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Appl Environ Microbiol, March 1998, p. 1066-1069, Vol. 64, No. 3
0099-2240/98/$04.00+0
Copyright © 1998, American Society for Microbiology. All rights reserved.
Ultradian Growth in
Prochlorococcus spp.
Alexi
Shalapyonok,
Robert J.
Olson,* and
Ludmila S.
Shalapyonok
Woods Hole Oceanographic Institution, Woods
Hole, Massachusetts 02543
Received 16 October 1997/Accepted 7 January 1998
 |
ABSTRACT |
Species of the widespread marine prokaryote
Prochlorococcus exhibited ultradian growth (faster than 1 division per day) both in situ and in culture, even though cell
division is strictly phased to the light-dark cycle. Under optimal
conditions a second DNA replication and cell division closely followed,
but did not overlap with, the first division. The timing of cell cycle
events was not affected by light intensity or duration, suggesting
control by a light-triggered timer or circadian clock rather than by
completion of a light-dependent assimilation phase. This mode of
ultradian growth has not been observed previously and poses new
questions about the regulation of cellular rhythms in prokaryotes. In
addition, it implies that conclusions regarding the lack of nutrient
limitation of Prochlorococcus in the open ocean, which were
based on the appearance that cells were growing at their maximal rate,
need to be reconsidered.
 |
INTRODUCTION |
Species of
Prochlorococcus, the smallest known photosynthetic
organism, account for a significant fraction of the autotrophic biomass and primary production in mid- and low-latitude oceans (3,
7, 17, 18, 23, 27). The cell cycle of Prochlorococcus is tightly phased to the light-dark cycle, with DNA replication during
the afternoon, followed by binary fission after dusk (18, 24,
27). This division pattern, coupled with the unique light scattering and fluorescence signature of these cells, allows
oceanographers to estimate the growth rate of
Prochlorococcus, by using flow cytometry to monitor DNA
frequency distributions in situ over the diel cycle. Such measurements
are attractive because, in addition to singling out a specific
organism, they provide information on the details of division patterns
as well as the overall rate, and they avoid incubation artifacts.
Prochlorococcus follows the slow-growth mode of the
prokaryotic cell cycle paradigm (10); DNA distributions
reveal peaks corresponding to either one or two genome copies, implying
that DNA replication rounds do not overlap. This has led to the use of
the terms usually reserved for the eukaryotic cell cycle
(G1, S, and G2 phases) to identify cells
according to their DNA content (see, e.g., references 2, 18,
24, and 27). The maximum growth rate of
Prochlorococcus is not yet well established. The tight
coupling of the cell cycle phasing to the light-dark cycle, with a
single division burst, suggested that Prochlorococcus could not grow faster than 1 division per day (div d
1), and
when slightly higher rates were computed from cell cycle analyses
(18, 27), they were attributed to uncertainties in estimating the duration of S plus G2 phases (a critical
parameter in the growth rate computation) or left unexplained. However, a few growth rate estimates from changes in cell numbers, in the highly
productive western Arabian Sea, have indicated that
Prochlorococcus can grow significantly faster than 1 doubling per day (25, 28). In addition, growth rates
slightly faster than 1 doubling per day have been observed in
laboratory cultures (21).
We used diel measurements of DNA frequency distributions to estimate
Prochlorococcus in situ growth rates, and to investigate the
underlying cell division patterns, in the northwestern Arabian Sea
during monsoon and intermonsoon seasons. Our observations indicated
growth rates exceeding 1 doubling per day and suggested that this
ultradian growth was occurring through a novel division pattern in
which some cells divided twice in rapid succession. These findings were
confirmed by subsequent laboratory culture studies.
 |
MATERIALS AND METHODS |
Prochlorococcus natural populations.
Seawater
samples were collected in 1995 as part of the U.S. Joint Global Ocean
Flux Study (Arabian Sea) aboard the R/V Thomas G. Thompson
at two locations in August (southwest monsoon, during a period of
intensive vertical mixing) and two locations in November (northeast
monsoon, with surface waters well stratified). Surface water was
sampled by using a conductivity-temperature-depth rosette and
supplemented by bucket sampling to obtain high-frequency samples (0.5 to 1.5 h) for at least 24 h. Seawater samples were fixed immediately in 0.1% glutaraldehyde for 10 min and were frozen in
liquid nitrogen until analysis in the laboratory.
