Isolation and identification of Vibrio parahaemolyticus from seawater and sediment samples in the southern coast of the Caspian Sea.

The objectives of this study were to investigate the occurrence of Vibrio parahaemolyticus in the seawater and its sediment by molecular techniques and conventional microbiological methods. Of 300 samples analyzed, 20.3 % was recorded positive for V. parahaemolyticus. Of the 62 strains isolated, 26 (8.3 %) were obtained from the seawater samples, and 36 (12 %); from sediments. Only three strains (4.83 %) showed hemolytic activity in Wagatsuma agar. The results of this study demonstrated the presence of V. parahaemolyticus in the southern coast of the Caspian Sea (Northern Iran). Furthermore, the PCR approach proved useful for reliable confirmation of species identification. V. parahaemolyticus is an important human pathogen responsible for food-borne gastroenteritis worldwide. These findings indicated the potential sanitary risk associated with the presence of pathogenic V. parahaemolyticus in the Caspian Sea.

Introduction

Vibrio parahaemolyticus is a human pathogen that is widely distributed in the marine environments. It has a single polar flagellum and is motile when grown in liquid medium (Broberg et al. 2011). V. parahaemolyticus is a marine bacterium easily recovered from estuarine and coastal waters worldwide, as well as from seawater (Hayat et al. 2006). V. parahaemolyticus requires presence of salinity with optimum levels of 1–3 % to survive and multiply, which is in the range of 0.8–3 % levels commonly found in marine environments (Yeung and Boor 2004). V. parahaemolyticus causes three major syndromes of clinical illness, i.e., gastroenteritis, wound infections, and septicemia. Gastrointestinal illness caused by V. parahaemolyticus is typically accompanied by symptoms including vomiting, diarrhea, headache, nausea, low-grade fever, and abdominal cramps, and is commonly self-limiting. The mean incubation period for V. parahaemolyticus infection is 15 h (Nair et al. 2007). Clinical isolates of V. parahaemolyticus most often produce either the thermostable direct hemolysin (TDH) or TDH-related hemolysin (TRH) encoded by tdh and trh genes, respectively. However, only bacteria producing virulence factors, i.e., TDH and/or TRH, are considered to be pathogenic and can cause acute gastroenteritis (or, more rarely, invasive septicemia) (Bisha et al. 2012). TDH is capable of producing β hemolysis on Wagatsuma agar which is called Kanagawa phenomenon (KP). Most of the strains (90 %) isolated from clinical cases show this type of hemolysis, while only 1–2 % of the strains of environmental origin are KP positive (Drake et al. 2007). TRH is another virulence factor that has been discovered in clinical strains lacking tdh gene. TRH is a 23-kDa protein, immunologically related to TDH and environmental strains producing this gene, and produces urease (Pal and Das 2010). Epidemiological studies have revealed an association between the Kanagawa phenomenon and gastroenteritis (Okuda et al. 1997). The objectives of the present study are, first, to determine the prevalence of total and pathogenic V. parahaemolyticus in seawater and sediment in the southern coast of the Caspian Sea and, second, to investigate the relationships with water temperature and salinity. The strains isolated were screened for hemolytic activity and for the presence of the tdh and trh genes. A limitation of the research was the long distance between the sampling sites and the laboratory.

Materials and methods

The seawater samples and sediments were collected at a depth of 50 and 10–20 cm, respectively, by aseptic techniques. Of the 300 total samples, 150 seawater and 150 sediment samples were collected from seven different sites in the Caspian Sea in April, May, June, July, and August (Fig. 1).

Fig. 1

Area of study and locations of the sampling sites in the southern coast of the Caspian Sea (Northern Iran). Site 1 Bandar Torkaman, site 2 Sari, site 3 Noor, site 4 Chalus, site 5 Ramsar, site 6 Chamkhaleh, site 7 Bandar Anzali

The samples were placed in sealed containers with dry ice and transported frozen to the laboratory for analysis. The time between sample collection and analysis was approximately 24 h, while sampling, water temperature, and salinity were measured.

