A 37-KILODALTON GLYCOPROTEIN OF BABESIA DIVERGENS IS A MAJOR COMPONENT OF A PROTECTIVE FRACTION CONTAINING LOW-MOLECULAR-MASS CULTURE-DERIVED EXOANTIGENS
B. Carcy et al., A 37-KILODALTON GLYCOPROTEIN OF BABESIA DIVERGENS IS A MAJOR COMPONENT OF A PROTECTIVE FRACTION CONTAINING LOW-MOLECULAR-MASS CULTURE-DERIVED EXOANTIGENS, Infection and immunity, 63(3), 1995, pp. 811-817
The supernatants of in vitro cultures of Babesia divergens Rouen 1987
in human erythrocytes, obtained by using a semidefined medium based on
human high-density lipoproteins, were fractionated by get filtration
chromatography into four fractions, F-1 to F-4. The crude supernatant
as well as each fraction adjuvanted with Quil-A protected gerbils from
mortality due to a homologous infectious challenge. Analysis of the h
umoral response of the 10 protected gerbils with fraction F-4, contain
ing major proteins with molecular masses lower than 50 kDa, showed tha
t a few antigens (from 50 to 17 kDa) could be important candidates for
an improved vaccine against B. divergens babesiosis. As an immunodomi
nant response was directed against the 37-kDa antigen (Bd37) in two di
fferent B. divergens strains tested, a polyclonal antibody directed ag
ainst Bd37 was produced in a rabbit. In an immunofluorescence assay, t
he anti-Bd37 antiserum strongly labelled small internal vesicles of th
e merozoites and the cell surface was diffusely labelled after fixatio
n, whereas on live merozoites, this labelling was not observed, [H-3]g
lucosamine-radiolabelling experiments demonstrate that Bd37 is a glyco
protein. The Bd37 protein can also be labelled with [C-14]palmitate bu
t not with [H-3]myristic acid, In Triton X-114 temperature phase parti
tioning of B. divergens-infected erythrocyte extracts, Bd37 was exclus
ively found into the detergent phase, indicating that the palmitoylate
d Bd37 protein was in the membrane fraction. In the in vitro supernata
nt, the glycoprotein Bd37 was found in a nonpalmitoylated form, indica
ting excretion and/or release of the glycoprotein from the merozoite.