Microbiology and Immunology

(Axel Boer) #1
Magnetotactic bacteria WORLD OF MICROBIOLOGY AND IMMUNOLOGY

360


article’s significance, it was later hailed as the beginning of a
revolution that led to the formation of molecular biology as a
scientific discipline.
MacLeod married Elizabeth Randol in 1938; they even-
tually had one daughter. In 1941, MacLeod became a citizen
of the United States, and was appointed professor and chair-
man of the department of microbiology at the New York
University School of Medicine, a position he held until 1956.
At New York University he was instrumental in creating a
combined program in which research-oriented students could
acquire both an M.D. and a Ph.D. In 1956, he became profes-
sor of research medicine at the Medical School of the
University of Pennsylvania. MacLeod returned to New York
University in 1960 as professor of medicine and remained in
that position until 1966.
From the time the United States entered World War II
until the end of his life, MacLeod was a scientific advisor to
the federal government. In 1941, he became director of the
Commission on Pneumonia of the United States Army
Epidemiological Board. Following the unification of the mili-
tary services in 1949, he became president of the Armed
Forces Epidemiological Board and served in that post until


  1. In the late 1950s, MacLeod helped establish the Health
    Research Council for the City of New York and served as its
    chairman from 1960 to 1970. In 1963, President John F.
    Kennedy appointed him deputy director of the Office of
    Science and Technology in the Executive Office of the
    President; from this position he was responsible for many pro-
    gram and policy initiatives, most notably the United
    States/Japan Cooperative Program in the Medical Sciences.
    In 1966, MacLeod became vice-president for Medical
    Affairs of the Commonwealth Fund, a philanthropic organiza-
    tion. He was honored by election to the National Academy of
    Sciences, the American Philosophical Society, and the
    American Academy of Arts and Sciences. MacLeod was en
    route from the United States to Dacca, Bangladesh, to visit a
    cholera laboratory when he died in his sleep in a hotel at the
    London airport in 1972. In the Yearbook of the American
    Philosophical Society,Maclyn McCarty wrote of MacLeod’s
    influence on younger scientists, “His insistence on rigorous
    principles in scientific research was not enforced by stern dis-
    cipline but was conveyed with such good nature and patience
    that it was simply part of the spirit of investigation in his lab-
    oratory.”


See alsoBacteria and bacterial infection; Microbial genetics;
Pneumonia, bacterial and viral

MAD COW DISEASE•seeBSE ANDCJD DISEASE

MMagnetotactic bacteriaAGNETOTACTIC BACTERIA

Magnetotactic bacteriaare bacteria that use the magnetic field
of Earth to orient themselves. This phenomenon is known as
magnetotaxis. Magnetotaxis is another means by which bacte-

ria can actively respond to their environment. Response to
light (phototaxis) and chemical concentration (chemotaxis)
exist in other species of bacteria.
The first magnetotactic bacterium, Aquasprilla magne-
totactumwas discovered in 1975 by Richard Blakemore. This
organism, which is now called Magnetospirillum magneto-
tacticum, inhabits swampy water, where because of the
decomposition of organic matter, the oxygen content in the
water drops off sharply with increasing depth. The bacteria
were shown to use the magnetic field to align themselves. By
this behavior, they were able to position themselves at the
region in the water where oxygen was almost depleted, the
environment in which they grow best. For example, if the bac-
teria stray too far above or below the preferred zone of habi-
tation, they reverse their direction and swim back down or up
the lines of the magnetic field until they reach the preferred
oxygen concentration. The bacteria have flagella, which
enables them to actively move around in the water. Thus, the
sensory system used to detect oxygen concentration is coordi-
nated with the movement of the flagella.
Magnetic orientation is possible because the magnetic
North Pole points downward in the Northern Hemisphere. So,
magnetotactic bacteria that are aligned to the fields are also
pointing down. In the Northern Hemisphere, the bacteria
would move into oxygen-depleted water by moving north
along the field. In the Southern Hemisphere, the magnetic
North Pole points up and at an angle. So, in the Southern
Hemisphere, magnetotactic bacteria are south-seeking and
also point downward. At the equator, where the magnetic
North Pole is not oriented up or down, magnetotactic bacteria
from both hemispheres can be found.
Since the initial discovery in 1975, magnetotactic bac-
teria have been found in freshwater and salt water, and in oxy-
gen rich as well oxygen poor zones at depths ranging from the
near-surface to 2000 meters beneath the surface.
Magnetotactic bacteria can be spiral-shaped, rods and spheres.
In general, the majority of magnetotactic bacteria discovered
so far gather at the so-called oxic-anoxic transition zone; the
zone above which the oxygen content is high and below which
the oxygen content is essentially zero.
Magnetotaxis is possible because the bacteria contain
magnetically responsive particles inside. These particles are
composed of an iron-rich compound called magnetite, or var-
ious iron and sulfur containing compounds (ferrimagnetite
greigite, pyrrhotite, and pyrite). Typically, these compounds
are present as small spheres arranged in a single chain or sev-
eral chains (the maximum found so far is five) in the cyto-
plasmof each bacterium. The spheres are enclosed in a
membrane. This structure is known as a magnetosome. Since
many bacterial membranes selectively allow the movement of
molecules across them, magnetosome membranes may func-
tion to create a unique environment within the bacterial cyto-
plasm in which the magnetosome crystal can form. The
membranes may also be a means of extending the chain of
magnetosome, with a new magnetosome forming at the end of
the chain.
Magnetotactic bacteria may not inhabit just Earth.
Examination of a 4.5 billion-year-old Martian meteorite in

womi_M 5/7/03 7:52 AM Page 360

Free download pdf