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Applied and Environmental Soil Science
Volume 2010 (2010), Article ID 726946, 7 pages
http://dx.doi.org/10.1155/2010/726946
Review Article

Heavy Metal-Induced Oxidative DNA Damage in Earthworms: A Review

1Department of Life and Environment Engineering, Faculty of Environmental Engineering, The University of Kitakyushu, Kitakyushu, Fukuoka 808-0135, Japan
2Division of Teacher Training, Faculty of Education and Culture, University of Miyazaki, Miyazaki 889-2192, Japan

Received 30 June 2009; Accepted 8 December 2009

Academic Editor: Natchimuthu Karmegam

Copyright © 2010 Takeshi Hirano and Kazuyoshi Tamae. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract

Earthworms can be used as a bio-indicator of metal contamination in soil, Earlier reports claimed the bioaccumulation of heavy metals in earthworm tissues, while the metal-induced mutagenicity reared in contaminated soils for long duration. But we examined the metal-induced mutagenicity in earthworms reared in metal containing culture beddings. In this experiment we observed the generation of 8-oxoguanine (8-oxo-Gua) in earthworms exposed to cadmium and nickel in soil. 8-oxo-Gua is a major premutagenic form of oxidative DNA damage that induces GC-to-TA point mutations, leading to carcinogenesis.

1. Introduction

Molecular oxygen is essential for the survival of all aerobic organisms, and reactive oxygen species (ROS), which are byproducts of oxygen metabolism, are harmful for living organisms. Thus, oxygen is a double-edged sword. In fact, ROS are known to directly attack vital cellular components, including proteins, lipids, and nucleic acids. The oxidation of these molecules is associated with cellular dysfunction, leading to various biological responses, such as inflammation and apoptosis. Since ROS, such as superoxide radical , H2O2, and hydroxyl radical , are constantly generated in vivo as byproducts of respiration, agent metabolism, or pathophysiological conditions [13], it is difficult to completely prevent their harmful effects on cellular components.

When ROS attack DNA, oxidized bases are frequently generated [4]. Among the various forms of oxidative DNA damage, 8-oxoguanine (7, 8-dihydro-8-oxoguanine, abbreviated as 8-oxo-Gua or 8-OH-Gua) has been most extensively investigated [5]. Since 8-oxo-Gua is premutagenic, it has been suggested to contribute to human diseases [6, 7]. On the other hand, living organisms have repair systems for oxidative DNA damage, to preserve genetic stability. Recent studies have revealed the complicated network of 8-oxo-Gua repair systems (termed as the “GO system”) [8]. However, if unrepaired oxidative DNA damage remains in DNA, then it can induce point mutations. Therefore, the ability to repair the damage is critical in terms of genetic stability. Such measurements of 8-oxo-Gua and its repair ability may open new fields in the studies of risk assessment, molecular epidemiology, and health promotion.

Among the many kinds of organisms living in soil, the earthworm is a quite useful organism for the evaluation of metal contamination in soil, because significant positive correlations have been found between the metal concentrations in the earthworm and the cadmium (Cd), copper (Cu), lead (Pb), and zinc (Zn) concentrations in soil [9]. This evidence prompted us to verify the utility of the earthworm as a biomonitor. Recently, we studied the 8-oxo-Gua generation in earthworms exposed to Cd or nickel (Ni), to examine the possibility that earthworms could be used as a biomonitor for DNA-damaging factors in soil.

This paper focuses on the possibility of using earthworms as a biomonitoring method for oxidative DNA damage-inducing factors in soil.

2. 8-Oxoguanine

Point mutations generated via oxidative DNA damage are involved in cancer development, because mutations are a common feature of human cancers. In this context, the studies of 8-oxo-Gua, which is an oxidized guanine, have significant implications for understanding the mechanisms of mutation-associated diseases, especially cancer [10]. 8-oxo-Gua is a mutagenic lesion formed spontaneously in the genomic DNA of aerobic organisms (Figure 1) and by the actions of exogenous factors, such as ionizing radiation, chemical pollutants, heavy metals, food, and bacteria. Although 8-oxo-Gua is not necessarily the most abundant form of oxidative DNA damage, it has been the most extensively studied, because it can be quantitated with high sensitivity by high-performance liquid chromatography coupled with electrochemical detection (HPLC-ECD), and it is quite easily measured in laboratories [5, 11]. 8-oxo-Gua and 8-oxoadenine (8-oxo-Ade) have been well studied in mutagenic oxidized DNA products, and their frequencies of generation in mammalian DNA and their degrees of mutagenicity are similar [1215].

