the western coastal region of Zhangjiang River Estuary. The results showed a decrease in the concentration of Pb, Cr, Cd, and Hg and increase in the concentration of As, Cu, and Zn from 2007 to 2013 in the ZMNNR sediments. For biota, the overall trend of the degree of accumulation of trace metals in the samples was as follows: Zn > Cu > As > Cr > Pb > Cd > Hg. Moreover, according to data from this study,Uca maracoani(UM) seems to have a greater bioaccumulation capacity than other species for all the metals (Cu, Pb, Cd, and Zn) considered except Cr. Correlation analysis and PCA illustrated that trace metals (Hg, Cd, Pb, Cr, Cu, Zn, As, and Hg) may derive from metal processing, electroplating industries, industrial and agricultural wastewater, and domestic sewage. And compared to other mangroves all over the world, Pb, Zn, and As are highly enriched in this ecosystem. According to the mean PLI value (0.77), the sediments of Zhangjiang River Estuary are unpolluted except C15 and DS02 station. Owing to the Müller scale, the results of I
g
e
o values indicated that Cd, Cu, Zn, and Hg showed an unpolluted situation at all stations and that Pb, Cr, and As show polluted situation in some station.



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*Source: 2167053-2016-10-04.xml*