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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

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