Abundance of the bacteria Listeria during the great rainy and dry seasons in some wells and lake waters in an urbanized equatorial zone of Cameroon (Central Africa)

Authors: Paule Jovanie Atou’ou1 and Yves Poutoum Yogne1 and Pélagie Ladibé1 and Florence Donnadieu-Bernard2 and Geneviève Bricheux2 and Philippe Bouchard2 and Télesphore Sime-Ngando2 and Moïse Nola1

Journal Name: Environmental Reports; An International Journal

DOI: https://doi.org/10.51470/ER.2026.8.2.01

Keywords: Listeria abundance, wells and lake water, dry season, rainy season, ecological factors

Abstract

Abundance of the bacteria Listeria during the great rainy and dry seasons in some wells and lake waters in an urbanized equatorial zone of Cameroon (Central Africa)
Bacteria of the Listeria genus are zoonotic pathogens responsible for listeriosis. This study aimed to investigate the abundance of Listeria in wells and lakes waters during the major rainy and dry seasons and assess the health risks faced by users. Samplings were carried out monthly on 4 wells and 4 lake water stations. Bacterial abundance was assessed using selective agar culture media. Physicochemical analyses indicated that wells are slightly acidic, contain lower dissolved dioxygen concentrations and higher content in dissolved CO2 levels than lake water, which was predominantly alkaline. In wells, abundance of Heterotrophic aerobic mesophilic bacteria (HAMB) varied from 2×104 to 89×105 CFU/100 mL during the rainy season, and from 4×104 to 8×105 CFU/100 mL during the dry season. That of Listeria varied from 6 to 14.5×102 CFU/100 mL during the rainy season, and from 1.28×102 to 20.5×102 CFU/100 mL during the dry season. In lakes, abundance of HAMB varied from 24×103 to 36×105 CFU/100 mL during the rainy season, and from 26×103 to 16×105 CFU/100 mL during the dry season. That of Listeria ranged from 40 to 4×102 CFU/100 mL during the rainy season, and from 98 to 41×102 CFU/100 mL during the dry season. Abundance of Listeria was negatively correlated with the water pH in wells during the rainy season, whereas with dissolved oxygen in lake during the dry season (P≤0.05). Dissolved CO2 seemed to favor Listeria abundance in lake during the dry season (P≤0.05). No significant difference in Listeria abundance was found between the rainy and dry season (P>0.05). The survival of Listeria in aquatic environment would greatly depend on factors other than those considered in this study. Despite the relative temporal variations in the abundance of the bacterial contaminant, the risk of listeriosis associated with the analyzed water appears unchanged with the season change.

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1. INTRODUCTION

   Aquatic bacteria play a crucial role in human health, contributing to the decomposition of organic matter, nutrient cycling, and water purification, but they can also be pathogenic and cause infections [1]. Listeriosis is a zoonotic, waterborne infectious disease of human origin, primarily caused by a bacterium of the genus Listeria monocytogenes, a species pathogenic to humans and animals, and widespread in nature [2]. It is transmitted by ingestion of contaminated water and mainly affects people with weakened immune systems [3]. These bacteria, once they colonize the intestines of their hosts, are released into the bloodstream by monocytes and multiply in target organs, namely the liver and spleen [4].

   Bacteria of the genus Listeria are of particular properties. They are Gram-positive bacilli, that can live alone, in chains, or in pairs in a V shape. They are often mobile due to the peritrichous cilia when grown between 20 and 25°C, and immobile at 37°C. They are neither spore-forming nor encapsulated and are capable of growing under aerobic or anaerobic conditions [5,6,7]. Biochemically, Listeria strains are catalase-positive, oxidase-negative, and hydrolyze esculin without producing gas. They ferment many carbohydrates such as glucose, fructose, mannose, salicin, cellobiose, maltose, trehalose, and D-arabitol in 24 hours. The genus Listeria comprises 17 species, among which six species are more frequent: Listeria monocytogenes, L. ivanovii, L. seeligeri, L. innocua, L. welshimeri and L. grayi [5,6,7]. Their biotopes include soil, natural and urban environment, plats, surface and ground water [8]. According to other authors, the contamination of surface and ground water may mostly originate from contaminated sewage or wastewater [9,10].