Cultures.
Prochlorococcus strain MIT 9302 (nonaxenic)
was isolated from the Sargasso Sea and provided to us by Lisa Moore,
Massachusetts Institute of Technology. Strain AS 9601 (nonaxenic) was
isolated from a water sample collected at 50 m in November 1995 in
the Arabian Sea (19°12'N, 67°10'E). Batch cultures were maintained in modified K/10(
Cu) medium (6), enriched with 100 µM
urea, 10 nM NiSO4, and 1 nM CuSO4, in 50-ml
culture tubes at 26°C under cool white fluorescent lamps.
Laboratory experiments.
Semicontinuous batch cultures were
acclimated to experimental light conditions for at least 3 weeks before
data were collected. Transfers to fresh medium were made every 4th day
before noon to keep the cultures in the exponential-growth phase. In
vivo chlorophyll fluorescence was monitored at noon daily. Light
intensities were measured with a Biospherical Instruments QSL-100
quantum scalar irradiance meter. Samples were taken every hour during the morning and late night and every 0.5 h during the afternoon and evening, when DNA replication and division occurred. Staining and
flow-cytometric analysis were performed immediately without fixation or
freezing.
Sample preparation and staining.
Experimental samples were
diluted 10- or 20-fold with filtered seawater before staining. Diluted
samples and thawed seawater samples were stained 15 to 25 min at room
temperature in the dark with the DNA-specific fluorochrome Hoechst
33342 (Sigma) at a final concentration of 1 µg/ml (2, 20).
Flow cytometry.
Following the addition of 0.57-µm-diameter
fluorescent beads (Polysciences, Inc.), stained samples were analyzed
with a single-beam Coulter EPICS-753 flow cytometer modified for high
sensitivity (23). An argon ion laser (Coherent, Inc.)
provided 250-mW UV (365 nm) excitation. Forward light scattering,
right-angle light scattering, and red, orange, and blue fluorescence
data were collected and analyzed as described previously
(27). Prochlorococcus cells were discriminated
from bacteria, cyanobacteria, and picoeukaryotes according to their
light-scattering and fluorescence characteristics (23). DNA
frequency distributions were analyzed with MCYCLE software (Phoenix
Flow Systems) in order to obtain cell fractions in G1, S,
and G2 phases.
Growth rate computations.
In situ specific growth rates
based on DNA distributions (µDNA, per day) were computed
as described previously (18, 27), based on the equation
(4, 19)
|
(1)
|
where n is the number of samples taken during the
24-h period, tS+G2 is the combined duration of S
and G2 phases, and fS+G2(i) is the
fraction of cells in S plus G2 for sample i. Our
computations of tS+G2 as twice the distance
between the peak of cells in S and the peak of cells in G2
yielded surprisingly low values of 2 to 3 h compared to the
previous 6-h (18, 27) or 4.5-h (24) estimates.
Therefore, we also estimated this duration as the time between the
appearance of the first S cells and that of the first newborn cells.
This approach yielded values of 3 to 4.5 h. We used the most
conservative estimate of 4.5 h for all calculations; using shorter
estimates of S plus G2 duration would result in
proportionally higher growth rates. Specific growth rates (µ, per
day) were converted to division rates (number of divisions per day) by
dividing by the natural logarithm of 2.
In situ specific growth rates based on cell numbers
(µcell, per day) were estimated as the difference between
observed cell abundances at the beginning and the end of division,
corrected for mortality rate (m, per day), as follows:
|
(2)
|
where Na is the cell number when division
is complete (at ta [see Fig. 1]),
Nb is the cell number just before the first
division occurred (at tb), and m is
the total mortality rate (per day) due to grazing and other losses. We
estimated m for the time period when
Prochlorococcus does not divide and computed it for 24 h (assuming m to be constant over the entire day) as
|
(3)
|
where N0 is the cell number at the
beginning of the period without division (at
t0), and tb
t0 is the duration of this period.