726946.fig.001
Figure 1: Structure of 8-oxo-Gua. 8-Oxo-Gua is formed by the hydroxylation of guanine at the C-8 position.

Since 8-oxo-Gua was discovered and reported in 1984 [16], this form of DNA damage and its repair systems have been studied vigorously. 8-oxo-Gua induces GC-to-TA transversion-type point mutations [17], and thus it is believed to have a key role in cancer development. Moreover, 8-oxo-Gua is efficiently removed from DNA via the short-patch base excision repair (BER) pathway, initiated by 8-oxoguanine DNA glycosylase 1 (OGG1).

3. Heavy Metals and 8-Oxoguanine/8-Oxo-Gua Repair System

Heavy metal pollution of soil is widespread across the globe and has caused biological problems, leading to potential toxicity to living organisms. Recent research found that the atmospheric input of heavy metals to agricultural systems also significantly contributed to metal loading in soil [19]. These complicated pathways of contamination make it difficult to avoid the exposure to the metals existing in our surroundings.

We previously reported the relationship between 8-oxo-Gua/its repair ability and some heavy metals [2023]. In the studies, we found that cadmium chloride and arsenic compounds increased the level of 8-oxo-Gua accumulation [20, 21, 24]. It is noteworthy that these heavy metals inhibited the 8-oxo-Gua repair activity. Other studies besides ours also generated similar data, as shown in Table 1. Some metals, such as hexavalent chromium (CrVI), manganese (Mn), and Pb, as well as Cd and arsenic (As), also reportedly inhibited the 8-oxo-Gua repair system [2529]. Among heavy metals, the association of Cd with 8-oxo-Gua repair systems has been studied since the early stage of the research. In 1997, we first described an association between Cd exposure and the inhibition of 8-oxo-Gua excision repair activity in rat testes [20]. After the cloning of mammalian OGG1, it was demonstrated that Cd exposure down-regulated OGG1 expression in rat lung and alveolar epithelial cells [30]. Youn et al. suggested that Cd attenuated the removal of -ray-induced 8-oxo-Gua adducts, which in turn increased the mutation frequency, and that this effect might, at least in part, result from the suppression of hOGG1 transcription via the inactivation of the Spl transcription factor, as a result of Cd treatment [22]. These inhibitory effects of Cd on OGG1 activity are similar to the inhibition of 8-oxo-dGTPase activity induced by Cd treatment, which led to the accumulation of 8-oxo-Gua in DNA [23]. Although it is likely that Cd exposure might broadly disturb the 8-oxo-Gua repair system, the exact mechanism of the inhibition remains unclear.

tab1
Table 1: Association of heavy metal exposure with 8-oxo-Gua repair.

4. Oxidative Stresses and Earthworms

Several oxygen radical studies using earthworms have been performed. The biochemical effects of tetrabromobisphenol A (TBBPA) on the earthworm Eisenia fetida (E. fetida) were examined to assess the ecological toxicity of TBBPA. The ROS generated in the earthworm was identified as ·OH. With increasing TBBPA concentrations, the levels of antioxidant enzymes, glutathione, and MDA varied significantly. The study indicated that TBBPA exerted its toxic effects on E. fetida by inducing the generation of ROS, resulting in oxidative damage [31].

Since earthworm skin contains several molecules (tetraene and triene sterol) similar to those in human beings, it is considered to be useful as a biomonitor for environmental factors for human beings. For example, the phototoxic effects of UVR in sunlight and its possible mechanism of action were analyzed by using earthworms [32]. In the study, the generation of ROS, the photooxidation of lipids, and the histopathological changes in the earthworm integument were examined. The study indicated that the UVR-exposed earthworm skin homogenate produced a significant amount of ROS, such as singlet oxygen (1O2), , , and photooxidized lipids. The authors concluded that the earthworm could be a simple, sensitive, and cost-effective test organism for assessing the hazard potential of solar radiation and also for planning safety measures for humans.

Thus, it is likely that the biological features of the earthworm are useful as biomonitors to estimate the oxidative damage that could occur in humans.

5. 8-Oxoguanine and Earthworms

Recent research has indicated that the earthworm is a candidate organism as a biomonitor for soil contaminants, because it plays an important role in the soil macrofauna biomass. The species E. fetida is most commonly used in ecotoxicology, as a useful biomonitor for soil [33]. In particular, this species’ proximity to the soil contaminants is a merit for the analysis [34, 35]. Among the many kinds of organisms living in soil, the earthworm is the most useful organism for the evaluation of metal contamination, because significant positive correlations have been found between the metal concentrations in the earthworm and the soil Cd, Cu, Pb, Zn, and Hg concentrations [9, 3639].