   Water is one of the essential nutrients for every human being [7]. Water commonly used by humans can be groundwater or surface water. Groundwater is often accessed through wells and boreholes. Surface water includes rivers and lakes. These three types of aquatic systems (well water, rivers, and lakes) function differently due to differences in flow velocities, chemical properties, and interactions with environmental factors. Furthermore, it is often said that the seasons, which are often determined by meteorological factors, impact the microbiological functioning of aquatic ecosystems.

   Many studies have already been conducted on various aquatic biotopes in Yaoundé, Cameroon. These studies have revealed that these waters harbor a diverse bacterial microflora composed of, among others, Pseudomonadaceae, Aeromonadaceae, Vibrionaceae, and Enterobacteriaceae [11,12], Their abundance dynamics are influenced by meteorological factors as well as factors related to bacterial species [13,14], Their transfer from the soil surface to the water table is influenced by various elements, some of which are related to the bacteria themselves, including the shape of the bacterial cell wall, the physiological state of the bacteria, and the presence or absence of surface appendages [15]. Other factors are related to the physicochemical and hydrological properties of the infiltrating waters [16].

   However, few studies have been conducted on bacteria belonging to the genus Listeria. Very little is known about the impact of seasonal variation on Listeria abundance dynamics, as well as the influence of ecological factors on Listeria distribution in the city of Yaoundé (Cameroon).



 

In the equatorial zone of Cameroon, the climate comprises four distinct seasons: a short rainy season from mid-March to mid-June, a short dry season from mid-June to mid-August, a long rainy season from mid-August to mid-November, and a long dry season from mid-November to mid-March of the following year. During the long rainy season, runoff can carry numerous pollutants into both surface and underground aquatic ecosystems, potentially impacting their microbial quality. It is often stated that seasonal variation is one of the factors influencing the microbiological functioning of aquatic ecosystems [17,18,19]. Meteorological factors determine the distribution of the seasons which in turn influence the infiltration of runoff into the soil. This process can transport a significant number of substances into aquatic ecosystems, both groundwater and surface water, that may impact the microbiological quality of the biotope [20,21].

Little is known about the differences or similarities that may exist in the abundance of a given bacterium in different water systems within the same geographic area during the same season or from one given season to another. This study aimed at assessing the abundance of Listeria in wells and lake water during the main rainy season and the main dry season in Yaoundé (Cameroon, Central Africa), and the potential impact of some abiotic factors.

 

2. MATERIALS AND METHODS

2.1. Description of the water sampling sites

The city of Yaoundé is located on the western edge of the South Cameroon Plateau, between 3°90’ North latitude and 11°50’ East longitude, specifically 300 km from the Atlantic coast, and covers an area of 304 km² [22]. Yaoundé’s hydrographic network is very diverse, consisting of streams, rivers, lakes, and ponds [23]. This explains the variety of water sources available to the population. Temperatures range from 18°C to 28°C during the wet season and from 16°C to 31°C during the dry season, with an estimated annual average of 23.5°C and an annual temperature range of 2.4°C. Average rainfall is 1564.7 mm per year, or an average of 153 days per year. Frequent winds are humid and blow from the Southwest [24].

            The study included four groundwater points and four water stations on two lakes. The groundwater points were coded Wells-1, Wells-2, Wells-3, and Wells-4. The stations on each lake were coded Lake1-Upst, Lake1-Down, Lake2-Upst, and Lake2-Down. The location of all these water points is shown in Figure 1. Similarly, the geographic coordinates for each point are recorded in Table 1.

Meteorological data for the sampling period were downloaded from the NASA website (https://power.larc.nasa.gov/data.access.viewer/). During this study, precipitation ranged from 0.01 to 7.34 mm/day. Air temperature ranged from 22.93 to 27.67°C. Relative humidity ranged from 60.53 to 88.27%, and solar irradiance from 3.15 to 4.96 kWh/m²/day. The temporal variations of these data are shown in Figure 2.

