Comparative day/night metatranscriptomic analysis of microbial ...
Comparative day/night metatranscriptomic analysis of microbial ...
Comparative day/night metatranscriptomic analysis of microbial ...
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general may be a relatively more important metabolic<br />
activity in the <strong>night</strong>. Prochlorococcus marinus has recently<br />
been shown to exhibit diel patterns <strong>of</strong> amino acid uptake,<br />
with acquisition occurring predominantly at dusk (Mary<br />
et al., 2008). Our data agree with this and further suggest<br />
that heterotrophic taxa also devote a greater percentage<br />
<strong>of</strong> their transcriptome to transporting and synthesizing<br />
amino acids at <strong>night</strong>. Night-time accumulation <strong>of</strong> amino<br />
acids might be a mechanism for nitrogen storage by many<br />
organisms, particularly for P. marinus, which undergoes<br />
cell division at <strong>night</strong>. Histidine, the amino acid with the<br />
most consistent signal for synthesis at <strong>night</strong> by both<br />
autotrophs and heterotrophs (Fig. 7A and Fig. S1), is one<br />
<strong>of</strong> the most nitrogen-rich amino acids (only arginine has<br />
more amino groups).<br />
Overall, bacterial community investment in this oligotrophic<br />
ocean system was skewed towards energy<br />
acquisition and metabolism during the <strong>day</strong>, while biosynthesis<br />
(specifically <strong>of</strong> membranes, amino acids and vitamins)<br />
received relatively greater investments at <strong>night</strong>.<br />
Many <strong>microbial</strong> processes expected to be differentially<br />
expressed over a <strong>day</strong>/<strong>night</strong> cycle, such as photosynthesis,<br />
oxidative phosphorylation and proteorhodopsin activity,<br />
were indeed captured in the sequence data. Less<br />
anticipated processes that emerged included the utilization<br />
<strong>of</strong> C1 compounds, the uptake <strong>of</strong> polyamines and the<br />
degradation <strong>of</strong> aromatic compounds (Table 3). Other<br />
metabolic processes ongoing in this <strong>microbial</strong> community,<br />
although without statistical evidence for <strong>day</strong>/<strong>night</strong> patterns,<br />
included: use <strong>of</strong> nitrate and urea as nitrogen<br />
sources; use <strong>of</strong> phosphate, phosphonate and carbonoxygen-phosphorus<br />
(C-O-P) compounds as phosphorus<br />
sources; oxidation <strong>of</strong> reduced sulphur compounds; oxidation<br />
<strong>of</strong> carbon monoxide; and uptake <strong>of</strong> multiple trace<br />
metals (Table 3). This comparative <strong>analysis</strong> <strong>of</strong> <strong>microbial</strong><br />
community transcripts has provided an inventory <strong>of</strong><br />
ongoing metabolic processes, <strong>of</strong>fered insights into their<br />
temporal patterns and supplied a new type <strong>of</strong> data for<br />
predictive modelling <strong>of</strong> environmental controls on ecosystem<br />
properties.<br />
Experimental procedures<br />
Sample collection<br />
Samples were collected at the Hawaiian Ocean Time-series<br />
(HOT) Station ALOHA, defined by the 6-nautical-mile radius<br />
circle centred at 22°45′N, 158°W in November, 2005 (HOT-<br />
175). For RNA extraction, sea water was collected from a<br />
depth <strong>of</strong> 25 m using Niskin bottles on a conductivitytemperature-depth<br />
rosette sampler. A <strong>night</strong> sample was collected<br />
at 03:00 on 11 November 2005, and a <strong>day</strong>time<br />
sample was collected at 13:00 on 13 November 2005.<br />
During HOT-175, the peak PAR level was at 12:00, with<br />
sunrise occurring around 07:00 and sunset just before<br />
18:00. Sea water (80 l for the <strong>night</strong> sample and 40 l for the<br />
<strong>Comparative</strong> Metatranscriptomic Analysis 1371<br />