We recently analyzed the 8-oxo-Gua accumulated in the DNA of E. fetida exposed to heavy metals, to determine if a method using earthworms as a biomonitor is useful for the assessment of soil mutagenicity [18]. We employed Cd and Ni as test metals, because the carcinogenic potentials of Cd and Ni have been established for humans and animals [40, 41], and these metals are known to generate 8-oxo-Gua in DNA [20, 4244].

In the study, E. fetida were kept in a 20-liter stainless steel tank at an ambient temperature of 24°C, using a mold with skim milk as a food source until heavy metal exposure. Three to six individuals were kept in a 600 mL glass container containing 50 g of soil with/without heavy metal. They were exposed to 10 or 200  g heavy metal/g soil for 1, 2, and 3 weeks or to 10  g heavy metal/g soil for 3 months (Figure 2). As a result, we detected a high level of Cd accumulation in E. fetida (Figures 3(a) and 3(c)). On the other hand, no Ni accumulation was observed (Figures 3(b) and 3(c)).

726946.fig.002
Figure 2: Experimental design. Metals (0, 0.5, or 10 mg as Cd or Ni) were added to 50 g soil in a 600 mL glass container. After 0-, 1-, 2-, 3-week, and 3 month exposures, E. fetida were cut into four rough segments (S1–S4). S1: head region, S2: anterior body region, S3: posterior body region, S4: tail region.
fig3
Figure 3: Heavy metal accumulation in E. fetida. Each data point represents the mean of three individuals. Heavy metal concentrations were measured by atomic absorption spectrometry, and are expressed as g per body weight. (Data are modified by Nakashima et al. [18]).

In addition, we observed positive staining of 8-oxo-Gua in the gut epithelial layers in almost all samples (Figures 4(a)4(f)). The metal absorption routes include the digestive system and the surface wall [45, 46], but the main route is the digestive system. Since gut epithelial layers are frequently exposed to ROS, 8-oxo-Gua accumulation was constantly detected. Although the 200  g Cd-exposed E. fetida showed relatively stronger signals (P1+++ in Table 2) at 2 weeks in comparison to the others, this did not seem to be significant evidence, because almost all of the specimens showed positive signals in the gut epithelial layers and the difference in the signal strength was too small to conclude that Cd exposure increased 8-oxo-Gua accumulation in the organs. On the other hand, the positive signals in the seminal vesicles were clearly detected only in E. fetida treated with 10  g of Cd for 3 months (Figure 4(h)). The seminal vesicles are considered as metallothionein-(MT-)poor organs. Therefore, it seems reasonable to speculate that a lower level of MT expression is involved in Cd-induced DNA damage accumulation.

tab2
Table 2: Profiling of immunohistochemical analyses of 8-oxo-Gua accumulation in E. fetida.
fig4
Figure 4: Immunohistochemical analyses of 8-oxo-dG accumulation in the gut epithelial layers and seminal vesicles (SV) of E. fetida (S1). Controls for the gut epithelial layer: 1 week (a), 2 weeks (c), 3 weeks (e). The gut epithelial layer of the Cd (200  g/g soil) treatment group: 1 week (b), 2 weeks (d), 3 weeks (f). (g) Negative staining of Cd (200  g/g soil, 1 week) with a 2% bovine serum albumin solution. Arrowheads show the gut epithelial layer. AC: alimentary canal. (h) The SV. Arrowheads show positive signals in SV. All scale bars are 100  m. (Data of (h) are modified by Nakashima et al. [18]).

6. Conclusions

In our recent study, we observed a high level of Cd accumulation and no Ni accumulation in E. fetida, accompanied with an increase in 8-OH-dG accumulation in the organs of Cd-exposed E. fetida. Based on these results, it is reasonable to conclude that the increase in 8-OH-dG accumulation is due to Cd accumulation.

Taken together, we demonstrated the possible utility of using earthworms as biomonitors, by measuring the oxidative DNA damage generated in the earthworms, as a biomonitoring method for assessing soil mutagenicity. However, many points remain unresolved. For example, this method could be reliable only for bioaccumulated metals, such as Cd, but not for non-bioaccumulated metals, such as Ni, even if they generate 8-oxo-Gua. To establish a broader biomonitoring method using earthworms to assess soil mutagenicity, further studies will be required.

Acknowledgments

The authors would like to thank Dr. Tamiji Nakashima, University of Occupational and Environmental Health, Japan, for his contribution, and Prof. Natchimuthu Karmegam, the editor-in-chief of Applied and Environmental Soil Science, for providing the opportunity to write this paper. This work was supported by a grant from The Foundation for Earth Environment.

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