 
 
 

2.2. Sampling

This study was carried out from September 2025 to February 2026, a period including the long rainy season and the long dry season. It consisted of taking and analyzing water samples on a monthly basis. The water samples were collected in 250 mL and 1000 mL double-capped polyethylene bottles for physicochemical analyses, and in sterile 500 mL glass bottles for bacteriological analyses.

2.3. Physicochemical analyses

The physicochemical parameters considered were pH, electrical conductivity, carbon dioxide, dissolved oxygen, nitrogen ammonia, nitrate and nitrite ions, and calcium and magnesium hardness. These analyses were performed according to the standard techniques [25]. Some parameters were measured and/or fixed in the field. Subsequently, the samples were transported to the laboratory in a temperature-controlled cooler [26].

2.4. Bacteriological analyses

   Bacteriological analyses consisted of isolating and enumerating heterotrophic aerobic mesophilic bacteria (HAMB) and bacteria belonging to the genus Listeria. For the enumeration of HAMB in lakes, 1mL of sample was diluted 1:100, and then 100µL of water sample (lakes and wells) was inoculated using the surface-spreading technique on ordinary agar. The Petri dishes were then incubated at 24 ± 2°C for 5 days [27]. Each analysis was performed in triplicate.

            Listeria bacteria were detected and isolated on Listeria Oxford Agar Base supplemented with antibiotics (cyclohexymide, colistin sulfate, acriflavin, cefotetan, and phosphomycin sodium salt)[28]. Lake water samples were analyzed by surface spreading on the agar, while groundwater samples were analyzed by membrane filtration using a cellulose acetate membrane with a pore size of 0.45 µm. Analyses were performed in triplicate. Petri dishes were then incubated at 37°C ± 1°C for 24 to 48h ± 2h. The isolated colonies were counted using the direct colony count method. Mean bacterial abundances were calculated and expressed as Colony Forming Units (CFU)/100 mL of analyzed water.

2.5. Data analysis

The mean values of abundances of the isolated bacteria were expressed in CFU/100 mL of water sample. The relationships between the considered parameters were assessed using Spearman’s correlation test. A comparison of cell abundances between different stations was made using the Mann-Whitney U test.

 

3. RESULTS

3.1. Physicochemical characteristics of waters samples

 The values of the abiotic parameters are presented in Figure 3 and Figure 4. This shows a spatio-temporal fluctuation of the values of each parameter, whether in lakes or in wells respectively.

3.1.1. Physicochemical parameters in Lakes

   The pH ranged from 7.3 to 10.76 U.C. (Figure 3). Dissolved CO2 levels fluctuated from 0.17 to 80.96 mg/L. The lowest value was recorded in Lake L2-Upst in December, while the highest was observed in Lake L1-Upst in November. Dissolved oxygen levels ranged from 0.27 to 7.99 mg/L. The highest value was recorded in Lake L1-Down in February, while the lowest was observed in Lake L1-Upst in January (Figure 3).

Electrical conductivity ranged from 212 to 474 μS/cm, with the lowest value recorded in Lake L2-Down in October and the highest in Lake L1-Upst in September. Calcium hardness fluctuated from 0.01 to 3.97 mg/L of CaCO3 with the highest value noted in Lake L1-Upst in November and the lowest value recorded in lake L2-Upst in February (Figure 3). Magnesium hardness ranged from 0.05 to 6.32 mg/L CaCO3, nitrite ion levels from 0.01 to 1.6 mg/L, nitrate ion levels from 0.06 to 8.2 mg/L, and ammonia nitrogen levels from 0.19 to 2.58 mg/L (Figure 3).

Mean values for abiotic parameters were calculated for all lakes. They were 8.23±0.83 U.C for pH, 23.84±19.52 mg/L for CO2, 3.74±2.29 mg/L for dissolved oxygen, 305.79±82.38 μS/cm for electrical conductivity, 1.48±1.08 mg/L of CaCO3 for calcium hardness, 2.04±1.38 mg/L of CaCO3 for magnesium hardness, 0.17±0.42 mg/L for nitrite, 1.39±1.64 mg/L for nitrate and 1.16 ± 0.61 mg/L for nitrogen ammonia.

