RNA from Lake Michigan sediment was hybridized with a DNA probe for ar
chaeal 16S rRNA. There was a peak of archaeal rRNA abundance in the ox
ic zone and another immediately below it. Six contributing species wer
e identified by PCR amplification of extracted DNA with primers specif
ic for archaeal rDNA: two related to Methanosarcina acetivorans and fo
ur related to marine crenarchaeotal sequences. rRNA quantification usi
ng a DNA probe specific for this crenarchaeotal assemblage showed it i
s most abundant in the oxic zone, where it accounts for about 10% of t
otal archaeal rRNA.