R. Massana et al., VERTICAL-DISTRIBUTION AND TEMPORAL VARIATION OF MARINE PLANKTONIC ARCHAEA IN THE GERLACHE STRAIT, ANTARCTICA, DURING EARLY SPRING, Limnology and oceanography, 43(4), 1998, pp. 607-617
A station located in the Gerlache Strait (Antarctic Peninsula) was sam
pled during early spring to determine the vertical distribution of mar
ine planktonic archaea and to further describe the dynamic environment
where they live. Chlorophyll concentration indicated that sampling oc
curred during the early stages of austral spring algal development. As
expected, prokaryote abundance was higher at surface than at depth, a
nd prokaryotic activity estimated by leucine incorporation was low at
the surface and extremely low at 500 m. The relative abundance of plan
ktonic archaeal, eucaryal, and bacterial ribosomal RNA was determined
by quantitative rRNA hybridization, and the performance of two differe
nt universal probes used to normalize group-specific probe hybridizati
on response was compared. Archaeal rRNA was detected in all samples an
alyzed, and was more abundant at depth (up to 25% of total rRNA) than
at the surface. In both years, the archaeal signal decreased during th
e sampling period, particularly at surface. Most of the archaeal signa
l was attributable to group I archaea, affiliated with the kingdom Cre
narchaeota. Planktonic euryarchaeotes (group II archaea) showed a larg
er contribution to the archaeal assemblage in surface waters than at d
epth. In total, our results verify that planktonic archaea are dynamic
and abundant components in marine picoplankton assemblages of the Ant
arctic Peninsula.