HR: 16:45h
AN: B14A-04 [Abstracts]
TI: Using Small Subunit Ribosomal RNA to Follow Dark Incorporation of 14C-bicarbonate by Bacteria and Archaea in Sandy Sediment
AU: * MacGregor, B J
EM: bmacgreg@unc.edu
AF: Department of Marine Sciences
Univ. of North Carolina - Chapel Hill, CB#3300
349 Chapman Hall, Chapel Hill, NC 27599, United States
AU: Musat, N
EM: nmusat@mpi-bremen.de
AF: Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, Bremen, D-28359, Germany
AU: Kuypers, M M
EM: mkuypers@mpi-bremen.de
AF: Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, Bremen, D-28359, Germany
AB:
Small subunit ribosomal RNA (SSU rRNA) and the genes encoding it have become the basis of modern
microbial phylogeny, and of numerous methods for characterizing the composition of bacterial, archaeal, and
even eukaryotic communities as they occur in nature. A limitation of this approach has been that phylogeny alone
is not a reliable guide to physiology, particularly for groups with no close relatives in culture.
We have been developing ways of using the SSU rRNA molecule itself to identify and (eventually) quantify the
carbon sources incorporated by particular phylogenetic groups. This can be done by taking advantage of natural
variations in carbon isotopic composition among growth substrates, or by following incorporation of 13C- or
14C-labeled compounds. 14C has the advantage that natural background levels are negligible.
In the present study, our goal is to identify species responsible for non-photosynthetic CO2 incorporation in
sandy sediments of the German Wadden Sea. Sediment cores collected from the Janssand sand flats were
percolated with 14C-bicarbonate at in situ temperature for 36-38h in the dark, total RNA isolated, and
domain-specific oligonucleotide probes used to capture bacterial and archaeal SSU rRNA. Total and/or captured
RNA was separated by denaturing polyacrylamide gel electrophoresis, and 14C detected by phosphor
imager, autoradiography, or beta imager. Detection was fastest and most sensitive with the beta imager. Both
Bacteria and Archaea had incorporated label, suggesting both groups may harbor non-photosynthetic autotrophs.
The next step will be to use more specific capture probes.
We are currently working to separate the captured domain-specific SSU rRNA on non-denaturing gels, with
detection by the high-resolution mode of the beta imager, so that individual species incorporating label can be
identified by RT-PCR and sequencing of labeled bands.
DE: 0410 Biodiversity
DE: 0428 Carbon cycling (4806)
DE: 0442 Estuarine and nearshore processes (4235)
DE: 0452 Instruments and techniques
DE: 0465 Microbiology: ecology, physiology and genomics (4840)
SC: Biogeosciences [B]
MN: 2007 Fall Meeting