V. parahaemolyticus isolation and identification

Twenty-five milliliters of seawater samples and 25 g of sediment samples were added to 225 ml of alkaline peptone water (APW) containing 1 % NaCl (pH 8.6), and 10−2 and 10−3 APW dilutions were prepared in duplicate and incubated at 37 °C for 6–24 h. Enrichment broth was streaked onto thiosulfate-citrate-bile salts-sucrose agar plates and incubated at 37 °C for 18–24 h. The green or blue-green colonies were presumptively selected as V. parahaemolyticus colonies and transferred to trypticase soy agar plate containing 3 % NaCl. After incubation at 37 °C for 24 h, the isolates were tested using conventional bacterial methods, including Gram's staining, culture sulfide indole motility and triple sugar iron tests media, cytochrome oxidase activity tests, lysine iron agar tests, urea tests, and tests for arabinose, lactose, mannitol, mannose, and sucrose fermentation (Colakoglu et al. 2006).

Hemolytic activity

Kanagawa test was performed using Wagatsuma agar supplemented with 5 % human erythrocytes. Each plate was inoculated with V. parahaemolyticus strains. Positive reactions were recorded as a zone of β hemolysis surrounding the spot of growth on the human blood plate. The interpretation times for the test were 24, 48, and 72 h (Canizalez-Roman et al. 2011).

DNA purification

V. parahaemolyticus strains were seeded in Luria–Bertani agar supplemented with 1 % NaCl and incubated at 37 °C for 24 h. Five colonies were selected, resuspended in 100 μl of filtered sterile distilled water, and boiled for 15–20 min to liberate the nucleic acid (Cabrera-Garcia et al. 2004).

Confirmation of strains by polymerase chain reaction

The tdh and trh genes were amplified with the following primer sets: 5′-GTAAAGGTCTCTGACTTTTGGAC-3′ and 5′-TGGAATAGAACCTTCATCTTCACC-3′ for tdh, and 5′-TTGGCTTCGATATTTTCAGTATCT-3′ and 5′-CATAACAAACATATGCCCATTTCCC-3′ for trh (Tada et al. 1992). These primer sets produced 251- and 373-bp amplicons, respectively. The reaction mixtures (final volume, 25 μl) contained 3 μl of the solution containing DNA, 2.5 μl of 10× reaction buffer, 4 μl of 25 mM MgCl2, 1 μl of Taq polymerase (5 U/μl), 4 μl of deoxynucleoside triphosphates (1 Mmol), 1 μl of each primer (20 pmol), and 8.5 μl of distilled water. The reactions were performed as follows: initial denaturation at 94 °C for 1 min, followed by 35 cycles of denaturation at 94 °C for 1 min, annealing at 55 °C for 1 min, extension at 72 °C for 1 min, and a final extension at 72 °C for 7 min. Positive and negative DNA controls were included in all assays. The amplified products were separated by electrophoresis in ethidium bromide-stained 2 % agarose gels in Tris–borate–EDTA buffer at 120 V for 30 min. The gels were visualized with a UV transilluminator.

Results

A total of 300 samples were analyzed; these samples included 150 seawater and 150 sediment samples. Overall, V. parahaemolyticus strains were isolated from 20.3 % of the samples (Table 1). The highest isolation rate of V. parahaemolyticus was observed in August, with a total of 23 positive samples (28.3 %). The temperatures ranged between 34 and 39 °C during the sampling period. By contrast, the lowest isolation rate of V. parahaemolyticus was observed in April, with a total of 3 positive samples (5 %). The temperature of the seawater ranged from 10 to 15 °C during the sampling period. Salinity was highest in summer (19 ppt), whereas the minimum levels were recorded during the spring (2 ppt). The average salinity was 10.5 ppt during the sampling period.

Table 1

Occurrence and the frequency of V. parahaemolyticus in the seawater and sediment

Month	April						May						June						July						August						Total frequency
Source	W		S		W + S		W		S		W + S		W		S		W + S		W		S		W + S		W		S		W + S
Sites	Frequency
	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%	N	%
Site 1	–	–	1	1.6	1	1.6	1	1.6	1	1.6	2	3.3	–	–	–	–	–	–	–	–	2	3.6	2	3.6	1	1.6	3	5	4	6.6	9	3
Site 2	–	–	1	1.6	1	1.6	–	–	–	–	–	–	1	1.6	1	1.6	2	3.3	–	–	1	1.6	1	1.6	–	–	2	3.6	2	3.6	6	2
Site 3	–	–	–	–	–	–	–	–	1	1.6	1	1.6	–	–	2	3.3	2	3.3	1	1.6	1	1.6	2	3.6	–	–	2	3.6	2	3.6	7	2.3
Site 4	1	1.6	–	–	1	1.6	1	1.6	1	1.6	2	3.3	–	–	1	1.6	–	–	3	5	2	3.6	5	8.3	2	3.6	2	3.6	4	6.6	13	4.3
Site 5	–	–	–	–	–	–	–	–	1	1.6	1	1.6	1	1.6	1	1.6	2	3.3	3	5	1	1.6	4	6.6	4	6.6	2	3.6	6	10	13	4.3
Site 6	–	–	–	–	–	–	–	–	–	–	–	–	1	1.6	1	1.6	2	3.3	–	–	–	–	–	–	1	1.6	1	1.6	2	3.6	4	1.3
Site 7	–	–	–	–	–	–	1	1.6	1	1.6	2	3.3	2	3.3	1	1.6	3	5	–	–	2	3.6	2	3.6	2	3.6	1	1.6	3	5	10	3.3
Total	1	1.6	2	3.3	3	5	3	5	5	8.3	8	13.3	5	8.3	7	11.6	11	18.3	7	11.6	9	15	16	26.6	10	16.6	13	21.6	23	28.3	62	20.3

