Location
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Leg-site
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Water depth (m)
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Depth (mbsf)
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Archaeal lineages (clone library %)
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References
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DSAG/MBG-B
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MG-I
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MGB-A
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MBG-D
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MCG
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SAGMEG
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TMEG
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UC-Iib
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Peru margin | 201-1229 | 150 | 6.7 | 4 | 4 | 88 | 4 | Parkes et al., 2005 | ||||
30.2 | 100 | |||||||||||
42 | 90 | 7 | ||||||||||
86.7 | 93 | 6 | ||||||||||
201-1227 | 427 | 1–151 | 6* | 2* | 3* | 48* | 38.6* | Inagaki et al., 2006 | ||||
Peru Trench | 201-1230 | 5086 | 1–278 | 41.6* | 50.7* | 1* | 1* | Inagaki et al., 2006 | ||||
Eastern equatorial Pacific | 201-1225 | 3760 | 1.5 | 44.4 | 37 | 14.8 | A. Lauer, unpubl. data | |||||
7.8 | 15.4 | 84.6 | ||||||||||
Peru Basin | 201-1231 | 4927 | 1.8 | 50 | 11 | 37 | Sørensen et al., 2004 | |||||
9 | 100 | |||||||||||
43 | 41 | |||||||||||
Okhotsk Sea† | NA | 1225 | 1–58 | 77 (in pelagic clay) | 6 (in pelagic clay) | 71(in ash layers) | 12 (in ash layers) | Inagaki et al., 2003 | ||||
Mediterranean sapropel‡ | NA | 2155 | 0.13–3.68 | 2.1* | 4.2* | 83.3*(58.3 in sapropel, plus 25.0 in sediment) | 8.3 | 2.1* | Coolen et al., 2002 | |||
Nankai Trough | NA | 945 | 165 | 86 | 14 | Reed et al., 2002 | ||||||
248 | 100 | |||||||||||
298 | 28.5 | 71 | ||||||||||
190-1173 | 4791 | 4.15 | 44.1 | 14.7 | 2.9 | 17.7 | 20.6 | Newberry et al., 2004 |
Notes: DSAG/MBG-B = Deep-Sea Archaeal Group, synonymous with Marine Benthic Group B (Vetriani et al., 1999) and Deep-Sea Hydrothermal Vent Crenarchaeotic Group (Takai and Horikoshi, 1999), MG-I = Marine Group I (DeLong, 1992, 1998), MBG-A = Marine Benthic Group A (Vetriani et al., 1999), MBG-D = Marine Benthic Group D (Vetriani et al., 1999), MCG = Miscellaneous Crenarchaeotal Group (Takai et al., 2001), SAGMEG = South African Goldmine Euryarchaeotal Groups 1 and 2 (Takai et al., 2001), TMEG = Terrestrial Miscellaneous Euryarchaeotal Group (Takai et al., 2001), UC-IIb = Uncultured Chimney Group II (Schrenk et al., 2003). * = average of all depths. † = alternate layers of pelagic clay and volcanic ash, ‡ = alternate sediment and sapropel layers; see supplementary information in Coolen et al. (2002).