3.1.2. Physicochemical parameters in wells

The pH ranged from 5.5 to 7.83 U.C. (Figure 4). The electrical conductivity ranged from 311 to 776 μS/cm. The concentrations of dissolved CO2, dissolved oxygen, calcium hardness, and magnesium hardness ranged from 14.08 to 117.92 mg/L, 3.06 to 5.62 mg/L, 0.01 to 4.88 mg/L, and 0.01 to 2.53 mg/L of CaCO3, respectively (Figure 4). Regarding nitrogen compounds, the concentrations ranged from 0.01 to 0.26 mg/L for nitrite, from 0.03 to 7.6 mg/L for nitrate, and from 0 to 4.32 mg/L for ammonia nitrogen (Figure 4).

The average values of the abiotic parameters were calculated for all analyzed well water points. They were 6.51±0.62 U.C. for pH, 64.36±27.51 mg/L for dissolved CO2, 4.33±0.73 mg/L for subsurface oxygen, 438.21±169.11 μS/cm for electrical conductivity, 1.73±1.52 mg/L of CaCO3 for calcium hardness, 1.01±0.73 mg/L of CaCO3 for magnesium hardness, 0.032±0.053 mg/L for nitrite, 1.86±0.083 mg/L for nitrate, and 1.83±2.08 mg/L for ammonia nitrogen.       

3.2. Bacterial abundance in water samples

The variation in the abundance of heterotrophic aerobic mesophilic bacteria (HAMB) and Listeria recorded in wells and lakes is shown in Figure 5. In wells, HAMB abundances ranged from 2×10⁴ to 89×105 CFU/100 mL. The lowest value was observed in well-3 in November, while the highest was obtained in well-4 in October (Figure 5). Listeria bacteria abundances fluctuated from 0.06×10² to 22.8×10² CFU/100 mL. The lowest value was obtained in well-3 in October, while the highest abundance was obtained in well-4 in December (Figure 5). Overall, it can be noted that abundance of Listeria in wells varied from 6 to 14.5×102 during the rainy season, and from 1.28×102 to 20.5×102 CFU/100 mL during the dry season. The abundance of Heterotrophic aerobic mesophilic bacteria (HAMB) varied from 2×104 to 89×105 CFU/100 mL during the rainy season, and from 4×104 to 8×105 CFU/100 mL during the dry season.

In lake waters,HAMB abundances ranged from 2.4×10⁴ to 333×10⁴ CFU/100 mL. Listeria abundances fluctuated from 38 to 41×10² CFU/100 mL (Figure 5). The lowest value was recorded in Lake L1-Down in October, while the highest abundance was recorded in Lake L1-Upst in January (Fig. 5). Overall, in can be noted that abundance of Listeria varied from 40 to 4×102 during the rainy season, and from 98 to 41×102 CFU/100 mL during the dry season. The abundance of HAMB varied from 24×103 to 36×105 CFU/100 mL during the rainy season, and from 26×103 to 16×105 CFU/100 mL during the dry season.

3.3. Correlations amongst the considered parameters

The Spearman correlation coefficients have been calculated between the bacterial abundances and the abiotic parameters considered. This has been done between the collected data.

3.3.1. Correlations between physicochemical parameters and bacterial abundances

During the rainy season, a significant negative correlation (P≤0.01) was observed between Listeria densities and water pH (Table 2). Significant negative correlations were also observed between HAMB abundances and dissolved O2 (P≤0.01) and nitrite (P≤0.01). However, a significant positive correlation (P≤0.05) was observed between HAMB and ammonia nitrogen (Table 2).

During the dry season, significant negative correlations (P≤0.05) were observed between HAMB abundance, dissolved O2, ammonia nitrogen, and calcium (Table 2). However, no significant correlation was observed between Listeria densities and the abiotic factors considered.