Since the mortality rate was negligible during laboratory experiments,
the specific growth rate was computed directly from cell numbers as
|
(4)
|
 |
RESULTS AND DISCUSSION |
Phasing of cell cycle events in situ was remarkably tight, as
observed in previous studies in the equatorial Pacific (18, 27) and tropical Atlantic (24); more than 95% of the
cells entered the DNA replication phase S early in the afternoon. The cells progressed through S phase in about 3 h and began dividing shortly before dusk (Fig. 1). DNA
distributions at 1435, 1635, and 1740 demonstrate a cohort of cells
entering, progressing through, and completing DNA replication,
respectively. By 1740 some cells had already divided, as evident from
the newly enlarged G1 peak; some of these cells apparently
then entered DNA replication again, widening the G1 peak to
the right. Progression of this smaller cohort through S phase is
reflected in distributions at 1900 to 2115 and resulted in a second
peak in the fraction of cells in G2 at 2115. All the cells
divided by 0300.

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FIG. 1.
Prochlorococcus division pattern in situ (22 to 23 July 1995; 19°10'N, 67°10'E). (A) Cell concentrations and
percentage of cells in G1 and G2 phases;
t0, ta, and
tb are the timing points used for growth rate
calculations (equations 2 and 3). (B) DNA frequency distributions for
selected samples (indicated by dashed lines) during the period of DNA
replication and cell division. At other time points only G1
cells were present. Ticks on the x axis mark the origin for
each distribution.
|
|
This second wave of division, which has not previously been observed,
could in these natural samples result from two populations of cells
with different temporal patterns of DNA replication. The division rate
estimates, however, suggest rather that some of the cells divided twice
in rapid succession: computations of growth rate from DNA distributions
(equation 1) yielded rates well in excess of 1 div d
1
(mean = 1.42 div d
1; standard deviation [SD] = 0.09) at all four locations where high-frequency diel sampling was
performed.
Independent estimates of division rates were made from observations of
changes in in situ cell concentrations over the diel cycle, corrected
for cell losses (equations 2 and 3). These values were similar in
magnitude (mean = 1.34 div d
1; SD = 0.36) to
the cell cycle-based values, though more variable. Our assumption of
constant mortality over the diel cycle may have resulted in
underestimation of the true growth rates, since some observations have
suggested that grazing on Prochlorococcus is highest at
night (18), when the cells are dividing. Even if we assumed
grazing to be zero during the division period, however, the cell number
data indicate growth rates in excess of 1 div d
1.
These data, though suggestive, are subject to uncertainty because of
the necessary assumptions about population homogeneity, S plus
G2 phase durations, and mortality rates in the field.
Therefore, we carried out similar diel experiments using cultures
isolated from the Sargasso Sea (MIT 9302) and the Arabian Sea (AS
9601), in which samples could be taken with higher time resolution, and in which growth rates could be precisely determined by direct cell
counts. The results of these measurements serve to confirm and clarify
the field observations.
On a light-dark cycle similar to that of the field studies (13 h of
light and 11 h of darkness), both Prochlorococcus isolates grew at rates well in excess of 1 div d
1 over a wide
range of light intensities (Table 1). The
pattern of cell cycle events was virtually the same at all light
intensities. The first cells entered S phase 6 h after the onset
of light and G2 phase about 4 h later, with newborn
cells appearing about 2 h afterward (1 h before the lights went
off) (Fig. 2, DNA distributions at 1100 to 1800). These observations are in general agreement with those for
natural populations (18, 24, 27) (Fig. 1), although the
durations of S and G2 phases were longer in culture. At
light intensities of 40 microeinsteins m
2
s
1 and higher, however, a second cohort of cells could
clearly be seen in S phase by 2000 (Fig. 2B). These cells reached
G2 phase by 2300 and divided before the end of the dark
period. The fact that the division rate was significantly higher than 1 div d
1 (Table 1) indicated that the second wave
constituted division of newly released daughter cells rather than a
delayed division of some of the cells. When the division rate was less
than 1 div d
1 (i.e., not all the cells divided), the
second wave was absent (MIT 9302 at 30 microeinsteins
m
2 s
1 [Fig.
3]). The second wave of division
differed from the first in the smaller number of cells involved (at
most, only about one-third of the cells divided twice [Table 1]) and
in the dramatically reduced duration of the G1 phase. The
time gap between the release of the first newborn cells and the
beginning of the second S phase suggests that G1 phase for
some cells in the second division is less than 1 h.

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FIG. 2.
Prochlorococcus strain MIT 9302 division
pattern in laboratory culture on a light-dark cycle (light intensity,
120 microeinsteins m 2 s 1). (A) Cell
concentrations and percentage of cells in G1 and
G2 phases. Symbols are as explained for Fig. 1. (B) DNA
frequency distributions for selected samples (indicated by dashed
lines).
|
|

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FIG. 3.