<strong>day</strong> sample) was prefiltered through a 5 mm, 142 mm polycarbonate<br />
filter (GE Osmonics, Minnetonka, MN) followed<br />
by a 0.2 mm, 142 mm Durapore (Millipore) filter using<br />
positive air pressure. The 0.2 mm filters were placed in a<br />
15 ml tube containing 2 ml Buffer RLT (containing<br />
b-mercaptoethanol) from the RNeasy kit (Qiagen, Valencia,<br />
CA) and flash-frozen in liquid nitrogen for RNA extraction.<br />
For DNA extraction, an additional 20 l <strong>of</strong> sea water were<br />
simultaneously filtered using the protocol outlined above at<br />
both time points. The 0.2 mm filters were placed in Whirlpack<br />
bags and flash-frozen. The total sampling time from initiation<br />
<strong>of</strong> collection until freezing in liquid nitrogen was approximately<br />
1.5 h. We obtained ~1 mg <strong>of</strong> total RNA from 40 to 80 l<br />
<strong>of</strong> sea water. Following mRNA enrichment and amplification,<br />
30–100 mg <strong>of</strong> mRNA was available for conversion to cDNA<br />
for sequencing. Typically, only 3–5 mg <strong>of</strong> DNA was required<br />
for pyrosequencing.<br />
RNA and DNA preparation<br />
DNA was extracted using a phenol : chlor<strong>of</strong>orm-based protocol<br />
(Fuhrman et al., 1988). Briefly, frozen filters inside Whirlpak<br />
bags were transferred to 50 ml Falcon centrifuge tubes.<br />
Ten millilitre extraction buffer [SDS (10% Sodium Doecyl<br />
Sulphate) : STE (100 mM NaCl, 10 mM Tris, 1 mM EDTA),<br />
9:1] was added to the tubes and boiled in a water bath for<br />
5 min. The extraction buffer was then removed from the<br />
tubes, placed into Oak Ridge round-bottom centrifuge tubes,<br />
to which 3 ml NaOAc and 28 ml 100% EtOH were added.<br />
Organic macromolecules were precipitated over<strong>night</strong> at<br />
-20°C, before the tubes were centrifuged for 1 h at 15 000 g.<br />
The supernatant was decanted, and pellets dried for 30 min<br />
in the air. The pellets were resuspended in 600 ml deionized<br />
water, and sequentially extracted with 500 ml phenol, 500 ml<br />
phenol : chlor<strong>of</strong>orm : isoamyl alcohol (24:1:0.1), and 500 ml<br />
chlor<strong>of</strong>orm:isoamyl alcohol (9:1); after each extraction the<br />
organic phase was removed and discarded. The supernatant<br />
was removed into a fresh tube at the end <strong>of</strong> last extraction,<br />
amended with 150 ml NaOAc and 1.2 ml 100% EtOH, and<br />
precipitated over<strong>night</strong>. The tube contents were then centrifuged<br />
at 15 000 g for 1 h, the supernatant decanted, and<br />
pellets dried in a speed vacuum dryer for 10 min. The DNA<br />
pellets were resuspended in 100 ml DNAse and RNAse-free<br />
deionized water (Ambion).<br />
RNA was extracted using a modified version <strong>of</strong> the RNeasy<br />
kit (Qiagen) that results in high RNA yields from material on<br />
polycarbonate filters (Poretsky et al., 2008). Frozen samples<br />
were first thawed slightly for 2 min in a 40–50°C water bath<br />
and then vortexed for 10 min with RNase-free beads from the<br />
Mo-Bio RNA PowerSoil kit (Carlsbad, CA). Following centrifugation<br />
for 5 min at 3000–5000 g, the supernatant was transferred<br />
to a new tube. Beginning with the RNeasy Midi kit,<br />
1 vol. <strong>of</strong> 70% ethanol was added to the lysate and, in order to<br />
shear large-molecular-weight nucleic acids, the lysate was<br />
drawn through a 22-gauge needle several (~5) times. RNA<br />
extraction then continued with the RNeasy Mini kit according<br />
to the manufacturer’s instructions.<br />
Following extraction, RNA was treated with DNase using<br />
the TURBO DNA-free kit (Ambion, Austin, TX). Two methods<br />
were employed to rid the RNA samples <strong>of</strong> rRNA. The RNA<br />
was first treated enzymatically with the mRNA-ONLY<br />
© 2009 The Authors<br />
Journal compilation © 2009 Society for Applied Microbiology and Blackwell Publishing Ltd, Environmental Microbiology, 11, 1358–1375