W water, S sediment

The highest prevalence of V. parahaemolyticus was detected at sampling sites 4 (4.3 %) and 5 (4.3 %). Of the 62 strains isolated, 26 (8.3 %) were obtained from seawater samples and 36 (12 %) from sediments. Only three strains (4.83 %) showed hemolytic activity in Wagatsuma agar. Only two of the 62 strains (2.53 %) amplified the 250-bp tdh gene fragment, which correlated with positive hemolytic activity. The trh gene fragment was amplified in four (5.06 %) of the strains analyzed.

Discussion

In the present study, we demonstrated the presence of V. parahaemolyticus in 20.3 % of the seawater and sediment samples analyzed. This study was the first research to investigate the isolation and distribution of this pathogen in the southern coast of the Caspian Sea. Cabrera-Garcia et al. (2004) reported that 15 % of the seawater samples contained V. parahaemolyticus. This pathogen has also been isolated in Canada (Kelly and Stroh 1988), France (Hervio-Heath et al. 2002), Asia (Alam et al. 2002), and the USA (DePaola et al. 2003). In the present study, of the 62 strains isolated, 26 (8.3 %) were obtained from seawater samples and 36 (12 %) from sediments. Velazquez-Roman et al. (2012) have reported that of the 144 strains isolated, 35 % was obtained from seawater samples and 16 % from sediment. Thus, it is speculated that the observed prevalence may also be produced by seasonal variation of the V. parahaemolyticus population due to salt and oxygen concentrations, interactions with the plankton, the presence of sediment, and the organic matter in the suspension, fish, and seafood. In one study, it was observed that the maximum probability of V. parahaemolyticus detection was around 25 ppt salinity (Martinez-Urtaza et al. 2008). The other reason for the low prevalence of V. parahaemolyticus in the southern coast of the Caspian Sea (the average salinity is 10.5 ppt) is its lower salinity than other seas. The distribution of V. parahaemolyticus in the marine environments is known to be related to the water temperatures. Studies have shown that the organism was rarely detected in seawater until water temperatures rose to 15 °C or higher. Ecological study of V. parahaemolyticus in the Chesapeake Bay of Maryland (USA) found that the organism survived in sediment during the winter and was released from sediment into water column when water temperatures rose to 14 °C in late spring or early summer (Kaneko and Colwell 1978). The isolation rate of V. parahaemolyticus was high (28.3 %) in August because a higher rate of evaporation results in high salinity. In one study, it was observed that only two pathogenic V. parahaemolyticus were confirmed in environmental samples. The extremely low presence of pathogenic populations of V. parahaemolyticus in environmental samples is a constant characteristic in most of the investigations carried out in different regions of the world (Martinez-Urtaza et al. 2008). The results of current investigation are consistent with previous reports. We observed positive tdh gene amplification in two of the 62 strains analyzed, which was correlated with the positive hemolytic activity in Wagatsuma agar (KP+). Virtually, all clinical isolates of V. parahaemolyticus are KP+, whereas only 1–2 % of environmental strains are KP+ (Drake et al. 2007). This implies that there is a source of human fecal contamination in the seawater and sediment of the southern coast of the Caspian Sea. This information may be important for preventing sanitary problems that may affect the health of the population. In conclusion, this study provided new information on the abundance of V. parahaemolyticus in seawater and sediment samples in the southern coast of the Caspian Sea. The data presented in the present study show the presence of pathogenic V. parahaemolyticus and suggest the need for a study of such organism in seafood in the Caspian Sea.