DNA frequency distributions of
Prochlorococcus strain MIT 9302 at 1800 to 2100 at division
rates of 0.69 div d 1 (30 microeinsteins m 2
s 1) (A) and 1.34 div d 1 (120 microeinsteins
m 2 s 1) (B). Note that when the division
rate is less than 1 div d 1 (panel A), there is no sign of
new G1 cells entering S phase, in contrast to the clearly
visible cohort of cells reentering S phase during ultradian growth
(panel B).
|
|
In two experiments in which the light period was longer than 13 h,
all cell cycle events (including the second wave) occurred at the same
time as in the shorter light regimens with respect to the onset of
light intensity (data not shown). This, together with the lack of
dependence of event timing on light intensity, suggests control of cell
cycle events by a light-triggered timer or the recently demonstrated
prokaryotic circadian clock (14, 15, 22) rather than by
completion of a light-dependent assimilation phase. When the light
period was longer, more cells completed division before darkness, and
more cells divided twice, even when the total amount of light received
was lower (Table 1), suggesting that a newborn cell must experience
some light to divide.
The strict timing of both DNA replication and cell division events and
the very short G1 phase before a second division makes Prochlorococcus quite different from other phytoplankton.
The closest known relative of Prochlorococcus, the
cyanobacterium Synechococcus spp., can grow much faster than
1 div d
1 but has continuous DNA replication and cell
divisions occurring all through the day and into the night (1,
22). Ultradian growth in many centric diatoms and in the
coccolithophore Hymenomonas carterae is characterized by the
presence of some dividing cells at all times of the day and night, and
the peaks in cell division rate are separated by about 12 h
(5, 8). The freshwater chlorophytes Chlamydomonas
spp. and Scenedesmus armatus carry out multiple mitoses
before dividing into four, eight, or more cells at once (9,
26). Another chlorophyte, Euglena gracilis, when grown
at high light intensity on a cycle of 14 h of light and 10 h
of darkness, exhibited phased ultradian growth, with cell division
confined to the dark period (12). Although
Euglena's DNA replication and cell division patterns under
ultradian growth conditions have not been studied, they might be
similar to those of Prochlorococcus.
Although the phased ultradian growth of Prochlorococcus is
the first such pattern to be observed in a marine species (as well as
the first observed in situ), it is probably not unique, and it may
represent a common mode of growth in natural communities of marine
phytoplankton. It is consistent with estimates by a variety of methods
of in situ division rates for the whole phytoplankton community being
faster than 1 div d
1 (13, 16), coupled with
recent observations that cell size in populations of pico- and
nanophytoplankton typically increases steadily over the day to reach a
maximum shortly before dusk (11). Such a division pattern
appears to combine the efficient use of daylight hours for
photosynthesis with the potential for maximum cell division during the
night (cells which have fixed enough carbon during the day may then
divide more than once).
Accurately measuring in situ growth rates by cell cycle analysis
requires high sampling frequency (hourly), since uncertainty in the
growth rate estimate is proportional to the error in estimated cell
cycle phase durations. Our observations of ultradian growth suggest
that the maximum achievable growth rate for Prochlorococcus has been underestimated in the past and complicate the use of this
organism as an indicator of environmental growth conditions. For
example, the conclusion that Prochlorococcus in the
equatorial Pacific Ocean is not nutrient limited, which was based on
the appearance that cells in situ were growing at their maximal rate (i.e., near 1 div d
1) (2, 18, 27), now appears
questionable.
 |
ACKNOWLEDGMENTS |
We thank chief scientists R. Barber and B. Balch and the
dedicated technical staff and crew of R/V Thomas G. Thompson
for their help during the cruises; L. Moore for providing
Prochlorococcus strain MIT 9302; and S. Chisholm, H. Sosik,
and J. Waterbury for critical reading of the manuscript.
This work was supported by National Science Foundation grant OCE
9311113.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Biology
Department, MS #32, Woods Hole Oceanographic Institution, Woods Hole,
MA 02543. Phone: (508) 289-2565. Fax: (508) 457-2169. E-mail:
rolson{at}whoi.edu.
 |
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Appl Environ Microbiol, March 1998, p. 1066-1069, Vol. 64, No. 3
0099-2240/98/$04.00+0
Copyright © 1998, American Society for Microbiology. All rights reserved.
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