3.3.2. Correlations between meteorological parameters and bacterial abundances of Listeria and HAMB

Correlation coefficients were calculated between meteorological factors and bacterial abundances (Table 3). In groundwater, during the rainy season, HAMB abundance are negatively correlated with temperature and insolation (P≤0.01) and positively correlated with rainfall and humidity (P≤0.01) in wells. In this biotope, Listeria densities are negatively correlated with rainfall and humidity (P≤0.05). In lakes waters, Listeria and HAMB are sometimes negatively or positively correlated with the considered meteorological factors (Table 3). The variability in correlation between meteorological factors and Listeria and HAMB, is also observed during the dry season whether considering wells or lake water (Table 3).

3.4. Comparison among the considered factors

Bacterial abundances and physicochemical parameters across all wells and lake sampling stations were compared using the Mann-Whitney U test. The results show that, in both the rainy and dry seasons, and in both lakes and wells, electrical conductivity and nitrogen ammonia varied significantly between sampling sites (P≤0.05) (Table 4). Bacterial abundances do not vary significantly between sites during either the rainy or the dry season (P>0.05) (Table 4).

Using the Mann-Whitney U test, bacterial abundances and physicochemical parameters in each type of biotope were compared between the dry and rainy seasons. It revealed that electrical conductivity, nitrogen ammonia, and magnesium concentrations vary significantly from one season to another in lakes and wells (P≤0.05) (Table 5). Carbon dioxide varies significantly in the lakes from the dry to the rainy season (P≤0.05). Bacterial abundances do not vary significantly between the rainy and the dry season (P>0.05) (Table 5).

4. DISCUSSION

The pH values of analyzed water samples ranged from 6 to 8 in most cases. This slight alkalinity in lakes could be due to the combined action of carbonate precipitation and photosynthesis through the consumption of carbon dioxide [29], while their values in groundwater could be linked to the soil mineralogy [30]. In Yaounde town, the bedrock is rich in minerals such as magnesium, potassium, and calcium, whose weathering can influence groundwater pH. It has also been established that the acidity of groundwater in urban areas could result from organic pollution [31]. More recent investigations in Cameroon corroborate this anthropogenic control. Using a multi-tracer approach on hard-rock aquifers, some authors showed that processes govern water quality in lateritic hillside areas, whereas anthropogenic inputs, mainly nitrate accumulation linked to human activity, predominate in valleys and on slopes [32]. These values correspond to the tolerance range of the majority of aquatic living organisms [33].

The electrical conductivity in lake water and groundwater indicated moderate mineralization. It is indicated that the mineralization of groundwater is primarily due to vertical movements that bring up mineralized fluxes from deeper layers [34]. This could also be due to human activity, and the said activity is influenced by the biodegradable organic matter which therefore reflects the level of pollution [35].

Bacteriological analysis of well and lake water samples revealed that these waters harbor a diverse bacterial community. The HAMB bacteria were present in all sampling points during the study period. The average bacterial abundance of HAMB in groundwater was higher than in lake water. This could be due to the fact that the environment surrounding the sampling points is conducive to their development, particularly due to an abundant source of mixed pollution, contaminated runoff, and infiltration. It has been indicated that surface and groundwater contamination depends on the pollutant load and the permeability of the overlying soil [20]. In this study, ammonia nitrogen appears to promote the emergence of total microflora in the studied sites.

The abundance of HAMB was relatively higher than that of Listeria. Listeria strains abundance in wells were relatively greater than lake water samples. This predominance could be explained by their ubiquitous nature and their ability to survive in harsh conditions. Listeria bacteria are widespread in nature; only their abundance varies from one environment to another [4]. The low abundances observed in lakes would indicate very low levels of biological and organic pollution, while the highest concentrations obtained could be linked to point sources of pollution identified near the sampling sites, to multiple inputs from runoff and infiltration, or to the resuspension of these bacteria by rain [36]. This point-source pattern mirrors more recent surveys of environmental waters. Multidrug-resistant and biofilm-forming Listeria cells have been reported across rivers, wastewater, and irrigation water in comparable proportions [37].

