Abstract
Polynucleotide sequence relationships between two reference Vibrio parahaemolyticus strains isolated from Japanese and American gastroenteritis patients were investigated by use of (32)P-DNA/DNA reassociation in free solution. In addition, these strains were similarly compared with 22 other strains of estuarine and marine vibrios, including 11 strains previously identified as V. parahaemolyticus (2 Japanese, 1 of unknown location, and 8 American strains obtained from diverse geographical locations and sources in North America), 3 strains of V. alginolyticus, and 8 of Vibrio spp. Deoxyribonucleic acid (DNA) from the Japanese and American gastroenteritis isolates showed high relative levels of intraspecific duplex formation (92 to 93%) when reassociated, reciprocally, at 60 C. Heterologous DNA duplexes exhibited thermal elution midpoint [Tm(e)] values comparable to those obtained from homologous duplexes (88.0) when thermally eluted from hydroxyapatite, thus indicating high base-pair complementarity. Other V. parahaemolyticus strains showed DNA homologies of 85% or greater, with correspondingly high Tm(e) values (86.0 to 88.0) for the heteroduplexes formed. DNA of two of three V. alginolyticus strains (ATCC 17749 and 166-70) was 55 to 60% homologous to reference V. parahaemolyticus DNA preparations; Vibrio sp. strain 5144 (originally classified as V. parahaemolyticus biotype 2 and subsequently as V. alginolyticus strain 5144) showed only 24 to 26% DNA homology to the same reference DNA. These data provide evidence that Vibrio sp. strain 5144 is genetically distinct from the other V. alginolyticus strains used in this study. Three bioluminescent strains thought to be closely related to V. parahaemolyticus demonstrated only 24 to 31% DNA homology to the reference V. parahaemolyticus DNA. These data firmly establish the existence in some Atlantic and Gulf Coast estuaries of organisms genetically very similar to V. parahaemolyticus, the causative agent of "shirasu" food poisoning in Japan.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
