| Literature DB >> 22957115 |
Munirul Alam1, Atiqul Islam, Nurul A Bhuiyan, Niaz Rahim, Anowar Hossain, G Yeahia Khan, Dilruba Ahmed, Haruo Watanabe, Hidemasa Izumiya, Abu S G Faruque, Ali S Akanda, Shafiqul Islam, R Bradley Sack, Anwar Huq, Rita R Colwell, Alejandro Cravioto.
Abstract
Vibrio cholerae is an estuarine bacterium associated with a single peak of cholera (March-May) in coastal villages of Bangladesh. For an unknown reason, however, cholera occurs in a unique dual peak (March-May and September-November) pattern in the city of Dhaka that is bordered by a heavily polluted freshwater river system and flood embankment. In August 2007, extreme flooding was accompanied by an unusually severe diarrhea outbreak in Dhaka that resulted in a record high illness. This study was aimed to understand the unusual outbreak and if it was related to the circulation of a new V. cholerae clone. Nineteen V. cholerae isolated during the peak of the 2007 outbreak were subjected to extensive phenotypic and molecular analyses, including multi-locus genetic screening by polymerase chain reaction (PCR), sequence-typing of the ctxB gene, and pulsed-field gel electrophoresis (PFGE). Factors associated with the unusual incidence of cholera were determined and analysis of the disease severity was done. Overall, microbiological and molecular data confirmed that the hypervirulent V. cholerae was O1 biotype El Tor (ET) that possessed cholera toxin (CT) of the classical biotype. The PFGE (NotI) and dendrogram clustering confirmed that the strains were clonal and related to the pre-2007 variant ET from Dhaka and Matlab and resembled one of two distinct clones of the variant ET confirmed to be present in the estuarine ecosystem of Bangladesh. Results of the analyses of both diarrheal case data for three consecutive years (2006-2008) and regional hydroclimatology over three decades (1980-2009) clearly indicate that the pattern of cholera occurring in Dhaka, and not seen at other endemic sites, was associated with flood waters transmitting the infectious clone circulating via the fecal-oral route during and between the dual seasonal cholera peaks in Dhaka. Circular river systems and flood embankment likely facilitate transmission of infectious V. cholerae throughout the year that leads to both sudden and off-season outbreaks in the densely populated urban ecosystem of Dhaka. Clonal recycling of hybrid El Tor with increasing virulence in a changing climate and in a region with a growing urban population represents a serious public health concern for Bangladesh.Entities:
Keywords: Cholera; Vibrio cholerae; clonal transmission; dual peak; fecal-oral; flood; off-season
Year: 2011 PMID: 22957115 PMCID: PMC3426334 DOI: 10.3402/iee.v1i0.7273
Source DB: PubMed Journal: Infect Ecol Epidemiol ISSN: 2000-8686
Fig. 1Molecular fingerprinting analysis using pulsed-field gel electrophoresis (PFGE) of NotI-digested genomic DNA obtained from V. cholerae serogroup O1 biotype El Tor strains isolated during the peak of the Dhaka epidemic, 2007, and pre-existing V. cholerae hybrid El Tor strains isolated between 2004 and 2007 in Dhaka and Matlab, two inland (freshwater) cholera endemic sites located 50 km apart and Barisal, a cholera endemic coastal ecosystem of Bangladesh. The dendrogram was constructed using digital images of PFGE patterns and Dice similarity coefficient and UPGMA clustering methods.
Fig. 2Comparative yearly data showing weekly admissions of diarrheal patients to the ICDDR,B hospital in Dhaka (2006–2008) during the unusual flood-related diarrheal epidemic that broke out in August 2007. The graph shows number of cases per week, based on actual numbers of diarrheal patients admitted to the ICDDR,B hospital. Number of cases for 2008 are included up to the third week of August.
Phenotypic and molecular characteristics of Vibrio cholerae Ol strains isolated during the flood-related Dhaka epidemic in 2007 and V. cholerae O1 strains isolated between 2004 and 2007 in Dhaka and Matlab. V. cholerae O1 classical and El Tor strains were included as controls
| Sl. No. | Location | Strain ID# | Serotype |
|
|
|
|
| wbe 01 |
| CCA | PolyB |
|
|
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 1 | Dhaka | 117514 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 2 | Dhaka | 117583 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 3 | Dhaka | 117645 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 4 | Dhaka | 117644 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 5 | Dhaka | 117685 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 6 | Dhaka | 117773 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 7 | Dhaka | 117633 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 8 | Dhaka | 117911 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 9 | Dhaka | 117935 | OGET | − | − | − | − | − | + | + | + | R | 2 | Classical |
| 10 | Dhaka | 118012 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 11 | Dhaka | 118113 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 12 | Dhaka | 117793 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 13 | Dhaka | 117902 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 14 | Dhaka | 117750 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 15 | Dhaka | 117743 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 16 | Dhaka | 117677 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 17 | Dhaka | 117675 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 18 | Dhaka | 117875 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 19 | Dhaka | 117865 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 20 | Matlab | L01-511 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 21 | Matlab | L01-928 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 22 | Matlab | L01-1786 | INET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 23 | Matlab | L01-1642 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 24 | Matlab | L01-1773 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 25 | Matlab | L01-1782 | OGET | + | + | − | + | + | + | + | + | R | 2 | Classical |
| 26 | 569B | CL Control. | + | + | + | − | + | + | + | − | S | 1 | Classical | |
| 27 | N16961 | ET Control. | + | + | − | + | + | + | + | + | R | 2 | ElTor |
Cca, chicken cell agglutination; Poly B, polymixixn B; R, resistant; S, sensitive; ET, El Tor; CL, classical; IN, Inaba; OG, Ogawa; ctxB type was confirmed by MAMA-PCR followed by DNA sequencing and analysis.
Fig. 3Map of Dhaka city showing the circular river systems along its border that receive the sewage effluent of nearly 15 million inhabitants. The city has an extensive, but not fully effective, sewage network linked to ponds, lakes, and canals that flow into the surrounding river systems. The circular arrows at the center indicate clonal recycling of V. cholerae in Dhaka, a fresh-water ecosystem situated 250 km distant from the estuarine ecosystem of the Bay of Bengal, Bangladesh. Unlike the estuarine ecosystem, where V. cholerae comprises a portion of the autochthonous microflora (12) in association with plankton year round (13,14), the water bodies of Dhaka serve as a constant source of highly transmissible V. cholerae. During extreme climatic conditions such as flooding in the poor urban setting of Dhaka, fecal-oral transmission is enhanced leading to significant off-season outbreaks, as occurred during flooding in 2007 in Dhaka. Flooding churns the waters, bringing sediment and V. cholerae biofilm attached to particulates into the surface water, thereby enriching the V. cholerae population.
Fig. 4(A) Climatological analysis of Bangladesh monsoon precipitation for 1980–2009 shows the relative magnitude of combined monsoon (JJAS: June–September) rainfall in 2007. The normalized anomaly values indicate 2007 was not a record year. (B) However, anomaly analysis of monthly rainfall shows that July 2007 was the highest monthly amount (for July) recorded for the Brahmaputra catchment areas in 30 years. In addition, the Ganges catchment areas also experienced very heavy rainfall in July 2007, as shown by the anomaly calculated against the 30 year base period (1980–2009).