The spread of Listeria in nature is exacerbated by certain ecological factors. In this study, factors such as temperature and insolation positively influenced the population of Listeria, while water pH and relative humidity negatively impacted bacterial density. It is indicated that Listeria bacteria have the ability to resist or thrive in saline and acidic environments [36]. This ubiquity allows them to develop numerous adaptation mechanisms to the unfavorable conditions present in the ecological hosting niches. Physiological works have clarified the molecular basis of this acid resilience, describing an acid tolerance response, together with glutamate decarboxylase, arginine de-aminase, and F1F0-ATPase systems that buffer the bacterium’s internal pH and allow cross-protection against related stresses such as bile salts and osmotic pressure [38]. This reinforces the hypothesis that the water pH recorded could act as a limiting factor rather than an eliminating factor for the pathogen [39].

Regarding the impact of seasonal factors on the HAMB abundance, the distribution of these germs during the study period did not take into account seasonal variation or ecosystem type ; they grow everywhere in search of vital resources. In the aquatic environment in general, multiple microorganisms coexist as communities competing for resources [20]. Similarly, Listeria bacteria, described as ubiquitous, do not take into account seasonal factors or biotope type. This is due to the ability of this pathogen to survive and grow in dry, cold, and high-salt environments. The bacterium can easily grow in different food matrices kept in the refrigerator. Listeria can adapt to the conditions of the gastrointestinal tract by overcoming unsuitable conditions of this microenvironment, including acidity, osmolality, low oxygen, and the antimicrobial effect of bile salts and peptides [7]. This capacity to withstand acid, cold, and osmotic stress simultaneously is now considered a hallmark of the species environmental persistence and a key factor in its recurrent detection in food-linked and aquatic environments alike [40].

A comparison between the dry and rainy seasons reveals that electrical conductivity and nitrogen ammonia vary significantly in both wells and lakes. This marked seasonal dynamic regarding mineralization and nitrogenous compounds aligns with the findings of some authors who linked such fluctuations in African surface waters to variations in runoff and soil leaching between dry and wet periods [37]. Conversely, bacterial abundances, both of HAMB and Listeria, do not differ significantly between the two seasons; this is consistent with observations during other studies, where the presence of Listeria in surface waters remained constant regardless of seasonal rainfall cycles [8]. This bacterial stability in the face of highly fluctuating water chemistry confirms that the environmental survival of Listeria depends more on the availability of organic matter and the protection afforded by biofilms than on the seasonal physicochemical parameters themselves.

5. CONCLUSION

Bacteriological analysis revealed widespread contamination of sampling sites by HAMB bacteria and Listeria, with higher abundance in wells than in lake water, reflecting the impact of infiltration and contaminated runoff. The ubiquitous nature of Listeria and its remarkable ability to adapt to environmental stressors could explain its persistence and the observed seasonal variations. These results confirm that the survival and proliferation of this pathogen depend more on the availability of favourable environmental conditions. The physicochemical parameters analyzed, specifically pH and electrical conductivity, revealed potability standards and requirements for aquatic life, although they reflected the combined influence of natural and anthropogenic processes. Given these findings, regular water quality monitoring and measures to manage pollution sources are essential to limit health risks associated with Listeria exposure in drinking and environmental waters in Yaounde (Cameroon).

Acknowledgment

We thank the University of Yaounde I for the laboratory equipment. We also thank our colleagues and fellow students who facilitated the implementation of this work, particularly during data collection.

Informed consent statement

No informed consent was required to conduct the study.

Ethical approval

No ethical approval was required to conduct this study

Declaration of interests

The authors declare no conflict of interest.

Authors’ contribution

Conceptualization: Geneviève Bricheux, Télesphore Sime-Ngando, Moïse Nola; Data collection: Paule J. Atou’ou; Pélagie Ladibé, Yves Poutoum Yogne; Data analysis: Paule J. Atou’ou, Yves Poutoum Yogne, Moïse Nola; Investigation: Télesphore Sime-Ngando, Moïse Nola, Philippe Bouchard; Methodology: Paule J. Atou’ou, Yves Poutoum Yogne, Florence Donnadieu-Bernard; General supervision: Moïse Nola, Télesphore Sime-Ngando and Moïse Nola; Writing original draft: Paule J. Atou’ou, Moïse Nola and Philippe Bouchard; Writing-review editing: Geneviève Bricheux, Moïse Nola and Télesphore Sime-Ngando. All authors agreed to submit final version of the manuscript.

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